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"eastwardly" Definitions
  1. toward or from the east : EASTERLY
"eastwardly" Antonyms

63 Sentences With "eastwardly"

How to use eastwardly in a sentence? Find typical usage patterns (collocations)/phrases/context for "eastwardly" and check conjugation/comparative form for "eastwardly". Mastering all the usages of "eastwardly" from sentence examples published by news publications.

Looking straight into the ocean doesn't usually mean looking in a perfect eastwardly or westwardly direction.
The county is drained by the Watonwan River and its tributaries; the river flows eastwardly through the northern part of the county.
The South English River rises just south of Montezuma in southern Poweshiek County and flows generally eastwardly through extreme northeastern Mahaska County and northern Keokuk County.
The Willis River rises in southern Buckingham County and initially flows eastwardly into Cumberland County, where it turns north-northeastwardly for the remainder of its course. It flows into the James River in northern Cumberland County, about southeast of Columbia.
The East Fork Little Sandy River, long, joins the main stream in Greenup County. It rises in northern Lawrence County and initially flows eastwardly before turning north-northwestwardly through Boyd and Greenup Counties. It flows past the Ashland suburb of Cannonsburg.
According to the United States Census Bureau, the township has a total area of , of which is land and (2.04%) is water. The Shell River flows eastwardly through the township from its source in Shell Lake in the northwestern part of the township.
The Dead Moose River rises in Salo Township of eastern Aitkin County and flows generally eastwardly through Automba, Kalevala and Silver townships of southwestern Carlton County. It joins the Kettle River from the west about northwest of the town of Kettle River.
The Rock River flows for its entire length in Windham County. It rises in the Green Mountain National Forest in the town of Dover and flows generally eastwardly into the town of Newfane, where it joins the West River.DeLorme (1996). Vermont Atlas & Gazetteer.
SR 106 traverses Butler and Crenshaw counties along a two-lane road. As it leads across Butler County, the route travels eastwardly, continuing this trajectory until it crosses into Crenshaw County. After crossing into Crenshaw County, the route turns southeastwardly until it reaches its terminus near Brantley.
SR 3 in rural Lancaster County State Route 3 is a primary state highway in the U.S. state of Virginia that extends from the town of Culpeper south and eastwardly to Gloucester in Virginia's Middle Peninsula region. For many years, a portion was named "Historyland Highway".
The English River flows for much of its course in north and south forks, which join in extreme northwestern Washington County. The English River then flows generally eastwardly for about , past the town of Riverside. It joins the Iowa River in northeastern Washington County, south of Iowa City.
The river in winter near Madelia, Minnesota Garden City Township in 1996 The Watonwan River rises in Amboy Township, approximately southwest of Jeffers in central Cottonwood County, and flows generally eastwardly across flat till plains through northern Watonwan and western Blue Earth counties, past the city of Madelia. It flows into the Blue Earth River approximately southwest of Mankato and upstream of the Blue Earth's confluence with the Minnesota River. The river's largest tributaries are its north and south forks. The South Fork Watonwan River, long, rises in southeastern Cottonwood County and initially flows eastwardly into southern Watonwan County, briefly entering Martin County and passing Odin; then northeastwardly through eastern Watonwan County to its confluence with the Watonwan River upstream of Madelia.
The South Branch, 62 miles (99 km) long, flows northeastwardly through Lincoln County into northwestern Lyon County, past Minneota. Other tributaries of the Yellow Medicine include Spring Creek, 46 miles (74 km) long, which flows eastwardly through Yellow Medicine County; and Mud Creek, 31 miles (50 km) long, which flows eastwardly through western Yellow Medicine County into northwestern Lyon County. The Minnesota Pollution Control Agency statistically combines the watershed of the Yellow Medicine River with that of Hawk Creek on the opposite bank of the Minnesota River, as well as small watersheds of nearby Minnesota River tributaries. According to the agency, 81% of the land in the Yellow Medicine-Hawk Creek watersheds is used for agriculture, with corn and soybeans being the predominant crops.
Wakatomika Creek rises in western Coshocton County and flows westwardly into Knox County; then southwardly into northeastern Licking and southwestern Coshocton Counties; and eastwardly through northwestern Muskingum County, past the southern edge of the village of Frazeysburg. It joins the Muskingum River from the west at the village of Dresden.DeLorme (1991). Ohio Atlas & Gazetteer.
