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The largest deposits form what geologists call a terminal moraine.

The moraine that shaped the city was all but forgotten.

MORAINE, Ohio (Reuters) - Chinese auto supplier Fuyao Glass Industry Group (703.

Her remains were discovered in the backyard of her former boyfriend's Moraine home.

A major General Motors plant in Moraine closed in 2008, eliminating about 2,000 jobs.

Ohio Governor Mike DeWine said GM's announcement was good news for Parma, Moraine and Toledo.

In addition, the bluestones don&apost look like glacial debris, known as moraine, he said.

The terminal moraine, the mounds of rubble left behind, form much of their high ground.

Workers at the plant in Moraine, owned by Fuyao Glass, voted 868 to 444 against unionizing.

Americans in Moraine, Ohio are working again, thanks to an enormous new factory that opened last year.

The terminal moraine which marks its greatest extent forms a strip of high ground across the borough.

"She was left for 17 months and it becomes pretty much skeletal remains," Moraine Police Department Sgt.

The course is set on 723 acres, 35 miles northwest of Milwaukee, in the Kettle Moraine hills.

VICE News spoke with Fuyao's chairman and visited employees in Moraine, Ohio to discuss the company's growing pains.

A person briefed on the matter said GM will make investments in its Toledo, Parma and Moraine operations.

The suit was filed by a mother of two students at Kettle Moraine High School in Wales, Wis.

I decided to write a story and determine the best times for Manhattanites to view the Queens-Brooklyn moraine.

Another plant adding jobs in Toledo is 160 miles away, while a third in Moraine, is about 250 miles away.

For Moraine, that influx helped solve the city's cash flow problems, like paving roads, after the General Motors factory closed.

Kettle Moraine School District Superintendent Patricia Deklotz told WFRV Hay was hired as a business and marketing teacher in 2005.

The crisp blue water and mountain-filled landscape of Moraine Lake in Banff National Park are even more stunning in person.

The Moraine building Fuyao is using once was a GM assembly plant that at one time employed more than 6,000 people.

The biggest icebergs become lodged on the moraine and the smaller ones crowd in behind, as in a monumental traffic jam.

The suit against Kettle Moraine High School was filed Thursday and is currently awaiting further paperwork from the defense before proceeding.

Starting off with a bang, the OnePlus 7 Pro makes Lake Moraine in Banff, Canada, really pop compared to the Pixel 3 ...

GM also said on Wednesday it will invest $700 million and add 450 jobs at its Toledo, Parma and Moraine, Ohio, operations.

Separately, G.M. said it would invest $700 million in three other Ohio cities — Toledo, Parma and Moraine — creating about 450 manufacturing jobs.

So in the book I go to Moraine, Ohio, which is where — there was a large automobile plant, and the place was empty.

Moraine Lake in Alberta, Canada is a beautiful, picturesque scene: a crystal-clear lake surrounded by snow-touched mountains and green pine trees.

In recent times, the resulting moraine got much scrutiny from scientists because of its proximity to one of the nation's first big cities.

We motored on, dodging refrigerator-size blocks of floating ice as well as several massive icebergs that had broken free from the moraine.

A towering wave of destruction crashed down through the Hudson gorge and proceeded to smash the southern end of the local moraine to smithereens.

In all of New York City, "this is the only place you can see the moraine clearly," Mr. Horenstein said, leaning into the wind.

The center line of the glacier, known as the medial moraine, was strewn with boulders that had tumbled and drifted down from the peak.

The fountain in La Colonnade will be filled with moraine, granite that was ground to a fine silt by glaciers in the last ice age.

Suddenly, I realized that the faraway hill I had seen repeatedly was no ordinary hill but a terminal moraine — a relic of the last ice age.

Mr. Hay was a high school principal in the suburban Milwaukee district of Kettle Moraine for several years but left in 2011, citing differences with the superintendent.

At Fort Wadsworth, a historic battlement next to the Verrazano Bridge, we stood atop the moraine and looked across the Narrows, the strait between Staten Island and Brooklyn.

His collection also sheds light on how moraine study in general helped geologists in New York and elsewhere discover that the planet had experienced a series of ice ages.

Ahead of the ceremonial opening of the Moraine, Ohio plant on Friday, Fuyao Chairman Cho Tak Wong said Fuyao has started renovating an industrial building in Plymouth, Michigan, outside of Detroit.

The surrounding area, known as the Kettle Moraine, is a mass of rocks, sediment and debris deposited by glaciers, which is why Erin Hills, which opened in 2006, has such dramatic topography.

Ceo Dewang, the chairman of Fuyao — one of China's largest autoglass companies — chose Moraine for the factory, an old General Motors plant that left almost 1,100 people without jobs when it closed in 553.

Ceo Dewang, the chairman of Fuyao — one of China's largest autoglass companies — chose Moraine for the factory, an old General Motors plant that left almost 1,100 people without jobs when it closed in 2008.

In Moraine, workers complain of a strict attendance policy that punishes them for absences with legitimate explanations, like having a sick child, and of being criticized or disciplined by managers for offering constructive input.

If you are just a middle-aged dude with decent habits and one transcendent skill that you are burying under a moraine of Long John Silver's crispies, how long can you make it work?

Meet the Chinese billionaire who opened shop in Ohio Meet the Chinese billionaire who opened shop in Ohio Americans in Moraine, Ohio are working again, thanks to an enormous new factory that opened last year.

Watch more on Daily VICE: After the glaciers receded from the Pacific Northwest some 10,000 years ago, glacial moraine was left behind—basically a big pile of rocks and rubble, with scattered patches of soil.

The vote, which began on Wednesday, involves roughly 0003,500 workers at the Fuyao Glass Industry Group Co Ltd plant in Moraine, a Dayton suburb that was once home to a large, unionized General Motors Co assembly plant.

The vote, which began on Wednesday, involved roughly 1,500 workers at the Fuyao Glass Industry Group Co Ltd plant in Moraine, a Dayton suburb that was once home to a large, unionized General Motors Co assembly plant.

And here's a photo taken with an ultrawide lens on the OnePlus 7 Pro, where I capture more of the lake, sky, and surroundings in general of this absurdly beautiful place called Lake Moraine in Banff, Canada.

Whether an overgrown street grid in Edgemere, Queens, where the homes were torn down for a development that never arrived, or a ridge of glacial moraine jutting from Manhattan, Workman makes New York, and its rough edges, look beautiful.

The documentary traces the lives of thousands of workers laid off from their auto jobs in Moraine, Ohio, in the 2008 recession, some of whom were hired six years later by Chinese company Fuyao Glass America to make automotive glass in the same plant.

Fuyao, a Chinese automotive glass supplier whose global customers include General Motors Co, Ford Motor Co, Fiat Chrysler Automobiles NV, Daimler AG and Toyota Motor Corp, opened the plant in Moraine in 2016 as part of a broader $1 billion expansion in the United States.

Mr. Hay took a leave of absence from his job as a high school principal in the Kettle Moraine School District in suburban Milwaukee in late 2010, and left that job in early 2011, citing differences with the district's superintendent, according to the Milwaukee Journal Sentinel.

Two recent investments in the American auto industry by Chinese firms include Geely Auto's planned $500 million Volvo plant in in Ridgeville S.C., which it says will support 2,000 jobs, and Fuyao Glass Industry's recent acquisition of a shuttered GM plant in Moraine, Ohio, that will employ 2,500.

NORTH KOREAN DETAINEE HAS EMOTIONAL REUNION WITH FAMILY IN OHIO News that yet another American had been taken prisoner by the authoritarian dictatorship of Kim Jong Un quickly made its way back to the U.S., and the small, southern Ohio town of Moraine, where Fowle had worked for 26 years in the streets department.

A report by the National Committee on US-China Relations and the Rhodium Group found that Chinese companies directly employ more than 140,000 Americans, often in areas that were left behind by globalization -- such as in Moraine, Ohio, where Fuyao Glass Industry Group has created over 1,500 jobs in an abandoned General Motors plant.

Part of America's rural cemetery movement when burial grounds were moved out of crowded churchyards and designed to inspire reverence and contemplation, Green-Wood's 478 sylvan acres, sandwiched between the BQE and Prospect Expressway, are set on a terminal moraine deposited by receding glaciers that left behind a startling landscape of hills, dales, and glacial ponds.

MORAINE, Ohio — When a giant Chinese glassmaker arrived here in 2014 and began spending what would become more than a half-billion dollars to fix up an abandoned General Motors plant, it seemed like a tale from opposite land: The Chinese are supposedly stealing American jobs — as no less an authority than President Trump has pointed out.

Analog Matte #20163 (Moraine), 2016 Analog Matte #004 (Padre Island), 2015 Analog Matte #003 (McAllister), 2015 Analog Matte #017 (Many Parks), 2016 Analog Matte #008 (Great Sand Dunes), 2016 Analog Matte #0123 (Bear Lake), 2016 Analog Matte #015 (Granby), 2016 Analog Matte #2015 (Medano Creek), 22016 Analog Matte #2011 (Rattlesnake Canyon), 22016 Analog Matte #2005 (San Isabel), 22016 Analog Matte #20163 (Carlsbad), 22016 Analog Matte #2006 (Moraine), 22016 Analog Matte #004 (Padre Island), 2015 Analog Matte #003 (McAllister), 2015 Analog Matte #017 (Many Parks), 2016 Analog Matte #0063 (Great Sand Dunes), 2016 Analog Matte #016 (Bear Lake), 2016 Analog Matte #015 (Granby), 2016 Analog Matte #011 (Medano Creek), 2016 Analog Matte #005 (Rattlesnake Canyon), 2016 Analog Matte #012 (San Isabel), 2016 Analog Matte #006 (Carlsbad), 2016 Photoshop makes it easy for even casual photographers to create mesmerizing tricks of the eye.

I managed an afternoon at Glasto, and I was sweating profusely by the time I made it out of that terminal moraine of the counter-culture ––because really, puh-lease, that's what it is: In this greeny-brown and not entirely unpleasant ground, the spirit of rebellion and experimentation that the 1960s unleashed, finally curled up on its air-mattress and carried on glamping.

After the Valparaiso Moraine was formed, the glacier retreated and formed the Tinley Moraine. Many towns in northwest Indiana and northeast Illinois are named after the Valparaiso Moraine or the Tinley Moraine. Also, many small creeks or rivers start in the Valparaiso Moraine. The moraine itself was named after the city of Valparaiso, Indiana, where the moraine is narrower and higher than in other places.

Trending east towards Valparaiso, Indiana, the Tinley Moraine rejoins the Valparaiso Moraine near Wheeler, Indiana. From here, eastward, the remnant Tinley Moraine becomes mixed with the Lake Border Moraine. The Lake Border Morainic System is younger than the Tinley Moraine and dates from the Glenwood stage of glacial Lake Chicago. The Tinley Moraine is considered pre-Glenwood.

The Buffalo Lake Moraine, alternately, the McGregor Moraine, was left, in Alberta, by the retreat of the Laurentide Ice Sheet, North America's last glaciation. It is an example of a hummocky moraine. It is one of four north- south oriented hummocky moraines, in Alberta, the other three being the Duffield Moraine, the Viking Moraine and the Couteau Moraine. The moraine varied appearance is caused by material embedded within the glacier being left in a layer, as the glacier melted.

Tinley moraine, a glacial feature of Illinois & Indiana. Based on Publication 6876-12989-1-PB; The Tinley Moraine in Indiana; Allan F. Schneider; Indiana Geological Survey; Indianapolis, Indiana; undatedThe Tinley Moraine is a moraine around the Lake Michigan basin in North America. It was formed during the Wisconsin Glaciation and is younger than the higher and wider terminal moraine called the Valparaiso Moraine, which is located farther from the lake than the Tinley Moraine. Compared to the Valparaiso Moraine, the Tinley Moraine is much narrower and occupies a similar swath, about closer to Lake Michigan, and passes through the communities of Flossmoor, Western Springs, and Arlington Heights.

A Veiki moraine (Swedish: Veikimorän) is a type of moraine found in northern Sweden, Troms og Finnmark in Norway, and parts of Canada. This moraine is characterized by forming a hummocky landscape of irregular moraine plateaus with elevated rims that are intercalated with ponds. Gunnar Hoppe was the first to define the Veiki moraine concept in 1952, naming it after a locality consisting of two farms located about 10 kilometers north of Gällivare and Malmberget. To the east in Finnish Lapland, a moraine type similar to Veiki moraine but smaller is known as Pulju moraine since 1967.

The Valparaiso Moraine, located south of the Lacustrine Plain, is an arc-shaped moraine complex that parallels the southern shore of Lake Michigan. The moraine divides LaPorte County into northern and southern drainage areas. The area north drains into Lake Michigan; south of the moraine water drains to the Kankakee River. Numerous kettle lakes sit on the moraine.

The Oro Moraine is a glacial moraine in Simcoe County, Ontario, Canada. The moraine covers north of Barrie, Ontario. The moraine drains into Georgian Bay on Lake Huron, and the smaller Lake Simcoe. Water transporting layers within the moraine, composed of sand and gravel, are separated by relatively impervious aquitard layers composed of or silt or clay.

The Valparaiso Moraine is the dominant geologic form that created the various landscape forms of the Indiana Dunes about 40,000 YBP. Within the arc created by the Valparaiso Moraine are the two younger recessional moraines of the Tinley Moraine and the Lake Border Moraine. Each moraine created an artificial dam across the southern outflow of the melt waters of the receding glaciers.

A washboard moraine, also known as minor or corrugated moraine, is a geomorphic feature caused by glaciers. The name "washboard moraine" refers to the fact that, from the air, it resembles a washboard.

This ridge is later than the Bluffton moraine, and may be a westward continuation of the Rawson moraine.

Map of Long Island topography and the generalized glacial moraine locations. The Harbor Hill Moraine, in the geography of Long Island, forms the northern of two ridges along the "backbone" of Long Island.Geological Survey: Quaternary History of the New York Bight: retrieved 23 August 2013. The Harbor Hill Moraine, skirting the North Shore, represents the terminal moraine of the most recent advance of the Wisconsinian glaciation, which reached its most southward advance about 18,000 years ago; the earlier Ronkonkoma Moraine, much cut through by outwash streams from the Harbor Hill Moraine, lies to the southeast.

The Lake Erie basin has two moraines of the same age as the Valparaiso Moraine, the Mississinewa Moraine and the Union Moraine. These moraines formed from the Lake Erie Lobe of the continental glacier.[2] In Michigan the Kalamazoo Moraine is of the same time period. It is the result of the Saginaw lobe of the Laurentian glacier.

The "Highland Flutes" lie between the moraine and the lake; the "Toimi Drumlin Field" is on the far side of the moraine, just west of the highlands. The North Shore Highlands therefore are composed of mafic outcroppings and volcanic ridges along the lakeshore overlain in places by a ground moraine, and an inland glacial moraine paralleling that shoreline.

What is now the city of Moraine was once a part of Van Buren Township followed by a brief period as a part of Kettering. Citizens of the Moraine area seceded from Kettering forming the new Moraine Township in 1953, before incorporating as a municipality in 1957.About the City, City of Moraine, Ohio 2006. Accessed 2008-01-05.

This moraine forms the northern border of Devil's Lake.Devil's Lake State Park, Landmark Nature Trail; Baraboo, Wisconsin, 2008 The moraine is approximately thick.Devil's Lake State Park, West Bluff Self-Guide Tour; Baraboo, Wisconsin, 2008 Southeast Glacial Moraine is located between the East Bluff-South Face and the South Bluff. The Group Camp is located atop the moraine.

The moraine probably was named after the village of Tinley Park, a village southwest of Chicago that lies on the moraine. The Tinley Moraine is a secondary ridge north of the Valparaiso Morainic System. Mapping suggests, that the Lake Michigan Lobe probably receded northward of the Valparaiso Moraine and then advanced towards the Valparaiso Moraine to form the Tinley Moraine.Publication 6876-12989-1-PB; The Tinley Moraine in Indiana; Allan F. Schneider; Indiana Geological Survey; Indianapolis, Indiana; undated The Tinley Moraine begins as an offshoot of the Valparaiso Moraine in southern Lake County, Illinois in the kettle lake region around Lake Zurich and follows the eastern crest southward through Des Plaines, Illinois, and Argonne National Laboratory, where it is broken by the Chicago Sanitary and Ship Canal, then sweeping southeast towards Dyer, Indiana.

The northern moraine, which directly abuts the North Shore of Long Island at points, is known as the Harbor Hill moraine. The more southerly moraine, known as the Ronkonkoma moraine, forms the "backbone" of Long Island; it runs primarily through the very center of Long Island, roughly coinciding with the length of the Long Island Expressway. The land to the south of this moraine to the South Shore is the outwash plain of the last glacier.

Splash Moraine is an abandoned outdoor water park located in Moraine, Ohio (a suburb of Dayton, Ohio). It has been closed since 2009.

The Viking Moraine is one of four large moraines in Alberta, Canada. The moraine "contains pre-glacial lacustrine and glaciofluvial sediments, diamicton and in situ Cretaceous bedrock." The moraine runs generally north–south, until it turns east–west at approximately 52 degrees north.

The area north drains into Lake Michigan; south of the moraine water drains to the Kankakee River. Numerous kettle lakes sit on the moraine.

The northern portion of Plum Island is a recessional moraine deposit, part of the Harbor Hill- Roanoke Point-Fishers Island-Charlestown Moraine, and thus is one of the Outer Lands. Boulders in the moraine can be seen in the eroding northern slope of the island.

Moraine Airpark is a public-use airport situated in the city of Moraine, Ohio, United States. southwest of the city of Dayton in Montgomery County.

For example, an outwash plain from the Cary glacier may have a newer cover of ground moraine from the Mankato glacier, or a Cary ground moraine may have been subsequently covered over by Mankato outwash. The majority of lakes in the world are kettle lakes produced by glacial activity. In Minnesota, the majority of kettles lakes reside in ground moraine and terminal moraine areas.

The Moraine Park Amphitheater The Moraine Park Museum and Amphitheater, also known as the Moraine Park Lodge and the Moraine Park Visitor Center, are located in Moraine Park, a glaciated meadow between two moraines in Rocky Mountain National Park. The two structures were built to serve visitors to the park, and are listed on the National Register of Historic Places. The museum was built in 1923 by Imogene Green MacPherson as the center of her private tourist development, and was then known as the Moraine Park Lodge. The National Park Service purchased the property in 1931 and demolished the surrounding cabins in following years.

Research conducted in the 1990s revealed that the moraine has multiple origins: its eastern area has subglacial depositions (Gorrell and McCrae, 1993); early parts of the moraine were deposited in an esker (Brennand and Shaw, 1994); and that the moraine is not continuous, but is composed of multiple depositional environments: subglacial, ice-marginal and proglacial lacustrine (Barnett et al., 1998). Current research efforts on the moraine are quite extensive. Because of the political implications of development on the moraine, and because its aquifers are a source of potable water for numerous communities, both federal and provincial governments have invested resources towards research on the moraine.

The moraine is currently a contested site in Ontario, since it stands in the path of major urban development (see political action). The Oak Ridges Moraine.

A Veiki moraine is a kind of hummocky moraine that forms irregular landscapes of ponds and plateaus surrounded by banks. It forms from the irregular melting of ice covered with a thick layer of debris. Veiki moraine is common in northern Sweden and parts of Canada.

It is a nature reserve because of the large colony of puffin. To the south, the moraine of Raen stretches towards the village of Nykvåg. This moraine is the end moraine from a glacier ending in the sea here. This area is also a nature reserve.

Moraine Cove () is a small cove at the north end of Mikkelsen Bay along the west coast of Graham Land, Antarctica. A moraine descends to the cove from the southwest end of Pavie Ridge. The name derives from the provisional name "Moraine Point," used by Professor Robert L. Nichols of the Ronne Antarctic Research Expedition, who examined the geology of this area in 1947. The name Moraine Cove retains the spirit of the naming by Nichols, and is considered more essential for reference purposes than a name for the moraine itself.

This moraine was actually one of several moraines deposited by the four glaciations, which include Medial Moraine and Bridalveil Moraine. After the Tioga Glacier retreated this moraine formed a lake that flooded nearly the entire valley. Gradual sedimentation filled Lake Yosemite, creating a broad and flat valley floor. Sediments of glacial origin continued to travel down the Merced River following then, helping to form the flat floor of the Central Valley.

The Moraine View State Recreation Area is a state park operated by the Department of Natural Resources (DNR) of the U.S. state of Illinois. The 1,687 acre (6.7 km2) recreation area is located near Le Roy, Illinois. The predecessor of Moraine View, the McLean County Conservation Area, traces its history to 1959. The park was renamed Moraine View State Park in 1975, then Moraine View State Recreation Area in 1995.

Within the arc created by the Valparaiso Moraine are two younger Cary substage moraines of the Tinley Moraine and the Lake Border Moraine. Younger still is the Port Huron system, which occurs in the northern portion of the Lake Michigan Basin. The Cary substage dates to around 30,000 years before present.

Bulletin no. 104, Illinois State Geological Survey, Champaign, Illinois. During the glacial Woodfordian Substage (middle Wisconsin Stage), ice of the Lake Michigan Glacial Lobe advanced rapidly, leaving a terminal moraine parallel to the modern Sangamon River. The ice stagnated and melted behind this moraine, without the meltwater overtopping the terminal moraine.

Lake Barbazan, north-west of the village at 452 m above sea level, is of glacial origin. It is surrounded by moraine deposits: sub-glacial moraine from Cumania and rocky outcrops of moraine west of the Lake. The Ruisseau de Corp flows west from the lake to join the Garonne.

Running parallel, the Mississinewa is renamed as the Broadway and Powel moraines in Hardin County. The St. Johns moraine is the Ohio continuation of the Salamoine moraine in Indiana.

Kames are also found in the kettle moraine area, and are mounds of compressed glacial till. Parts of the area have been protected in the Kettle Moraine State Forest.

The Mississinawa Moraine begins in Ohio east of Lima in Hardin County, then running in a shallow arc to the south of Grand Lake St. Marys and St. Marys in Mercer County towards Fort Recovery, Ohio. Just west of Fort Recovery, the moraine again arches southward towards the Mississinewa River. The moraine follows the eastern bank of the river northwestward to where it enters the Wabash River at Wabash, Indiana. Angling towards the north and a little east, the Mississinawa moraine merges with the Packerton Moraine north of the Eel River in Whitley County near Columbia City.

Moraines south of Lake Michigan and southwest of Lake Erie. A composite of three maps (Leverett 1915) (Leverett 1902) (Larsen 1986) and other sources. Colors represent moraines from the same time period of the Wisconsin Glacial epochThe Fort Wayne Moraine is considered contemporary to the last stages of the Valparaiso Moraine. Centered on Fort Wayne, Indiana, the northern leg of the moraine is mostly overlaid by the younger Wabash Moraine angling northeastward through Williams County, Ohio.

The ridge is named after the town of Marengo, located on the moraine. North of the Marengo Moraine and to the west of the North Branch Kishwaukee River is a deep depression, or notch, across the Marengo Moraine. The depression is a subglacial channel, easily differentiated from a valley by the lack of rivers and streams along its bottom. The channel once carried meltwater from under and in front of the glacier when it was depositing its moraine.

The channel tunnels were primarily created by the erosion from glacial rivers, a typical process before moraine formation. Characteristic of this moraine is the transition of deposition layers from glaciofluvial to glaciolacustrine. Sedimentary glaciofluvial areas form the core of the Oak Ridges Moraine, though restricted to subglacial cavity fills of confined subaqueous fans. Overlaying this core is a glaciolacustrine sedimentary layer that is younger and topographically lower, principally in the delta and basin areas of the moraine.

Much of that erosion took place in repeated glaciations. The most recent of these glaciations, the Wisconsin, included the Superior lobe, which passed over the area along the lake basin from the northeast to southwest. This left a terminal moraine where the glacier halted, and a ground moraine in other areas once covered by the continental glacier. The terminal moraine, known as the "Highlands Moraine", parallels the lakeshore, and forms the inland hills of the North Shore Highlands.

The Withrow Moraine and Jameson Lake Drumlin Field is a National Park Service–designated privately owned National Natural Landmark located in Douglas County, Washington state, United States. Withrow Moraine is the only Ice Age terminal moraine on the Waterville Plateau section of the Columbia Plateau. The drumlin field includes excellent examples of glacially-formed elongated hills.

The Rodado stage edifice has several moraine stages on its southern slopes. Another small cirque with a moraine has been found in the northeastern side of the Cerro Cumbre Negra summit next to an Azufrera stage lava flow. A small moraine lies on the south side of the Angulo edifice; some lavas from that edifice overlie glacial deposits.

In 2013, Fuyao began looking at establishing a factory presence in the United States, considering several sites in Ohio and Michigan before deciding on the former General Motors Moraine Assembly plant in Moraine, Ohio."Moraine no longer home to former GM Assembly Plant; Site now officially home of Fuyao Glass America Inc". Englewood Independent. 5/15, 2014.

Moraine Lake is located in North Cascades National Park, in the U. S. state of Washington. Moraine Lake is in a remote section of the park and well off any designated trails. During warmer months, melt from both the Inspiration and Forbidden Glaciers flow into Moraine Lake. Mount Torment is less than south of the lake.

Today the two rivers are separated by the terminal moraine of an ice front that spread up the Pilchuck valley and impounded the Sultan River, creating a lake. This glacial lake eventually drained westward, creating a delta moraine. The postglacial Sultan River cut through the delta moraine, establishing its present course out of the lower Sultan basin.

Hells Gate Moraine is a glacial moraine at the head of Evans Cove on the coast of Victoria Land, Antarctica. It extends southward to Hells Gate from nearby Vegetation Island and Cape Confusion.

The government also released the Oak Ridges Moraine Conservation Plan regulation, which defined land use and planning policies consistent with the Act, and assigned interim directors to the new Oak Ridges Moraine Foundation.

In Østfold, this moraine is referred to as the "Raet".

The western margin of the moraine is delineated by the Niagara Escarpment, a prominent cuesta that was fundamental to the development of the moraine. The escarpment's channels provided a route for drainage of ice-marginal meltwater; the channel system was eroded into the cuesta, and along its exposed eastern facing. Meltwater drained southwest and northeast along these corridors during the formation of the Oak Ridges Moraine. The Niagara Escarpment probably controlled regional water levels throughout the formation of the moraine.

Moraine View State Recreation Area is located atop a moraine, a low, rolling ridge located where a vanished ice sheet dumped ground rock and till while melting. Moraines are common post- glacial geological features, and can be found throughout the U.S. Midwest. This moraine was produced by the Wisconsin glaciation, about 70,000 to 10,000 years before present. Moraine View SRA is the headwaters for Salt Creek, a major tributary of the Sangamon River, one of the largest rivers in central Illinois.

Once the water reached the top of this moraine dam, it began to cut a channel through it. Most moraine dammed lakes drain quickly because water cuts entirely through the moraine. However, Flathead Lake remains because a bedrock hill buried underneath the Polson Moraine prevented the moraine from being completely cut through so the meltwater never completely drained. At one time, probably when the valley was partially filled by a glacier, the level of Flathead Lake was about higher and drained through the valley west of Elmo, Montana, which is at the end of Big Arm Bay, bottom center in the aerial photo above.

As ice melted, a lake formed behind the moraine and drained southward over top of it. The southerly drainage over the moraine eventually stopped and the Kootenay River began to follow its present course.

The Wisconsin ice sheet advanced roughly to the Lake Shelbyville Dam, forming a terminal moraine. The meltwater overtopped the moraine, forming the modern Kaskaskia River, which flowed on through land of older Illinoian Stage.

Moraine Township is a township in Lake County, Illinois, USA. As of the 2010 census, its population was 34,129. Moraine Township was originally called Deerfield Township, but the name was changed on October 29, 1998.

Scenic bluffs line the valley as it passes through the moraine.

The Oak Ridges Moraine Conservation Act, officially known as the Oak Ridges Moraine Conservation Act, 2001, is a conservation plan for land situated on or near the Oak Ridges Moraine in Ontario, Canada. The legislation was enacted by the Government of Ontario in 2001. The primary purpose of the legislation is to protect the ecological and hydrological integrity of the Oak Ridges Moraine. The legislation was passed by the Legislative Assembly of Ontario on 13 December 2001, and received Royal Assent the next day.

Large parts of today's old town of Constance are on the terminal moraine, and the north-south direction of the old town is due to the direction of the moraine. By contract, Stadelhofen, the southernmost town of the Constance area, was built on the former lake bed. In Kreuzlingen, the moraine extends along the Hauptstrasse ("Main Street"), roughly from the border to the intersection with Remisbergstrasse. Both the old and the new location of the monastery at Kreuzlingen are in the area of the moraine.

The Waterloo Moraine provides drinking water for over 300,000 people throughout Waterloo Region, and approximately 75% of its potable water. The Waterloo Moraine is currently not protected by provincial legislation although there is an active movement from citizens to see that this takes place. Louisette Lanteigne and David Wellhauser of Waterloo have used the Environmental Bill of Rights to submit a Request for Review for a Waterloo Moraine Protection Act. This resulted in a 16-month review of source water and groundwater protection for the Waterloo Moraine.

A map showing the area, labeled here as "Kettle Range" Kettle Moraine is a large moraine in the state of Wisconsin, United States. It stretches from Walworth County in the south to Kewaunee County in the north. It has also been referred to as the Kettle Range and, in geological texts, as the Kettle Interlobate Moraine. The moraine was created when the Green Bay Lobe of the Laurentide Ice Sheet, on the west, collided with the Lake Michigan Lobe of that glacier, on the east, depositing sediment.

Norris, Taku, Hole-in–the- Wall, Twin and Tulsequah glaciers emerge out on the southeastern side and flow into the trench of the Taku Inlet and Taku River. Two ice-streams join here to form a fan slope, ending in a terminal moraine. The sandy level of the moraine is cut by several watercourses; crimson epilobium blanket the beds of moraine.

Geologically, Jomfruland is part of a large residual moraine from the Ice Age called the Ra step. Jomfruland is the product of the back parts of the moraine (Ra) sticking out of the water. Eastward, the moraine remains underwater from Jomfruland to Mølen in Brunlanes, before it reappears after crossing Tromøy. Where the Ra is connected to the mainland it forms pebble beaches.

Official documentation alternatively refers to the park as the Chippewa Moraine Ice Age Reserve or the Chippewa Moraine Ice Age National Scientific Reserve. It is located in northwestern Chippewa County. The Chippewa Moraine Interpretive Center offers exhibits about the area's geology, natural history, and cultural history, as well as naturalist-led programs for school groups. The center is located east of New Auburn.

The Vestfold moraine, a continuation of the Østfold moraine at Moss, is an ice-formed formation which stretches as a cohesive gravel ridge through the county, from Horten in the east to Mølen in the south.

From the east, the St. Joseph River valley drained the meltwaters from the southern edge of the Saginaw Lobe and the northwestern shoulder of the Huron-Erie Lobe.The Glacial Lakes Around Michigan; William R. Farrand, Bulletin 4, Michigan Department of Environmental Quality, Geological Survey Division; Lansing, Michigan; revised 1988 The Valparaiso Moraine formed the southern flank of the Michigan Lobe as well as the northern ridge of the Kankakee Valley. At the northern end of the valley, the Dowagiac River valley extended northward between the Valparaiso Moraine on the west and the Kalamazoo Moraine on the east. The Kalamazoo Moraine formed one side of the melting Saginaw Lobe, with the southern flank sitting on the Sturgis Moraine.

Terminal moraine of Wordie Glacier, Greenland Map of the Salpausselkä terminal moraines in Southern Finland A terminal moraine, also called end moraine, is a type of moraine that forms at the snout (edge) of a glacier, marking its maximum advance. At this point, debris that has accumulated by plucking and abrasion, and has been pushed by the front edge of the ice, is driven no further and instead is dumped in a heap. Because the glacier acts very much like a conveyor belt, the longer it stays in one place, the greater the amount of material that will be deposited. The moraine is left as the marking point of the terminal extent of the ice.

Root River in Olmsted County Relief map of Southeastern Minnesota: Owatonna Moraine on extreme west; junction of the state's principal rivers in Central Minnesota in northwest; the Wisconsin border along the Mississippi River to the east. Southeastern Minnesota is separated from Southwestern Minnesota by the Owatonna Moraine, the eastern branch of the Bemis Moraine, a terminal moraine of the Des Moines lobe from the last Wisconsin glaciation. Ojakangas and Matsch extend the region west past the moraine to a line running north from the Iowa border between Mankato and New Ulm to the latitude of the Twin Cities, then encompassing the latter metropolis with a broad arc east to the St. Croix River.Minnesota’s Geology, p.

Randa attended Kettle Moraine High School in Wales, Wisconsin, lettering in football, basketball, baseball, and tennis. Randa's #12 was retired by the Lasers. He is also a member of the Kettle Moraine Laser Trailblazer Hall of Fame.

In northern Van Buren County it becomes associated with the Saginaw moraine.

Reusch's Moraine in northern Norway may have been deposited during this period.

Moraine State Park is part of the Appalachian mixed mesophytic forests ecoregion.

However, the lowest beds in the moraine may have experienced synchronous sedimentation.

The Trafalgar Moraine is a geological landform straddling Oakville and Milton in Ontario, Canada. A small portion of the moraine extends into Burlington at Milton's southern border. It is a subtler topological feature than the better- known Oak Ridges Moraine, primarily because it was formed as an end moraine at the terminus of a glacial ice sheet, instead of between two retreating ice lobes (known as interlobate). The ice sheet pushed material to form the ridge, which is composed of Halton Till sediment, rich in silt and clay.

Valparaiso Moraine at Mink Lake, north of Valparaiso, Indiana, US The Valparaiso Moraine is a recessional moraine that forms an immense U around the Lake Michigan basin in North America. It is a band of high, hilly terrain made up of glacial till and sand. It begins near the border of Wisconsin and Illinois and extends south through Lake, McHenry, Cook, DuPage and Will counties in Illinois, and then turns southeast, entering Indiana. From this point, the moraine curves northeast through Lake, Porter, and LaPorte counties of Indiana into Michigan.

Fisher and Alexander in the early 1990s described a "metropolitan" invasion of the Oak Ridges Moraine, in response to which organizations such as Save the Oak Ridges Moraine (STORM) were formed. Conservation Authorities Moraine Coalition (CAMC) is a coalition of nine Conservation Authorities with watersheds on the Oak Ridges Moraine (ORM). The Coalition formed in 2000 two years prior to the ORM conservation Plan, in response to the need for a comprehensive policy, planning and management approach geared to sustaining the health of the entire ORM. The CAMC is a partnership organization.

Other prominent examples of terminal moraines are the Tinley Moraine and the Valparaiso Moraine, perhaps the best examples of terminal moraines in North America. These moraines are most clearly seen southwest of Chicago. In Europe, virtually all the terrain in the central Netherlands is made up of an extended terminal moraine. In Switzerland, alpine terminal moraines can be found, one striking example being the moraine at the end of the valley of the Forno Glacier in the south-eastern canton of Graubünden near St. Moritz and the Italian border.

The Oak Ridges Moraine began to come to public awareness in the late 1980s. The establishment, in 1989, of the Save the Oak Ridges Moraine (STORM) Coalition contributed to a growing sense among local residents that action needed to be taken to save the moraine. The Government of Ontario created the Oak Ridges Moraine Technical Working Committee in June 1991 with the joint membership of the Ministry of Natural Resources, the Ministry of the Environment and the Ministry of Municipal Affairs. The STORM Coalition played a significant role in the Committee's work.

The western lobe formed Green Bay, Lake Winnebago and the Horicon Marsh. The major part of the Kettle Moraine area is considered interlobate moraine, though other types of moraine features, and other glacial features are common. A small kettle in the area The moraine is dotted with kettles caused by buried glacial ice that calved off the terminus of a receding glacier and got entirely or partly buried in glacial sediment and subsequently melted. This process left depressions ranging from small ponds to large lakes and enclosed valleys.

The melt waters began to form a lake between the southern front of the glacier and the moraine, which acted as a dam. The water collected until it found a low spot in the moraine, near modern Palos Hills, Illinois. Here, it topped the moraine and began cutting an outlet. At around above sea level, it stopped cutting downward and a stable lake formed.

Parts of Pottageville, particularly the ecological areas outside the village, are located on the northern face of the sensitive Oak Ridges Moraine. Characteristic of other parts of the moraine, the ecological areas of Pottageville exhibit a range of features.

Palos Heights students can readily commute to Moraine Valley Community College in nearby Palos Hills. Moraine Valley serves the local residents through classes, seminars, lectures, concerts, plays, and other activities. Trinity Christian College is also located in Palos Heights.

The Harbor Hill moraine is represented by the North Fork of eastern Long Island and in three disjunct sections farther east, Plum Island, Great Gull Island, and Fisher's Island. The Harbor Hill Moraine, named for its prominence at Harbor Hill, Roslyn, New York, the highest point in Nassau County, resulted from a lingering equilibrium stage in the glacier's episodic retreat, creating a stationary melting front;Garvies Point Museum and Reserve: the Geology of Long Island. the Long Island area became permanently free of glacial ice in the range of 13,000 to 12,000 YBP (Years Before Present).Phil Stoffer and Paula Messina (CUNY), "The Transient Atlantic Shoreline" The Harbor Hill Moraine intersects with the earlier Ronkonkoma Moraine at Lake Success: east of the lake the two moraines may be seen, but west of Lake Success the Harbor Hill moraine overrode and effaced the Ronkonkoma moraine.

These plains are usually found beyond the end moraine deposited by the glacier.

Moraine Township covers an area of ; of this, or 0.27 percent is water.

The Blenheim moraine is a glacial moraine in Kent County, Ontario, north of Lake Erie. Bluffs and beaches left from glacial lakes Arkona, Whittlesey, and Warren are found on the southern bank. The moraine's underwater extension is called the Erieau Ridge.

In order to understand the process by which the moraine formed, it is necessary to understand the physical geography in which it currently exists (that is, its physiography), and the layers of sediments found within it (the stratigraphy of the moraine).

Elephant Moraine () is an isolated moraine, long, located west of Reckling Peak, to the west of the head of Mawson Glacier in Victoria Land, Antarctica. The moraine, described in some reports as an ice core moraine, is situated along a long, narrow patch of bare ice that extends west from Reckling Peak for . The feature was noted in U.S. satellite imagery of 1973, and in aerial photographs obtained subsequently, by William R. MacDonald of the United States Geological Survey, who originally described it to William A. Cassidy as "a possible nunatak having an outline similar to an elephant." Several United States Antarctic Research Program field parties led by Cassidy collected meteorites at this moraine during the 1979–80 ANSMET season, including the Martian meteorite EETA 79001.

The Ogemaw Hills Pathway trail system traverses a well defined ridge of hills north of West Branch, Michigan referred to by geologists as the West Branch Moraine, a recessional moraine outwash formed by the Saginaw Lobe of the Laurentide Ice Sheet. The West Branch Moraine marks a norther border of the Pleistocene proglacial Lake Saginaw that formed in front of the melting Saginaw Lobe and retreated into present day Saginaw Bay.

The Salt Creek watershed covers 19% of Porter County and , including the communities of Valparaiso, South Haven, Portage and Burns Harbor, Indiana. The watershed begins in the physiographic unit known as the Valparaiso Morainal Area. The Valparaiso Moraine, located south of the Lacustrine Plain, is an arc-shaped moraine complex that parallels the southern shore of Lake Michigan. The moraine divides LaPorte and Porter County into northern and southern drainage areas.

The committee's aim was to create a regional planning strategy to coordinate the activities of various regional and municipal governments with jurisdiction over parts of the moraine. This multi-stakeholder process produced a comprehensive long-term strategy for the Moraine in 1994. However the strategy was subsequently dismissed in favour of local government administration of the affected lands. This led to intense development on some portions of the moraine.

