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370 Sentences With "waterbody"

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

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EQM said it is working through the project's remaining challenges, including securing a Nationwide 12 Permit from the U.S. Army Corps of Engineers for stream and waterbody crossings, which it expects sometime this summer.
Waterbody; Waterbody system; Area in ha; location of the nearest significant settlement; Remarks The standing waterbodies are sorted by type. Their boundaries are however, somewhat fluid.
Kern Glen Creek is not designated as an impaired waterbody.
Indian Cave Creek is not designated as an impaired waterbody.
East Branch Martins Creek is not designated as an impaired waterbody.
Halfway Run is not designated as an impaired waterbody. Halfway Run is a clear stream.
Tinker Creek is not designated as an impaired waterbody. The alkalinity concentration of the creek is .
Stone Run is not designated as an impaired waterbody. The concentration of alkalinity in the stream is .
Hettesheimer Run is not designated as an impaired waterbody. The concentration of alkalinity in Hettesheimer Run is .
Dry Creek is not designated as an impaired waterbody. The creek only seasonally flows into Martins Creek.
Rock Creek is not designated as an impaired waterbody. The total concentration of alkalinity in the creek is .
The entire length of Dymond Creek attains its designated uses and thus is not designated as an impaired waterbody.
Sugar Hollow Creek is not designated as an impaired waterbody. The concentration of alkalinity in Sugar Hollow Creek is .
As of 2013, the status of this project is unknown. Chapman Creek is not designated as an impaired waterbody.
Locating old Rhine waterbodies in the list: Some names of old Rhine waterbodies include the name of a nearby town or village; others do not. In order to make it easy to find in every case, the nearby settlement is usually written in alphabetical order and italics before each waterbody name as a means of locating it. Next, the coordinates of the waterbody and its position on the Rhine (l/r = left/right) follow, then comes either the waterbody name itself in normal lettering, as well as other names of the waterbody in italics. Or there may just be a reference to the name of another place name behind the town name, under which the river is listed in italics.
Spring Creek is not designated as an impaired waterbody. The creek's watershed is a USDA/NRCS priority watershed in Lycoming County.
Horton Creek is not designated as an impaired waterbody. The average annual rate of precipitation in the watershed of Horton Creek is .
The brewery's logo features an ostrich, with an egg, and a distant windmill. The brewery is named after the nearby IJ waterbody.
North Branch Bowman Creek is not designated as an impaired waterbody. However, in the 1980s, the creek was considered to be vulnerable to acidification.
Louisiana Department of Wildlife and Fisheries. Office of Fisheries-Inland Section. (2009). "Bayou DeSiard: Lake History & Management Issues". Part VI-A, Waterbody Management Plan series.
However, it is not designated as an impaired waterbody and is inhabited by trout. The creek has been a major source of flooding in Hellertown.
In the Atacama Altiplano, Laguna Miscanti is among the biggest waterbodies. The mountains Cerro Miscanti () and Cerro Miniques () lie northeast and south of the lake, respectively. south of the lake lies another waterbody, Laguna Miniques. In the past, the two lakes were connected, producing a large waterbody which has left beach terraces in the landscape and whose water levels were about higher than today.
Locust Creek has no named tributaries, but it has one unnamed tributary. This tributary is known as UNT #18656 and of it is an impaired waterbody.
Bedrock consisting of sandstone and shale occurs in the surficial geology on parts of some hills near the stream. Tower Branch is not designated as an impaired waterbody.
It may also refer more specifically to a walkway accessing the centre of an enclosed waterbody. The term derives from the French word ', "thrown", signifying something thrown out.
However, there are patches of fill and alluvial terrace, as well as a few small lakes near the headwaters. Taques Creek is not designated as an impaired waterbody.
The waterbody that gives the community its name is due north of the junction, and Thompson's Lake State Park is a short distance to the northwest along NY 157.
Sealholtz Run is not designated as an impaired waterbody. PPL was once given a National Pollutant Discharge Elimination System permit to discharge stormwater into the stream for construction purposes.
A reach of Fiddle Lake Creek is designated as an impaired waterbody. The causes of impairment are water temperature and one unknown cause. The impairment comes from natural sources.
Edwardes Lake is a recreational waterbody in the Melbourne, Australia, suburb of Reservoir, formed by the damming of Edgars Creek at Edwards Road. it is surrounded by Edwardes Lake Park.
A reach of Susquehecka Creek is designated as an impaired waterbody. The cause of the impairment is siltation/sedimentation and the likely source of the impairment is grazing- related agriculture.
Spring Run is designated as an impaired waterbody. The causes of impairment are an unknown cause and sedimentation/siltation. The probable sources of impairment are agriculture and urban runoff/storm sewers.
It flows down into the broad valley of White Deer Hole Creek. Beartrap Hollow is in the Ridge and Valley Freestone region. Beartrap Hollow is not designated as an impaired waterbody.
The elevation near the mouth of Black Run is above sea level. The elevation of the stream's source is between above sea level. Black Run is not designated as an impaired waterbody.
The watershed of Sugar Run has an area of . The stream is entirely within the United States Geological Survey quadrangle of Center Moreland. Sugar Run is not designated as an impaired waterbody.
Trout Run is not designated as an impaired waterbody. The stream has a high level of water quality and no part of it or any of its tributaries is designated as impaired.
The Aubach (Wiehl) in Germany (Watercourse) A fjord (Lysefjord) in Norway A body of water or waterbody"waterbody noun (pl. -ies) a body of water forming a physiographical feature, for example a sea or a reservoir." New Oxford Dictionary of English (often spelled water body) is any significant accumulation of water, generally on a planet's surface. The term most often refers to oceans, seas, and lakes, but it includes smaller pools of water such as ponds, wetlands, or more rarely, puddles.
In the south the road link runs along a causeway (the Poeldamm) over a low peninsula to Poel over the Breitling. The waterbody is about five kilometres long and no more than one kilometre wide.
A reach of Aline Creek is designated as an impaired waterbody due to siltation/sedimentation from agriculture and removal of vegetation. The creek's drainage basin is designated as a Coldwater Fishery and a Migratory Fishery.