Elm Creek is an U.S. Geological Survey. National Hydrography Dataset high- resolution flowline data. The National Map , accessed October 5, 2012 tributary of the Blue Earth River in southern Minnesota. It rises in northeastern Jackson County and flows eastwardly through Martin County into northeastern Faribault County, where it joins the Blue Earth River near the city of Winnebago.
It rises in Shenandoah National Park and flows generally eastwardly through Rappahannock and Culpeper counties. It joins the Rappahannock River from the west about northwest of Remington. The Hazel's largest tributaries are the Hughes River, which joins it at the border of Rappahannock and Culpeper counties, and the Thornton River, which joins it in Culpeper County.
The Pigg River is a river in south-central Virginia in the United States. It is a tributary of the Roanoke River, which flows to the Atlantic Ocean via Albemarle Sound. The Pigg River rises on Fivemile Mountain in western Franklin County and flows generally eastwardly through Franklin and Pittsylvania Counties, past the town of Rocky Mount.DeLorme (2005).
The region is bound to the north by the Ghouta and Marj plains around Damascus and to the south by the desert steppe of Jordan.Rohmer 2008, p. 1. Its western boundary is marked by the Ruqqad tributary, which separates it from the Golan Heights (al-Jawlān in Arabic). It is eastwardly bound by the al-Hamad and al- Safa desert steppes.
The North English River is the longer of the two forks. It rises just south of Grinnell in western Poweshiek County and flows generally east-southeastwardly through Iowa County, past the town of Guernsey. In Iowa County it collects two minor tributaries, the Deep River and the Middle English River, both of which rise in Poweshiek County and flow eastwardly for short distances.
The National Map, accessed May 26, 2011 and drains an area of .Iowa Department of Natural Resources. Watershed Monitoring and Assessment: North River Via the Des Moines River, it is part of the watershed of the Mississippi River. The North River rises northeast of Casey in southern Guthrie County and flows generally eastwardly through Adair, Madison and Warren counties, past Carlisle, into southeastern Polk County,DeLorme (1998).
SR 168 is aligned along a two-lane road for its duration. From its western origin at Douglas in southeastern Marshall County, the route travels eastwardly as it leads towards Boaz. At Boaz, the route turns northeastwardly, crossing US 431 and leading into DeKalb County. The eastern terminus of the route is at Kilpatrick, an unincorporated community near the border of DeKalb and Marshall Counties.
The Moormans River flows for its entire length in northwestern Albemarle County. It rises in the Blue Ridge Mountains as two streams, its north and south forks, which flow through Shenandoah National Park. Below their confluence in a small reservoir serving Charlottesville, the river flows generally eastwardly. It joins the Mechums River to form the South Fork of the Rivanna River about northwest of Charlottesville.
The Guest River flows for nearly its entire length in Wise County. It rises in the north-central part of the county and flows initially south-southeastwardly to the city of Norton; then eastwardly to the town of Coeburn; then southeastwardly for the remainder of its course. It flows into the Clinch on the common boundary of Wise and Scott Counties. Portions of the river flow through the Jefferson National Forest.
The Wolf River is a U.S. Geological Survey. National Hydrography Dataset high- resolution flowline data. The National Map, accessed March 30, 2011 tributary of the Missouri River in northeastern Kansas in the United States, draining an area of in the Dissected Till Plains region. It rises in Brown County, approximately north of Powhattan, and flows generally eastwardly into Doniphan County, past the communities of Robinson, Leona, and Severance.
According to the Geographic Names Information System, it has also been known historically as "Clear Creek" and as "Clear Fork Mohecan Creek". The Clear Fork rises in northeastern Morrow County and flows generally eastwardly through southern Richland and Ashland Counties, past the towns of Lexington, Bellville and Butler, and through Mohican State Park. It joins the Black Fork to form the Mohican River in Ashland County, about southwest of Loudonville.DeLorme (1991).
Alabama State Route 86, west of Carrollton, Alabama. SR 86 is aligned along a two-lane roadway as it enters Alabama. Just east of the Mississippi state line, the highway crosses the Tom Bevill Lock and Dam and enters the town of Pickensville. The highway travels to the east as it continues across Pickens County, connecting Pickensville with Carrollton and Gordo, where it intersects US 82, which leads eastwardly to Tuscaloosa.