Withrow Moraine is the only Ice Age terminal moraine on the Waterville Plateau section of the Columbia Plateau. It lies on the terminal moraine for the Okanogan lobe of the Cordilleran Ice Sheet, which flowed southward through the Okanogan trough from the Interior Plateau of British Columbia blocking the course of the Columbia River and ending on the elevations of the Waterville Plateau. Illustration of the glacial impacts.

The peak forms part of the backdrop to Moraine Lake in Banff National Park.

The moraine forms a major portion of the eastern divide of the Fox River Basin and then the western bank of the Des Plaines River. The moraine continues southward along the Des Plaines River following the route of the modern Tri- State Tollway (I-294) around the west side of Chicago. Where the Des Plaines River bends to the west and forms the Illinois River, the moraine angles south and east, continuing along I-294 towards Chicago Heights. In this area, the moraine has widened out towards the south and east, becoming a broad plain covering large portions of Will and Kankakee counties.

Granite Apron draping southwestern margin of Moraine Dome Moraine Dome is a granite dome in Yosemite National Park along the northern margin of Little Yosemite Valley at which rises to an elevation of AMSL, above the Merced River. Moraine Dome is notable because the presence of lateral moraines from the Merced Glacier. It is likely that these moraines represent the highest level attained by glacial ice in Little Yosemite Valley. Although it is about as high as Sentinel Dome Moraine Dome is dwarfed to relative insignificance by its proximity to the bulk and elevation of Clouds Rest to the north.

The moraine contains one of the last large contiguous forested spans in southern Ontario. Some of the wide variety of plant and animal species found in the moraine are species at risk in Canada and Ontario, including the West Virginia white butterfly, Jefferson salamander, red-shouldered hawk, and American ginseng. Unique ecosystems in the moraine include wetlands similar to those of boreal forests in Northern Ontario, and remnants of tallgrass prairie and oak-pine savanna that are globally threatened ecosystems. A representative portion of the moraine may be found in the Happy Valley Forests, in York Region, north of Toronto.

Although preservation of the moraine was first suggested in the 1940s, it was not until 1991 that the issue achieved prominence in political discourse. Part of the reason for its entry into political discourse, was due to the formation, in 1989, of the Save the Oak Ridges Moraine (STORM) Coalition. The Government of Ontario created the Oak Ridges Moraine Technical Working Committee in June 1991, with the aim of creating a regional planning strategy for the moraine. The plan was completed in 1994, but was subsequently dismissed in favour of local government administration of the affected lands.

The politics of the Oak Ridges Moraine in southern Ontario, Canada, have centred on the question of how to preserve this extensive natural resource that is increasingly threatened by human modification. Although preservation of the moraine was first suggested in the 1940s, and intermittently over the subsequent fifty years, it was not until 1991 that the issue achieved prominence in political discourse. For the ensuing decade, use of the moraine was hotly contested between the interests of local residents, developers and environmentalists. On December 14, 2001 legislation was enacted, along with a provincial land use plan for the Oak Ridges Moraine.

The Polson Moraine, near present-day Polson, Montana, marks the southernmost extent of the glacier during the last ice age and thus is the site of the glacier's terminal moraine. Some clouds over Flathead Lake in Polson, Montana, as the sun is setting The large size of the Polson Moraine indicates that the glacier stalled here for many years before retreating. As the climate warmed, a portion of the glacier in the Mission Valley receded more slowly than the main body, which kept the lake basin from being filled with sediment. Eventually this ice also melted, forming a lake behind the moraine.

The low, rolling, ground moraine landscape is fertile and supports highly productive arable farming. The chain of lakes and end moraine ridges are popular holiday areas. The poorer, sandy areas are largely covered by pine forest (e. g. Schorfheide, Tucheler Heide, Rominter Heide).

Tinley Park is located at (41.573800, −87.803891). According to the 2010 census, Tinley Park has a total area of , of which (or 99.88%) is land and (or 0.12%) is water. The village lies on the Tinley Moraine and/or the Valparaiso Moraine.

His cabin eventually became the county courthouse. The first businesses were blacksmith shops, a general store and stage coach stop, and a grist mill. The terminal moraine of the Wisconsin Glacier is located near Shelbyville. This is referred to as the Shelbyville Moraine.

The chapel stands on a glacial moraine and gives a broad view over Lake Constance.

The glacial sediments constituting the moraine rest upon the Guelph and Salina carbonate bedrock formations.

The plains to the east between the Fort Wayne and Defiance is wide and is occupied by faint terminal moraines. These are closely related to the Fort Wayne moraine. Two moraines run parallel with the main crest of the Fort Wayne moraine in the vicinity of Lima, Ohio. The Bluffton moraine is west of Mount Cory to Bluffton and then turns southwest to within a mile (1.6 km) of Cairo and Elida.

Moraine Assembly Sticker placed on vehicles assembled at the plant Moraine Assembly was a General Motors automobile factory in Moraine, Ohio, United States, a suburb of Dayton. A Frigidaire appliance plant had originally operated on the site from 1951 to 1979. Starting in 1981, the Chevrolet S-10 small pickup was produced along with Shreveport Assembly. In 1987 through 1994 the plant produced the rolling chassis for the Grumman LLV Postal Vehicle.

Vestbanen Moraine is a medial moraine in Humboldt Graben, originating near Zwiesel Mountain and trending north in string-like fashion for 13 miles (21 km) along the west flank of the Petermann Ranges, Wohlthat Mountains. First plotted from air photos by German Antarctic Expedition, 1938–39. Remapped by Norwegian Antarctic Expedition, 1956–60, and named "Vestbanen" ("the west path"). The feature is similar to Austbanen Moraine which parallels it 7 miles (11 km) eastward.

A Pulju moraine (Swedish: Pulju-morän) is a type of moraine found in northern Finland. Pulju moraines were first identified as distinct moraine type in 1967 by Finnish geologist Raimo Kujansuu who noticed moraines that resembled Veiki moraines as those described by Gunnar Hoppe in 1952 but were smaller. Raimo Kujansuu described Pulju moraines with the following words: Together with Veiki moraines Pulju moraines form landscapes of the type "ice-walled lake plains".

The park is situated on the Bemis Moraine, which marks the southern extent of a glacial lobe during the Wisconsin glaciation 10,000 years ago. As the glacier retreated, the moraine caused the meltwater to back up behind it. Albert Lea Lake was created as a moraine-dammed lake and today covers . The park also contains an esker, a sinuous ridge of sand and gravel dropped by a stream running under the glacier.

The end moraines in the Constance depression were formed along the edge of the ice during the Constance stage (see above). In the area of the old town of Constance, we find a moraine surrounded by Lake deposits. The section of the moraine in Kreuzlingen, however, is surrounded predominantly by Pleistocene talus. Sections of the end moraine are found further north east and south east, in the area of the Bodanrück and Seerücken, respectively.

The Oak Ridges Moraine is a geological landform that runs east-west across south central Ontario, Canada. It developed about 12,000 years ago, during the Wisconsin glaciation in North America. A complex ridge of sedimentary material, the moraine is known to have partially developed under water. The Niagara Escarpment played a key role in forming the moraine in that it acted as a dam for glacial meltwater trapped between it and two ice lobes.

The topography of Long Island including that of the Jamaica neighborhood was formed during glaciation, which created a terminal moraine running east-to-west across the center of the island. The Jamaica Hills neighborhood and the current Jamaica High School building lie at the peak of the moraine, while Hillside Avenue where the old building is situated forms the southern edge of the moraine, and thus is at a much lower elevation.

The idea of a route along the Kettle Moraine was believed to be conceived in the early 1940s by the Kettle Moraine Committee of the Izaak Walton League – Milwaukee Chapter, which was the backbone behind the development of the Kettle Moraine State Forest units. The first surveying of the area did not begin until 1946. The Wisconsin Highway Commission approved the route in 1948 and the first paving project was completed in 1950.

By contrast, the Oak Ridges Moraine is primarily sand and gravel. The ridge was probably formed during a pause in the retreat of the ice sheet. The moraine covers an area of 892.5 hectares of primarily private land, though a small portion is public.

Mel Moraine () is a moraine at the north end of the Gagarin Mountains, in the Orvin Mountains of Queen Maud Land, Antarctica. It was mapped by Norwegian cartographers from air photos and surveys by the Sixth Norwegian Antarctic Expedition, 1956–60, and named Mel (meal).

To the north of Toronto is the Oak Ridges Moraine. The largest ravines are home to the rivers running south from the Moraine to Lake Ontario: the Humber River, the Don River, and the Rouge River.Cundiff, Brad. The Hike Ontario guide to walks around Toronto.

The Nottawasaga River's headwaters originate in the Niagara Escarpment, Simcoe Uplands, Oak Ridges Moraine and Oro Moraine. The area of the drainage basin is , and as well as Dufferin County and Simcoe County, is located in Grey County and the Regional Municipality of Peel.

McHenry is surrounded by natural lakes and streams, grassy moraine hills, gravel banks and shallow nutrient-rich peat bogs, remnants of receding glaciers from the last ice age. Moraine Hills State Park and Volo Bog State Natural Area preserve some of these natural features.

Some of the more spectacular are Bow, Hector, Louise, Maligne, Moraine, Peyto, Pyramid and Vermilion lakes.

A terminal moraine is visible at the north end of the lake on the northeast edge.

OSHA cited Fuyao for a total of thirteen different safety violations and fined the manufacturing firm approximately $725,000. Subsequently, they were met with a $7 million investment by Fuyao towards improving safety features throughout the Moraine Assembly plant. Additionally, Fuyao has since formed an environmental safety team within the Moraine assembly that provides in-depth training to the plant employees in both English and Mandarin Chinese. Since the majority of the labor force at Fuyao Glass America's Moraine Assembly plant had previously worked at the General Motors Moraine Assembly that was located on the same property, many workers wished to reform their connections with a major American labor union.

222 (map). This moraine runs south from the Twin Cities in the general area of Minnesota State Highway 13 and Interstate 35. Sansome attaches this moraine to her description of West- Central Minnesota, given its similarity in glacial features to that region.Sansome, Minnesota Underfoot, p. 110.

Firura has well preserved moraine systems. A major moraine system with a relief of was left by the Last Glacial Maximum, although expansion of glaciers on the northern flank was constrained on a high plateau. The prevalent aridity of the climate impedes the degradation of these moraines.

The nature park lies near Neumünster only a few kilometres west of the A 7 motorway. Two landscape forms occur in the park: the flat and pure loamy ground moraine landscape and the considerably more subdivided push moraine landscape, that rises to about 80 metres above NN.

There is little difference between the soils mixture of the Tinley Moraine and the Valparaiso Moraine. There is a greater quantity of silt and clay similar to a fine grained lake sediments. The clay-rich and pebble-poor till implies that existence of a glacial lake on the margin of the ice. The till mixture predates the Lake Chicago beaches, of which the Glenwood Beach is the oldest and contemporary with the Lake Border Moraine along the Michigan shore.

The Oak Ridges Moraine is an ecologically important geological landform in the Mixedwood Plains of south-central Ontario, Canada. The moraine covers a geographic area of between Caledon and Rice Lake, near Peterborough. One of the most significant landforms in southern Ontario, the moraine gets its name from the rolling hills and river valleys extending from the Niagara Escarpment east to Rice Lake. It was formed 12,000 years ago by advancing and retreating glaciers (see geological origins, below).

That is, the western portion of the moraine received earlier and more frequent sedimentary deposition than the eastern portion, as the ice lobes which controlled the moraine's eastern formation slowly retreated. The Rice Lake wedge is separated from the other wedges where the Oak Ridges Moraine intersects Rice Lake. To the north are drumlinized uplands, referred to as the Peterborough drumlin field. Highway 115 is visible in the centre of the picture as it ascends the Moraine.

Kendall County has two primary ranges of low-lying hills formed by what is known as an end moraine. Ransom, the more predominant of the two moraines, runs through the west and north-central part of the county. This moraine has created elevations over , in contrast to elevations in southern Kendall County that drop to the lower range. Minooka, the other major end moraine ridge in Kendall County, runs along its entire eastern border with Will County.

The Strange Till Plain is a flat ground moraine with underlying glacial till. It was formed by the Ontario ice lobe during the Port Huron Stadial. It is believed that this till plain exhibits the original surface; very little erosion or surface deposition is observable throughout its 3 square kilometre range. This Till plain is located between and within the Albion and Uxbridge wedges of the Oak Ridges Moraine, and is a constituent part of that moraine.

The Lüneburg Heath seen from the Wilseder Berg in northern Germany. The Lüneburg Heath consists of pushed moraines made from Neogene sand deposits. These form nutrient-poor soils and are generally shrublands covered in heaths. A push moraine or pushed moraine is in geomorphology a moraine (a landform formed by glacial processes) that forms when the terminus advance of a lowland glacier pushes unstratified glacial sediment into a pile or linear ridge in front of it.

The origin of the neighborhood's name is disputed. One theory is that it came from the Ridgewood Reservoir in Highland Park, in Brooklyn just south of Ridgewood. The reservoir was on a high ridge in the middle of the Harbor Hill Moraine, a terminal moraine that runs the length of Long Island. Another possible etymology is the forests that covered the area before colonial settlement, and that early English settlers called the moraine the "ridge" of Long Island.

Most of this development was suburban detached single-family dwellings with road networks to accommodate them. In particular, Vaughan, Richmond Hill and Newmarket experienced significant growth in the 1990s. In early 1999, the Oak Ridges Moraine became a sensitive political issue; developers targeted Richmond Hill for large subdivisions on the moraine, which would house over 100,000 people. Environmental groups began a media campaign to raise public awareness of the moraine, referring to it as the "rain barrel of Ontario".

Development on the moraine has been limited to regions in Mississauga, and the construction of Highway 407.

The town lies on the Valparaiso Moraine and the small stream, Plum Creek, runs through the area.

They also have a rivalry with Chargers of Kettle Moraine Lutheran High School, another WELS high school.

Dobin am See lies on the northeastern shore of Schwerin Lake amid a hilly terminal moraine landscape.

Wisconsinan Till Moraine, Wisconsinan Bouldery Till, Wisconsinan Flow-Till, and Wisconsinan Till all occur near the stream.

Along this stretch, the eastern part of the watershed of the Sangamon therefore consists of short creeks, two to three miles (3–5 km) in length, that drain the face of the moraine. This forms an asymmetric watershed typical of rivers formed along the face of a terminal moraine.

The Oak Ridges Moraine. The Oak Ridges Moraine covers a 1,900 square kilometres (734 sq mi) between Caledon and Rice Lake, near Peterborough. It is a hydrological system of streams, wetlands, kettle lakes and ponds and their catchment areas, seepage areas, springs, and aquifers and other recharge areas.

Alnwick/Haldimand is part of the Oak Ridges Moraine: a significant land form in Ontario. 31.3 km² of the Cobourg Creek watershed runs through the Township. The majority of this area is located within the Oak Ridges Moraine. The Creek supports a diverse ecosystem including forests, meadows and wetlands.

Moraine Valley happened to be the same school his father attended. After Moraine Valley, Saul played in the IBL (semi-pro) league for the Ohio Hidden Gems. After playing in the IBL, he landed himself with The World Famous Harlem Globetrotters. Saul White Jr. continues to follow his dreams.

Northern terminus The Kettle Moraine Scenic Drive is a designated scenic route in southeastern Wisconsin that links the two units of the Kettle Moraine State Forest. The route traverses through scenic and historic areas, including landscape shaped by glaciers from the latest ice age, known as the Wisconsin glaciation.

The Aeolian sands form the southern boundary of Lake Kankakee as they result from the wind moving sand from the shoreline inland. This feature begins in the northeast along the Maxinkuckee moraine of the Saginaw ice lobe in Marshall County, Indiana near Lake Maxinkuckee and Culver, Indiana. While a few dunes are found on the moraine, the sand beds are along the western edge. The Maxinkuckee moraine follows the north side of Tippecanoe River into Fulton County eastward towards Rochester.

Austbanen Moraine is a medial moraine in the glacier between the Westliche Petermann Range and the Mittlere Petermann Range in the Wohlthat Mountains, originating at Svarttindane Peaks and trending north for . It was first roughly plotted from air photos by the Third German Antarctic Expedition between 1938 and 1939. It was mapped by the Sixth Norwegian Antarctic Expedition from 1956 to 1960, from air photos and from surveys, and named "Austbanen" ("the east path"). Vestbanen Moraine, a similar paralleling feature, lies westward.

This led to intense development on some portions of the moraine. In early 1999, developers targeted Richmond Hill for large subdivisions on the moraine which would house over 100,000 people. On July 20, 1999, Minister of Municipal Affairs and Housing Steve Gilchrist announced, on "Rouge Park Day", that he would be implementing a ban on all development on the Oak Ridges Moraine. This announcement sparked considerable opposition by the development industry which, in turn, attracted considerable media attention and public interest.

Moraine Country Club is a country club located in Kettering, Ohio, in the Dayton Metropolitan Area. The development of the Moraine Country Club started at a meeting in 1927, when Colonel Deeds, Charles Kettering, Frederick Rike, Governor James Cox, Robert Patterson, John Haswell & William Keyes decided to turn a portion of "Moraine Farm" into a golf course. Alec Campbell designed the course and in 1930 the club was incorporated. The golf course there hosted the PGA Championship in 1945 which Byron Nelson won.

Its waters flow from Beaver Creek to the Lake Moraine reservoir, a supplier of water to Colorado Springs.

The Kaskawulsh Glacier in the Kluane National Park, Yukon, has a ridge of medial moraine 1 km wide.

The campus of the Moraine Park Technical Institute was severely damaged by the tornado and classes were disrupted.

Won by Michel Détroyat flying a Moraine Saulnier MS.234, completing the course at an average speed of .

STORM has played an important role in triggering political action to preserve the Oak Ridges Moraine. Soon after its formation, it raised the profile of the Moraine at both the local and provincial levels, causing the provincial government to declare an "expression of provincial interest" in the Moraine in 1990. STORM was appointed as a member of the government-sponsored Oak Ridges Moraine Technical Working Committee. In addition to STORM, membership on the committee included: Regional Municipalities of Durham, Peel and York, MNR, MMAH, MOE, Toronto and Region Conservation Authority (TRCA), Ganaraska Region Conservation Authority (GRCA), Conservation Council of Ontario (CCO), Urban Development Institute (UDI), Aggregate Producers Association of Ontario (APAO), and Federation of Ontario Naturalists (FON).

The Tinley Moraine would be an earlier recession of the Michigan Lobe a short ways north, returning southward, with both wind and water driven drifts, mixed with the return of the ice front for a short duration before the northward retreat of the ice front, establishing the Lake Chicago sequence of shorelines and moraine features in northern Wisconsin and Michigan. The impounded meltwater trapped between the ice front and the Valparaiso Moraine, found a breach in the moraine east of the Illinois-Indiana boundary following West Creek into the sluiceway of the Kankakee River. An additional release may have been in the vicinity of the Deep River – Stoney Run divide east of Crown Point.

South of the Sturgis Moraine, the future St. Joseph River was a marshy plain, extending southeastward towards the toe of the Huron-Erie Lobe. First the Union City Moraine formed, then as the ice receded and again stabilized the Mississinawa Moraine formed along the front of this ice The Saginaw Lobe's meltwater flowed across the St. Joseph valley, while the Huron- Erie Lobe's meltwater and sediments first flowed into the upper Tippecanoe River. When the glacier moved back to the Mississinawa Moraine, the off flowing water created the Eel River valley. The waters coming down the St. Joseph valley crossed the till plain south and east of the future South Bend entering the valley of the Kankakee River.

The headwaters of the Rouge River and its tributaries are found in the Oak Ridges Moraine. Water flows down from the elevated moraine to Lake Ontario. The Rouge River meets Lake Ontario at Rouge Beach. At Rouge Beach, the Rouge Marsh is to the north and Lake Ontario to the south.

Water backed up, until it began to flow southward along the course of the ancestral Tuscarawas River. As the ice sheet retreated, it left behind a recessional moraine near Akron, Ohio. The ice sheet retreated further, then made a minor advance. This advance left behind another recessional moraine near Defiance, Ohio.

The terrain is hilly, erosion-moraine. In the west the moraine chain goes to the Belarusian ridge . The Dnieper (west) and the Volga (east) rivers drain its hill. The watersheds feed three seas: the Baltic (Kasplya → Western Dvina), Black (Dnieper) and the Caspian (the Volga, the Oka River and their tributaries).

Hunter Geographic Information Systems (November 30, 2001). Oak Ridges Moraine Experience (to September 2001). Retrieved on 2010-05-30.

Moraine Park is also a popular place to watch elk, because many elk congregate here for the fall rut.

A section of the Ice Age National Scenic Trail runs through the park as it follows the Kettle Moraine.

Beneath this relatively thin layer of soil is unconsolidated moraine, soil and rock left behind as the glaciers retreated.

The town lies in the New Holstein/Moraine Park Technical College and Chilton/Fox Valley Technical College school districts.

Many glacial erratics can be found throughout the city. The moraine has left the city with mostly clay soil.

During this time, the Superior Lobe had retreated from the St. Croix Moraine northeastward to the Thompson Moraine. Between 14,000 and 11,500 BP calibrated (12,000 and 10,000 14C uncalibrated), an extensive set of ice marginal channels drained meltwater from the Thompson Moraine by way of the Brule channel into the newly formed St. Croix River.Hobbs, H.C., Breckenridge, A., Miller, J.D., Hudak, G.J., Wittkop, C. and McLaughlin, P.I., 2011. Ice advances and retreats, inlets and outlets, sediments and strandlines of the western Lake Superior basin.

The trail roughly follows the location of the terminal moraine from the last Ice Age. As the route traverses the moraine, it sometimes meanders into areas west of the moraine, including the Driftless Area in southwestern Wisconsin. The trail passes through 30 of Wisconsin's 72 counties, from the northwestern part of the state to the Lake Michigan shoreline in the east. The western end of the trail is at Interstate State Park along the St. Croix River, which is the border between northwestern Wisconsin and eastern Minnesota.

The presence of the moraine is evident in the course of St. Mary's River. Its headwaters in Auglaize and Mercer counties, flow north toward the Maumee until it comes to the moraine ridge. Here it turns to the west. The ridge forms the watershed between the St. Mary's and the Auglaize River.

Henry Moraine is a small moraine on the northwest side of Mount Bjerke in the Conrad Mountains of Queen Maud Land, Antarctica. It was mapped by Norway from air photos and surveys by the Sixth Norwegian Antarctic Expedition, 1956–60, and named for Henry Bjerke, a mechanic with the expedition, 1957–59.

The Smalfjord diamictite, Bigganjargga Tillite or Reusch's Moraine is a diamictite in Finnmark, northern Norway. The rock was first identified as a tillite by Hans Reusch in 1891, hence its name. The tillite overlies sandstone whose contact surface is striated. Reusch's Moraine belong to the Smalfjord Formation, a geological formation of Neoproterozoic age.

Entrance to the Koffler Scientific Reserve. In 1829, John Bigsby conducted the first investigation of the moraine. He noted the elevation, and styled the area Oak Ridge, identifying the portion of moraine north of Toronto. The moraine's extent was not established until 1863 when William Logan conducted the Geological Survey of Canada.

In recent years, several mayors have been recalled and removed from office. Moraine has a municipal income tax of 2%.

The Union Moraine begins in Ohio, east of Bellefontaine and the highest point in that state, (Campbell Hill, )Rand McNally Road Atlas, Rand McNally Co; Chicago, IL, towards Greenville in Darke County. Traveling southwestward and arcing a little northward, the moraine reaches Union City, Ohio for which it is named. From here, it travels almost directly westward to Muncie, Indiana. From Muncie, the moraine runs northwest ending in the bluffs overlooking Pipe Creek at Bunker Hill,Indiana, just south of Peru on the Wabash River.Glacial Map of the United States East of the Rocky Mountains, U.S. Geological Survey, Department of the Interior The ‘’’Union City Moraine’’ is the outer ring of a series of moraines created by the Huron-Erie lobe of the Laurentian Glacier.

This band of hills is called the Perkinstown terminal moraine. North and west of the moraine, in the corner of the county toward Jump River, that last glacier left behind a more gently rolling plain of glacial till.Glacial landforms of Taylor County. The striking glacial features in this area are glacial erratic boulders and eskers.

In New Zealand the Franz Josef Glacier on the West Coast has created the terminal moraine called the Waiho Loop. "The Mothership", a terminal lobe of a glacier flowing down from the interior ice cap on top of the Byam Martin Mountains, Bylot Island, Nunavut, Canada. Note the terminal moraine "bulldozed" at the ice front.

Moraine is a city in Montgomery County, Ohio, United States. The population was 6,307 at the 2010 census. The city is part of the Dayton Metropolitan Statistical Area, which includes Montgomery County. Moraine, as part of the Dayton area, is situated within the Miami Valley region of Ohio, just north of the Cincinnati metropolitan area.

The northeastern face of the same moraine, outside the state recreation area, is the headwaters of the main stem of the Sangamon. Although Salt Creek and the main stem of the Sangamon arise on opposite sides of this moraine, they flow more than west before they meet again. View of Dawson Lake, north end.

The Trafalgar Moraine is formed primarily of silty, clay- rich sand, and underpinned by shale bedrock, all of which hinder water absorption. Nonetheless, a few areas serve as surface water reservoirs, allowing for some groundwater regeneration, given the almost impermeable soils. The Trafalgar Moraine is approximately 20 km long, 30 m high and 4 km wide, extending from the Niagara Escarpment north of Nelson to Streetsville in an east-northeast trend; at the Oakville boundary, the trend shifts northeast. The moraine has impacted the flow of the eastern branch of the 16 Mile Creek.

Physiography of the Kankakee Outwash and Lacustrine Plain (pale green area) The Kankakee Outwash Plain is a flat plain interspersed with sand dunes in the Kankakee River valley in northwestern Indiana and northeastern Illinois of the United States. It is just south of the Valparaiso Moraine and was formed during the Wisconsin Glaciation. As the glacier, stopped at the Valparaiso Moraine, melted, the meltwater was carried away to the outwash plain. On the south side of the moraine, where the elevation drops, the meltwaters eroded away valleys, carrying sand and mud with them.

Eastern Parkway is located on the high edge of Harbor Hill Moraine, a terminal moraine. Approximately 17,000 years ago the moraine of the receding Wisconsin Glacier that formed Long Island established a string of hills. Mount Prospect (or Prospect Hill), near the present-day intersection of Flatbush Avenue and Eastern Parkway, is one of the tallest hills in Brooklyn, rising 200 feet (61 m) above sea level. During the American Revolutionary War (1775-1783), the area was a site of the Battle of Long Island (aka Battle of Brooklyn).

During at least three glacial periods, including the Wisconsin glaciation around 20,000 years ago, ice sheets advanced south across North America carving moraines, valleys, and hills. In particular, bays and estuaries were formed along the north shore of Long Island. During glaciation, the meadows surrounding the Flushing River were formed just north of the terminal moraine that runs across Long Island, which consisted of sand, gravel, clay and boulders. The moraine created a drainage divide, with rivers north of the moraine such as the future Flushing River emptying into the north shore.

Sandy shore along the Kankakee River, west of Illinois–Indiana state line The Kankakee River Basin is a product of the Wisconsin Glacial Episode. It is a remnant of the glacial lakes that comprised the Lake Michigan lobe of the ice sheet. Landscape elements include 1) the nearly level plains of a ground moraine, 2) eolian (wind driven deposits) plains, 3) outwash deposits, 4) the central river basin and 5) end moraines forming the north, middle and southern borders. Local relief varies from along the Iroquois Moraine, up to on the Valparaiso Moraine.

During at least three glacial periods, including the Wisconsin glaciation around 20,000 years ago, ice sheets advanced south across North America carving moraines, valleys, and hills. In particular, bays and estuaries were formed along the north shore of Long Island. During glaciation, what is now Flushing Meadows Park was formed just north of the terminal moraine that runs across Long Island, which consisted of sand, gravel, clay and boulders.; ; ; The moraine created a drainage divide, with rivers north of the moraine such as the future Flushing River emptying into the north shore.

Proglacial lakes in the Great Lakes basin Whenever the ice sheet melted from the north at a moraine, water would begin to pond in the divide between a moraine and the ice front. The ice would act as a dam as water could not drain through the ice sheet, which in the Wisconsin period covered most of the proglacial river valleys. Numerous small, isolated water bodies formed between the moraine and the ice front. As the ice sheet would continue to melt and recede northward, these ponds combined into proglacial lakes.

View from the endpoint of the peninsula. Hindens rev is a long, narrow, straight peninsula that projects westwards from Kålland into Dalbosjön, the western part of lake Vänern. Hindens rev is a terminal moraine and is part of what is known as the central Swedish terminal moraine zone. The latter is in turn part of a series of terminal moraines that runs from southern Norway through Dalsland, Skaraborg and Östergötland, continuing under the Baltic Sea into southern Finland and Russia as the Salpausselkä moraine which separates lakes Ladoga and Saimaa.

In general, estimating the ages of moraines is difficult. A retreating glacier will deposit successive moraines but an advancing one can destroy older moraines less extensive than the glacier advance. Dates obtained from organic material behind a moraine may be considerably younger than the moraine as its development occurs with a lag from deglaciation, while organic matter in or underneath a moraine may be considerably older. Changes in sediment fluxes to lakes west of Quelccaya appear to reflect advances and retreats of glaciers, with meltwater formed during retreats increasing sediment fluxes.

The Waterloo Moraine is a landform and sediment body that was created as a moraine in the Regional Municipality of Waterloo, in Ontario, Canada. It covers a large portion of the cities of Waterloo and Kitchener and the township of Wilmot, and some parts of the townships of Wellesley and North Dumfries. About 90% of the water supply of the Regional Municipality of Waterloo is derived from groundwater of the Waterloo Moraine aquifer system. During late 1989 and early 1990, groundwater contamination in Elmira forced the Region to shut down some well fields.

Efforts to establish a trail along the Oak Ridges Moraine first began in 1973. The Ontario Trail Riders' Association established the Great Pine Ridge Equestrian Trail located primarily along existing roads and road allowances. In 1991, a group of volunteers gathered through the cooperation of STORM (Save the Oak Ridges Moraine), the Metro Toronto and Region Conservation Authority and Hike Ontario. These volunteers developed the idea of a system of public recreational trails along the full length of the moraine, from Albion Hills in the west, to the Northumberland Forest in the east.

Town of Withrow with the hills that comprise the terminal moraine for the Okanagan lobe of the Cordilleran Ice Sheet immediately behind it. The Withrow Moraine includes erratics on glacial till at the terminus of the Okanogan lobe just north of Withrow. Withrow is an unincorporated community in Douglas County, Washington, United States. Named for a cattleman named J.J. Withrow, Withrow lies at the base of the Withrow Moraine and Jameson Lake Drumlin Field is a National Park Service designated privately owned National Natural Landmark located in Douglas County, Washington state, United States.

Albert Lea Lake is highly eutrophic. Moraine dammed lakes typically fill in, but this process has been exacerbated by agricultural runoff.

In a basal flow in Moraine Park, the slaggy and compact phases show differences in phenocrysts as well as in groundmass.

Drawing of Lake Chicago at the Glenwood Stage showing the Chicago area.The Michigan Lobe of the continental glacier had been growing and receding since 70,000 BCE. The glacier had been static along the Valparaiso Moraine for many years before it again began to recede northward. Around 12,000 BCE the glacier began receding north of the Valparaiso Moraine.

Schüssel Moraine () is a large morainal deposit occupying Schüssel Cirque in the north-central Humboldt Mountains of Queen Maud Land. It was discovered and first plotted by the German Antarctic Expedition, 1938–39, who named the cirque. The moraine was named in association with Schüssel Cirque by the Soviet expedition which obtained air photos of the feature in 1961.

According to the United States Census Bureau, the city has a total area of , of which, is land and is water. Hartford is located within the Kettle Moraine, a large moraine formed when the Green Bay and Lake Michigan Lobes collided. These glacial movements created varied land formations such as kettles, lakes, hills, and kames that distinguish the region.

Recessional moraines are often observed as a series of transverse ridges running across a valley behind a terminal moraine. They form perpendicular to the lateral moraines that they reside between and are composed of unconsolidated debris deposited by the glacier. They are created during temporary halts in a glacier's retreat."Moraine". Columbia Electronic Encyclopedia, 6th Edition (2009): 1.

It is also made from glacial moraine, and is similar in makeup to nearby Fishers Island. The same moraine that Fishers Island is made out of resurfaces in Watch Hill, the village which contains Napatree Point. This region of the Northeastern United States made by glacial moraines from the Wisconsonian glaciation is known as the Outer Lands.

Camp II Point () is a point of ice-cored moraine that extends east into Koettlitz Glacier at the south side of lower Renegar Glacier. So named by the New Zealand Geographic Board in 1994 because the second camp of a NZGS field party led by D. N. B. Skinner, 1977–78, was made on the moraine.

Farris is a 20 km long fresh water moraine-dammed lake near the Norwegian coastal town Larvik. The lake would have been a salt water fjord had it not been dammed by an end moraine left by the latest ice age. Farris is drinking water reservoir for some 170,000 people. The largest island in the lake is Bjørnøya.

Suttle Lake is the result of glaciation during the Pleistocene Epoch, when the Cascade Mountains were buried in ice. A glacier carved out a deep valley leaving a lateral moraine where it stopped. Over time, the moraine trapped water creating the lake. Today, Suttle Lake occupies a long, narrow valley with relatively steep slopes to the north and south.

The developments affected the forests of the Oak Ridges Moraine which supplies water to the GTA, which would cause environmental damage to Toronto. It continued for about two years. There were protests against the clear-cutting of forests of the Oak Ridges Moraine. In about 2001, Bayview began to expand to connect with the rest of Bayview.

In spring 2002, the glacier again approached Bert Point. It pushed a terminal moraine ahead of its face and closed the opening again in July. On August 14, the terminal moraine was washed away after rains had raised the water level behind the dam it formed to above sea level. The fjord could become dammed again, and perhaps permanently.

The lake is formed by spring-loading of the valley of the Kokbulak river (Blue spring), an ancient moraine, and a landslide. This is confirmed by the huge fragments of rocks lying at the foot of a powerful moraine. The length of the reservoir is the width is the Depth is very small. on average , but no more than .

Kettleby has a continental climate moderated by the Great Lakes and influenced by warm, moist air masses from the south, and cold, dry air from the north. The Oak Ridges Moraine affects levels of precipitation: as an air mass arrives from Lake Ontario and reaches the elevated ground surface of the moraine, it rises causing precipitation.

During World War I, the Delco plant in Moraine, Ohio, was expanded to manufacture the De Havilland DH.4 bomber, the only American-built airplane to see action in World War I. More than 3,000 were built in Moraine for the Dayton-Wright Airplane Company. Delco was also one of the manufacturers that produced the Liberty aircraft engine.

The plan was released in October 2001, and was both praised and condemned. It became the basis for the Oak Ridges Moraine Conservation Act, dividing the area into four zones of increasingly stringent controls on development. Under the Act, only eight percent of the moraine can be developed, and only in lands designated as "settlement areas".

A large patch of Wisconsinan Till Moraine occurs along the upper reaches of the stream, and beyond it there is Wisconsinan Till.

On the sides of the moraine, wave-cut terraces and segments of raised shoreline indicate the former limit of glacial Lake Agassiz.

Sand, gravel, clay, moraine, and in the valleys and basins of the rivers silt, sand and river peat predominate on the surface.

By the end of 2016 the plant brought an estimated $280 million to the Ohio economy and employed 2,000 people in Moraine.

In each case they are growing on glacial till or, more commonly, a glacial moraine with much deeper soil and water availability.

There are ongoing conflicts between conservationists and developers over land use. Most contentious is the conflict use of the Oak Ridges Moraine.

Through Indiana, the moraine forms a "continental divide" between the drainage of the Great Lakes and the Gulf of Mexico by the Mississippi River.Environmental Setting of the Upper Illinois River basin and Implications for Water Quality; Water-Resources Investigation Report (WRIR) 98-4268, Dept of the Interior, U.S. Geological Survey; Urbana, Illinois, 1999 The moraine then turns northeast, passing just north of La Porte, Indiana, through the county of the same name. Upon entering Michigan the moraine forms much of the shoreline of Lake Michigan northward through St. Joseph. From here northward the moraine angles more eastward, missing Holland and passing through Grand Rapids, finally ending in a mingling of inter-lobe moraines about northwest of Grand Rapids in Montcalm County.Moore, Powell A.; The Calumet Region, Indiana’s Last Frontier; Indiana Historical Collections, Vol.

Lake Wayne was correlated with the Two Creeks Interstade and with eastward drainage into the Hudson River.Leverett and Taylor (1915), Hough (1958), and Bretz (1966), Field studies in western New York are inconclusive.Strand Lines and Chronology of the Glacial Great Lakes in Northwestern New York; Parker E. Calkin; Department of Geological Sciences, State University of New York at Buffalo; The Ohio Journal of Science 70(2): 78, March, 1970 Based on studies of the Buffalo Moraine, the Alden Moraine, and the Niagara Falls Moraine it is believed that a local series of rapid glacial melting led to sand and gravel deposition, followed by an advance of the ice sheet. Because subdued pebble beach ridges, the Wayne Lake may have persisted until the ice margin had retreated north to near the Niagara Falls Moraine.

In particular, the unexpected activism of exurban homeowners and urban environmentalists protesting applications for development on the Oak Ridges Moraine "challenged urban sprawl…and introduced the notion of integrated regional planning that would simultaneously preserve nature and control development." To address these concerns, the Harris government articulated a "smart growth" vision for development in the GGH region and established multi-stakeholder regional smart growth panels in April 2001. The Oak Ridges Moraine Conservation Act, 2001 introduced significant land use and development restrictions in designated areas throughout the Oak Ridges Moraine. While this partially addressed the smart growth goal of ecological preservation, it failed to enact any controls on urban expansion in others areas throughout the GGH or address concerns over preservation of prime agricultural lands outside the Moraine.

The moraine was mapped and named by the Northern Party of the British Terra Nova Expedition (1910–13), in association with Hells Gate.

The low ridge of the Westerberg an end moraine from the Saale glaciation period lies in the vicinity of Lamstedt's locality of Rahden.

Surficial geology in the area mainly consists of alluvium, Boulder Colluvium, Wisconsinan Till Moraine, Wisconsinan Till, and bedrock consisting of sandstone and shale.

Bowmanville Creek, to the east, also has its headwaters in the Oak Ridges Moraine, while Farewell Creek, that lies between them, stops short.

The river rises from several short headstreams in southern McLean County that arise from a glacial moraine southeast of Bloomington- Normal, Illinois. Part of the moraine is publicly owned as the Moraine View State Recreation Area. The river's course forms a large arc through central Illinois, first flowing east into Champaign County, Illinois, south through Mahomet, then west through Monticello and Decatur, then turning northwest to flow along the north side of Springfield. It receives Salt Creek at , approximately north-northwest of Springfield; then the river turns west, forming the southern boundary of Mason County with Menard and Cass counties.

The north of the county was shaped by earlier glaciers, which deposited glacial till, the basis for the heavy soil there. The Marshfield moraine in the northwest corner is probably a terminal moraine from one of these earlier glaciers, or from a series of them. Its age is unclear, but its relatively smooth surface indicates that it has eroded for a much longer time than the choppy terminal moraines left 13,000 years ago, like the Perkinstown moraine near Medford. Much of the county except for the northeast corner is underlain by a layer of Cambrian sandstone, formed long before the last ice age.