Of the total area of the lake, the waterbody is spread across 9.1 acres and the land area covers 6.9 acres. An anglers club was functioning till the 1940s in the lake, whose members visited the small island in the midst of the waterbody for fishing. Although not used for drinking purposes, the lake was a source of groundwater recharge for the surrounding areas. As the water quality is not saline, the lake has a few varieties of fishes such as rohu, catla and mrigal.
Mills Lake is a California waterbody along the Sierra Crest east of Ruby Peak and Mount Mills near Little Lakes Valley. The discharge of Mills Lake flows through Ruby Lake, Rock Creek Lake, and into Rock Creek.
The total volume of the lava field is about . Neighbouring mountains include the high northwest and the high close to Negriales de Lastarria in the southwest. Almost due north of Lastarria lies the , a salt pan with a waterbody that is almost a lake, its name is a reference to the sulfur deposits of Lastarria. This waterbody may be a source of water for the fumarolic system Water levels in the lake were higher in the past, as evidenced by two recognizable shorelines, and the lake's surface area reached .
Walchsee is a lake in Kufstein District in both Walchsee and Kössen municipalities, Tyrol, Austria. Its surface area of makes it the fourth largest natural waterbody in the state. Its maximum depth is , and its maximum volume is .
The elevation near the mouth of Boyers Run is above sea level. The elevation of the stream's source is . Boyers Run is located to the south of Turkey Ridge. Boyers Run is not designated as an impaired waterbody.
Furnace Run is designated as an impaired waterbody. The cause of the impairment is sedimentation and siltation. The source of the impairment is urban runoff and storm sewers. As of 2006, a total maximum daily load is needed.
The elevation near the mouth of Bellas Brook is above sea level. The elevation near the stream's source is above sea level. Bellas Brook is a small and secluded stream. Bellas Brook is not designated as an impaired waterbody.
Millard Creek is not designated as an impaired waterbody. The total sediment load in Millard Creek is per year. Cropland is by far the largest contributor, accounting for per year. Deciduous forest an hay/pastures/grass contribute per year respectively.
Koggala Lagoon ()is a coastal waterbody located in Galle District, Southern Sri Lanka. It is situated near the town of Koggala and adjacent to the southern coast, about south of Colombo. The lagoon is embellished with eight ecologically rich small islands.
The elevation near the mouth of Opossum Brook is above sea level. The elevation near the source of the stream is above sea level. The stream flows in a generally northerly direction. Opossum Brook is not designated as an impaired waterbody.
Kennedy Creek is not designated as an impaired waterbody. In June 2006, trace concentrations of trichloroethylene were found in Kennedy Creek at the Interstate 81 overpass. However, in September 2006, the creek was found not to contain trichloroethylene, perchloroethylene, or DCE.
The lake is roughly in area, and consists of a main waterbody with two elongate arms. The main waterbody is roughly rectangular, with its long side oriented along a north-westerly axis. A narrow arm, essentially a network of anastomosing creeks, arises from near the eastern edge, stretching north almost to Meekatharra; the lake receives inflow from this arm and also some smaller creeks on the west and north side. Drainage is via the other arm, which arises from near the western edge and reaches almost to headwaters of the Hope River, into which Lake Anneen flows following heavy rains.
Loch Etchachan is a remote freshwater loch set deep within the central Cairngorms plateau, in the Cairngorms National Park, located in the eastern Highlands of Scotland. It is the highest waterbody of its size in the UK, the surface being above sea level.
Locust Creek has poor water quality. The entire length of Locust Creek is designated as an impaired waterbody. The cause of the impairment is metals and the source is abandoned mine drainage. The acid mine drainage impacts to the creek are severe.
Millard Creek is a tributary of Tunkhannock Creek in Susquehanna County, Pennsylvania. It is approximately long and flows through Harford Township and Lenox Township. The watershed of the creek has an area of . The creek is not designated as an impaired waterbody.
Swale Brook is not designated as an impaired waterbody. The Tunkhannock Area School District once applied for and/or received a permit to discharge stormwater into the stream during construction activities. Swale Brook was once described as a stream of "pure, cold water".
Rekawa Lagoon () is a coastal waterbody located in Hambantota Districtt in the Southern Province, Sri Lanka and it is located south of Colombo. The lagoon possesses a rich biodiversity with a variety of flora (ex; mangroves) and fauna (ex; fish, crustaceans, birds).
York Run is not designated as an impaired waterbody. The concentration of alkalinity in York Run is . Mehoopany Wind Energy, LLC. once applied for and/or received a National Pollutant Discharge Elimination System to discharge stormwater into York Run during construction activities.
Buttermilk Creek is not designated as an impaired waterbody. Along with Gardner Creek, it is one of only two perennial streams in the Ransom quadrangle. In the early 1900s, the average annual rate of precipitation in the watershed of Buttermilk Creek was .
There are some patches of peat bogs, wetlands, and lakes near the creek, but the surficial geology in the upper reaches mostly consists of alluvium and Wisconsinan Till, with some bedrock further away. Bear Swamp is not designated as an impaired waterbody.
Mill Run is not designated as an impaired waterbody. The mouth of Mill Run is in the United States Geological Survey quadrangle of Tunkhannock. However, its source is in the quadrangle of Factoryville. The designated use of the stream is for aquatic life.
Major inlets include Sydney Inlet, Shelter Inlet, Herbert Inlet, Bedwell Inlet, Lemmens Inlet, and Tofino Inlet. Major islands include Flores Island, Vargas Island, and Meares Island. The name is also used for the larger region of land around the waterbody (essentially its watershed).
The elevation near the mouth of Dry Run is above sea level. The elevation of the stream's source is above sea level. A total of of Dry Run is designated as an impaired waterbody. The impairment is siltation due to agricultural activity.
Deep Creek is not designated as an impaired waterbody as of 2004. However, the Dauphin County conservation District has observed that nitrate concentrations in the creek are among the highest in Dauphin County. It is also likely that sediment loads are relatively high.
Such kolks generally represent the non-evaporating excess water of a bog. The central waterbody of these bogs exhibit almost no sedimentation. The accumulation of nutrients can lead to the formation of floating mats. Their vegetation differs from that of other structures in the bog.
Effects of Hypoxia on Fish Assemblages in a Vegetated Waterbody. Aquatic Plant Management 39:40-44. The bowfins are known to be occasional predators on the pygmy sunfish family. Occasionally, the grass pickerel and live-bearers are competitors for food with the pygmy sunfish.
