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567 Sentences With "flows over"

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

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Electricity flows over the northern and southern U.S. borders in both directions.
At that temperature, when natural gas mixed with steam flows over one surface of the cell while oxygen flows over the other, a reaction results in the release of electricity, steam that is recycled through the process and carbon dioxide.
But his determination as an entrepreneur flows over into his belief in Puerto Rico.
The salmon-colored areas show lava flows over the Big Island since May 3, 2018.
If pollution flows over ground and into water, everyone agreed that it should be regulated.
China keeps a tight rein on the amount of money that flows over its borders.
The so-called IRR is an investment's return based on its related cash flows over time.
It flows over and about the outlines of its harmonic riverbed, and freed of any set rhythm.
But they may want to keep a close eye on China's export flows over the coming few months.
Because right now if you have time-based media, even this podcast, it just sort of flows over.
Pressure drops as air flows over the wing and propeller tips, allowing air to expand while dropping in temperature.
The two prevailing theories include eruptions, which spread lava flows over a large area, or overturning waves of lava.
There is no question that a return to equity fund flows over bonds would have a significant market impact.
Investors have noticed: USMV/SPLV show negative money flows over the past week to the tune of $770 million.
With relatively stable operating fundamentals, Fitch believes Trilogy should be able to increase cash flows over the rating horizon.
The company is also studying how water flows over the skin of fish to reduce the drag created during acceleration.
Many people flock to Horsetail Fall, which flows over the famous El Capitan, to get a glimpse of the glow.
In addition, construction and development also affects how water flows over the natural land, which can cause further flooding problems.
London's voice flows over scenes of the actress driving in South Los Angeles as she passes by various memorials for Hussle.
As the CO2 and hydrogen flows over the powder, it triggers a chemical reaction that produces methane and other useful hydrocarbons.
NAFTA was originally billed as one of the first trade deals ever to safeguard intellectual property that flows over national borders.
As more and more data flows over mobile networks and as Huawei has become more ubiquitous in them, governments have grown uncomfortable.
A pre-crime move, if you will, and a drastic one, since much critical information in that country flows over these platforms.
Tapping into the data Beyond just listening into voice chatter, there's a lot of interpretable data that also flows over the airwaves.
It's the gatekeeping mechanisms the platforms use to control the nature of the user-generated content that flows over their branded spaces.
A mountain wave is a type of atmospheric gravity wave created by topographical elements like mountains and the way wind flows over them.
The splits, which also cover fish, wood and certain metals, have been calculated based on actual trade flows over a three-year period.
Currently, power in the United States flows over a cluster of separate electrical grids that are maintained by many local or regional utilities.
The scientists found that beyond the mysterious, newly identified layer, there's another, much thicker boundary layer where interstellar plasma flows over the heliopause.
Net FDI flows over the 12 months to December totaled 4.7 percent of GDP, the highest since June 2001, the central bank said.
So whether you realize it or not, a fair portion of your web browsing traffic likely flows over Cloudflare's servers every day anyway.
In all previous Kindles with built-in lighting, which flows over the top of the E-Ink screen, I could always see the LEDs.
"Panther Like a Panther" sees Killer Mike and El-P on blistering form as usual, spitting quick flows over the sparse but funky beat.
Left in its wake is a melancholy melody that ebbs and flows over bubbling, shimmering textures, while that menacing bass lurks in the background.
Essentially, net neutrality — or the open internet — is the view that internet service providers (ISPs) should treat all data that flows over the internet equally.
A specialized compound flows over the intricate geometries of the housing, removing imperfections, establishing a seamlessness between materials and producing a pristine mirror-like surface.
Throughout the day and night it ponderously flows over the luminous ice cores, quietly asking if our future will be anything like this frozen past.
The Lumber River flows over Interstate 95 after Hurricane Matthew caused power outages, downed trees and massive flooding in Lumberton, NC, affecting millions across the area.
He said the refinery had generated strong cash flows over the past five years that far exceed the investment needed to keep the refinery running well.
Now the traditional mode of journalism is now Facebook or something like that, where there's a feed of stuff and stuff sort of flows over you.
Flows over the emergency spillway had stopped, while about 100,000 cubic feet-per-second of water continued down the main spillway, the Department of Water Resources said.
"Improvement in the liquidity and FX flows over the medium-term, possibly driven by increased agricultural output, (could) improve electricity supply and minerals production," Acheampong told CNBC.
We do not expect capex to translate into substantial cash flows over the medium term, given the moderate-to-high execution risks facing the group's export strategy.
Currently, as both sides are members of the European Union, trade flows over the border unimpeded, thanks to their membership in the single market and customs union.
The front wing is the most critical part of the car for creating downforce, Lowe says, because it affects how air flows over the rest of the vehicle.
This is why fixed exchange rate regimes have been so common: but they have collapsed as the growth of capital flows over time have turned them into straitjackets.
The increase in the buyback amount also comes as a surprise and shows the management's confidence in generating strong free cash flows over the next few years, analyst Arment said.
They lay memorable, earworm flows over colorful yet dystopian, future-leaning production that sits somewhere between the tone of Vince Staples' Big Fish Theory and London's rain-soaked evening streets.
Neighbouring Uzbekistan, for instance, has repeatedly urged Tajikistan not to build Rogun - a project conceived in the Soviet era - due to the effect on river flows over their mutual border.
The trend of capital flows over the last little while has been international investors have been looking at their opportunities and decided to spread their resources, whereas Canadian investors have stepped up.
There is little Rolls-Royce can do about this – the best way to cope is to have other business units that are exposed to different cycles and balance cash flows over time.
"It's not the first time they have seen some broken glass on the ground — they've seen the ebbs and flows over time and have a longtime perspective on the market," he said.
Like a telephone service, the intermediaries couldn't be responsible for the content that flows over their network and like a private computer service, operators have a right to get rid of dangerous content.
The CleanSurge Rapid Self-Cleaning is an exclusive feature that uses a built-in motor that repeatedly extracts and retracts the nozzle while water flows over it at the push of a button.
In fact, he said, flows over the past few days in equity funds have been modestly positive, indicating that sentiment hasn't turned negative enough yet to indicate that the end of selling is at hand.
That is why the report also looked at tax and benefit flows over time, observing an immigrant from arrival and projecting his taxes and benefits and that of his or her descendants over the next 75 years.
The bedroom in the ground-floor Quarry Suite steps up to a bathroom with decorative tile, a white marble sink with a copper faucet and an exposed wall of granite that water flows over, like a waterfall.
"We are buying into an operation with cash flowing today so we expect this to have a strong impact on the overall cash flows over the next year or two," Gold Fields Chief Executive Nick Holland told Reuters.
The massive reduction in illegal migration flows over the past decade, due in large part to enduring demographic and economic changes in Mexico, provides a promising foundation, if policy-makers are smart about how to build on it.
A spokesman for the Greek migration ministry, Alexis Bouzis, denied any financial misuse on the part of the government, and attributed the situation to a small rise in migration flows over the summer, which led to a backlog.
Authorities say continued flooding in the days ahead is unlikely to reach the widespread, catastrophic scale seen in Nebraska and Iowa - as excess flow dissipates along the length of the river and water breaches or flows over the tops of levees.
In this case, how the pressure of the water flows over the swimmer's hands—which are usually the only things they can see—is measured by a system that includes two gloves with tube ends that serve as pressure sensors.
" Beijing, it said, "fears the destabilizing effects of a humanitarian crisis, significant refugee flows over its borders, and the uncertainty of how other nations, particularly the United States, would assert themselves on the peninsula in the event of a power vacuum.
While the drugmaker's 12-month trailing payout ratio of 102% might be a tad worrisome, Pfizer has ample free cash flows -- over $15 billion -- and cash reserves -- $14.7 billion -- to more than cover its dividend in the years to come.
The group ebbs and flows over the course of the trilogy, but among them are Sturm, the tragic and noble knight; Tasslehoff, the comic relief trickster; and Flint the dwarf, who is basically just Gimli from Lord of the Rings.
From the flood of inspiration and speculation that flows over 13,000 pages of mirror-writing in Leonardo da Vinci's notebooks to the weather-battered logs that accompanied Ernest Hemingway on the adventures that fuelled his fiction, the spontaneous note is the seed of genius.
In addition, the EU's stated desire to break down data localization measures to stimulate data flows over the internet has run into a brick wall, as France, Germany, and other Member States have sought to create virtual dams that hold data within individual Member States.
The dress is paired with a billowing, floor-length garment that flows over the top and back of the dress and is covered in thick layers of embroidery symbolizing "beautiful life and wealth" and inspired by the type of embroidery used in Japanese Noh Opera.
If Covid-19 cases continue to increase exponentially in the U.S., the prime minister will be left to grapple with how to balance the necessary trade of food and medical supplies that flows over the shared border with the goal of "planking" the coronavirus curve within Canada.
It's unclear what advantage going "round" would bring, as the style's adoption among app makers and designers tends to be more of a trend that ebbs and flows over time, rather than a format that's proven to have a significant advantage over the classic and familiar square/rectangular style.
The Economist has attempted to estimate them by using UNHCR figures for selected crises and averaging the yearly flows over 52 weeks (when yearly data are available, eg, for Iraq and Syria), or by averaging the overall number of refugees over the relevant time period (eg, for Liberia and Afghanistan).
Pacaya, located some 48 kilometers (30 miles) south of the capital, is spewing a column of ash and gas some 3,500 meters (11,483 feet) into the air and has produced different low-level lava flows over the last few months, the seismological, volcanic and meteorological institute Insivumeh said in a statement.
"The best way to confront cable monopolies isn't with inadequate and unenforceable merger conditions, but by ensuring universal and affordable access to big, open pipes, with network owners barred from discriminating against the content that flows over them," said Craig Aaron, the president of Free Press, in a statement following reports that the deal had been approved.
Peter DeSantis, VP of global infrastructure and customer support at AWS speaking at an event Monday night at AWS Re:Invent, explained that much of AWS customer traffic already flows over their massive network, and customers are using AWS Direct Connect to help applications get consistent performance and low network variability as customers move between AWS regions.
If you'd like to know, because I'm going to write about it in the New York Times next week and they're very nervous, Section 230 of the Communications Decency Act gives internet companies broad immunity from anything that flows over, it's sort of treating them like a phone company essentially, and it was done at the time, and I was there and I wrote about it for the Washington Post, actually, in order to allow these companies to grow.
Shrubs: Sorbus and Padus. The Big Cheremshanka River flows over the territory of the selo.
The elevation near the mouth of Blackberry Run is above sea level. The source of the stream is approximately above sea level. The lower half of Blackberry Run flows over rock of the Catskill Formation. Further upstream, the stream flows over the Huntley Mountain Formation.
Some rock outcroppings are present near the stream. Shanty Run flows over soil of the Deep-Wellsboro-Oquaga association in its lower reaches. In its upper reaches, it flows over soil of the Oquaga soil association and the Norris soil association. All of the soils in the watershed are strongly acidic.
The waterfall is located on McGalliard Creek, where it flows over a large bedrock to a lower plunge pool.
The waterfall is located on Moravian Creek, where it flows over a large bedrock to a lower plunge pool.
"As the Beer Flows Over Me" was the catalyst for the album."Head Heritage - Julian Cope's Drunken Songs". Headheritage.co.uk.
At Vanishing Falls, the Salisbury River flows over a dolerite plateau underlain by limestone. The river flows over the edge of the dolerite sill and drains straight into a cave system in the limestone, a phenomenon attributed to karst processes. The above-ground channel downstream of the plunge pool flows only during floods. The Salisbury River is a tributary of the New River.
The river flows over several soil types including Loam, Sand and Alluvium. There are over of drainage ditches that feed into the river, but few natural tributaries.
The water flows over the left bank lip of the mound down to the river at the upstream end of pool into the downstream side of the river.
From the lake, the river travels before emptying into the Laval Bay. In the last segment of its course, the river flows over in the municipality of Forestville.
The water flows over the falls into the lake Ringedalsvatnet (which has a dam at its western end) before flowing through the short river Tysso which empties into the Sørfjorden.
Pilling's Cascade, also known as Renshawe's Cascade, is a waterfall in Piute County, Utah. The waterfall flows over a massive cliff of rocks which are cut by joints, common of Bullion Canyon.
The wings of a fixed-wing aircraft are static planes extending either side of the aircraft. When the aircraft travels forwards, air flows over the wings which are shaped to create lift.
Ancient Egyptians had heard rumours of Lake Tana but had no idea how important the Blue Nile that flows over the Smoking Fire Falls with its fertile volcanic soil was to their civilisation.
Other right bank tributaries include the Llantywaun and Llanerch brooks. It flows over a landscape formed in the mudstones and sandstones of the St Maughans and Brownstones formations of the Old Red Sandstone.
Stairstep Falls is a small, unspectacular waterfall on an unnamed stream flowing into the West Fork. About tall, its highest drop is tall. Its name comes from the rock steps it flows over.
Within the park, this type of falls usually flows over thin layers of Huntley Mountain Formation sandstone. In bridal-veil falls, the second type, water falls over a ledge and drops vertically into a plunge pool in the stream bed below. Within the park, this type of falls flows over Catskill Formation rocks or the red shale and sandstone of the Huntley Formation. In the park, the harder caprock which forms the ledge from which the bridal-veil falls drops is gray sandstone.
Horseshoe Falls, also known as Canadian Falls, is the largest of the three waterfalls that collectively form Niagara Falls on the Niagara River along the Canada–United States border. Approximately 90% of the Niagara River, after diversions for hydropower generation, flows over Horseshoe Falls. The remaining 10% flows over American Falls and Bridal Veil Falls. It is located between Terrapin Point on Goat Island in the US state of New York, and Table Rock in the Canadian province of Ontario.
8, pp. 762–764, Aug. 2005. The effect of this estimation error is equivalent to modifying the underlying utility functions to favor new flows over existing flows. Method to eliminate this error is suggested in.
Upstream of Rush, Wyalusing Creek is braided with logjams and strainers in places. However, there are no deadfalls or fences along it. The creek flows over cobbles. It has riffles and a relatively fast current.
While the turbulent layer grows, the laminar layer thickness decreases. This results in a thinner laminar boundary layer which, relative to laminar flow, depreciates the magnitude of friction force as fluid flows over the object.
Hamlet, the film, directed by Franco Zeffirelli (1990) A northern fork of the Burn of Muchalls flows over lands of Muchalls Castle prior to the confluence with the mainstem Burn of Muchalls within the Bridge of Muchalls.
The Upper Falls Power Plant incorporates a Francis turbine capable of generating 10 MW. The water not diverted to the south fork by the dam flows over the Upper Falls. The north fork of the river splits again at Canada Island and flows over the two Upper Falls on either side of the island. The north fork converges again after the Upper Falls, and is also rejoined by the diverted south fork (through the outlet on the Upper Falls Intake). The Lower Falls is the site of a second diversion dam, the Monroe Street Dam.
The Polomka () is a river in Perm Krai of Russia. It is a left tributary of the Gayva, which is a tributary of the Kama. The Polomka is long. It flows over the north-western part of Perm.
300px Goluboy Dunay River ( - Sky blue Danube) is a river in Voronezh Oblast of Russia. It is a left tributary of the Don River. The Goluboy Dunay is long. It flows over the north-western part of Voronezh.
It passes through the small town of Sili, where it is joined by a major tributary, before reaching the Pacific Ocean at the settlement of Puleia. At its mouth, the river flows over a small cataract, Mu Pagoa Waterfall.
The Patía River () is a river in southwestern Colombia. It flows over to drain into the Pacific Ocean north of Tumaco. The Patía River is the longest river on the Colombian Pacific Coast. The last is navigable by boat.
Repeated lava flows over the last 15,000 years have raised the land surface enough to expose it to the prevailing southwesterly winds, which help to keep the area dry. Together these conditions make life on the lava field difficult.
He was department chair 1970–72. He retired in 1980. Wolfgang Wasow's main research area was singular perturbation theory. A classical application is the thin boundary layer that forms on a solid surface as a fluid flows over it.
The stream is in the Hazleton Basin, which is the largest coal basin in the Eastern Middle Anthracite Field. Long Run flows over an outcrop of coal in one location. There are coal measures near the source of the stream.
The Karanja River is a tributary of the Manjira River. The river basin is up to 2,422 km sq. The Karanja river is perennial river. It flows over a distance of 74 km with Karanja reservoir being major water source.
Due to its location, the artifacts show influence of cultures such as Teotihuacan, the Purépechas and the Toltecs. It has several levels and built over a large hill. When it rains, water flows over the upper levels like a waterfall.
It then flows over the base metal (in a process known as wetting) and is then cooled to join the work pieces together. A major advantage of brazing is the ability to join the same or different metals with considerable strength.
Beaverdam Creek drains of area. The confluence is at the border of felsic gneiss, but the stream then flows over Falls Leucogneiss. The watershed receives an average of 46.6 in/year of precipitation and has a wetness index of 390.31.
Euclid Creek near the intersection of Metropark Blvd. and Highland Road in 1913. The creek has exposed about of the Chagrin Shale, topped by about of the Cleveland Shale. Euclid Creek flows over bedrock more than 360 million years old.
At Rocky Point the Missouri River flows over a Bearpaw shale reef. This provided a rocky bottom and a low-water ford.Axline, Jon, Conveniences Sorely Needed: Montana's Historic Highway Bridges, 1860-1956, Montana Historical Society Press, 2005, p. 119, 120.
Upstream of this confluence, it flows over such soil associations as the Wellsboro association, the Oquaga association, and the Norwich association. Another minor soil association is found near its headwaters. Most of the soil in the watershed is strongly acidic.
The field covers a surface area of with 164 individual centres. It contains lava flows, over 150 cinder cones and 8 tuff rings. 9 or 8 maars are found in the field's western half. These maars have depths ranging between .
Bala Falls at the head of the Moon River The river begins at the Bala Falls in the community of Bala, where those falls drain Lake Muskoka. The river heads northeast, passes through Moon Chute, at which point the Musquash River diverges to the south. The river continues northeast and passes into Wahta Mohawk Territory, flows over the Island Portage Falls, takes in the right tributary Haggart Creek, and passes into the municipality of Georgian Bay. The Moon River continues northeast, flows over Jack Knife Rapids then under Ontario Highway 400, and passes through Moon River Conservation Reserve.
At Rochester it flows over the precipitous edges of the Niagara limestone, forming the Upper Genesee Falls; and below it flows over the edge of the Medina sandstone, forming the Lower Genesee Falls. The principal tributaries of this stream are Canaseraga, Honeoye, and Conesus creeks from the south, and Oatka and Black creeks from the west. Honeoye, Canadice, Hemlock, and Conesus lakes—four of the Finger Lakes—lie within the Genesee Basin. The third subdivision includes the Oswego River and its tributaries, and the small streams flowing into Lake Ontario between the Genesee and Oswego rivers.
Therefore, the pressure decreases and velocity increases partially in the nozzle. This is then passed over the set of moving blades. As the steam flows over the moving blades nearly all its velocity is absorbed. However, the pressure remains constant during this process.
The Kazym () is a river in Russia. It flows over the West Siberian Plain, and is a right tributary of the Ob. The Kazym is long, with a drainage basin of . Its average discharge is . The town of Beloyarsky is along the Kazym.
The vibrations send out a constant noise as water flows over structure, and may lead to cracks or air cavitation which cause catastrophic failure. The phenomenon results from Kelvin–Helmholtz instability, the shear forces that occur between two fluids of different velocities.
Mill ponds are created by a weir that impounds water that then flows over the structure. The energy created by the change in height of the water can then be used to power waterwheels and power sawmills, grinding wheels, and other equipment.
However, if one were to rule out the possibility of a large-scale Indo-Aryan migration, these findings suggest that the genetic affinities of both Indian ancestral components are the result of multiple gene flows over the course of thousands of years.
Chapainawabganj District (Rajshahi division) has an area of 1702.55 km2. Many rivers flows over this area. The main rivers are the Ganges, and Mahananda.300x300pxGoogle Map Most of the land of this area are plain land with many small ponds and water reservoirs.
The source area of the Schilde lies on the North Sea / Baltic Sea watershed: while the Schilde flows over the Elbe into the North Sea, the area north of the springs drains over the Stepenitz and the Trave into the Baltic Sea.
There are some rock outcroppings in the watershed. Most of Quinn Run flows over soil of the Deep-Wellsboro-Oquaga soil association. However, its upper reaches are on soil of the Oquaga association and the Morris association. These soils are all highly acidic.
The elevation near the mouth of Hunts Run is above sea level. The elevation of the stream's source is between and . The headwaters of Hunts Run are on Burgoon Sandstone. The rest of the stream flows over rock of the Huntley Mountain Formation.
The Lisitsa, also known as Bolshaya Lisitsa (), is a river in Tomsk Oblast in Russia, a right tributary of the Ket (Ob basin). The river is long, and its basin covers . The Lisitsa flows over the West Siberian Plain. Its biggest tributary is the Rayga.
The creek turns southwest into the community of Waterdown, and flows over the Niagara Escarpment at Boundary Falls. It re-enters Burlington at the community of Aldershot, turns west, and reaches its mouth at Hamilton Harbour on Lake Ontario, adjacent to the Royal Botanical Gardens.
The stream begins on the Allegheny Plateau and passes through the Fall Brook Gap. It also flows over the Fall Brook Falls, which are high. Fall Brook is situated within the Coal Region. The upper reaches of the watershed of Fall Brook are mainly forested.
However, further downstream, its width is . Its gradient at this location is . Scotch Run flows over rock of the Mauch Chunk Formation for its entire length. However, the headwaters of its unnamed tributary, "Trib 27547 to Scotch Run" are on rock of the Pocono Formation.
Scotch Run flows through the Scotch Valley. The stream flows over the lowest point between Nescopeck Mountain and McCauley Mountain. Scotch Valley is relatively narrow, but becomes somewhat wider downstream of Mifflin Cross Roads. A pond or small lake is located at the stream's headwaters.
The wings of a fixed- wing aircraft are static planes extending either side of the aircraft. When the aircraft travels forwards, air flows over the wings, which are shaped to create lift. This shape is called an airfoil and is shaped like a bird's wing.
The hot mineral water emerges from the spring in the upper canyon at 110°F. The water then flows over a 25-foot waterfall where it is cooled to 95°F and collects in a gravel-bottomed rock soaking pool accessible by a ladder.
Map showing the Benué River drainage basin. The Faro River can be seen to the south of it. The Faro River is a river that flows over the Nigeria–Cameroon border in Africa. Its source is on the Adamawa Plateau, which lies southeast of Ngaoundéré.
This is the source of the Actopan river. It is a beautiful place, full of vegetation and fauna, where the river flows over a cliff. Visitors can descend the cliff while rafting and abseiling (rapelling). The river empties into the Gulf of Mexico at Chachalacas.
The Wisconsinan Boulder Till is typically at least thick. It is upper reaches, the stream flows over bedrock consisting of sandstone and shale. The sandstone and shale are interbedded and are red and gray in color. The bedrock's diamict is reddish-brown to yellowish-brown.
The Orlovka () is a river in Tomsk Oblast with its origins in Krasnoyarsk Krai in Russia, a right tributary of the Ket (Ob basin). The river is long. The area of its basin is . The Orlovka originates from Lake Burgunku and flows over the West Siberian Plain.
The elevation near the mouth of Walker Run is above sea level. The elevation of the stream's source is between above sea level. Walker Run flows over rock of the Mahantango Formation in its lower reaches. Further upstream is a narrow band of the Harrell Formation.
The Salt's headwaters tributaries, the Black River and East Fork, increase the river's total length to about 300 miles (480 km). The name Salt River comes from the fact that the river flows over large salt deposits shortly after the merging of the White and Black Rivers.
The elevation near the mouth of Gallows Run is above sea level. The elevation near the stream's source is between above sea level. For most of its length, Gallows Run flows over bedrock consisting of shale and sandstone. However, Wisconsinan Bouldery Till occurs near the stream's mouth.
The Barysh () is a river in Ulyanovsk Oblast, Russia. It is a right tributary of the Sura (in Volga's drainage basin). It is long, and has a drainage basin of .«Река БАРЫШ», Russian State Water Registry The river flows over the northern parts of the Volga Upland.
Roush Creek Falls is a steep cascade in North Cascades National Park, Washington, U.S. Glacial melt waters from Eldorado Glacier flow south creating Roush Creek. Not far from its origination, Roush Creek flows over Roush Creek Falls, which at , is one of the tallest waterfalls in Washington.
Wolf is a river of Baden-Württemberg, Germany. The historical name of the river is Wolfach. It passes through Bad Rippoldsau-Schapbach and flows into the Kinzig in Wolfach. One of its tributaries flows over the Burgbach Waterfall, one of the highest free-falling waterfalls in Germany.
The elevation of Pigeon Run near its mouth is above sea level. The elevation of the source is between and above sea level. The mouth of Pigeon Run is over rock of the Catskill Formation. Further upstream, it flows over rock of the Huntley Mountain Formation.
The Catawba River flows over 2 major waterfalls in a short distance. The first drop, called Upper Catawba Falls, consists of an upper free-fall drop, while the second drop a short distance downstream, often called just Catawba Falls, is a higher series of free-falls and cascades.
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.
Virdnejávri is a lake in the municipality of Kautokeino-Guovdageaidnu in Troms og Finnmark county, Norway. The lake is a man-made lake located on the river Kautokeinoelva which flows over the Finnmarksvidda plateau. The dam at the northern end is part of the Alta Hydroelectric Power Station.