The Oak Ridges Moraine is a pair of large ridges composed of four elevated wedges. It is bounded to the west by the Niagara Escarpment, a cuesta which was critical to the formation of the moraine, and to the east by the Trent River and Rice Lake. The four wedges (Albion, Uxbridge, Pontypool and Rice Lake from west to east) formed in stages, though some synchronous formation also occurred at an early period of formation. The moraine peaks at the Uxbridge wedge, generally rising from east to west, a result of the moraine's west-to-east formation.

A media campaign by environmental groups built on the public opposition of the developments, and the issue was transferred to the Ontario Municipal Board (OMB) in 2000. By May 2001, with the issue still unresolved, the provincial Conservative government announced a six-month moratorium on moraine development. A panel was formed to create a land-use plan consistent with the current "smart growth" policy. The plan was released in October 2001, and became the basis for Bill 122, the Oak Ridges Moraine Conservation Act, 2001, which divided the moraine into four zones with increasingly stringent controls on development in each.

The Act prevented development of over 92% of the land mass of the moraine and only those development projects which had already received zoning and planning approval were allowed to be completed. During the provincial election of 2003, the Liberal Party of Ontario promised to terminate development on the moraine as part of their election campaign. The government, in its attempt to halt developments, proposed the North Pickering Land Exchange. This involved exchanging government-owned public lands in North Pickering (the Seaton lands) for privately owned lands on the Oak Ridges Moraine in Richmond Hill and Uxbridge.

Use of the moraine is currently under dispute; environmental groups such as the Sierra Club maintain the area's delicate ecosystems are threatened by development pressures. Attractive forests and hilly relief typical of the moraine are a magnet for developers looking for building opportunities in the densely populated Greater Toronto Area. However, many planners and residents see a need to preserve the moraine from the negative aspects of urban sprawl. Moreover, because it is a rich resource for sand and gravel, it has become a significant source of materials for the aggregate industry of the Greater Toronto Area.

This moraine path of the Mauricie, between Saint-Paulin at the west end and Saint-Raymond at the East end, is about 120 kilometers long. It is referred to as "Saint-Narcisse Moraine" because this moraine is more prominent at the height of Saint- Narcisse. This geological formation was shaped about 11,000 years ago, at the end of the last glacial period, with the deposition of various layers of rock at the foot of the gigantic glaciers.Marcel Trudel, "Saint-Narcisse-de- Champlain, au pays de Batiscan" (Saint-Narcisse-de-Champlain, in the country of Batiscan), Municipality of Saint-Narcisse, 2001, page 23.

The other path of the fork followed the east side of the river and angled cross- country to King Creek, joining the other fork before crossing the river near Nobleton, some north of Lake Ontario. From there it runs north over the Oak Ridges Moraine to the western branch of the Holland River, and from there north-east into Lake Simcoe some north. A second route of the trail runs from Lake Ontario at the Rouge River, following the river northwest to the Oak Ridges Moraine. Crossing the Moraine it met the eastern branch of the Holland River near Aurora, Ontario.

Lake Bassano was a proglacial lake that formed in the Late Pleistocene during the deglaciation of south-central Alberta by the impoundment of a re- established drainage system and addition of glacial meltwater. It is associated with the development of through-flowing drainage within the Red Deer River basin in particular, and the South Saskatchewan drainage network in general. Approximately 7,500 square kilometers of the Bassano basin is covered with lacustrine sediments. These sediments are bordered by the topographically higher Buffalo Lake Moraine to the west, the Suffield Moraine to the east and the Lethbridge Moraine to the south.

The Damme Hills are part of a series of ice age end moraines from the part of the Saale glaciation, the so-called Drenthe I stage. The Lingen Heights, the Ankum Heights, the Kellenberg and the Brelinger Berg also belong to this push moraine, also called the Rehburg Phase, which can be dated to about 230,000 years ago. The Rehburg Hills by the lake of the Steinhuder Meer, are not, however, part of the moraine. Together with their almost symmetrical counterpart, the Ankum Heights, the Damme Hills display the most marked glacial lobes of this push moraine.

The Ankum Heights are part of a series of ice age end moraines from the early part of the Saale glaciation, the so-called Drenthe I stage. The Lingen Heights, the Damme Hills, the Kellenberg and the Brelinger Berg also belong to this push moraine, also called the Rehburg Phase, which can be dated to about 230,000 years ago. The Rehburg Hills by the lake of the Steinhuder Meer, are not, however, part of the moraine. Together with their almost symmetrical counterpart, the Damme Hills, the Ankum Heights display the most marked glacial lobes of this push moraine.

The development of MacLeod's Landing, as it is now known, was completed in late 2005. One of the developers, Brookfield Homes, had used the Oak Ridges Moraine Conservation Plan as a marketing device, claiming that "as one of the last approved developments on the Oak Ridges Moraine, rest assured that the preservation of the natural landscape that surrounds you is forever." The other developers of the community were Kaitlin Group and Aspen Ridge Homes. The site was desirable for development because of the presence of Phillips Lake and a dozen other small kettle lakes, regular features throughout the Oak Ridges Moraine.

Preliminary research on the hydrology of the Oak Ridges Moraine began in the 1970s, but a broader research effort including the impact of urban development on the aquifer system and Great Lakes water quality was established in 1993. The research locus is the Geological Survey of Canada and the University of Toronto Groundwater Research Group, though other groups have made substantial contributions to this project. The moraine serves to recharge streams and rivers in the surrounding region, acting as an underground reservoir. Rain and snow melt slowly soak into the moraine, being filtered and purified in its many sand and gravel aquifers.

To the east of the Thimble Islands, inland moraines along the Connecticut coast include the broken Madison Moraine and the Old Saybrook Moraine. The Long Island Sound basin existed before the glaciers came. It probably had been formed by stream flows. A relatively thick cover of sand and gravel (termed outwash) was left in the basin from glacial meltwater streams.

The Valparaiso Moraine forms part of the Saint Lawrence River Divide, bounding the Great Lakes Basin. Water on one side of the moraine flows into Lake Michigan, through the Great Lakes, and eventually into the Atlantic Ocean via the Saint Lawrence River, while water on the other side flows into tributaries of the Mississippi River, which eventually flows into the Gulf of Mexico.

Turning eastward, the moraine enters Indiana. The moraine is wide as it passes through Lake County, Indiana,Moore, Powell A.; The Calumet Region, Indiana’s Last Frontier; Indiana Historical Collections, Vol. XXXIX; Indiana Historical Bureau, Reprint 1977 covering nearly half of the county's midsection. As it passes through Porter County, Indiana, it is under the city of Valparaiso, from which it derives its name.

The drumlins are oriented in a northeastern direction reflecting the movement of the ice sheet. The northeast corner of the township is situated upon the Dummer Moraine. Moraines are buildup areas of rocks and soil pushed by glaciers as they move. The soil of the Dummer Moraine is characterized by the presence of an excessive amount of rocks and boulders.

Moraine landscape Menzingen has an area, , of . Of this area, 62.5% is used for agricultural purposes, while 28.3% is forested. Of the rest of the land, 7.6% is settled (buildings or roads) and the remainder (1.5%) is non-productive (rivers, glaciers or mountains). The municipality is located on a moraine plateau between the Lorze and Sihl rivers at an elevation of about .

There is a large Adélie penguin colony on a raised beach called Cadwalader Beach at the south-western end of the island. The island also has several breeding colonies of south polar skua. The island has an extensive area of vegetation on a moraine bench above the beach at the north end of the island. The moraine bench is up to wide.

The last Ice Age pushed large amounts of gravel and stones ahead of it, and deposited it as a moraine through all of Vestfold, known as Vestfoldraet. Raet meets the ocean at Mølen, where the moraine sinks into the sea. Its encounter with the Skagerrak ocean waves has uncovered and polished the huge round stone floor for centuries.Bertelsen, Hans Kristian (1998).

In the east of the Netherlands, remains are found of the last ice age, which ended approximately ten thousand years ago. As the continental ice sheet moved in from the north, it pushed moraine forward. The ice sheet halted as it covered the eastern half of the Netherlands. After the ice age ended, the moraine remained in the form a long hill-line.

These are the remaining traces of the Reuss Glacier. The moraine and drumlin landscape of Menzingen and Neuheim are the result of the convergence of the Reuss Glacier and the Linth Glacier. The Swiss geologist Albert Heim (1849–1937) once noted that "this must be the most impressive moraine landscape in Switzerland". The glaciation of the Zug mountains stopped in around 15,000 BCE.

While the moraine is of Wisconsinan age (about 10,000 years before present), the land to the south is of Illinoian age (about 100,000 years before present). The small oil field to the south of the moraine is also attributed to glacial activity: The weight of the glacier to the north created cracks in the underlying bedrock. Oil collected adjacent to these cracks.

Kettle Moraine Scenic Drive generally follows county and local roads. It begins near Whitewater – at the southern expanse of the Kettle Moraine State Forest's southern unit (), the drive takes a northeast trek and passes through six counties: Walworth, Jefferson, Waukesha, Washington, Fond du Lac, and Sheboygan. The route's northern terminus is near Sheboygan County Broughton Marsh Park northwest of Elkhart Lake ().

There is a moraine at the confluence of Coles Creek with Fishing Creek. This causes there to be cone-shaped hills in the area.

West Carrollton City School District is the school district serving Miami Township, Moraine, and West Carrollton, Ohio with an enrollment of over 3800 students.

Well over half of the delta population resides in and near The Pas, situated on The Pas Moraine between the upper and lower deltas.

This morainic ridge extends to Willoughby, Ohio, from Euclid Creek. A portion of the east branch flows along the south edge of this moraine.

On the north side of the moraine is Hollowell Park and the Mill Creek Basin. The steep south side sits above Bear Creek Road.

In Allegan County the moraine has its greatest variation. The highest point is , while the low point near the Kalamazoo River is a little above .

It was formed as a frontal moraine of Perunika Glacier between the 13th and 17th centuries. The feature takes its name from the Vergilov Rocks.

The arms thus symbolise the moraine and glacial path from the Ice ages that runs through the municipality. The colour green symbolises the fertile soil.

Moraine Valley Community College is the area community college. Worth Public Library District operates public libraries.Home. Worth Public Library District. Retrieved on January 20, 2017.

Location of the Nauen Plateau within its surrounding natural regions. The Nauen Plateau () is a low plateau in the German states of Brandenburg and Berlin. It rises above the surrounding countryside by an average of and is a largely contiguous upland area that was formed during the Saale and Weichselian glaciations. It consists predominantly of ground moraine deposits, partly overlain by gently rolling end moraine formations.

Lake Shetek and the surrounding landscape of wetlands and rolling hills are the result of glaciation. The lake lies on the Altamont Moraine, a terminal moraine marking the farthest extent of an ice lobe during the Wisconsin glaciation. This most- recent glaciation deposited a very thick blanket of till over the area. Lake Shetek began forming as the climate started to warm 15,000 years ago.

Moraine Canyon () is a canyon with very steep rock walls, long, indenting northern Nilsen Plateau just west of Fram Mesa, in the Queen Maud Mountains of Antarctica. It was mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1960–64, and was so named by the Advisory Committee on Antarctic Names because the canyon floor is completely covered by glacial moraine.

The Rawson moraine runs west from Rawson and curves to the southwest roughly parallel with the Bluffton moraine Leverett, Frank, Glacial formations and drainage features of the Erie and Ohio basins: Monograph, U. S. Geological Survey, vol. 41, 1902, pp. 566-581 some 2 or 3 miles (3.2 or 4.8 km) north. A third significant ridge runs across Allen, Van Wert and into Adams and Allen counties.

The most distinguishable topographical feature is Cedar Creek Canyon, just north of the city proper near Huntertown. The Fort Wayne Moraine follows two of the city's three rivers: the St. Marys and St. Joseph. The two rivers converge to form the Maumee, which eventually empties into Lake Erie. Land east of the moraine includes the former Great Black Swamp, a lacustrine plain formed by Glacial Lake Maumee.

In areas without an available outlet, the water levels would either continue to rise until reaching one or more low spots along the rim of a moraine, or the ice sheet would retreat, opening access to a lower portion of the moraine. Multiple outlets could form through low spots too until one would become dominant after erosion lowered both the outlet and lake surface.

Wherever a subglacial tunnel began infilling, long winding formations known as eskers would form. The sweeping plain of sand and gravel beyond the ice margin and a terminal moraine is called an outwash plain . The materials left under the glacier when it melts back is called the ground moraine or till plain. Till is highly permeable and creates a large ground reserve for water.

Therefore, Ledyard has its share of interesting glacial geology. The glaciers that covered Ledyard carried the many large boulders that litter the town. The town has set aside land designated as a "Glacial Park" which consists of a section of end moraine and outwash deposits (containing kettles). This area encompasses a segment of the "Ledyard Moraine"—a clast-supported boulder deposit that is anomalous in nature.

Moraine is known for its manufacturing history. From 1917-1923 the Dayton Wright Airplane company operated an aircraft manufacturing plant on the current site of the Moraine Assembly. During its years of operation over 4000 aircraft were built including the DeHavilland observer/bomber plane (a first world war British design). Dayton-Wright was sold to General Motors in 1919 and GM exited the aircraft business in 1923.

The developments affected the forests of the Oak Ridges Moraine which supplies water to the Greater Toronto Area which it was believed would cause environmental damage to Toronto and local communities. It continued for about two years. There were protests against the clear-cutting of forests of the Oak Ridges Moraine. In about 2001, Bayview began to expand to connect with the rest of Bayview.

The depressions filled with snowmelt and rainwater producing kettle lakes. Kettle lakes may be formed within the ground moraine region behind the terminal moraines. They can be of any size and their shorelines can be composed of anything from clay to sand to boulders. In a terminal moraine region, the kettles are fairly small but deep, to fit between the moraine's steep and hilly ridges.

Bierstadt Lake rests on a plateau on the Bierstadt Moraine, which is a "massive" moraine created by debris left from the receding Bartholf Glacier. The glacier, never more than long, "originated on the highest mountain in the park". Because it was a steep glacier, "its gouging action was vigorous". Glacial lobes at Glacier Gorge, Loch Vale, and Flattop Mountain joined and moved iced in Barthlolf Park.

As a result, new land use management guidelines and water protection measures have been enacted. The Waterloo Moraine is the largest of fourteen moraines in the Region, spanning approximately 400 square kilometres. It is an interlobate moraine, consisting primarily of sand and gravel. It contains large aquifers, which discharge into the Grand River and its tributaries and maintain a base water flow rate into that system.

Chicago Heights lies on the high land of the Tinley Moraine, with the higher and older Valparaiso Moraine lying just to the south of the city. According to the 2010 census, Chicago Heights has a total area of , of which (or 99.87%) is land and (or 0.13%) is water. The city's major crossroads are at Dixie Highway (Illinois Route 1) and Lincoln Highway (U.S. Route 30).

Above the Iroquois Plain the topography includes two features, the South Slope and the Peel Plain. The South Slope is the southern part of an interlobular moraine the Oak Ridges Moraine. The South Slope has a gentle slope as well, and experiences relatively high runoff as water infiltration is relatively low. The Peel Plain is mostly clay and generally flatter than the South Slope.

Reuss Ice Age Visitor Center The Kettle Moraine State Forest is a state forest in southeastern Wisconsin. The chief feature of the reserve is the Kettle Moraine, a highly glaciated area. The area contains very hilly terrain and glacial landforms, such as kettles, kames and eskers. The forest is divided into two large and three small units, which are spread across a hundred miles.

Moraines south of Lake Michigan and southwest of Lake Erie. A composite of three maps (Leverett 1915) (Leverett 1902) (Larsen 1986) and other sources. Colors represent moraines from the same time period of the Wisconsin Glacial epochThe Mississinewa moraine runs northeast from the Wabash River at Lagro through Wabash, Whitley, eastern Noble and western and northern Steuben counties, into Michigan.Handbook of Indiana Geology; Publication No. 21; W.N. Logan, Clyde A. Malott,; Indiana Department of Conservation, Department of Geology; 1922 Continuing to the northeast, the moraine crosses into Hillsdale County and the northwestern corner of Lenawee County, where it merges with the younger Wabash moraine.

A detailed geomorphological study of Long Island provides evidence of glacial history of the kame and terminal moraines of the island which were formed by the advance and retreat of two ice sheets. Long Island, as part of the Outer Lands region, is formed largely of two spines of glacial moraine, with a large, sandy outwash plain beyond. These moraines consist of gravel and loose rock left behind during the two most recent pulses of Wisconsin glaciation during the ice ages some 21,000 years ago (19,000 BC). The northern moraine, which directly abuts the North Shore of Long Island at points, is known as the Harbor Hill moraine.

The more southerly moraine, known as the Ronkonkoma moraine, forms the "backbone" of Long Island; it runs primarily through the very center of Long Island, roughly coinciding with the length of the Long Island Expressway. The land to the south of this moraine to the South Shore is the outwash plain of the last glacier. One part of the outwash plain was known as the Hempstead Plains, and this land contained one of the few natural prairies to exist east of the Appalachian Mountains. The glaciers melted and receded to the north, resulting in the difference between the topography of the North Shore beaches and the South Shore beaches.

Beyond the Pittsburgh area, I-79 traverses more rural areas in Butler, Lawrence, Mercer, Crawford, and Erie counties before arriving at its termination point in Erie. In Erie, I-90 provides an important connection from I-79 to Buffalo, New York and the border with Canada. The ghost ramps around the 100 mile marker near Moraine State Park. Around the 100-mile marker on the northbound side are two ghost ramps that were specifically built for the Boy Scouts of America in order to have access to Moraine State Park without having to get on U.S. Route 422 for the 1973 and 1977 National Scout Jamborees, which were held at Moraine.

In the late 1860s both tarns were modified by building dams. A dam was built in 1868 to increase the capacity of Red Tarn and to regulate the beck supplying water to the Low Mill. In Keppel Cove a natural tarn had formed behind a glacial moraine across the floor of the valley. To draw on this water in times of low rainfall, a tunnel was made through the moraine and an 18-inch cast iron pipe laid through it to extract water from the bottom of the tarn. The top of the moraine was flattened and widened, and the work completed in 1871.

The East Arm of the Little Calumet River flows west under the Indiana Toll Road and into Round Lake at Holmesville, then is joined by Carver Ditch on the right, and then on the left by Reynolds Creek, Sand Creek, Coffee Creek, Salt Creek and by the Little Calumet River (west arm), then exits via the Burns Waterway into Lake Michigan. The watershed begins in the physiographic unit known as the Valparaiso Morainal Area. The Valparaiso Moraine, located south of the Lacustrine Plain, is an arc-shaped moraine complex that parallels the southern shore of Lake Michigan. The moraine divides LaPorte and Porter County into northern and southern drainage areas.

Lake Maumee had reached above sea level when the lake poured through a sag in the Fort Wayne Moraine into the ancestral Little River and then the Wabash River. There is some evidence that the final rise in lake level that caused it to overtop the moraine was caused by a minor re-advance of the glacier further east in the basin. The soft till of the moraine was quickly eroded by the volume of water in the lake, releasing a massive volume of water. A second outlet opened at Six-Mile Creek into the St. Marys River and into the Little River Valley.

The headwaters of the river are in the Dundalk Till plain, and the remainder of the river in the Horseshoe Moraine and the Teeswater Drumlin field.

To the north, it is adjacent to the Omemee Esker. The drumlin, part of the Peterborough Drumlin Field, is a rarity on the Oak Ridges Moraine.

1, no. 8, 1950, pp. 461-465. Dirt, dust, or moraine deposit material will fall into the crevasse in the glacier and build up over time.

Fowle is from Miamisburg, Ohio, and worked in the Moraine, Ohio municipal street department. His wife, Tatyana was born in Russia, and they have three children.

The upper portions of the valley was carved by the Reuss Glacier. Large moraine deposits remain at Zetzwil and Gontenschwil. The surrounding hills are largely molasse.

The glaciers then formed a moraine at Waldhof. This was exceeded once more at the Falkau, which marks its maximum extent. After that, the glacier retreated again.

There are several islands within the bay, including Falsen Island at its headwaters. Moraine ridges are found along eastern Victoria Island from Denmark Bay to Greely Haven.

Jackson Elementary School is the public elementary school in Jackson. Kettle Moraine Lutheran High School is a high school of the Wisconsin Evangelical Lutheran Synod in Jackson.

Ski, as most of Follo, lies on ancient rock foundations. Throughout the local area from east to west there is a moraine left from the Ice age.

Travertine is also common, including travertine which preserved a cranial mold of a Neanderthal from Gánovce. Moraine formations remain in the high mountains from the Pleistocene glaciations.

Moraine is located at (39.695650, -84.227677). According to the United States Census Bureau, the city has a total area of , of which is land and is water.

The longest, Bowmanville Creek, to the east, has its headwaters in the Oak Ridges Moraine. The other three watersheds were Tooley Creek, Farewell Creek, and Westside Creek.

Both prominences may represent the remains of "crag and tail" structures from the Wurm glacial episode 10,000 years ago, the Escrick moraine lying further north at York.

Moraine Park Technical College Sign Fond du Lac Campus Moraine Park Technical College (MPTC) is a public technical college with multiple locations in Wisconsin. It is part of the Wisconsin Technical College System. The college features over 100 associate of applied science degrees, technical diplomas and certificates. Traditional classroom, online, and blended formats are available at the college's campuses in Beaver Dam, Fond du Lac, and West Bend.

Moraine Assembly's closing is the subject of the HBO short documentary, The Last Truck: Closing of a GM Plant. It was filmed by local directors Julia Reichert and Steve Bognar with the help of several Moraine Assembly workers. The film was nominated for the Academy Award for Best Documentary (Short Subject) in 2009. The Fuyao Glass plant is the focus of Netflix's American Factory, also made by Reichert and Bognar.

Map of the southwestern coast of Proglacial lake Lake Chicago at the Valparaiso Moraine. The Valparaiso system includes five moraines north of Chicago. The most northerly reach is to the headwaters of the Fox River in Waukesha County, west of Milwaukee. The moraine angles to the south and east, reaching the headwaters of the Des Plaines River west of Kenosha, Wisconsin, in the county of the same name.

The largest Cenozoic volcanic areas in Germany are the Vogelsberg Mountains, the Westerwald, the Rhön Mountains and the Eifel. In northern Germany, almost the entire surface geology is made of Cenozoic sediments, mainly of Pleistocene and Holocene glacial or fluvioglacial deposits. Moraines and urstromtals determine the relief . Thus the Southern Ridge (German: ) is a moraine of the Saale glaciation and the Northern Ridge (German: ) is a moraine of the Weichselian glaciation.

Glaciers act much like a conveyor belt, carrying debris from the top of the glacier to the bottom where it deposits it in end moraines. End moraine size and shape are determined by whether the glacier is advancing, receding or at equilibrium. The longer the terminus of the glacier stays in one place, the more debris accumulate in the moraine. There are two types of end moraines: terminal and recessional.

Medial moraines, Nuussuaq Peninsula, Greenland. A medial moraine is a ridge of moraine that runs down the center of a valley floor. It forms when two glaciers meet and the debris on the edges of the adjacent valley sides join and are carried on top of the enlarged glacier. As the glacier melts or retreats, the debris is deposited and a ridge down the middle of the valley floor is created.

The glacial origin of the Kettle Mucubají is evident because of the visible footprint left by the Mucubají ravine tens of thousands of years ago. This ravine was created by the action of a receding glacier, which was also sealed by an accumulation of unconsolidated glacial debris (moraine) created by the lake. This moraine changed the course of the ravine from Rio Chama to Rio Orinoco and to the Atlantic Ocean.

Nearly all of Minnesota's glacial landforms derive from the last of them, the Wisconsin glaciation. One feature of this time in the park are the rock ridges near the campground, scoured smooth by the glacier and known as roches moutonnées. Another is the Thomson Moraine, a ridge along the northwest boundary. This terminal moraine comprises rock and debris dropped at the farthest reach of the Laurentide Ice Sheet's Superior Lobe.

Whitchurch–Stouffville has a continental climate moderated by the Great Lakes and influenced by warm, moist air masses from the south, and cold, dry air from the north. The Oak Ridges Moraine affects levels of precipitation: as air masses arrive from Lake Ontario and reach the elevated ground surface of the moraine, they rise causing precipitation.Cf. Toronto and Region Conservation Authority, Rouge River Watershed Plan Report (2007), 15.

Monson Lake State Park lies on a band of lakes and rolling hills called the Alexandria Moraine. This moraine was formed by rocks and sediments dropped by the Wadena Lobe of the Laurentide Ice Sheet 30,000 years ago during the last glacial period. The whole region is thickly blanketed with till thick. Blocks of ice that broke off from the glacier melted in place, forming the park's trio of kettle lakes.

The park was the location of the 1973 and 1977 National Scout Jamborees. Moraine State Park is at the intersection of Interstate 79 and U.S. Route 422 and shares a border with Jennings Environmental Education Center to the north. Moraine State Park was chosen by the Pennsylvania Department of Conservation and Natural Resources (DCNR) and its Bureau of State Parks as one of "25 Must- See Pennsylvania State Parks".

Khufu Corrie () is a cirque roughly across formed between Drune Hill to the north and Khufu Peak to the south on the east coast of Alexander Island, Antarctica. It was referred to as the "Fossil Bluff Glacier" in scientific reports in the early 1960s, Fossil Bluff being nearby, and is sometimes referred to today as "Moraine Corrie" and "Moraine Corrie Valley". The name is derived from Khufu Peak.

Rogen Nature Reserve () is a nature reserve in Jämtland County in Sweden. It is part of the EU-wide Natura 2000-network. The nature reserve is centred on Lake Rogen and is part of a wider network of nature protection areas that extend also on the other side of the border with Norway. The landscape is distinctly characterised by Rogen moraine, a type of moraine named after the area.

At its western end, near Delphi in Caroll County, the Packerton moraine is wide. It is on the north side of the Wabash River as far as Logansport, continuing along the north side of the Eel River. In Miami and Wabash Counties the moraine is wider and further from the Eel River, separated by a belt of outwash wide. Its hummocky topography shows numerous kames, eskers and lakes.

The Mosquito Creek Valley was originally formed by glaciers. The rolling wooded hills and moraines in the region formed where the glacier stopped, creating a ridge along the ice front. One moraine known as the Farmersville moraine surrounds the valley on three sides. There are mounds of sand and gravel deposits, called kame, from water melting along the glaciers' edge along the southeastern end of what is now Kiser Lake.

Schomberg has a continental climate moderated by the Great Lakes and influenced by warm, moist air masses from the south, and cold, dry air from the north. The Oak Ridges Moraine affects levels of precipitation: as an air mass arrives from Lake Ontario and reaches the elevated ground surface of the moraine, it rises causing precipitation.Cf. Toronto and Region Conservation Authority, Rouge River Watershed Plan Report (2007), 15.

Lake Shetek and the surrounding landscape of wetlands and rolling hills are the result of glaciation. The lake and park lie on the Altamont Moraine, a terminal moraine marking the farthest extent of an ice lobe during the Wisconsin glaciation. This most-recent glaciation deposited a very thick blanket of till over the area. A well just outside the park was drilled through of till without reaching bedrock.

Oshawa Creek is a watercourse that flows from its headwaters in the Oak Ridges Moraine to its mouth on Lake Ontario, at Oshawa, Ontario. It drains a watershed of . In its lowest reaches, in Oshawa, two tributaries, Goodman's Creek and Montgomery Creek, join the watercourse. To the west it borders Lynde Creek, which also has its headwaters in the Oak Ridges Moraine, and the shorter watercourses Pringle Creek and Corbett Creek.

Earth Science ANSIs display significant geological features representative of their region. The Linton-Kelly Lake Channels "marks the junction of the Oak Ridges Moraine and the Palgrave Moraine". It is a 588 hectare region at which the two moraines merge. The Glenville Hills Kames are kames in the northeast portion of the township, southwest of central Newmarket, that mark "the southernmost advance of Lake Simcoe sublobe during [the] Port Bruce Stadial".

Kettle Moraine High School (KMHS) is a secondary school located in Wales, Wisconsin. It serves students from Delafield, Dousman, Eagle, Genesee, North Prairie, Ottawa, Sullivan, Summit, and Wales. It is accredited by the North Central Association of Colleges and Schools (NCA CASI).Institution Summary, AdvancED, Retrieved 2012-07-08 Kettle Moraine was named a National Blue Ribbon School of Excellence in 2002 by the U.S. Department of Education.

Lloydtown has a continental climate moderated by the Great Lakes and influenced by warm, moist air masses from the south, and cold, dry air from the north. The Oak Ridges Moraine affects levels of precipitation: as an air mass arrives from Lake Ontario and reaches the elevated ground surface of the moraine, it rises causing precipitation.Cf. Toronto and Region Conservation Authority, Rouge River Watershed Plan Report (2007), 15.

Pottageville has a continental climate moderated by the Great Lakes and influenced by warm, moist air masses from the south, and cold, dry air from the north. The Oak Ridges Moraine affects levels of precipitation: as an air mass arrives from Lake Ontario and reaches the elevated ground surface of the moraine, it rises causing precipitation.Cf. Toronto and Region Conservation Authority, Rouge River Watershed Plan Report (2007), 15.

Located in the fertile Holland Marsh, the area is considered to be the Breadbasket of Ontario. The Ansnorveldt Wetland Complex, which is a provincially significant wetland area, is located on the edge of the Holland Marsh; its southern extent reaches the northern slopes of the geologically important Oak Ridges Moraine. The wetlands in the complex are hydrologically connected along a discharge zone at the base of the Oak Ridges Moraine.

The most accepted theory of the development of the Oak Ridges Moraine is that proposed by Barnett et al. (1998). "Moraine development is highlighted in four stages and evolved rapidly from a glaciofluvial-dominated core to flanking glaciolacustrine-dominated wedge sediments." (Barnett et al., 1998, pg 1160) The four distinct stages of the model are: # subglacial sedimentation, # subaqueous fan sedimentation, # fan to delta sedimentation, and # ice-marginal sedimentation.

King City has a continental climate moderated by the Great Lakes and influenced by warm, moist air masses from the south, and cold, dry air from the north. The Oak Ridges Moraine affects levels of precipitation: as an air mass arrives from Lake Ontario and reaches the elevated ground surface of the moraine, it rises causing precipitation.Cf. Toronto and Region Conservation Authority, Rouge River Watershed Plan Report (2007), 15.

Loess covers most of the hills and forms the parent material of a brown silt loam soil. The lake is surrounded by a mixed conifer-deciduous forest and the Baraboo Hills are also home to one of the largest contiguous hardwood forests in the Midwest. North Glacial Moraine is well covered by the north shore developments. The parking lots, concession building and the picnic shelter all sit atop the moraine.

This increase in glacial lake formation also indicates an increase in occurrence of glacial lake outburst flood events caused by damming and subsequent breaking of moraine and ice.

Alluvium, Wisconsinan Outwash, Wisconsinan Till, Wisconsinan Ice-Contact Stratified Drift, Wisconsinan Bouldery Till, Wisconsinan Till Moraine, and bedrock consisting of shale and sandstone all occur near the creek.

To the north are ground moraines that have been deposited over a large area. Only south of Ludwigsfelde, does the contiguous ground moraine plateau of the Teltow begin.

She is buried in Mount Auburn Cemetery with her husband. The monument is a boulder selected from the moraine of the Aar Glaciers, near where Agassiz once lived.

Ongoing urban growth, mostly low-density residential suburbs (in accordance with requests by land developers), will cover increasing amounts of the remaining undeveloped portions of the Waterloo Moraine.

The Little Rouge River which flows through Cedar Grove is a tributary of the Rouge River, with water flowing south from the Oak Ridges Moraine to Lake Ontario.

Physical characteristics include a gravel and sand moraine ridge on its southwestern shore. There are also tidewater glaciers. The main discharge of Lefferts Glacier is into Rosse Bay.

Ellis, Cathy - Moraine Lake's Rockpile Trail to receive upgrades. Rocky Mountain Outlook, August 28, 2008 That view of the mountains behind the lake in Valley of the Ten Peaks is known as the "Twenty Dollar View", as Moraine Lake was featured on the reverse side of the 1969 and 1979 issues of the Canadian twenty dollar bill. The area is plagued by traffic jams and parking chaos due to out-of-control tourism.. Bank of Canada - 1969-1979 Canadian $20 Bank note featuring Moraine LakeWeddell, Peggy - Banff: A Rocky Mountain Treasure. Legion Magazine, January 1, 1997 Along the same trail-head, the Consolation Lakes trail starts, which is approximately long, with an elevation change of .

The Lehigh Valley starts at the terminal moraine of the Wisconsin Glacier slightly north of Belvidere. It extends from the Delaware River south to where the Musconetcong River goes into the Delaware River, northeast to the Jenny Jump Mountains and then along Route 80 to the Allamuchy Mountains to the terminal moraine near Hackettstown. The Kittatinny Valley is north of the terminal moraine; it runs north of Belvidere, to south of Great Meadows, then east to the north of Hackettstown. Towns such as Blairstown, Johnsonburg, Hope and Allamuchy are in the Kittatinny Valley The highest elevation is above sea level on the Kittatinny Ridge, at two areas just south of Upper Yards Creek Reservoir, west of Blairstown.

Yeager Rock, a haystack rock resting on ground moraine composed of glacial till on Waterville Plateau, Washington, USA Boulder Park National Natural Landmark, of Douglas County, Washington, along with the nearby McNeil Canyon Haystack Rocks and Sims Corner Eskers and Kames natural landmarks, illustrate well-preserved examples of classic Pleistocene ice stagnation landforms that are found in Washington. These landforms include numerous glacial erratics and haystack rocks that occur near and on the Withrow Moraine, which is the terminal moraine of the Okanogan ice lobe.Bjornstad, B., and Kiver, E., 2012, On the Trail of the Ice Age Floods: The Northern Reaches: A geological field guide to northern Idaho and the Channeled Scabland. Keokee Books, Sandpoint, Idaho.

The south western margin of Moraine Dome is wrapped by a broad, striped granite apron with an approximately 40° slope that appears to rise some from the valley floor.

The municipality (originally the parish) is named after the old Rovde farm (). The first element of the name is which means "moraine" and the last element which means "meadow".

The southern margin of the glacier exhibits a forefield exposed since the retreat from the 'Little Ice Age' maximum with a well formed end moraine marking a former margin.

The lake district was shaped by glaciers during the Pleistocene ice age. Many of its hills are parts of moraines and many of its lakes are moraine-dammed lakes.

Ford Heights is located at . According to the 2010 census, Ford Heights has a total area of , all land. The village lies on the edge of the Tinley Moraine.

Lowell's request was turned down in 1991. Lowell lies on the Valparaiso Moraine, almost on the Kankakee Outwash Plain. The town also lies near the St. Lawrence Seaway Divide.

The southern arm runs to the southeast from the Wabash along the northern shore of the Mississinewa River from which it takes its name. It crosses the northeast and eastern half of Grant County and its county seat, Marion. Turning eastward across Blackford County, entering Ohio south of Fort Recovery in Mercer County. In a sweeping arc across northern Mercer County, the Mississinewa moraine merges with the St. Johns moraine in Auglaize and Shelby counties.

Forbidden Valley is a valley to the south of Citadel Peak in the Hays Mountains of Antarctica. The valley drains east-northeast from Mount Crockett to Scott Glacier and is partly covered by glacier and moraine. It was visited in December 1987 by a United States Antarctic Research Program – Arizona State University geological party led by Edmund Stump. The mouth of the valley is blocked by a moraine which denies easy access, hence the name.

It rises from the base of the Annapurna massif, and flows south and south-east past Pokhara and Damauli to join the Trishuli River near Devghat. The lakes of Pokhara were created through a geological process. As the Seti river carried the moraine from Annapurna Himalayas after the burst of glacial lakes at various pre-historical time periods, the moraine were deposited on the routes of the rivers. This caused formation of natural lakes.

Moraine State Park is a Pennsylvania state park on in Brady, Clay, Franklin, Muddy Creek, and Worth townships in Butler County, Pennsylvania, in the United States. The park's main feature is its man-made lake, Lake Arthur, formed by impounding Muddy Creek, which is and is used for recreational purposes. The surrounding park is used for hiking, bicycling, group camping, picnicking, and hunting. Moraine State Park hosts the annual Regatta at Lake Arthur in August.

Just to the west of the city is Baden Hill, in Wilmot Township. This glacial kame remnant formation is the highest elevation for many miles. The other dominant glacial feature is the Waterloo Moraine, which snakes its way through the region and holds a significant quantity of artesian wells, from which the city derives most of its drinking water. The settlement's first name, Sandhills, is an accurate description of the higher points of the moraine.

Schreiner, map Sections od end moraine connecting these to the Constance section may have been eroded away, or they may never have existed due to water movement during the Constance stage. Originally, most of the basin floor was swampy or even rather wet. The moraines, however, were suitable for human settlement. The moraine of Constance has been the location of several prehistoric and early historic settlement, among them a Roman predecessor of Constance.

The high ground at either side is formed by a legacy of the last ice age, the recessional Llanfoist moraine which underlies both the village which gives it its name, the town centre and the Nevill Hall area. The older parts of the town north of its centre are built upon a relatively flat- lying alluvial fan extending west from the area of St Mary's Priory to Cantref and of similar age to the moraine.

The linear "street" village of Newton is not however placed along the old pathway along the top of the moraine, The Geological map of 1872 shows that there was a line of natural springs and wells along what is now Main Street and therefore the siting of the village offset from the road along the top of the moraine would be a sensible thing to do to capitalise on the existence of water.

The hill chain of the Ruhner Berge, which was designated a protected area in 1994, was heaped up into a terminal moraine by glacial push during the Pomeranian stage of the Weichselian glaciation; thus it is also referred to as a push moraine. Today it is mostly covered by mixed forest. An educational path illuminates the features of nature. The wooded region of the hills is called the Marnitz Beeches (Marnitzer Buchen).

Physiography of the Upper Illinois River Basin South of the Chicago Lake Plain in the central parts of Lake and Porter County and northern LaPorte county is the hilly Wheaton Morainal Plain. The Wheaton Morainal Plain consist of the Valparaiso Moraine and Tinley Moraine, paralleling the Lake Michigan Shoreline. The plain consist of rolling Wisconsinan-age moraines. The Morainal Plain is clayey till, and sandy and loamy till, with areas of sand and gravel.

The retreat of glaciers also spread moraines of different types in the landscape. Besides the terminal moraines, there is also an excellent example of Rogen moraine responsible for the archipelago south of Lake Tärnasjön. A well formed moraine over 3 km long can be seen on the west side of the valley Marsivagge; its origin is still not well understood. A few eskers can also be found in some areas of the reserve.p.

On a clear day, it is possible to get first glimpse of Auden's Col. Gangotri Group Base Camp—Auden's Col Base Camp (4720 m) : Again gradual climb on moraine and ridge through a valley surrounded by Gangotri and Jogin peaks, with glacier flowing on the right. Auden's Col becomes clearly visible and increasingly prominent. Auden's Col Base Camp—Auden's Col Advanced Base Camp (4975 m) : More of gradual climb on moraine and ridge.

According to the 2010 census, Mattoon has a total area of , of which (or 99.96%) is land and (or 0.04%) is water. Nearby rivers have been dammed to form Lake Paradise and Lake Mattoon south of the city. The terminal moraine of the Wisconsin Glacier is located just to the south of Mattoon. Heading south on I-57 there is an impressive vista from the top of the moraine at the south Mattoon exit.

Moraine deposits can be seen on Cape Cod. Originally hills when the ice retreated, they have eroded and shifted over time to help produce the characteristic arm of the Cape.

Glaciers extended well down the mountain forming moraine ridges, clearly visible now on the southern flanks down to about . At present only a small fraction of the glacial cover remains.

The Greater Toronto Bioregion represents a unique ecosystem that co-exists with the urban sprawl of the Greater Toronto Area. It is also part of the Oak Ridges Moraine system.