The community of Forkston, which is located near Bowman Hollow, is one of only two areas of residential development in the watershed of Mehoopany Creek. Bowman Hollow is not designated as an impaired waterbody. The stream is classified as a High-Quality Coldwater Fishery.
Swale Brook is a tributary of Tunkhannock Creek in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through Tunkhannock Township and Tunkhannock. The watershed of the stream has an area of . The stream is not designated as an impaired waterbody.
Bowman Creek is not designated as an impaired waterbody. However, in the creek's middle or upper reaches, of streams are impaired by atmospheric deposition. The upper reaches of the creek experience seasonal acidity problems. During the summer months, the creek is shallow and clear.
Dry Run is designated as an impaired waterbody. The cause of impairment is sedimentation/siltation. The likely source of impairment is agriculture. At the point where Dry Run crosses a Conrail railroad, the stream's peak annual discharge has a 10 percent chance of reaching .
The aquatic flora of the estuary are dominated by the small green algae Polyphysa peniculus the stonewort Lamprothamnium papulosum and the seagrass Ruppia megacarpa. The waterbody of the inlet is fringed with Salt Water Paperbarks with sedges and samphire common along the sandy sections.
Keeler Creek is a tributary of the Susquehanna River in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through Falls Township. The watershed of the creek has an area of . The stream is not designated as an impaired waterbody.
Fitch Creek is a tributary of the Susquehanna River in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through Falls Township. The watershed of the creek has an area of . The creek is not designated as an impaired waterbody.
Lewis Creek is not designated as an impaired waterbody. The creek's water chemistry is typical for streams of its geology and land use. It is fertile enough to avoid experiencing acid flushes. The concentration of alkalinity in Lewis Creek is 42 milligrams per liter.
Hettesheimer Run (also known as Hettesheimer's Run) is a tributary of Bowman Creek in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through Noxen Township. The watershed of the stream has an area of . It is not designated as an impaired waterbody.
Cider Run is a tributary of Bowman Creek in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through Forkston Township and Noxen Township. The watershed of the stream has an area of . The stream is not designated as an impaired waterbody.
Sugar Hollow Creek is a tributary of Bowman Creek in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through Mehoopany Township and Eaton Township. The watershed of the creek has an area of . The creek is not designated as an impaired waterbody.
Turkey Run is a tributary of the West Branch Susquehanna River in Lycoming County, Pennsylvania, in the United States. It is approximately long and flows through Clinton Township. The watershed of the stream has an area of . The stream is not designated as an impaired waterbody.
Newton Run is a tributary of Roaring Run in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through Eaton Township and Monroe Township. The watershed of the stream has an area of . The stream is not designated as an impaired waterbody.
Larval quagga mussels were found in the water.Action on mussel delayed. After 5 years of negative testing Lake Granby, Colorado has been classified as a negative waterbody for quagga mussel veligers. Quagga mussels are now in all parts of Lake Powell on the Utah and Arizona border.
Luphers Run is designated as an impaired waterbody. The cause of the impairment is nutrients and organic enrichment/low dissolved oxygen. The likely source of the impairment is municipal point source discharges. Additionally, the headwaters of the stream are impacted by acid deposition and low pH.
Thurston Hollow (also known as Thurston Hollow Creek) is a tributary of Moneypenny Creek in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through Eaton Township. The stream's watershed has an area of . Thurston Hollow is not designated as an impaired waterbody.
Miller Brook is a tributary of North Branch Mehoopany Creek in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through North Branch Township. The watershed of the stream has an area of . The stream is not designated as an impaired waterbody.
Butler Creek is not designated as an impaired waterbody. The average annual discharge of Butler Creek at Gibson between 1974 and 1979 ranged from in 1976 to in 1979. In 1974 and 1975, the discharges were , respectively. In 1977 and 1978, the average annual discharges were .
Millers Run is an unimpaired waterbody, as are all other streams in its watershed. It is not impacted by mining. In April 1975, the specific conductance of Millers Run was measured to be 71 micro-siemens per centimeter. The concentration of water hardness in the stream was .
The U.S. Environmental Protection Agency lists Anaheim Bay as an impaired waterbody, with high concentrations of dieldrin, nickel, PCBs and sediment toxicity. Huntington Harbor is also contaminated by chlordane, copper, lead, nickel, and PCBs. Urban runoff has also introduced high concentrations of pathogens such as E.coli into the bay.
Esplanade is a neighbourhood of Central Kolkata, in Kolkata district in the Indian state of West Bengal. This is not a conventional esplanade in the sense that the place is not exactly situated alongside a waterbody. However, the Ganga river (Ganges), also known as Hooghly river, flows nearby.
Quaker Run is designated as an impaired waterbody due to metals from abandoned mine drainage. Raw sewage and stormwater have also been discharged into it at times. The channel of Quaker Run is flanked by walls in some reaches. Iron precipitate is also caked thickly along the stream.
The locality presumably takes its name from the waterbody Lake Eacham in the north-west of the locality (). The name of the lake is believed to be an Aboriginal word yeetcham meaning big spring. Lake Eacham State School opened on 1911. In 1919 it was renamed Peeramon State School.
North Branch Bowman Creek is a tributary of Bowman Creek in Luzerne County, Pennsylvania, in the United States. It is approximately long and flows through Fairmount Township and Ross Township. The watershed of the creek has an area of . The creek is not designated as an impaired waterbody.
Manns Beach is a small community based near Port Albert, Victoria, Australia. It contains lavatory facilities, jetty and boat ramp that provides boating access to the water body. The waterbody mouths into offshore waters of Bass Strait. At the 2006 census, Manns Beach had a population of 135.
Stone Run (also known as Slife Run) is a tributary of Bowman Creek in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through Noxen Township. The watershed of the stream has an area of . The stream is not designated as an impaired waterbody.
Baker Run (also known as Windfall Run) is a tributary of Bowman Creek in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through Noxen Township. The watershed of the stream has an area of . The stream is not designated as an impaired waterbody.
Benson Hollow is a tributary of Bowman Creek in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through Eaton Township. The watershed of the stream has an area of . Benson Hollow is a first-order stream and is not designated as an impaired waterbody.
East Branch Martins Creek is a tributary of Martins Creek in Susquehanna County, Pennsylvania, in the United States. It is approximately long and flows through New Milford Township and Harford Township. The watershed of the creek has an area of . The creek is not designated as an impaired waterbody.