In times of flood, the river flows over the road creating a ford. A road sign suggests that pedestrians and motorists should "Use causeway if flooded". Grandborough's church is dedicated to St Peter. The church spire, and the two tall Wellingtonia trees which flank it, are notable local landmarks.
The stream flows over Hazleton soil for its entire length. Little Crooked Run is a small stream, with a width of . It has a high gradient of 57.4 meters per kilometer. Some areas in the vicinity of Little Crooked Run in its lower reaches are prone to flooding.
Forestburgh is a town in Sullivan County, New York, United States. The population was 819 at the 2010 census. It is where the Neversink River enters the Neversink Gorge and flows over High Falls."The Legendary Neversink" by Justin Askins The ZIP code of Forestburgh, New York is 12777.
The upper reaches of the creek are relatively slow-moving. At the outflow of Flow Pond, the channel of Mill Run is clean and rocky. Upstream of the pond, the channel is clean and marshy. In its upper reaches, the stream flows over glacial drift in a buried valley.
A scow shoots the Big Cascade Rapids, on the Athabasca River. The Big Cascade Rapids is a navigational hazards on the Athabasca River, near Athabasca Landing, Alberta. The river flows over a series of ridges, with a total height of . Barges can shoot the rapids, during high water.
Yarrabandai Creek is a CreekYARRABANDAI CREEK at NSW Geographic names Board. in New South Wales. It is located at and is in Forbes Shire. The creek starts at an elevation of 289m at an elevation of 254m and flows over near the town of Trundle, New South Wales.
The elevation near the mouth of Ashelman Run is above sea level. The elevation of the stream's source is between above sea level. For most of its length, Ashelman Run flows over a glacial till known as the Wisconsinan Till. This glacial till is typically more than thick.
The entire length of the stream flows over soil of the Deep-Wellsboro-Oquaga soil association, except for the headwaters, which are on soil of the Oquaga and another, minor soil association. Most of these soils are highly acidic. There is a bed of iron ore on Ore Run.
65, John Wiley & Sons, New York The Kutta condition gives some insight into why airfoils usually have sharp trailing edges, even though this is undesirable from structural and manufacturing viewpoints. In irrotational, inviscid, incompressible flow (potential flow) over an airfoil, the Kutta condition can be implemented by calculating the stream function over the airfoil surface.Farzad Mohebbi and Mathieu Sellier (2014) "On the Kutta Condition in Potential Flow over Airfoil", Journal of Aerodynamics Farzad Mohebbi (2018) "FOILincom: A fast and robust program for solving two dimensional inviscid steady incompressible flows (potential flows) over isolated airfoils", . The same Kutta condition implementation method is also used for solving two dimensional subsonic (subcritical) inviscid steady compressible flows over isolated airfoils.
The Frederick House River begins at Night Hawk Lake in Timmins at an elevation of . It flows north into Frederick House Lake at the community of Connaught, near the site of the Hudson's Bay Company Frederick House post, continues north out of the lake into Cochrane, Unorganized, North Part, flows over a small dam and the Wanatango Falls, and takes in the right tributary Wicklow River. It continues north passing along the western border of the town of Cochrane. It flows over the Neelands Rapids, under the Ontario Highway 11 and Ontario Northland Railway (formerly a section of the National Transcontinental Railway) bridges, and over the Sankey Rapids at the community of Frederick.
The river begins at Savage Pond, near the corner of High and Chestnut Streets, in Plainville, Massachusetts. From there, it flows generally south through North Attleborough, Attleboro and Seekonk before entering Rhode Island and flowing through Pawtucket and East Providence where it flows over the Omega Dam into the Seekonk River.
These culminate at Sable Island. A southwesterly ocean current, (occasionally containing runoff from the Gulf of St Lawrence) flows over the inner shelf. The water flow over the banks is weaker and tends have greater variation. The Scotian Shelf contains a canyon called the "Gully", which is more than deep.
Near Te Anga, the river flows over the picturesqueMarokopa Falls walk ("often described as the most beautiful in the country", from the New Zealand Department of Conservation website. Accessed 2013-07-20.) Marokopa Falls. The settlements of Awamarino and Marokopa are located on the river's banks. Trout were introduced about 1910.
After the confluence of its headstreams, the Warme Bode flows over the waterfall of the Unterer Bodefall towards Braunlage. There it is joined by the Ulrichswasser. It continues in the direction of Sorge. From the state border with Saxony-Anhalt it runs parallel to the B 242 federal road to Tanne.
Above the Buttermilk Falls, Buttermilk Creek flows over glacial drift. The creek is a relatively small stream with headwaters in a mountain lake. The surficial geology along most of Buttermilk Creek consists of alluvium. However, in the creek's upper reaches, Wisconinan Till makes up all the surficial geology along it.
The elevation near the mouth of Rattling Run is above sea level. The elevation of the stream's source is between and above sea level. Rattling Run flows over rock of the Mauch Chunk Formation for its entire length. This rock formation consists of siltstone, sandstone, grayish- red shale, and conglomerate.
The falls has a large, deep pool at the bottom commonly known as the "Chug Hole". The river flows over a large, sloping slab of rock before curving steeper and finally dropping into the pool. The appearance of the rock, similar to a turtle's shell, gives the falls its name.
The elevation near the mouth of Marsh Run is above sea level. The elevation of the stream's source is between above sea level. The stream is relatively small and has marshes along it. For most of its length, Marsh Run flows over a glacial till known as the Wisconsinian Till.
The Dudypta () is a river in Krasnoyarsk Krai in Russia, a right tributary of the Pyasina. The river is long, and its drainage basin covers . The Dudypta originates from Lake Makar (Dudypta Lakes) and flows over the central part of the North Siberian Lowland. The river is navigable for upstream from its estuary.
In 1842 Lord Vernon presented to Stockport Corporation of land about southeast of the town. The council laid it out as a public park. One portion rises from the bank of the River Goyt which flows over a weir making a waterfall. There are statues, ponds, rock work, a fountain and planting.
Yercaud is a hill station about from Mecheri, in the Shevaroy Hills of the Eastern Ghats. At an altitude of above sea level, its highest point is the Servarayan temple, at . The Cauvery River flows over a waterfall in Hoganakkal, about from Mecheri. Mettur Dam is a scenic location near the town.
Botkin, p. 255. The Missouri River in this area flows over and through the Kootenai Formation, a mostly nonmarine sandstone laid down by rivers, glaciers, and lakes in the past. Some of the Kootenai Formation is marine, however, laid down by shallow seas.See, generally, Farshori and Hopkins, 1989; Haney and Schwartz, 2003.
However, it cuts through the drift approximately upstream of its mouth. In the lower reaches of Mill Run, the stream flows over some cascades with a height of . In an 1887 book, these cascades were said to give the stream "splendid" water power. A preglacial valley also occurs in the stream's watershed.
The river resumes a southwest course, enters geographic Homer Township, takes in the left tributary East Pukaskwa River, flows over the Schist Falls, and reaches its mouth at Lake Superior. From upstream of the East Pukaskwa River confluence to the river mouth, the Pukaskwa River forms the southern boundary of Pukaskwa National Park.
Known in the Hawaiian language as Waiānuenue (literally "rainbow water"), the falls flows over a natural lava cave, the mythological home to Hina, an ancient Hawaiian goddess. Rainbow Falls derives its name from the fact that, on sunny mornings around 10am, rainbows can be seen in the mist thrown up by the waterfall.
The underlying bedrock includes Fahan slate formation. The river valley of the Mill River flows over a narrow band of Culdaff limestone with a sill of metadolerite along the river's southern embankment extending from the estuarine zone inland. Sandy gravels and conglomerates overlie bedrock. The geology was formed during the Lower Carboniferous Period.
Garbage has been dumped along the stream in its lower reaches. In its lower reaches, it has been ripraped and flows through a flood control debris basin. The debris basin was constructed by the Pennsylvania Department of Environmental Protection and prevents flooding on Bloom Street. Leach Creek flows over cobbles in some reaches.
Ashford Lake's inflows consist of intermittent small streams and runoff, along with springs at the bottom of the pond. The pond's waters are held back by an earthen embankment dam on its south shore. Ashford Lake's outlet is Goss Brook, which flows over the dam's spillway and eventually into the Mount Hope River.
The Pennsylvania Department of Transportation also has a permit to maintain a box culvert made of reinforced concrete on the stream. This culvert is long and high and is sunk into the streambed. Culley Run flows over alluvium in its lower reaches. This alluvium contains stratified sand, silt, gravel, and some boulders.
There are abandoned glacial meltwater channels near the stream's headwaters. Some bedrock ledge outcrops are present in the upper reaches of the watershed. For most of its lower reaches, Chimneystack Run flows over a glacial till known as the Wisconsinan Bouldery Till. It is also present near the headwaters of the stream.
The design of the dividing inner-wall (zweizonige) exhibits the round-arched arcade design typical of Roman-Gothic style. Prior to World War II damage, the arched gallery was open. But it had been only roughly rebuilt when reconstruction began. The light coming in from the large rectangular windows, flows over the gallery.
Buck Creek flows over the dam at Helena, Alabama, during the autumn low-water flow. Helena is located at (33.279715, -86.856060). According to the U.S. Census Bureau, the city has a total area of , of which is land and (0.12%) is covered by water. The Cahaba River and its tributary Buck Creek run through Helena.
Bowman Hollow (also known as Bowman Hollow Creek) is a tributary of Mehoopany Creek in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through Forkston Township. The watershed of the stream has an area of . The stream flows over a highly secluded waterfall known as the Bowman Hollow Falls.
Further downstream, the creek flows over splash dams. Bowman Creek has been known to flood "from time to time". However, because the creek's floodplain is not developed, such floods typically cause a relatively small amount of damage. A flood on the creek in 1850 carried away many buildings such as houses, barns, and mills.
The hamlet of Cannonsville was destroyed to make room for the reservoir. It has the largest drainage basin of all of the NYC reservoirs, at . The reservoir's capacity is . This water flows over halfway through the reservoir to enter the West Delaware Tunnel in the town of Tompkins, just east of the town of Deposit.
The southwestern section of Lookout Mountain is in Alabama. The Little River, in Little River Canyon on the mountain. The river flows over the DeSoto Falls in DeSoto State Park. The Noccalula Falls Park, featuring a pioneer village showcasing several nineteenth-century homes, is located at the southern terminus of Lookout Mountain, in Gadsden, Alabama.
Stratified (smooth) flow exists when the gravitational separation is complete. The liquid flows along the bottom of the pipe as gas flows over the top. Liquid holdup in this regime can be large but the gas velocities are low. Stratified wave flow is similar to stratified smooth flow, but with a higher gas velocity.
According to the U.S. Census Bureau, the county has a total area of , of which is land and (1.2%) is water. Numerous small creeks and streams flow through the county. The Catawba River crosses the county and empties into Lake James. It flows over Catawba Falls on its way, which is accessible to the public.
It is a cave surrounded by a garden. #Kumaradhara river (Bathing Ghat): The river originates from Kumaraparvatha. It flows into the Nethravathi, a river of Dakshina Kannada district, and joins the Arabian Sea. As the river flows over the rocks and thick forest areas it is believed to have medicinal powers to cure skin diseases.
Angel Falls in Venezuela is the world's tallest waterfall at 979 m (3,212 ft). A waterfall is an area where water flows over a vertical drop or a series of steep drops in the course of a stream or river. Waterfalls also occur where meltwater drops over the edge of a tabular iceberg or ice shelf.
When wind flows over a shallow sloped hip roof, the roof can behave like an airplane wing. Lift is then created on the leeward side. The flatter the roof, the more likely this will happen. A steeper pitched hip roof tends to cause the wind to stall as it goes over the roof, breaking up the effect.
The Savala () is a river in the Tambov and Voronezh oblasts of Russia. It is a right tributary of the Khopyor (a tributary of the Don).Савала, Great Soviet Encyclopedia The Savala is long, with a drainage basin of .Река Савала, Russian State Water Registry It flows over the southern part of the Oka–Don Lowland.
Many check dams tend to form stream pools. Under low-flow circumstances, water either infiltrates into the ground, evaporates, or seeps through or under the dam. Under high flow - flood - conditions, water flows over or through the structure. Coarse and medium-grained sediment from runoff tends to be deposited behind check dams, while finer grains flow through.
The Boating Lake (the northern lake) at Stanborough is in size. It is a shallow lake, under three feet in depth with several small islands.The boating lake is fed by water from the River Lea at its north end and from a spring. Excess water flows over a weir back into the river at the south end.
These holes are made by the animal's proboscis, held in place with mucus, and are used for inhalating and exhalating water. Feeding particles are captured as the inhaled water flows over the animal's gills, become embedded in mucus, and are moved along a ciliary tract that leads to the animal's mouth, where they are finally ingested.
The creek flows over the Ginninderra Falls, descending , and through Ginninderra Gorge, to its confluence with the Murrumbidgee River. The catchment of Ginninderra Creek covers approximately . The Ginninderra Creek catchment carries approximately a quarter of Canberra's urban runoff, and there is considerable risk of runoff from urban areas harming aquatic ecosystems in the Murrumbidgee River system.
Minnehaha Creek () is a 22-mile-long (35 km) tributary of the Mississippi River that flows east from Gray's Bay Dam on Lake Minnetonka through the suburban cities of Minnetonka, Hopkins, Saint Louis Park, and Edina, and the city of Minneapolis. The creek flows over Minnehaha Falls in Minnehaha Park near its mouth at the Mississippi River.
The elevation near the mouth of Crooked Run is above sea level. The elevation of the source of the stream is just over above sea level. The upper reaches of Crooked Run are on rock of the Pocono Formation, which dates to the Mississippian Period. The rest of the stream flows over rock of the Mauch Chunk Formation.
The presence of surface flow patterns, in conjunction with crosscutting valleys, has given rise to the hypothesis that these plains likely formed by global lava flows over a short timescale and were subsequently exposed to compressional and extensional stresses. Structurally, plains are often deformed in belts of ridges (dorsa) or fractures (lineae) of various orientation and morphology.
In 1890 a project called the Grand Ditch began. The ditch is a water diversion project. Streams and creeks that flow from the highest peaks are diverted into the ditch, which flows over La Poudre pass, delivering the water into the Atlantic Basin for the use of eastern plains farmers. The ditch wasn't completed until 1936.
North Clear Creek Falls is a waterfall in Hinsdale County, Colorado, located within the Rio Grande National Forest. North Clear Creek is a tributary of the Rio Grande. The waterfall flows over a deck of Nelson Mountain tuff, solidified ash from a volcano in the San Juan volcanic field that erupted about 27 million years ago.
This upper garment flows over both shoulders; but below Hiranyakasipu, the demon-figure placed horizontally across Narasiṃha's body, a twisted waist-band suggests a separate garment covering the legs. The demon's hair streams behind him, cushioning his head against the man-lion's right knee. He wears a simple single strand of beads. His body seems relaxed, even pliant.
The river flows through Murkurti, Pykara and Glenmorgan dams, and forms part of an important hydro-electric power project. The river flows over a series of waterfalls, the last two of and being known as Pykara Falls. The falls are approximately from the bridge on the main road. There is a forest rest house at Pykara.
The crack is the result of a tension fracture along a hingeline produced by the draping of Green Mountain lava flows over the edge of upthrown side of the concealed fault zone. The fissure is located at the southwest corner of Four Craters Lava Field. Hikers can walk the length of the main crack and explore its tributaries.
During storms, minor tributaries also wash large quantities of urban debris and coal waste into the river, degrading it further. In its upper reaches, the Lackawanna River is highly rocky and flows over cobbles. It has virtually continuous whitewater. There are also a few strainers within this reach of the river, due to its small size.
This water is less dense than (DSOW) and lays above it as it flows cyclonically in the Irminger Basin. DSOW is the coldest, densest, and freshest water mass of NADW. DSOW formed behind the ridge flows over the Denmark Strait at a depth of 600m. The most significant water mass contributing to DSOW is Arctic Intermediate Water (AIW).
The composition may reflect magma differentiation in a solitary magma chamber, but with occasional replenishment with more primitive magma. Magma mixing and plagioclase crystallization occurred in it. A lithospheric structure probably directed magma flows over long time periods along the same pathway. The depth of the magma source probably varied over the history of the volcano.
The line from Bedburg to Neuss Hauptbahnhof (main station) runs next to the Erft. The railway crosses the Erft twice between Bedburg and Gustorf. Over the Gustorf–Bedburg section, it flows over a longer distance almost parallel to the railway line. The line is mainly single track; it has two tracks only between Grevenbroich and Holzheim.
Below the bridge it flows over Cantine Dam, creating Cantine Falls. It bends north, then south, and returns to the east, as docks and structures abound on either side. After the Esopus empties into the Hudson, north of its mouth in New York City at Saugerties Light, a few feet (1-2 m) above sea level.
It then flows over the base metal (in a process known as wetting) and is then cooled to join the work pieces together. A major advantage of brazing is the ability to join the same or different metals with considerable strength. The filling materiel used for the joints has a melting point that is above 800°F (427°C).
The cairn is surrounded by 11 standing stones. The River Enrick passes Corrimony, before flowing down Glenurquhart to Loch Ness. The river flows over Corrimony Falls, a waterfall to the south of the settlement.Ordnance Survey 1:25,000 scale Explorer map series, sheets 309-470 An upland area to the south is owned by the RSPB, and run as Corrimony nature reserve.
The waterfall Svartifoss (Black Fall) flows over a step of about 20 metres. Its name comes from the black basalt columns behind it. In the Middle Ages there were a number of large farms in this area, but they were abandoned after two volcanic eruptions and the ensuing glacier runs. The two surviving farms now mostly make a living from tourism.
Hammersley Fork flows over bedrock or large cobbles for much of the stretch between Dry Hollow and Nelson Branch. From the mouth of Nelson Branch to downstream, the stream mostly flows in the central part of its valley. The tributary Nelson Branch has a patch of erosion that is high and long. There is a floodplain at the mouth of Hammersley Fork.
This happens in two not so clearly separated stages, of which the upper one has a height of , and the lower one . The width of the two stages is around . Below the waterfall, Boka Creek flows over a steep valley with stony bottom and empties into the Soča River after less than , which makes it one of the shortest streams in Slovenia.
About 15 million years ago during the Langhian volcanoes poured basaltic lava flows over parts of the area. Still during the Langhian, rivers started to erode their former sediments. In the Pliocene about 5 million years ago the Lower Main river and its tributaries recommenced to deposit sand, gravel and silt. In lakes and swamps also clay layers and lignite developed.
It flows through ten pipes whose diameters range from . The headwaters of Lucky Run are in springs and wetlands on Bald Mountain. One reach of the stream flows over land that has been heavily strip mined. A reach of it was removed by strip mining in the 1940s, but a rock-lined channel was constructed for the stream in the 1970s.
This comprises up to seven thick columnar cooling units of alkali basalt separated by buff-weathered vesicular lava flows. Renewed volcanism sent a series of massive ankaramite lava flows over the second unit and have a total thickness of . These lava flows, comprising the third unit, are spheroidally weathered. The mafic shield-building stage culminated with emplacement of the fourth and highest unit.
Indian Falls is a hamletTown of Pembroke website located closely within the northern border of the town of Pembroke and the western edge of Genesee County, Western New York, United States. Located in what was traditional Seneca nation territory for hundreds of years, the town was named also for a waterfall near its center, where Tonawanda Creek flows over the Onondaga escarpment.
The Gut is a geological feature and conservation area east of Apsley, Ontario, Canada, with unusual Precambrian rock formations and a waterfall."Hope for the Cottageless: an insider’s guide to vacationing in cottage country". Toronto Life, retrieved 20 August 2013. A branch of the Crowe River which passes through the conservation area flows over an exposed basalt lava ridge,Wake, Winifred Cairns.
South of the Wolcott Avenue (NY 9D) bridge, the shores become wooded again as it flows over Tioronda Dam and under the remains of Tioronda Bridge. Below here the creek's estuary opens up, and after being split by a small island it flows under a causeway carrying Metro-North's Hudson Line and empties into the Hudson south of Denning Point.
The river flows south, turns east, then turns south again and subsequently southwest. The mouth of the Yashera is upstream the Luga, northwest of the urban-type settlement of Tolmachyovo. The Yashchera mostly flows over deserted and swampy areas. The drainage basin of the Yashchera includes areas in the north of Luzhsky District and in the south of Gatchinsky District of Leningrad Oblast.
Along some wooded stretches, the creek quietly flows over rocks and is as scenic as any in western North Carolina. In other areas, South Ellerbe is a troubled creek. Its history is marred by rampant pollution and devastating abuse. Though community organizations have arisen to advocate on behalf of the small drainage in recent years, future developments pose significant challenges.
Little Catawissa Creek at the huylkill County Bridge No. 95 The elevation near the mouth of Little Catawissa Creek is above sea level. The elevation of the creek's source is between and above sea level. Little Catawissa Creek flows over rock of the Mauch Chunk Formation for its entire length. Most of the rest of the watershed is also on this rock formation.
Minneopa Creek drains a small watershed in Blue Earth County and a small part of eastern Brown County. Most of its flow through farmland before entering the park. upstream from its mouth, Minneopa Creek flows over two waterfalls. The creek cascades about 6 or 7 feet (2 m) over the upper falls and flows before dropping over the lower falls.
At the 'Cascades', just to the west of the village, the Coliban River flows over and among huge granite boulders and outcrops, creating many rock pools, small and large. The place is popular all year round for walks, picnics and swimming. The Metcalfe Tractor Pull, held in September each year, attracts participants and spectators from all over the state, and beyond.
The water flows over wide concrete slabs, down the bluff towards the river. The west leg of the staircase leads towards city sidewalks and the municipal elevator. When a new elevator was installed and moved slightly in 1955, the Grand Staircase was reconfigured accordingly. Oregon City's Kiwanis club performed maintenance on the promenade in 1969 clearing overgrowth, and they installed lighting in 1972.
High water simply flows over the spillway and out of the canal. The longest spillway, near Chain Bridge, is 354 feet long, was made in 1830 (but has been worked on since). Another spillway near Foxhall road at mile 1.51, was made in 1835. The spillway and waste weir at Big Pool was built in the 1840s An informal overflow.
Its main tributaries are the Churova (right), Pyshega (left), and Tineva (left). The Vyya flows over the hilly landscape of the plain between the valleys of the Northern Dvina and the Pinega, in the conifer forests. The source of the Vyya is located in the southern part of Pinezhsky District. The Vyya initially flows to the south and enters Verkhnetoyemsky District.
Its main tributary is the Pinegskaya Yentala (left). The Ilesha flows over the hilly landscape, in the conifer forests (taiga). The source of the Ilesha is located in the north-eastern part of Verkhnetoyemsky District. The Ilesha initially flows to the south-east, enters briefly Udorsky District, turns south, enters briefly Krasnoborsky District, and then turns south-west and reenters Verkhnetoyemsky District.
A small waterfall on Maple Run The concentration of alkalinity in the waters of Maple Run is 5 milligrams per liter. The elevation near the mouth of Maple Run is above sea level. The elevation of the stream's source is between above sea level. For a significant portion of its length, Maple Run flows over alluvium, mostly in its middle reaches.
Copper Lake Falls is a waterfall about upstream from Malachite Falls. Its three tiers total about in height, and its tallest drop is . The two lower drops probably disappear into the talus they cascade over during lower stream flows, but the upper tier flows over rock hard enough to sustain it all year. The falls flows best from April to July.
The river also crosses the château de la Roche- Maurice and many abandoned mills, and on the banks of its maritime part are several family properties belonging to families in Brest (Park an Coat, le Frout, Beau Repos, le Petit Manoir de Poul ar Velin). At low tide the mud is met, at high tide the sea flows over the countryside.
The elevation near the mouth of Meeker Run is above sea level. The elevation of the stream's source is between and above sea level. The lower reaches of Meeker Run are on rock of the Huntley Mountain Formation and the upper reaches are on Burgoon Sandstone. Below its unnamed tributary, the stream flows over soil of the Deep-Wellsboro-Oquaga soil association.
The dam is located next to Park Drive, a major roadway that cuts throughout the city's park system and interconnects with Route 49. Just across the turnpike in Deerfield it opens over in the "Silly Pond". The water from Sunset Lake flows over the spillway dam and into the Cohansey River. Originally, the lake was known as Tumbling Dam Pond.
Indian Creek begins near Union, West Virginia in Monroe County, closely following United States Route 219, West Virginia Route 122, CR-23 and CR-27. Although only being a creek, it is one of Monroe County's main drainage basins. It passes under the Indian Creek Covered Bridge, near Salt Sulphur Springs. After crossing under West Virginia Route 12, it flows over a hole 9–14 feet deep.
Compounding of steam turbine is used to reduce the rotor speed. It is the process by which rotor speed come to its desired value. A multiple system of rotors are connected in series keyed to a common shaft and the steam pressure or velocity is absorbed in stages as it flows over the blades. The steam produced in the boiler has sufficiently high enthalpy when superheated.
Aubrey Cosens VC Memorial Bridge carrying Ontario Highway 11, attains OPG Hound Chute Generating Station and dam and further downstream Canadian Hydro Developers' Ragged Chute Generating Station and dam. The river flows over Fountain Falls and the Paugan Rapids, and enters the reservoir of the OPG Lower Notch Generating Station and dam. It then passes through the generating station to reach its mouth at Lake Timiskaming.