The trail travels through the Kettle Moraine region of Wisconsin. The landscape is dotted with glacial landforms. The trail runs along the Milwaukee River near West Bend, including three bridges.

The Hooker Hut on the eastern side of the pass, which was on the traditional route for the crossing, is no longer accessible, but is stranded on an eroding moraine.

According to the 2010 census, Hazel Crest has a total area of , of which (or 99.38%) is land and (or 0.62%) is water. The village lies on the Tinley Moraine.

In modern geology, the term is used more broadly and is applied to a series of formations, all of which are composed of till. Moraines can also create moraine-dammed lakes.

Efforts are being made to preserve undeveloped land on the moraine, and to encourage land owners to leave their property as a legacy to the regional conservation authorities in their wills.

West Deerfield Township is located in Lake County, Illinois. The population was 31,077 at the 2010 census. West Deerfield Township was formed from former Deerfield Township (now Moraine Township) in 1888.

Kettle Moraine Lutheran High School is accredited by the Wisconsin Religious and Independent Schools Accreditation (WRISA), and by the Wisconsin Evangelical Lutheran Synod School Accreditation (WELSSA).Accreditation, accessed July 9, 2007.

Saarnaki laid shown in red. Aerial photograph of Saarnaki laid. Saarnaki laid is an uninhabited, moraine-based island in the Baltic Sea belonging to the country of Estonia. Its coordinates are .

Save the Oak Ridges Moraine (STORM) is a coalition of 25 citizen's groups and individuals dedicated to preserving the ecologically sensitive Oak Ridges Moraine in Ontario, Canada. Formed in 1989, its primary goal has been to lobby the Government of Ontario to create legislation to protect the moraine. The coalition was founded when two groups (one from Peterborough that was supporting a group in Durham Region, and one in King Township) discovered that they had the same name (STORM), and networked with other local groups to organize a first coalition meeting. The brief that the Peterborough group prepared had a significant impact on the Environmental Assessment Advisory Committee who held a hearing to hear perspectives on the disputed land use proposal near Kendall in Durham.

The plant saw some obstacles during the first two years of operation within the United States, including concerns about safety, inability to turn a profit, and politicizing employee concerns regarding the unionization of the Moraine Assembly plant's labor force. Additionally, conflicts arose from clashes in cultural norms and customs between the Chinese and American employees within the Moraine assembly. Shortly after the Moraine Assembly officially opened, the facility was cited by the Occupational Safety and Health Administration (OSHA) for several critical safety violations, including the failure to provide protective equipment, the lack of HAZMAT training, and the failure to properly cover moving machinery. The infractions violated the Occupational Safety and Health Act (United States) of 1970, which prevents employers from knowingly exposing employees to hazardous work conditions.

The village stands on the Escrick moraine which was formed during the retreat of the last Ice Age, some 10,000 years ago. This moraine forms a low ridge, standing above the Vale of York. The ridge, at this point is about above the surrounding countryside which itself is some above sea level it stretches, in a curve, from the west of Escrick in the south to near Stamford Bridge in the north. There were droveways for moving stock and these trackways crossed the vale of York by the natural bridges provided by the moraines. It thus seems likely that there would be a pathway along the top of the moraine along what would now be the road from Wilberfoss and what is now called Back ‘o Newton.

The moraine has no significant feature, but represents a late surge in the glacial lobe.The Erie Lobe Margin in East-Central Indiana, During the Wisconsin Glaciation; William J. Wayne, Indiana Geological Survey; State Geologist, Geological Survey, Department of Natural Resources of Indiana; ca 1970 The moraine in east-central Indiana is covered with low relief ice- disintegration ridges and hummocks crossed by many ice-walled channels and eskers. This creates a rugged terrain in southern Delaware County.

The Moraine Park Technical College District comprises all of Fond du Lac, and Green Lake counties, most of Dodge, and Washington counties, and portions of six other counties. Twenty- six (26) K-12 school districts are found within the Moraine Park Technical College District borders. The college has campuses in Beaver Dam, Fond du Lac, and West Bend; regional centers in Jackson, and Ripon; and offers evening classes at high schools and other facilities throughout the District.

Glacial Lake Chicago when the Calumet Shoreline formedThe Calumet Shoreline is an ancient shoreline of Lake Michigan located in the Lake Michigan Basin. It can be clearly seen as a sand ridge along Ridge Road south of Chicago. Closer to the lake from the Calumet Shoreline, there are the Tolleston shorelines and farther from the lake are the Glenwood Shoreline, the Tinley Moraine, and the Valparaiso Moraine. The shoreline is named after the Calumet Region of Northern Indiana.

Here, all the water flowing off the front of the glacier had to pass westward, for south of glacial Lake Kankakee, the Iroquois Moraine blocked all drainage. Slight though it might be, it was higher than the limestone ridge. Between the Iroquois Moraine and the Momence Ridge, the waters from the glacier collected. Lacustrine deposits are those deposited in lake water, and only when the lake drains or the land rises does it become dry land.

Lake Kankakee was over higher than the current river. It topped the western divide near Morris, Illinois, where a lake had formed as the glacier retreated from the Marseilles moraine. Initially, this water body, drained through numerous gaps in the moraine at the to above sea level, until the gap on the present Illinois River dropped lower than the rest, becoming the outlet for this lake. This outlet crosses exposed bedrock implying that it was a long slow process.

Medial moraines are formed when two different glaciers merge and the lateral moraines of each coalesce to form a moraine in the middle of the combined glacier. Less apparent are ground moraines, also called glacial drift, which often blankets the surface underneath the glacier downslope from the equilibrium line. The term moraine is of French origin. It was coined by peasants to describe alluvial embankments and rims found near the margins of glaciers in the French Alps.

Ashburn is designated as an Oak Ridges Moraine Rural Settlement Area, and development is limited by the Oak Ridges Moraine Conservation Act of 2001. Its surrounding area has a high aquifer vulnerability, and the western edge has a woodland and wetland designated as hydrologically sensitive.Town of Whitby, "Hamlet of Ashburn Secondary Plan," Official Plan: Text (2010), pp. 177-182; Official Plan: Appendix (2010), Schedules R, S, T. The Ashburn subwatershed (which extends as far north as Chalk Lake),Cf.

The greatest portion of Whitchurch–Stouffville lies on the Oak Ridges Moraine.Ontario Ministry of Municipal Affairs and Housing, Land Use Planning: The Oak Ridges Moraine (Map). The moraine consists of knobby hills between 290 and 373 meters above sea level of irregularly bedded layers of unconsolidated sand and gravel (built-up glacial debris) deposited by the meltwater of the Wisconsin glacier some twenty-five thousand to ten thousand years ago.For the following, see Barkey, et al.

Streams and rivers at the top of the Oak Ridges Moraine flow northward into the Lake Simcoe basin, part of the Lake Huron watershed. The southern sections (south of Bloomington Road) make up the headwaters of the Rouge River and Duffins Creek, both of which flow into the Lake Ontario basin.York Region, Official Plan: Oak Ridges Moraine Aquifer Vulnerability Areas and Watershed Boundaries, Map 7. These headwaters include many smaller streams and creeks throughout southern Whitchurch–Stouffville.

The reason for this is the second ice sheet, the Wisconsinan advanced over the area 25,000 to 13,500 years ago and covered over most of the prior glacial deposits.The Kishwaukee River Basin, 1997 Inventory of the Region's Resources. The end moraines that mark where the glacial margin once stood. One of the more visible of these formations is the Marengo Moraine which is a north–south moraine in western McHenry County which extends southwest across northwestern Kane County.

It left behind a bowl shape, deepest at the base of the headwall where the glacial ice had been the deepest and most abrasive. The bowl shape extended to its northeast edge, where there was a terminal moraine of smaller rocks and debris which had been deposited by the glacier. When the bowl-shaped crater filled with water, this terminal moraine acted as a natural dam, helping to contain the water in the newly formed cirque lake.

Taylor formally defined the landform as the Oak Ridges Moraine in 1913. He described its extent to be from King and Maple in the west to the Trent River in the east. He also proposed that its origin was overlapping, interlobate glaciation retreat, between the Lake Ontario Lobe and the older Lake Simcoe Lobe. This has become the accepted explanation for the moraine's development, though research in the 1970s suggested the moraine may not be interlobate.

It collaborates with numerous groups and individuals to achieve common objectives to support a robust and resilient environment across the ORM landscape. These objectives include; undertaking science-based research; providing opportunities for recreation; taking action for the protection and restoration of the ORM and; providing expert advice for environmental planning and policy matters. Local concerns for preserving wildlife habitat on the moraine have increased in recent years. In April 2000, the Oak Ridges Moraine Land Trust was formed.

The Peja glacier which was long, formed the Rugova Gorge, leaving large amounts of moraine material, , which was the biggest moraine in the Balkans region. Low relief settlements along the Mbushtria river include Shtupeqi i Madh and Kuqishta village. Shaped pit settlements include Drelaj, Koshutan, Haxhaj and Llaz-Bellopaqi, which is the deepest pit in the region, formed by tectonic movements or it might be a crater of a volcano. Kuqishta and Shkreli are in the form of hills.

Almost all the landscape elements that originated during the Weichselian Glaciation in the state of Brandenburg are united within the Central Brandenburg Plateaux and Lowlands. These are dominated by ground moraine plateaux of varying extent alternating with wide lowlands. Adjacent to the Nauen and Teltow ground moraine plateaux in the north are the lowlands of Havel, Nuthe and Notte. They are followed by the regions of the Karow Plateau, the Lehnin Land and the heaths of Beelitz and Luckenwald.

The Maple River flows west-northwestward through the upper central part of the county, entering from Freeborn County and exiting to Blue Earth County. The Cobb River also flows through the NE part of the county, from Freeborn to Blue Earth county.Faribault County MN Google Maps (accessed 8 March 2019) The county terrain consists of semi-arid rolling hills, devoted to agriculture. The SE portion is a glacial moraine near Kiester, and is known as the Kiester Moraine.

The wetlands, and Mosquito Creek itself, are fed by natural springs found along the edge of the moraine, as well as rainwater runoff and the natural bowl shape of the area. This drainage and water flows in a generally northwestern direction towards the Great Miami River near Sidney in Shelby County. The eastern side of the moraine drains easterly towards the Mad River.Ramey, Ralph, 50 Hikes in Ohio (4th Edition), The Countryman Press, April 18, 2016, Pg. 132.

American Factory () is a 2019 American documentary film directed by Steven Bognar and Julia Reichert, about Chinese company Fuyao's factory in Moraine, a city near Dayton, Ohio, that occupies Moraine Assembly, a shuttered General Motors plant. The film had its festival premiere at the 2019 Sundance Film Festival. It is distributed by Netflix and is the first film produced by Barack and Michelle Obama's production company, Higher Ground Productions. It won an Academy Award for Best Documentary Feature.

The Dayton region is also known for the many golf courses and clubs that it hosts. The Miami Valley Golf Club, Moraine Country Club, NCR Country Club, and the Pipestone Golf Course are some of the more notable courses. Also, several PGA Championships have been held at area golf courses. The Miami Valley Golf Club hosted the 1957 PGA Championship, the Moraine Country Club hosted the 1945 PGA Championship, and the NCR Country club hosted the 1969 PGA Championship.

Bowmanville Creek is a watercourse in Durham County, that flows from its headwaters in the Oak Ridges Moraine to its mouth on Lake Ontario, at Bowmanville, Ontario. It borders Oshawa Creek, and Soper Creek, to the west and east, which have their headwaters in the Oak Ridges Moraine. Between Bowmanville Creek and Oshawa Creek, there are five smaller creeks, Farewell Creek, Robinson Creek, Tooley Creek, Darlington Creek and Westside Creek. Bowmanville Creek has been dammed in several places.

The Pottageville Southeast Upland, which is contiguous with the swamp, is the only ANSI which is not provincially significant. It is just north of Happy Valley Forest, on the northern slope of the Oak Ridges Moraine. Cold Creek Conservation Area is a park and reserve on the south slope of the Oak Ridges Moraine, northwest of Nobleton, at the southwestern edge of the township. It consists of mature coniferous swamp in its basin, and cedar swamp at its margin.

Born in Oak Lawn, Illinois Kooyenga grew up the oldest of four siblings in the southwest Chicago suburb of Evergreen Park, Illinois. He attended Chicago Christian High School and went on to attend Moraine Valley Community College. Kooyenga played basketball at Moraine Valley and was subsequently recruited by Lakeland College in Sheboygan, Wisconsin where he played NCAA Div III basketball and graduated with honors. Kooyenga earned a Bachelor of Arts in 2000 and MBA from Marquette University in 2007.

The trail is 25 miles long. It passes through the cities of West Bend, Kewaskum, Campbellsport, and ends at the Community Park in Eden, running along the west side of the northern unit of the Kettle Moraine State Forest and crossing the Ice Age Trail. The trail is partially paved and partially covered in crushed limestone. A ribbon-cutting ceremony opening a connection to the Moraine Park Technical College Campus in West Bend occurred on September 4, 2014.

New Zealand 1:50000 Topographic Map series sheet BX15 – Fox Glacier The river passes to the south of an ancient glacial moraine which separates its lower reaches from the Cook River valley.

Also, the primary athletic field at Denison University, Deeds Field, was named in his honor. Deeds died at his home, Moraine Farm, in 1960. He is buried at Woodland Cemetery in Dayton.

The Kettle Moraine Correctional Institution is a medium security penitentiary located 10 miles west of Plymouth, Wisconsin, USA off Wisconsin Highway 67 just east of the Sheboygan/Fond du Lac County line.

These recent tectonic features are found in the central and east, often associated with hot springs. Research published in 1983 indicated seven glacial periods during the Pleistocene, based on terminal moraine distribution.

The estate which covers 533 acres offers birdlife along the coasts of the North Sea and Nissum Fjord. The forested area also contains a moraine landscape around Skovbjerg Bakkesø to the southeast.

The commune covers 716 ha of glacial moraine from the Rhône, deposited about 10,000 years ago, and called the Montagne de Sion. The highest point in the commune is at 733 m.

The material making up these cones can be sorted or unsorted. Sorted moraine material is sorted by water. Sorting refers to the material size. Well-sorted material is all the same size.

The cliffs of the Niagara Escarpment, the rolling terrain of the Vinemount Moraine and the deeply incised gorge of the Forty Mile Creek are the most prominent topographic features of the area.

The soils are markedly less weathered than those of the Old Drift. On areas of ground moraine, the depth of decalcification of the glacial till is thus often less than 1 metre.

Taggart Lake running eastward of the moraine drains Upper and Lower Taggart lakes into the head of the fiord. The Prince of Wales Icefield lies on the eastern flank of this valley.

Washboard moraines, also known as minor or corrugated moraines, are low-amplitude geomorphic features caused by glaciers. The name "washboard moraine" refers to the fact that, from the air, it resembles a washboard.

The Sevetti moraine is a particular assemblage of morainic forms found between Partakko and Sevettijärvi in northern Finland. The Sevetti moraines are disposed in trains about long and wide. They have rugged surfaces.

In 2014, GM Moraine Assembly was purchased from IRG by China-based Fuyao Glass Industry Group Co. Ltd. Fuyao manufactures automotive glass for GM and other automakers. They began operations in late 2015.

Below the Feldsee, between the heaps of moraine, used to be another, smaller lake that, through the formation of peat has silted up to become the present-day, botanically valuable bog of Feldseemoor.

The community lies in a picturesque setting in an ice-age moraine landscape about 500 m in elevation and lends itself well to hiking. In the heights of the moraine that ring the town are lakes, among them the Steinsee, a bathing lake also favoured by visitors from Munich. Somewhat farther away lies the Kitzlsee, a protected landscape. Moosach comprises a number of surrounding hamlets and lone homesteads such as Falkenberg (with a stable and a beergarden), Baumhau, Altenburg and Berghofen.

Stephenson Glacier () is a glacier close west of Dovers Moraine on the east side of Heard Island in the southern Indian Ocean. Its terminus is between Dovers Moraine and Stephenson Lagoon, with part of the glacier flowing to Doppler Hill and Sealers Beach. To the north of Stephenson Glacier is Brown Glacier, whose terminus is located at Brown Lagoon. To the southwest of Stephenson Glacier is Winston Glacier, whose terminus is located at Winston Lagoon, between Cape Lockyer and Oatt Rocks.

A savanna is a naturally occurring area that is open like a prairie with grasses and herbaceous shrubs dominating, but having a substantial canopy from trees. The canopy is less than 80% of the area, but more than 10%. Where the soils is sandy, the dominant trees are black oak and white oak. When the soil is predominately a silty loam, burr oak and other oaks are common. Savanna’s begin along the Tinley Moraine and southward onto the Valparaiso Moraine.

During Ice Ages, glacial activity shaped much of New England’s landscape, eroding mountains, leaving glacial till scattered everywhere, and forming glacial lakes. At its greatest extent, one of these glaciers left behind a moraine which became today's Long Island. One of the biggest glacial lakes of the time was Glacial Lake Hitchcock. It formed when the Laurentide Ice Sheet retreated and glacial meltwater began to accumulate at the glacier's terminal moraine in Rocky Hill, Connecticut and back up into the Connecticut River.

The third, called the 'moraine camp' () lies just below the ice of the first glacier. It is also possible to set up a camp in the col right on the glacier, as there is a convenient flat part. Some parties travel from Huaraz and climb to the moraine camp in one day, then summit and return to Huaraz the next. Climbing involves mostly walking on snow slopes up to 35 degrees, but there is one section of about 100m of steep ice.

Jayne's Hill (also known as High Hill, West Hills, Oakley's Hill, and Janes Hill) is the highest point on Long Island, New York, with an elevation of between and above sea level. It is situated on the Harbor Hill moraine, a terminal moraine that makes up the northern spine of Long IslandQuaternary History of the New York Bight - usgs.gov - Retrieved October 12, 2009 in West Hills County Park in Suffolk County, a little more than a mile to the north of Melville.

The Oak Ridges Moraine Land Trust (ORMLT) is a Canadian charitable non-profit and Land Trust, and has been protecting Ontario's natural legacy since 2,000. Its mission is to ensure a healthy ecosystem and natural environment that thrives forever, on and near the Oak Ridges Moraine. With the help of caring donors, the ORMLT strategically protects land from development, and stewards it to ensure its ecological features and Species-at-Risk thrive. They typically protect land through land donations or conservation easements.

It then passes through the Oak Ridges Moraine, passing a number of parks and conservation areas. North of the moraine the street again enters urban areas, passing through Aurora and Newmarket. It ends in Newmarket where it turns into Prospect Street. Bayview Avenue is also home to major places of worship of almost every major religious tradition including synagogues, an Islamic mosque, the city’s largest evangelical churches, Canada’s largest Buddhist Temple, Toronto’s largest Eastern Orthodox cathedral, and Canada’s only Zoroastrian Temple.

The construction of this portion of U.S. Interstate 55 from 1973 to 1978 greatly reduced the height and area of Mount Fulcher. When U.S. Route 66 was the major highway, Mount Fulcher was a predominant feature of the local landscape, second only to nearby Elkhart Hill. Nevertheless, one can still readily observe a portion of the moraine to the east of the railroad and interstate, while the much larger portion of the moraine on the west side of the Interstate is clearly apparent.

Tower of Babel The Tower of Babel is a conspicuous quartzite monolith at the northern end of the mountain, and is apparent to park visitors at Moraine Lake. It was named in 1899 by Walter D. Wilcox because its profile reminded him of the biblical Tower of Babel. The first ascent of the tower was made in 1959 by G. Boles, B. Greenwood, and A. Washington. Mount Babel acquired its name from its outlier tower that rises above Moraine Lake.

The city is located on the mostly flat Masovian Plain, but the city centre is at a higher elevation than the suburbs. Warsaw is located on two main geomorphologic formations: the plain moraine plateau and the Vistula Valley with its asymmetrical pattern of different terraces. The Vistula River is the specific axis of Warsaw, which divides the city into two parts, left and right. The left one is situated both on the moraine plateau ( above Vistula level) and on the Vistula terraces (max.

The Jungfrau Marathon at km 40 in 2004 Swiss alphorn players and flag-waver Spectators in Wengen Moraine Bagpiper at the moraine The Jungfrau Marathon is one of the best known mountain marathons in the world, in full view of the famous Eiger, Mönch, and Jungfrau mountains in the Bernese Oberland area of the Swiss Alps. The first Jungfrau Marathon was held in 1993. Approximately 3,500 runners from 35 different nations participate. The Jungfrau Marathon takes place each year in September.

Water from the Huron-Erie Lobe came through the upper Tippecanoe valley, spreading across the till plain, in Starke, Pulaski, Jasper, and Newton counties, merging with the shallow waters in the Kankakee basin of St. Joseph, LaPorte, Porter and Lake counties. The meltwaters were trapped between the ice masses to the north and east and the Nebo-Gilboa Ridge, an offshoot of the Bloomington Moraine to the south Chapter VI. The Saginaw Lobe; Frank; Monographs of the United States Geological Survey, Volume LIII, Government Printing Office, Washington; 1915 and the Marseilles moraine. On the west, the Marseilles moraine formed the final and lowest barrier. In the vicinity of Marseilles, Illinois the waters crested the divide and created an outlet into the pre-glacial Mississippi River, creating the modern Illinois River.

28 Coon maintains that the "narrow neck of land" was small enough compared to the lands of Desolation and Bountiful, to be described as being "by" the borders of these lands.Alma 63:5 Olive's mound builder setting identifies the narrow neck with a moraine that is known to have divided New York's ancient Lake Tonawanda into western and eastern portions. This moraine (the Batavia moraine), situates according to Olive, "by the place where the sea [singular] divides the land [Desolation]" Ether 10:20 which may or may not have been visible during Book of Mormon times. says that "they did fortify ... from the west sea, even unto the east; it being a day's journey for a Nephite, on the line which they had fortified ..." (traveling north according to the Tehuantepec theory).

Amesville is located at (39.401497, -81.955134). Amesville is situated in the foothills of the Appalachian Mountains, approximately 45 miles south by southeast of the terminal moraine, a topographical feature often associated with the boundaries of glaciers, and is surrounded by wooded hills, narrow valleys, and numerous creeks flanked by lowland pastures and farmland. These features are largely indicative of the areas in the State of Ohio that fall to the south of the terminal moraine. The terminal moraine in the State of Ohio, and to the north of Amesville, effectively serves to bisect the state along a line running on a west to east axis across the south by southeastern third of Ohio thereby contributing to certain distinctive topographical, socio-economic, and cultural attributes on either side of this feature.

While its rocks are considerably older, Mont Ham is surrounded by moraine that was deposited approximately 12,200 years BP during glaciation. The bedrock of the mountain is composed of boninite in an ophiolite complex.

The elevation rises to the southwest and northeast of the valley. A portion of the area is mantled by moraine deposits. The remainder of the area is covered by glacial till or boulder clay.

Gantenbein, Doug (November 13, 1997). "Re-plumbed pedaler braces for winter". Great Falls Tribune (Great Falls, Montana). p. 3. The same year, their hiking boot Moraine was rated Best Hiking Boot in Backpacker Magazine.

Cascade lake was formed from a mountain glacier that carved out a basin and while it traveled to Lake Tahoe, the glacier deposited debris to form a lateral moraine that separates the two lakes.

Lateral moraine on a glacier joining the Gorner Glacier, Zermatt, Switzerland. In Principles of Geology (first edition, vol. 3, ch. 2, 1833) Lyell proposed that icebergs could be the means of transport for erratics.

Svartknausflya is also the largest moraine area in Nordaustlandet; it measures about . Glacial activity has shaped the landscape in Nordaustlandet through several ice ages. Gentle plateaus and rounded mountains are the most common sight.

Kettle Moraine Lutheran High School offers basketball, cross-country, cheerleading, chess, soccer, fast-pitch softball, track, and volleyball for girls; and baseball, basketball, chess, cross country, football, golf, soccer, wrestling, and track for boys.

Outdoor recreation opportunities include hiking, biking, cross-country skiing, snowshoeing, horseback riding, and snowmobiling. Fourteen trailheads are dispersed throughout the Northern Unit of the Kettle Moraine State Forest and 17 in the Southern Unit.

County Highway J runs concurrent with the Kettle Moraine Scenic Drive through the city. They enter the city from the northwest, run north/south through the center of the city, and exit to the southwest.

Saint Croix Bluffs Regional Park lies atop glacial moraine like much of Washington County. It has some surviving prairies and oak savannas. It borders the Saint Croix River for nearly three quarters of a mile.

Terminal moraines mark the maximum advance of the glacier. Recessional moraines are small ridges left as a glacier pauses during its retreat. After a glacier retreats, the end moraine may be destroyed by postglacial erosion.

In many parts of the park, there are spread-out holes (kettle holes) created by small remains of ice age glaciers, and peculiar small hills called "eskers" made by ground moraine released by melting glaciers.

Moraine belts are usually studied in places with palaeoglacier presented. As for ocean sediments, the variations of alkenone levels and faunal abundances were measured to model paleotemperatures in separate studies showed in the following sections.

Examples of cirques include the Cirque de Pessons in the east, Llac de Tristaina in the northwest, and the two cirques at approximately elevation on Pic de Casamanya (). Santa Coloma has a glacial terminal moraine.

New Prospect is located in the town of Auburn, in Fond du Lac County, Wisconsin, United States. New Prospect is located in the Kettle Moraine State Forest along County Highway SS, east-northeast of Campbellsport.

They frequently terminate at a recessional moraine. Tunnel valleys from successive glaciations may crosscut one another.“Principles of glacier mechanics”; Roger LeB. Hooke; 2nd Edition; 2005; Cambridge Tunnel valleys frequently run along roughly parallel courses.

The Dutchman's Cap View from the Dutchman's Cap The Dutchman's Cap () is a hill with a 24.4 m high bluff, which is in Lithuania's Seaside Regional Park, near Karklė and 2 km north of Giruliai on the Baltic Sea coast. It was created 12000–15000 years ago during the last Baltic glaciation. The hill is a parabolic dune created by Aeolian processes on a moraine ridge. The location is now subject to strong erosion by the Baltic Sea, which is exposing various- sized boulders from the moraine.

Several ground moraine plateaux of Saale and Weichselian glacial origin form the heart of the North Brandenburg Plateaux and Upland. In addition there are sandur and valley sand areas as well as the push and terminal moraine ridges of the Ruhn Hills with heights of up to zu . With the exceptionof the Gransee Plateau in the east, the land descends mainly from north to south. Correspondingly the countryside is drained by the Elde, Löcknitz, Stepenitz, Dosse and Rhin and their tributaries into the Rhinluch and the Elbe.

Moraine Valley () is a valley filled with morainic debris, long, which drains north into Elephant Flats on the east side of Signy Island, in the South Orkney Islands off Antarctica. In summer a stream, fed by the ice slopes at its south end, runs in this valley. It was named by the Falkland Islands Dependencies Survey following their survey of 1947. Orwell Lake is a small lake in Moraine Valley, lying southeast of Orwell Glacier in the east part of Signy Island, South Orkney Islands.

A map of the Waskahegan Trail system. The green areas on the right are, from north to south, Elk Island National Park, the Blackfoot Recreation Area, and Miquelon Lake Provincial Park (north and south blocks). The Beaver Hills (), also known as the Beaver Hills Moraine and the Cooking Lake Moraine, are a rolling upland region in Central Alberta, just to the east of Edmonton, the provincial capital. It consists of of "knob and kettle" terrain, containing many glacial moraines and depressions filled with small lakes.

This section runs parallel to Atlantic Avenue and is aligned with the Crown Heights street grid. East of Ralph Avenue, it turns to the northeast, still following the moraine, until it terminates at Bushwick Avenue near the Evergreen Cemetery, where the moraine climbs steeply toward a peak at Ridgewood Reservoir. The initial portion of Eastern Parkway, west of Ralph Avenue, contains landscaped medians and is officially called by that name. The part east of Ralph Avenue is narrower and is officially known as Eastern Parkway Extension.

Because lateral moraines are deposited on top of the glacier, they do not experience the postglacial erosion of the valley floor and therefore, as the glacier melts, lateral moraines are usually preserved as high ridges. Moraines clearly seen on a side glacier of the Gorner Glacier, Zermatt, Switzerland. The lateral moraine is the high snow-free bank of debris in the top left hand quarter of the picture. The medial moraine is the double line of debris running down the centre-line of the glacier.

Big Thompson River in Moraine Park in the Rocky Mountain National Park The headwaters of the Big Thompson River begin in Forest Canyon within Rocky Mountain National Park in Larimer County, Colorado. The river flows east through Moraine Park to the town of Estes Park. There it is held in Lake Estes by Olympus Dam before being released into the Big Thompson Canyon. The North Fork Big Thompson River also begins in Rocky Mountain National Park, on the northern slopes of the Mummy Range.

The hooded warbler is a threatened species in Canada. Happy Valley Forests is one of the few remaining Canadian habitats for this species. The ecologically diverse moraine is the water source for many headwaters streams flowing south into rivers that drain into Lake Ontario and north into rivers that drain into Lake Scugog and Lake Simcoe. Varied landforms on the moraine, such as woodlands, wetlands, watercourses, kettle lakes and bogs, have provided an environment suitable for significant flora and fauna communities to develop and thrive.

Nobleton is at an elevation of approximately 300 m, just south of the regional peak of the Oak Ridges Moraine. The Humber River flows in the southwestern part with a conservation area covering the southwest. The Oak Ridges Moraine is to the north and is covered with pine forests with a few other types of trees and lakes to the north and the northeast. Nobleton Lakes is located nearly 2 to 3 km north and includes two lakes and a golf and Country Club.

Rising above these lowlands is a geographical region comprising four hilly districts of moraines and moraine-dammed lakes formed during and after the Pleistocene ice age. These lake districts are the Pomeranian Lake District, the Greater Polish Lake District, the Kashubian Lake District, and the Masurian Lake District. The Masurian Lake District is the largest of the four and covers much of north-eastern Poland. The lake districts form part of the Baltic Ridge, a series of moraine belts along the southern shore of the Baltic Sea.

Geographically, the SRD consists of two parts---western and eastern---separated by a prominent moraine (The Pas Moraine) that was deposited by the Laurentide Ice Sheet during late stages of the Wisconsinan glacial epoch. These two components, commonly termed the "upper delta" and "lower delta", together occupy an area of approximately making the SRD one of the largest active inland delta in North America.Page 129 of: The broad wetland tracts of the upper delta in Saskatchewan are sometimes referred to as the Cumberland Marshes.

One is on the road which winds along the north side of Beaver Creek for . The other is a trail that leaves the dirt road, crosses the stream and runs along the south side of the meadow at the base of the moraine. Elk may be seen bedded down among the trees near the trail or along the stream. The trail runs through Upper Beaver Meadows and connects with a number of trails, including Ute Trail, Deer Ridge Trail, Moraine Park, and Windy Gulch.

'View from Battle Hill' by James Smillie. Battle Hill is the highest natural point in Brooklyn, New York, United States, at above sea level. The hill is part of the Harbor Hill Moraine, a terminal moraine formed during the last glacial period. Battle Hill, located in what is today Green-Wood Cemetery, received its name from the battle which occurred on its slopes between American troops under the immediate command of General Samuel Holden Parsons and British troops under the command of General James Grant.

Garvies Point Museum and Reserve: the Geology of Long Island South of the moraines is a broad outwash plain sloping towards the Atlantic Ocean, much of which has been submerged as ocean levels rose in the post-glacial period. The Harbor Hill Moraine forms the major drainage divide in Nassau County: streams to the northwest of the moraine flow into Long Island Sound, whereas those to the south empty into the series of bays or sounds behind the barrier islands and so into the Atlantic.

Illustration of the glacial impacts showing the events leading to formation of Moses Coulee. Pleistocene glaciers advanced onto the Waterville Plateau, with the Okanogan Lobe of the Cordilleran Ice Sheet reaching as far south as the town of Withrow. Evidence for glaciation on the Waterville Plateau includes polished and striated bedrock, glacial erratics, drumlinoid topography, eskers, moraines, meltwater channels, and glacial till. The Withrow Moraine complex marks the maximum southern extent of the Okanogan Lobe, and a series of recessional moraine complexes represent retreating ice margins.

Moraine View State Recreation Area was one of eleven state parks slated to close indefinitely on November 1, 2008 due to budget cuts by former Illinois governor Rod Blagojevich. After delay, which restored funding for some of the parks, a proposal to close seven state parks and a dozen state historic sites, including Moraine View, went ahead on November 30, 2008.Garcia, Monique and Gregory, Ted. "State park closings a tough pill for some to swallow", Chicago Tribune, November 29, 2008, accessed April 12, 2009.

This moraine contains the headwaters for six creeks in Oakville. It is home to 496 plant species, 10 fish species, and 220 animal species, of which 168 are birds, 34 are mammals, and 18 are amphibians.

Moomaw Glacier is an alpine glacier in Rocky Mountain National Park in the U.S. state of Colorado. Moomaw Glacier is almost northeast of Isolation Peak and the old terminal moraine of the glacier impounds Frigid Lake.

The soil was specially treated with fertilizer to allow for the growth of thousands of trees, shrubs and grasses. Lake Arthur was completed in 1970 with the opening of Moraine State Park on May 23, 1970.

Proglacial lakes form as meltwater trapped behind a glacial feature such as an end moraine. These lakes have an intake of sediment deposited by streams within the glacier and their deposits are recorded within the varves.

The municipality is unilingually Finnish. The municipality is probably best known of the moraine region of Rokua, which is a popular summer and sports resort. The popular rockgroup 22-Pistepirkko was formed in Utajärvi in 1980.

The old moraine landscape of Lower Saxony emerged in the course of four great glacial advances of the Scandinavian ice sheet 350,000 to 130,000 years ago – one during the Elster glaciation and three during the Saale glaciation. The glacier of the most recent, Weichselian glaciation only reached the northeastern edge of the present Elbe valley depression, so that the existing terminal moraines beyond that point there were only affected periglacially, for example in the shape of solifluction over the frozen ground, by meltwater erosion and sediments or through wind- blown deposits of sand. The last two Saale glaciation advances in particular, the Drenthe II and the Warthe stadia, unfolded the East Hanonerian Terminal Moraine. It is therefore geomorphologically younger than the geest in western and central Lower Saxony, but clearly older than the young moraine landscapes in Mecklenburg-Vorpommern and Ostholstein (= Baltic Uplands).

Deposits range from in the lower basin (western). The deepest deposits of are in the upper basin (eastern). Along the Valparaiso Moraine, deposits can reach thick. Outwash deposits occur primarily along the northern border of the basin.

About 400 litres of groundwater naturally flow into Öresund from Alnarpsströmmen every second through quaternary moraine. The width of the aquifer is around 20 km, and the flow of the water is just 10 metres a year.

Waite was the head coach at Moraine Valley Community College in Palos Hills, Illinois, leading the Cyclones to the 1985 North Central Community College Conference championship. Waite was named the conference coach of the year in 1985.

Bala Lake lies in a glacial valley blocked by a terminal moraine, but the other lakes are reservoirs created by impounding rivers, to provide drinking water, hydroelectric schemes or flood defences, and many are also used recreationally.

The cool, fresh water is discharged into the headwaters of streams and rivers which eventually flow into Lake Simcoe, Lake Scugog and Lake Ontario. The aquifers are also the water supply for some communities on the Moraine.

Alta Township is a civil township in Barnes County, North Dakota, United States. As of the 2000 census, its population was 98. The township is named after Alta Ridge, a moraine belt overlooking the Sheyenne River Valley.

The village of Hurden is located on a peninsula protruding from the southern shore of Lake Zürich at its narrowest point. The peninsula has its origin in the retreat of the Linth glacier at the end of the last glacial period when Lake Zürich was formed. This retreat left a moraine across the valley now occupied by Lake Zürich. The higher southern section of this moraine extends above the lake's water level and forms the peninsula, whilst the lower northern section forms a shallow section in the otherwise deep lake.

The ice carved through younger sediments exposing more ancient rock. A large terminal moraine was formed in the ocean at the edge of the ice sheet during the first pulse of glaciation, creating Block Island along with Long Island, Martha's Vineyard and Nantucket. The last Wisconsin glaciation began to retreat 18,000 before the present, leaving behind a sediment strewn landscape. Much of the surficial geology of the towns of Westerly, Charlestown and Narragansett resulted from the extensive Charlestown moraine, stretching in a line from Long Island to Fishers Island the southern coast of Rhode Island.

The Seven Lakes water supply of one hundred or more acres consists of small bodies of water at in altitude which flow south into Beaver Creek and then Lake Moraine, a source of water for the city of Colorado Springs by 1899. The seven natural lakes formed by glaciers were: Isoetes Lake, Lake of the Rocks, Marsh Lake, Michigan Lake, Mirror Lake, Ramona Lake, and Ribbon Lake. The city of Colorado Springs purchased Seven Lakes land for $70,000 in 1891. That year they built the Lake Moraine Dam.

The Waldoboro terminal moraine sits on the southeastern coast, while the Highland front moraine parallels the northwestern border. Large continental ice sheets (see Laurentide Ice Sheet) most likely created the large moraines, as it takes time for the long, lumpy ridges to form at a massive scale. New England is best known for its high density of erratics, which are displaced rocks that differ from the immediate bedrock composition of the region and range from the size of pebbles to boulders. Their surfaces are generally rounded and polished due to rasping.

Moraines south of Lake Michigan and southwest of Lake Erie. A composite of three maps (Leverett 1915) (Leverett 1902) (Larsen 1986) and other sources. Colors represent moraines from the same time period of the Wisconsin Glacial epochThe Valparaiso Moraine formed as the first major moraine of the Cary substage of the Wisconsin Glacial period (10,000-50,000 years before present).Hough, Jack L.; Geology of the Great Lakes; University of Illinois Press, Urbana; 1958, pg 97 There are three minor moraines that have been identified in northeastern Illinois, the Minooka, Rockdale, and Manhattan.

On June 3, 2008, GM Chairman Rick Wagoner announced that the Moraine plant would close in December, citing high fuel prices and decreased demand for the SUV and trucks produced by the plant. There were no plans to reconfigure the plant to produce other products.Dayton Daily News, 3 June 2008 issue The last vehicle that rolled off the line was a white GMC Envoy. Workers at the plant in Moraine were given a letter on October 3, 2008,GM spokesman Chris Lee said plant managers shut the line down at 2:30 p.m.

Measurements are more difficult than on other glaciers as a result of the covering of moraine. In 1965 the glacier was about 5.5 km long from head to snout and had an area of just under 6 km². Due to its covering of moraine, variations in these dimensions are less than those of other glaciers of similar size that are not so covered. The meltwaters of the Glacier Noir pass down the Torrent du Glacier Noir, the Gyr, the Gyronde, the Durance and finally the Rhône into the Mediterranean Sea.

Arctic vegetation has distinct postglacial development characteristics compared to more temperate zones of lower latitudes. A study of postglacial moraines conducted in the Canadian Arctic on Ellesmere Island have found that dwarf shrubs of Dryas integrifolia and Cassiope tetragona are often good indicators of vegetation development and progression. Dwarf shrubs have been found to increase with the age of the moraine, with Dryas integrifolia becoming the most predominant. As well the cover of vegetation, including lichens and bryophytes showed consistent increase with the moraine age, suggesting directional vegetation development.

Scenic attractions include the world-famous attractions of the Lysefjord with the mountain Preikestolen ("Pulpit Rock") and the mountain Kjerag. The landscape of Ryfylke is characterized by high mountains in the interior; the highest and wildest are located in the north and are formed by hard, igneous rock. At Haukalivatnet lake (near Lysefjorden) there is a distinct end moraine presumably created by a prehistoric glacier. This moraine led professor Jens Esmark (in 1824) to formulate the theory of an ice age over Scandinavia and other parts of the world.