Marsh Creek is a tributary of Bowman Creek in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through Northmoreland Township, Eaton Township, and Monroe Township. The watershed of the creek has an area of . The creek is not designated as an impaired waterbody.
South Run (also known as South Run Creek) is a tributary of Bowman Creek in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through Monroe Township. The watershed of the stream has an area of . It is not designated as an impaired waterbody.
Sand Spring Run is a tributary of White Deer Creek in Union County, Pennsylvania, in the United States. It is approximately long and flows through Lewis Township and West Buffalo Township. The watershed of the stream has an area of . The stream is not designated as an impaired waterbody.
Sealholtz Run is a tributary of the Susquehanna River in Northumberland County, Pennsylvania, in the United States. It is approximately long and flows through Lower Augusta Township and Upper Augusta Township. The watershed of the stream has an area of . The stream is not designated as an impaired waterbody.
Leslie Creek is a tributary of Nine Partners Creek in Susquehanna County, Pennsylvania, in the United States. It is approximately long and flows through New Milford Township and Harford Township. The watershed of the creek has an area of . The creek is not designated as an impaired waterbody.
Kennedy Creek is a tributary of South Branch Tunkhannock Creek in Lackawanna County, Pennsylvania, in the United States. It is approximately long and flows through Scott Township and North Abington Township. The watershed of the creek has an area of . The creek is not designated as an impaired waterbody.
Black River is not designated as an impaired waterbody. At its mouth, the peak annual discharge has a 10 percent chance of reaching . It has a 2 percent chance of reaching and a 1 percent chance of reaching . The peak annual discharge has a 0.2 percent chance of reaching .
Millers Run is a tributary of Shamokin Creek in Northumberland County, Pennsylvania, in the United States. It is approximately long and flows through Ralpho Township. The watershed of the stream has an area of . The stream is not impacted by mining and is not designated as an impaired waterbody.
Tower Branch is a tributary of Tunkhannock Creek in Susquehanna County, Pennsylvania, in the United States. It is approximately long and flows through Harford Township and Lenox Township. The watershed of the stream has an area of . The stream is not designated as an impaired waterbody and has no named tributaries.
The river flow volume from six rivers typically exceeds the volume of the incoming tide. Combined with the bottleneck of The Chops, the result is a tidal waterbody with very little salt, known as brackish. Located about from the ocean, Merrymeeting Bay has many river delta characteristics. The tides average about .
The Chécatica River is about long, and runs from north to south. In some sections it widens into lakes, including Lake Chécatica. It enters Jacques-Cartier Bay on the Saint Lawrence about west of Blanc-Sablon. The bay is a waterbody with an irregular outline, containing many points, inlets and islands.
This small waterbody gains its name from Lancelot Dobson, an earlier landowner. It was later bought by the owners of Patterdale Hall, the Marshall family, and extended by damming. In addition to fishing, the tarn was used as a source of ice in winter, and the ice house still stands nearby.
Cowbell Hollow (also known as Cowbell Hollow Run) is a tributary of White Deer Creek in Union County, Pennsylvania, in the United States. It is approximately long and flows through West Buffalo Township. The watershed of the stream has an area of . The stream is not designated as an impaired waterbody.
Beartrap Hollow (also known as Bear Trap Hollow) is a tributary of White Deer Hole Creek in Lycoming County, Pennsylvania, in the United States. It is approximately long and flows through Washington Township. The watershed of the stream has an area of . The stream is not designated as an impaired waterbody.
Hallowing Run (also known as Hollowing Run) is a tributary of the Susquehanna River in Northumberland County, Pennsylvania, in the United States. It is approximately long and flows through Lower Augusta Township. The watershed of the stream has an area of . The stream is not designated as an impaired waterbody.
Rolling Green Run is a tributary of the Susquehanna River in Snyder County, Pennsylvania, in the United States. It is approximately long and flows through Monroe Township. The watershed of the stream has an area of . The stream is designated as an impaired waterbody due to habitat alteration from golf courses.
Upstream of the lake on Kern Run, the watershed of the stream consists of 99 percent forested land, and 1 percent bodies of water, wetlands, and pastures. Kern Run can be accessed via Township Road 588 from US Route 522. One reach of Kern Run is designated as an impaired waterbody.
West Branch Rausch Creek is a tributary of Rausch Creek in Schuylkill County, Pennsylvania, in the United States. It is approximately long and flows through Hegins Township. The watershed of the creek has an area of . The creek is designated as an impaired waterbody due to metals from abandoned mine drainage.
The Richtenberger See (also: Franzburg-Richtenberger See) is a lake between the towns of Franzburg and Richtenberg in Western Pomerania in northeast Germany. The waterbody was drained in 1936, but refilled as part of an ecological measure to compensate for environmental damage caused by the construction of the A 20 motorway.
Tinker Hollow is a tributary of Little Creek in Susquehanna County, Pennsylvania, in the United States. It is approximately long and flows through Clifford Township. The watershed of the stream has an area of . The stream is not designated as an impaired waterbody and has wild trout naturally reproducing within it.
Hull Creek is considered to be an impaired waterbody. The cause of the impairment is habitat alteration and the probable source of the impairment is channelization. Additionally, runoff from Pennsylvania Route 347 and residential properties impacts the water quality of the creek in Blakely. The creek loses flow to underground mines.
Tinker Creek is a tributary of East Branch Tunkhannock Creek in Susquehanna County, Pennsylvania, in the United States. It is approximately long and flows through Clifford Township. The watershed of the creek has an area of . The creek is not designated as an impaired waterbody and has no named tributaries.
Idlewild Creek is a tributary of East Branch Tunkhannock Creek in Susquehanna County, Pennsylvania, in the United States. It is approximately long and flows through Clifford Township. The watershed of the creek has an area of . The creek is not designated as an impaired waterbody and has no named tributaries.
Like other forms with a similar body structure, it is likely that Unionopterus was a benthic (living at the lowest level of the waterbody) organism. Its body and lifestyle were capable of and adapted to not only swimming, but also crawling. However, Unionopterus would not have been so active as other relatives.
Kern Glen Creek (also known as Meadow Brook) is a tributary of Billings Mill Brook in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through Lemon Township and Tunkhannock Township. The watershed of the creek has an area of . The creek is not designated as an impaired waterbody.