SR 89 travels through the heart of Alabama's Black Belt, recognized as one of the poorer areas of the state. The highway serves as an extension of the northbound leg of SR 21, which turns eastwardly in eastern Wilcox County. The path of SR 89 travels through rural areas and does not traverse any incorporated communities. The northern terminus of the highway is in Dallas County at Elm Bluff.
The Chikaskia River begins as an intermittent stream in southwestern Pratt County, Kansas and initially flows eastwardly into Kingman County, where it turns southeastward for the remainder of its course through Harper and Sumner counties in Kansas and Grant and Kay counties in Oklahoma. In Kay County the river flows past the town of Blackwell and flows into the Salt Fork southeast of Tonkawa.DeLorme (2003). Kansas Atlas & Gazetteer.
The Appoquinimink River is a river flowing to Delaware Bay in northern Delaware in the United States. The river is long and drains an area of on the Atlantic Coastal Plain. The Appoquinimink flows for its entire length in southern New Castle County. It rises approximately west of Townsend and flows generally eastwardly, south of Middletown and past Odessa, to its mouth at the northern end of Delaware Bay, approximately east of Odessa.
The Ottauquechee rises in the Green Mountains in eastern Rutland County in the town of Killington, and flows generally eastwardly into Windsor County, where it passes through or along the boundaries of the towns of Bridgewater, Woodstock, Pomfret, Hartford and Hartland; and the villages of Woodstock and Quechee. It joins the Connecticut River in the town of Hartland, about 4 miles (6 km) south- southwest of White River Junction.DeLorme (1996). Vermont Atlas & Gazetteer.
Namu-Myo-Ho-Ren-Ge-Kyo in village Kam'yanka, Lutuhyne Raion, Luhansk Oblast. Junsei Terasawa (2005) in Japan The northern outskirts of the village adjoin a chalk mountain slope named Zmiyina. Eastwardly of the Ancient Mound () on it a Peace Pagoda () or Stupa is being built by the international sect of Buddhist monks Nipponzan Myohoji. The Stupa is being financed by donations and voluntary labor, following many years labor by all the monks of the sect.
The Banister River is a tributary of the Dan River, about 65 mi (105 km) long, in southern Virginia in the United States. Via the Dan, it is part of the watershed of the Roanoke River, which flows to the Atlantic Ocean. It rises on Brier Mountain in western Pittsylvania County and flows generally eastwardly into Halifax County, past the town of Halifax. It joins the Dan River 6 mi (9.7 km) east of the town of South Boston.
From Milton, the Broadkill River flows generally eastwardly, passing through wetlands and salt marshes in the Prime Hook National Wildlife Refuge. After approaching to within of Delaware Bay, the river parallels the shoreline a short distance inland for approximately before flowing into the bay, approximately northwest of Lewes. The United States Coast Guard maintains a station near the mouth of the Broadkill. The mouth is connected to Rehoboth Bay by the Lewes and Rehoboth Canal, which forms part of the Atlantic Intracoastal Waterway.
M. breweri can only be found on Muskeget Island, off the west coast of Nantucket, Massachusetts, United States. However, throughout the history of Muskeget Island, it might also have appeared on nearby South Point and Adams Islands, which are considered as a part of Muskeget Island in a rather broad point of view. Moreover, the island has moved about 1,000 feet eastwardly over the last about 200 years, along with its changing process of shape, size and position due erosion and tidal buildup.
At a point of today's 210 Freeway, there was a fork in the road that veered obliquely to the northwest. This was an access to the greatest local water source in Millard Canyon, and was named New Fair Oaks Road. Eventually this road was renamed Lincoln Avenue and Old Fair Oaks Road just became Fair Oaks Avenue. Long considered the center of town, the corner of Colorado and Fair Oaks lost its centrality by the ever eastwardly expansion of the city.
Yarmouth, Maine: DeLorme. In the town of Bradford, it collects a short stream known as the South Branch Waits River, which flows eastwardly from Corinth. Further upstream, just south of the village of East Corinth, the Waits collects another tributary known as the Tabor Branch Waits River. The Tabor rises in the northwestern section of the Town of Topsham in an area known as "The Territory" as two smaller branches and flows southeasterly to the village of East Topsham, then southerly toward and through East Corinth.