168 between the Saginaw and the Erie lobes. The northeast-southwest direction of the eskers north of Disko, Wabash County, and the southeast- northwest trend south of there indicated that the part of the Packerton moraine south of Disko was built by the Erie lobe and the part north of Disko by the Saginaw lobe. An esker, Miami County shows a northeast-southwest alignment, providing evidence that Packerton moraine in Miami County was built by the Erie lobe. A small area in the northwestern was deposited by the Saginaw lobe.

The Geology of Miami County, Indiana; William D. Thornbury and Harold L. Deane; Indiana Department of Conservation Geological Survey Bulletin No. 8 ; 1955 It is named the Packerton moraine from the village of Packerton in Kosciusko County. Thirteen kames and eskers complexes are mixed with sand and gravel. The till is, sandier, especially in the part deposited by the Saginaw lobe, than in the lobe passed over some source of sand, whereas the Erie lobe did not. Water-laid or wind-blown sands are found throughout the moraine.

The Grand River flows southward along the city's east side. Its most significant tributary within the city is Laurel Creek, whose source lies just to the west of the city limits and its mouth just to the east, and crosses much of the city's central areas, including the University of Waterloo lands and Waterloo Park; it flows under the uptown area in a culvert. In the city's west end, the Waterloo Moraine provides over 300,000 people in the region with drinking water. Much of the gently hilly Waterloo Moraine underlies existing developed areas.

The Oak Ridges Moraine probably formed in the Late Wisconsin glacial period. Ice melt from the Niagara Escarpment flowed into the western boundaries of the moraine, wherein conduits beneath the ice expanded to form a west-to-east passage between the main Laurentide Ice Sheet and a mass of ice in the Lake Ontario basin. Stratified sediment was deposited rapidly on the high-relief erosional surface. Up to 150 m (500 ft) in some areas, the deposits occurred on surfaces defined by highly eroded channels and drumlin uplands.

The greatest threat to the function of the moraine is land development on and below its surface, particularly in the headwaters. The estimated current population on the moraine land itself is roughly 200,000 but this number continues to grow at a frantic pace, with large urban developments occurring in Stouffville, Vaughan, Richmond Hill, and Aurora. This rapid development is especially apparent in Oak Ridges, where land previously set aside for conservation has, as recently as 2009, been opened up by the Richmond Hill Town Council for development. Another five million people live in close proximity.

Stone Bank is situated about 4.5 miles northeast of the city of Oconomowoc along Waukesha County Highways K and C. It is on the north shore of Okauchee Lake and also has extensive shorelines with Moose Lake. The surface geology of the Oconomowoc region as a whole is glacial, part of the Kettle Moraine region of Southeastern Wisconsin. Okauchee and Moose lakes are both kettle lakes as are all nearby lakes.Wisconsin DNR page on the Kettle Moraine forest's geology The soil is, therefore, very rich with clays and organics, suitable for farming.

Terminal moraines are one of the most prominent types of moraines in the Arctic. One notable terminal moraine is Trollgarden in Norway, once thought to be magically constructed by trolls. In North America, the Outer Lands is a name given to the terminal moraine archipelago of the northeastern region of the United States (Cape Cod, Martha's Vineyard, Nantucket, Block Island and Long Island). According to geologist George Frederick Wright some of the most prominent examples of terminal moraines on Long Island are "the most remarkable in the world".

Goose Pond is located at the north edge of the Harbor Hill Moraine, a terminal moraine across Long Island that was formed during the Wisconsin glaciation. The pond contains a bird sanctuary, "the smallest island in the smallest natural body of water" within New York City. In the early 20th century it was a popular ice-skating area during the winters. A natural spring under the pond was discovered to still be flowing in 1980, but during a renovation in the 1990s, Goose Pond was turned into an aerated lagoon with seven artificial jets.

Moraine is served by a council–manager form of government, where a seven-member city council appoints a professional city manager, who serves as the administrative head of the city. The city council of Moraine, Ohio, consists of 7 members. A mayor and two council members-at-large are elected by the entire city, while four additional members of council are elected to represent each of four wards. The mayor presides over meetings of the council as chairman, and may vote as a member of council, but has no veto.

Moraine Valley offers its students many opportunities to get involved on campus. There are about 40 clubs and organizations in which students can participate. The focus of these groups include, but are not limited to, special academic interests, religion, diversity and awareness, service and student government. Additionally, Moraine Valley provides various facilities for its students to spend their free time, such as the library, Fine and Performing Arts Center, Student Union, the Health, Fitness & Recreation Center, a 1.45-mile jogging path, and the Jack G. Bradley observation deck.

EETA 79001, also known as Elephant Moraine 79001, is a Martian meteorite. It was found in Elephant Moraine, in the Antarctic during the 1979–1980 collecting season. EETA79001 NASA photo # S80-37633 An image showing EETA79001 as found in Antarctica, NASA photo # S80-28838 rarefraction wave pushes back towards the crater in response, and material is ejected from the crater. If any of this material is moving at a rate faster than the escape velocity (5.0 km/s) of Mars, it may leave the influence of Martian gravity.

Mount Fulcher is an unincorporated community in Logan County, Illinois, United States. Mount Fulcher is located along Interstate 55 and former U.S. Route 66, northeast of Williamsville. "Mount" Fulcher is an end, or terminal moraine, a deposit of rocks and soil left by glaciers at the end of the last ice age. This large natural moraine was greatly reduced by the cutting of the railroad right-of-way between 1853 and 1945, and later by the cutting of right-of-way for the successive highways Illinois Route 4, U.S. Route 66, then U.S. Interstate 55.

Valley of the Ten Peaks () is a valley in Banff National Park in Alberta, Canada, which is crowned by ten notable peaks and also includes Moraine Lake. The valley can be reached by following the Moraine Lake road near Lake Louise. The ten peaks were originally named by Samuel Allen, an early explorer of the region, who simply referred to them by using the numerals from one to ten in the Stoney First Nations Language. He may have learned the terms from his Native American guides, who helped him with the horses.

The meltwater eventually created a network of subglacial channels; many subglacial cavities also formed throughout the ice in the region. The sediment-laden meltwater travelled along these channels, increasingly depositing material in the cavities, and in the channels as the flow waned. The channel fills along the core of the Oak Ridges Moraine are primarily coarse to fine, though the channel bases exhibit a thick sequence of coarse sediments. Moreover, analysis of eskers within the deep valleys to the north of the moraine show that they tend to broaden to form gravel sheets.

Marshfield is located at 44.6649, -90.1760, sitting on a low ridge called the Marshfield moraine by geologists. According to the United States Census Bureau, the city has a total area of , of which is land and is water.

McCann Butte in the Bearpaws, view to the west across glacial moraine. 1920 USGS photograph. Locals refer to the range as the Bearpaws.Montana Place Names Companion Website Aarstad, Rich, Ellie Arguimbau, Ellen Baumler, Charlene Porsild, and Brian Shovers.

Moraine Valley Community College is a public community college in Palos Hills, Illinois. Founded in 1967, it is surrounded by the Cook County Forest Preserves. The college also operates satellite centers in Blue Island and Tinley Park, Illinois.

Führerbuch, p. 34. Parker later commented that they also climbed Mount Temple from Moraine Lake, where "Hans Kaufmann most kindly and ably assisted me in my scientific observations for the determination of altitude."Kaufmann, Hans. Führerbuch, p. 35.

Laurel Lake is located in Grand Teton National Park, in the U. S. state of Wyoming. Laurel Lake is WNW of Jenny Lake and is impounded by a terminal moraine but also lies directly along the Teton Fault.

The islet on which Dragsholm Castle was built is surrounded by lakes and meadows just south of the border moraine deposit, which ends at Vejrhøj (123 m) to the north. Consequently, Dragsholm means the islet by the ”drag”.

The Fox River flows through the area, providing ample opportunity for summer and winter water sports. Four state parks and six county conservation areas are nearby, including Moraine Hills State Park and the Volo Bog State Natural Area.

The ice sheet halted as it covered the eastern half of the Netherlands. After the ice age ended, the moraine remained in the form a long hill-line. The cities of Arnhem and Nijmegen are built upon these hills.

The Kettle Moraine School District serves most of Delafield. Cushing Elementary provides education for children in grades K-5. St. John's Northwestern Military Academy, a private Episcopal military school for 7th through 12th grade, is also located in Delafield.

One of these moraines abuts Cerro Chao, indicating that the dome must be older than the moraine and thus older than the last glaciation 11,000 years ago. An active magmatic body may still exist under Cerro Chao and Paniri.

This rare crescentic terminal moraine is a relic of the southern edge of the ice sheet of the last glaciation, and can be seen from the upper parts of the village as a distinctive elevation of the valley floor.

"Bernard L. Whelan, 1890-1983." Early Aviators, 13 July 2011. Retrieved: 29 August 2011. Whelan and Howard Rinehart (another company test pilot) set up the Rinehart-Whelan Company at Moraine City, Ohio, and acquired the Aerial Coupe in 1923.

The glacier ranges in elevation from at the foot of the steep cliff to at the moraine. One arm of the glacier extends south down to . Between 1904 and 2006, Crescent Glacier lost 6 percent of its surface area.

Muslingodden is a headland at the western side of Nordfjorden in Oscar II Land, Spitsbergen. It has a length of about 1.5 kilometer, formed by the moraine of the glacier Sveabreen. The bay Yoldiabukta is located south of Muslingodden.

The river is fed by rain and meltwater. It is shallow and its bed consists of glacial moraine – gravel and pebbles. It is heavily polluted by the mining industry of Norilsk, namely Nornickel, so fishing is no longer possible.

A community college education is offered at Moraine Valley Community College, in nearby Palos Hills. Sixty percent of Orland Park households have someone with at least a bachelor's degree, with a significant number of residents having completed postgraduate work.

The architect's drawings for the opera house were used by Jones in the package he prepared to justify his successful application for membership in the Royal Architectural Institute of Canada. Moraine Valley Community College operates a satellite facility uptown.

The net effect is that for a glacier which retains its overall shape, glacier mass will be transferred by water flow to accrete new ice, by sediment transport into meters thick layers observed in the accretion zone, and by movement of the total ice mass to restore the ice lost to ablation. The sediment-transport capacity and sediment load in subglacial stream glaciers in which the water is not supercooled and for a glacier far into the supercooling regime vary significantly. When a moraine or moraine shoal (bedrock) has developed, the overdeepening terminates in a growing sediment-floored feature. When there is a significant increase in the elevation on the adverse slope, ice grows from supercooling of streams flowing up the overly steep face of the moraine shoal causes transport capacity to drop below load delivered, producing deposition to fill the adverse face of the overdeepening back towards the supercooling threshold.

East of Landeck, southwest of Delphos, the ridge is indistinct through Venedocia, to the Auglaize River, northeast of Southworth. West, the ridge is distinct Monroeville, Indiana. Through Indiana the ridge is a double crest. North of Glenmore the moraine turns northwest.

According to the United States Census Bureau, the CDP has a total area of , all of it land. Most of Chelsea is hilly, with small glacial lakes. It lies within the Perkinstown terminal moraine, which is described under Taylor County.

The name Valsörarna is of Swedish origin. It is believed that the name was derived from the stone-clad shores and the moraine which resembles a whale. The Finnish name Valassaaret is believed to have been derived from the Swedish word.

Kanter said "Not only should green lands be protected, but they should be linked wherever possible by trail systems, local parks, river valleys and other green corridors." The report placed special emphasis on the protection of the Oak Ridges Moraine.

Around 1960, the division’s name was changed to United Delco. With the Delco name becoming more well-known with consumers, the “Delco” name was incorporated into all of the division's branches (Delco Remy, Delco Harrison, Delco Packard (Packard Electric), Delco Moraine).

After retiring from football, he worked as a foreman at the Frigidaire plant in Moraine, Ohio. He lived in Dayton, Ohio, for approximately the last 40 years of his life. He died in an automobile accident in 1955 at age 51.

"Driver dies while towing historic trolley". Dayton Daily News, p. 3-A. The center also displays the final SUV made at the former General Motors Moraine Assembly, next to the first windshield made by Fuyao Glass America, which redeveloped the factory.

Glacial action forming a cirque which may host a tarn A tarn (or corrie loch) is a proglacial mountain lake, pond or pool, formed in a cirque excavated by a glacier. A moraine may form a natural dam below a tarn.

Israel Russell and exploring party on Malaspina Glacier Moraine, approach route to Mount St Elias, Alaska, 1890 Israel Cook Russell, LL.D. (December 10, 1852 – May 1, 1906) was an American geologist and geographer who explored Alaska in the late 19th century.

It is located in the eastern Prignitz region on the Dosse River near the confluence with its Glinze tributary, about east of Pritzwalk and northwest of Berlin. Wittstock is situated in a terminal moraine landscape south of the Mecklenburg Lake District.

Crown Point lies on the Valparaiso Moraine. According to the 2010 census, Crown Point has a total area of , of which (or 99.92%) is land and (or 0.08%) is water. Crown Point is situated approximately 40 miles southeast of Chicago's Loop.

Moraine Strait () is a strait on the McMurdo Ice Shelf of Antarctica that trends north–south between Brown Peninsula, Mount Discovery, and Minna Bluff on the west, and Black Island on the east. The surface of the strait, especially the northern part between Brown Peninsula and Black Island, is noteworthy for the presence of broad moraine belts that obscure much of the ice and suggest the name. The strait was discovered by the British National Antarctic Expedition, 1901–04, led by Robert Falcon Scott, and was named by the Advisory Committee on Antarctic Names in 1999.

Upon reaching Consolation Lakes hikers may continue along to the upper lake, which is not visible from the end of the lower lake. There is, however, no clearly marked trail, and can often be a scramble over large rocky areas. Canoe docks Near the canoe docks of Moraine Lake LodgeMoraine Lake Lodge there is another trail-head. This trail-head is the start of two trails, one of which branches out into four different trails - so there are in total, five trails starting at that trail-head (Moraine Lake Lake shore Trail, Eiffel Lake, Wenkchemna Pass, Larch Valley, and Sentinel Pass).

According to the United States Census Bureau, the town has a total area of 74.8 square miles (193.8 km2), of which, 30.1 square miles (77.9 km2) of it is land and 44.7 square miles (115.8 km2) of it (59.78%) is water. Westerly sits atop a glacial moraine, a series of small hills of debris left behind by receding glaciers in the last Ice Age. A pristine sample of the moraine encompasses a preserve owned in perpetuity by the Westerly Land Trust. Within the trust land are the rare "kettle" formations that extend out under the sea to Block Island.

Campbell was the head professional at several golf clubs, including The Country Club (Brookline, Massachusetts, 1896–1916), Baltimore Country Club (Baltimore, Maryland), Northmoor Golf Club (Celina, Ohio), Losantiville Country Club (Cincinnati, Ohio), Miami Valley Golf Club and Moraine Country Club (Dayton, Ohio). He was also a golf course architect, designing the Moraine Country Club. In 1913, at The Country Club, he played a friendly match against Wilfrid Reid upon the Englishman's arrival in Boston to play in the 1913 U.S. Open. During his 20-year career at The Country Club, he was involved in the development of caddy Francis Ouimet as a player.

In the Morris Basin was Lake Wauponsee, which reached east up the Kankakee Valley into Indiana. It flowed south via the Iroquois River into Lake Watseka over the Chatsworth ridge of the Marseilles morainic system to the Vermillion River Valley, past Pontiac, Illinois. The volume of water was blocked at the gap in the Farm Ridge moraine, a unit of the Bloomington morainic system near LaSalle, Illinois. This blockage created Lake Ottawa between Farm Ridge and the Marseilles moraine in the Illinois Valley, and Lake Pontiac between the Cropsey (unit of the Bloomington morainic system), and Marseilles moraines in the Vermilion Valley.

At its longest, Lake Hitchcock stretched from the moraine dam at present-day Rocky Hill, Connecticut, to St. Johnsbury, Vermont (about ). Although the rift valley through which the river flows above Rocky Hill actually continues south to New Haven, on Long Island Sound, the obstructing moraine at Rocky Hill diverted the river southeast to its present mouth at Old Saybrook. Lake Hitchcock is an important part of the geology of Connecticut. It experienced annual layering of sediments, or varves: silt and sand in the summertime (due to glacial meltwater) and clay in the wintertime (as the lake froze).

Mueller, Hooker and Tasman Glaciers in the Southern Alps, showing major retreat in the ~10 years circa 1990 to 2000. Notice the larger terminal lakes, the retreat of the white ice (ice free of moraine cover, high up on the glaciers), and (more subtly) the increase in height of the moraine walls due to ice thinning. The glacier remained at a constant in length for all of its recorded history in the 20th century before starting its current period of rapid melting in the 1990s. Between 2000 and 2008 alone, the glacier terminus receded 3.7 km.

The proglacial Tasman Lake is a popular destination for boat tours among the icebergs often floating in the lake. Boats are not allowed closer than to the tall terminal face of Tasman Glacier for safety reasons. The Ball Shelter Track, part of the Ball Hut Route, leads along the western side of the glacier, separated from Tasman Lake by a tall moraine wall until about 6 kilometres in, where it climbs high enough for the view to open up. At that point, the rock-covered lower Tasman Glacier in the valley between the moraine walls is wide.

The lake sits precariously; moraines on the volcano are steep, unstable, and populated with boulders. Before September of 1960, there was a partial breach of this moraine-dammed lake that covered an area of near the moraine's base. Since 1960, there have been at least three incidents in which moraine-dammed lakes on the volcano have caused floods down the slopes, including a significant flood and debris flow in 2012. Local soil is thin, and it has been buried by a layer of weathered Holocene tephra from Three Fingered Jack, which has a maximum thickness of .

Niagara Falls is also a product of the glaciation, as is the course of the Ohio River, which largely supplanted the prior Teays River. With the assistance of several very broad glacial lakes, it released floods through the gorge of the Upper Mississippi River, which in turn was formed during an earlier glacial period. In its retreat, the Wisconsin Episode glaciation left terminal moraines that form Long Island, Block Island, Cape Cod, Nomans Land, Martha's Vineyard, Nantucket, Sable Island, and the Oak Ridges Moraine in south central Ontario, Canada. In Wisconsin itself, it left the Kettle Moraine.

Tully is geologically noted for the terminal moraine deposited there by the glacier, filling the deep Tully Valley, which might have been another Finger Lake had the moraine been left closer to Syracuse, impounding water. Tully is at the divide between two major watersheds, one flowing northward to the Atlantic Ocean by way of the St. Lawrence River and the other southward to the ocean via the Susquehanna River. Oneida Lake, the Finger Lakes, and smaller bodies of water provide recreation. The Appalachian hills have several ski areas, waterfalls and historic villages as well as large parks and forest preserves.

Glacial activity can also form natural dams, such as the damming of the Clark Fork in Montana by the Cordilleran Ice Sheet, which formed the Glacial Lake Missoula near the end of the last Ice Age. Moraine deposits left behind by glaciers can also dam rivers to form lakes, such as at Flathead Lake, also in Montana (see Moraine-dammed lake). Natural disasters such as earthquakes and landslides frequently create landslide dams in mountainous regions with unstable local geology. Historical examples include the Usoi Dam in Tajikistan, which blocks the Murghab River to create Sarez Lake.

The terminal moraine stretching across the former river gorge in Devil's Lake State Park View of the Northern shore of Devil's Lake Devil's Lake was originally a gorge of the Wisconsin River prior to the last ice age. At what is now the southern end of the lake, the river turned from a southerly direction to an easterly direction. During the ice age, a lobe of the glacier passed to the east of the Baraboo Hills and came up the river valley. It deposited materials and then melted, leaving a terminal moraine blocking the river, forming an earthen dam.

As a member of the NJCAA, the Moraine Valley Cyclones participate in 12 intercollegiate sports, including men's baseball, cross-country, basketball, golf and soccer, and women's basketball, cross-country, golf, soccer, softball and volleyball. Moraine Valley is a member of the Illinois Skyway Collegiate Conference, which consists of seven other junior colleges in the surrounding area. The athletics program is housed in the Health, Fitness & Recreation Center (Building H) on campus and is quite successful with many teams advancing to national competitions. In 1998, the mascot for the college was changed from the Marauders to the Cyclones.

Beneath the drift deposits of the Vale of York lie Triassic sandstone and mudstone, and lower Jurassic mudstone but these are completely masked by the surface deposits. These deposits include glacial till, sand and gravel and both terminal and recessional moraines left by receding ice sheets at the end of the last ice age. The Escrick moraine extends across the vale from west to east and the York moraine, 8 miles further north, forms a similar curving ridge from York eastwards to Sand Hutton. To the north of these ridges are deposits of clay, sand and gravel left by a glacial lake.

The Southern Unit of the Kettle Moraine State Forest includes more than 22,000 acres of land throughout southern Wisconsin and spans several state parks and natural areas. The area also features varied environments from restored prairie, forests, and lakes, along with providing a multitude of recreational opportunities such as hiking, birdwatching, fishing, camping, and hunting. The Kettle Moraine Scenic Drive also extends within this region as well as through a larger portion of the state. This section of the state forest has campgrounds at some of the larger nature reserves like Whitewater Lake, Ottawa Lake, and Pinewoods.

Holmes is the son of two Doctors of Divinity who run a Chicago-area church. In high school, Holmes grew from a 6'2" guard into a 6'9" forward, but did not receive any Division I college basketball scholarship offers until he had already committed to playing for Moraine Valley Community College. In his only season at Moraine Valley, Holmes averaged 19.3 points, 9.3 rebounds and 5.2 blocks per game. After earning junior college All-American honors, Holmes transferred to Bowling Green. In his sophomore season at Bowling Green, Holmes averaged 6.5 points, 5.0 rebounds and 2.3 blocks per game.

During the provincial election of 2003, the Liberal Party of Ontario promised to terminate development on the moraine as part of its election campaign. Once elected, the party failed to deliver on that promise, as a development in the northern part of Richmond Hill consisting of over 6600 housing units continued. The government, in its attempt to halt other nearby developments, proposed the North Pickering Land Exchange. Discussed as early as November 2001, it involved exchanging government-owned public lands in North Pickering for privately owned lands on the Oak Ridges Moraine in Richmond Hill and Uxbridge.

The basin of the "Rivière des chutes" began to be colonized in the late eighteenth century. The pioneers were heading north, crossing the moraine of Saint- Narcisse, to settle on new plots of land because there was little available lots remaining in the valley of the Saint Lawrence River (in Champlain and Sainte-Geneviève-de-Batiscan) at the foot of the moraine of Saint-Narcisse. The sawmill Albert Cossette, powered by water flow, was erected in the North of the Falls River Falls. The dammed water was repressed by the mill up to the "Grande ligne" (Great Line).

In this area, human activity includes fruit and dairy agriculture, major urban areas, and some forestry and tourism attractions. The most prominent wildlife observed are white tailed deer, moose, and the grey squirrel, and vegetation includes a wide range of trees such as oak, hickory, maple, beech, and some pine and basswood species. The second sub-ecoregion is the Central USA Plains, an area of , that has a landform of smooth plains. The majority of this region’s surface material is moraine with some lacustrine, and the soil consists of calcium enriched prairie soils and forest soils on moraine.

Trollgarden is a glacial moraine in the municipality of Hjelmeland in Rogaland county, Norway. The moraine is a tall ridge of stones, rocks, and boulders that runs for about from the east side of the lake Kvivatnet across the moorland to the northern side of the mountain Brendeknuten in the Hjelmelandsheiane mountains. The name "Trollgarden" is translated to English as The Troll's stone fence since it looks like a rock wall that a troll may have built around its farm. The ridge sits about southeast of the village of Jøsenfjorden and about northeast of the village of Hjelmelandsvågen.

The North Mowich River's headwater tributaries drain North Mowich Glacier near an area of Mount Rainier called Division Rook. Shortly below the toe of the glacier, the river drops over a large wall, forming Moraine Falls, the first of two waterfalls on the river, both of which are very difficult to access and would take several days to reach on foot. Giant Falls, just as difficult to reach, is located a ways downstream of Moraine Falls. Ptarmigan Ridge separates the North Mowich River's headwaters from Spray Park, much of which is drained by other tributaries of the North Mowich River.

Chippewa Moraine Lakes is a Wisconsin Department of Natural Resources- designated State Natural Area that comprises nine separate sites, spread out over roughly 30 square miles (78 km2). Each site features a primarily undisturbed lake located within the rough terminal moraine topography of northern Chippewa County. Each lake has its own unique species assemblage due to physical and chemical characteristics of the lake. The nine lakes are: Camp Lake, a 6-acre (2.4 ha) lake ringed by a floating sphagnum bog mat containing such plant species as white beak rush, narrow-leaved sundew, small cranberry, and grass pink orchid.

Maligne Lake in Jasper National Park Spirit Island on Maligne Lake Maligne Lake is the largest lake in Jasper National Park. The valley in which the lake lies was carved and excavated by valley glaciers, and the lake has been dammed at its northern end by an end moraine deposited by the last glacier, which flowed down the valley towards the Athabasca River. The glacial deposits and landforms forming the end moraine are excellent examples of glacial deposition.www.ags.gov.ab.ca The highest peak in the area is Mount Brazeau (), which stands southeast of Maligne Lake at the head of the Brazeau Icefield.

Recent work suggests that the area outside the South Ireland End Moraine was inundated by Irish Ice during and after the LGM. At the same time parts of the area outside the South Wales End Moraine must also have been inundated by ice. Another puzzle is the extent to which the long profile of the Irish Sea Glacier, at the time of its maximum extent, approximated to the classic equilibrium profile. Work in analogous situations in Marie Byrd Land, Antarctica, suggests that the ice surface altitude over the mountains might have been around 800m lower than predicted.

The study on late-glacial climate change in White Mountains (New Hampshire, USA) refined the deglaciation history of White Mountain Moraine System (WMMS) by mapping moraine belts and related lake sequences. The result suggests that the Littleton-Bethlehem (L-B) readvance of ice sheet occurred between 14,000 and 13,800 years BP. The L-B readvance coincided with the Older Dryas events and provides the first well-documented and dated evidence of Older Dryas. Another Glacial chronology and palaeoclimate study on moraine suggests a cold oscillation in the second late- glacial (LG2) following the first late-glacial readvance (LG1) at around 14,000±700 to 13,700±1200 years BP. The LG2 cold oscillation around 14,000 years BP can correspond to the cooling of Greenland Interstadial 1 (GI-1d-Older Dryas) that happened around the same time period, which is the first chronological evidence that supports the presence of Older Dryas in the Tatra Mountains.

Camping opportunities near the Glacial Drumlin State Trail are available throughout the year at campgrounds in the Southern Unit of the Kettle Moraine State Forest, Lake Kegonsa State Park, the Capital Springs State Recreation Area, and at the Sandhill Station State Campground.

The hooded warbler is a threatened species in Canada. Happy Valley Forests is one of the few remaining Canadian habitats for this species. The Oak Ridges Moraine lies in Southern Ontario, Canada. It contains the headwaters of sixty- five rivers and streams.

According to the available information, Caribou Island consists of a mixture of glacial sediments and Precambrian sandstone. Caribou Island is part of a large glacial moraine that accumulated south of Michipicoten Island.Dell, C.I., 1976. Sediment distribution and bottom topography of southeastern Lake Superior.

Minong is a name derived from the Ojibwe language, referring to the high hill or moraine that was geologically formed just south of town. A post office called Minong has been in operation since 1887. The village was laid out in 1888.

Multiple erratics on the terminal moraine of the Okanogan Lobe. Cascade mountains in the background. End moraines, or terminal moraines, are ridges of unconsolidated debris deposited at the snout or end of the glacier. They usually reflect the shape of the glacier's terminus.

Between Pine Creek and the mouth, the elevation decreases by per mile. The headwaters of Huntington Creek are on North Mountain. The watershed is also crossed by a terminal moraine. The channel of Huntington Creek flows through rock formations of shale and sandstone.

There are several large lakes in the municipality including Nilsebuvatnet, Øvre Tysdalsvatnet, and Tysdalsvatnet. The large lake Blåsjø partially lies in the municipality. The Trollgarden glacial moraine lies atop a mountain in Hjelmeland. The Ritland crater is also located in the municipality.

Sediments are dominated by coarser (coarse sand/gravel) fragments, and the accumulation rate can be immense: up to 1 metre per year near the shores of larger lakes. Upon melting of the glacier, deposits may be preserved as superglacial till (alias supraglacial moraine).

The Mittelradde, one of the rivers in the Hümmling The Hümmling (Homelinghen, from hömil = small stone) is a ground moraine landscape, up to , in the Emsland region on the North German Plain in the western part of the German state of Lower Saxony.

The parish was named after the old Ås (Norse Áss) farm, since the first church was built there. The name is identical with the word áss meaning "hill", "ridge" or "esker" (height in moraine landscape). Prior to 1921, the name was spelled Aas.

Beverly Hill is a name seldom used. It refers to the steep rise on U.S. 6, east of Indiana 49. The highway pass’ through the upper reaches of the Coffee Creek valley and then climbs to the top of the Valparaiso Moraine.

The Dahio Trotwood Airport, also known as Dayton-New Lebanon Airport, is a privately owned, public-use airport west of the central business district of Dayton. The Moraine Airpark is a privately owned, public-use airport southwest of the city of Dayton.

Farewell Creek is a watercourse in Durham County, that empties into Lake Ontario, at Oshawa, Ontario. It drains a watershed of . To the west and east it borders Oshawa Creek, and Bowmanville Creek, which have their headwaters in the Oak Ridges Moraine.

The Plan builds on existing initiatives for the wise use and management of all resources, natural heritage, agriculture and mineral aggregates in the Ontario Heritage Act, 1990 the PPS, the Greenbelt Plan, the Oak Ridges Moraine Conservation Plan, and the Niagara Escarpment Plan.

Meremäe Hill () is a hillock in southeastern Estonia. Located on Vaaksaare upland, that belongs to the eastern part of Haanja Upland. Height from sea- level is 204 m. Vaaksaare uplands is a moraine hillock, where agricultural patches alternate with forests and meadows.

The St. Croix Moraine runs through the park. This rolling and uneven landform is a result of the Wisconsin glaciation and two previous glaciations. Irregular hills and ridges (kames) surround kettles, depressions left by melting blocks of ice during the glaciers' retreat.

2008 in the Khibiny Mountains, Kola Peninsula could be described as discrete debris accumulations, although their origin is postulated by these authors as being moraine remnants of an ice sheet pushing into these cirques rather than as rock glaciers formed within the cirques.

Their coastlines are smoother. These areas were carved more by water erosion. The formation and characteristics of glacial lakes vary between location and can be classified into glacial erosion lake, ice-blocked lake, moraine-dammed lake, other glacial lake, supraglacial lake, and subglacial lake.

Water from the melting glaciers carved channels into the moraine. Where one channel—now occupied by Beaver Creek—intersected the channel now occupied by the Des Moines River, a buildup of sediment and slumping banks partially dammed the outflow, creating a large, shallow lake.

Roosevelt Glacier is located on the north slopes of Mount Baker in the North Cascades of the U.S. state of Washington. Roosevelt Glacier descends to nearly at Chromatic Moraine. In the middle of its course, Roosevelt Glacier is connected to Coleman Glacier to its south.

The moraine runs between and above sea level, or to above the surface of Lake Michigan. From the inner border there is usually a rise of or more. In some places of or more. The crest in Illinois ranges from about to above sea level.

Located east of the Kettle Moraine State Forest, Plymouth is a recreational destination. The city has 17 parks that offer recreational opportunities that include baseball (Plymouth Youth Athletic Association]), soccer (Plymouth Soccer Club) frisbee-golf, biking, swimming (Plymouth Aquatic Center), tennis, nature walks and more.

Kettering was born July 15, 1907 in Bellevue, Kentucky to architect and marble importer Norman and Clara Weiffenbach. She was their only child. She attended Moraine Park School, where she met husband-to-be Eugene Kettering, Margaret Morrison Carnegie College, Carnegie Tech, and Lutherville Seminary.

Dorothy Lake State Natural Area is a Wisconsin Department of Natural Resources-designated State Natural Area featuring forested end moraine topography, with many steep-sided ridges and depressions. This results in a diverse mosaic of natural communities, including forests, swamps, fens, lakes, and streams.

It was formed as a frontal moraine of Huntress Glacier between the 13th and 17th centuries. The feature is named after Victor Quiroga Martínez, captain of the Spanish ocean exploration ship BIO Hespérides that rendered logistic support to the Bulgarian Antarctic campaigns in the 1990s.

Boardwalk at the Spruce Lake Bog Spruce Lake Bog is a bog in Fond du Lac County, Wisconsin. It is located within Kettle Moraine State Forest. The bog was designated a Wisconsin State Natural Area in 1968 and a National Natural Landmark in 1973.

The ORMLT is a non-profit organization that raises funds to protect areas on the moraine through conservation easements and outright purchases. They have protected . The Nature Conservancy of Canada is also active and are raising funds to protect a property called Happy Valley Forest.

Horsens lies at the end of Horsens Fjord in eastern Jutland. The city is surrounded by typical moraine landscape with low hills and valleys created by glaciers during the last ice ages. Horsens is south of Aarhus and north of Vejle, and approximately from Copenhagen.

The lake lies in a glacial valley which follows the Bala to Tal-y-Llyn fault line. The valley was blocked by a terminal moraine in the area of the village of Bala, thus forming the lake, which has fairly straight and parallel sides.

Defiance is located at (41.281891, -84.362856). According to the United States Census Bureau, the city has a total area of , of which, is land and is water. Defiance lends its name to a distinct end moraine from the Wisconsian glaciation. As Cushing et al.

Luna Lake is located in North Cascades National Park, in the U. S. state of Washington. Situated southwest of Luna Peak which is the tallest mountain in the rugged Picket Range, Luna Lake is a proglacial lake impounded by the moraine of a retreated glacier.

Amphitheatre Glacier () is a moraine-covered glacier that flows north from The Amphitheatre into Roaring Valley, in the Royal Society Range of Antarctica. It was named by a New Zealand Geographical Society field party in the area, 1977-78, in association with The Amphitheatre.

Connections with the Bradford Bypass freeway, as well as Highway 400 and Highway 11 north of Barrie were considered. In the past decade, there has been little discussion of this highway extension due to concerns with traversing the Oak Ridges Moraine and Minesing Swamp.

Being a remnant of glacial moraine, the North Shore is somewhat hilly, and its beaches are more rocky than those on the flat, sandy outwash plain of the South Shore along the Atlantic Ocean. Large boulders known as glacial erratics are scattered across the area.

Faizievite is a single-locality mineral, coming from the moraine of the Darai-Pioz glacier, Tien Shan Mountains, Tajikistan. Alkaline rocks of this site are famous for containing numerous rare minerals, often enriched in boron, caesium, lithium, titanium, rare earth elements, barium, and others.

The glacier finishes at its merger with another glacier, the Kronebreen, another surge glacier moving at around 750 metres per year, along a ice front with dirty 5- to 20-metre-high ice cliffs, as the Kongsbreen picks up medial moraine and englacial debris.

Sauk Village is located at (41.488535, -87.565658). According to the 2010 census, Sauk Village has a total area of , of which (or 99.02%) is land and (or 0.98%) is water. The village stands on the Tinley Moraine. The Glenwood Shoreline cuts through the village.

University Park is located at (41.439460, -87.697299). According to the 2010 census, University Park has a total area of , of which (or 99.98%) is land and (or 0.02%) is water. The village lies on the Valparaiso Moraine, which is also the Eastern Continental Divide.

Near the end of the last ice age about 18,000 years ago it extended to the present-day coastline or even beyond. As it retreated the glacier left behind moraines of accumulated rock and chunks of ice which created coastal hills and lakes. Lake Wombat is a kettle lake created by ice left in a moraine 9000 years ago, while Peters Pool close to the glacier's face arose in the same fashion just 210 years ago. The Waiho Loop 4 km north of the settlement of Franz Josef is the terminal moraine of Franz Josef Glacier, deposited by the retreating glacier about 12,000–3,000 years ago.

Two small icebergs at right clearly retain fragments of the moraine (rock debris) that forms a dark line along the upper surface of the glacier. The inclusion of the moraine illustrates how land-based rocks and sediment are carried by ice. Erratics provide an important tool in characterizing the directions of glacier flows, which are routinely reconstructed used on a combination of moraines, eskers, drumlins, meltwater channels, and similar data. Erratic distributions and glacial till properties allow for identification of the source rock from which they derive, which confirms the flow direction, particularly when the erratic source outcrop is unique to a limited locality.

The Interstate 75 interchange allows motorists to more easily enter I-75 North from Moraine and also allows Moraine's neighbor city, West Carrollton, to enter I-75 South without having to first enter the Moraine and then execute a U-turn. The entrances include: southbound Dixie Drive access to I-75N, northbound Central Avenue access to I-75S, I-75N access to southbound Dixie Drive and I-75S to access South Dixie Drive. The project also makes it possible to execute a left turn at Dryden Road onto Dixie Drive. The exit was originally built in the early 1960s and never completed into a traditional highway exit until 2012.

Geologically, Appalachian Ohio corresponds closely to the terminal moraine of an ancient glacier that runs southwest to northeast through the state. Areas south and east of the moraine are characterized by rough, irregular hills and hollows, characteristic of the Allegheny Plateau and Cumberland Plateaus of the western Appalachian Plateau System. Unlike eastern Appalachia, this region does not have long fin-like ridges like those of the Ridge-and-Valley Appalachians subranges, but a network of rocky hollows and hills going in all directions. The region is considered part of "central Appalachia", a political, cultural, and bioregional classification that includes southeastern Ohio, Eastern Kentucky, most of West Virginia and Southwestern Virginia.

Until the 1990s, farmlands used to dominate the northern part of Oak Ridges, except in the east. The western edge of Oak Ridges is now entirely residential or commercial; the McLeod's Landing development in the southwest consumed the last undeveloped land in the western part of Oak Ridges. This development was part of a contentious political battle that ultimately became an issue in the 2003 Ontario provincial election. In their campaign, the Liberal party promised to halt development on the Oak Ridges Moraine, specifically in Richmond Hill (see; Politics of the Oak Ridges Moraine for a more extensive discussion and; Development in Oak Ridges for ongoing development in Oak Ridges).

Argentinian proglacial lakes: Lago Viedma (middle), Lago Argentino (left) and Lago San Martin (right). Retreating glaciers are visible at the top. Tarn—a proglacial lake impounded by the terminal moraine of the retreating Schoolroom Glacier in Grand Teton National Park, Wyoming In geology, a proglacial lake is a lake formed either by the damming action of a moraine during the retreat of a melting glacier, a glacial ice dam, or by meltwater trapped against an ice sheet due to isostatic depression of the crust around the ice. At the end of the last ice age about 10,000 years ago, large proglacial lakes were a widespread feature in the northern hemisphere.

There is a strait to the southwest, separating Hove from the islands of Merdø and Gjessøya, and northeast of Hove is Spornes, with a beach that alternates between a sandy beach and a pebble beach depending on the wind and weather. Tromøy Church and the Brekka farm stand further to the northeast. The entire area is characterized by a large moraine, which creates the natural basis for pebble beaches, sandy beaches, and large areas of Aust-Agder's best arable land. The outer part of the Hove area is part of a moraine landscape area with the protected Hove Woods (Hoveskogen), containing windswept Scots pine.

The temporary dam, in conjunction with one of the Lake Missoula floods, caused the water to flow back up the Wenatchee Valley, where it was stopped by the glacier at Leavenworth. As the leading edge of the glacier interacted with the flood, ice rafts formed carrying granite erratics from the Stuart batholith, which ended up in the town of Dryden about 15 miles down the valley from Leavenworth. As the glacier retreated, the south side of Leavenworth was a lake dammed up by the moraine. The bridge on the east side of town is a good vantage point to see where the Wenatchee River cuts through the moraine today.