Glade Run is not designated as an impaired waterbody. The peak annual discharge of Glade Run at its mouth has a 10 percent chance of reaching . It has a 2 percent chance of reaching and a 1 percent chance of reaching . The peak annual discharge has a 0.2 percent chance of reaching .
When the largest man-made waterbody in the area, Bhimsagar, was being dug, many antiquities were recovered and some were believed to belong to the Shunga-Kushan era (around 1st BC to 1st century AD). Much later, the Contai area was a part of the Hijli Kingdom, which existed between 1687 and 1886.
Bear Swamp Creek is a tributary of Tunkhannock Creek in Susquehanna County, Pennsylvania, in the United States. It is approximately long and flows through Gibson Township and Clifford Township. The watershed of the creek has an area of . The creek has no named tributaries, and is not designated as an impaired waterbody.
Catlin Brook is not designated as an impaired waterbody. The stream has water for most of the year, but often dwindles to a trickle in the summertime. However, it was dry when Pennsylvania Fish and Boat Commission biologists visited it while studying the North Branch Mehoopany Creek watershed in the summer of 2001.
They should be updated every six years. To facilitate data recoding, each stretch of water is given a "Water Framework Directive ID" ("WFDID" or "Waterbody ID"). For example, the stretch of the River Tame, in the West Midlands of England, from the River Blythe to River Anker is referred to as GB104028046440.
Rock Creek is a tributary of Tunkhannock Creek in Susquehanna County, Pennsylvania, in the United States. It is approximately long and flows through Herrick Township, Ararat Township, and Gibson Township. The watershed of the creek has an area of . The creek has no named tributaries and is not designated as an impaired waterbody.
Ackerly Creek is not designated as an impaired waterbody. However, its tributary UNT 28835 is impaired. According to the Pennsylvania Department of Environmental Protection, the watershed of Ackerly Creek is the most "stressed" watershed in the Tunkhannock Creek drainage basin. In the 1970s, Ackerly Creek was found to be in good condition.
Taques Creek is a tributary of the Susquehanna River in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through Washington Township and Tunkhannock Township. The watershed of the creek has an area of . The creek is not designated as an impaired waterbody and has no named tributaries.
Chapman Creek is a tributary of the Susquehanna River in Snyder County, Pennsylvania, in the United States. It is approximately long and flows through Union Township and Chapman Township. The watershed of the creek has an area of . The creek has no named tributaries and is not designated as an impaired waterbody.
The elevation near the mouth of Aline Creek is above sea level. The elevation of the creek's source is above sea level. A reach of Aline Creek is designated as an impaired waterbody. The cause of the impairment is sedimentation/siltation and the likely sources of impairment are agriculture and removal of vegetation.
Deep Creek is a tributary of Mahantango Creek in Dauphin County, Pennsylvania, in the United States. It is approximately long and flows through Lykens Township and Pillow. The watershed of the creek has an area of . It is not designated as an impaired waterbody, but is nevertheless observed to have high nitrate concentrations.
The elevation near the mouth of Leiningers Run is above sea level. The elevation near the stream's source is above sea level. A reach of Leiningers Run is designated as an impaired waterbody. The cause of impairment is miscellaneous habitat alterations and the probable source is habitat modification that is not hydromodification.
None was large enough to have been reproductively mature (see below) and would have needed to survive in any new habitat for several months before reproducing. Passive dispersal may also occur via weed on boats and boat trailers and via water pumped from one waterbody to another for industrial and irrigation purposes. In the Nseleni River juvenile Tarebia granifera were commonly found with another invasive snail, Pseudosuccinea columella, on floating clumps of water hyacinth Eichhornia crassipes which provide a vehicle for rapid downstream dispersal. Once established in a particular waterbody Tarebia granifera is likely to disperse actively, both up and downstream in the case of flowing systems, as far as environmental factors like current speed and food availability will allow.
Lake Pohorile (, means 'burn lake') is a lake in the south-western Ukraine, in the delta of the Dniester River. It is located south from the city of Bilyayivka. The lake is characterized my low flow. The water source of the waterbody gets from several small canals, which connect the lake with the Turunchuk River.
Coal Run is a tributary of Shamokin Creek in Northumberland County, Pennsylvania, in the United States. It is approximately long and flows through Mount Carmel Township, Coal Township, and Shamokin. The watershed of the stream has an area of . The stream is designated as an impaired waterbody due to metals from abandoned mine drainage.
East Branch Tunkhannock Creek is not designated as an impaired waterbody. The water of the creek tends to be cooler than that of either South Branch Tunkhannock Creek or the main stem of Tunkhannock Creek. In the early 1900s, the annual rate of precipitation in the watershed of East Branch Tunkhannock Creek was typically per.
Henry Lott Brook 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 is not designated as an impaired waterbody and it is classified as a High-Quality Coldwater Fishery.
Beaver Run is a tributary of Bowman Creek in Luzerne County and Wyoming County, in Pennsylvania, in the United States. It is approximately long and flows through Lake Township in Luzerne County and Noxen Township in Wyoming County. The watershed of the stream has an area of . It is not designated as an impaired waterbody.
Beaver Run is not designated as an impaired waterbody. At Greenbriar Road, where Beaver Run drains , the stream's peak annual discharge has a 10 percent chance of reaching . It has a 2 percent chance of reaching and a 1 percent chance of reaching . The peak annual discharge has a 0.2 percent chance of reaching .
Black Run is not designated as an impaired waterbody. The Lycoming County RMS Recycling Facility and the Lycoming County RMS Southside Stockpile once applied for a permit to discharge stormwater into an unnamed tributary or tributaries of the stream. The Federal Correctional Complex, Allenwood has discharged effluent from its wastewater treatment plant into the stream.
Limestone Run is designated as an impaired waterbody by the Pennsylvania Department of Environmental Protection. The cause of the impairment is siltation and the source is agriculture. No part of Limestone Run or its tributaries attains stream standards set by the Pennsylvania Department of Environmental Protection. The annual load of sediment in Limestone Run is .
Dry Creek is a tributary of Martins Creek in Susquehanna County, Pennsylvania, in the United States. It is approximately long and flows through Brooklyn Township and Lathrop Township. The watershed of the creek has an area of . The creek is not designated as an impaired waterbody and is a Coldwater Fishery and a Migratory Fishery.