The Valdayka () is a river in Valdaysky District of Novgorod Oblast and in Bologovsky District of Tver Oblast in Russia. It is a tributary of Lake Piros and belongs to the basin of the river Msta. It is long, and the area of its basin . The Valdayka flows over the Valdai Hills and is a part of the waterway from Lake Valdayskoye to Lake Ilmen.
A salt spring discharges into the Clearwater River in northeastern Alberta. In its upper reaches, the Clearwater River flows over the Precambrian rocks of the Canadian Shield. That section of the river is rough, characterized by rapids, small waterfalls, and a gorge. The river leaves the Shield near the Alberta border and enters the Interior Plains where it becomes meandering, with numerous sand bars and small islands.
The name Bele Vode is originally a hydronym, literally meaning 'white waters'. The adjective bele 'white' may refer to the light color of the water as it flows over rocks, or it may refer to limestone cliffs or deciduous (in comparison to "black", i.e. coniferous) forest that the water flows through. It may also be an old designation indicating 'west', 'right', 'large', or 'major'.
Gordale Scar is a limestone ravine northeast of Malham, North Yorkshire, England. It contains two waterfalls and has overhanging limestone cliffs over high. The gorge could have been formed by water from melting glaciers or a cavern collapse. The stream flowing through the scar is Gordale Beck, which on leaving the gorge flows over Janet's Foss before joining Malham Beck downstream to form the River Aire.
The length of the Sestra is , and the area of its basin is . The Sestra flows over the Karelian Isthmus. The source of the river is in swamps west of the settlement of Vaskelovo, and the Sestra flows in the general direction south, having its mouth in the town of Sestroretsk. It used to fall into the Gulf of Finland until the early 18th century.
The Chuna (), called Uda (; , Üd) above the settlement of Chunsky, is a river in Irkutsk Oblast and Krasnoyarsk Krai of Russia. It is long, with a drainage basin of . The river has its sources in the southwestern parts of Irkutsk Oblast, on the northern slopes of the eastern Sayan Mountains. It then flows over the Central Siberian Plateau, and passes the Nevanka and Nizhneudinsk.
The water is chlorine-free; instead, plants and algae which naturally filter and clean the water are planted in one section of the pool. From this mini-lake, filtered water flows over several small steps into the pool. The shape of the pool is inspired by the Serbian ramonda flower, while the nearby hotel is shaped like a pyramid, mimicking the shape of the mountain itself.
The creek then passes to the east of the hamlet of Marshville, and under Mc Ewan Road. Shortly after crossing under Mc Ewan Road, it curves to the east and begins to parallel Maple Hill. Roughly halfway along Maple Hill, the creek enters into the Canajoharie Gorge, as it passes Wintergreen Flats. Then roughly from the mouth, the creek flows over the Canajoharie Falls.
In the summer, air is drawn down through sinkholes, flows over very cold groundwater and is released out vents on the slopes. Summer temperatures on the slopes range from to . In winter, the air is drawn into the vents, and the groundwater again freezes. Because of the cool temperatures and moist conditions, unusual plants for this part of the country grow on the slopes.
Drainage systems are a crucial compromise between human habitability and a secure, sustainable watershed. Paved areas and lawns or turf do not allow much precipitation to filter through the ground to recharge aquifers. They can cause flooding and damage in neighbourhoods, as the water flows over the surface towards a low point. Typically, elaborate, capital-intensive storm sewer networks are engineered to deal with stormwater.
In reality, the Coriolis parameter varies with latitude, and so the f-plane approximation is not appropriate when considering flows over large lengthscales. The f-plane approximation is also poor near the equator, where variations in f are on the same order of magnitude as f. The beta plane approximation is an improvement on the f-plane approximation which takes leading-order variations in f into account.
The flow over a body may begin as laminar. As a fluid flows over a surface shear stresses within the fluid slow additional fluid particles causing the boundary layer to grow in thickness. At some point along the flow direction, the flow becomes unstable and becomes turbulent. Turbulent flow has a fluctuating and irregular pattern of flow which is made obvious by the formation of vortices.
Water flow over the gills correlates with locomotion, and an octopus can propel its body when it expels water out of its siphon. The thin skin of the octopus absorbs additional oxygen. When resting, around 41% of an octopus's oxygen absorption is through the skin. This decreases to 33% when it swims, as more water flows over the gills; skin oxygen uptake also increases.
The Kerikeri River is a short river of the Waikato region of New Zealand's North Island. It flows into the northern shore of Raglan Harbour. The valley is largely along the line of the fault on the eastern edge of Whaingaroa Harbour. It flows over Coleman Conglomerate and, at its lower end, blue-grey Puti Siltstone, both of Puaroan age (about 150 million years ago).
On that account it is often called the Evrotas Furrow. The Eurotas flows over a flood plain and also through a shallow aquifer of sand and gravel 10–60 m deep, graded with the deep end downstream. The gradient of the aquifer is a steep 1–3%. The highest hydraulic conductivity and transmissivity are near the junction of the Xerias and the Eurotas south of Sparti.
Dams such as the Aylesworth Dam and the Edgerton Dam are also in the watershed of the creek in Archbald. In its upper reaches, the creek's watershed contains wetlands and ravines. The creek flows over coal measures and sees its first mining impacts between the Edgerton Reservoir and the Aylesworth Reservoir. In the lower reaches of the creek, its bank is encroached by overburden and culm.
The hydrologic cycle describes the continuous movement of water on, above, and below the surface on the earth. This flow is altered by ecosystems at numerous points. Transpiration from plants provides the majority of flow of water to the atmosphere. Water is influenced by vegetative cover as it flows over the land surface, while river channels can be shaped by the vegetation within them.
Flowstone formations are curtain-like formations that flow along the sides of caverns or passages. They are the most common formation found in "solution caves" in limestone, such as Cave of the Winds. Sometimes called draperies or curtains, they are formed over thousands of years as the mineral-rich water flows over surfaces leaving calcite behind. The rarest and most delicate formations are called helictites.
It turns east, takes in the left tributary Depot Creek, passes into the northwest corner of geographic Levack Township, Greater Sudbury, flows over a series of rapids, heads around both sides of a small hill, and reaches its mouth at the Onaping River, upstream of the community of Levack. The Onaping River flows via the Vermilion River and the Spanish River to Lake Huron.
After it does, and turns to the east, it flows over the Akron Formation, Bertie Group of dolomitic shales, and the Salina Group. The latter is diverse, including evaporites such as halite and gypsum in addition to its limestones and shales. In the lower section of the creek there is significant groundwater entering the creek. As it discharges, it weathers the gypsum and limestone.
The creek begins at Onapaping Dam on Turceotte Bay on Onaping Lake in geographic Emo Township, Sudbury District, and flows southeast then south, and takes in the left tributary Michaud River. It continues south, passes into geographic Levack Township, Greater Sudbury, takes in the right tributary Carhess Creek, flows over a long series of rapids, enters geographic Dowling Township and passes under Ontario Highway 144 at the community of Levack. The river then flows over the High Falls, which can be viewed from a scenic lookout and nature and geologic trail accessible from the adjacent Ontario Highway 144 (the original Canadian Pacific Railway transcontinental main line — served on this portion of the track by the Via Rail Sudbury – White River train — is also tangent to the right bank of the river at this point). The falls were captured by renowned Group of Seven painter A. Y. Jackson.
The present bridge was built in 1715 and is now a grade II listed structure. A bridge had existed here previously but was only wide enough to take a single horse and was widened when financed by a local man in his will in 1623. The river joins the Ure just south of Masham town and the section of bedrock it flows over at this point is magnesian limestone deposits.
Herefossfjorden is a lake in the municipality of Birkenes in Agder county, Norway. The lake is about long and it is part of the Tovdalselva river. The Gauslåfjorden and Uldalsåna lakes flow into Herefossfjorden near the village of Herefoss at the northern end of the lake. The Uldalsåna lake is held back by a dam and the Gauslåfjorden flows over a waterfall (called the Herefossen) into the Herefossfjorden.
The narrative is ultimately followed by the shaman's delivery of the chasa's message as divined through the mengdu. In one 2002 aek-magi, the chasa announced that the worshipping family would be exempt from an upcoming visit to the village, and explained why: > We can't ignore The offered sacrifice. As your sincerity was utmost, We > accepted the sacrifice. The myth of Saman thus "flows over into the reality" of the worshippers.
The memorial is a fountain in the form of an asymmetric inverted stone cone. A film of water flows over the base of the cone, which contains the 41 names included. It is possible to touch the smooth film of water and to alter it temporarily, which quickly returns to smoothness. As such, the memorial represents the aspirations of the civil rights movement to end legal racial segregation.
The Kármán constant is often used in turbulence modeling, for instance in boundary-layer meteorology to calculate fluxes of momentum, heat and moisture from the atmosphere to the land surface. It is considered to be a universal (κ ≈ 0.40). Gaudio, Miglio and Dey argued that the Kármán constant is however nonuniversal in flows over mobile sediment beds. In recent years the von Kármán constant has been subject to periodic scrutiny.
Spray at the falls' base is immense. The average volume of the falls is 300-500 cubic feet per second of water, which flows over a nearly 1,000-foot (300 m) high cliff as a 125-foot (38 m)-wide river. Reaching the falls is challenging. One has to drive up Depot Creek FSR from the Canadian side, which is in poor condition, before hiking about to the falls.
Jagged terrain combines to produce unpredictable flow patterns and turbulence, such as rotors. Strong updrafts, downdrafts and eddies develop as the air flows over hills and down valleys. Wind direction changes due to the contour of the land. If there is a pass in the mountain range, winds will rush through the pass with considerable speed due to the Bernoulli principle that describes an inverse relationship between speed and pressure.
According to the United States Census Bureau, the city has a total area of , of which is land and is water. Part of the city includes the eastern tip of Lake Minnetonka, one of the largest lakes in Minnesota. The outlet of Lake Minnetonka is Minnehaha Creek, which winds through south Minneapolis and flows over Minnehaha Falls and into the Mississippi River. Minnetonka is located west of Minneapolis, in Hennepin County.
Excessive formation of the biological film may lead to certain problems such as sloughing, it is an important factor to maintain optimum biological film. Maintaining the biological film is accomplished by proper moisture content. For this purpose the humidity of the air is adjusted within the reaction chamber before the vapor flows over the packing media. The biological packing media may be natural or made of synthetic plastic.
Seif and barchan dunes in the Hellespontus region on the surface of Mars. Dunes are mobile landforms created by the transport of large volumes of sand by wind. Rivers and streams are not only conduits of water, but also of sediment. The water, as it flows over the channel bed, is able to mobilize sediment and transport it downstream, either as bed load, suspended load or dissolved load.
In planar graphs, colorings with k distinct colors are dual to nowhere zero flows over the ring \Z_k of integers modulo k. In this duality, the difference between the colors of two adjacent regions is represented by a flow value across the edge separating the regions. In particular, the existence of nowhere zero 4-flows is equivalent to the four color theorem. The snark theorem generalizes this result to nonplanar graphs.
The South Fork Mashel River begins at the outlet of another tiny, unnamed lake which is 0.6 miles due east of the lake where the main fork begins and just lower in elevation. It flows generally northwest from its source to its mouth, a distance of about . The South Fork has no major tributaries but receives many minor streams. Near its mouth the South Fork flows over a waterfall.
Furtado began work on Loose by holding with emcee Jellystone what she referred to as a "hip-hop workshop", in which they would "write rhymes, dissect them, and try different flows over beats." The first producers she worked with were Track & Field—who co-produced her first two albums, Whoa, Nelly! (2000) and Folklore (2003)—and by May 2005, she had collaborated with Swollen Members and K'naan.McNeil, Jason (4 May 2005).
By the end of the period, England had a hot arid desert climate, with frequent flash floods leaving deposits that formed red beds, somewhat similar to the later, Triassic New Red Sandstone. After the end of the Carboniferous period, an intrusion of quartz dolerite formed the Whin Sill. The River Tees flows over this at High Force on the Alston Block. Whin Sill is also seen again at Hadrian's Wall.
At the beginning of the 20th century, part of the Snake River was diverted for irrigation of the Magic Valley. Now, the flows over the falls can be viewed seasonally based on snowfall, irrigation needs and hydroelectric demands. Irrigation and hydroelectric power stations built on the falls were major contributors to the early economic development of southern Idaho. The City of Twin Falls owns and operates a park overlooking the waterfall.
Bridalveil Fall, in Yosemite, flows over the edge of a glacially-carved hanging valley. Sharp changes in slope are common in rivers flowing through the heavily carved landscape left behind when glaciers retreat. Glacial valleys, as well as isostatic rebound resulting from the removal of the mass of glacial ice contribute to this. Niagara Falls, on the border of the United States and Canada, is a characteristic example of knickpoint.
No record of the salt-production process exists prior to the reports of Europeans in the 1800s. The salt-production techniques described by early Europeans differ in many ways from the techniques employed by present-day Kibiro residents. Today in Kibiro, water from hot springs flows over the area's salty soil, keeping it moist. Workers sprinkle dry earth over this, which draws the salt up from the earth.
A kite in flight A kite is an aircraft tethered to a fixed point so that the wind blows over its wings.''Beginner's Guide to Aeronautics'' , NASA (11 July 2008). Lift is generated when air flows over the kite's wing, producing low pressure above the wing and high pressure below it, and deflecting the airflow downwards. This deflection also generates horizontal drag in the direction of the wind.
Fluid flows over clusters of mouthlets near the base of the oral arm disk in the centre of the cylinder. The feeding process is continuous since the jellyfish must be swimming in order to move the prey to different mouthlets so they can be digested.D'Ambra, I., Costello, J. H., & Bentivegna, F. (2001). Flow and prey capture by the scyphomedusa Phyllorhiza punctata von Lendenfeld, 1884. Springer Link, 451(1), 223-227.
Its average discharge at the mouth, according to a USGS stream gauge, is . A peak flow of was recorded there in 2006. The river reaches its highest peaks in the winter and early spring, while it reduces to a trickle by summer and autumn. The river mainly flows over and through coarse Columbia River basalts that comprise the Columbia Plateau, similar in geology to the Palouse River farther west.
The Cavern Cascade waterfall flows over the trail. The park has comfortable camping sites, as well as picnic tables and pavilions, food, playground, a gift shop, pool, dump stations, showers, recreation programs, tent and trailer sites, fishing, hiking, hunting and cross-country skiing. The entrance fee for a day picnic is $8 per car. The park is open year-round, but not all facilities are available at all times.
The Pandavleni complex is in the bed of Gomai river carved in one solid rock. The Pandavleni is around 10 metres below the rest of terrain. There are rather identical two structures around 15 metres apart in east-west line. Sculptures in rock are carved in such a way that water in river flows over the rock, water falls in sculpture complex but force of water do not impact sculptures.
There are also thousands of spotless white storks in the region. The centre of district, Vĩnh Thuận town, lies on the Cái Lớn river which flows over from Hau Giang Province to Cà Mau Province (the part flowing through Thới Bình District, Cà Mau Province called Sông Trẹm (Trẹm river)). Thanks to the Cà Mau Natural Electrical Plant, this river plays an important role in river traffic of the region.
These minerals are deposited on any surface the water flows over, gradually coating it and forming tufa structures known as rimstone dams and gours. Eventually, the older pools begin to fill with deposited minerals, which causes the water to spill over the edges and form new pools. The pools were formed after the end of the last glacial period, some 10,000 years ago, when the continental ice caps retreated.
The difference of these methods could be demonstrated with the methods used in waste water processing: in the clarification phase, sludge sinks to the bottom of the pool and clear water flows over the clear water grooves and continues its journey. The obtained sludge is then pumped into the thickeners, where sludge thickens farther and is then obtained to be pumped into digestion to be prepared into fertilizer.
South of the Pottsville Formation is the Mauch Chunk Formation and then the Pocono Formation. The southernmost reaches of the watershed are occupied by rock of the Duncannon Member formation. The area near the mouth of the creek, it flows over a coal sheet called Sheet III. South of the middle reaches of the tributary Reservoir Creek, all of the soil belongs to the Lackawanna-Arnot-Morris series.
No-till farming practices occur where, in the presence of mulching, ploughing is intentionally forgone as to maintain the sequestration of carbon-rich organic matter in soil. This practice prevents soil exposure to atmospheric oxygen, leaching, and erosion. Ceasing practice of ploughing has been alleged to encourage ant predation on wood- eating termites, allow weeds to regenerate soil, and help slow water flows over land. Shepherds with their sheep.
Most water falls back into the oceans or onto land as rain, where the water flows over the ground as surface runoff. A portion of runoff enters rivers in valleys in the landscape, with streamflow moving water towards the oceans. Runoff and water emerging from the ground (groundwater) may be stored as freshwater in lakes. Not all runoff flows into rivers; much of it soaks into the ground as infiltration.
Bog Creek is a stream in Apache County of northeastern Arizona. It is a tributary to the North Fork White River. The stream source area is on the Mogollon Rim east of Bog Butte and west of Cinder Pit Mountain at elevation . The stream flows west to southwest crossing Arizona Route 260 and then flows over the Rim to its confluence with the North Fork just below the Rim.
A tectonic aneurysm is an isolated zone of extreme uplift and exhumation rates. This forms when uplift from local tectonics are combined with very weak crust and uplift from a river anticline. When a major river flows over an area of tectonic uplift, the erosion from the river will erode the uplifted material. This will cause extremely rapid exhumation along the major rivers, of up to 10 mm per year.
The water flows over a shelf of erosion- resistant sandstone. The falls can be seen from a trail accessible from a parking lot on M-28 or from a sturdy railroad bridge which now is part of a snowmobile and atv trail. This bridge, which once carried the tracks of the Duluth, South Shore and Atlantic Railway, spans the falls. A roadside picnic area offers simple recreational opportunities.
The NRHP-listed Cloyd Hotel (now the Thomas House) is located across Whitley Branch to the south. The Donoho faces East Main Street, which runs parallel to Salt Lick Creek. The Red Boiling Springs area is underlain by a type of black shale (Chattanooga shale), which is exposed in some stream beds. As water flows over this shale, it collects and dissolves iron sulfate, giving the area's springs their once- sought after mineral potency.
The River Geirionydd (Afon Geirionydd in Welsh) is a river in Snowdonia, North Wales. It is a tributary of the River Crafnant (Afon Crafnant), which flows over the Fairy Falls waterfall in Trefriw, and thence on into the River Conwy (Afon Conwy), which is the main river of the Conwy valley. It flows from Llyn Geirionydd down a steep gorge before joining the river Crafnant. It is less than a mile in length.
Flows over 25,000 m³/s have been measured where the Kosi exits the Himalayan foothills, enough to create a flow of water 30 km wide. At this rate, in one week enough water would accumulate to cover the entire megafan to a depth of 1.5 meters. Preventative flood control measures include upstream reservoirs that can also serve irrigation needs and produce hydroelectric power. However, in Nepal these are mostly in the planning stages.
The scheme was technically feasible and financially viable. The main identified environmental impacts were significantly reduced flows over the Aniwhenua Falls, inundation of productive farm land and the displacement of one family, as well as the long term accumulation of sediment in the lake that the project would create. The issue of the reduced flow was managed by the imposing of a minimum residual flow over the falls. The estimated cost was NZ$12.5 million.
This pattern increases nutrients for marine life in the region. Offshore river deltas, freshwater flows over the top of the denser seawater, which allows it to heat faster due to limited vertical mixing. Remotely sensed SST can be used to detect the surface temperature signature due to tropical cyclones. In general, an SST cooling is observed after the passing of a hurricane primarily as the result of mixed layer deepening and surface heat losses.
North of Buttevant the river flows through flat agricultural land, while south of Buttevant the river generally flows through a narrow, steep-sided valley with wooded sides. For the most part the river flows over Carboniferous limestone.National Parks & Wildlife Service The river supports a range of plant species including dropwort, pondweed, club-rush, water-cress and Ranunculus. The river is largely fringed by a narrow strip of marsh vegetation, dominated by reed-canary grass.
The threat from lava flows in the Garibaldi Belt is minor unless an eruption takes place in winter or under or adjacent to areas of glacial ice, such as ice fields. When lava flows over large areas of snow, it creates meltwater. This can produce lahars that could flow further than the associated lavas. If water were to enter a volcanic vent that is erupting basaltic lava, it may create a massive explosive eruption.
The Turbulent Flow Duct provides supersonic, turbulent high temperature air flows over flat surfaces. The TFD is powered by a 20-MW Hüls arc heater and can test samples in size. The Aerodynamic Heating Facility (AHF) has similar characteristics to the IHF arc heater, offering a wide range of operating conditions, sample sizes and extended test times. A cold-air- mixing plenum allows for simulations of ascent or high-speed flight conditions.
A cataract bog is a rare ecological community formed where a permanent stream flows over a granite outcropping. The sheeting of water keeps the edges of the rock wet without eroding the soil; in this precarious location no tree or large shrub can maintain a roothold. The result is a narrow, permanently wet, sunny habitat. While a cataract bog is host to plants typical of a bog, it is technically a fen.
Shōmyō Falls (left) and Hannoki Falls (right) are located in the town of Tateyama, Toyama Prefecture, Japan. Shōmyō-daki is the highest waterfall in Japan at 350 m (1,148 ft). The falls have four stages: the first 70 m, the second 58 m, the third 96 m and the last 126 m high. The greatest amount of water flows over the falls in the early mid summer, when the snow in the Tateyama Mountains melts.
The waterfall is situated in the Girringun National Park as it descends from the Atherton Tableland, where the Stony Creek, a tributary of the Herbert River, flows over an escarpment in the Seaview Range. The falls initially descend over a small number of cascades before the horsetail drop. In total, the falls descend over . Based on the falls' single- drop descent, the World Waterfall Database places Wallaman Falls at 294 in its world rankings.
In hydraulic engineering, a nappe is a sheet or curtain of water that flows over a weir or dam. The upper and lower water surface have well-defined characteristics that are created by the crest of a dam or weir. Both structures have different features that characterize how a nappe might flow through or over impervious concrete structures. Hydraulic engineers distinguish these two water structures in characterizing and calculating the formation of a nappe.
Many pathways of water can enter through a dam structure to produce a well-defined nappe. However, engineers classify dams as either overflow dams, where water consistently flows over or is blocked through a gate on top of crest, or non-overflow dams, which channel water through or around the dam with emergency flood gates. They both range in size. An overflow dam has a similar nappe typology to weirs (free, depressed and clinging nappes).
Almost all of Wainui River's course is through dense native bush, with the lower half meandering through a narrow gorge where the river eventually flows over the tall Wainui Falls, one of the most accessible waterfalls in the Tasman region. Wainui Falls can be reached from a car park in Wainui Bay via the gentle Wainui Falls Track. Wainui Falls, which can be reached at the end of the Wainui Falls Track.
For the kinematic wave it is assumed that the flow is uniform, and that the friction slope is approximately equal to the slope of the channel. This simplifies the full Saint-Venant equation to the kinematic wave: :S_f - S = 0. The kinematic wave is valid when the change in wave height over distance and velocity over distance and time is negligible relative to the bed slope, e.g. for shallow flows over steep slopes.
The valley of the river is much wider, and the river itself spreads out across shallow water and flows over many shifting sand bars. Low-lying, flat areas border the river for much of this section. The final section of the river, from Prince Albert to the Saskatchewan River Forks, has many rapids. The valley is more shallow than the previous sections of the river, and the channel is much better defined.
The Loobu is a river in Northern Estonia. Its source is about 12 km southwest from Rakvere in Lääne-Viru County and it drains into Eru Bay (part of Finnish Gulf) near the village of Vihasoo in Lahemaa National Park. Its drainage basin is rather small and narrow, Loobu lacks any major tributaries. At Joaveski, 10 km upstream from its mouth, the Loobu flows over the Baltic Klint, forming the Joaveski Waterfall.
Rilian is then declared King of Narnia amid the weeping crowd. Aslan appears and congratulates Eustace and Jill on achieving their goal, then returns them to the stream in his country where Jill first met him. The body of King Caspian appears in the stream, and Aslan instructs Eustace to drive a thorn into the lion's paw. Eustace obeys, and Aslan's blood flows over the dead King, who is revived and returned to youth.
Tillman Ravine is a habitat for the barred owl and other endangered species. The ravine was created when the Wisconsin glacier melted and the melt water created a stream by traveling through the weaknesses of the bedrock of the Kittatinny Mountains. Tillman Creek flows over Buttermilk Falls and joins the Flat Brook in the Delaware Water Gap National Recreation Area two-miles south of the hamlet of Walpack Centre in Walpack Township, New Jersey.
The Boronia Park is bordered in Hunters Hill by Park Road to the west, High Street to the north, Ryde Road to the south and the Lane Cove River and Boronia Avenue to the east. Boronia Park Reserve contains Brickmakers Creek where the water flows over Tipperary Falls, a high waterfall on a Hawkesbury sandstone escarpment before entering the Lane Cove River through a tidal pool lined with saltmarsh, mangrove, Avicienna marina and Casuarina glauca.
The Kaibuskong River is a small river in Nipissing District in northeastern Ontario, Canada that runs south through the Township of Bonfield from its source at Lake Nosbonsing. The river flows over a small dam just north of its source, then through two small lakes, La Chappelle Lake and Sheedy Lake, before emptying into Kaibuskong Bay on Lake Talon, from which it flows as part of the Mattawa River system to the Ottawa River.