The Waterloo Moraine was formed as the three ice lobes of the Laurentide Ice Sheet retreated across what is now Waterloo Region from Lake Huron in the west, Georgian Bay in the northeast, Lake Ontario in the east and Lake Erie in the southeast. As the glacier moved, it carried with it huge boulders, sand, gravel and debris. As the ice disappeared, the Waterloo Moraine remained, a huge complex of glacial sediments that is between 30 metres and more than 100 metres thick. Meltwater streams cascading from the surface of the ice lobes carried enormous deposits of sand and gravel and blocks of bedrock.

Sylling is located on Holsfjorden, the southeastern arm of Tyrifjorden. Sylling is known for agriculture, particularly the cultivation of fruit. Local farms have a long history of cultivation of strawberries and vegetables. The good soil is due to gravel after the Last glacial period including Sylling-moraine.

The Gruvleflesa Knolls () are two low rock knolls rising above the Antarctic glacial moraine west of the Gruvletindane Crags, in the Kurze Mountains of Queen Maud Land. They were mapped from surveys and air photos by the Sixth Norwegian Antarctic Expedition (1956–60) and named Gruvleflesa.

The South Branch Kishwaukee River, a major tributary of the Kishwaukee River,James, L. Allan. Management and Restoration of Fluvial Systems with Broad Historical Changes and Human Impacts, (Google Books link), Geological Society of America, 2009, pp. 110-111, (), (). originates on the Cropsey Moraine, near Shabbona, Illinois.

According to the United States Census Bureau, the city has a total area of , of which, is land and is water. West Bend is in the Kettle Moraine region, and its topography is varied. The glacial activity has formed many kettles and hills throughout the region.

Lateral moraines are formed at the side of the ice flow and terminal moraines at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines (till-covered areas with irregular topography) and medial moraines (moraines formed where two glaciers meet).

Salem Bear Creek Church, Salem Evangelical Lutheran Church (Ellerton Lutheran and German Reformed Church District) is a historic district roughly bounded by Union Road, Dayton Germantown Pike, and Bear Creek in Moraine, Ohio. The area was added to the National Register of Historic Places in 1990.

Sakai, Akiko, et al. "Role of supraglacial ponds in the ablation process of a debris-covered glacier in the Nepal Himalayas." IAHS PUBLICATION (2000): 119-132. Moraine (glacial debris) is moved by natural processes that allow for down-slope movement of materials on the glacier body.

Muddy Creek is a tributary of Slippery Rock Creek in Butler and Lawrence Counties in Pennsylvania in the United States. The run is long, flows generally west, and its watershed is in area. Muddy Creek is the main water source for Lake Arthur in Moraine State Park.

Location of the Osterholz Geest Relief map of the Osterholz Geest Wallhöfen High bank of the River Lesum The Osterholz Geest (Northern Low Saxon: Oosterholter Geest) is an undulating, sandy area of ground moraine between the city of Bremen and the towns of Bremerhaven and Bremervörde.

Rifflsee is a lake of Tyrol, Austria. It is the largest lake in the Ötztal Alps. The mountain lake is located in the Kaunergrat west of the Pitztal and is a typical moraine reservoir. The lake fills an extensive valley, the glacier-turbid water looks greenish.

Nieden, one of the smallest towns in the surrounding district, lies on a relatively flat glacial moraine on the east bank of the Uecker river. The town is on the state line of Brandenburg and is about half way between the cities of Pasewalk und Prenzlau.

Zemu Glacier has seen significant retreat in recent years. The lateral moraine ridges on either side of the glacier are on average 150 feet high. These ridges were created during the Little Ice Age advance. Lateral moraines never get higher than glacier surfaces that create them.

The Defiance Moraine trends across the entire state of Ohio Defiance is a city in and the county seat of Defiance County, Ohio, United States, about southwest of Toledo and northeast of Fort Wayne, Indiana, in Ohio's northwestern corner. The population was 16,494 at the 2010 census.

There are still tarns in some of these old cirques, partly a result of the anthropogenic elevation of the low- side lip of the cirque, such as the Mummelsee, Wildsee, Schurmsee, Glaswaldsee, Buhlbachsee, Nonnenmattweiher, and Feldsee. The Titisee formed as glacial lake behind a glacial moraine.

McLaughlin Creek flows west from the swamp underneath PA 89 and then southwest around Fink and Gilson Ridges. Once around the ridges, it turns south and rapidly falls through Bog Hollow to meet Thompson Creek at the bottom. Bog Hollow marks the terminal moraine for glaciation.

The moraine is also host to a staggering amount of biodiversity and in recent years there has been a considerable amount of pressure applied to government to shield the area from development. Consequently, a considerable portion of Richmond Hill is subject to the Ontario Government's Greenbelt legislation.

Geographical features around Lake Annecy. Beach of Albigny. The commune is 50% urbanised with 33 hectares of public forest, and 50% agricultural and forests. The commune is located on the foothills of Mount Veyrier (1,291 m), on a moraine at the junction of two old large glaciers.

The scenic Hollowell Park trail leads to the Bierstadt Lake area through dense sagebrush and meadows on the north side of Bierstadt Moraine and to the Mill Creek Basin. Fern Lake and Cub Lake trails are also in the vicinity. No picnicking or fishing is allowed.

The lake sits atop a lateral moraine on the side and end of Bartholf Glacier and drains into Mill Creek. It is named for Albert Bierstadt, a noted landscape artist, whose 1870s paintings of Longs Peak and Bierstadt Lake are among the Denver Art Museum's collection.

Superficial deposits refer to geological deposits typically of Quaternary age (less than 2.6 million years old). These geologically recent unconsolidated sediments may include stream channel and floodplain deposits, beach sands, talus gravels and glacial drift and moraine. All pre-Quaternary deposits are referred to as bedrock.

Elveflya (The River Plain) is a coastal plain in Wedel Jarlsberg Land at Spitsbergen, Svalbard. It is located between Nottinghambukta and the front of Torellbreen, west of the mountain Tonefjellet. The plain has a width of about five kilometers, and is characterized by moraine deposits and rivers.

Sylvia Falls is high and wide and cascades across a glacial moraine. The falls is noticeably eroding upstream and changing its appearance faster than other waterfalls in the park, since glacial deposits are fairly soft. Only downstream is Goodwin Falls which is high and wide.Neave, Roland (2015).

There are also natural terraces from moraine deposits. The old farm is located on the sandy beach and the terraces were used for tilled fields and meadows. The Sjønstå farm was given protected status in 2006 by the Norwegian Directorate for Cultural Heritage.Ingvaldsen, Jan-Olav. 2013.

Where ice blocks had been left behind, sand filled the depressions. Runoff from the Valparaiso Moraine built outwash ridges of sand leading into the lake. On the south, the winds built dunes. As the volume of water decreased from the glacier melting northward, the lake slowly drained and filled.

Kristiania: Fabritius. The German use of the word ' for long narrow bays on their Baltic Sea coastline, indicates a common Germanic origin of the word. The landscape consists mainly of moraine heaps. The ' and some "fjords" on the east side of Jutland, Denmark are also of glacial origin.

The river flows over ground formed from Old Red Sandstone rocks laid down during the Devonian period. The valley was inundated by ice during the last glacial period as evidenced by the low mounds of moraine present in the valley and through which the river has since cut.

Slinger is located at (43.328466, -88.283461). According to the United States Census Bureau, the village has a total area of , of which, of it is land and is water. Slinger is known as the "village of seven hills" as it rests in the heart of the Kettle Moraine.

In the last ice age, a glacial tongue descended from the north-eastern slopes into the valley of Gresse-en-Vercors, depositing a glacial moraine which is visible today to the west of the village. However, there is no longer any permanent ice or snow on le Grand Veymont.

The quaternary geology has left the area as a moraine plain consisting of glacial deposits. The bedrock geology is the pembina member of Vermillion River Formation and Riding Mountain Formation. Yorkton is located in the physiographic region of the Quill Lake-Yorkton Plain region of the Saskatchewan Plains Region.

Environmental organizations like the Oak Ridges Moraine Land Trust have organized tree- planting events in Ashburn to help rebuild the habitat of the redside dace. In response to local environmental concerns, some citizens of Ashburn have formed the Ashburn Environmental Coalition.Asburn Environmental Coalition (AEC), accessed March 18, 2012.

Hunting is permitted on of Moraine State Park. Hunters are expected to follow the rules and regulations of the Pennsylvania Game Commission. The common game species are ruffed grouse, waterfowl, squirrels, pheasants, bear, turkey, white-tailed deer, and rabbits. The hunting of groundhogs is not permitted at the park.

The amphitheater is built about one hundred feet from the lodge, with seating interspersed with trees. A projection booth and screen once existed, but were removed. An elaborate arrangement of stone gutters and culverts provides drainage. The Moraine Park Lodge adjoins the William Allen White Cabins historic district.

Lyell Lake () is a lake on the east side of Lyell Glacier, South Georgia. The moraine-dammed lake has a series of terraces above the current shoreline, marking former lake levels. It was named by the UK Antarctic Place-Names Committee in 1991 in association with Lyell Glacier.

From southeast to northwest, Pfannenstiel is part of a chain of peaks respectively mountains: Guldenen (), Wassberg (), Öschbrig (), Adlisberg (), Zürichberg (), Käferberg-Waidberg () and Hönggerberg (). The area alongside Lake Zürich had been formed as the left moraine of the Ice Age glacier, the bed of which is now the Lake Zürich.

Alexandersville, Ohio was a town located in Montgomery County, Ohio, United States just north of West Carrollton and south of Moraine. It was incorporated into West Carrollton in 1943. Alexandersville was platted in 1815. A post office called Alexandersville was established in 1828, and remained in operation until 1907.

Haag was born on August 3, 1992 to Jeff and Chris Haag. He has a brother and sister. Haag attended Amos Alonzo Stagg High School in Palos Hills, Illinois and graduated in 2010. He has also completed a two- year course in business studies at Moraine Valley Community College.

It is a moraine shaped by a glacier that, by moving, broke up from the bedrock of the Canadian Shield, fragments that it disaggregated and rounded by rolling over them, moving them and leaving them in this basin, some thousand years ago, at the end of the Wisconsin glaciation.

Glacial Lake Nantucket Sound was a glacial lake that formed during the late Pleistocene epoch inside modern Nantucket Sound. After the Laurentide Ice Sheet retreated, glacial ice melt washed over the terminal moraine of Cape Cod and the glacial meltwater settled in the modern day sound, creating the lake.

Almost 75% of the province's population lives in the Calgary–Edmonton Corridor. The land grant policy to the railroads served as a means to populate the province in its early years. Moraine Lake at Banff National Park. The Alberta Mountain forests makes up the southwestern boundary of Alberta.

Michael A. Lehman (April 24, 1943 - August 7, 2017) was an American Republican politician from Wisconsin. Born in Rice Lake, Wisconsin, Lehman graduated from Hartford Union High School in Hartford, Wisconsin. He went to Moraine Park Technical College and Milwaukee Area Technical College. Lehman lived in Hartford, Wisconsin.

Eutin station Neustadt in Holstein station The line ran through the terminal moraine of Ostholstein. It joined the county town of Eutin with the Baltic port of Neustadt. These were three stations on the line: Röbel, Bujendorf and Oevelgönne. Of these, only Bujendorf had a substantial station building.

The county has gently rolling moraine hills left from the retreating glaciers. Because of the glacial action, the soils are highly productive for agriculture. The soils are blount, pewamo and glynwood. The city is located about north of Ohio's capital city, Columbus, due north along U.S. Route 23.

The original crater was probably over high; higher than Kilimanjaro. Since it became extinct there have been two major periods of glaciation, which are shown by two main rings of moraines below the glaciers. The lowest moraine is found at around . Today the glaciers reach no lower than .

2018-19 season Moraine Valley Community College Fine & Performing Arts Center booklet for the 2018-2019 Mainstage season Hirte is a Joseph Jefferson award winner, and a veteran of the Goodman Theater stage, playing their featured actor in their production of Dickens' Christmas Carol for over 20 years.

Tenaya Lake was created by the Tenaya Glacier, which flowed out of the vast Tuolumne Ice Sheet and down to Yosemite Valley. This same glacier created Half Dome. The Tenaya Glacier was lightly loaded with debris, and did not leave a large amount of moraine material near Tenaya Lake.

The northern sector has a large plain behind moraine ridges and hills. The southern sector has more hills and evidence of mid-ridge moraines. The relief is gentle, with sharp edges only on stream banks. The shapes of the lake shorelines are heavily influenced by the activities of beavers.

In the Humber River basin, "interbedded glaciolacustrine stratified sediments and massive to bedded diamicton" occurs in the upper deposition layers (Barnett et al., 1998, pg 1162). Some of these were deposited ice-marginally. In the east, deposition predominantly focused along the glacial margin, for example at the Palgrave Moraine.

The Chicago Lake Plain covers the relatively flat northern quarter of Northwest Indiana north of the moraines. Initially, the plain was flat, composed of glacio-lacustrine deposits. These formed under the waters of glacial Lake Michigan. The lake formed from the melting glaciers north of the Valparaiso Moraine.

"Kivijata" The Lauhanvuori mountain is a high moraine mountain and one of the highest points in Western Finland. The summit area was uncovered 9500 BCE when the glacier retreated, and it has never been under the water. Indeed, it was an island in the middle of the Ancylus Lake.

The islands are often windswept, but have a wild beauty. The severe climate of the outer archipelago gives Brändöskär an unusually barren environment. The terrain consists of rocky outcrops, weathered moraine, rocks and sand. Most outcrops show the effects of glaciation in polishing the rock and creating striations.

The landforms and hydrology of the Eastside, including Forbes Creek, are due to the ice age glaciation. Forbes Creek watershed displays every aspect of typical Eastside moraines described by Harvey Manning and Ira Spring, as an "'unorganized' geography on glacial moraine with bogs and creeks reaching lake level".

The Kaskaskia River has been dammed where it breaches the Shelbyville Moraine, forming Lake Shelbyville. The Army Corps of Engineers broke ground on the dam in 1963, and construction was completed in the early summer of 1970. Tours of the dam are given at 3 P.M. Saturdays and Sundays.

A short track leads off the main path to small tarn, before the track skirts around the moraine wall as it climbs gently to the height of the moraine wall, reaching a lookout point with picnic tables, overlooking the proglacial Hooker Lake. From the lookout, a small path leads down to the shore of the lake.Icebergs floating in Hooker Lake in summer During the summer months, icebergs can be seen floating in the lake, and the lookout also offers views across the lake to the terminus of Hooker Glacier. Frozen lake in winter with broken ice around a small iceberg remnant In winter, there can be snow and ice on the track, and the lake regularly freezes over.

Dubuque is the only metropolitan area. The region is distinct from the "Iowan Erosion Surface to the west and the Southern Iowa Drift Plain to the south."Stephanie A. Tassier-Surine, (Iowa Department of Natural Resources, Geological Survey Bureau), Quaternary Geology of the Paleozoic Plateau Region of Northeastern Iowa , Retrieved July 30, 2007 A line east of the most easterly tributaries of the Wapsipinicon River defines the terminal moraine that marks the western boundary of the Driftless, with the catchment of the Maquoketa River south of Bellevue serving as a southern boundary. The most western tributaries of the Upper Iowa, Yellow and Turkey Rivers flow east and south from the vicinity of this moraine.

From its source in the moraine this river of the Batiscanie flows from north-east to south-west on 11.3 km, at the foot of the large moraine (mountain line extending parallel to St. Lawrence River in the South-West to Nord-East direction). This river flows into the Batiscan River at the heart of the village of Sainte-Geneviève-de-Batiscan and empties near the church. The "Rivière à Veillet" valley covers 37,1 km². The upper valley of the river Veillet was the fourth area of colonization in Lordship of Batiscan (after the bank of St. Lawrence River, of Batiscan River then rivière-à-la-Lime) at the beginning of 18th Century.

Sunset Park is located between Fifth Avenue to the west, Seventh Avenue to the east, 41st Street to the north, and 44th Street to the south, atop a hill that is part of the Harbor Hill Moraine, a terminal moraine formed during the last glacial period. The park's elevated location offers views of New York Harbor; Manhattan; the Statue of Liberty; and, more distantly, the hills of Staten Island and the U.S. state of New Jersey. Initially, Sunset Park contained a pond within its borders. According to Sergey Kadinsky, author of the book Hidden Waters of New York City, the pond was likely artificial since it did not appear on any maps prior to the park's creation.

According to the United States Census Bureau, the CDP has a total area of , of which is land and , or 3.48%, is water. Fishers Island represents a section of the same terminal moraine that formed the North Fork of Long Island, which comes ashore at Watch Hill, Rhode Island. During the late phase of the Wisconsin glaciation, glacial Lake Connecticut formed at the retreating fore edge of the ice sheet, over what is now Long Island Sound; it formed an outlet in its moraine dam at The Race, famous for rip currents, which still separates Fishers Island from the North Fork. Fishers Island is essentially a long barrow of rocky till scoured from the surface of southern Connecticut.

The exchange settled outstanding disputes being considered by the OMB involving moraine lands in Richmond Hill and Uxbridge. Lands acquired by the developers had been previously identified as high-growth urban areas in regional and local Official Plans, often referred to as Seaton. However, the process by which the exchange was settled angered environmentalists, who considered the lack of transparency in the process a betrayal: Josh Matlow, founder of Earthroots, accused the Tories of making a "sleazy, secret, sweetheart deal" with developers. Moreover, the swap allowed the development of 600 acres (2.4 km²) on the moraine; the northern Richmond Hill development ceased operations for several days after the 2003 election, but resumed soon thereafter.

On a clear day, Manhattan's skyscrapers are visible. Geologists generally consider the islands to be terminal moraines --material left by glaciers--deposited about 17,500 years ago as the ice cap paused in its retreat northward. Above water, the moraines are characterized by various rocks, gravel, sand, silt and clay, sometimes sorted out by waves."Norwalk Islands Canoe/Kayak Trail / Calf Pasture Beach, Norwalk, Connecticut" brochure published by he South Western Regional Planning Agency, dated October 1, 2001 The Captain islands in Greenwich to the west are part of the same moraine (but not the Fish islands in Darien), and submerged parts of the same moraine are located between the Norwalk Islands and Charles Island, off Milford, to the east.

Moraine Ridge () is a small ridge in the northeastern part of the Cartographers Range, descending to the southwest flank of Tucker Glacier just south of the junction with Pearl Harbor Glacier, in Victoria Land, Antarctica. It was so named by the New Zealand Geological Survey Antarctic Expedition of 1957–58.

North of Fort Wayne the moraine is simple in structure. It extends from Ft. Wayne along the left bank of the St. Joseph River into Michigan. Through Indiana it is four miles (6.4 km) wide and gets broader through Ohio and Michigan. It rises from to above the Maumee Lake bed.

The Obersee is a natural lake in the extreme southeast Berchtesgadener Land district of the German state of Bavaria, near the Austrian border. All of the lake is within the Berchtesgaden National Park. It is located southeast of the much larger Königssee. The two lakes are separated through a moraine.

Tourism is an important industry for Plymouth, which hosts visitors to events all over Sheboygan County. With an abundance of parks, citywide events, easy access to the Kettle Moraine National Forest and ski hills, Plymouth is an attractive destination for tourists from all over the country. See recreational opportunities below.

Elkhart Lake is located approximately one mile southeast of the northern terminus of the Kettle Moraine Scenic Drive. The Scenic Drive was part of the road racing circuit used in the 1950s. Wisconsin Highway 67 runs north/south through the city. Secondary routes include County Highway A from the northeast.

These terminal moraine ridges mark the southernmost extreme of the prehistoric glacier expansion.Demidov et al., p. 330 Yury Arbat, an ethnographer who studied the folk art of Arkhangelsk outback in the 1960s, described the place: > Nizhnyaya Toyma is not a village ... but a group of villages under a common > title.

Geographically, the area is north of the Oak Ridges Moraine. Bradford West Gwillimbury consists of the town of Bradford and the former Township of West Gwillimbury, and includes the communities of Bond Head, Coulson's Hill,Cottrell Lake - Courtland, GeoNames Index, Ontario Terminology Deerhurst, Dunkerron, Green Valley, Newton Robinson and Pinkerton.

Schinkel's National monument for the Liberation Wars. The Viktoriapark () is an urban park in the locality of Kreuzberg in Berlin, Germany. It opened in 1894. It is situated on the Tempelhofer Berge range, forming the northern slope of the ground moraine Teltow Plateau, overlooking the glacial valley with Berlin's city centre.

The expressway bypass of Butler was built in the early 1960s. Previously, the road ran through downtown Butler. The section that runs through Moraine State Park near Butler was upgraded to expressway standards in 1969. In the 1970s, bypasses were built around the cities of New Castle, Kittanning and Indiana.

It is an "excellent representation of kame moraine features", which are uncommon in the region. It is in the East Holland River subwatershed. The site also demarcates the southernmost advance of the Lake Simcoe sublobe during the Port Bruce Stadial, though most sediments were deposited by the Lake Ontario lobe.

The park contains several glacial landforms such as drumlins and moraine. The most prominent glacial landform in Jacques-Cartier National Park is the Jacques-Cartier Valley (French:Vallée de la Jacques-Cartier). The U-shaped valley is deep and was formed during the last glacial period.Le parc de la Jacques-Cartier - CGQ .

The village sits above the floodplain of the river Mangfall. The landscape is typically post-glacier deranged drainage, with Vagen sited upon a terminal moraine, left by the last glacier in the Vagen area, the Inn-Chiemsee glacier of the Würm glaciation. The area is scattered with longitudinal moraines called drumlins.

Nobleton (2016 population 4,614) is an unincorporated community in southwestern King, Ontario, Canada. It is the third-largest community in the township, after King City and Schomberg. Located south of the Oak Ridges Moraine, Nobleton is surrounded by hills and forests. Many horse farms are found on Nobleton's eastern periphery.

This land was once covered with glaciers. As the glaciers receded they scoured the land creating a moraine, knob like hills, and kettle holes. Some of these kettles are at the top of the hill. This has caused the unusual formation of a swamp at the top of a hill.

Copmanthorpe lies 4 miles south-west of York city centre. The village lies on glacial moraine of sandstone overlain with boulder clay. The highest point of the village is on Top Lane at 81 feet above sea level. The village has two greens, Low Green and the smaller Memorial Green.

Académie de la Moraine is a French first language elementary school located in Richmond Hill, Ontario, Canada. It serves the French population of the GTA. If French is not the student's first language, an admission test can permit one to enrol. It offers busing to students that need that service.

Taycheedah offers adult education, special education, and English as a second language classes to inmates. Inmates can also earn certificates from the nearby Moraine Park Technical College in one of three programs. Credits can be transferred to the Wisconsin Technical College System for continuing education. The prison also offers vocational training.

Kuksina Hill is the highest top of Vaaksaare upland, the eastern part of Haanja upland, with a height of 212 m over sea level. Kuksina Hill is the highest top of Meremäe rural municipality.ehitusinfo.ee, retrieved 25.02.2014 Vaaksaare uplands is a moraine hillock, where agricultural patches alternate with forests and meadows.

However, the stream's lower reaches are on alluvium containing stratified silt, sand, and gravel. The alluvium is approximately thick. The stream also passes through a small patch of fill near its headwaters, where it crosses Pennsylvania Route 118. The Wisconsinan Till Moraine occurs a short distance north of its headwaters.

The Chaypee Woods Trail snakes its way through stone walls that hearken back to farming days when dairy cattle, ducks, and chickens were raised there. Steep steps and slopes mix with the vistas of the salt marsh, oak-hickory forest, freshwater wetlands, kettleholes, moraine, and a Native American midden site.

Forst is a settlement with scattered building in the moraine landscape of Upper Gürbetal. The most important boroughs are Dörfli, Allmid (Allmend), Chromen, Längmoos, and Riedhubel. Of the entire municipal territory of 185 hectares, 79.7% is used for agriculture, 11.8% is forested, and a mere 8% is used for settlements.

Strathcona Fiord is a southern tributary of Bay Fiord. The landscape in the region is fragile and spectacular. The steep hills forming the sides of the valley rise about above sea level. The striking arc of a terminal moraine marks the limit of the last ice advance in the area.

The nine lakes are located within the Chippewa Moraine State Recreation Area (part of the Ice Age National Scientific Reserve), and the Chippewa County Forest, in northern Chippewa County. A network of roads and trails in the Recreation Area and County Forest provide ways to access each of the lakes.

The committee operated from 19911994. Its task was to develop a long-term preservation strategy for the moraine. The committee's final report, submitted to the province in 1994, was never implemented. Instead, the province expanded the powers of the municipalities in administration of the lands that were the subject of the committee's report.

Soil borings used in the investigation Mississinewa moraine and drift located a preglacial valley in Grant and Jay Counties in Indiana. This valley ranged from to respectively in each county. Across its length; it is filed with sand and gravel from the Wisconsin glacial period. This valley may relate to the Teays River.

He was sentenced to one year, but the sentence was never served as the convictions were successfully appealed. Deeds' barn at his Moraine Farm Kettering and Deeds had a lifelong professional relationship and friendship. Deeds provided space in one of his barns for Kettering to work on an electric starter for automobiles.

Aurkleven Cirque is a large cirque, the bottom of which is partially covered with moraine, between Kubus Mountain and Klevekampen Mountain in the Filchner Mountains of Queen Maud Land. It was plotted from surveys and from air photos by the Sixth Norwegian Antarctic Expedition (1956–60) and named "Aurkleven" ("the gravel closet").

The prevailing westerly winds began to treat the 'Lake Kankakee' like the shores of Lake Michigan. Dunes began to form along the south and eastern shoreline. Where ice blocks had been left behind, sand filled the depressions. Runoff from the Valparaiso Moraine built [2] outwash ridges of sand leading into the lake.

Prairie View Elementary School is located on Highway E, set into the gently rolling hills and oak savanna of the kettle moraine area of Wisconsin. The elementary school is a part of the Mukwonago Area School District.Prairie View Elementary Home Page There are three kindergarten classes and three teachers in every grade.

The Usme Fault is located in the Eastern Ranges of the Colombian Andes, south of Bogotá and extends along the western margin of the Tunjuelo River valley. The fault underlies the Sumapaz Páramo.Paris et al., 2000b The fault displaces Cretaceous and Tertiary rocks as well as Quaternary alluvial and glacial (moraine) deposits.

The National Park is divided into two separated areas, Müritz and Serrahn. The first, larger portion extends from the eastern shore of Lake Müritz to the town of Neustrelitz. The latter, smaller part is situated east of Neustrelitz. The landscape features of the park are made up from terminal moraine, sandur and lowlands.

Clarence W. Belt (27 February 1890 in Xenia, Ohio - 15 September 1969 in Moraine, Ohio) was an American racecar driver. He failed to qualify for the 1925 Indianapolis 500 but qualified for the 1928 race. In 1927 he attempted two other Championship Car races but failed to qualify for both of them.

The Wingst is a small geest ridge, covered by mixed woods, that was formed by an ice age moraine. It is surrounded by flat, divided marsh and bog landscapes, that are sometimes only 1 metre above sea level. Dolmens situated within the Wingst indicate that there were early settlements in the local area.

Features of a glacial landscape Glaciers, while geographically restricted, are effective agents of landscape change. The gradual movement of ice down a valley causes abrasion and plucking of the underlying rock. Abrasion produces fine sediment, termed glacial flour. The debris transported by the glacier, when the glacier recedes, is termed a moraine.

During the realignment of several conferences within northeastern Wisconsin, eight schools were joined to form a new conference. Members included: Berlin, Campellsport, Kewaskum, Kettle Moraine Lutheran, Plymouth, Ripon, Waupun and Winneconne. The members choose to name the new conference the East Central Conference as several members were once part of the original ECC.

After university, Peapples joined the General Motors financial staff in Detroit. In 1968, he was transferred to the GM treasurer's office in New York City. There, he was promoted in 1971 to director of the capital analysis and investments section. In 1973, he became assistant divisional comptroller of GM's Delco Moraine division.

Jesse Kremer (born February 28, 1977) is a former American politician, emergency medical technician (EMT), and firefighter. From Kewaskum, Wisconsin, Kremer was born in Moline, Illinois on February 28, 1977. He served in the United States Army and Wisconsin Army National Guard. In 1995, Kremer graduated from Kettle Moraine Lutheran High School.

Narew National Park () is a National Park in Podlaskie Voivodeship, north- eastern Poland, created in 1996.Rozporządzenie Rady Ministrów z dnia 1 lipca 1996 r. w sprawie utworzenia Narwiańskiego Parku Narodowego, The park is a section of the Narew River. It is a swampy valley with moraine hills typical of a braided river.

All the water in the municipality is in lakes. The municipality is located in the Wasseramt district, in the upper moraine landscape along the Solothurn-Herzogenbuchsee main road. It consists of the village of Aeschi as well as, the hamlet of Burgäschi. Burgäschi was part of Aeschi until 1829 and after 1994.

The observation tower at the top of the hill Lapham Peak is a Wisconsin state park located in the Kettle Moraine State Forest. It is just south of Delafield and seven miles (11 km) west of Waukesha. The park entrance is two miles (3 km) north of the Glacial Drumlin State Trail.

The terrain of SR 347 is mainly flat though near US 33, the route skirts the Union Moraine, location of the highest point in the state. No segment of SR 347 is inclusive within the National Highway System (NHS), a network of highways deemed most important for the country's economy, mobility and defense.

Urban Stouffville is approximately 4.5 km long, stretching from the York-Durham Line to Highway 48, and approximately 2.7 km wide with development north and south of Main Street. Stouffville is bounded by farmland and a golf course. The community is located on the Oak Ridges Moraine and the Rouge River watershed.

Muskeget Island is part of the terminal moraine marking the maximum extent of the last glacial ice sheet to reach the northeastern coast. It has an area of . The Muskeget Island group contains Dry Shoal, Skiff Island, Tombolo Point, and Adams Island. Much of Muskeget is owned by the town of Nantucket.

Geographically, it is part of the long moraine ridge known as Vilkyškiai ridge formed during the last glacial period. A large landslide in length and in width occurred on 12 September 1835. Smaller landslides occurred on 21 July 1878 (about in length) and in summer 1926. Today, only its northern slope survives.

The water flowing over this stage is generally clear. As the water passes underneath the lower lobe, however; it has a muddy appearance caused by glacial moraine, which explains the muddy appearance of Kautz Creek. On Pearl Creek (a sub-tributary of Kautz Creek) a few miles to the west, is Pearl Falls.

With new instrument readings, it has been confirmed that lobate debris aprons contain almost pure ice that is covered with a layer of rocks. A ridge interpreted as the terminal moraine of an alpine glacier. Location is Ismenius Lacus quadrangle. Moving ice carries rock material, then drops it as the ice disappears.

The Hanko Peninsula, on which the city is located, is the southernmost tip of continental Finland. The soil is a sandy moraine, and vegetation consists mainly of pine and low shrubs, mostly Calluna. Hanko is known for its beautiful archipelago. The town has a coastline of approximately , of which are sandy beaches.

"Nightlife whirs around you, comfortably, in 'Cocktail Hour: The Show'." The Jersey Journal, 13 Dec. 2018. Web: 23 May 2019. Ballets with a Twist traveled to the Midwest in early 2019, making stops at The Grand Oshkosh, in Wisconsin, and the Moraine Valley Community College Fine and Performing Arts Center, in Illinois.

Road America is a permanent road course. It is located midway between the cities of Milwaukee and Green Bay, and classified as an FIA Grade Two circuit. The track is situated on near the Kettle Moraine Scenic Drive. It has hosted races since September 1955 and currently hosts over 400 events a year.

Unlike some other species of North American pit vipers, such as the timber rattlesnake and Sistrurus catenatus, A. contortrix has mostly not re-established itself north of the terminal moraine after the last glacial period (the Wisconsin glaciation),Anonymous. (year?). Copperhead Snake, Life History Notes. Ohio Division of Wildlife. Publication 373 (399).

The Eastern Continental Divide runs through the region following the top of the Valparaiso Moraine. Besides a few urban areas, much of Northern Indiana lies in the agricultural Corn Belt. Northern Indiana is known for having the third-highest Amish population in the U.S., especially in Allen, Adams, Elkhart, and LaGrange counties.

The word ra is of Old Norwegian origin and means a ridge of gravel. The word is used in Norwegian as a general term about terminal moraine. This structure goes a long way over land and elsewhere under water. In Vestfold and Østfold, this geological formation is very visible and well- known.

The Coldwater River is a river in Simcoe County in Central Ontario, Canada. It is in the Great Lakes Basin and flows from the Oro moraine west of Lake Simcoe to Lake Huron. The river is believed to take its name from its Ojibwa name gisinaa nibiish, which means "cold pool of water".

The biosphere reserve lies in a young moraine landscape formed in the Weichsel glaciation. To the east is the Baltic Uplands, pierced by the Trave, and which runs across the whole of Mecklenburg. In the lake of Schaalsee, that gives the reserve its name, are several islands including Kampenwerder, Stintenburginsel and Rethwiese.

The stream issuing from the glacier will then become clearer as glacial flour diminishes. Lakes and ponds can also be caused by glacial movement. Kettle lakes form when a retreating glacier leaves behind an underground chunk of ice. Moraine-dammed lakes occur when a stream (or snow runoff) is dammed by glacial till.

See the tables on Politics of Massachusetts, Barnstable County, Dukes County, and Nantucket The bulk of the land in the area is glacial terminal moraine and represents the southernmost extent of glacial coverage in southeast New England; similar glacial formations make up Long Island in New York and Block Island in Rhode Island.

The ground moraine and terminal moraine depositions of the Nauen Plateau are partially overlain by marls and glacial sands, left behind by the waters of the thawing ice sheet about 15,000 years before the end of the Weichsel glaciation. The glacial shaping of the relief resulted in a succession of glacial drift, confined space in a change from clays, tills, sands and gravels. On the slopes of the plateau above the Havel lowlands, layers of sand, 10 metres thick, occur at the surface near Groß Glienicke, Kladow and Gatow, such as at the Gatow hill of Windmühlenberg, on the Gatow Heath or near Karolinenhöhe. The dry, nutrient-poor sand here is ideal for the extreme habitat needed for dry grassland.

The basin is bordered at its lower end by a terminal moraine from a lateral valley, and the gravel fill is the result of the lessened gradient behind this morainal dam. Through its boulder-like channel across the moraine the stream descends in rapids, to emerge into a narrow gravel-floored valley bordered by benchlike terraces of gravel and snowing no rock outcrops. These conditions prevail to a point within half a mile of the mouth of the valley, where the stream enters a rock canyon, with nearly vertical walls, that extends to its mouth. Throughout the basin of Crow Creek, the bedrock consists predominantly of interbedded argillites or shales and graywackes, with some conglomerates, cut by numerous granitic dikes and sills.

He founded the Dayton-Wright Airplane Company with Orville Wright, H. E. Talbott, and Kettering. Deeds was appointed Chief of Aircraft Production in Washington D.C. The Delco plant in Moraine, Ohio was expanded to manufacture the DeHavilland DH.4 bomber, the only American-built airplane to see action in World War I. More than 3,000 were built in Moraine. The company produced the Liberty engine. In 1917, he joined the United States Army with the rank of colonel, taking the responsibility for military aircraft procurement at McCook Field, precursor to Wright-Patterson Air Force Base. But, despite the expenditure of $1,000,000,000, no US-built military aircraft reached the front in World War I, and President Wilson appointed Charles Evans Hughes to investigate.

Altar Rock at , Saul's Hill at , and Sankaty Head at are some of the highest points on the island. NASA satellite Image of Nantucket Island Nantucket was formed by the outermost reach of the Laurentide Ice Sheet during the recent Wisconsin Glaciation, shaped by the subsequent rise in sea level. The low ridge across the northern section of the island was deposited as glacial moraine during a period of glacial standstill, a period during which till continued to arrive and was deposited as the glacier melted at a stationary front. The southern part of the island is an outwash plain, sloping away from the arc of the moraine and shaped at its margins by the sorting actions and transport of longshore drift.

Moraine at Dugdale Glacier, ca November 1899 by Carsten Borchgrevink Termination of Moraine at Dugdale Glacier ca November 1899, by Carsten Borchgrevink The Dugdale Glacier is located just below the centre of this map Dugdale Glacier () is a glacier about long, draining northeast from the Admiralty Mountains into Robertson Bay on the north coast of Victoria Land, Antarctica. The geographical feature flows along the west side of Geikie Ridge before coalescing with Murray Glacier just west of Duke of York Island. It was charted by the British Antarctic Expedition, 1898–1900, under Carsten Borchgrevink, who named it for Frank Dugdale of Snitterfield, Stratford-on- Avon. The glacier lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.

At the end of the Wisconsin glaciation, the glacier's Erie Lobe retreated toward the northeast, leaving large debris deposits called moraines. The St. Joseph formed as a meltwater channel between the north limbs of two of these moraines, the Wabash Moraine on the west and the Fort Wayne Moraine on the east. At that time it joined the St. Marys River to drain into the Wabash River. Later, the shrinkage of Glacial Lake Maumee, the ancestor of modern Lake Erie, brought about the opening of the modern Maumee River, which captured the flow of the St. Joseph and the St. Marys, causing the St. Marys to reverse its course to meet the flow of the St. Joseph almost head-on.

Earth Science Field Trip, Guide Leaflet, Kankakee Area, Kankakee High School; 18 May 1957; John C. Frye; State Geological Survey; Urbana, Illinois; 1957 The water came from the melting "Valparaiso glacier", the glacier that deposited first the Manhattan moraine and then other moraines to the northeast in the Valparaiso morainic system. The melt-water came from three glacial lobes of the Laurentide Ice Sheet. In addition to the melt-water from the Michigan lobe in the Michigan basin, melt-water came from the Huron- Erie lobe to the east in the Maumee valley in Ohio and from the Sturgis Lobe coming out of Michigan across northeast Indiana. The water backed up behind the Marseilles moraine, forming a series of lakes.

Moraine Music Group is one of Nashville's leading independent publishers, with a reputation for unique songs that result in career-making hit singles. For a relatively small company, Moraine's songs have appeared on numerous multi- million selling albums spanning various genres of music. Moraine has received over 50 music publishing awards, including 1998 SESAC Publisher of the Year and numerous Canadian Country Music Association Awards for Song, Single, Video and Album of the Year. Moraine’s songs and artists have been included in feature films, television shows, and advertisements including Gareth Dunlop and SHEL's "Hold On" in The Best of Me, SHEL's "I Was Born A Dreamer" in a Toys R Us Christmas advertisement, and Gareth Dunlop's "Devil Like You" in Lucifer.

Raet National Park is named for the long moraine formed by the retreat of a huge glacier about 12,000 years ago, which dumped an enormous quantity of boulders, pebbles, gravel, sand and clay that it had picked up over the centuries. This quaternary geological formation can be traced all over Scandinavia; in Raet National Park it is partly on land and partly under the sea. Pebble beaches are characteristic in areas where the material is graded by heavy seas, but in more protected areas, the moraine forms fine sandy beaches that are attractive to bathers, as occur at Hove on Tromøya and on the island of Merdø. Further inland there is farmland in many places, but these areas are outside the park's boundaries.

The eastern edge of the valley follows the western base of Hamburg Mountain to the New York State line. The valley is about twenty-one miles long and ten miles wide. North of the New York state line is the Hudson Valley. South of the terminal moraine of the Wisconsin Glacier is the Lehigh Valley.