In the upper reaches, the surficial geology along the creek mainly consists of Wisconsinan Till, but there is some alluvium, wetlands, and lakes. Leslie Creek has been described as a "small creek". It passes through a lake known as Tingley Lake in its upper reaches. Leslie Creek is not designated as an impaired waterbody.
Gardner Creek (also known as Gardiners Creek or Gardners Creek) is a tributary of the Susquehanna River in Lackawanna County, Pennsylvania, in the United States. It is approximately long and flows through Newton Township and Ransom Township. The watershed of the creek has an area of . The creek is not designated as an impaired waterbody.
The criteria include numeric pollutant concentration limits, narrative goals (e.g., free from algae blooms), and narrative biological criteria (i.e., the aquatic life that should be able to live in the waterbody). If the water body fails the existing WQS criteria, the state must develop a Total Maximum Daily Load (TMDL) for pollutants of concern.
Kehly Run is designated as an impaired waterbody. The stream is impacted by abandoned mine drainage. However, it has been described as having "very good" water quality at site S11, in its upper reaches. In the late 1800s, the stream was described as having once been a stream of "good, soft, pure mountain water".
North Mahanoy Creek is designated as an impaired waterbody. The causes of impairment are sedimentation/siltation and water/flow variation and the likely source of impairment is abandoned mine drainage. The creek loses most or all of its flow to underground mines. The lower reaches of the creek are ephemeral due to this flow loss.
The elevation near the mouth of Little Meshoppen Creek is above sea level. The elevation near the creek's source is above sea level. Little Meshoppen Creek is not designated as an impaired waterbody. In a court case from the 1890s, several parties provided evidence that the creek had been shrinking for around 40 years.
Little Mehoopany Creek is not designated as an impaired waterbody. There are zero miles of impaired streams in the creek's watershed. The average discharge of Little Mehoopany Creek is at a monitoring station near its mouth. The maximum time for water to flow from the headwaters to the mouth is 8 hours and 50 minutes.
Miller Brook is not designated as an impaired waterbody. In 2001, the pH of Miller Brook near its mouth was measured to be 7.4, while the alkalinity was . The water hardness of the stream was and the specific conductance was 146 umhos. When the nearby air temperature was , the water temperature was measured to be .
East Branch Saucon Creek (also known as Laubachs Creek) is a tributary of Saucon Creek in Northampton County, Pennsylvania, in the United States. It is approximately long and flows through Lower Saucon Township and Bethlehem. The watershed of the creek has an area of . A reach of the creek is designated as an impaired waterbody.
Silver Creek is not designated as an impaired waterbody. At the downstream border of Hellertown, the peak annual discharge of Silver Creek has a 10 percent chance of reaching . It has a 2 percent chance of reaching and a 1 percent chance of reaching . The peak annual discharge has a 0.2 percent chance of reaching .
Hoffer Creek is a tributary of the Susquehanna River in Snyder County, Pennsylvania, in the United States. It is approximately long and flows through Chapman Township. The watershed of the creek has an area of . At least part of the creek is designated as an impaired waterbody due to sedimentation/siltation from grazing-related agriculture.
Hunlock Creek is not designated as an impaired waterbody, meaning that it attains standards for water quality. The peak annual discharge of Hunlock Creek at its mouth has a 10 percent chance of reaching . The discharge has a 2 percent chance of reaching and a 1 percent chance of reaching . It has a 0.2 percent chance of reaching .
The entire length of Carbon Run is designated as an impaired waterbody. The cause of the impairment is metals other than mercury and the source of the impairment is abandoned mine drainage. Its two unnamed tributaries are also impaired. The stream is impacted by acid mine drainage and the Sterling Mine discharge is in its watershed.
Bahadurpur Forest situated by the side of NH 34 in Krishnanagar II Block has been chosen as a prospective spot for jungle safari. Hasadanga Beel, adjacent to Bahadurpur Forest, is a vast waterbody which can be transformed into a water sports complex. This beel has the potential to be developed as a safe haven for seasonal migratory birds.
There are rapids on Mehoopany Creek both upstream and downstream of the point where Henry Lott Brook joins the creek. A cascade is located at the confluence of the two streams. Coal deposits were rumored to be present at the headwaters of Henry Lott Brook in the late 1800s. Henry Lott Brook is not designated as an impaired waterbody.
Kasson Brook (also known as Cassan Brook) 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 is not designated as an impaired waterbody and is classified as a High-Quality Coldwater Fishery.
East Branch Field Brook is a tributary of Field Brook in Susquehanna County and Wyoming County, in Pennsylvania, in the United States. It is approximately long and flows through Lathrop Township in Susquehanna County and Nicholson Township in Wyoming County. The watershed of the stream has an area of . The stream is not designated as an impaired waterbody.
Hop Bottom Creek (also known as Hopbottom Creek) is a tributary of Martins Creek in Susquehanna County, Pennsylvania, in the United States. It is approximately long and flows through Bridgewater Township, New Milford Township, Brooklyn Township, Lathrop Township, and Hop Bottom. The watershed of the creek has an area of . The creek is not designated as an impaired waterbody.
Spring Run (also known as The Gut) is a tributary of the West Branch Susquehanna River in Northumberland County, Pennsylvania, in the United States. It is approximately long and flows through Delaware Township and Watsontown. The watershed of the stream has an area of . The stream is designated as an impaired waterbody due to sedimentation/siltation and unknown causes.
Somer Brook is not designated as an impaired waterbody. In August 1995, Somer Brook received several water quality measurements. The water temperature ranged from , with an average of . The pH of the stream ranged from 5.0 to 5.1, with an average of 5.0, and the conductivity ranged from 3.3 to 3.5 uohms/cm with an average of 3.4.
Black Run is a tributary of the West Branch Susquehanna River in Lycoming County and Union County, in Pennsylvania, in the United States. It is approximately long and flows through Brady Township in Lycoming County and Gregg Township in Union County. The watershed of the stream has an area of . The stream is not designated as an impaired waterbody.
Spring Creek is a tributary of White Deer Hole Creek in Lycoming County and Union County, in Pennsylvania, in the United States. It is approximately long and flows through Washington Township in Lycoming County and Gregg Township in Union County. The watershed of the creek has an area of . The creek is not designated as an impaired waterbody.