Judyville is located along the western border of the township, about northwest of the county seat of Williamsport in fertile farmland and sits on a gentle rise with an elevation of approximately 770 feet. Spring Branch creek starts just to the north of town, and Fall Creek, which flows over Indiana's tallest waterfall in Williamsport, starts to its south. The town is located on County Road 300 North, a quarter-mile east of County Road 425 West.
As the steam flows over the blades, due to the shape of the blades, it imparts some of its momentum to the blades and loses some velocity. Only a part of the high kinetic energy is absorbed by these blades. The remainder is exhausted on to the next ring of fixed blade. The function of the fixed blades is to redirect the steam leaving from the first ring of moving blades to the second ring of moving blades.
Similarly, if African proposals that are included in the Doha draft were applied to trade flows over the ten-year period that the study examines, U.S. export volumes would have fallen by 16 percent on average. Average export volumes would have increased dramatically for Brazil and India (12-14 percent), and by a lower but still substantial amount in Uzbekistan, the ‘C-4′ West African cotton producing countries (Benin, Burkina Faso, Chad and Mali), and Australia (2-2.5 percent).
This Felta soil is characterized by an upper surface grayish-brown color and texture of a fine, sticky and plastic nature. West of U.S. Highway 101, Piner Creek flows over the Santa Rosa Plain at gradients of less than two percent. Here the predominant soil type is Zamora silty clay loam, which has been deposited as an alluvial fan as the floodplain formed. The upper soil surface of the Zamora material is grayish- brown hard, firm, sticky and plastic.
Volcanism within the field has also created the -high Helmcken Falls, which is the fourth highest waterfall in Canada. It owes its foundation to the deposits of volcanic rock that were placed down in the wide valley of the Murtle River. Layer upon layer of fresh lava created flat areas, over which enormous floods flowed during the last ice age. These floods shaped the upright cliff in the lava flows over which the river now flows.
The Falls River is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline data. The National Map , accessed January 3, 2012 stream that drains Baraga County in the Upper Peninsula of Michigan in the United States, and flows into Lake Superior in the community of L'Anse. Its name derives from the fact that it flows over slate bedrock with a gradient (rate of descent) that increases as it nears its mouth, cascading over numerous slate waterfalls.
Mount Fuji, Japan All stratovolcanoes and shield volcanoes have a tendency to form a cone at the surface. However, stratovolcanoes are able to form steeper sides whilst shield volcanoes only form very flat cones. The reason for this is that stratovolcanoes are composed largely of solid, eruptive material, whereas shield volcanoes are built up mainly by fluid lava flows. Over the course of time, after several eruptions, a cone of debris forms from the eruptive material.
Ipasha Glacier is located in the US state of Montana in Glacier National Park. The glacier is situated in a cirque to the southeast of Chaney Glacier and immediately east of the Continental Divide at an elevation between and above sea level. The glacier covers an area of approximately as measured in 2005, which is a third smaller than it was in 1966. Melt water from the glacier flows over Ipasha Falls en route to Ipasha Lake.
Below the bridge, the River Sprint flows over a weir to join the river on the north bank. On the outskirts of Kendal, the river turns to the south and is joined by the River Mint on its east bank. Below the junction, a large lagoon was constructed in the 1970s as part of a flood alleviation scheme. It acts as a gravel trap for gravel carried downstream when there are high flows in either river.
Drainage basin of the Adams River The headwaters of the Adams are several unnamed glaciers at roughly elevation in the north-east region of the Monashee Range of the Columbia Mountains. The upper portion of the river flows roughly south and southwest through wetlands and passes through two small lakes, Tumtum and Mica. It has sections of rapids and whitewater, and flows over cataracts below Tumtum Lake. Its flow drops by per kilometre in certain sections.
The Tia River flows over Tia Falls and through the Tia Gorge which are part of the Oxley Wild Rivers National Park are typical New England Tablelands country and can be accessed by a six kilometre gravel access road off the Oxley Highway. Two walking tracks follow the gorge rim. The Falls walk goes to the Falls lookout and Tia Gorge viewing area and is 1.5 km return. Camping, information and picnic areas are available there.
The Chickahominy River is a Coastal Plain tributary to the James River with headwaters northwest of Richmond. For its first , the Chickahominy flows over igneous and metamorphic bedrock of the Piedmont, but soon becomes a Coastal Plain stream near Mechanicsville. The low-gradient Chickahominy sluggishly flows through broad swampy lowlands for from Henrico County to eastern New Kent County. southeast of Providence Forge, the Chickahominy River becomes an estuary and makes a turn towards to the south.
The river basin is situated within Moquegua Region's Mariscal Nieto and Ilo provinces. It is geographically located between parallels 16 º 52 'and 17 º 43' south latitude and between the meridians 70 º 26 'and 71 ° 20' west longitude. The hydrographic system is part of the Pacific slope. The river flows along a geological fault known as Cholo fault, and flows over a length of draining an area of (of which are in a wet basin, located above ).
Wind flow modeling software aims to predict important characteristics of the wind resource at locations where measurements are not available. The most commonly used such software application is WAsP, created at Risø National Laboratory in Denmark. WAsP uses a potential flow model to predict how wind flows over the terrain at a site. Meteodyn WT and WindStation are similar applications that use computational fluid dynamics (CFD) calculations instead, which are potentially more accurate, particularly for complex terrains.
The NX, Clay Street, and Stickel bridges are seen in this view looking downstream, or south, to Newark Gateway. Five bridges over the Passaic River at Newark. The Lower Passaic River in New Jersey is the section of the Passaic River below the Great Falls which flows over the Dundee Dam to the river mouth at Newark Bay in the northeastern part of the state. Its midpoint generally delineates the Essex-Hudson and Passaic-Bergen county lines.
Tahquitz Falls is a waterfall on Tahquitz Creek in the west skirt of the city Palm Springs, in the U.S. state of California. The waterfall is located in lower Tahquitz Canyon, a short distance upstream from the Visitor Center. The name of the canyon and its waterfall is from a Cahuilla native of the Agua Caliente folklore. The river flows over a slab of granite atop the falls, after which it plunges about into a pool.
Each incorporates water walls, brick or granite paving, cast concrete bluestone-clad seating, plantings and lighting. At The University of Texas at San Antonio an austere conical granite fountain forms the center of the "Healer's Spring" rotunda. In the "Wall of the Tides", water flows over a mosaic while spheres across a stainless steel arch above reflect both the moving water and the passing clouds. Two of her major works form prominent centerpieces in airport concourses.
On June 15, 1991 five kayakers descended the river from its source and through the private, posted property of the Adirondack League Club. The journey was to test the laws regarding the rights of the public to paddle on water that flows over private property. The League Club was given advance notice, and the trip was taped by both groups as evidence. As expected the League Club promptly sued the paddlers, and the Sierra Club for five million dollars.
When a nickel coin, or any coin, is struck, the metal must "flow" into the contours of the front and back dies. It is through the atoms of the metal flowing into the dies that flow lines are created. However, when metal flows over a sharp corner in the die, like the edges of a mintmark or words, it tends to roll the detail out. It wears on the die, and a little detail is lost with every strike.
Grand Union Falls, also called Grand Junction Falls or Blue Grouse Falls, is an often overlooked waterfall on Eagle Creek just below the famed Tunnel Falls. It is similar in appearance, geology and form to Sevenmile Falls not too far upstream. The falls drop about in a punchbowl form, ending in a large, clear pool below. The cliff it flows over consists of the same columnar basalt that is very common in the Columbia River Gorge area.
Laminar flow over a body occurs when layers of the fluid move smoothly past each other in parallel lines. In nature, this kind of flow is rare. As the fluid flows over an object, it applies frictional forces to the surface of the object which works to impede forward movement of the object; the result is called skin friction drag. Skin friction drag is often the major component of parasitic drag on objects in a flow.
Source of the Tietê River in Salesópolis: The water flows over stones. The river starts in the Serra do Mar, to the east of São Paulo city. Ihe municipality of Salesópolis, it encounters one of the first hydroelectric power stations constructed in Brazil, "Usina Parque de Salesópolis", constructed in 1912 by the old São Paulo Tramway, Light and Power Company. It generated energy from an artificial waterfall with a height of 72 m of the river.
The river begins at Lake St. Joseph at an elevation of . and flows over the Rat Rapids dam and under Ontario Highway 599 into Osnaburgh Lake. From there it flows via a Main Channel (northern) and South Channel around Kagami Island northeast, and takes in the right tributary Misehkow River and left tributary Etowamami River. The river continues over the Upper Eskakwa Falls, takes in the right tributary Shabuskwia River, and travels over the Eskakwa Falls and Snake Falls.
A branch of Kitchen Creek flows from the southern end of the lake; downstream it enters Lake Jean in Ricketts Glen State Park. From there the water flows through Ganoga Glen and its 10 named waterfalls, then joins the main stem of the creek at Waters Meet; below this it flows over five more named waterfalls. Kitchen Creek is a tributary of Huntington Creek, which flows into Fishing Creek, which is a tributary of the Susquehanna River.
However, with the increasing number of businesses that operate globally distributed data centers connected using private inter-data center networks, it is likely to see increasing research effort in this realm. A very recent work on reducing the completion times of flows over private WAN discusses modeling routing as a graph optimization problem by pushing all the queuing to the end-points. Authors also propose a heuristic to solve the problem efficiently while sacrificing negligible performance.
They are also very common in agricultural areas because sustained agriculture depletes the soil of much of its organic content, increasing the erodibility of the soil. Agricultural machines, such as tractors, compact the soil to the point where water flows over the surface rather than seeping into the soil. Tractor wheel impressions often channel water, providing a perfect environment for the generation of rills. If left alone, these rills may erode considerable amounts of arable soil.
A cataract bog is a rare ecological community, formed where a permanent stream flows over a granite outcropping. The sheeting of water keeps the edges of the rock wet without eroding the soil, but in this precarious location no tree or large shrub can maintain a roothold. The result is a narrow, permanently wet, sunny habitat. While a cataract bog is host to plants typical of a bog, it is technically a fen, not a bog.
They are very effective in reducing wind and water erosion which results in sediment trapping and water infiltration. They function in similar fashion to a contour buffer strip, just much narrower. Field borders are bands or strips of perennial vegetation that is found on the edge of a cropland field. Field borders help with runoff only when it flows over the strip. They’re very effective in benefiting spraying operations because they allow for extra room between adjacent fields.
Bacon Creek is a glacial stream in Whatcom County, Washington. It originates in a glacier on the southwest face of Bacon Peak, flows into a small tarn, then flows over the Berdeen Falls. At the base of the waterfall, the creek turns southeast and joins the Skagit River near and discharges into the Skagit River near Marblemount.Waterfalls NW retrieved 6th Dec 2009 Bacon Creek was named for prospector Albert Bacon, who arrived in the area around 1879.
An antecedent stream is a stream that maintains its original course and pattern despite the changes in underlying rock topography. A stream with a dendritic drainage pattern, for example, can be subject to slow tectonic uplift. However, as the uplift occurs, the stream erodes through the rising ridge to form a steep-walled gorge. The stream thus keeps its dendritic pattern even though it flows over a landscape that will normally produce a trellis drainage pattern.
Between the state line and Elk Mills, it flows over Twisting Falls, a drop of approximately 30 feet (nine m). At this point, it is bridged by U.S. Highway 321. Shortly below this point, its waters become slack as part of an embayment of Watauga Lake, a sizable reservoir of the Watauga Dam Project of the Tennessee Valley Authority. This project has flooded the actual site of the original confluence of the Elk and Watauga rivers.
Because of bottom drag, as water flows over the bottom the lower tube opening has a lower fluid speed and thus a higher pressure than the upper tube opening. The benthic suspension feeder can hide in the tube as the pressure difference between the tube ends drives water and suspended particles through the tube. The body shapes of many benthic creatures also exploit Bernoulli's Principle not only decrease the friction and drag but also to create lift when they move through the current.
Round Mountain Radar Station, from the air The northern slopes of Round Mountain are drained by the Guy Fawkes River which flows over the Ebor Falls and eventually goes into the Clarence River. The south slopes of Round Mountain are drained by the Styx River which flows to the Macleay River and the Oaky River which drains into the Chandler River. A radar air navigation station, for the control and guidance of aircraft, is located on the summit of Round Mountain.
Water flows over lumpy deposits of tufa at Big Hill Springs Provincial Park. A series of springs feed the small stream that flows through the park, and its waterfalls flow across deposits of tufa that precipitated from the spring water.Benham, P. and Guan, Y. 2019. Hike 69, Big Hill Springs Provincial Park; In: Benham, P. McKenzie, B., Chatellier, J.Y., and Tippet, C. (eds.); Go Take A Hike, The geology of trails in the Canadian Rockies and surrounding areas, p. 240-241.
Water flows over an embankment near Talsarnau Gwynedd On the Welsh coast 100 residents were evacuated from vulnerable homes in Borth and Aberystwyth. Aberystwyth was hit by destructive high waves for the second time this winter, after it was hit by a storm which followed the St. Jude storm on 2–3 November 2013. Aberystwyth sea front has previously been severely damaged by storms in October 1927 and January 1938. Damage occurred to sea defences and gardens at St Bees, Cumbria.
Banklick Creek rises in rural areas near the Boone-Kenton County line near the city of Walton then flows northeasterly through Kenton County and empties into the Licking River near Latonia in a highly urbanized area, less than from the Licking's confluence with the Ohio River. Covering more than , the topography of the Banklick's watershed ranges from steep to gently sloping. Throughout most of its length, Banklick Creek is shallow and flows over a narrow, gravelly, and sometimes rocky streambed. However, approximately ¾ mi.
Metals are also used for heat sinks to protect sensitive equipment from overheating. The high reflectivity of some metals enables their use in mirrors, including precision astronomical instruments, and adds to the aesthetics of metallic jewelry. Some metals have specialized uses; mercury is a liquid at room temperature and is used in switches to complete a circuit when it flows over the switch contacts. Radioactive metals such as uranium and plutonium are used in nuclear power plants to produce energy via nuclear fission.
The North Shore Channel near the Bahá'í House of Worship in Wilmette, Illinois. At the south end of the North Shore Channel, the North Branch of the Chicago River flows over a small dam, now removed, into the confluence. View looking northwest, near River Park in Chicago. Chicago area rivers The North Shore Channel is a drainage canal built between 1907 and 1910 to flush the sewage-filled North Branch of the Chicago River down the Chicago Sanitary and Ship Canal.
The Spechty Kopf Formation occurs on the northernmost edge of the watershed and the Pottsville Formation occurs not far to the south of the stream. Mining land in various stages of reclamation also occurs to the south of the stream, on McCauley Mountain. Scotch Run flows over Leck Kill soil, a deep and well- drained fine loamy soil for its entire length. However, the northern and southern edges of the watershed are on Hazleton soil, a deep, loamy, siliceous, well-drained soil.
It is joined in this section by the Tazin River, its largest tributary. There is a hydroelectric generating plant at the Twin Gorges Forebay, from where the water flows over Elsie Falls and then for to Tsu Lake over a series of rapids and through the Nende Chute, a narrow gorge, before entering Tsu Lake. The Konth River drains from the northeast into Tsu Lake. The average flow from 1960 to 1995, measured at a gauge at Tsu Lake Dam, was .
Walnut Creek is a long tributary stream of the Colorado River in Texas. It flows from north to south, crossing the Edwards Plateau on the western side of Austin, down to the Blackland Prairie on the eastern side of the city where it then drains into the Colorado River downstream of Longhorn Dam. The stream's upper region flows over limestone, while the southern stretch passes through deeper clay soils and hardwood forest. Walnut Creek's watershed, spanning , is the largest in Central Austin.
The upper Spruceton Valley is underlain by rocks of the Lower Walton Formation; puddingstones and other conglomerates are found in the Upper Walton Formation at high elevations. From just above the hamlet of West Kill to its mouth, the West Kill flows over rocks of the Oneonta Formation. The superficial deposits within the watershed also reflect its glacial origins. While the high elevations are covered with rock, glacial till dominates further down, including in much of the West Kill's upper reaches.
Sindhi has extended its boundaries beyond the province of Sindh . In northern Sindh it flows over the north-west into Balochistan province, former Bahawalpur state (now in Punjab), on the west it is bounded by the mountain range separating Sindh from Balochistan. This boundary has not been crossed by Sindhi, except in the southern part of the hilly area of Kohistan. Here in general, the language spoken is Balochi but Sindhi is also spoken by a large number of population.
The commune includes within its confines the sources of the Anger and Mouzon rivers which set off in opposite directions before they connect between Pompierre and Circourt after about thirty kilometres (nineteen miles). The valley of the Mouzon, which sets off in a westerly direction before turning to the north, flows over relatively flat plateau land rather than in some form of a gorge: claims appropriate to a spa village are made for the health giving properties of the air here.
Below Renk the White Nile enters Sudan, it flows north to Khartoum and meets the Blue Nile. The course of the Nile in Sudan is distinctive. It flows over six groups of cataracts, from the sixth at Sabaloka just north of Khartoum northward to Abu Hamed. Due to the tectonic uplift of the Nubian Swell, the river is then diverted to flow for over 300 km south- west following the structure of the Central African Shear Zone embracing the Bayuda Desert.
As it flows over the holy lingams, the river attains a sanctified status and passes through the temples that are downstream. The visible lingams are in a rectangular enclosure with a channel flowing out, which is interpreted to represent the yoni as the "female principle". Beyond these lingams, the river stretch of about includes a small rocky island and ends over a fall into a pool. In this stretch of the river, there are bas reliefs on the rock faces.
Soon after Pierstown was formed, mills were built on Leatherstocking Creek, the water eventually flows over Leatherstocking Falls, was used to generate power. At one point there were three sawmills, three gristmills and a carding machine in operation. There were also at different times five taverns, three stores, two tanneries, four blacksmith shops, a pottery, a brewery, a wagon shop, a lead pipe factory and several weaver shops. By 1886 all that remained of the businesses was a blacksmith shop.
They can exhibit reverse gradients, which result when pressurized meltwater flows over obstacles such as ridges or hills along the glacier bed. Tunnel valleys can be formed under extremely thick glacial ice – examples have been observed on the bottom of Lake Superior and in the oceans offshore in Antarctica. The course of a tunnel valley typically runs from thickest glacial ice to the glacier margin; as a result the glacial ice pressurizes the water such that it runs uphill toward its end.
The Rivière des Chutes (English: River of the Falls) drains mainly the municipality of Saint-Narcisse, and also Saint-Stanislas, at the end of its course. These municipalities are located in the Les Chenaux Regional County Municipality, in the administrative region of Mauricie, in the province of Quebec, Canada. The Rivière des Chutes flows over (including 1.7 km in Saint- Stanislas at the end of it path) and drains a watershed of an area of (including watershed Sanschagrin stream, in Saint-Stanislas).
An early instrumental of the song from the Viva la Vida sessions was leaked into the internet in 2009, it contained an excerpt from a previously performed song named "Solid Ground (Until the Water Flows Over)" as the intro, but it was scratched and the song remained unreleased. The song is the first anti-war protest song from the band, and it borrows its rhythm from The Beatles. "Violet Hill" derives its title from a street of the same name near Abbey Road.
Ramm also wrote the pamphlets En forsvarsbrochure in 1915 and Ruhr-aksjonen in 1925. He is especially known for the article "En skitten strøm flyter over landet" (A Dirty Stream Flows Over the Country) on 28 October 1931, an attack on Gyldendal Norsk Forlag's novel contest in 1931. Ramm saw the entrants to this contest as being infested by Freudianism. He especially lambasted the runner-up, the radical intellectual writer Sigurd Hoel, but also Hans Backer Fürst, Rolf Stenersen and Karo Espeseth.
The river flows over a length of in a zigzag course. Before the river joins the sea, at about upstream it forms two branches; the western branch is called the York River and the eastern branch is called the McKillop River. The York River rises on the eastern flanks of Brooks Mountain, the highest point in the York Mountains, in the central part of the Teller Quadrangle. It flows in a northeast direction and then confluences with the McKillop River.
Falls Creek emanates from springs of the Arbuckle aquifer and flows over several waterfalls, the most notable being Price Falls, before dumping into the Washita River. The geologic formations surrounding Falls Creek have been dated to the Ordovician and contain many fossils of organisms that lived during that time. A large graben is present in the camp which contains the clastic materials of the Royer Dolomite which underwent karsting and was redeposited during the Pennsylvanian as the Collins Ranch Conglomerate.
The bridge was designated a National Historic Landmark in 1982. A platform under the bridge's central arch lets visitors hear the echo that earned the bridge its name. There is direct access to the top of the bridge from the parking area. At the northern end of the park, just before the river flows under Route 9, it flows over a horseshoe-shaped dam constructed in the early 20th century at a site that housed a mill as early as the 18th century.
If the surface flow of the runoff is diverted and concentrated by drains that create constant flows over the beach above the sea or river level, the beach will be eroded and ultimately form an inlet unless longshore flows deposit sediments to repair the breach. Once eroded, an inlet may allow tidal inflows of salt water to pollute areas inland from the beach and may also affect the quality of underground water supplies and the height of the water table.
Isle Royale geologic map The two main rock assemblages found on the island include the Portage Lake Volcanics and the Copper Harbor Conglomerate, both Precambrian in age. The volcanics are mainly ophitic flood basalts, some 100 individual flows over an accumulated thickness of at least 10,000 feet. The conglomerate outcrops on the southwestern portion of the island and consists of sedimentary rock derived from volcanic rocks in present-day Minnesota. Glacial erosion accentuated the ridge and valley topography from pre-glacial stream erosion.
The preserve is situated in northern Dallas County, and features old-growth bottomland forest with a gentle, wide spring water stream that flows over a bed of solid limestone. The force of the water has cut cliffs from the surrounding Austin Chalk. The towering 20- to 40-foot-tall () cliffs contain Cretaceous fossils dated at 87 million years old, a combination primarily found only in Garland. Austin Chalk is also found in the eastern portion of the DFW Metroplex heading toward the Texas Hill Country.
The land lowered between the Ramapo fault in western Parsippany and the fault that was west of Paterson. The Wisconsin Glacier covered area from 21,000 to 13,000 BC. When the glacier melted due to climate change, Lake Passaic was formed, covering all of what is now Lake Hiawatha. Lake Passaic slowly drained and much of the area is swamps or low-lying meadows such as Troy Meadows. The Rockaway River flows over the Ramapo fault in Boonton and then flows along the northwestern edge of Lake Hiawatha.
In mountainous areas, local distortion of the airflow becomes severe. Jagged terrain combines to produce unpredictable flow patterns and turbulence, such as rotors, which can be topped by lenticular clouds. Strong updrafts, downdrafts, and eddies develop as the air flows over hills and down valleys. Orographic precipitation occurs on the windward side of mountains and is caused by the rising air motion of a large-scale flow of moist air across the mountain ridge, also known as upslope flow, resulting in adiabatic cooling and condensation.
River Deveron near Inverkeithny The River Deveron (), known anciently as the Dovern, is a river in the north east of Scotland. The river has a length of , and has a reputation for its Atlantic salmon, sea trout and brown trout fishing. In its upper reaches peaty water flows over a bottom of shingle and rock and is fast flowing. Before being bridged, the river had to be crossed by "an uncertain ferry which would have landed you somewhere in the neighbourhood of the Old Market Place".
The stream heads in Nizina Glacier, flows southward about to a point near the mouth of Dan Creek, where it takes an easterly course, which it follows for about to its junction with the Chitina. It drains an area of and is nearly as large as the Chitina at their junction. For the first of its course, it flows over a gravel flood plain from wide, bordered by steep-sloped mountains in height. At low water, it follows one or more constantly shifting channels.
As the fast-flowing water of the river flows over the sharp, near- vertical rock exposure at the widest reach of the river, it generates misty clouds and then hits into a pond formed in a semicircular shape at the bottom of the falls. Adventure sports enthusiasts use boats in the stormy part of this pond. Pilgrims bathe in the calmer part of the lake. In the low-flow season, paddle boats are used in pools formed in the upstream part of the falls.
The Worth Valley reservoirs and their drinking water supply. Water for Ponden Reservoir either flows downstream from Watersheddles reservoir, or through the streams that feed the reservoir separately. One of the major tributaries is Ponden Clough, which flows over sandstone beds, typically composed of grit, mudstone and Keighley Bluestone (a hard wearing stone used in road building locally). A catchment tower was built at the head of Ponden Clough which takes water away from the stream and straight into Watersheddles by the means of a conduit.
The observation that old windows are sometimes found to be thicker at the bottom than at the top is often offered as supporting evidence for the view that glass flows over a timescale of centuries, the assumption being that the glass has exhibited the liquid property of flowing from one shape to another. This assumption is incorrect, as once solidified, glass stops flowing. Instead, glass manufacturing processes in the past produced sheets of non-uniform thickness leading to observed sagging and ripples in old windows.
Hexagons Pool Hexagons Pool The Hexagon Pool (, Breichat HaMeshushim) is a natural pool in the Meshushim Reserve, part of the Yehudiya Forest Nature Reserve, in the central Golan Heights. The pool, at the bottom of a canyon, is named after the shape of the hexagonal basalt columns that make up its walls. This geological formation was created by the slow cooling of layers of lava flows over a long period. When the lava solidified and cooled, it was split into polygonal shapes due to its contraction.