However, the commissioners were unable to agree on where the border should go upon exiting the channel between St. Joseph and St. Tammany. This question would wait another 20 years until the 1842 Webster–Ashburton Treaty finally established the boundary "along the ship channel between Saint Joseph and St. Tammany Islands, to the division of the channel at or near the head of St. Joseph's Island [sic]; thence, turning eastwardly and northwardly, around the lower end of SE George's or Sugar Island" so as to assign Sugar Island to the United States.
The Heart River rises in the prairie country of Billings County, in the Little Missouri National Grassland near the south unit of Theodore Roosevelt National Park. It flows generally eastwardly through Stark County to Gladstone, past Belfield and South Heart, through the Patterson Reservoir and past Dickinson. It is joined by the Green River at Gladstone, and turns east-southeastward into Grant County, passing through Lake Tschida, which is formed by the Heart Butte Dam. Below this dam, the river turns northeastward into Morton County, where it joins the Missouri River at Mandan.
In part because of the problems created by collectivisation, agriculture was largely de-collectivised in Poland in 1957. The fact that Poland nevertheless managed to carry out large-scale centrally planned industrialisation with no more difficulty than its collectivised Eastern Bloc neighbours further called into question the need for collectivisation in such planned economies. Only Poland's "western territories", those eastwardly adjacent to the Oder-Neisse line that were annexed from Germany, were substantially collectivised, largely in order to settle large numbers of Poles on good farmland which had been taken from German farmers.
The Obed River flows eastwardly from Cumberland County through a scenic gorge before emptying into the Emory just west of Wartburg. Wartburg is situated around the junction of U.S. Route 27, which connects the city to Kentucky to the north and Harriman and Interstate 40 to the south, and State Route 62, which connects Wartburg to Oak Ridge to the east and the rural areas of Morgan County and Fentress County to the west. According to the United States Census Bureau, the city has a total area of , all of it land.
The Kettle River, also known as Kettle Creek, is a tributary of the Blueberry River, 17 miles (28 km) long, in north-central Minnesota in the United States. Via the Blueberry, Shell, and Crow Wing Rivers, it is part of the watershed of the Mississippi River, draining a rural area. The Blueberry River rises approximately one mile (2 km) south of Wolf Lake in Spruce Grove Township in southeastern Becker County and flows generally eastwardly through Runeberg Township into northwestern Wadena County. It flows into the Blueberry River in Blueberry Township, approximately two miles (3 km) west of Menahga.
The thickly forested hills and plateaus of the Ardennes are more rugged and rocky with caves and small gorges. Extending westward into France, this area is eastwardly connected to the Eifel in Germany by the High Fens plateau, on which the Signal de Botrange forms the country's highest point at . The Meuse river between Dinant and Hastière High Fens landscape near the German border The climate is maritime temperate with significant precipitation in all seasons (Köppen climate classification: Cfb), like most of northwest Europe. (direct: Final Revised Paper ) The average temperature is lowest in January at and highest in July at .
Late in 1928 Colonial extended westwardly from Syracuse to Rochester, then early in 1929 eastwardly from Albany to Boston (in Massachusetts) and westwardly again from Rochester to Buffalo. In 1928 Colonial began acquiring the intrastate rights between Syracuse and Buffalo, by buying existing firms; that process continued until 1930, after it had become a member of the Greyhound family. In 1929 the Motor Transit Corporation (MTC) bought the Colonial Motor Coach Corporation, and (in a separate transaction) the MTC became renamed as The Greyhound Corporation. Colonial became renamed as the Eastern Greyhound Lines (EGL) of New York.
The North Fork Watonwan River, long, rises in Cottonwood County and flows eastwardly into northern Watonwan County, joining the Watonwan River about a mile (2 km) southeast of La Salle. Approximately 84% of the larger watershed of the Blue Earth River, which includes that of the Watonwan River, is used for agricultural cultivation, primarily that of corn and soybeans. Small lakes and wetlands in the Watonwan watershed provide significant habitat for Minnesota's waterfowl population, though many stretches of the river and its tributaries have been subject to ditching and channelization for agricultural production and localized flood reduction.
The Wild Rice River near Abercrombie in 2007 The Wild Rice River rises as an intermittent stream in Brampton Township in southeastern Sargent County, approximately south of Cogswell. It initially flows generally eastwardly in a winding course through Sargent and Richland counties, through the Tewaukon National Wildlife Refuge and past the towns of Cayuga, Mantador and Great Bend. Past Great Bend, the river turns northward; from west of the city of Wahpeton it generally parallels the Red River in a winding channel at a distance of approximately . It flows into the Red River in southeastern Cass County, approximately southeast of Frontier and south of Fargo.