It is not designated as an impaired waterbody, but it is affected by sediment and nutrients. Spruce Run mainly flows through mountainous terrain and the Spruce Run Reservoir is in its watershed. The watershed of its main stem is mostly forested. There used to be a mill near the stream's mouth and lumbering was done in the surrounding area.
Muddy Run is a tributary of Spruce Run in Union County, Pennsylvania, in the United States. It is approximately long and flows through West Buffalo Township and Buffalo Township. The watershed of the stream has an area of . Part of the stream is designated as an impaired waterbody due to sedimentation and siltation from grazing-related agriculture.
Black Run (also known as Black's Run) is a tributary of Spruce Run in Union County, Pennsylvania, in the United States. It is approximately long and flows through West Buffalo Township and Buffalo Township. The watershed of the stream has an area of . The stream has two unnamed tributaries and is not designated as an impaired waterbody.
Boile Run (also known as Boyle Run) is a tributary of the Susquehanna River in Northumberland County, Pennsylvania, in the United States. It is approximately long and flows through Lower Augusta Township. The watershed of the stream has an area of . The stream is not designated as an impaired waterbody and is a relatively small stream.
Falls Creek is not designated as an impaired waterbody. At the point where Falls Creek drains an area of , its peak annual discharge has a 10 percent chance of reaching . It has a 2 percent chance of reaching and a 1 percent chance of reaching . The peak annual discharge has a 0.2 percent chance of reaching .
Hans Yost Creek is designated as an impaired waterbody for its entire length. The causes of the impairment are metals and pH and the probable source of impairment is abandoned mine drainage. There are two abandoned mine discharges in the creek's watershed. One is known as the Moser Mine Pool Discharge and enters the creek in its upper reaches.
Snow Creek is a tributary of Mahantango Creek in Northumberland County, Pennsylvania, in the United States. It is approximately long and flows through Upper Mahanoy Township and Jordan Township. The watershed of the creek has an area of . The creek has no named tributaries and is not designated as an impaired waterbody in any stream segment.
Sciota Brook is not designated as an impaired waterbody. In an August 2001 study, it was noted to have a low stream flow. In its lower reaches, the pH of Sciota Brook was measured in the August 2001 study to be 7.2, while the alkalinity was . The water hardness was and the specific conductance was 84 umhos.
Little Mehoopany Creek is a tributary of the Susquehanna River in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through Windham Township and Mehoopany Township. The watershed of the creek has an area of , most of which is forested land and agricultural land. No stream in the watershed is designated as an impaired waterbody.
UST Global's campus model Thiruvananthapuram (Kerala) Technopark, Thiruvananthapuram UST Global has started its expansion plans in the capital city Thiruvananthapuram with the construction of an own campus, near Technopark. The campus is spread over . The campus will also feature a waterbody channeling through the various blocks of the campus. One of the main building construction completed.
Bellas Brook (also known as Hiller Brook) 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 is not designated as an impaired waterbody and is classified as a High-Quality Coldwater Fishery.
Wolf Run is not designated as an impaired waterbody. In 2001, the pH of Wolf Run upstream of its mouth was measured to be 7.2, while the alkalinity was . The water hardness of the stream was and the specific conductance was 60 umhos. When the ambient air temperature was , the water temperature was measured to be .
Horton Creek is a tributary of Oxbow Creek in Susquehanna County and Wyoming County, in Pennsylvania, in the United States. It is approximately long and flows through Springville Township in Susquehanna County and Lemon Township and Nicholson Township in Wyoming County. The watershed of the creek has an area of . The creek is not designated as an impaired waterbody.
Dundaff Creek is not designated as an impaired waterbody. At the Lackawanna County/Susquehanna County line, the peak annual discharge of Dundaff Creek has a 10 percent chance of reaching . It has a 2 percent chance of reaching and a 1 percent chance of reaching . The peak annual discharge has a 0.2 percent chance of reaching .
"Bottom feeding coarse fish" must be removed, because they may "uproot plants and disturb sediments." "Appropriate nesting and feeding conditions are maintained" with regard to open land, scrub and reeded areas. "Recreational activities should be managed sympathetically to avoid conflict with the management of the waterbody for nature conservation," and "recreational use of woodland should be discouraged" should the site contain a heronry.
He argued that a nexus exists where the wetland or waterbody, either by itself or in combination with other similar sites, significantly affects the physical, biological, and chemical integrity of the downstream navigable waterway.United States Environmental Protection Agency, Clean Water Act Jurisdiction Following the U.S. Supreme Court's Decision in Rapanos v. United States & Carabell v. United States, December 2, 2008.
A steep sided, rather marshy valley, Greenburn's waters join the River Brathay at Little Langdale Tarn. Greenburn itself bears a tarn, or more correctly the remains of a reservoir. A natural waterbody was dammed in the early 18th century to provide water for the Greenburn Mine. The 250 yard long barrage has now been breached to leave a collection of pools and bogs.
Measurements showed unusual subglacial radar returns, indicating the presence of a waterbody at some 2.6 kilometers depth under the ice. An initial mapping with an ice-penetrating radar confirmed the finding. The research team returned in summer of 2015 and the mapping was completed. The findings were published in a Geophysical Research Letters report by four members of the CECs Glaciology Laboratory.
Somer Brook (also known as Somers Brook) is a tributary of Mehoopany Creek in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through Noxen Township and Forkston Township. The watershed of the stream has an area of . The stream is not designated as an impaired waterbody and is classified as a High-Quality Coldwater Fishery.
Glade Run is a tributary of the West Branch Susquehanna River in Northumberland County and Lycoming County, in Pennsylvania, in the United States. It is approximately long and flows through Lewis Township in Northumberland County and Muncy Creek Township and Muncy in Lycoming County. The watershed of the stream has an area of . The stream is not designated as an impaired waterbody.
After the devastating 1906 San Francisco earthquake, the city decided to reclaim the creek using earthquake debris, reducing the waterbody to its present size. Though much of Islais Creek has been converted to an underground culvert, remnants still exist today at both Glen Canyon Park and Third Street. Several community organizations are dedicated to preserve these remnants, as they are important wildlife habitats.