These will eventually exhaust any amount of buffering in the switch. However, blocking the sending link will cause all flows over that link to be delayed, even those that are not causing any congestion. This situation is a case of head-of-line blocking (HOL), and can happen more often in core network switches due to the large numbers of flows generally being aggregated. Many switches use a technique called virtual output queues to eliminate the HOL blocking internally, so will never send pause frames.
On later maps, such as the 1839 Cass County map (Cass being the original name for Bartow County), it was referred to as "Hightower River", a name that was used in most early Cherokee records. The large Amicalola Creek (which flows over Amicalola Falls) is a primary tributary near the beginning of the river. The Etowah then flows west-southwest through Canton, Georgia, and soon forms Lake Allatoona. From the dam at the lake, it passes Cartersville and the Etowah Indian Mounds archaeological site.
Midway along it is a small stone foot bridge, with battered stone piers and an arch, with the same voussoirs as the retaining wall arch but a shouldered keystone. From there it flows over another waterfall and under the drive bridge, similar to the foot bridge but heavier, then into another culvert under North Washington Avenue. There are two playgrounds within the park. A smaller, older one is in the northwest corner, and a newer and larger one in the southwest, near the library.
A roof rack is a common trait on many SUV and station wagon vehicles. While roof racks are very useful in carrying extra storage on a vehicle, they also increase the frontal area of the vehicle and increase the drag coefficient. This is because the air flows over the top of the vehicle, following the smooth lines of the hood and windshield, then collides with the roof rack and causes turbulence. The removal of this part has led to increases in fuel efficiency in several studies.
Waterfalls downtown Granby. The North Yamaska river (in French: Rivière Yamaska Nord) is a tributary of the Yamaska river. It flows over on the south shore of the Saint Lawrence river in Quebec, Canada and passes through five municipalities, some of them sourcing their fresh water from it. Like the rest of the Yamaska, it is an important source of life, though urban development, agriculture and industrial uses have had a negative impact on the ecosystem depending on its waters since the colonization of the Eastern Townships.
The Twenty Mile Creek watershed contains five sub-watersheds including the main channel of Twenty Mile Creek; Gavora Ditch, Spring Creek, North Creek and Sinkhole Creek. The Twenty Mile Creek watershed contains several areas of natural and scientific interest, environmentally sensitive areas, and regionally significant wetlands. The upper reaches of the Twenty Mile Creek watershed are characterized by rolling topography with fairly steep slopes in the headwaters. Further downstream, the watershed contains gently rolling to flat topography before the creek flows over the Niagara Escarpment.
However, other rock formations also occur in the watershed. A substantial area of the Pocono Formation can be found in the northwestern part of the watershed and large areas of rock of the Pottsville Formation occupy portions of the southern and western parts of the watershed. Small areas of the Spechty Kopf Formation and the Buddys Run Member of the Catskill Formation are found in the northwestern part of the watershed. Little Catawissa Creek flows over Leck Kill soil for most of its length.
The Tsunami UDP Protocol is a UDP-based protocol that was developed for high- speed file transfer over network paths that have a high bandwidth-delay product. Such protocols are needed because standard TCP does not perform well over paths with high bandwidth-delay products .How Tsunami Works Tsunami effects a file transfer by chunking the file into numbered blocks of 32 KB. Communication between the client and server applications flows over a low bandwidth TCP connection, and the bulk data is transferred over UDP.
The Lake totals approximately and is supplied by the River Teise (contributory to the River Medway), which rises in the valley Dunorlan Park is set into. The river was dammed twice to form a pond, and subsequently the lake. The lake then flows over a cascade into the Victorian water garden and pond before reaching the fountain. Protracted repairs to the main dam required the lake to be lowered, drawing attention to the heavy silting and the failure of the stream feeding the water system.
Mt. Susitna is a roche moutonnée, a landform created when a glacier flows over a resistant, topographically high, bedrock body, creating a smooth-sided and teardrop shaped feature aligned with the direction of ice flow. The Anchorage bowl topography has been influenced by 5-7 glaciations. Over several thousand years, thick ice sheets from the Talkeetna, Chugach and Alaska Ranges flowed down Cook Inlet. The five well documented glaciations from oldest to most recent were the Mt Susitna, Caribou Hills, Eklutna, Knik and Naptowne.
The sacred veil of the goddess in the temple flows over Yug and the girl as they stare in to each other's eyes. (This was exactly how Yug and Vrinda met for the first time.) Then they snap out of their eye lock and stand up straight. The girl introduces herself as Radha and Yug, mesmerised by her beauty (this is the first time Yug is mesmerised by anyone other than Vrinda) offers to drop her home. Radha accepts Yug's offer and gets into his car.
Mechanical pumps may be submerged in the fluid they are pumping or be placed external to the fluid. Pumps can be classified by their method of displacement into positive-displacement pumps, impulse pumps, velocity pumps, gravity pumps, steam pumps and valveless pumps. There are three basic types of pumps: positive-displacement, centrifugal and axial- flow pumps. In centrifugal pumps the direction of flow of the fluid changes by ninety degrees as it flows over impeller, while in axial flow pumps the direction of flow is unchanged.
The reservoir of the Hardap Dam on the ephemeral Fish River in Southern Namibia is the largest in the country. Many of the ephemeral (=seasonally flowing) rivers of the Namibian interior are dammed and, according to the FAO, provide a 95%-assured yield of 96 million m3/year, based on historical rainfall data. These dams have low safe yields in comparison to their total volume, because of uneven flows over time and high evaporation losses. Thus only about half the water from ephemeral rivers is usable.
Dry Falls, also known as Upper Cullasaja Falls, is a 65-foot (20.1 m) waterfall located in the Nantahala National Forest, northwest of Highlands, North Carolina. Dry Falls flows on the Cullasaja River through the Nantahala National Forest. It is part of a series of waterfalls on a stretch of the river that eventually ends with Cullasaja Falls. Dry Falls flows over an overhanging bluff that allows visitors to walk up under the falls and remain relatively dry when the waterflow is low, hence its name.
Bridal Veil Falls is a 45-foot (20.1 m) waterfall located in the Nantahala National Forest, southeast of Franklin. With a short curve of roadway located behind the falls, it has the distinction of being the only waterfall in the state that one can drive a vehicle under. Bridal Veil Falls flows on a tributary of the Cullasaja River through the Nantahala National Forest. The falls flows over an overhanging bluff that allows visitors to walk behind the falls and remain dry when the waterflow is low.
It flows south over Skootamatta Dam, continues south and reaches Slave Lake at an elevation of . It continues south over a small dam, takes in the right tributary Partridge Creek, and arrives in the community of Flinton. The Skootamatta River then flows over Flinton Dam, heads southwest, passes into Hastings County and takes in the left tributary Flinton Creek at an elevation of . The river continues south, takes in the left tributary Little Skootamatta Creek at an elevation of , and turns west just north of Highway 7.
The Piney River is a stream that drains a portion of Tennessee's Cumberland Plateau generally known as Walden Ridge. The Piney River rises near the Rhea County – Bledsoe County line and is referred to as Piney Creek in its upper reaches roughly until its confluence with Duskin Creek. Its major tributary, Little Piney Creek, flows over two spectacular waterfalls which are located in Piney Falls State Natural Area near the community of Grandview. A tributary of Little Piney Creek is Soak Creek, Tennessee's newest State Scenic River.
The name Cray possibly derives from the Anglo-Saxon crecca, meaning brook or rivulet, though it also relates to the Welsh word craie, meaning fresh water. The name may also derive from the Latin word creta, meaning chalk, as the River Cray flows over a chalk bed. The village name derives from the dedication of the parish church to the Blessed Virgin Mary. Roman and Saxon remains have been found in the Fordcroft area. An excavation in 1960 was conducted by members of Bromley Museum in Orpington.
For only second time in its 59-year history water flows over the spillway at Narrows Dam Narrows Dam is a dam located 6 miles north of Murfreesboro, Arkansas, that impounds the water of the Little Missouri River (Arkansas) to create Lake Greeson. Narrows Dam was authorized as a flood control and hydroelectric power project by the Flood Control Act of 1941. The dam is a feature of the comprehensive plan for the Ouachita River Basin. Lake Greeson is operated for hydroelectric power, recreation, and flood control.
This water flows over halfway through the reservoir to enter the West Delaware Tunnel in Tompkins, New York. Then it flows through the aqueduct into the Rondout Reservoir, where the water enters the Delaware Aqueduct, that contributes to roughly 50% of the city's drinking water supply. At Deposit, on the border between Broome and Delaware counties, it turns sharply to the southeast and is paralleled by New York State Route 17\. It joins the East Branch at above sea level at Hancock to form the Delaware.
Typical of the San Francisco Bay Area, Palo Alto has a Mediterranean climate with cool, wet winters and warm, dry summers. Typically, in the warmer months, as the sun goes down, the fog bank flows over the foothills to the west and covers the night sky, thus creating a blanket that helps trap the summer warmth absorbed during the day. Even so, it is rare for the overnight low temperature to exceed . Fog from the Pacific rolling over the Foothills In January, average temperatures range from to .
The Tully River rises in the Cardwell Range, part of the Great Dividing Range on the northern boundary of the Kirrama State Forest. The river flows generally north through Lake Koombooloomba and flows over the Tully Falls near and descends through the Tully Gorge within the Tully Gorge National Park, part of the UNESCO World Heritagelisted Wet Tropics site. Below the dam wall, the river is joined by five minor tributaries before emptying into the Coral Sea at Tully Heads. The river descends over its course.
Nevertheless, understanding potential flow is important in many branches of fluid mechanics. In particular, simple potential flows (called elementary flows) such as the free vortex and the point source possess ready analytical solutions. These solutions can be superposed to create more complex flows satisfying a variety of boundary conditions. These flows correspond closely to real-life flows over the whole of fluid mechanics; in addition, many valuable insights arise when considering the deviation (often slight) between an observed flow and the corresponding potential flow.
Dry Falls, also known as Upper Cullasaja Falls, is a 65-foot (20.1 m) waterfall located in the Nantahala National Forest, northwest of Highlands, North Carolina. Dry Falls flows on the Cullasaja River through the Nantahala National Forest. It is part of a series of waterfalls on an stretch of the river that eventually ends with Cullasaja Falls. Dry Falls flows over an overhanging bluff that allows visitors to walk up under the falls and remain relatively dry when the water flow is low, hence its name.
The eastern areas of the Western Ghats do not receive much rain from this monsoon as the wind does not cross the Western Ghats. The Bay of Bengal Branch of Southwest Monsoon flows over the Bay of Bengal heading towards North-East India and Bengal, picking up more moisture from the Bay of Bengal. The winds arrive at the Eastern Himalayas with large amounts of rain. Mawsynram, situated on the southern slopes of the Khasi Hills in Meghalaya, India, is one of the wettest places on Earth.
Liam McDonald, PC Gamer, January 1997, "Reviews: Mode"., Corel never fully released Mode, the division responsible for the CD Home Collection was shut downFrank, Issue 237, January 15, 1997, "Blood flows over Corel video game bomb", and its software assets were sold to Hoffmann + Associates of Toronto. Mode did receive many favourable reviews at the time, and has since developed an international fan base, see Reception below. Edited playthroughs by one player posted on YouTube between 2012 and 2014 have collectively received over 100,000 views.
The Sand River begins at Sand Lake, in geographic Stoney Township, on which is located the railway point of Sand Lake on the Algoma Central Railway. It leaves the lake South over Sand Lake Dam about west of the community of Millwood. It travels South into geographic Barnes Township, geographic Barager Township, and geographic Broome Township, the latter in which it heads over Calwin Falls. The river continues south into geographic Goodwillie Township, flows over Lady Evelyn Falls, and takes in the left tributary Kwagama Creek.
The Firehole River flows through several significant geyser basins in Yellowstone National Park to include the Upper Geyser Basin, which contains the world-famous geyser Old Faithful. The river was named by early trappers for the steam that makes it appear to be smoking as if on fire. The Firehole flows over three of Yellowstone's major waterfalls: Kepler Cascades south of Old Faithful, Firehole Falls and the Cascades of the Firehole in Firehole Canyon. The river is surrounded by geothermal features which empty water into it.
In bridal-veil falls, the second type, water falls over a ledge and drops vertically into a plunge pool in the stream bed below. Within the park, this type of falls flows over Catskill Formation rocks or the red shale and sandstone of the Huntley Formation. In the park, the harder caprock which forms the ledge from which the bridal-veil falls drops is grey sandstone. The softer red shale below is eroded away by water, sand and gravel to form the plunge pool.
31–35, 153–155. Note: The entire "Atlas of Preliminary Geologic Quadrangle Maps of Pennsylvania" is available as a zip file at #61, here Note: Map 67 is available as a zip file at #67, here Geologists classify the falls at Ricketts Glen State Park into two types. Wedding-cake falls descend in a series of small steps, forming waterfalls that are said to resemble a wedding cake. Within the park, this type of falls usually flows over thin layers of Huntley Mountain Formation sandstone.
Honeoye Creek emerges from the north end of Honeoye Lake, one of the Finger Lakes, in the town of Richmond, Ontario County. The hamlet of Honeoye within Richmond is located on the creek where it passes under US Route 20A. As Honeoye Creek flows northward, it is joined by the Hemlock Outlet Creek and then becomes the border between Ontario County and Livingston County. The stream flows into Monroe County, passing the village of Honeoye Falls in Mendon, where it flows over a waterfall.
A river sometimes flows over a large step in the rocks that may have been formed by a fault line. Waterfalls can occur along the edge of a glacial trough, where a stream or river flowing into a glacier continues to flow into a valley after the glacier has receded or melted. The large waterfalls in Yosemite Valley are examples of this phenomenon, which is referred to as a hanging valley. Another reason hanging valleys may form is where two rivers join and one is flowing faster than the other.
This is looking northwards towards Stanbury across the dam head. The reservoir dams Sladen Beck watercourse and takes water directly from the surrounding moorland including the stream that flows over the Bronte Waterfall. The catchment area is and the Sladen Valley and Beck are part of the larger catchment of the River Worth and ultimately the River Aire. The reservoir has an embankment as the dam head which is straight and extends to a length of , a height of and which also supports a road between Oxenhope and Stanbury village.
During the Ice Age, a glacier forced water to build up in what are now the valleys that hold the Pott Beck and the River Burn. This created large lakes that deposited minerals such as limestone and chert. The river flows over several types of bedrock (limestone, sandstone, mudstone and shale) which is covered by gravel and silty clay which is a result of riverine alluvia. When tested in the 1990s, this alluvia was found to be the largest and coarsest of all sediment that was flowing out through the Humber basin.
The Berwinne () is a small river in the north-eastern part of Belgium. It's a right-bank tributary to the Meuse river and flows over a distance of 31.9 kilometres (19.8 miles) through the provinces of Liège and Limburg. Its source is located in the eastern part of the municipality of Aubel, near the Henri- Chapelle American Cemetery and Memorial. From there the Berwinne river flows, generally spoken, in northwestern direction, through places like Val-Dieu Abbey, Dalhem and Moelingen, before joining the Meuse between Visé and the Dutch border.
Fourbit Creek begins near Mount McLoughlin, where massive faults may allow water to seep into it from nearby Fourmile Lake in the Klamath River watershed. The South Fork turns west and receives Willow Creek on the left. Big Butte Springs are located on Willow Creek, and the Medford Aqueduct, which carries drinking water to cities in the Rogue Valley, parallels the South Fork from there all the way to Butte Falls. The South Fork flows over the Butte Falls—the nearby city's namesake—and merges with the North Fork about downstream.
For a large part of its course, however, the Smestow flows over deep Bunter deposits of sandstone, also known as Triassic Sherwood sandstone – similar to the deposits underlying Sherwood Forest in Nottinghamshire and Cannock Chase in Staffordshire. These are highly permeable, allowing the land above to drain quickly and reducing the flow within river courses. As a result, the areas of South Staffordshire around the river, despite fairly high rainfall, had a natural vegetation of heath and open birch woodland. This was modified progressively after the Anglo-Saxon settlement, with a gradual clearance of farmland.
The Sturgeon River rises on the glacially-eroded plateau that forms much of southern Baraga County. Flowing westward through the Copper Country State Forest, it enters the Ottawa National Forest north of Watton. The length of the river's course in this national forest has been listed as a wild and scenic river, with designated as wild and as scenic. On this stretch, which crosses and recrosses the border between Baraga County and Houghton County, the river helps to form the Sturgeon River Gorge Wilderness and flows over Sturgeon Falls.
A waterfall known as the Nay Aug Falls is on Roaring Brook and the stream flows through the a gorge or canyon Nay Aug Gorge, which is listed on the National Register of Geologic Landmarks. The waterfall is a cascade with a height of and cuts through a soft siltstone formation and flows over conglomerate. A spring known as Chico's Spring is in the stream's watershed in Dunmore, as is a feature known as Barneys Ledge. The Madisonville Cliffs and Glen are located in the watershed in Madison Township and Covington Township.
It is the bronchioles, or parabronchi that generally open into the microscopic alveoli in mammals and atria in birds. Air has to be pumped from the environment into the alveoli or atria by the process of breathing which involves the muscles of respiration. In most fish, and a number of other aquatic animals (both vertebrates and invertebrates) the respiratory system consists of gills, which are either partially or completely external organs, bathed in the watery environment. This water flows over the gills by a variety of active or passive means.
The atmospheric internal waves that form wave clouds are created as stable air flows over a raised land feature such as a mountain range, and can form either directly above or in the lee of the feature. As an air mass travels through the wave, it undergoes repeated uplift and descent. If there is enough moisture in the atmosphere, clouds will form at the cooled crests of these waves. In the descending part of the wave, those clouds will evaporate due to adiabatic heating, leading to the characteristic clouded and clear bands.
A fully rap song "Rules" follows, which some reviewers found it influenced by Kendrick Lamar, with Doja making statements such as "Said play with my pussy, but don't play my emotions". The fourth song, "Bottom Bitch", sampled the 1999 Blink-182 song, "What's My Age Again?", described a traditional pop song by critics, further demonstrates Doja’s confidence to say whatever she likes. On the fifth track, "Say So", Doja gave a groovy nod to the 70s, as she seamlessly switches between floaty vocals and skilfully contained flows over a disco-inspired beat.
Bentley Brook is a stream in Derbyshire, England. It rises on Matlock Moor, flowing south through Cuckoostone Dale, under the A632, into Lumsdale, gathering the valley's waters—notably from Knabhall Brook, out of Tansley, itself dammed and supporting large mills. In Lumsdale it enters a now disused mill pond or reservoir, then flows over a waterfall in the course of passing several historical mill ruins. Finally, it runs through control gates into the outside bend of a tight oxbow of the River Derwent, just beyond Hall Leys Park in Matlock.
Wilderness Falls is located in Waterfalls Canyon, Grand Teton National Park in the U.S. state of Wyoming. The cascade drops approximately in Waterfalls Canyon, fed by unnamed intermittent stream off a glacial lake. The waterfall also receives snowmelt from Ranger Peak to the north and Doane Peak to the southwest. Less than downstream, the same unnamed creek flows over another steep section known as Columbine Cascade The peak time for waterflow is during spring snowmelt and the falls are visible across Jackson Lake from the Colter Bay Village area.
The mafic shield- building stage began with the eruption of thin mafic lava flows over an erosion surface. Successive eruptions sent lava pouring in all directions from central vents, forming a broad, gently sloping volcano of flat, domical shape, with a profile much like that of a warrior's shield. Alkali basalts and ankaramites were the primary lavas produced during this stage of activity which, due to their low silica content, were able to travel great distances away from their source. These lavas also erupted from vents on the flanks of the volcano.
Further, as the threat from Sauron grows, the number of inset poems and songs diminishes. The literary genre is signalled as what Northrop Frye classifies as Romance by the way the Elvish songs speak of fading away. This mirrors what the Elves know is their own imminent passing, while the number of songs of Men increases. The Anglo-Saxon style verse and language of the Rohirrim adds a feeling of real historical depth, and that, Ankeny suggests, flows over into a feeling of verisimilitude for the invented Elvish languages also.
Volcanic passive margins (VPM) and non-volcanic passive margins are the two forms of transitional crust that lie beneath passive continental margins that occur on Earth as the result of the formation of ocean basins via continental rifting. Initiation of igneous processes associated with volcanic passive margins occurs before and/or during the rifting process depending on the cause of rifting. There are two accepted models for VPM formation: hotspots/mantle plumes and slab pull. Both result in large, quick lava flows over a relatively short period of geologic time (i.e.
They have a confluence a little below the former Klondyke Mill, which used water from both rivers. Klondyke was a mining and milling complex connected with some of the metal mines of the Gwydir Forest. The Crafnant is also fed by a number of unnamed streams draining from Cefn Cyfarwydd, the ridge to the north-west. At Trefriw some water from the river is extracted to pass through the Trefriw Woollen Mills to generate hydro-electricity for the machinery, after which the river flows over the Fairy Falls, a popular attraction.
It flows through the gorge to Athelstone, passing over the Eden Fault Zone of the Adelaide Hills face and associated escarpment. After the scarp it flows over sedimentary rocks of varying resistance to erosion, which has led to interspersed narrows and broad basins. From the base of the Adelaide Hills to Adelaide's central business district it runs in a shallow valley with a terraced floor, then down the slope of its own alluvial fan. The structure of this fan shows that the river formerly entered Gulf St Vincent via the Port River.
Some 35 kilometers north of Lijiang is the Baishui Terrace (), an area where spring water flows over a sinter terrace, leaving behind travertine. Fifteen kilometers north of Lijiang is the village of Baisha, famous for the Baisha Fresco and the Naxi Hand-made Embroidery Institute. The Fresco was built in the Ming Dynasty 600 years ago, the Naxi Hand-made Embroidery Institute was built 800 years ago, it is the headquarters of the Naxi embroideries and also, a school for the Naxi embroiderers. There are many Naxi embroidery masters, teachers, students and local farmers there.
On the lower slopes of the mountain, it combines with a branch from Legananny Mountain, just opposite Slieve Croob. The river then turns east to Magheralin into a broad plain between the plateaus of Antrim and Down. The river drains approximately 609 square km of agricultural land and flows over 70 km from the Mourne Mountains to the Stranmillis Weir, from which point on it is estuarine. The catchment consists mainly of enriched agricultural grassland in the upper parts, with a lower section draining urban Belfast and Lisburn.
Tom Tom Falls, at , also known as Upper Little Mashel Falls, is the first major waterfall in the main gorge of the Little Mashel River. The river flows over an old dam, an artifact of an old millpond, before narrowing and plunging about 25 feet over a cliff into a pool below. The falls are only 5 feet wide, so they are quite powerful. In high water, a small portion of the river completely bypasses the falls and its cliff, forming a series of cascades and ending at the river roughly downstream.
La Verna is part of the , , and Gouffre des Partages cave system. Explorations still continue in this and in other systems within the extensive Pierre-Saint-Martin karst area where 13 underground rivers and a total of of passages, chambers and shafts have been mapped.ARSIP INFO Edition Spéciale "Les Traversées de La Pierre-Saint-Martin" p.15 - 2014 Most of the Gouffre de la Pierre-Saint-Martin is formed by dissolution in Cretaceous limestones, and the main river reaches a base level where it flows over insoluble schists of the Paleozoic basement rocks.
The glacier gains more area from additional glacier ice that collects from drifting snow and avalanches below the Suksdorf Ridge as the ridge turns south. The Mazama Glacier terminates at about and is the source of Hellroaring Creek, which flows over several waterfalls before it joins Big Muddy Creek. Klickitat Glacier on the volcano's eastern flank originates in a wide cirque and is fed by two smaller glaciers from the summit ice cap. It terminates around , where it becomes the source of Big Muddy Creek, a tributary of the Klickitat River.
Joala Falls in spring 2010 Between the southeast part of the city of Narva and the rest, facing the Russian city of Ivangorod, the river flows over the Baltic Klint, forming the Narva Waterfall, at times, as it historically was, the most powerful in Europe. Before the water reaches the falls it is split into two branches by the Kreenholm island, thus the falls consist of two branches. Kreenholm Falls, west of the island, is wide and high with multiple terraces. Joala Falls, to the east, is wide and makes the same descent.
Nowadaga Creek flows over a bedrock bed for much of its length and, therefore, is not subject to alluvial processes as seen in many similarly sized river basins. Despite its natural and relatively undeveloped setting, for much of its length the creek lacks a well- developed natural floodplain. In many areas along the creek, the bedrock channel is disintegrating, and pieces of stone that originate from the channel bed are conveyed downstream and deposited in lower velocity reaches of the channel, contributing to debris jams, avulsions, and flooding.
The distillery The spirit is most frequently matured in American oak casks. The malt is peated to a phenol level of approximately 18–22 parts per million (ppm), which is a medium peating level. Additionally, the water used for production, from Cnoc nan Speireag (Hawk Hill), flows over peat which adds additional complexity to the whisky. The distillery began producing special bottlings of the whisky for connoisseurs in the early 2000s, with a 20- and 25-year bottling (where previously only a 10-year and 18-year were available).
The land between the Ramapo fault and the fault west of Paterson lowered, thus the Boonton Gorge was born. The river flows over rocks then cascades over a thirty foot water fall into an oval shaped pool of water with a rock in the center. This pool is about fifty yards long and was a swimming hole until a local ordinance prohibited swimming in 1990 (Ord. 205-5). Then the river drops over a small falls of about seven feet and flows under an arched stone walk-way bridge.