The Mullet River is a tributary of the Sheboygan River, 40 miles (64 km) long, in eastern Wisconsin in the United States. Via the Sheboygan, it is part of the watershed of Lake Michigan, draining an area of 88 square miles (228 km²) in a primarily agricultural area of the Eastern Ridges and Lowlands region of Wisconsin. The Mullet River issues from Mullet Lake in the town of Forest in eastern Fond du Lac County and flows generally eastwardly into Sheboygan County, passing through the village of Glenbeulah and the city of Plymouth. It joins the Sheboygan River from the south in the city of Sheboygan Falls.
The river's north and south forks each rise in South Dakota on the Coteau des Prairies, a morainic plateau dividing the Mississippi and Missouri River watersheds, and flow across till plainsWatersheds of the Minnesota River Basin. into Minnesota. The north fork issues from Round Lake near South Shore in northeastern Codington County, South Dakota, and flows eastwardly for through central Grant County into northwestern Lac qui Parle County, Minnesota. The south fork rises in northwestern Deuel County, South Dakota, approximately six miles (10 km) southwest of Strandburg, and flows generally northeastwardly for through southern Grant County and western Lac qui Parle County, passing near the community of Nassau, Minnesota.
The headwaters of the Long Prairie River are in a region of numerous lakes north of Alexandria. It issues from Lake Carlos in Carlos Township in Douglas County, just south of Lake Carlos State Park and approximately north-northeast of Alexandria. Tributaries to Lake Carlos, which drain several lakes including Lake Darling, Lake Ida, Lake Miltona, and Geneva Lake, account for approximately a quarter of the Long Prairie River's watershed. The river initially flows eastwardly into Todd County; ditches in its upper course connect the river to Lake Osakis, which is the source of the Sauk River, thereby joining the two rivers' watersheds during periods of high water.
SR 160 begins as a primary highway at an intersection with US 11E/SR 34 (W Andrew Johnson Highway)in a concurrency with SR 342 in Morristown, heading southeastward as a 4-lane divided highway, serving essentially as a southern bypass of Morristown. SR 342 (Alpha Valley Home Road) exits after SR 160 curves more eastwardly, and has an intersection with SR 474 (Merchants Greene Boulevard) shortly afterwards. The highway then has a short concurrency with SR 66. SR 160 continues east to have an interchange with SR 343 (S Cumberland Street) before coming to an interchange with US 25E/SR 32 (S Davy Crockett Parkway; Exit 1 on US 25E).
SR 536 became SR 190 in the 1933 renumbering, and in October 1933 it was extended another , taking it across the North Landing River to SR 615.: "1. Be it enacted by the General Assembly of Virginia, That the location of route number one hundred and ninety of the State highway system, formerly route number five hundred and thirty-six in Princess Anne county, shall be southwardly from the Norfolk county line to a point near Blackwater river, and thence eastwardly across North Landing river to connect with Munden Point road." SR 190 was downgraded to secondary SR 726 in 1952, effective once the new Pungo Ferry Bridge (which replaced Pungo Ferry) was complete, which happened in 1954.
The Cottonwood River flows generally eastwardly throughout its course. It rises southwest of Balaton in Rock Lake Township in southern Lyon County, as an intermittent stream on the Coteau des Prairies, a morainic plateau dividing the Mississippi and Missouri River watersheds. The river flows off the Coteau in a wooded valley in southeastern Lyon County, dropping 200 feet (60 m) in five miles (3 km), and enters a region of till plains, flowing through southern Redwood County, the northeastern corner of Cottonwood County, and northern Brown County, past the communities of Sanborn and Springfield. It enters a wooded valley near its mouth, flowing through Flandrau State Park and entering the Minnesota River just southeast of New Ulm.
Pauper’s Drain is a small tributary of the River Trent in North Lincolnshire, England, and is 9 km (6 miles) long. It has a catchment area of 42 square kilometres(16 square miles) of flat arable, agricultural land to the east of the Isle of Axholme. The start of the drain is the outflow of the Crowle sewage treatment works; from there it flows in an eastwardly direction, south of the village of Eastoft before it reaches the Paupers pumping station at the side of the tidal River Trent, to the north of Amcotts. The station contains three pumps, which are used to maintain water levels in the drain by discharging water into the Trent as required.