Exodus Valley () is a steep moraine-filled valley which descends northward from Midnight Plateau between Colosseum Ridge and Exodus Glacier, in the Darwin Mountains of Antarctica. It was so named by the Victoria University of Wellington Antarctic Expedition (1962–63) because the valley is virtually the only easy route of descent from Midnight Plateau.

WOLX-FM's signal can reach 33 of Wisconsin's 72 counties, including those along the Lake Michigan shoreline on clear days, though reception is usually blocked by the Kettle Moraine hills northeast of Madison. The station can also be heard in the western suburbs of Milwaukee, in Sheboygan County, and in portions of Illinois and Iowa.

The substrate is covered by the complex of quaternary sediments (glacial, limno-glacial and fluvio-glacial). Moraine is dominant on the area of the northern and middle parts of the county. Gravels, sands, loams and bog sediments are diverged. The geological construction of the substrate is complicated (thickness is varying 10–100 m and more).

The park lies on a glacial moraine, scribed with deep ravines running down to the St. Croix River. Sandstone outcrops have been exposed in some of the ravines. The vertical drop from the blufftop to the water is . A few patches of remnant prairie survived the decades of farming that took place on the blufftop.

The church was built with stone from what would become the Kettle Moraine State Forest. In the 1920s, the church steeple was struck by lightning was replaced with one smaller in height. The church underwent a change of its name in 1965, changing from The German Lutheran Church: St. Johannes to its current name.

When circular, or roughly circular, the diameter of this lichen species has been widely used to help determining the relative age of deposits, e.g. moraine systems, thus revealing evidence of glacial advances. The process is termed lichenometry. This technique is generally attributed to the work of Roland Beschel in the Alps Beschel, R. E. 1950.

The midsection of Queens is crossed by the Long Island straddling terminal moraine created by the Wisconsin Glacier. The Rockaway Peninsula, the southernmost part of all of Queens, sits between Jamaica Bay and the Atlantic Ocean, featuring of beaches.Perez-Rivas, Manuel (February 22, 1994). "Queens in Albany: Beach Nourished by $$$ Series". Newsday. p. 21.

The course of the Missouri in and around the Great Falls has changed very little since then, in comparison to lower regions of the river on the ground moraine that forms much of the upper Great Plains.Maschner, Herbert D. G., and Chippindale, Christopher. Handbook of Archaeological Methods. Vol. 1. New York: Rowman Altamira, 2005.

There are eleven modern cabins available to rent at Moraine State Park. They are heated with electricity and sleep up to six people in two bedrooms. The cabins also have modern bathrooms, kitchens, a dining/living area and a dock on Lake Arthur. Renters need to bring their own bed linens, towels, cookware and tableware.

Neuheim has an area, , of . Of this area, 65.8% is used for agricultural purposes, while 18.1% is forested. Of the rest of the land, 14.3% is settled (buildings or roads) and the remainder (1.8%) is non-productive (rivers, glaciers or mountains). The municipality is located in the moraine landscape between the Lorze and Sihl rivers.

The terrain in this zone is dominated by ice, snow, rock, and glaciers. Glacier-related features like cirques, talus, alpine lakes and moraine are common. Climate is a major barrier to life; the growing season is extremely short. Mean average temperature usually ranges from to , and even in summer the average temperature does not exceed .

He called it Neuburg and it was completed by 1133. In the 14th and 15th centuries the castle fell into ruins. Locals used the stone for buildings and dug into the moraine for gravel. The last remaining stones were used to build the church in 1683, so no physical evidence remains of the castle.

A new logo and more technical synthetic fibers were becoming more specialized. Wigwam developed the Poly-Wool line of performance socks as well as the overnight success—Moraine. From the mid-1980s through the late 1990s the Wigwam 622 slouch socks became very popular. They were worn by kids, tweens, teens, college students and adults.

The northern edge of Glen Oaks is a line of hills which are part of the terminal moraine of the last glacial period. These hills include the highest point in Queens: above sea level. Google Preview retrieved 2009-10-0. Note this book incorrectly relies on ZIP Codes to define the boundaries of Glen Oaks.

Radiocarbon dating of charcoal on a lateral moraine near Nash Crater gave an age of 2,590 ± 150 BP. The Lost Lake cinder cones erupted about 1,950 years ago, along a fissure that trended from north to south near the northern end of the volcanic field. These eruptions blocked the Lost Creek tributary, forming Lost Lake.

Such is the case of the "Comparsa de Morenos de los Veleros" born in 1913 and "Comparsa de los Morenos" of 1924 founded by Aymara migrant families and that come from the ancient dancers of the "moraine comparsas" of the mid- century XIX, finally adopts the name of Morenada in 1950 and 1954, respectively.

The entire county is within the drainage area of the Wabash River. North of Rockville, the gently undulating land is glacial till resulting from Wisconsinan glaciation. The Shelbyville moraine divides this from the nearly level Illinoisan till plain in the south part of the county. Turkey Run State Park is located in northern Parke County.

John R. Sheehy (July 30, 1947) was a Democratic member of the Illinois House of Representatives for a single term from 1993 to 1995. He represented the 37th district, which was located in Chicago's south suburbs. Born in Chicago, Illinois. Sheehy attended Moraine Valley Community College and graduated from Worsham College of Mortuary Science.

Remaining large fragments of ice, leave kettle lakes, when they finally melt. Portions of the layers of glacial till, and gravel, are eroded away, leaving a landscape of lakes and bogs, mixed with hills consisting of layers of different kinds of deposits. Scholars once thought that this moraine marked the edge of the glaciation.

Portersville has several events each year in the immediate and surrounding areas. The Portersville Steam Show occurs three times a year (May, August, and October). This event displays older steam engines and farm machinery to the public. The Moraine/Lake Arthur Regatta (in August each year) has water related activities for the entire family.

They can develop in one winter season or they can be a product of several seasons. Sometimes, they form as a single cone or as multiple cones in a ridge on moraine deposits. Generally, there are many cones on a glacier, snow patch, or ice sheet. They may be similar in size and material.

The Sysen Dam () is a rock-fill embankment dam in the municipality of Eidfjord in Hordaland, Norway. The dam is long, high, and wide at its base. It is built of of stone and moraine deposits. The dam holds back Lake Sysen, which is the main reservoir for the Sy-Sima Hydroelectric Power Station.

The river Lorze is the principal drainage in the canton. It originates in Ägerisee, from where it flows northward through moraine deposits in a deep gorge with fine stalactite caverns. The river eventually enters the Zugersee, very near to where the Reuss originates. The Reuss forms the boundary of the canton in the north west.

The discharge flowed down Boxley Creek Valley, destroying the town of Edgewick, sawmills (owned by North Bend Lumber Company), and parts of the Milwaukee Railroad. The failure did not occur at the dam, but 6,000 feet on the moraine side of the reservoir. Initial discharge rates were estimated between 3,000 and 20,000 second-feet.

Its former location was 13200 Yonge Street in Richmond Hill. However, after George Street P.S. closed, Moraine took up its space. George St P.S students went to Aurora Senior/Wellington P.S. The classes have been split. In the past, there has been a class with both grade 5 and 6 at the same time.

North of the city of Butler, PA 8 meets U.S. Route 422 at an interchange. Near Moraine State Park, PA 8 meets Pennsylvania Route 528 and Pennsylvania Route 173. About east of Slippery Rock, PA 8 meets Pennsylvania Route 108. In the town of Harrisville, PA 8 intersects Pennsylvania Route 58 (Grove City Harrisville Road).

Anvil Crag () is a rock crag rising to west-southwest of Sphinx Hill, King George Island. The vertical crag is at the head of a medial moraine. It was descriptively named by the UK Antarctic Place-Names Committee in 1977; with its three rock faces and flat top, it has the appearance of an anvil.

" Banbridge Leader 20 March 2012, 21. Print. In 2011, he was chosen to perform in the Belfast Nashville Singer Songwriter's Festival where he was awarded 2011 Young Songwriter of the Year. The festival brought Dunlop to Nashville, leading to US tours and a publishing deal with Moraine Music and Nettwerk Music Group."Ones To Watch.

The Peterborough drumlin field is a large physiographic feature to the north of the Oak Ridges Moraine. It has a northeast to southwest orientation, and is cut by a network of deep valleys with wide, flat floors. The valleys are steep-sided, and have a branching pattern. The valley floors also exhibit inset eskers.

However, it seems clear that regulation, alone, is insufficient to preserving these valuable lands. Implementing the plan has required "political will, an engaged and informed public, and... broad based private and public partnerships." Monitoring of the Moraine project by citizens and environmental organizations, along with credible ecological information are essential to its continued preservation.

Nomenklaturen – Amtliches Gemeindeverzeichnis der Schweiz accessed 4 April 2011 The municipality is located in the Vaudois Jura. The town lies on the end moraine of the ice age era Rhone glacier. It consists of the village of Bullet (elevation ) and the hamlets of Les Rasses, Les Cluds, La Crochère, Les Crosats and La Frétaz.

Another is the Frontenac Axis, an exposure of Canadian shield rocks that extends south to the St. Lawrence River near Kingston, creating the Thousand Islands. In south-central Ontario, the ecologically important and politically sensitive Oak Ridges Moraine is a major feature.Eyles, N. Ontario Rocks: Three Billion Years of Environmental Change. Fitzhenry & Whiteside, Markham, Ontario.

Lewis Glacier is in Wenatchee National Forest in the U.S. state of Washington and is southeast of Black Peak. Lewis Glacier is located on the north flank of Corteo Peak just east of the border of North Cascades National Park and has a pronounced terminal moraine now well below the current terminus of the glacier.

Another view of Dawson Lake, north end. The centerpiece of Moraine View is the 158 acre (0.6 km2) Dawson Lake, an artificial reservoir built in 1962-1963. Fish stocked in the lake by the DNR include largemouth bass, bluegill (the state fish of Illinois), sunfish, bullhead, crappie, channel catfish, walleye, yellow perch and northern pike.

Even though he didn't win state, it was a great experience for him. He also qualified for outdoor state as well, with another jump of 6 ft 6. Saul didn't get many schools looking at him finishing up his Senior year. He happened receive a full scholarship to play basketball at Moraine Valley Community College.

A view of the lake from the north-eastern shore. The surface of the lake is approximately 25 to 35 hectares, reaching 65 m in depth. No surface water escapes from the lake. The natural water-retaining formation appeared approximately 400 years ago, when a rockslide added material to an already present glacial moraine.

Here the terminal moraine of the "mini glacier" can be seen from the Feldsee. It has impounded water and formed a bog. The glacial history of the Würm stage, 10,000–11,000 years ago, at the Feldberg evolved as follows: The emergence of the Feldsee happened as the "Feldberg glacier" spread out. The adjacent Feldseemoor was the next stage.

The island is almost entirely granite with some moraine deposits. The inner part of the island is much more hospitable, with oak and other deciduous trees. The island is divided nearly in two halves by the Rasvågfjorden, and the Eie Canal was built through the remaining isthmus so that small boats can pass all the way through.

The Gruvletindane Crags () are rock crags, rising to and forming the north end of the Kurze Mountains of Queen Maud Land, Antarctica. They were mapped from surveys and air photos by the Sixth Norwegian Antarctic Expedition (1956–60) and named Gruvletindane. The feature is bounded on the western side by a large and prominent glacial moraine.

The Hamberg Lakes () are two adjoining lakes lying near the northern outlet of Hamberg Glacier, west of Moraine Fjord, Cumberland East Bay, South Georgia. They were first surveyed by the Swedish Antarctic Expedition, 1901–04, under Otto Nordenskiöld. The name derives from nearby Hamberg Glacier, and was given by A. Szielasko who explored this vicinity in 1906.

U.S. 20 continues as a freeway east of Waterloo. It intersects Iowa Highway 150 at Independence and Iowa Highway 13 at Manchester, as well as junctioning a number of county roads serving smaller communities. Approximately between Independence and Manchester go over a terminal moraine and enter the Driftless Area, a region it will not exit until reaching Stockton, Illinois.

It is a ubiquitous part of the scenery, visible wherever there is no soil cover. Moraine or till is the most common type of soil, covered by a thin layer of humus of biological origin. Podzol profile development is seen in most forest soils except where drainage is poor. Gleysols and peat bogs occupy poorly drained areas.

Aurhø Peak () is a peak with a gravel moraine on the northwest side, situated east of Slettfjell in the Ahlmann Ridge of Queen Maud Land. It was mapped by Norwegian cartographers from surveys and from air photos by the Norwegian- British-Swedish Antarctic Expedition (1949–1952), led by John Schjelderup Giæver, and named "Aurhø" (gravel height).

Aurnupen Peak () is a peak with a gravel moraine on the northwest side, situated north of Flarjuven Bluff on the Ahlmann Ridge in Queen Maud Land. It was mapped by Norwegian cartographers from surveys and from air photos by the Norwegian-British-Swedish Antarctic Expedition (1949–1952), led by John Schjelderup Giæver and named Aurnupen (the gravel peak).

Later, the Cordilleran Ice Sheet carved a deep, north-trending U-shaped valley into the eastern flank of this edifice. The Black Tusk towering above a flower-covered mountain meadow. The light-coloured ridge to the right is a glacial moraine. The Table, a hornblende andesite tuya situated about southeast of Mount Price, rises precipitously above glaciated basement rocks.

Moraine Lake is a glacially fed lake in Banff National Park, outside the Village of Lake Louise, Alberta, Canada. It is situated in the Valley of the Ten Peaks, at an elevation of approximately . The lake has a surface area of . The lake, being glacially fed, does not reach its crest until mid to late June.

Moraine Nature Preserve is located north of Valparaiso, Indiana, east of State Route 49 and south of US Route 6 on County Road 750 North (Meska Rd). Indiana Department of Natural Resources maintains . The preserve has numerous trails through rolling ridges and steep hills left by the glaciers. The area includes potholes and a shallow pond.

The area was also a site classified for the International Biological Program. The Life Science area, known as Cold Creek Swamp, is composed of a swamp and forest. Cold Creek has hiking trails that cover the Oak Ridges Moraine and a boreal peat bog, among others. At least 110 species of birds have been observed at Cold Creek.

Not being able to cut a channel through the limestone ridge in Momence, the Kankakee Lake became of marshland. The outer margin of the Valparaiso Moraine extends from Porter County east into Michigan. It consists of an extensive outwash apron. It slopes to the southeast over an to distance, dropping from or to above sea level.

The land where Lakeview now exists was annexed in the period between 1975 and 1979. It includes part of the Sutherland Moraine, a ridge that forms a local topographic high. Home construction was at its peak from 1981 until 1985. Lakeview School officially opened on November 24, 1981, and St. Bernard School opened on April 2, 1982.

Rolf's Educational Center provides Head Start, Title I, and Early childhood education programs. The district also operates an alternative school, the West Bend Online Learning Academy. Post- secondary schools in West Bend include University of Wisconsin-Milwaukee at Washington County (UWM-WC) and Moraine Park Technical College. There are also a number of private schools in West Bend.

The Wuhle is a small right-bank tributary of the Spree. It originates in a ground moraine in Brandenburg near Ahrensfelde and flows through the Berlin boroughs of Marzahn-Hellersdorf and Treptow-Köpenick before joining the Spree. It is the primary in- and outflow of the Wuhlebecken. The Wuhle is depicted in the coat of arms of Marzahn-Hellersdorf.

Bertrand Lake is a Chilean lake located in the Aysén del General Carlos Ibáñez del Campo Region. It is separated from Plomo Lake by a terminal moraine and is flanked on the west by the summits of the Cordón Contreras. The village of Puerto Bertrand is located at the southern tip of the lake, where Baker River originates.

Out of the forested land, all of the forested land area is covered with heavy forests. Of the agricultural land, 55.2% is used for growing crops and 8.5% is pastures. All the water in the municipality is in lakes. The municipality is located in the Wasseramt district, on the moraine landscape left behind by the Rhone glacier.

Out of the forested land, all of the forested land area is covered with heavy forests. Of the agricultural land, 41.1% is used for growing crops and 11.8% is pastures. All the water in the municipality is flowing water. The municipality is located in the Wasseramt district, on the Solothurn-Herzogenbuchsee in the hills created from a terminal moraine.

Accessed July 25, 2014. Wood County spans two of Wisconsin's five geographical regions. The northern part of the county is in the Northern Highlands, with mostly rich cropland with heavy clay soil, used for corn, soybeans, hay and dairy. In the northwest corner the Marshfield moraine runs from Marathon County through Marshfield, Bakerville and Nasonville into Clark County.

Morschach Aerial view (1953) Morschach has an area, , of . Of this area, 52.3% is used for agricultural purposes, while 36.2% is forested. Of the rest of the land, 2.9% is settled (buildings or roads) and the remainder (8.6%) is non-productive (rivers, glaciers or mountains). The municipality is located on a glacier moraine above the Lake of Lucerne.

Gutiérrez Lake () is a lake of the lake region of northern Patagonia in the province of Río Negro, in Argentina. It is of glacial origin, being a Moraine- dammed lake. The lake is connected to Nahuel Huapi Lake. It was named by explorer and naturalist Francisco P. Moreno as an homage to his academic mentor Juan María Gutiérrez.

In 2006 the Conference ceased to exist and members were reassigned. St. Francis, Pewaukee, and Brown Deer went to the Woodland Conference. Whitefish Bay Dominican now competes in the Midwest Classic-Classic Division; Watertown Luther Prep joined the Capitol-Northern Division; Slinger shifted to the Wisconsin Little Ten; and Kettle Moraine Lutheran moved to the Wisconsin Flyway.

This can be attributed to the Cocos Plateau formed from glaciers during the last ice age. The reason the Opasquia Park has been protected as a wilderness park has more to do with its distinctive geology. A ridge of glacial till two kilometres wide rises 100 metres above its surroundings here. This is called the Opasquia Moraine.

The South Branch of the Kishwaukee River originates near Shabbona on the Cropsey Moraine. The river flows north to Genoa where it then turns westward and then flows north-northwest and joins the North Branch near Cherry Valley. The South Branch's average width is . The Kishwaukee River drainage area includes McHenry, Boone, Kane, DeKalb, Ogle, and Winnebago Counties.

Hamberg Glacier () is a glacier which flows in an east-northeasterly direction from the northeast side of Mount Sugartop to the west side of the head of Moraine Fjord, South Georgia. It was charted by the Swedish Antarctic Expedition, 1901–04, under Otto Nordenskiöld, who named it for Axel Hamberg, a Swedish geographer, mineralogist and Arctic explorer.

It is located hinter der Egg or behind the left-hand side moraine that was left behind after the Reuss glacier retreated from the upper Wyne valley at the end of the last Ice Age. It consists of the village of Gontenschwil and the hamlets of Geisshof (that transferred from Reinach to Gontenschwil in 1901) and Hasel.

Camping shelter at Lake Tennyson The small glacial lake is above sea level. A broad moraine with a number of tarns (i.e. mountain pools) forms the downstream side of the lake. There is a basic camp ground provided by the Department of Conservation next to the lake, free to use on a first come, first served basis.

Little Temple is a mountain summit located in Banff National Park of the Canadian Rockies of Alberta, Canada. Little Temple is situated in the Bow River Valley between Paradise Creek and Moraine Creek, south of Lake Louise, Alberta. The mountain can be seen from the Icefields Parkway along with its nearest higher peak, Mount Temple, to the southwest.

Geologically, the falls were formed at the end of the last ice age approximately 13,000 years ago. Formerly the Passaic had followed a shorter course through the Watchung Mountains near present-day Summit. As the glacier receded, the river's previous course was blocked by a newly formed moraine. A large lake, called Glacial Lake Passaic, formed behind the Watchungs.

Ernen and Fiesch viewed from Fiescheralp Ernen has an area, , of . Of this area, 36.1% is used for agricultural purposes, while 35.4% is forested. Of the rest of the land, 1.5% is settled (buildings or roads) and 27.0% is unproductive land. The municipality is located on a moraine terrace above the left side of the Rhone.

Upstream of the Totowa Stage, and lying between Second and Third Watchung Mountain, was the Stanley Stage. The lake occupied an area between Stanley (near Summit) and Millington, and was held back by moraine deposits. As with the Totowa stage, the lake's earthen dam eroded away until the lake reached its modern level, forming Glenhurst Meadows.

The municipality comprises the villages of Bartenshagen, Parkentin, Huetten, Neuhof and Bollbruecke. Bartenshagen-Parkentin lies between Bad Doberan and the Hanseatic city of Rostock. The municipality has two parts: Bartenshagen lies on the slightly raised area of basal moraine of Haegerort approximately 7 km from the Baltic See. Parkentin lies approximately 3 km south from the centre of Bartenshagen.

A friend of the family made a connection with Grammy- winning producer Brent Maher of Moraine Music Group, which led to a publishing deal. Over three years SHEL completed several EPs, and released a self-titled debut album. Between 2010 and 2011, they were signed with Republic Nashville, but did not release anything for the label.

The Alb has a gorge there with small waterfalls, one of them manmade. A little higher up, a prominent end moraine embankment crosses the valley. The narrow water gap of the stream, the Menzenschwand splash dam reservoir (Menzenschwander Kluse), was previously used to store water for log rafting. The basin-shaped mouth area is a sedimented, former lake.

The glacier was, at that time, a glacier that nearly reached tidewater.(Wilderness Essays, The Alaska Trip (pg 60) John Muir). It has since receded into the mountains, becoming a valley glacier, and created its very own glacial lake in the glacier's moraine (similar to the Mendenhall Glacier and lake) about one mile inland from the Chilkat Inlet.

Payne Brook is a river that begins southeast of the Village of Madison in Madison County, New York. It flows west then turns southwest before flowing into Lake Moraine. It then exits the lake and flows southwest through the Village of Hamilton, flowing through Taylor Lake in the village, before converging with the Chenango River by Randallsville.

Montana was signed to a songwriting deal with Moraine Music in 1994. He was picked up by Curb Publishing in a joint venture in 2000. The following year, Jo Dee Messina released Montana's "Bring On the Rain" as a single. The song topped Billboard's Hot Country Singles & Tracks in March 2002 and was nominated for a Grammy Award.

Forbidden Glacier is on the north slopes of Forbidden Peak, North Cascades National Park in the U.S. state of Washington. The glacier is approximately in length, in width at its terminus and descends from . The glacier is separated by an arête from Boston Glacier to the east and south. Meltwaters from Forbidden Glacier flow into Moraine Lake.

For an old moraine landscape the Heide-Itzehoe has relatively large height differences. At just under 80 metres above sea level the highest elevations on the west coast of the state are found on the Heide-Itzehoe Geest. The soils are very unsuitable for agriculture (with an 'arable value' of between 26 and 35 on a scale of 100).

Fonthill shares its name with the Fonthill Kame, on which it is located, formed by glacial deposits. Effingham Creek, a cold-water stream, originates in the glacial silts and sands of Short Hills area of the moraine, northwest of Fonthill. Effingham Creek is a tributary to Twelve-Mile Creek, which empties into Lake Ontario.Short Hills Nature Sanctuary .

During the Second World War the tunnels of the as-yet-to-be-commercially used Wanstead underground station were utilised for aircraft production. Wanstead Flats was used for Anti-Aircraft batteries protecting London, Barracks for Pre-D-Day troops and a Prisoner-of-War Camp subsequently. Due to terminal moraine (left by glaciers) the soil was relatively infertile.

In the beginning a fissure opened at right angles to the ice flow which was from the southeast to the northwest. It was about 15 km from the glacier snout. There is a big terminal moraine at the coast at Álftanes. Rapid ice melting was the consequence of explosive eruption and therefore magma fragmentation from the beginning on.

Badger is located on the terminal moraine of the outwash plain of a glacier that stopped in the area during the Wisconsin Glaciation approximately 12,000 years ago. The bedrock in the area consists of quartzite, sandstone, shale, and limestone. Groundwater flow is influenced by the Baraboo Hills to the north and the Wisconsin River to the east.

I-79 leads south to Pittsburgh and north to Erie. Moraine State Park, situated around Lake Arthur, is a short distance east of I-79. Portersville lies between the cities of Butler east and New Castle to the west. According to the United States Census Bureau, the borough has a total area of , all of it land.

The upper Aire valley was formed 12,000 years ago by a retreating glacier. A moraine formed in the Cononley area and the lake stretched as far north as Gargrave. Colonisation by man developed later on, especially during the Iron Age. The peoples that occupied the Aire Valley (and much of north eastern England) were called Brigantes by the Romans.

The core of snow is protected from ablation while the surrounding snow patch continues to melt. This is another way dirt cones can form. Even areas with a very small debris load, like Antarctica, can have dirt cones. The dirt cones in Antarctica are formed from the moraine deposit material left behind when a glacier retreats.

Myrmel (Myrmæl Bruk) is one of the largest and oldest farms the sub-parish of Sande in Sunnfjord, Vestland county, Norway. Myrmæl - Norway (stad.com) Myrmel lies on a sunny hill with moraine soil, which is excellent to cultivate. On the other hand, it was full of big stones, thus it was sometimes difficult during the haying.

Lake Shetek began forming as the climate started to warm 15,000 years ago. Water from the melting glaciers carved channels into the moraine. Where one channel—now occupied by Beaver Creek—intersected the channel now occupied by the Des Moines River, a buildup of sediment and slumping banks partially dammed the outflow, creating a large, shallow lake.

Whitewater is a city located in Walworth and Jefferson counties in the U.S. state of Wisconsin. Located near the southern portion of the Kettle Moraine State Forest, Whitewater is the home of the University of Wisconsin–Whitewater. As of the 2010 census, the city's population was 14,390, which includes 11,150 in Walworth County and 3,240 in Jefferson County.

The largest and best known forests of the municipality include the Honeret, Guggenbüehl and Röhrenmoos. The Honeret forest lies on a side moraine of the Linth glacier ("Linthgletscher"). There are over 200 prominent stones through the woods, up to erratic boulders as big as . The Honeret and the Guggenbüehl-Wald are separated by only one main street.

Lying directly atop the Cretaceous rocks is till just a few thousand years old. All intermediate rock had eroded away before the till was deposited in a ground moraine by continental glaciers. Within Flandrau State Park this glacial debris is thick. While the till contains some rock from Canada and northern Minnesota, most is from the local region.

From the Parking lot "Alpingrad" ascents are made to the peaks of Amangeldy, the pioneer-Teacher array, Panfilov Heroes, Manshuk Mametova, Antikainen. Then there is the well-known moraine lake No. 6. The Mynzhylki mountain plateau is located at the source of the Little (Malaya) Almaatinka river, 28 kilometers South of Almaty. The tract is surrounded by Tuyuksu glaciers.

The dam can consist of glacier ice or a terminal moraine. Failure can happen due to erosion, a buildup of water pressure, an avalanche of rock or heavy snow, an earthquake or cryoseism, volcanic eruptions under the ice, or massive displacement of water in a glacial lake when a large portion of an adjacent glacier collapses into it.

Watershed of Big Creek, Ontario. Big Otter Creek (alternately Otter River, Big Creek) is a waterway that empties into Lake Erie at Port Burwell, Ontario. It is long, and the area of its drainage basin is . The creek's headwaters are north of the Horseshoe Moraine, and its mouth is just west of the Long Point Conservation Area.

Forest–Moraine Residential Historic District is a national historic district located at Hammond, Lake County, Indiana. The district encompasses 108 contributing buildings in an exclusively residential section of Hammond. It developed between about 1913 and 1950, and includes notable example of Renaissance Revival, Colonial Revival, Tudor Revival, and English Cottage style residential architecture. Note: This includes and Accompanying photographs.

The Hahnheide is a wooded moraine landscape in the east of the municipality Trittau (Stormarn County) in Schleswig-Holstein, in Germany. The name Hahnheide means derived in today's language High Heath. In the Middle Ages the Hahnheide was still associated with the Sachsenwald. Due to the economic use until 1821 the forest stock shrank more and more.

Most residents in rural Dover Township rely on wells or ponds for water. Most of the township gets its water from the Oak Openings Beach Ridge Aquifer. Eastern portions closer to the Tiffin River draw from the Lake Maumee Lacustrine Aquifer. A small northern portion of higher elevations in the north are Williams End Moraine Aquifer.

The formation continues under water as a series of reefs. At high tide its extreme point becomes five small island called Killingarna ("the [goat] Kids"). The moraine reappears twelve kilometers away on the western shore of Vänern, where it is known as Hjortens udde. In addition to pines, rowans, birches and aspens grow on Hindens rev.

The villages Gödnitz and Flötz are between the towns Zerbst and Barby. Next to the villages there is the Gödnitz Lake which is an oxbow of the Elbe. Both villages are on the eastern side of the Elbe at the end of the moraine. The western part of Gödnitz/Flötz is a part of the Mittelelbe Biosphere.

Armonini Nunatak () is a partly snow-covered rock outcrop about east-southeast of Mount Reu in the Prince Charles Mountains. There is an area of moraine on the northwest side. It was plotted from Australian National Antarctic Research Expeditions air photos taken in 1960, and named for G.C. Armonini, a weather observer at Davis Station in 1962.

Koepp was born in Pewaukee, Wisconsin, to a family therapist mother, and Donald Koepp, who owned a billboard company. While attending Kettle Moraine High School in Wales, Wisconsin, he worked evenings and weekends at the McDonald's restaurant in Delafield. He received his bachelor's degree in film from UCLA. He has a wife, Melissa, and four children.

Raet also attracted settlements, so that the oldest, largest and best farms are still there. Similarly tumuli in Iron Age often was located along Raet.Einar Østmo: Arkeologi for alle (s. 94), Landbruksforlaget, Oslo 1998, The top of the moraine has been used as road from prehistoric times, and in some places Raveien is the name of the road.

The western part of Anholt is a moraine landscape. The small village is situated in the middle of the landscape, whereas the harbour (built 1902) is at the northwestern tip of the island. The eastern part of the island is known as Ørkenen (the desert). This desert-like area is the largest of its kind in Northern Europe.

Lithograph by R. de Moraine from 1864 showing townsfolk burning the exhumed skeleton of an alleged vampire. Many myths surrounding vampires originated during the medieval period. The 12th-century British historians and chroniclers Walter Map and William of Newburgh recorded accounts of revenants, though records in English legends of vampiric beings after this date are scant.Jones, p. 121.

The trail passes through a climax community of pacific silver fir and related species of disparate ages with many standing snags. In the fall, a large variety of mushroom species emerge. Near elevation, the trail ascends a lateral glacial moraine. At the route ascends about of Class 2 rock and of steep subalpine forest to reach the ridge crest.

The river that drained from Lake Agassiz is called the Glacial River Warren. It flowed over the top of a recessional moraine at Browns Valley. As the water eroded away the glacial deposits, the level in the lake dropped. Eventually enough large boulders were left behind that a boulder pavement was produced, which inhibited further downward cutting.

The Bungsberg is an ice age terminal moraine. Unusually, though, it was formed in the Saale glaciation period about 150,000 years ago. During the subsequent Weichselian glaciation – only about 10,000 years ago – the ice sheet could not cover the hill due to its height, it could only flow around it, and it therefore formed a nunatak.

The Bloomington Ridged Plain covers only the most southern part of Northwest Indiana in the valley of the Iroquois River in southern Newton and Jasper counties. This area consists of low and rolling hills, i.e., moraines like the Iroquois Moraine with less than 300 ft changes in elevation. The soils are loamy till, lake clay and silt.

This moraine is a major source of gravel for the region which adjoins Anacortes, Washington. The trails in this corridor are maintained but are of variable quality. Almost all are ideal for mountain biking, in particular. Little Cranberry Lake is a popular swimming location, especially for visitors to the annual summer music celebration, What the Heck Fest.

Affoltern has an area of . Of this area, 45.7% is used for agricultural purposes, while 28.9% is forested. Of the rest of the land, 25% is settled (buildings or roads) and the remainder (0.5%) is non-productive (rivers, glaciers or mountains). The municipality is located west of the Albis hills in the moraine landscape around the Reuss.

Solitary tree (Fraxinus excelsior) on Kõrgelaid Kõrgelaid is a small, uninhabited, moraine-based island in the Baltic Sea, belonging to the country of Estonia. Its coordinates .Wikimapia.org Kõrgelaid lies off the western coast of the Estonian mainland between the islands of Hiiumaa and Muhu, just south of the small island of Rooglaid. It is administered by Hiiu County.

The principal drainage divide between the North Sea and the Baltic Sea runs across the Barnim plateau from Northeast to Southwest. It also runs between the drainage basins of the Elbe and Oder rivers. Its course roughly follows that of the Frankfurt push moraine. The main features along the divide include the Wandlitzer See and the Liepnitzsee.

The lighthouse sits on 88 wooden piles driven into glacial moraine. These are linked horizontally by walling pieces, using 500 cast-iron plants and bolts. These would have formed a box, probably square or octagonal, which would have been excavated and partially filled with concrete. The materials were delivered by boat and work undertaken during low tide.

The viaduct is located on the Rhaetian Railway's metre gauge line from Chur to the holiday and recreation resort of Arosa (the Chur-Arosa line), between Peist and Langwies, at a place known as Matten-Gründji. It leads the railway line over the Gründjitobel, a steeply eroded gravel moraine gorge, with sandy formations known as "Steimannli".

A small portion of the valley of Hemlock Run is on bedrock consisting of sandstone and shale. The Wisconsinan Till Moraine occurs near the stream in its lower reaches, as does the Wisconsinan Bouldery Till. Both of these are glacial or resedimented glacial tills. The latter has boulders consisting of quartz, sandstone, and conglomerate on the surface.

Firn and snow fields were reported in the middle 20th century on the El Tatio volcanic group, at elevations of . The region is too dry to support glaciers today, but in the past higher moisture allowed their formation on mountains of this part of the Andes; glacially eroded mountains and moraines testify to their existence in the form of large valley glaciers. A large moraine complex, including both terminal structures and well-developed lateral moraines, can be found north of the geyser field and reflects the existence of a long glacier, the longest valley glacier in the region. Two more moraine systems extend westward both northeast and southeast of El Tatio, and the terrain surrounding the geyser field is covered by sands that are interpreted as glacial outwash sands.

These are the Muncie esker system and a pair of ice- walled troughs in southern Grant County. North of the edge of overlap by the Lagro Formation, ice-disintegration ridges change character because of the changes in till lithology, and long, narrow, shallow ice-walled channels extend across the till plain. These channels are floored with Lagro till, although in many gravel lies below the till, and some segments of the Muncie esker system are capped with the same till. Northwest of Alexandria the edge of the Lagro till is distinct and readily mapped along the low Union City Moraine but from Alexandria to eastern Delaware County the moraine ceases to look like an active ice feature and seems to merge with the dead ice topography of that region.

Pleasant River in flood The outlet control structure at the south end of Little Sebago Lake failed on 4 June 1814, and within a few hours water draining to the Pleasant River eroded a channel through the moraine, dropping the lake elevation . The resulting flood swept away two mills and six bridges along the Pleasant and Presumpscot rivers as far downstream as South Windham.Varney, George J. A Gazetteer of the State of Maine (1886) B.B.Russell, Boston Drainage from Little Sebago Lake was permanently diverted from Outlet Brook into the Pleasant River by destruction of the moraine, although the lake level was partially restored by construction of a stone dam at the narrows in 1860. That dam failed with similar downstream damage on 7 May 1861, but has subsequently been rebuilt.

More commonly, these sediments lose their original structure through the mixture processes associated with subglacial transport and they solely contribute to form the more or less uniform matrix of the till. Till is deposited at the terminal moraine, along the lateral and medial moraines and in the ground moraine of a glacier. As a glacier melts, especially a continental glacier, large amounts of till are washed away and deposited as outwash in sandurs by the rivers flowing from the glacier, and as varves (annual layers) in any proglacial lakes which may form. Till may contain detectable concentrations of gems or other valuable ore minerals picked up by the glacier during its advance, for example the diamonds found in the U.S. states of Wisconsin and Indiana, and in Canada.

The Charest River flows south, crossing the rows St. Paul, St. Achilles and Sainte-Anne, in Saint-Ubalde and gradually goes away from the boundaries of the Lac-aux-Sables. In his course, going toward the boundary Saint-Ubalde and Saint-Adelphe, this river gets water from lakes Sainte-Anne and Perch. Then the river flows South-East (almost in parallel to the Batiscan River) and through 16 lots in the First Price Row in the Eastern section of Saint-Adelphe, where its course becomes very coil. After descending the moraine more than a kilometer in the North-East row in the municipality of Sainte-Anne-de-la-Pérade, Charest River forks to 90 degrees to the right (southbound) entering Saint-Prosper-de-Champlain, moving towards the village, along the foot of the moraine.

The northwestern corner of Whitchurch–Stouffville is outside the moraine and is part of the Schomberg Lake plain, an ancient lake-bed overlain by silts and fine sands. The soil formed over the former lake-bed is well-drained, arable farmland. The southernmost portion of Whitchurch–Stouffville west of Highway 48 lies below the moraine and is a clay-loam till plain. Tree species native to Whitchurch–Stouffville include: American Mountain Ash, Balsam Fir, Bitternut Hickory, Black Cherry, Black Spruce, Bur Oak, Eastern Hemlock, Eastern White Cedar, Peachleaf Willow, Pin Cherry, Red Oak, Red Maple, Red Pine, Shagbark Hickory, Silver Maple, Sugar Maple, Tamarack, Trembling Aspen, White Birch, White Oak, White Pine and White Spruce.For more detail, see Ontario Ministry of Natural Resources, Ontario Tree Atlas: Ecodistrict 6E-7.

Sources from the 14th to the 16th century counted the entire upper and lower geest west of the Jeetze plain and east of the Uelzen-Bevensen Bowl as well as the Dahlenburg Basin as the Drawehn. In this sense the term is defined as the main ridge of the East Hanoverian End Moraine including its foothills as well as the flatter eastern slopes to the fluviatile Lüchow plain. The northern end of the East Hanoverian End Moraine can be further subdivided into the Göhrde and Klötzie regions – with no clear cut transition or boundary. The Klötzie (also the Elbhöhen or "Elbe Heights") is the northern edge of the ridge, up to 70 metres high, which slopes steeply down to the glacial valley of the River Elbe between Hitzacker and Neu Darchau.

The Battle Pass area from the 1776 Battle of Brooklyn in the American Revolutionary War (1775–1783), an etching circa 1792 Approximately 17,000 years ago the terminal moraine of the receding Wisconsin Glacier that formed Long Island, known as the Harbor Hill Moraine, established a string of hills and kettles in the northern part of the park and a lower lying outwash plain in the southern part. Mount Prospect (or Prospect Hill), near the intersection of Flatbush Avenue and Eastern Parkway, is one of the tallest hills in Brooklyn, rising 200 feet (61 m) above sea level. It is the highest among a string of hills that extends into the park, including Sullivan, Breeze, and Lookout hills. The area was originally forested, but became open pasture after two centuries of European colonization.

Map of Glacial Lake Maumee, Saginaw, and Chicago, based on the USGS Report of 1915As the Erie Lobe retreated to the northeast, it left large debris deposits called moraines running at right angles to its line of retreat. One of these, called the Fort Wayne Moraine, was left at the site of present-day Fort Wayne, Indiana, where it acted as a dam that held back the waters of the lake. When the water was at its highest point, about 800 feet above sea level (ASL) (244 m), it left beach ridges that later became the routes of trails and highways. During this stage, the waters of the lake, possibly in response to an advance of the ice front at the lake's eastern end, overtopped a "sag" in the Fort Wayne Moraine.

Lake Llanquihue is the second-largest lake in Chile with an area of about . It is situated in the southern Los Lagos Region in the Llanquihue and Osorno provinces. The lake's fan-like form was created by successive piedmont glaciers during the Quaternary glaciations. The last glacial period is called Llanquihue glaciation in Chile after the terminal moraine systems around the lake.