A genetic algorithm was developed described in reference that iterates multiple thermal traces and compares them with the results from thermal simulator to find the best power correlation. The first step is to measure the temperature using IR camera and within the oil coolant that flows over the top of the chip surface, the detailed setup information is described in reference. Oil is chosen because of ease in modeling and accuracy. The infrared cameras must be calibrated to compensate for different material thermal emissions, lens configurations, and other factors in reference.
This is a deeply flooded area in the low-red soil plateau of Madhupur tract. The floodplain is inundated when water flows over the banks of the Turag-Bangshi river making all the low areas become a connected sheet of water in the monsoon. By late November, most of the water recedes and boro rice is planted in almost all of the low-lying areas. During the rainy season the water area is about 43 km² while in the dry season the water area becomes less than 7 km².
Spiral counter-current heat exchange schematic In countercurrent flow, the two flows move in opposite directions. Two tubes have a liquid flowing in opposite directions, transferring a property from one tube to the other. For example, this could be transferring heat from a hot flow of liquid to a cold one, or transferring the concentration of a dissolved solute from a high concentration flow of liquid to a low concentration flow. The counter-current exchange system can maintain a nearly constant gradient between the two flows over their entire length of contact.
A alt=Water flows over a low dam over a river; one tree-lined bank of the river is visible. The army sent about 800 soldiers to Toronto to assist with the cleanup, providing blankets and mattresses. Toronto residents helped out with the relief effort: the Salvation Army received so many donations of clothes, footwear, blankets, food, and money that its storage facilities were overfilled, forcing it to advise against further donations until they were needed. A Hurricane Relief Fund was established to coordinate financial donations, ultimately raising about $5.3 million (CAD).
A central consonant, also known as a median consonant, is a consonant sound that is produced when air flows across the center of the mouth over the tongue. The class contrasts with lateral consonants, in which air flows over the sides of the tongue rather than down its center. Examples of central consonants are the voiced alveolar fricative (the "z" in the English word "zoo") and the palatal approximant (the "y" in the English word "yes"). Others are the central fricatives , the central approximants , the trills , and the central flaps .
From there it flows east-northeast through the semi-arid foothills of the Coast Ranges past Henleyville, Richfield and Tehama to join the Sacramento River at river mile 226 (km 364). The upper watershed is rugged, mountainous and highly prone to flooding and landslides. The highest point in the watershed is the summit of Mount Linn (South Yolla Bolly Mountain) at in the Yolla Bolly-Middle Eel Wilderness. The lower part of the creek flows over a wide cobbled alluvial bed composed of coarse gravel and large boulders.
Another waterfall, which is on the opposite side of the valley and joins Sulphide Creek Falls at its base, should not be confused with Sulphide Creek Falls. This falls is much more visible, but only about one-half as high as Sulphide Creek Falls. This falls is sometimes referred to as Sulphide Valley Falls. Above Sulphide Lake is a further of cascades, informally referred to as Sulphide Basin Falls, flowing from the Sulphide and Crystal Glaciers, which provide most of the water that flows over Sulphide Creek Falls.
Despite the rarity of the species, and the lack of information about the Appalachian elktoe, their habitat is very easily described because of the similarity to that of other species of freshwater mussels. Alasmidonta raveneliana is found mostly in shallow to medium-sized creeks or rivers. They prefer cooler temperature water with fast-flowing to moderately-flowing currents. They are found near sections of the water where there is more rock or gravel at the bottom, as opposed to water that flows over areas with clay or silt on the bottom.
She drapes herself over an altar she has created to Lorenzo from an elaborately inlaid prie-dieu over which a richly embroidered cloth has been placed. On the cloth is the majolica pot, decorated with skulls, in which Lorenzo's head is interred. Her abundant hair flows over the pot and around the flourishing plant, reflecting Keats's words that Isabella "hung over her sweet Basil evermore,/And moistened it with tears unto the core." Behind her, next to the doorway, are a pair of pattens, next to the edge of a cassone.
Coastal areas can be significantly flooded as the result of tsunami waves which propagate through the ocean as the result of the displacement of a significant body of water through earthquakes, landslides, volcanic eruptions and glacier calvings. There is also evidence to suggest that significant tsunami have been caused in the past by meteor impact into the ocean. Tsunami waves are so destructive due to the velocity of the approaching waves, the height of the waves when they reach land and the debris the water entrains as it flows over land can cause further damage.
The Marina Bay Sands SkyPark Infinity Pool in Singapore, viewed from the poolside The Infinity Pool at Kerry Hotel Hong Kong An infinity pool or infinity edge pool is a reflecting or swimming pool where the water flows over one or more edges, producing a visual effect of water with no boundary. Such pools are often designed so that the edge appears to merge with a larger body of water such as the ocean, or with the sky. They are often seen at resorts, estates, and in other luxurious places.
In many countries, it is now a legal requirement to build fish ladders into the design of a weir that ensure that fish can bypass the barriers and access upstream habitats. Unlike dams, weirs do not usually prevent downstream fish migration (as water flows over the top and allows fish to bypass the structure in that water), although they can create flow conditions that injure juvenile fish. Recent studies suggest that navigation locks have also potential to provide increased access for a range of biota, including poor swimmers.
The eruptions from the field were accompanied by a slight sinking of the older rock surface. This shallow, graben-like sink is about 3 kilometers wide and extends to the south into an old lake basin. Crack-in-the- Ground marks the western edge of this small, volcano-tectonic depression and is nearly 9 meters deep and over a meter wide. The crack is the result of a tension fracture along a hingeline produced by the draping of Green Mountain lava flows over the edge of upthrown side of the concealed fault zone.
The column effluent flows over one of the resistors while the reference flow is over a second resistor in the four-resistor circuit. TCD schematic A schematic of a classic thermal conductivity detector design utilizing a Wheatstone bridge circuit is shown. The reference flow across resistor 4 of the circuit compensates for drift due to flow or temperature fluctuations. Changes in the thermal conductivity of the column effluent flow across resistor 3 will result in a temperature change of the resistor and therefore a resistance change which can be measured as a signal.
Bridal Veil Falls is a 45-foot (20.1 m) waterfall located in the Nantahala National Forest, southeast of Franklin. With a short curve of roadway located behind the falls, it has the distinction of being the only waterfall in the state that one can drive a vehicle under. Bridal Veil Falls flows on a tributary of the Cullasaja River through the Nantahala National Forest. The falls flows over an overhanging bluff that allows visitors to walk behind the falls and remain dry when the water flow is low.
The tract is located approximately ten miles from the end of limited access on Georgia 400 in Cumming. An area of previously occupied by GNAL was restricted following 1978 testing which found residual nuclear radiation from the experiments performed there. Subsequent studies in 1991 and 1997 found radiation levels to be at or slightly above normal background radiation levels. The property also encompasses Amicalola Creek, which various groups are lobbying to be designated as a scenic river, and which flows over Amicalola Falls within Amicalola Falls State Park.
Bathtub Rocks is an area owned by the Nature Conservancy that lies within the J.T. Nickel Family Nature and Wildlife Preserve. Cold, fresh water flows over the rocks from a nearby spring before draining into Cedar Creek, a tributary of the Illinois River. The rocks can be visited by the public, and are accessible from any of three trails in the Nickel Preserve. In the last few years vandalism and littering have become more than a nuisance in this area, costing the Nature Conservancy scarce funds to try to keep the area clean for visitors.
From the oldest formations in the north as represented by Serie Tilitos ad Serie Produtiva with coal seams (Beaufort), sedimentation progressed continuously to fossiliferous sandstones, often cross-bedded, including clay-marly beds (Stromberg) - which closed the Karroo sedimentation. Volcanic formation of Stromberg Series consists of amygdaloid basalts plates in the form of lava flows over Karroo sandstones, and dolerite in the form of dykes. Post-Karroo deposits are commonly represented by sandstones and conglomerates with interstratified Mesozoic or younger volcanic rocks. In the Monte Muambe region they are recognized as rocks of Lupata Series.
Care work of a volunteer Today, there are four parts of the economy: Business, Household, Public, and Non-profit. Typically, we only think that the business sector creates any wealth, and that the other three serve the business sector and alongside it. The truth is that all four parts of the economy generate wealth, and that wealth flows over into other sections of the economy as well. Part of the reason that unpaid care work is largely ignored is because of this belief that the household does not form wealth.
Aliso Creek flows over highly erosive marine sedimentary rock of late Eocene to Pliocene age. What would become the Aliso Creek watershed originally lay at the bottom of the Pacific Ocean, before being uplifted as recently as 10 million years ago. About 1.2 million years ago, the San Joaquin Hills began to uplift in the path of Aliso Creek. Occasionally swollen by wetter climates during glacial periods, the creek carved the deep water gap known today as Aliso Canyon, the main feature of Aliso and Wood Canyons Wilderness Park.
The valley is drained via the Bodenbach, which flows over the Tschauko waterfall in the Tscheppa Gorge. Having one of the most beautiful valley closures of the Limestone Alps, the formerly agricultural 4 km-long mountain valley has developed into a popular leisure area. In summer there is hiking – for example in the nature reserve or to the Klagenfurter Hütte mountain hut. In winter, the valley is one of the few winter sport regions of the Karavanks with ski slope, cross-country skiing, winter hiking and sleigh riding.
It is notable for being the only equestrian monument in Cincinnati. The monument originally faced East toward Vine Street but was moved in 1988 to its present location. Flanking Race Street in Piatt Park are two circular reflecting pools with granite slabs that mirror the surrounding urban landscape. Beneath a curtain of water that flows over the granite surfaces are carved symbols for water, air and land. Cincinnati artist Stuart Fink’s fountain was dedicated in 1989 in memory of local delicatessen owner Isadore “Izzy” Kadetz, who died in 1983.
Rogie Falls The Black Water (Scottish Gaelic: An t-Alltan Dubh) is a river in the Highlands of Scotland. It begins at the confluence of the Glascarnoch River with the Abhainn Srath a' Bhàthaich, near where it is crossed by the Black Bridge, carrying the A835 road. It flows in a south-easterly direction past the village of Garve, then passing through Loch Garve and Loch na Cròic, and around Eilean nan Daraich. It flows over Rogie Falls, then past Contin, around Contin Island, before flowing into the River Conon near Moy Bridge.
460 From Lake Coeur d'Alene, the Spokane River traverses the Rathdrum Prairie until reaching Post Falls, Idaho where it passes over a dam, and a natural 40-foot waterfall. Continuing westward it passes over 6 more dams, three of which (Upriver Dam, Upper Falls Dam, Monroe Street Dam) are located in the city of Spokane. In Spokane, it flows over the Spokane Falls, which are located in the heart of Downtown Spokane, approximately one third of the way down the river's length. About a mile later, the river receives Latah Creek from the southeast.
By shooting the dollhouse and rephotography sequences in-camera, an illusion of time is created by multiple characters crossing through the same space or gestures crossing through multiple rooms. Since Geiser used minimal markers when it came to making the video, much was left to be exposed to the elements. For example, some of the image flows over the border as if they were being produced by a projector on an unfitting screen. This condemns the film a non- traditional frame-by-frame shot, with figures illuminating towards off-screen spaces.
However variations can also be caused by differences in respective fluid temperatures, dissolved matter concentrations and by particulate matter suspended in flows. Examples of particulate suspension intrusions include sediment laden river outflows within oceans, 'short-circuit' sewage sedimentation tank intrusions and turbidity current flows over hypersaline Mediterranean pools. Examples also exist of particulate intrusions caused by the lateral spread of thermals or plumes along planes of neutral buoyancy; such as intrusions containing metalliferous sediments formed from deep ocean hydrothermal vents. Or equally crystal laden intrusions formed by plumes within volcanic magma chambers.
Kaieteur Falls is the world's largest single drop waterfall by the volume of water flowing over it. Located on the Potaro River in the Kaieteur National Park, it sits in a section of the Amazon rainforest included in the Potaro- Siparuni region of Guyana. It is 226 metres (741 ft) high when measured from its plunge over a sandstone and conglomerate cliff to the first break. It then flows over a series of steep cascades that, when included in the measurements, bring the total height to 251 metres (822 ft).
She conjectures that there is an element, wæsse, perhaps Old English, that signifies very specifically "land by a meandering river which floods and drains quickly", and her examples are primarily Midland and northern. This seems to fit the Erewash perfectly. A good example of the meandering character of the river will be seen around Gallows Inn Playing Fields, Ilkeston, where rapid flooding and draining occur frequently. As it meanders through Toton and Long Eaton the river splits into two sections; the main course veers to the east and the relief channel flows over a low weir in a straight southerly direction.
A one-armed man named Vogler built a cabin east of Devil's Peak in the 1880s, later purchased by the Comings family, for whom the location and creek are named today. (They continued to use the cabin until the early 1950s.) The South Fork of the river flows over granite bedrock, with portions of limestone and marble bedrock. The river has eroded the limestone and marble such that it travels underground in several locations. Tributaries on the South Fork include Rocky Creek, Turner Creek, Bixby Creek, Mill Creek, and Lachance Creek, many of them named for former homesteaders like Antare P. Lachance.
From its origin, the river flows south through a medium-density upscale residential neighborhood. The river then enters a culvert running partly under Fenway Golf Course, where it re-surfaces and drains into Fenway Pond. From the pond, the river flows south/southwest past the Heathcote Five Corners intersection from Scarsdale to New Rochelle, eventually ending up in Carpenter Pond.Carpenter's Pond The river flows over the dam at Carpenter Pond, where it widens to an average width of 15 feet and then flows south under the Hutchinson River Parkway and along Pine Brook Boulevard for approximately where it enters Sheldrake Lake.
This was one of the largest areas enclosed in north Shropshire, and although the scheme was more costly and difficult than enclosing some of the dryer areas, the resultant land was more fertile, and so justified the cost. Below the large meander at Ruyton, where a narrow valley cuts through sandstone, the bed flows over boulder clay with some glacial debris, and becomes stony again. The lower section retains some of its natural features, including meanders and riffle- pool sequences, which provide habitat for fish. Much of the upper section has been heavily modified, with the river canalised to improve flow.
It has two branches, the East Onny and West Onny, which converge at Eaton, to the east of Lydham. The River Onny then flows in a south-easterly direction, through Craven Arms and Onibury (a village it gives its name to), before it finally has its confluence with the River Teme just upstream of Ludlow at Bromfield. From White Grit to Bromfield, the river flows over a distance of . Geologically, the Onny has the type section just west of Craven Arms of the Caradoc series of the Ordovician system and there is a trilobite genus Onnia which was first defined here.
The supply of mercury is contained in the reservoir on the left. It flows over into the bulb B, where it forms drops which fall into the long tube on the right. These drops entrap between them the air in B. The mercury which runs out is collected and poured back into reservoir on the left. In this manner practically all the air can be removed from the bulb B, and hence from any vessel R, which may be connected with B. At M is a manometer which indicates the pressure in the vessel R, which is being exhausted.
The small power station is a run-of-river power station in which the water level of the headrace and tailrace canals is the same and the water can only be stored for a short time by closing the overflow or idle gate. When the gate is closed, the water is backed up until it flows over the gates out of wooden panel. In operating mode, the idle channel is closed and the turbine inlet channel is opened. By lifting the turbine inlet gate, the water from the headrace channel can flow through the flotsam screen into the turbine inlet.
Volt-VAR Control or VVC refers to the process of managing voltage levels and reactive power (VAR) throughout the power distribution systems. These two quantities are related, because as reactive power flows over an inductive line (and all lines have some inductance) that line sees a voltage drop. VVC encompasses devices that purposely inject reactive power into the grid to alter the size of that voltage drop, in addition to equipment that more directly controls voltage. In the legacy grid, there are three primary tools for carrying out voltage management: Load Tap Changers (LTCs), voltage regulators, and capacitor banks.
The reaction force of the deflected air mass must then act on the wing to give it an equal and opposite upward component." In: Anderson and Eberhardt (2001)Langewiesche (1944)"When air flows over and under an airfoil inclined at a small angle to its direction, the air is turned from its course. Now, when a body is moving in a uniform speed in a straight line, it requires force to alter either its direction or speed. Therefore, the sails exert a force on the wind and, since action and reaction are equal and opposite, the wind exerts a force on the sails.
Columbine Cascade is a waterfall in Waterfalls Canyon, a part of the Grand Teton National Park in the U.S. state of Wyoming. The cascade drops approximately in Hanging Canyon, fed by an unnamed intermittent stream off a glacial lake. The waterfall also receives snowmelt from Ranger Peak to the north Doane Peak to the southwest and Eagles Rest Peak to the south. Less than upstream, the same unnamed creek flows over another steep section known as Wilderness Falls The peak time for waterflow is during spring snowmelt and the falls are visible across Jackson Lake from the Colter Bay Village area.
The major outflow is also the Madawaska River, which flows over the dam at the Ontario Power Generation Mountain Chute Generating Station (hydroelectric) to Norcan Lake at the southeast. Norcan Lake drains via the Madawaska River to the Ottawa River to the Saint Lawrence River and thence to the Atlantic Ocean. The settlement of Black Donald appears in the Natural Resources Canada Place names database and displays as being located on the southeast shore of the lake at the intersection of Chimo Road South and Far Side Lane. In fact, there is no town of Black Donald, at that location or anywhere else.
Bolds's spectral analysis of aircraft vibration and noise was called "substantial" and "instrumental" in suggesting ways to correct the adverse effects of the severe aeroacoustic environment created by operating high performance aircraft with their weapons bay doors open.Kaufman, I. I., Louis, G., Maciulaitis, A., & Clark, R. L. (1983). Mach 0.6 to 3.0 flows over rectangular cavities (No. AFWAL-TR-82-3112). Air Force Wright Aeronautical Labs, Wright-Patterson AFB, OH. Her work on helicopter vibration frequencies helped to demonstrate that the Helicopter Vibration Test Curve "M" in use in 1970 was inadequate, potentially allowing for many instances of field equipment failure.
The creek's headwaters are at the Grant Lakes (), and it flows southwest to drop over Yosemite Falls to Yosemite Valley, then flows southeast to its mouth at the Merced River, just southwest of Yosemite Village. () The Merced is a tributary of the San Joaquin River, in the San Joaquin Valley. Today, Yosemite Creek flows over the Yosemite Valley rim to create Upper Yosemite Fall. Before its diversion about 130,000 years ago, Yosemite Creek flowed down an older channel just to the west, from which it cascaded down through the steep ravine that is now the route of the Yosemite Falls Trail.
These features are readily noted along the eastern faces of the ridges, which often present mural precipices, or vertical escarpments. Similar features can also be seen in the Palisades Sill, although these were formed within the Earth's crust. Additionally, the Watchungs feature not only blocky aa lava, but also ropey and billowing pahoehoe flows. Water flows over a trap rock surface in the Watchungs The magma which generated the Watchungs and the Palisades also formed the intrusive igneous Sourland Mountain in Central New Jersey, as well as a series of smaller outlying volcanic ridges in the region.
Of the 6 sverdrup (Sv) of dense water that flows southward over the GSR, 3 Sv does so via the Denmark Strait forming Denmark Strait Overflow Water (DSOW). 0.5-1 Sv flows over the Iceland-Faroe ridge and the remaining 2–2.5 Sv returns through the Faroe-Shetland Channel; these two flows form Iceland Scotland Overflow Water (ISOW). The majority of flow over the Faroe-Shetland ridge flows through the Faroe-Bank channel and soon joins that which flowed over the Iceland-Faroe ridge, to flow southward at depth along the Eastern flank of the Reykjanes Ridge.
Valaste Waterfall () is the highest waterfall in Estonia and neighboring regions (30.5 m) situated between Ontika and Valaste in the Toila Parish of the Ida-Viru County and formed by a stream, as it flows over the Baltic Klint not far from the shore of the Gulf of Finland. It is a popular tourist attraction with its spray freezing up in winter. There is a parking lot, some explanatory signs, and a trail using a double spiral staircase to get down the cliff. Opposite of the waterfall, a viewing platform has been built, and this offers views of the falls.
The river leaves the lake via two channels, an eastern channel Moira River and the named West Channel, which enclose Sugar Island. It heads southwest, and is paralleled by Highway 37 from Tweed all the way to Belleville. The river flows through the northwest corner of the township of Tyendinaga and enters the city of Belleville, continuing southeast. It takes in the right tributaries Chrysal Creek and Palliser Creek, flows over the Belleville Yardmen Dam through the former Laziers Dam Site, the McLeod Dam and the Lott Dam and reaches its mouth at the Bay of Quinte, Lake Ontario.
Surveryor's map of the Gananoque River, 1787 The Gananoque River begins at Gananoque Lake in incorporated Leeds and the Thousand Islands township. It flows south, passes through the community of Marble Rock, then turns southwest and reaches the community of Maple Grove. It heads again south, takes in the right tributary Mud Creek, passes under Ontario Highway 401, and enters the town of Gananoque. It then flows over the concrete dam for the Gananoque Generating Station, in service since 1939, and empties into the Saint Lawrence River where that river is part of the Thousand Islands region.
Shale rip-up clasts in a nearshore marine sandstone, Matilija Fm. Topatopa Mountains, California. A giant shale rip-up clast at the base of a high- density turbidite, Cozy Dell Fm. Topatopa Mountains, California. Rip-up clasts are gravel-size pieces of clay or mud created when an erosive current flows over a bed of clay or mud and removes pieces of clayey sediment, and transports them some distance. Because clayey sediments can be quite cohesive, even when freshly deposited, large clasts of clayey sediment can be ripped up, transported and subsequently preserved when the eroding current finally deposits its sediment.
The geology of the river consists of three different rock types. At the top of the river there is the Devonian Quartzite (Metamorphic), in the middle of the river there is the Permo-Triassic Marl (Sedimentary) and the lower part of the river consists of Jurassic Limestone (Sedimentary). The first two rock types are impermeable meaning there is little drainage for the river but the river depth becomes smaller as the water flows over the permeable limestone which will allow water to pass through. Quartzite is also very resistant to chemical weathering and can form ridges.
These territories include present-day Baden-Württemberg and the Cantons of Schaffhausen, Aargau, Basel-land, and Basel-Stadt. Schaffhausen and Aargau attained canton status in the peace settlement of 1803, a de facto acceptance of the Swiss Revolution of 1798-99; Basel-land and Basel-Stadt were created from the Canton Basel in 1833. The stretch between Rheinfall, by Schaffhausen and Basel, called the High Rhine, cuts through steep hillsides and flows over a gravel bed; in such places as the former rapids at Laufenburg, it moved in torrents.Laufenburg now has dams and barrages to control the flow of water.
The Rusk Glacier does not start from the summit ice cap, but starts at below the Roosevelt Cliff and is fed by avalanching snow and ice from the summit cap. It is enclosed on the south by Battlement Ridge and Victory Ridge on the north and terminates at about . It is the source of Rusk Creek, which flows over two waterfalls before joining the Big Muddy on its way to the Klickitat. The Wilson Glacier, like the Rusk Glacier, starts below the Roosevelt Cliff and is fed by avalanching snow and ice; however, the Wilson Glacier starts slightly higher at about .
The river flows over the Millstone Grit outcrop from some way beyond Hepste Bridge.Ordnance Survey Explorer map sheet 12 'Brecon Beacons National Park: western area'British Geological Survey 1:50,000 map no 231 'Merthyr Tydfil' & accompanying memoir The Hepste plunges over a band of resistant gritstone to form Sgwd yr Eira (translated from Welsh as 'fall of snow'). A public footpath runs behind this fall, making it one of the most popular destinations in an area that has become known as Waterfall Country. One mile downstream of the fall, the river joins the Afon Mellte near to the village of Ystradfellte.
The trail also connects to a large network of hiking, running, and mountain biking trail systems stretching eastward into the Sierra Nevada mountain range, near Lake Tahoe. Because the dam is designed so that the river flows over its top, a waterfall is created that grows impressively large in winter and spring when rain and snow melt cause high river flows. Upper Lake Clementine is accessed by car via separate entrance from Lower Lake Clementine or by non-motorized vehicles. Upper Lake Clementine is seasonally opened from May 1 through October 15 from sunrise to thirty minutes before sunset.
One can think of conditioning on conjugate priors as defining a kind of (discrete time) dynamical system: from a given set of hyperparameters, incoming data updates these hyperparameters, so one can see the change in hyperparameters as a kind of "time evolution" of the system, corresponding to "learning". Starting at different points yields different flows over time. This is again analogous with the dynamical system defined by a linear operator, but note that since different samples lead to different inference, this is not simply dependent on time, but rather on data over time. For related approaches, see Recursive Bayesian estimation and Data assimilation.
This river is characterized by cold waters of exceptional clarity, a key factor in ensuring good conditions for salmon fishing. The clarity of the water is caused by the fact that the river flows over a rocky bottom, in places with stones and pebbles. Bonaventure River The economy of the recreational salmon fishery is under the auspices of two organizations that share the exploitation of the salmon resource: "l'Association des pêcheurs sportifs de la Bonaventure" and "Le Club de pêche au saumon « Le Canadien »". In the territory of the ZEC, many water pits are caught fording.
Several attempts were made over the years to remove or demolish the dam, but it proved very sturdy, even to dynamite. The center of the dam top was dislodged by dynamite in the mid 1900s and in the late 80s was concreted over to allow large debris flows over the dam and lessen possible damage. The mill was one of the first homes in the area to have electricity, powered by the dam itself and provided milling services for much of the valley. The mill has undergone several attempts to maintain the structure after several, very destructive storm seasons.