By the beginning of the 19th century large parts of the parish were still little more than a morass, and the risk of flood was a constant one: in June 1816, for example, the parish was once again completely deluged following a period of heavy rain that caused several local rivers to overflow their banks.The Monthly Magazine, or British Register (Volume 41, Pt. 1 for 1816). (1816). p.473. Critical to controlling events like this was the establishment of the Catchwater Drain. Plans for making the drain were implemented in 1805, an intention being announced to cut and embank ‘the intended Catch-water Drain from or near to Skellingthorpe Wood, in the parish of Skellingthorpe, through the said parish, in an Eastwardly direction’.
The river was formerly dammed to form a lake in the state park, but the dam was not rebuilt after being washed out by floods in 1965 and 1969. Due to the northeastward slope of the Coteau des Prairies and the presence of a terminal moraine along the northern side of the river, very few tributaries enter the Cottonwood River from the north. The largest is Sleepy Eye Creek, 51 miles (82 km) long, which flows eastwardly through Redwood and Brown Counties, past Cobden. Tributaries from the south include Plum Creek, 35 miles (56 km) long, which flows northeastwardly through Murray and Redwood Counties, past Walnut Grove; and Dutch Charley Creek, 46 miles (74 km) long, which flows northeastwardly through Murray, Cottonwood, and Redwood Counties.
National Hydrography Dataset high- resolution flowline data. The National Map , accessed October 5, 2012 rises on the coteau in eastern Deuel County, South Dakota, and flows initially northeastwardly as an intermittent stream, past Gary, South Dakota, then eastwardly through Lac qui Parle County, past Dawson. Other tributaries include two small trout streams: Canby Creek, 24 miles (39 km) long, which flows northeastwardly on the Coteau in western Yellow Medicine County, through Canby; and Tenmile Creek, 33 miles (53 km) long, which flows eastward and northwardy through Lac qui Parle County, through Boyd. According to the Minnesota Pollution Control Agency, of the of the river's watershed in Minnesota, 79% of the land is used for agricultural cultivation, primarily corn and soybeans.
Admiral William Halsey Jr., which had already led the Third Fleet into the deadly Typhoon Cobra in December 1944, now managed to lead the Third Fleet yet again into the eyewall of another deadly storm, ignoring reports by Rear Admiral Beary, who was convinced that Halsey's eastwardly course would put his carriers into the storm. By the time this had become evident, the replenishment carriers had already found themselves navigating independently of each other. As Windham Bay neared the center of the storm, at around 3:00, her crew began to witness the aircraft stored upon the flight deck work free of their restraints and slip into the sea. F4U-2 Corsairs of Marine Night Fighting Squadron 523 (VMF(N)-532) photographed being transported on the flight deck of Windham Bay, 12 July 1945.
The Salt Fork near Alva, Oklahoma The Salt Fork rises in Comanche County, Kansas, and flows initially southeastwardly through Barber County, Kansas, and Woods County, Oklahoma, to the town of Alva, where it turns eastwardly for the remainder of its course through Alfalfa, Grant, Kay and Noble counties in Oklahoma, past the towns of Pond Creek, Lamont and Tonkawa. It flows into the Arkansas River in southern Kay County, south of Ponca City. In Alfalfa County, a dam on the river impounds Great Salt Plains Lake, which is lined with salt flats and is the site of Salt Plains National Wildlife Refuge and a state park. The Salt Fork's largest tributaries are the Medicine Lodge River, which joins it in Alfalfa County, and the Chikaskia River, which joins it in Kay County.
The Shell River issues from Shell Lake approximately southwest of Pine Point in Carsonville Township in eastern Becker County, and initially flows southeastwardly through the Smoky Hills State Forest into southwestern Hubbard County and northwestern Wadena County, to Blueberry Lake, which collects the Blueberry River. From Blueberry Lake, the Shell River flows eastwardly in a winding course through northern Wadena and southern Hubbard counties, passing through Huntersville State Forest and collecting the Fish Hook River from the north. It flows into the Crow Wing River in Crow Wing Lake Township in Hubbard County. The Shell River is the Crow Wing River's first significant tributary, and is substantially the larger of the two at their confluence; the Shell's average discharge of 250 cubic feet per second (7 m³/s) is approximately three times the Crow Wing's discharge above the confluence.