This tarn formed in the hollow that was scoured out by the ice pushing down the headwall of the cirque. Gradually the ice created a bowl that now holds the 33-metre-deep Feldsee. A moraine on the shores of the Feldsee testifies to this process. The Feldseemoor, a few metres away, is also a remnant of the ice age.

He also expounded on Fenton's modesty, describing him as infinitely more mature than himself and Martin Amis. Fenton and Hitchens shared a house together in their third year, and continued to be close friends until Hitchens's death. Fenton read his poem 'For Andrew Wood' at the Vanity Fair Hitchens memorial service. His first collection, Terminal Moraine (1972) won a Gregory Award.

Mafic dikes up to 20 feet in width occur throughout the area. Glacial advances occurred 7,000, 5,000 and 500 years ago, with the last extending to the entrance of the bay, where it left a huge semicircular terminal moraine. The consequent surface glacial deposits include gravels as outwash and moraines. Glacial gravels extend up to 2000 feet up the mountain slopes.

Moraine Bluff () is a bluff in Antarctica, high, on the east side of Skelton Glacier, lying north of Red Dike Bluff. It was surveyed and named in 1957 by the New Zealand party of the Commonwealth Trans-Antarctic Expedition (1956–58), and so named because a long morainic strip extends from the foot of the bluff on to Skelton Glacier.

The only lake of any size is Ljungsjön, situated in the central part of the parish. The highest shore-line passes through the parish, resulting in varied ground conditions. An ice lake delta once covered the eastern parts of the parish, leading to deposits of gravel and sand, which are being exploited. Moraine eskers are found in the northern and eastern parts.

The Settle to Carlisle railway runs along the western side of the valley here. Mid Wensleydale is made of Great Scar limestone under Yoredale beds that make up the valley sides which are marked with stepped limestone scars. The valley floor is made from glacial drift tails and moraine. The river here is broad and gently flowing in meanders in a stony channel.

Schloss Lauterbach stands on a moraine hill in the east of the village of Lauterbach, about west of the town of Dachau north of the autobahn between Augsburg and Munich. The main castle complex is surrounded by a moat to the south and west, almost always dry, which is scarcely visible due to the woods that have been allowed to grow.

The Aurkvaevane Cirques are a set of three cirques with moraine-covered floors, indenting the west side of Kvaevefjellet Mountain in the Payer Mountains of Queen Maud Land. They were discovered and plotted from air photos by the Third German Antarctic Expedition, 1938–39, and re-plotted from air photos and from surveys, and named, by the Sixth Norwegian Antarctic Expedition, 1956–60.

In 2014, GM Moraine Assembly was purchased from IRG by China-based Fuyao Glass Industry Group Co. Ltd. Fuyao manufactures automotive glass for GM and other automakers. Operations at the Fuyao plant began in late 2015. Fuyao Glass America's first customer was Hyundai Motor Company; additional clients added since startup include GM, Volkswagen, Fiat Chrysler, BMW, Honda, and US replacement-glass chain Safelite.

It continues into Michigan as far as Montcalm County. It was formed during the Crown Point Phase of the Wisconsin glaciation. At this time the glacier covering the area had grown thin, so it was restrained by dolomite rock layers in the Lake Michigan basin. Where the glacier stopped, glacial till and sand was deposited, creating the hills of the moraine.

It is a mildly flat area between the uplands with some lonely moraine hills. The Valleys of Koiva River and Mustjõe River together with the Aheru Lake form a very picturesque area. The area of forest land of the county is almost 114,000 hectares, which forms 56.7% of the area of Valga County. Pine and spruce are the main species.

Lake Hauroko. There are some 3,820 lakes in New Zealand with a surface area larger than one hectare. Much of the higher country in the South Island was covered by ice during the glacial periods of the last two million years. Advancing glaciers eroded large steep-sided valleys, and often carried piles of moraine (rocks and soil) that acted as natural dams.

The composition of this proglacial region is reported to be a mixture of ground/recessional moraines with linear country outcrops protruding out. The glaciation must have extended up to a little downstream of Dhanchu as revealed by the terminal moraine hump. During the last 37 years, the glacier receded by with an average retreat of /year. The area vacated is estimated at .

Thorn Creek is a U.S. Geological Survey. National Hydrography Dataset high- resolution flowline data. The National Map, accessed May 19, 2011 tributary of the Little Calumet River that travels through Will and Cook counties in northeastern Illinois just south of Chicago. It starts in the high land of the Valparaiso Moraine before dropping to the lower elevations of the Little Calumet River valley.

Birch Island Provincial Park is a remote provincial park located on Lake Winnipegosis in Manitoba, Canada. The park is bordered on its western boundary by the Swan-Pelican Provincial Forest and on its eastern side by Chitek Lake Anishinaabe Provincial Park. Surface bedrock on Birch Island is Devonian limestone and dolomite. The Keewatin Glacier contributed a 4 foot layer of ground moraine.

Thus, this lake and Lake Kankakee were held in check. The terraces and beaches in the Morris Basin are above sea level or above the present head of the Illinois River. This shows that this lake existed during the Valparaiso Moraine stage. The lakes level extended up the Kankakee River Valley about as far as Braidwood, where the sand dunes set in.

Lewis 1969; Calkin and Feenstra 1985; Holcombe et.al. 2003 The increase in water, the growing humidity in the climate, and increased water levels created a large delta in western basin at the mouth of the ancestral Detroit River.(Herdendorf and Bailey 1989 The remaining depositional features in Lake Erie (i.e. the Buffalo Ridge, Norfolk Moraine, Conneaut Bank, and Presque Isle Bank) were flooded.

According to the United States Census Bureau, the town has a total area of 74.9 square miles (193.9 km2), of which 74.0 square miles (191.7 km2) is land and 0.9 square miles (2.2 km2) (1.14%) is water. Much of Rib Lake is hilly, with small glacial lakes. It lies within the Perkinstown terminal moraine, which is described under Taylor County.

Aurdalen Valley () is a small moraine-covered valley between Grakammen Ridge and Aurdalsegga Ridge, in the Petermann Ranges of the Wohlthat Mountains. It was discovered and plotted from air photos by the Third German Antarctic Expedition, 1938-39, re-plotted from air photos and from surveys by the Sixth Norwegian Antarctic Expedition, 1956–60, and named "Aurdalen" ("the gravel valley").

Swiss Federal Statistical Office-Land Use Statistics 2009 data accessed 25 March 2010 The former municipality is located on a hill built up from a moraine on the road between Halten and Seeberg. It consists of the villages of Heinrichswil and Winistorf. Hersiwil had an area, , of . Of this area, or 67.8% is used for agricultural purposes, while or 22.4% is forested.

With the Kankakee River, the Illinois River watershed stretches from the Illinois border in northwest Indiana and up into Michigan's Berrien County, adjacent to St. Joseph County. This drainage area include most of the state known as the Northwest Indiana, including the city of La Porte but excluding the area north of the Valparaiso Moraine which drains into Lake Michigan.

Baxter is just north of Minnesota's geographical center, in a terminal moraine area created by the Superior Lobe of the Labradorian ice sheet. The city is home to numerous lakes and ponds. Baxter is bordered on the west by Cass County and on the east by Brainerd. The Mississippi River marks the southern border but expansion both north and south is possible.

The highway crosses the Oak Ridges Moraine as it passes into the City of Kawartha Lakes. The terrain flattens approaching Lindsay, which the highway bypasses. Between Lindsay and Coboconk, the route is generally straight and crosses through a mix of agricultural lands and forest. After passing through Coboconk, it descends from the flat limestone plateau into the rocky Canadian Shield south of Norland.

The 9-7X was built at GM's Moraine, Ohio assembly plant. The Saab 9-7X is classified as a midsize luxury SUV. When the 2005 Saab 9-7X had been introduced, it had served as the replacement for the Oldsmobile Bravada (which was discontinued as a direct result of the Oldsmobile brand being discontinued in 2004), along with the Buick Rainier.

The mountain originally was formed by volcanic ashfall from one of the eruptions of the Yellowstone hotspot. The peak is also partially a glacial moraine formed by a receding glacier that came south out of the Yellowstone icecap.'Creation of the Teton Landscape' by David D. Love & John C. Reed This same glacier also created neighboring Jackson Lake. View from the summit.

It runs for to Crater Creek, including of trail that passes right by the volcano and Crook Glacier. There is also an unofficial trail that runs up the moraine of Crook Glacier. The northern slopes of Broken Top can be accessed by trailheads north of Tam McArthur Rim, while its southern slopes can be reached by trailheads near Crater Creek.

Moraine State Park is named for the glacial moraines that cover its land. The moraines were formed at the conclusion of the Last glacial period, a time when glaciers covered much of North America. A tongue of the glacier reached into Pennsylvania and, as the ice receded, left deposits of gravel, sand and clay. These created a landscape of gently rolling hills.

Moraine State Park is open year-round, and it stays busy with visitors during the winter months. Pleasant Valley and Sunken Garden Trails are part of a larger network of trails open for cross-country skiing. There are approximately of trails open to snowmobiling. Sledding is a very popular activity on the south shore near the Pleasant View Picnic Area.

Healthy skiing industries have been established in snowbelt regions located near major cities such as Buffalo and Toronto. The Erie/Ontario snowbelt, which extends to the northern slopes of the Allegheny Plateau, has lent the region its nickname: ski country. To the south of Georgian Bay, ski resorts are found on the Niagara Escarpment at Blue Mountain and on the Oro Moraine.

Obsidian debris (talus), Obsidian Dome, California. In geology, debris usually applies to the remains of geological activity including landslides, volcanic explosions, avalanches, mudflows or Glacial lake outburst floods (Jökulhlaups) and moraine, lahars, and lava eruptions. Geological debris sometimes moves in a stream called a debris flow. When it accumulates at the base of hillsides, it can be called "talus" or "scree".

The glacier has a relatively high rate of moraine materials, consisting of "friable phyllites and schistose grauwackes". At the foot of the glacier is a lake that was created by glacier recession. Reports from 1892 and 1934 indicated it had "an anomalously slow lake development". The Douglas River (formerly known as the Twain) begins in the lake at the foot of the glacier.

The force of outflow scoured some of the dolomite bedrock, which can be seen in the gravel bars. The heavy flow of water transported boulders downstream and moved glacial erratics from the tills. The faster flow towards center created a channel, which the modern river still follows. Floodwaters were confined to the inter-moraine channels, which moved it west, then to the south.

Basilica on the Holy Mountain in Głogówko, Poland, is a historic Oratorian, Renaissance basilica minor. The shrine is modelled on the Venetian Santa Maria della Salute. The basilica minor is located on a raised moraine known as Holy Mountain (Święta Góra) near Gostyń, located to its north. In 2008, the basilica minor was entered onto the List of Historic Monuments of Poland.

In July 1981, a sudden ice avalanche caused a Glacial Lake Outburst Flood in the moraine- dammed Zhangzangbu-Cho Lake in the headwaters of the Bhote Koshi. The ensuing debris flow destroyed bridges, and sections of both the Arniko and the Nepal–China highways.Mool, P. K.; Joshi, S. P.; Bajracharya, S. R. (2001). Glacial Lake Outburst Floods and Damage in the Country.

Moraines south of Lake Michigan and southwest of Lake Erie. A composite of three maps (Leverett 1915) (Leverett 1902) (Larsen 1986) and other sources. Colors represent moraines from the same time period of the Wisconsin Glacial epoch. The Packerton Moraine in north-central Indiana has been considered by most persons who have studied it to be a large interlobate moraineDryer; 1892, p.

At the end of the Wisconsin Glacial Episode a glacial moraine blocked the outflow of the Sacandaga River, forming "Glacial Lake Sacandaga". The rising water eventually found an outlet over a small divide at Conklingville. The outlet gradually eroded, draining the lake. The Conklingville dam was proposed to block this outlet, and nearly restore the configuration of the glacial lake.

Måkläppen Måkläppen is a nature reserve that stands out from the Falsterbo peninsula, in south western Sweden. It was created by sandbanks built on top of a moraine core. The Måkläppen nature reserve and nature conservation association was formed in 1899. The appearance of Måkläppen changes as sand builds up and is taken away by ocean currents, wind, storm surge and high tide.

It was first described in 1868 and named for Italian mining engineer and mineralogist Quintino Sella (1827–1884). The type locality is Gébroulaz glacier, Val Thorens, Savoie, Rhône-Alpes, France. At its type locality, sellaite occurred within a bitumen bearing dolomite-anhydrite clasts within a moraine deposit. It has been reported from Bleicherode, Thuringia, Germany, where it occurs in an evaporite deposit.

Drifter Cirque () is a cirque between Mount Schmidtman and Mount Naab at the northeast end of Eastwind Ridge in the Convoy Range of Victoria Land. Iceflow from Eastwind Ridge is insufficient to carry surficial moraine away into Fry Glacier and moraines lie in a tangled eddy. So named by the New Zealand Geographic Board which also considered the name Eddy Cirque.

The surroundings become more forested as the route enters Moraine State Park, where it crosses Lake Arthur. A short distance north of the lake, PA 528 continues into Brady Township and runs through more of the state park. The route passes northeast through forested areas of the Jennings Environmental Education Center prior to reaching its northern terminus at PA 8.

Don met Phyllis in 1918. While on a mountaineering trip an incident occurred which, in Don's words, "lends itself readily to being given a romantic aspect."Munday p 1 Don lost his footing on a glacial moraine, and was in danger of slipping into a crevasse. Phyllis jumped to help him restore his balance, and in so doing lost hers.

Puppy Dome is south of Lembert Dome, and southwest of Moraine Flat. Puppy Dome is across from Lembert Dome. By standards in Tuolumne, Puppy Dome is of the smallest domes in Yosemite National Park, next to much larger Lembert Dome. Most are so awe-struck by the area's huge formations that they walk by without realizing it is only away.

King (2016 population 24,512) is a township in York Region north of Toronto, within the Greater Toronto Area in Ontario, Canada. The rolling hills of the Oak Ridges Moraine are the most prominent visible geographical feature of King. The Holland Marsh, considered to be Ontario's "vegetable basket", straddles King Township and Bradford West Gwillimbury. King is known for its horse and cattle farms.

Sefströmbreen is a glacier in James I Land at Spitsbergen, Svalbard. It is debouching into Ekmanfjorden at the northern side of Isfjorden. The glacier is named after Nils Gabriel Sefström. During a surge in 1896 the glacier deposited large moraine ridges in the inner part of the fjord, and these can be seen at the islands of Coraholmen and Flintholmen.

Selby in Troublesome, Colorado Mark Otis Selby (September 2, 1961 – September 18, 2017) was an American blues rock singer-songwriter, guitarist, multi- instrumentalist, and record producer. Born in Enid, Oklahoma,Maher, Dianna. Mark Selby Biography, Nashville: Moraine Music Group, 2006. he was a solo artist, signed to ZYX Records in Europe, and one half of performing duo with his wife, songwriter Tia Sillers.

Sundrud then played some of his own songs for producer Maher and his daughter, Dianna, who ran Maher's publishing company, Moraine Music. They liked the songs and signed Sundrud to their publishing company as a songwriter. Maher and the band then recorded more tracks of Sundrud’s material, with Sundrud on lead vocals. The band showcased for RCA, and they passed.

Glacial Lake Cape Cod was a glacial lake that formed during the late Pleistocene epoch inside modern Cape Cod Bay. After the Laurentide Ice Sheet retreated, glacial ice melt accumulated at the terminal moraine and blocked up the escape of glacial meltwater, creating the lake. Drainage from the lake occurred at Bass River, the location of the Cape Cod Canal and Orleans Harbor.

The glacier produces a sound that often has steep, near vertical sides that extend deep under water. The sea floor is often flat and deeper at the landward end than the seaward end, due to glacial moraine deposits. This type of sound is more properly termed a fjord (or fiord). The sounds in Fiordland, New Zealand, have been formed this way.

Some notably hilly terrain (Ringland Hills) lies within the parish to the east of the village and north of the Wensum. The hills are thought to be a glacial terminal moraine, much the same as Cromer ridge. The soil here is extremely sandy and full of smooth flint pebbles. Painter Alfred Munnings produced a work entitled Ponies on Ringland Hills.

The Kaiser is part of the Northern Limestone Alps and consists mainly of Wetterstein limestone and dolomite. The Wetterstein limestone has a maximum thickness of about 1000 m, which corresponds to the maximum height of the rock faces (Felsabbrüche) of the Kaiser. The younger dolomites are mainly found in the valley hollows. Extensive moraine fields are a remnant of the Würm glaciation.

Being near the city Zurich, the area is a known recreation area. The area alongside Lake Zürich had been formed as the left moraine of the Ice Age glacier, the bed of which is now the Lake Zürich and the valley of the Sihl river. The soil is mostly a conglomerate of gravel, some of it large, and glacial loess.

Under the care of the Swiss guide, Christian Kaufmann, she made the ascent by a different route, and the two parties met upon the summit." “Report of the Chief Mountaineer. Report Camp Yoho.” Canadian Alpine Journal 1 (1907), p. 175. and, on July 21, they were the first to stand on "the summit of Peak Seven (Shagowa; 3,245 m) above Alberta’s Moraine Lake . . . .

His positions include Local Chairman of the Chicago Lung Association and former Chairman of the Burbank Chamber of Commerce. Currently, Viverito is an associate member for the Crisis Center of South Suburbia for Abused Women, a life member of the Veterans of Foreign Wars, a member of the American Legion and a former member of the Moraine Valley Community College Economic Development Board.

Muddy Creek Township is located along the western border of Butler County, with Lawrence County to the west. Muddy Creek, a tributary of Slippery Rock Creek, forms the northern boundary of the township. The creek is impounded in the township to form Lake Arthur, surrounded by Moraine State Park. The township surrounds the borough of Portersville but is separate from it.

Slippery Rock Creek flows through the northern corner of the township, and Muddy Creek forms the township's southern boundary. The creek is impounded to form Lake Arthur, which is surrounded by Moraine State Park, a recreational area. According to the United States Census Bureau, the township has a total area of , of which is land and , or 3.89%, is water.

The confluence of flow through Glacial Lakes Drumheller, Gleichen and Lethbridge utilized Etzikom Coulee to enter the Missouri Drainage System. When Etzikom Coulee was abandoned at 915m (the height of the Lethbridge Moraine Divide) discharge from the lakes was entirely within Alberta. Glacial Lake Drumheller abandoned the Strathmore Channel at 945m, whereupon discharge was directed through the smaller Crowfoot channel until 915m.

Romer Lake is famous for its impressive Elephant Foot Glacier, a wide piedmont glacier with a strikingly-shaped wide terminal lobe flowing into the lake from the SE in its central part.GoogleEarthElephant Foot Glacier - Amusing Planet View of the Elephant Foot end moraine at Romer Lake. NASA picture of the southern part of Romer Lake with the Elephant Foot Glacier.

Druid Lake is a kettle lake located in the town of Erin, Wisconsin, Washington County, Wisconsin near Hartford, Wisconsin. Druid Lake is a natural glacial- formed lake. Druid Lake is surrounded by rugged mixed woods and glacial drumlins in the Southern Savannah Region of southeastern Wisconsin's Kettle Moraine area about 25 miles northwest of Milwaukee. The lake has a maximum depth of .

A Geologic Tour of the Baraboo Ranges and Devil's Lake Gorge Another moraine was deposited at the north end of the lake. The river eventually found a new course to the east of the Baraboo Hills, where the glacier had been, leaving a portion of the river gorge between the moraines filled with water. This body of water is Devil's Lake.

Jotabeche does not currently display any perennial snow, only during summer is snow observed in the area. Likewise, rock glaciers are only found as fossil remnants. However, moraines are found at Jotabeche, and glaciers advanced north from a cirque on its northern flank into the Laguna de Negro Francisco, where a peninsula marks the position of the most extensive moraine.

Since then, the original lineup of the group (augmented by Stuart Carter) have played live a few times in London and Poland. More live work is planned to promote the reissue of 1996's 'Moraine' album on Fourth Dimension Records in late 2017. This reissue also features new recordings based on the original two lengthy songs constituting the first LP.

Black Rapids Roadhouse is across the Delta River from the Black Rapids Glacier. For three months in 1937 the Black Rapids Glacier made national news by advancing across the valley at the rate of a mile a month-it was known as the "galloping glacier." The long glacier has since retreated, but the moraine can still be seen from Richardson Highway pullout.

Through the town flows the Hennigbach, into which empties the Gigginger Bach southwest of Markt Schwaben. The River Sempt flows by to the east. The highest point in town is in the Wittelsbacher Höhe (heights) on the town's southern outskirts, which forms part of an alpine terminal moraine. Also in the south is the sport centre with its bathing pond.

Askham Bog formed within the Vale of York in a hollow which became flooded with melt-water from the last glacial melt about 15,000 years ago. Two ridges of terminal moraine had formed on both sides of the hollow and contained the glacial melt-water between and behind them.Fitter AH, Smith CJ. 1979. A Wood in Ascam, a Study in Wetland Conservation.

Phyllis met her future husband in 1918. While on a mountaineering trip an incident occurred which, in Don's words, "lends itself readily to being given a romantic aspect."Munday p 1 Don lost his footing on a glacial moraine, and was in danger of slipping into a crevasse. Phyllis jumped to help him restore his balance, and in so doing lost hers.

Lake Pukaki, looking towards Mount Cook, in summer Lake Pukaki is the largest of three roughly parallel alpine lakes running north–south along the northern edge of the Mackenzie Basin on New Zealand's South Island. The others are Lakes Tekapo and Ohau. All three lakes were formed when the terminal moraines of receding glaciers blocked their respective valleys, forming moraine-dammed lakes.

Cliffs at Gedser Odde, Falster Gedser Odde on the island of Falster in the Baltic Sea is Denmark's southernmost point. The terminal moraine from Idestrup through Skelby to Gedser is part of the maximum glaciation line across Falster, from Orehoved to Gedser. Fronted by low cliffs, the ridge, high, continues underwater a further south-east to Gedser Rev."Gedser Odde", Den Store Danske.

Stony Creek Lake is a man-made lake built by damming Stony Creek, a tributary of the Clinton River. Stony Creek drains 72 square miles (116 km²) of northern Oakland County and the lake formed from the dams covers . Stony Creek Metropark is situated on a moraine which makes for varied landscape. The park has forests, hills, prairies, as well as swamps.

The Kettle Moraine High School campus contains three charter schools in addition to the regular school, nicknamed "Legacy". Charter school students may participate in any extracurricular activities, including sports, open to Legacy students. KM Global, founded in 2011, uses seminars, field trips, and internships to teach a global perspective and leadership. Global blends elements of traditional high school with that of cyber schools.

Ottersberg lies on a sandy ridge, part of a glacial moraine in the valley of the Wümme. In winter the lowland areas are often under water for weeks at a time and form a valuable bird sanctuary of international importance. It lies on the A 1 road between Bremen and Hamburg. The Bremen - Hamburg railway line originally passed south the village.

Only the western moraine hills are inhabited. The eastern part, called "Ørkenen" (The Desert) is treeless; the government has protected the area and permits no building there. The desert has never been ploughed. For this reason the original stone age topography from when the glaciation ceased, at the end of the last ice age 10,000 years ago, is still visible in many places.

Mount Temple in winter Mount Temple is a mountain in Banff National Park of the Canadian Rockies of Alberta, Canada. Mt. Temple is located in the Bow River Valley between Paradise Creek and Moraine Creek and is the highest peak in the Lake Louise area. The peak dominates the western landscape along the Trans-Canada Highway from Castle Junction to Lake Louise.

The starting point is in Saint-Jacques (1,680 metres a.s.l.), a hamlet in Ayas. The participants pass Verraz (2,380 metres a.s.l.), Saint-Oyen, and then the Blue Lake (), then they take back the main track and meet to the moraine of the Grand Glacier of Verraz (, ) to reach the Refuge Ottorino Mezzalama, which is the turning point of the circuit.

The Volkovysk archaeological complex includes three heights: "the Swedish mountain" (picture), Zamchishche, and Muravelnik. "The Swedish mountain" is located in a southeast suburb of modern Volkovysk. There is a legend that during The Deluge, "the Swedish mountain" was created by Swedish soldiers above the tomb of their commander. It is the highest point among associates Volkovysk of hills a moraine of a ridge.

The glaciers deposited the eroded spoil as moraines. There are several types of moraine on the corrie floor, including lateral boulder moraines, fluted moraines below the corrie lip, and hummocky moraines. The presence of these moraines has led the Fee Burn to take a highly meandering path through the lower corrie.The Story of Corrie Fee National Nature Reserve. p. 9.

The hamlets and isolated farms that make up the valley lie some distance above the frost-prone valley floor. The glacial features in the Menzenschwand valley are even more striking. The Menzenschwander Kluse is a well-known terminal moraine. Below the Kluse, the Menzenschwand Alb plunges with several waterfalls through a small ravine to a basin created by the former Krunkelbach valley glacier.

Norsminde Fjord is an East Jutland Fjord, a glacial moraine valley, created during the Weichselian glaciation c. 20,000 to 70,000 years ago. The stream Rævs Å flows into the fjord and over time it has suffered silting and become increasingly shallow. In 1832 the southern part of the Fjord was drained and made into farmland or wet meadows for animal grazing.

A jökulhlaup is a glacial outburst flood. Jökulhlaup is an Icelandic word, and in Iceland many glacial outburst floods are triggered by sub-glacial volcanic eruptions. (Iceland sits atop the Mid-Atlantic Ridge, which is formed by a chain of mostly submarine volcanoes). Elsewhere, a more common cause of jökulhlaups is the breaching of ice-dammed or moraine-dammed lakes.

The relief of the Kashubian Lake District was caused by several factors: the Scandinavian ice sheet, and river-glacial forms, causing U-shaped valleys. This has caused the region to be labelled a glacial region. Another factor contributing to the relief of the land is the accumulated erosion caused by the rivers. The moraine uplands dominate the landscape of the mesoregion.

The surficial geology in the vicinity of West Branch Little Muncy Creek includes alluvium, bedrock, fill, Wisconsinan and Reworked Illinoian Till, Wisconsinan Till, Wisconsinan Flow-Till, Wisconsinan Till Moraine, and Boulder Colluvium. The creek designated as a Coldwater Fishery and a Migratory Fishery and is being considered for addition to the wild trout waters list of the Pennsylvania Fish and Boat Commission.

During the last deglaciation of the Weichselian Ice Sheet the South Swedish highlands was a place of ice flow divergence. Deglaciation of southern Sweden was relatively slow with ice margin retreat rates of less than 150 m/yr. The retreat was interrupted multiple times by small glacier advances. These advances led to the formation of a series of end moraine systems.

Maple is located in the Golden Horseshoe of Southern Ontario. To the northeast of is the Oak Ridges Moraine, which supplies a lot of water to the Greater Toronto Area. The west branch of the Don River rises to the northwest and flows 1 km west of Maple. Several creeks are to the east and the Black Creek begins slightly west of Vellore.

To the north is the Regina Lake Plain, which is lower in elevation. The Missouri Coteau from whence the hills arise, is lower than these hills. Between the Alberta and Saskatchewan Plains is the Missouri Coteau, dead ice moraine, a major escarpment, a long meandering ridge of hill country. The area is probably underlain with marine shale of the Bearpaw Formation.

The story of Ashokan begins over 400 million years ago during the Devonian Period. The vastly swollen Esopus Creek struggled to find its present path through Ashokan which was well-blocked by glacial moraine. Winchell's Falls and Cathedral Gorge are relatively recent (past ten-thousand years) features. The newly uncovered till (glacial soil) was rocky and sterile, and much like northern Canada today.

Moscow Upland is the eastern part of the Smolensk-Moscow Upland, located inside the Moscow (Klin-Dmitrov Ridge) and Vladimir (Yuryevo Opole) regions of Russia. Extends from the headwaters of Moscow and to the headwaters of the river Vorya Koloksha. The greatest height - 310 meters Relief - erosion and moraine. The hill is covered with mixed forests (major tree species - pine, birch and aspen).

Lake Villa is located at (42.417546, -88.082360). According to the 2010 census, Lake Villa has a total area of , of which (or 88.5%) is land and (or 11.5%) is water. The village lies in a gently rolling moraine landscape, dominated by lakes of glacial origin. Among these are Cedar Lake, north of the village center, and Deep Lake, to the east.

A total of was declared "wild" along the entire main stem as well as Copper, Bonanza, Hosford, Derwent, Flat-Orthmer, Crescent, and Moraine creeks. The Charley River watershed is forested chiefly with black spruce and white spruce.J.G. Clough et al. 1995 This general locus within the Yukon River catchment is the approximate westernmost limit of the black spruce, Picea mariana.

As war escalated in the 19th century between the westward expanding Cree, middlemen with the Hudson's Bay Company, and the equine-proficient Blackfeet, the hilly moraine country became neutral territory where neither tribe ventured, and the last of the bison herds took refuge.Jenish, D. 1999. Indian fall: the last great days of the Plains Cree and the Blackfoot confederacy. Penguin Books Canada Ltd.

Capensis Chardonnay is produced using grapes from across the Western Cape, including the Fijnbosch vinyard. Yverdon vineyard on Napa's Spring Mountain was purchased by the company in 2013. Jackson Family Wines also acquired Zena Crown Vineyard in Yamhill, Oregon in 2013, and established the Gran Moraine Winery in Yamhill in 2014. It acquired Siduri and Novy Family Wines in 2015.

The largest glaciers are the Zharsai with an exposed length of and an area of , the Grigoriev with a length of and an area of , and the Pal'gov at long with a surface of . They descend from the crest of the main divide, which has an average absolute height of more than . Within the mountains the river is long, the gradient of its longitudinal profile is per kilometer, and the basin area is . In its upper reaches the river flows down a very steep slope (10-15°) over the deposits of a moraine overgrown with some vegetation and forms a deep (as much as 70 m) canyon; then, in front of the terminal vegetation-free moraine of the Pal'gov glacier, its longitudinal profile flattens out abruptly_ Here the river forms numerous branches over an outwash plain.

The delta expanded eastward as the lake shallowed by glacial rebound, eventually exposing the earlier-formed The Pas Moraine between 8200 and 8700 years ago. Morozova, G.S., and Smith, N.D., 1999, Holocene avulsion history of the lower Saskatchewan fluvial system, Cumberland Marshes, Saskatchewan- Manitoba, Canada: in Smith, N.D., and Rogers, J. (eds), Fluvial Sedimentology VI, International Association of Sedimentologists Special Publication 28, p. 231-249. Channel incision of the moraine followed, establishing through-flow of the Saskatchewan River and initiation of the lower delta. Growth of both the upper and lower components of the SRD has continued to the present, but now mostly by expansion of the lower delta into Cedar Lake, a remnant of Glacial Lake Agassiz, and to a lesser extent the delta of the Mossy River at Cumberland Lake north of Cumberland House.

The dam itself can be composed of moraine, glacial till, or a lip of the underlying bedrock. The fluvial cirque or makhtesh, found in karst landscapes, is formed by intermittent river flow cutting through layers of limestone and chalk leaving sheer cliffs. A common feature for all fluvial-erosion cirques is a terrain which includes erosion resistant upper structures overlying materials which are more easily eroded.

Pipecleaner Glacier () is a glacier formed by the coalescence of numerous small alpine glaciers on the east side of Mount Huggins. Together with Glimpse Glacier it joins the Radian Glacier where that stream meets the north arm of Dismal Ridge. Its surface is marked by innumerable bands of moraine reminiscent of pipecleaners. Named by New Zealand Victoria University of Wellington Antarctic Expedition (VUWAE), 1960–61.

Joyeux lies less than from the wildlife park at Villars-les-Dombes and from Lyon in the natural region of the Dombes, a wide extent of middle and upper Pleistocene moraine left near the margin of the Alpine ice sheets. The commune includes some thirty lakes which together represent some 4 square kilometres of water. The land between them is of gravel, sand and clay.

It is about from the St. Mary's and the Auglaize. In Allen County, Indiana the Wayne trace, or old Piqua road follows the crest. The inner slope is gentle, while the outer slope is steep. On the west side of Six Mile Creek gap the moraine is a bold bluff to high to the point where the Wabash and Erie Canal once crossed the St. Mary's.

The good moraine of rock and rubble insulates it from water erosion. As a result, during freezing temperatures that exists all the year, the glacier advances. When the insulation and erosion effect of the hills gets reduced erosion sets in and along with rising temperatures the glaciers start retreating. Another unpredictable phenomenon that is observed in many glaciers in the Glacier Bay is that of calving.

The area around the lake has several walking/hiking trails which are, from time to time, restricted. The trail most commonly taken by tourists is The Rockpile Trail, which is along the actual moraine. The trail is approximately long, with an elevation change of . The view of the lake from the top of the rockpile is one of the most photographed locations in all of Canada.

He dug through the rocks in the slope of the pit and found blue ice about down. The ice contained bubbles and was therefore probably glacial in origin. Over the years, the glacier has been the site of multiple injuries and several fatalities. Emerald Lake is a small proglacial lake which lies at the terminal moraine left behind by the now mostly vanished Timpanogos Glacier.

The drift across the Valparaiso moraine and outwash plains is the result of repetitive ice advances and intervening recessions. This drift and the drift from the previous ice sheets of the Illinoian and Iowan glacial periods are present across northeastern Illinois and northwestern Indiana. The early Wisconsin drift are similar to that of the Valparaiso drift that identification of each period is not currently possible.

WTUE (104.7 FM) is a classic rock formatted radio station with studios in Dayton. The station is owned and operated by iHeartMedia. Its transmitter is located in Moraine and can be heard clearly throughout Southwest Ohio, including nearly all of Greater Cincinnati. 104.7 WTUE can also be heard as far north as Wapakoneta also to the east in places London and over to the west Richmond, Indiana.

He worked for WKYC in Cleveland as a sportscaster from 1977 to 1980. He also later served as president of a management consultant firm in Moraine, Ohio. From 1981 to 1987, he worked as director of player relations for the Browns, and from 2004 to 2010 was senior adviser to the general manager for the team. Warfield is retired and resides in Rancho Mirage, California.

Prouty Glacier is located in the U.S. state of Oregon. The glacier is situated in the Cascade Range at an elevation generally between . Prouty Glacier is on the northeast slopes of South Sister, a dormant stratovolcano. Beyond the current range of the glacier, glacially formed Carver Lake lies to the immediate northeast of Prouty Glacier and is impounded by the old terminal moraine of the glacier.

There are also flood plains along the creek. Near its mouth, it cuts through Montour Ridge, and a basalt-containing section of the Catskill Formation extends to the creek's banks in Hemlock Township. Other rock formations along the banks include the Clinton Formation, the Selena Formation, the Lower Helderburg Formation, and the Hamilton Formation. There is a terminal moraine, which crosses the creek near Benton.

Feather Woman Falls is a waterfall located in Glacier National Park, Montana, US. The falls emerge from the base of a terminal moraine and drop towards the valley below. Altogether there are at least four waterfalls in this series, each originating from a permanent snowfield where a glacier once laid. The waterfall can be reached after a short hike from the Sperry Chalet via the Sperry Trail.

Once this breach in the Marseilles moraine was created, it became the discharged for Lake Chicago . Combined with Lake Wauponsee's waters, the outlet deepened. Lake Kankakee at this time was draining much of the St. Joseph Rivers watershed, which was fed by the Saginaw lobe. The erosion by this quantity of water created many of the features along the Illinois River and the lower Kankakee River.

Smith Nunatak is a nunatak just southeast of Mount Starlight in the Athos Range, Prince Charles Mountains. The nunatak is marked by a moraine which extends 2 nautical miles (3.7 km) north from it. Plotted from ANARE (Australian National Antarctic Research Expeditions) air photos of 1965. Named by Antarctic Names Committee of Australia (ANCA) for J.C. Smith, diesel mechanic at Wilkes Station in 1960.

Norges vassdrags- og energidirektorat (Norwegian Water Resources and Energy Directorate). Accessed 13 June 2015 Such lakes created by glacial action are also called fjord lakes or moraine-dammed lakes. Some of these lakes were salt after the ice age but later cut off from the ocean during the post-glacial rebound. At the end of the ice age Eastern Norway was about lower (the marine limit).

Rogen moraines or ribbed moraines are a type of basal moraines that form a series of ribs perpendicular to the ice flow in an ice sheet. The depressions between the ribs are sometimes filled with water, making the Rogen moraines look like tigerstripes on aerial photographs. Rogen moraines are named after Lake RogenMöller, P., 2006. Rogen moraine: an example of glacial reshaping of preexisting landforms.

Laurel Run is a tributary of West Branch Fishing Creek in Sullivan County, Pennsylvania, in the United States. It is approximately long and flows through Davidson Township. The stream is in the United States Geological Survey quadrangle of Elk Grove. Wisconsinan Flow-Till, Boulder Colluvium, Wisconsinan Till Moraine, alluvium, and alluvial fan occur in the vicinity of the stream, as does bedrock consisting of sandstone and shale.

It is a resedimented till that is texturally a diamict. This glacial till occurs in the upper reaches of the bottom of the stream's valley. Boulder Colluvium occurs in the lower reaches of the valley and contains boulders consisting of quartz, sandstone, and conglomerate. Wisconsinan Till Moraine and a glacial or resedimented till known as the Wisconsinan Till occur in the upper reaches of the stream's watershed.

In southern Wisconsin it encounters the terminal moraine formed during the last ice age, where it forms the Dells of the Wisconsin River. North of Madison at Portage, the river turns to the west, flowing through Wisconsin's hilly Western Upland and joining the Mississippi approximately 3 miles (4.8 km) south of Prairie du Chien. The highest waterfall on the river is Grandfather Falls in Lincoln County.

Wenkchemna Peak is located on the border of Alberta and British Columbia. It was named in 1894 by Samuel E. S. Allen.Wenkchemna Peak Wenkchemna is the 10th peak in The Valley of the Ten Peaks, as they are normally numbered (left to right as seen from Moraine Lake). It is an extension into the valley of the ridge formed by Mount Hungabee and Ringrose Peaks.

Most of the city is heavily wooded, on moraine topography with many slopes and wetlands and three small private lakes – Hornbeam Lake, Horseshoe Lake, and the eponymous Sunfish Lake, which was formerly known as Lake Thereau by the early French settlers of the area. For new construction, the minimum lot size is of buildable land to keep with the city's goal of maintaining a rural atmosphere.

The village is situated on a terminal moraine, stretching along the eastern bank of the Elbe River. It is located about north of the state capital of Magdeburg, halfway between Stendal in the west and Rathenow in the east. Since 1 January 2010 Schönhausen includes the former municipality of Hohengöhren. Schönhausen station is a stop on the Berlin–Lehrte railway line, served by Regionalbahn trains.

Jason Santerre, "Mushroom Cloud over Ashburn," Harrowsmith Country Life (Dec. 1, 2004): 38. In 2011, the Ashburn company received a grant of $3.1 million under Ontario's Rural Economic Development Program (RED), to expand their facilities on the Oak Ridges Moraine, and to support the creation of 80 new jobs.Ministry of Agriculture, Food and Rural Affairs Ontario,New Food Processing Plant Creating Jobs in Durham (July 5, 2011).

This bypass connects Wyrzysk with Piła (37 km) and Bydgoszcz (55 km). The railway station in Osiek nad Notecią also provides a railway connection with Piła (39 km) and Bydgoszcz (48 km). The commune lies in Krajna Plateau. Its southern border is formed by the River Noteć with its tributary, the Łobżonka, which cuts through the picturesque moraine hills rising over the wide valley of the Noteć.

One of these hills, Dębowa Góra, reaches a height of 192 metres above sea level and is the highest elevation of the Krajna Region. Over 60 per cent of the commune is protected as an area of scenic beauty. Conditions favourable for human settlement occurred in the present Wyrzysk Region in the postglacial period. Its relics are now left on the moraine hills along the Noteć River.