As Araceli's magic flows over him, Darien instructs him to find a pattern which she suspects exists but she is unable to see as she is not of royal blood. Inside Araceli's magic, Nicias discovers incredibly subtle and discreet persuasion magics of the same kind that Lilian used on him to keep him from seeing the evil of Ahnmik. These were woven by Syfka, who had been planning on using Araceli to destroy Cjarsa. In the process Araceli would also have been destroyed and as third in line to the throne, Syfka would have ruled Ahnmik.
The county is home to a number of important buildings and landscapes, including the well-preserved 17th-century city walls of Derry; the National Trust–owned Plantation estate at Springhill; Mussenden Temple on the Atlantic coast; the dikes, artificial coastlines and the bird sanctuaries on the eastern shore of Lough Foyle; and the visitor centre at Bellaghy Bawn, close to the childhood home of Nobel laureate Seamus Heaney. In the centre of the county are the old-growth deciduous forests at Banagher and Ness Wood, where the Burntollet River flows over the highest waterfalls in Northern Ireland.
A broadcrest weir at the Thorp grist mill in Thorp, Washington, USA Commonly, weirs are used to prevent flooding, measure water discharge, and help render rivers more navigable by boat. In some locations, the terms dam and weir are synonymous, but normally there is a clear distinction made between the structures. Usually, a dam is designed specifically to impound water behind a wall, whilst a weir is designed to alter the river flow characteristics. A common distinction between dams and weirs is that water flows over the top (crest) of a weir or underneath it for at least some of its length.
The Dobson River is a river in the South Island of New Zealand. It flows south between the Neumann and Ohau ranges for from its source to the east of Mount Hopkins, in the Southern Alps, before joining with the Hopkins River, close to the latter's entry into the northern end of Lake Ohau in the Mackenzie Country. The river flows over wide shingle beds, and has no rapids of interest to whitewater enthusiasts. It was named by Julius von Haast in the 1860s for his father-in-law, Edward Dobson, who was the Canterbury Provincial Engineer.
Using MGS and Odyssey data, combined with developments in the study of glaciers, scientists suggest that glaciers once existed on Pavonis Mons and probably still do to some extent. Evidence for this includes concentric ridges (moraines "dropped" by glaciers), a knobby area (caused by ice sublimating), and a smooth section that flows over other deposits (debris-covered glacial ice). The ice could have been deposited when the tilt of Mars changed the climate, thereby causing more moisture to be present in the atmosphere. Studies suggest the glaciation happened in the Late Amazonian period, the most recent period in Mars chronology.
When moist, stable air flows over a larger eddie, such as those caused by mountains, a series of large-scale standing waves form on the leeward side of the mountain. If the temperature at the crest of the wave drops below the local dew point, moisture in the air may condense to form lenticular clouds. Under certain conditions, long strings of lenticular clouds may form near the crest of each successive wave, creating a formation known as a "wave cloud". These wave systems can produce large updrafts, occasionally enough for water vapour to condense and produce precipitation.
In the past, load balancing by per-packet multipath routing was generally deprecated due to the impact of rapidly changing latency, packet reordering and maximum transmission unit (MTU) differences within a network flow, which could disrupt the operation of many Internet protocols, most notably TCP and path MTU discovery. RFC 2992 analyzed one particular multipath routing strategy involving the assignment of flows to bins by hashing flow-related data in the packet header, which is designed to avoid these problems by sending all packets from any particular network flow down a single deterministic path, while balancing multiple flows over multiple paths in general.
The falls are situated at the foot of the southern face of Mount Bartle Frere in the Wooroonooran National Park. They descend from the Atherton Tableland at an elevation of above sea level in the range of near a popular recreation site as the water flows over a large rock to form a natural waterslide on Josephine Creek, a tributary of the Russell River. Access to falls is via a sealed road off the Bruce Highway between Babinda and Innisfail. The natural rock slide can be dangerous and the occasional flash flooding occurs without warning, with a sudden increase in the water volume.
The river begins at Big Bob Lake in geographic Paxton Township and flows east, passes briefly through geographic Butt Township and geographic Devine Township, turns north into geographic Biggar Township, then back east, over Stewart's Dam and through the Allen Rapids, and into geographic Osler Township. It continues east over Graham's Dam, the High Falls and Gauthier's Dam, enters geographic Lister Township, flows over the Perley Dam and Rolling Dam, and empties into Cedar Lake on the Petawawa River, across the lake from the community of Brent. The Petawawa flows via the Ottawa River to the Saint Lawrence River.
Urastoma cyprinae is believed to feed on the mucus secreted by its host and its presence alters the protease composition of gills in C. virginica. Urastoma cyprinae is negatively phototatic and is more attracted to oysters when compared to other mollusc species such as mussels and clams. Urastoma cyprinae attaches its anterior end to gill filaments, presumably in a feeding posture, and arches its body back and forth, wagging its posterior end, which bears the terminal orogenital pore, within the mucus that flows over the gills. Ingestion of foods is likely to be driven by the sphincters on the orogenital atrium.
Grand Saline's first settlers were the ancient Caddo Indians and Cherokee Indians tribes who discovered and made use of a large salt prairie south of the town. The Native Americans used evaporated salt from the brine stream that flows over the flats as a commodity they traded for other needed goods. By the mid-nineteenth century, the tribes had been forced out of the area by Mirabeau B. Lamar, second president of the Republic of Texas and by general anti-Indian sentiment and moved southeast. Only a few years after the Indians left the salt prairie behind, a new group of settlers arrived.
Hard rock mining was common in the upper watershed from about 1870 into the 1990s. The upper of the stream is located within the Upper Tenmile Creek National Priorities List, a federal Superfund site about in size. Arsenic, cadmium, copper, lead, nitrate, phosphorus, and zinc are released into the stream when water flows over or through mines or main tailings and reaches Tenmile Creek. At times, water in the creek contains levels of arsenic, cadmium, and lead which exceed State of Montana limits for safe human consumption, and water treatment is needed to render the water safe to drink and use.
Narva Waterfall (eastern part) in spring 2010 Narva Waterwall (1845) Narva Waterfall () is the waterfall on Narva River, Estonia and Russia. Between the southeast part of the city of Narva and the rest, facing the Russian city of Ivangorod, the Narva flows over the Baltic Klint, forming Narva Waterfall, once among the most powerful in Europe. Before the water reaches the falls it is split into two branches by the Kreenholm island, thus the falls consist of two sections. Kreenholm Falls, west of the island, is 60 m wide and 6.5 m high with multiple terraces.
The stream is about long and heads in the mountain mass dominated by Pyramid Peak, from which Chititu Creek, Dan Creek, and Canyon Creek receive much of their waters. The water of Young Creek is derived in part from melting snow and glacier ice, and during the warm summer days is discolored with glacial silt. Young Creek occupies a typical glacial valley of broad U-shaped cross section. The upper part of the stream, formed by the union of two short forks, each a little more than long, flows over a flood plain between low brush-covered gravel benches.
Thus, if the speed of flow is doubled, the flow would dislodge objects with 64 times as much submerged weight. In mountainous torrential zones this can be seen as erosion channels through hard rocks and the creation of sands and gravels from the destruction of larger rocks. A river valley that was created from a U-shaped glaciated valley, can often easily be identified by the V-shaped channel that it has carved. In the middle reaches where a river flows over flatter land, meanders may form through erosion of the river banks and deposition on the inside of bends.
At Buckabank the river flows over a weir that provides a mill stream to the cotton mill and there is a salmon ladder. Flowing under Hawksdale Bridge at Bridge End and Dalston's two other bridges (Jubilee Bridge and the White Bridge) the river then flows towards Cummersdale where another weir used to exist above the now modernised textile mill. In 2016 the floodwaters of the swollen river Caldew washed away the eighteenth-century Bell Bridge at Sebergham. The river enters the suburbs of Carlisle north of Cummersdale flowing over a weir in Denton Holme at the site of a large Victorian mill.
With the headwaters beginning from the Northwestern slopes of Peak Mountain, it flows west to Banner Elk then towards Elk Park. For most of the river's course, it runs in a deep gorge. Just before the Elk River crosses into Tennessee it flows over "Big Falls" (also called "Elk Falls"), a locally-known attraction which is approximately a 60-foot (18 m) drop. It then flows down a narrow, relatively steep valley to the tiny community of Elk Mills, which is named for a former water-powered mill built on this river at this point by early white settlers.
A commercial chocolate fountain in a shop in Brussels, Belgium A chocolate fountain is a device for serving chocolate fondue. Typical examples resemble a stepped cone, standing 2–4 feet tall with a crown at the top and stacked tiers over a basin at the bottom. The basin is heated to keep the chocolate in a liquid state so it can be pulled into a center cylinder then vertically transported to the top of the fountain by an Archimedes screw. From there it flows over the tiers creating a chocolate "waterfall" in which food items like strawberries or marshmallows can be dipped.
Along this section gauges monitor the water levels from the Inniscarra Dam. The river flows over the Lee weir and then is split into the north and south channels at a sluice (it historically occupied the city area as a maze of channels). This area is popular for recreation, kayaking and fishing. The two channels join again at the Cork docks and enter the extensive estuary and harbour, south of Glanmire, passing either side of Great Island (Cobh lies on the south coast) to fill the outer harbour, and reaching the open sea between Whitegate and Crosshaven.
The group watches as a huge torrent of water flows over the salt deposits at the canyon's edge, reaching the monoliths; their growth is finally halted when the last huge formation of monoliths crashes down into the salty water. Dan reveals to the group that he had finally reached the governor who told him not to blow up the dam, pauses, and adds unless Dave was absolutely certain of success. As they all laugh, Dave then comments, first repeating Martin's earlier assertion that the region's salt flat was "Mother Nature's worst mistake", then pointing out, ironically, that this near-disaster has just proved otherwise.
The project garnered broad support from organizations such as the Sierra Club along with the governments of the many cities the rivers pass through. Most of the Rio Hondo is a concrete-lined channel to serve its primary flood control function, but in two places the river flows over open ground: the Peck Road Water Conservation Park, and the Whittier Narrows Recreation Area. Large spreading grounds for water conservation surround much of the river, and its bike paths are very popular. The river passes through the location of the Battle of Rio San Gabriel, fought on January 8, 1847, and which resulted in a U.S. victory.
It very effective for handling hot, dry inlet gases that contain dust, or particles which are abrasive or corrosive, such as kiln or furnace gasses. Wetting of the throat can be achieved with a spray directed at the walls or with a weir encircling the converging section which water flows over. This method can be used only at liquid injection source as the high velocity gas will shear droplets from the walls. Liquid can also be introduced by spray nozzles directly into the gas stream and for low gas flow velocities this may provide more efficient operation, either or both methods may be employed depending on the application.
The Dahla Dam is built on the Arghandab River which flows over a length of . Over the years its reservoir was subject to siltation, and its canal system reduced irrigation benefits. This necessitated undertaking rehabilitation of the dam which involved desiltation works and pertinent components of the project to improve the water delivery system; this component was completed during March 2012 with assistance provided by Canada. The second phase involved raising the height of the dam and the relevant dykes to compensate for the loss of storage in its reservoir due to siltation, and to achieve the full benefits of irrigation for which the dam was originally built.
Vortex lift works by capturing vortices generated from the sharply swept leading edge of the wing. The vortex, formed roughly parallel to the leading edge of the wing, is trapped by the airflow and remains fixed to the upper surface of the wing. As the air flows around the leading edge, it flows over the trapped vortex and is pulled in and down to generate the lift. A straight, or moderate sweep, wing may experience, depending on its airfoil section, a leading-edge stall and loss of lift, as a result of flow separation at the leading edgeDesign For Air Combat, Ray Whitford 1987, , p.
Its course traverses deep sedimentary basins flanked by the Huachuca, Mule, Whetstone, Dragoon, Rincon, Little Rincon, Winchester, Galiuro, Tortilla, and Santa Catalina Mountains. The San Pedro is fed by numerous tributaries, which in general, drain relatively short and steep catchments oriented more or less perpendicular to the mainstem. For most of its length the San Pedro flows over sedimentary basin fill deposits, although it is bound by bedrock at the Tombstone Hills at Charleston and near Fairbank, “the Narrows” south of Cascabel, near Redington, and again at Dudleyville (Heindl, 1952). Two major tributaries, Babocomari River and Aravaipa Creek, each have extensive bedrock-lined stretches.
As the temperature drops, the two slowly embrace for warmth and gradually begin to have sex, Randy assuring her that he will keep an eye on the creature. However, he is distracted by pleasure and, when LaVerne's hair falls over the side of the raft, the creature tangles itself in her hair and flows over her face. Knowing he will be unable to save her, he kicks her over the side of the raft in a panic, quickening her death. Randy barely gets any sleep as night falls, since the creature flows under the raft every time Randy tries to sit down, forcing him to remain permanently standing.
It differs from Wi-Fi calling; there remains a control channel using LTE, but all data (not just phone calls) flows over the unlicensed 5 GHz band, instead of the carrier's frequencies. In 2014, the LTE-U Forum was created by Verizon, in conjunction with Alcatel-Lucent, Ericsson, Qualcomm, and Samsung as members. The forum collaborates and creates technical specifications for base stations and consumer devices passing LTE-U on the unlicensed 5 GHz band, as well as coexistence specs to handle traffic contention with existing Wi-Fi devices. T-Mobile and Verizon Wireless have indicated early interest in deploying such a system as soon as 2016.
The Wesachewan River is a short river in the Hudson Bay drainage basin in Census Division No. 22 - Thompson-North Central, Northern Region, Manitoba, Canada. It flows out of Vermilyea Lake via twin channels which combine at , then flows over the Namaykos Rapids, and empties into Wesachewan Bay on Gods Lake. The main channel from Vermilyea Lake is the east channel, given as the primary source in the Infobox at right, which is straighter and shorter than its twin ( versus ), the west channel, given as the secondary source. The length of the river given in the Infobox is the length using the shorter east channel.
The second context explains ganying "cosmic resonance" with examples of bingwu burning- mirrors, moon-mirrors, and tulong 土龍 "clay dragons" believed analogously to cause rainfall like Chinese long dragons. It describes a dispute between Han astronomer Liu Xin, who used a clay dragon in a rain sacrifice, but could not explain the reason why it worked, when the scholar Huan Tan argued that only a genuine lodestone can attract needles. > The objection that the dragon was not genuine, is all right, but it is wrong > not to insist on relationship. When an east wind blows, wine flows over, and > [when a whale dies, a comet appears.
The river again reaches (and forms) the Putnam-White county line before entering Burgess Falls Lake, a reservoir built in the early 1920s to provide electricity for Cookeville. The river passes under State Highway 135 just upstream from the reservoir's dam. Beyond the dam, the river enters a gorge and flows over a series of three waterfalls, culminating in the 136-foot Burgess Falls, as it drops from the Highland Rim to the Nashville Basin. At the base of Burgess Falls, the river enters Center Hill Lake, an impoundment of the Caney Fork created by the U.S. Army Corps of Engineers' Center Hill Dam.
The Vyrnwy dam is high from the bottom of the valley, and thick at the base; it is long and has a road bridge running along the top. It is decorated with over 25 arches and two small towers each with four corner turrets rising above the road surface. The dam was the first to carry water over its crest instead of in a channel at the side. At the bottom of the dam is a body of water known as a stilling basin necessary to absorb the energy when the water flows over the crest and into the valley, and to stop the water eroding the foundations of the dam.
The Johnstone River, comprising the North Johnstone River and the South Johnstone River, is a river system located in Far North and North Queensland, Australia. The headwaters of the river system rise in the Atherton Tablelands. The north branch of the river system rises below Merivale, flows over the Malanda Falls and through the town of and then flows generally south by east, around Francis Range and over the Jones Falls, before flowing east, covering a distance of . The south branch of the river system rises below Mount Father Clancy and generally flows east over Binda Falls, through the settlement of , before flowing north, covering a distance of .
A new hypothesis for the function of the horns was presented by South African paleontologist Arthur Cruickshank & fluid dynamicist B.W. Skews in a 1980 paper. They proposed that the tabular horns acted as a hydrofoil, allowing the animal to more easily control how water flows over its head. In the process of their investigation, Cruickshank & Skews developed a full-scale model of the head and a portion of the body of a Diplocaulus, constructed from balsa wood and modelling clay. The model was placed in a wind tunnel, and subjected to several tests to determine drag, lift, and other forces experienced by the head in different situations.
The mixed snow melt-rainfall rivers of the Snowy Mountains can be defined by strong seasonal patterns and remain permanent throughout the year, with no record of zero flow ever observed in the Lower Snowy. Prolonged base flows over the summer months are another feature of these types of rivers, driven by snowmelt derived groundwater. In the lower reaches of the Snowy River catchment, the larger tributaries have a distinctly different flow regime to the snow melt rivers of the Alps. These tributaries are typically dominated by the winter rainfall and often have peak monthly flows a few months earlier than the snow melt tributaries.
The name of the city comes from the French word dalle, meaning either "sluice", akin to English "dale" and German T[h]al, "valley", or "flagstone", referring to the columnar basalt rocks carved by the river (in voyageur French used to refer to rapids), which was used by the French- Canadian employees of the North West Company to refer to the rapids of the Columbia River between the present-day city and Celilo Falls. Also in the same area was the Petite Dalles or Little Dalles, or Short Narrows. In French, "Les dalles" means "The slabs". When a river flows over hard flat rocks, it becomes shallow, and rapids are created.
Between Chesterfield and Tapton, the river flows over a large weir while the canal is protected from flooding by a flood gate. The two waterways remain close as they flow northwards between New Whittington and Brimington, where the River Drone joins from the west. At Old Whittington both turn to the east, before turning north again at Staveley. Just before Renishaw, the river passes Slittingmill Farm, once the site of a slitting mill constructed by George Sitwell in the 1650s, used to split iron bars from his furnaces into thin strips for the production of nails, and the first to be constructed in the East Midlands.
Initiation of volcanism at Coso preceded the onset of Basin and Range crustal extension there, as expressed by normal faulting. The earlier of the two principal periods of volcanism began with the emplacement of basalt flows over a surface of little relief. Then, during the ensuing period of approximately 1.5 million years, eruptive activity included chemically more evolved rocks erupted upon a faulted terrain of substantial relief. Following a 1.5-million-year hiatus with few eruptions, a bimodal volcanic field of basalt lava flows and rhyolite lava domes and flows developed on Basin and Range terrain of essentially the same form as today's landscape.
The Sturgeon river begins at an unnamed spring between the Simcoe Highlands and the western edge of the Oro Moraine, and just west of the community of Horseshoe Valley in Oro-Medonte. It passes north through Craigs Swamp, then under Ontario Highway 400 and into Springwater southeast of the community of Hillsdale. It flows over Rumbles Dam and re- enters Oro-Medonte. The river continues north, passes under Simcoe County Road 23 into Tay, then passes under Ontario Highway 12 and through the communities of Sturgeon Bay and Sturgeon Beach to reach its mouth at Sturgeon Bay on Severn Sound, part of Georgian Bay on Lake Huron.
Such a spillway can be used to regulate downstream flows – by releasing water in small amounts before the reservoir is full, operators can prevent sudden large releases that would happen if the dam were overtopped. Other uses of the term "spillway" include bypasses of dams or outlets of channels used during high water, and outlet channels carved through natural dams such as moraines. Water normally flows over a spillway only during flood periods – when the reservoir cannot hold the excess of water entering the reservoir over the amount used. In contrast, an intake tower is a structure used to release water on a regular basis for water supply, hydroelectricity generation, etc.
The history of the Bärenbrucher Teich goes back to 1634. The water of the Bärenbrucher Teich can be channelled along the Bärenbruch Ditch (Bärenbrucher Wasserlauf), laid in 1948, through a sequence of six water tunnels and intermediate ditches to the Rosenhof, where it was used to supply power to the Rosenhof Pit and, later, the Ottiliae Shaft Power Station. Another drainage outlet is the normal bottom outlet, which discharges water into the Ziegenberger Teich located immediately below it. Today the Bärenbrucher Teich is normally operated as a spillway basin, that is, the bottom outlets are closed and water simply flows over the spillway into the Ziegenberger Teich.
When air flows over a swept wing, it encounters a force towards the wing tip. At high speeds, this force is too small to have an effect before the air is past the wing. At lower speeds, this sideways motion becomes more evident, and as the sideways motion pushes on the air outboard of it, this spanwise flow becomes more and more noticeable towards the wing tips. At very low speeds, the flow can become so sideways that the front-to-back flow, which is what gives rise to lift, is no longer above the stall speed of the airfoil, and the wing tips may stall.
Lake Hackett (Mekinac) has a length of 4.8 km in the north-south axis (and a maximum width of 1.7 km), including the long strait in the southern part, resulting into the "Lac du Canard" (Duck Lake) which as a large area consisting of marshes. The headwaters of the subwatershed is Calau lake (1 km long) which flows to the north-east into the Suève lake (710 m long). The discharge of the later flows over 1.25 km to the northeast and empties into "Lac du Canard". A strait of 2.8 km at northeast (which forms the lake logic) connects the Hackett Lake to Garneau Lake (2.6 km long, shaped like a "U").
20 There were two primary crossings of the Little Colorado—one at the Grand Falls, and one at Black Falls, a smaller waterfall some downstream. It was easier to ford the river at the two waterfalls because at that point, it flows over hard bedrock, making the crossing much easier. The Mormons also made many attempts to construct dams on the river to provide irrigation water—as far upstream as the confluence of the river's forks and as far downstream as below Grand Falls—but most of them failed because of the Little Colorado's fickle variations in discharge. Finally, they managed to construct one at Joseph City that lasted for 29 years.
Shoshone Falls () is a waterfall on the Snake River in southern Idaho, United States, approximately northeast of the city of Twin Falls. Sometimes called the "Niagara of the West," Shoshone Falls is high— higher than Niagara Falls—and flows over a rim nearly wide. Formed by the cataclysmic outburst flooding of Lake Bonneville during the Pleistocene ice age about 14,000 years ago, Shoshone Falls marks the historical upper limit of fish migration (including salmon) in the Snake River, and was an important fishing and trading place for Native Americans. The falls were documented by Europeans as early as the 1840s; despite the isolated location, it became a tourist attraction starting in the 1860s.
The Chulym () is a river in the endorheic drainage basin of Lake Chany in the southeastern part of the West Siberian Plain in Russia. The river is long, with a drainage basin of . The Chulym is formed by several tributaries in the Toyskoye Zaymishche (Russian: Тойское Займище) and Troshinskoye Zaymishche (Russian: Трошинское Займище) swamps north of Baraba Steppe, some northwest of Novosibirsk, at an elevation of . The river flows over the Baraba Steppe in a southwesterly direction, and flows through the lakes of Sargul (Russian: Саргуль), , and Uryum (Russian: Урюм), , before it finally terminates, at elevation, in Lake Malye Chany (Russian: Малые Чаны - Little Chany), which is connected to Lake Chany through a short strait.
When fluid flows over a surface which diverts it upward, this flow can rise above the rest of the fluid in a standing wave which remains in one place while the flow lasts. An example of a natural standing wave may be found in swift-flowing streams, downstream from a boulder in the stream bed. Artificial reefs can also be placed into natural wave environments to enhance the quality of the incoming breaking wave for surfing. Wave focusing areas can build up wave power and height prior to breaking, and breaking surfaces then trip the wave up to make it break; the surfing surface then carries the breaking wave along an angle that maximises its value for surfing.
The race offers a free Derby entry to the winner and had been upgraded to Listed status in 2018. John Gosden trained the winner of the race for a sixth time with Crossed Baton, who took an early lead and held on in the final furlong to beat My Lord And Master by a head. The colt was already entered for the Derby and Gosden commented "If we get a hot summer he could be back [for the Derby]...he's a big boy but with not the biggest feet and he flows over faster ground." On 27 April the Bet365 Classic Trial at Sandown Park produced a second trial winner for John Gosden.
The liberated nitric oxide is sparingly soluble in water, and returns to the gas in the chamber where it reacts with oxygen in the air to reform nitrogen dioxide. Some percentage of the nitrogen oxides is sequestered in the reaction liquor as nitrosylsulfuric acid and as nitric acid, so fresh nitric oxide must be added as the process proceeds. Later versions of chamber plants included a high-temperature Glover tower to recover the nitrogen oxides from the chamber liquor, while concentrating the chamber acid to as much as 78% H2SO4. Exhaust gases from the chambers are scrubbed by passing them into a tower, through which some of the Glover acid flows over broken tile.
Spanwise flow of the boundary layer When a swept wing travels at high speed, the airflow has little time to react and simply flows over the wing almost straight from front to back. At lower speeds the air does have time to react, and is pushed spanwise by the angled leading edge, towards the wing tip. At the wing root, by the fuselage, this has little noticeable effect, but as one moves towards the wingtip the airflow is pushed spanwise not only by the leading edge, but the spanwise moving air beside it. At the tip the airflow is moving along the wing instead of over it, a problem known as spanwise flow.
The Forks River begins at Forks Lake in the northwest of the Unorganized West Part of Timiskaming District at an elevation of and exits east to Lower Forks Lake. Portions of both lakes lie in the northeastern portion of the Unorganized, North Part of Sudbury District, meaning that the Forks River drainage basin is in three Ontario districts. It heads northeast, then north, flows over a small dam, and takes in the left tributary Little Forks Creek arriving from Little Forks Lake. The river turns northwest, then curves back northeast, flows into the city of Timmins in Cochrane District, and reaches its mouth at St. Peter Bay at the southern tip of Night Hawk Lake at an elevation of .