The headwaters of the Redwood River are in Aetna Township in northeastern Pipestone County, approximately four miles (6 km) west of Ruthton, on the Coteau des Prairies, a morainic plateau dividing the Mississippi and Missouri River watersheds. It flows initially eastwardly as an intermittent stream, through Ruthton and into northwestern Murray County, then northwardly into Lyon County, where it turns northeastward and flows through Russell, Lynd, and Marshall. Between Russell and Marshall, the river flows off the Coteau in a wooded valley, dropping 300 feet (90 m) in 15 miles (24 km); Camden State Park is located along this stretch of the river. Downstream of Marshall, the Redwood flows through a flat till plain and turns eastward into Redwood County, passing Vesta and Seaforth; sections of the river in this stretch have been straightened to form agricultural ditches.
A satellite image of the Kaziranga area showing the shifting waters of the Brahmaputra Asian elephants grazing Per the plate tectonics, Assam is in the easternmost projection of the Indian Plate, where it is thrusting underneath the Eurasian Plate creating a subduction zone. It is postulated that due to the northeasterly movement of the Indian plate, the sediment layers of an ancient geosyncline called Tethys (in between Indian and Eurasian Plates) have been pushed upward to form the Himalayas mountain range. Karbi Anglong plateau, which is situated to the south of the Kaziranga (along with the Khasi and Garo Hills) is originally part of the South Indian Plateau system. It is believed that due to the force exerted by the north-eastwardly movement of the Indian plate at the time of the Himalayan origin, a huge fault was created between the Rajmahal hills and the Karbi-Meghalaya plateau.
Tributaries of the river in its upper course include the East Branch Blue Earth River, long, which rises in southwestern Freeborn County and flows westwardly through Faribault County to the city of Blue Earth; and Elm Creek, long, which rises in northeastern Jackson County and flows eastwardly through Martin County into northeastern Faribault County, where it joins the Blue Earth River near Winnebago. The Blue Earth River flows in most of its course through till plains and the plain of a former glacial lake. The drain of the glacial lake, Union Slough, drains in two directions, south into the East Fork of the Des Moines River and north, as Union Slough, into the West Branch of the Blue Earth River. The lower (northern) part of the river's watershed was historically covered by the Big Woods, a tract of hardwoods that has since been largely converted to agricultural use; segments of the woodland extended southward along the riparian corridors of the Blue Earth River and its tributaries.
Port Hopetoun was a basin between Semple Street and Lothian Road, and Morrison Street and Fountainbridge. However, the final mile has been filled in and the Edinburgh terminal is now at Lochrin Basin in Tollcross, adjacent to Fountainbridge. The canal has several navigable aqueducts, including the Slateford Aqueduct that takes the canal over the Water of Leith in Edinburgh, the Almond Aqueduct near Ratho and the Avon Aqueduct near Linlithgow, the second-longest in the United Kingdom. Priestley describes the route and structures in some detail: > [The] Canal commences from the sixteenth lock of the Forth and Clyde > Navigation, about two miles west of Falkirk, in the county of Sterling , > whence it takes an eastwardly course on the south side of the above- > mentioned town, by some collieries; thence, through Black Hill Tunnel, and > across the Glen Water, on which stream, at a short distance to the > southward, is constructed a considerable reservoir.
Priestley, writing in 1828,Joseph Priestley, A Historical Account of the Navigable Rivers, Canals, and Railways, of Great Britain, Longman, Rees, Orme, Brown & Green, London, 1831, accessible at described it: > This railway commences on the south side of the city of Edinburgh, near > Salisbury Craigs, [sic] from whence it proceeds in an eastwardly direction, > skirting the King's Park; thence, on the south side of Duddingston House, > and by the village of Hunters Hall, to Redrow, where it communicates with > the Edmonstone Railway. It afterwards takes a southerly course by Miller > Hill Row, to within half a mile of the west side of the town of Dalkeith, > where it crosses the North Esk River; thence, to the banks of South Esk > River, at Dalhousie Mains, near Newbattle Abbey, from whence, the last act > [i.e. a second Act of Parliament] enables the company to extend it to Newton > Grange. There is a branch from Wanton Walls to Fisher Row Harbour, on the > Firth of Forth; another from Cairney to the collieries situate on the east > side of the Esk, at Cowpits, near Musselburgh ; and another by a subsequent > act, which extends to Leith Harbour.

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