The Northern Hemisphere and the Southern Hemisphere each have a polar jet and a subtropical jet. The northern hemisphere polar jet flows over the middle to northern latitudes of North America, Europe, and Asia and their intervening oceans, while the southern hemisphere polar jet mostly circles Antarctica all year round. The southern hemisphere mid-latitude jet is a relatively narrow band of strong winds stretching from the Earth's surface to the top of the troposphere at about 12 km increasing steadily in strength with height. Jet streams are the product of two factors: the atmospheric heating by solar radiation that produces the large-scale Polar, Ferrel, and Hadley circulation cells, and the action of the Coriolis force acting on those moving masses.
Geological Survey of Ireland (GSI) regard the valley as a "stunning example of a glaciated U-shaped valley, with oversteepened cliff sides and a flat floor". The valley dates from the last glacial period called the quaternary glaciation or Ice Age, and contains moraines marking the positions of the ice-front as it retreated back towards the source area higher up in the centre of the Wicklow mountains. The GSI highlight an impressive moraine about halfway between the waterfall and Laragh and can be seen as a boulder-strewn mound running right across the valley. Glenmacnass Waterfall flows over grey-colored, smooth porphyritic granite bedrock (part of the Lugnaquilla pluton, which is itself from the late-Caledonian (405 Ma) Leinster Granite Batholith Formation).
Most of the rocks underlying the Snake River Plain originated from massive lava flows related to eruptions of the Yellowstone hotspot over many millions of years. Shoshone Falls flows over a 6-million-year-old rhyolite or trachyte lava flow that intersects the weaker basalt layers comprising the surrounding Snake River Plain, creating a natural knickpoint that resists water erosion. The falls themselves were created quite suddenly during the cataclysmic Bonneville Flood at the end of the Pleistocene ice age about 14,500–17,500 years ago, when pluvial Lake Bonneville, an immense freshwater lake that covered much of the Great Basin, overflowed through Red Rock Pass into the Snake River. About of water were released–1500 times the average annual flow of the Snake River at Twin Falls.
Banganga Temple shikhara According to local legend, it sprang forth when the Lord Rama, the exiled hero of the epic Ramayana, stopped at the spot in search of his kidnapped wife Sita. As the legend goes, overcome with fatigue and thirst, Rama asked his brother Lakshmana to bring him some water. Laxman instantly shot an arrow into the ground, and water gushed forth from the ground, creating a tributary of the Ganges, which flows over a thousand miles away, hence its name, Banganga, the Ganga created by a baan (arrow).Destinations in Mumbai The Banganga also houses the 'Shri Kashi Math' and 'Shri Kaivalya or Kavale Math' of the Goud Saraswat Brahmins at its banks and samadhis of their various past heads of the Math.
Principal tributaries of the Redwood River include Coon Creek, 37 miles (60 km) long, which flows from Lake Benton in Lincoln County westwardly to Russell in Lyon County; Three Mile Creek, 50 miles (81 km) long, which rises in Lincoln County and flows northeastwardly and southeastwardly through Lyon County, joining the Redwood downstream of Marshall; and Ramsey Creek, 10 miles (16 km) long, which flows over a waterfall in Ramsey City Park in Redwood Falls. Approximately 82% of the land in the Redwood River watershed is used for agriculture, primarily for the cultivation of corn and soybeans. Hundreds of miles of streams in the watershed have been converted to agricultural ditches, disrupting habitat and reducing the ability of the land to absorb flooding.
The height of the Alps is sufficient to divide the weather patterns in Europe into a wet north and a dry south because moisture is sucked from the air as it flows over the high peaks.Fleming (2000), 3 The Aletsch Glacier with pine trees growing on the hillside (2007; the surface is lower than 150 years ago) The severe weather in the Alps has been studied since the 18th century; particularly the weather patterns such as the seasonal foehn wind. Numerous weather stations were placed in the mountains early in the early 20th century, providing continuous data for climatologists.Ceben (1998), 22–24 Some of the valleys are quite arid such as the Aosta valley in Italy, the Maurienne in France, the Valais in Switzerland, and northern Tyrol.
Kastane is a short traditional ceremonial/decorative single-edged Sri Lankan sword. Kastanes often have elaborate hilts, especially shaped and described as a rich mythical style inherited from Buddhism in blending a variety of Icons including, Lions, Kirtimukha Serapendiya, Nagas, crocodile/human monsters and other dragon and gargoyle like effigies. Some appear seemingly emitted onto the hand guard and cross guard with Vajra style pseudo-quillons whose finials are also decorated by minor monsters and a rain-guard decorated by the Makara or Serapendiya peacock tail or fish scales which occasionally flows over and onto the blade at the throat. The scabbard is occasionally seen with a miniature beasts head at the chape also emitting an icon or cloud pattern.
The eastern areas of the Western Ghats do not receive much rain from this monsoon as the wind does not cross the Western Ghats. The Bay of Bengal Branch of Southwest Monsoon flows over the Bay of Bengal heading towards northeast India and Bengal, picking up more moisture from the Bay of Bengal. The winds arrive at the Eastern Himalayas with large amounts of rain. Mawsynram, situated on the southern slopes of the Eastern Himalayas in Shillong, India, is one of the wettest places on Earth. After the arrival at the Eastern Himalayas, the winds turns towards the west, travelling over the Indo-Gangetic Plain at a rate of roughly 1–2 weeks per state, pouring rain all along its way.
A left tributary of the Danube river, the Váh is long, including its Čierny Váh branch. Its two sources, the Biely Váh (White Váh) and the Čierny Váh (Black Váh), are located in the Vysoké Tatry (High Tatras) and Nízke Tatry (Low Tatra) mountains, respectively, and it flows over northern and western Slovakia and finally feeds into the Danube near Komárno. The left tributaries are Demänovka, Revúca, Ľubochnianka, Turiec, Rajčanka and Nitra rivers, and the right tributaries are Belá, Orava, Varínka, Kysuca, Biela voda, Vlára, Dubová, Dudváh and Malý Dunaj rivers. In late medieval time it was a property of Stibor of Stiboricz and his son Stibor of Beckov of the Clan of Ostoja, later passing to Maurice Benyovszky as a gift of Maria Theresa.
Just past Metcalf Bottoms, Little River becomes more rapid and volatile as it slices through Little River Gorge, a narrow valley between Round Top Mountain and Curry She Mountain. Among the gorge's more notable landmarks is an area known as "The Sinks." The Sinks is where the river flows over a ten-foot (three meters) waterfall into a large pool, and then seems to disappear for a small distance. (Unlike streams in a limestone area, which may actually "sink" for a considerable distance, this is more a question of appearance than of the stream truly "sinking", which is not feasible in this area of ancient Precambrian metamorphic rock.) Below the Sinks, Little River is navigable in high water with a canoe or kayak.
Underlying the Arbuckle Mountains is the Arbuckle-Simpson aquifer, housing freshwater which emanates at springs to provide the base flows of the Blue River and Honey Creek, which flows over Turner Falls south of Davis. As a result of the karst topography, standing water is rarely found atop the Arbuckle Mountains, the water seeps through fractures and planes of separation in the limestone bedrock, dissolving the rock to produce a network of caves and solution conduits throughout the limestone formations. Organizations such as the Arbuckle Karst Conservancy and Arbuckle Mountains Grotto of the National Speleological Society actively study the karst features of the Arbuckle Mountains to preserve the biological ecosystems and groundwater resources. The organizations currently maintain databases of more than 1,000 caves and springs in the Arbuckle Mountains.
The Mole catchment area includes twelve Sites of Special Scientific Interest (SSSIs) that include wetland habitats, The Mole Gap forms part of a Special Area of Conservation and is an SSSI of European importance. The stretch of river between Thorncroft Manor ( south of Leatherhead) and River Lane in Fetcham has been designated a Local Nature Reserve. Although much of the surrounding land has been taken by residential and commercial development, this section of the Mole supports 20 different mammal species, 20 butterfly species and 15 species of dragonfly. The geology of the local area is complex, since the river leaves the chalk of the Mole Gap at this point and flows over gravel and clay, creating a patchwork of different habitats including scrub, woodland, hedges, banks, and meadows as well as the water itself.
When water flows over a dam spillway, the irregularities on the spillway surface will cause small areas of flow separation in a high-speed flow, and, in these regions, the pressure will be lowered. If the flow velocities are high enough the pressure may fall to below the local vapor pressure of the water and vapor bubbles will form. When these are carried downstream into a high pressure region the bubbles collapse giving rise to high pressures and possible cavitation damage. Experimental investigations show that the damage on concrete chute and tunnel spillways can start at clear water flow velocities of between , and, up to flow velocities of , it may be possible to protect the surface by streamlining the boundaries, improving the surface finishes or using resistant materials.
The river begins at the outflow of an unnamed lake at an elevation of and flows west into Sussex Lake, then north to Muskox Lake, at the border between the Northwest Territories and the Kivalliq Region, Nunavut, where it takes in the left tributary Icy River. It flows over the Muskox Rapids, takes in the left tributary Contwoyto River, and heads east through the Heywood Range. The Back River heads over the Malley Rapids, takes in the left tributary Siorak River and enters the long lake-expansion Lake Beechey in a southeast direction. It heads east, takes in the right tributary Baillie River, left tributary Warren River, right tributary Jervoise River, passes over the Hawk Rapids, takes in the right tributary McKinley River and right tributary Consul River.
Urbanization has major effects on erosion processes—first by denuding the land of vegetative cover, altering drainage patterns, and compacting the soil during construction; and next by covering the land in an impermeable layer of asphalt or concrete that increases the amount of surface runoff and increases surface wind speeds. Much of the sediment carried in runoff from urban areas (especially roads) is highly contaminated with fuel, oil, and other chemicals. This increased runoff, in addition to eroding and degrading the land that it flows over, also causes major disruption to surrounding watersheds by altering the volume and rate of water that flows through them, and filling them with chemically polluted sedimentation. The increased flow of water through local waterways also causes a large increase in the rate of bank erosion.
At 30 miles in length, the River Frome is only half the length of the Stour, however unlike the Stour, the Frome lies wholly within the county boundary, rising in the village of Evershot on the Dorset Downs, and entering the English Channel through Poole Harbour. Its catchment area is 181 square miles, or one sixth of the county. It also differs from the Stour in that in its upper reaches it is a chalk stream, and even when it leaves the chalk and flows over acid sands and gravels east of Dorchester, its load of sediment from the chalk is sufficient to counteract the acidity and create fertile pasture and watermeadows.Wightman, R.,"Portrait Of Dorset", Hale, 1983, p11 The main tributaries of the Frome are the River Hooke and River Cerne.
The river begins at Powderhorn Lake and flows southwest to Raven Lake, then passes under Ontario Highway 35 and into the municipality of Lake of Bays, District Municipality of Muskoka. It continues southwest into Minden Hills, Haliburton County, then back into Muskoka District in the municipality of Bracebridge, passes under Ontario Highway 118 and flows by the community of Vankoughnet, and enters the city of Kawartha Lakes. The river turns west, flows over the Ragged Rapids, exits Kawartha Lakes, briefly forms the border between Simcoe County and Muskoka District, flows through the Big Eddy, then reaches the community of Cooper's Falls in the municipality of Ramara, Simcoe County. It turns south, then heads west, takes in the left tributary Head River, turns north, and reaches its mouth at the Severn River's easternmost outflow from the latter river's source at Lake Couchiching.
The effective tension caused by the contrast of "thou launchest navies of full-freighted worlds" and "there's that in here that still remains indifferent" in "The Candles" (Ch. 119) makes the last clause lead to a "compulsion to strike the breast," which suggests "how thoroughly the drama has come to inhere in the words;" Second, Melville took advantage of the Shakespearean energy of verbal compounds, as in "full-freighted". Third, Melville employed the device of making one part of speech act as another, for example, 'earthquake' as an adjective, or turning an adjective into a noun, as in "placeless". Melville's style, in Nathalia Wright's analysis, seamlessly flows over into theme, because all these borrowings have an artistic purpose, which is to suggest an appearance "larger and more significant than life" for characters and themes that are in fact unremarkable.
It exits the lake from Crowe River Bay to the east over Belmont Dam to Crowe Lake, where it once again enters Marmora and Lake township, takes in the major left tributary Beaver Creek, and reaches the community of Marmora on Ontario Highway 7. There, the Crowe River passes over Marmora Dam, heads southwest into the township of Stirling-Rawdon, passes over two one-metre (3 ft 3 in)-high and -wide falls at Callaghan's Rapids Conservation Area, enters the municipality of Trent Hills in Northumberland County, flows over Allan Mills dam, passes over several falls at Crow Bridge Conservation Area, and reaches its mouth at Crowe Bay on the Trent River, just upstream of the Trent–Severn Waterway Crowe Bay lock and dam. The Trent River flows to the Bay of Quinte on Lake Ontario at Trenton.
Hydroelectric dam near the mouth of the Sault aux Cochons River in Forestville (upstream view). The Sault aux Cochons River has its source in Breault Lake, south of Pipmuacan Reservoir. It then flows in a southwesterly direction and crosses Sault aux Cochons Lake halfway through. It flows over a length of according to the Commission de toponymie du Québec or of according to the Organisme des basins versants de la Haute-Côte-Nord to flow into the St. Lawrence River at Forestville.. The fifteen kilometer downstream of Sault aux Cochons Lake is encased in a canyon.. The area of its watershed is .. The wetlands cover .. In 2003, a portion of the waters of the Sault aux Cochons River was diverted to the Pipmuacan reservoir by the Lionnet River in order to increase the capacity of the power stations Bersimis-1 and Bersimis-2..
Atlas of Canada - Department of Natural Resources Canada - Petit lac Wayagamac - Measurements provided by the measurement tools of the Internet application. Little Bostonnais River From the outlet of Petit lac Wayagamac, the Petite Rivière Bostonnais (English: Little Bostonnais River) runs 4.4 km (measured by water) before emptying into Lake Wayagamac (southeast side). Lake Wayagamac in turn empties from the west into the Little Bostonnais River which is approximately 10.6 km long (measured by water), between the Wayagamac lake dam and the mouth of the river which flows into the Saint-Maurice River at the southern limit of the town of La Tuque (just south of the airport). From the outlet of Petit lac Wayagamac, the water from the Petite rivière Bostonnais flows over 23.6 km, 8.6 km of which cross Lake Wayagamac from East to West.
The final few miles of the Aucilla below the mouth of the Wacissa flows over a broad floodplain. Although the Wacissa River is the largest tributary of the Aucilla River, it breaks into a number of braided channels before reaching the Aucilla. In the first half of the 19th Century cotton growers of Jefferson and Madison Counties wanted to carry their cotton to sea ports on the coast, but the intermittent underground segments of the Aucilla River and the narrow and shallow braided channels of the lower Wacissa did not permit the passage of barges. The Wacissa and Aucilla Navigation Company was chartered in 1831 to dig a canal from the navigable portion of the Wacissa to below Nuttall Rise, where the Aucilla returns above ground for the last time before reaching the Gulf of Mexico.
Air preheaters: Rotating regenerative heat exchangers In the tri-sector design, the largest sector (usually spanning about half the cross-section of the casing) is connected to the boiler hot gas outlet. The hot exhaust gas flows over the central element, transferring some of its heat to the element, and is then ducted away for further treatment in dust collectors and other equipment before being expelled from the flue gas stack. The second, smaller sector, is fed with ambient air by a fan, which passes over the heated element as it rotates into the sector, and is heated before being carried to the boiler furnace for combustion. The third sector is the smallest one and it heats air which is routed into the pulverizers and used to carry the coal-air mixture to coal boiler burners.
Amazing Tales from Indiana By Fred D. Cavinder, 1990, Pg 5 The Lost River begins as a normal river in Washington County, but soon after rising, the river flows over and into a limestone bed (karst) for several miles until the stream bed turns dry; the water is absorbed into the limestone and sinks beneath the surface to a hidden cavern. The river then flows underground through a network of caves and channels through part of Orleans Township, Paoli Township, and part of Orangeville Township before reappearing on the surface near the village of Orangeville. Where the river rises to the surface in Orange County it produces a spring that is deep, with the very bottom connecting to the actual underground channel. This spring, the second largest in the state, is known as the True Rise, because many inaccurately believe that the Orangeville Rise is the main channel of the river.
The river starts at Ralph Bice Lake (formerly Butt Lake) in northern Algonquin Provincial Park in the geographic township of Butt in the Unorganized South Part of Nipissing District. It flows south to Daisy Lake then east to Big Trout Lake. The river heads north out the lake over Big Trout Lake Dam, takes in the left tributary Tim River, flows over the Portal Rapids, Cedar Rapids, Snowshoe Rapids, Catfish Rapids, and Stacks Rapids to reach Cedar Lake, the location of the community of Brent, where it takes in the left tributary Nipissing River. The river exits the lake over a dam, heads through the Devil's Chute, reaches Radiant Lake, where it takes in the left tributary North River and right tributary Little Madawaska River, and passes through the Squirrel Rapids, Big Sawyer Rapids, Battery Rapids Cascade Rapids and White Horse Rapids, and takes in the right tributary Crow River.
In these cases, a generalized compressibility chart or an alternative equation of state better suited to the problem must be utilized to produce accurate results. A related situation occurs in hypersonic aerodynamics, where dissociation causes an increase in the “notional” molar volume, because a mole of oxygen, as O2, becomes 2 moles of monatomic oxygen and N2 similarly dissociates to 2 N. Since this occurs dynamically as air flows over the aerospace object, it is convenient to alter , defined for an initial 30 gram moles of air, rather than track the varying mean molecular weight, millisecond by millisecond. This pressure dependent transition occurs for atmospheric oxygen in the 2,500–4,000 K temperature range, and in the 5,000–10,000 K range for nitrogen. In transition regions, where this pressure dependent dissociation is incomplete, both beta (the volume/pressure differential ratio) and the differential, constant pressure heat capacity greatly increases.
If water is poured slowly into the bowl it simply flows over the rim of the waterway and pours slowly down the drain—thus the toilet does not flush properly. After flushing, the flapper valve in the water tank closes or the flush valve shuts; water lines and valves connected to the water supply refill the toilet tank and bowl. Then the toilet is again ready for use. Note with this flush design: With age the forward (“flush”) jet connection to the upper inlet in the toilet may slowly clog and (over many years) eventually lead to poor, or no flushing action – despite the fact that the main bowl's exit pipe and the toilet's air vent are both open... A test for this is if a “normal flush” evacuation of the bowl occurs when a large amount of water is poured into the bowl at a fast rate.
Geological Survey of Ireland (GSI) regard the waterfalls an "important site for both the glacial feature and for the geological influence of the rocks themselves on the formation of the waterfall"; and describe the Powerscourt corrie, in which the waterfall sits, as "a fine example of glacial erosion, where accumulated ice has scoured out a deep basin, with a waterfall flowing down the steep backwall". The Powerscourt waterfall flows over Irish Ribband Group schists, which sit in a metamorphic aureole of Leinster granite. The cleavage (or schistosity) dips steeply outwards, paralleling the sides of the granite pluton, which forms the surface over which the water cascades; however, the GSI note the contact between schist and granite is some distance upstream of the waterfall. Both boulders of schist (a silvery-sheen appearance), and of granite (a speckled crystalline appearance), can be seen in the pools at the base of the waterfall.
9 The current administration has placed an emphasis on how to create jobs in Mexico, enhance border security, and protect Mexican citizens living abroad. Traditionally, Mexico built a reputation as one of the classic asylum countries, with a varying attitude toward refugees from Spain and other European countries before and during World War II, from Latin America's Southern Cone in the 1970s, and from Central America since the beginning of the 1980s. However, in recent years refugees who solicit asylum are usually treated as if they were just immigrants, with exhaustive administrative processes. The southern border of Mexico has experienced a significant increase in legal and illegal flows over the past decade, in particular for migrants seeking to transit Mexico to reach the U.S. José Luis Soberanes, president of the National Human Rights Commission, condemned the repressing policy implemented by the Mexican government against illegal immigrants who cross the country's southern border.
The material that is expelled in a volcanic eruption can be classified into three types: #Volcanic gases, a mixture made mostly of steam, carbon dioxide, and a sulfur compound (either sulfur dioxide, SO2, or hydrogen sulfide, H2S, depending on the temperature) #Lava, the name of magma when it emerges and flows over the surface #Tephra, particles of solid material of all shapes and sizes ejected and thrown through the air Light-microscope image of tuff as seen in thin section (long dimension is several mm): The curved shapes of altered glass shards (ash fragments) are well preserved, although the glass is partly altered. The shapes were formed about bubbles of expanding, water- rich gas. Tephra is made when magma inside the volcano is blown apart by the rapid expansion of hot volcanic gases. Magma commonly explodes as the gas dissolved in it comes out of solution as the pressure decreases when it flows to the surface.
The river flows to the south of the A473 Pontypridd to Bridgend (') road (Talbot Green By-Pass), where it is fed from the south by Nant Mwyndy. Nant Mwyndy flows over a bedrock of Carboniferous Limestone, rising in Creigiau and, flowing westwards, immediately north of Groesfaen, passing a small industrial estate at Mwyndy, feeding a lake resulting from Victorian opencast iron mining (see History below) and turning south to flow past Cefn-y-Parc Cemetery, Penygawsi, before reaching its confluence with the Afon Clun.Location of Cefn-y-Parc Cemetery Confluence of Ely (left/north) and Afon Clun (right/east), at PontyclunThe Clun then flows beneath the main A4119 (Tonypandy to Cardiff Bay) route about south of the roundabout by Glamorgan Vale Retail Park, Talbot Green. At this point, the river often overflows onto the meadows to the north, providing a wetland wildlife habitat, although drainage of floodplain grasslands, for industrialisation, housing and associated infrastructure, has affected wildlife by reducing its available area.
The impetus behind the research into sweeping jet actuators lies in the realization that any vertical tail structure on an aircraft is a parasitic surface in level flight. The design specification that must be met by the vertical stabilizer of any multi-engined aircraft is that it be able to produce enough lift to counteract any thrust asymmetry that would come as a result of engine failure during rotation (takeoff); but in any condition that is not an emergency or where a yaw moment is not desired the vertical stabilizer will only contribute added weight and drag to the aircraft. The jet nozzles (located directly upstream of the hinge around which the rudder moves) eject a subsonic stream of air that flows over the rudder and act to retain or reattach the boundary layer to the control surface as it is deflected beyond the incidence angle where natural flow would separate, generating as much as a 30-percent increase in the effective lift produced by the rudder.
Depending on the composition of the lava and the substrate, Tawhaki Vallis may have formed over a period of 400–600 days (for ultramafic lava flowing over ultramafic plains), 10–60 days (for sulfur lava flow over sulfur plains), or hours to a few days when a high-temperature lava flows over a substrate with a much cooler melting point, such as ultramafic lava over plains composed primarily of sulfur. Considering the need to keep the lava liquid enough to flow over these long distances and typical duration of eruptions that could carve a channel like this, the latter possibility (high- temperature lava over a surface with a cooler melting temperature) is considered the most likely. Similar channels to Tawhaki Vallis have also been observed near Zamama and Emakong Patera. Those channels are clearly associated with their respective volcano, but based on the images available, it is not known if an eruption at Tawhaki Patera was responsible for the formation of Tawhaki Vallis.
The river begins at Crocker Bay at the northwest of Raleigh Lake, flows northwest over the Raleigh Falls, then under Ontario Highway 17 and the Canadian Pacific Railway transcontinental main line at the settlement of Raleigh. It continues northwest, takes in the right tributary Little Wabigoon River, then turns southwest back under the CP line and Highway 17 at the settlement of Taché. The river takes in the left tributary Mennin River, flows over Walker Falls, and takes in the right tributary Melgund Creek all near the settlement of Borups Corners, enters Dinorwic Lake, and flows into Wabigoon Lake, where it takes in the left tributary Crooked River. The Wabigoon River exits the lake at the northwest at Dryden, and flows northwest, through Wainwright Township dam and generating station (operated by Regional Power, a subsidiary of Manulife Financial), takes in the left tributary Eagle River, passes under Ontario Highway 105 at Upper Falls, then under Ontario Highway 609 and the Canadian National Railway transcontinental main line and over Quibell Dam the latter three at the settlement of Quibell.
The waters of this great river draw wildlife in great numbers to its banks, creating an oasis of green. Samburu, Shaba and Buffalo Springs National Reserves in Northern Kenya teem with wildlife in an otherwise arid land, because of the water of the river. Below Sericho, the river expands into the Lorian Swamp, a large area of wetlands. The ecological diversity throughout the catchment is unique to the Ewaso Ng’iro watershed specifically, as it originates from the high agriculturally potent lands of Mount Kenya, right at Thome Area of Nanyuki-Laikipia County, that means the exact start point of this river is at the Thome village where it is formed out of covergence of Naromoru River, sourcing water from Mt. Kenya and Ngarinyiru River sourcing water from Aberdares and it flows over the following seven arid to semi arid land districts Meru, Laikipia, Samburu, Isiolo, Wajir, Marsabit, and Garissa (Said et al. 14). Following the independence of Kenya, the stretches of land covered by the Ewaso Ng’iro watershed shifted ownership from the colonial farmers to small scale farmers (Thenya et al. 2).

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