To the north- west of Bowfell the main ridge drops to the depression of Ore Gap, named after its reddish soil, rich in haematite. Below the col on the northern side is Angle Tarn. This round waterbody occupies a corrie beneath Hanging Knotts, small trout lurking in its 50 ft depths. Its outflow is a tributary of the Langstrath Beck, making for Stonethwaite.
Sand Spring Run is not designated as an impaired waterbody. The average daily discharge of the stream was once found to be approximately . Between water year 1969 and water year 1980, the average annual discharge of the stream ranged from in water year 1969 to in water year 1978. There is a stream gauge on Sand Spring Run near White Deer.
Buttermilk Creek is a tributary of the Susquehanna River in Lackawanna County and Wyoming County, in Pennsylvania, in the United States. It is approximately long and flows through Newton Township in Lackawanna County and Falls Township in Wyoming County. The watershed of the creek has an area of . The creek is a perennial stream and is not designated as an impaired waterbody.
Falls Creek (also known as Falls Creek No. 2) is a tributary of Buttermilk Creek in Lackawanna County and Wyoming County, in Pennsylvania, in the United States. It is approximately long and flows through Newton Township in Lackawanna County and Falls Township. The watershed of the creek has an area of . The creek is not designated as an impaired waterbody.
A few yards to the south is Red Screes Tarn, a small permanent waterbody with no plant life in evidence. A number of smaller pools can be found after rain.Don Blair, Exploring Lakeland Tarns: Lakeland Manor Press (2003): The view is excellent in all directions. Helvellyn is seen to good advantage, beyond the crags of Dove Crag and Fairfield and over Deepdale Hause.
The organisation is known for cleaning the beach stretch between Veli and Vizhinjiam in Thiruvananthapuram part of the Beach Habitat Restoration. Ramanujar Pond Restoration in Kanchipuram. An ancient waterbody, located in front of the Sri Ramanujar Sannadhi at Sevilimedu in Kancheepuram taluk, was revived by the Environmentalist Foundation of India (E.F.I). The work coincided with the 1,000th birth anniversary of Sri Ramanuja.
Hans Yost Creek is a tributary of Deep Creek in Schuylkill County, Pennsylvania, in the United States. It is approximately long and flows through Foster Township and Barry Township. The watershed of the creek has an area of . The creek is designated as an impaired waterbody, with the causes being metals and pH and the probable source being abandoned mine drainage.
North Mahanoy Creek is a tributary of Mahanoy Creek in Schuylkill County, Pennsylvania, in the United States. It is approximately long and flows through Delano Township, Mahanoy Township, and Mahanoy City. The watershed of the creek has an area of . The creek is designated as an impaired waterbody due to sedimentation/siltation and water/flow variation from abandoned mine drainage.
Smith Cabin Run is not designated as an impaired waterbody. In an August 2001 study, the stream was found to be dry except in a single pool. When the ambient air temperature was , the water temperature was measured to be . In the August 2001 study, the pH of Smith Cabin Run upstream of its mouth was 7.0 and the alkalinity was .
About 5,000 years ago the waterbody was cut off from the Baltic by the bar of the Schmale Heide. Its only link to the Baltic is the drainage ditch of the Ahlbeck stream. As a result of natural silting-up processes it is today a shallow lake. In the centre it has a depth of only one to two metres.
It is not designated as an impaired waterbody. The surficial geology in its vicinity mostly consists of Wisconsinan Till, alluvium, Wisconsinan Ice-Contact Stratified Drift, and bedrock. The area near the mouth of Oxbow Creek was settled before 1800 and some mills were constructed on it in the 19th century. A number of bridges have also been constructed across the creek.
Polk Valley Run (also known as Poke Valley Run or Snipe Valley Creek) is a tributary of Saucon Creek in Northampton County, Pennsylvania. It is approximately long and flows through Lower Saucon Township and Hellertown. The watershed of the stream has an area of . A reach of the stream is designated as an impaired waterbody due to siltation from agriculture.
Monroe Creek (also known as Bartholomew Creek) is a tributary of Tunkhannock Creek in Susquehanna County and Wyoming County, in Pennsylvania, in the United States. It is approximately long and flows through Springville Township in Susquehanna County and Nicholson Township in Wyoming County. The watershed of the creek has an area of . The creek is not designated as an impaired waterbody.
Dundaff Creek is a tributary of East Branch Tunkhannock Creek in Susquehanna County and Lackawanna County, in Pennsylvania, in the United States. It is approximately long and flows through Clifford Township in Susquehanna County and Greenfield Township in Lackawanna County. The watershed of the creek has an area of . The creek has no named tributaries and is not designated as an impaired waterbody.
Further upstream, the surficial geology is mostly Wisconsinan Till, except for Lake Idlewild, a wetland, and some patches of bedrock consisting of sandstone and shale on nearby hills. A lake known as Lake Idlewild is located in the watershed of Idlewild Creek. The designated uses of the lake are aquatic life and potable water. Idlewild Creek is not designated as an impaired waterbody.
Butler Creek is a tributary of Nine Partners Creek in Susquehanna County, Pennsylvania, in the United States. It is approximately long and flows through Jackson Township, Gibson Township, and Harford Township. The watershed of the creek has an area of . The creek has one named tributary, which is known as Little Butler Creek, and is not designated as an impaired waterbody.
View of the dam that impounds the upper Salmon River Reservoir, October 2008. The Salmon River Reservoir, also known as the Redfield Reservoir, is a man-made waterbody in Oswego County (). The reservoir was created with the completion of a hydroelectric dam in 1912. It covers an area of with a maximum depth of and has the capacity to hold of water.
Dalmatia Creek is designated as an impaired waterbody. The cause of impairment is sedimentation/siltation and the probable sources of impairment are crop- related agriculture and removal of vegetation. The peak annual discharge at the mouth of Dalmatia Creek has a 10 percent chance of reaching . It has a 2 percent chance of reaching and a 1 percent chance of reaching .
Boyers Run is a tributary of the Susquehanna River in Juniata County and Perry County, in Pennsylvania, in the United States. It is approximately long and flows through Susquehanna Township in Juniata County and Liverpool Township in Perry County. The watershed of the stream has an area of . The stream has one unnamed tributary and is not designated as an impaired waterbody.
Leiningers Run is a tributary of West Branch Mahantango Creek in Juniata County, Pennsylvania, in the United States. It is approximately long and flows through Greenwood Township and Susquehanna Township. The watershed of the stream has an area of . A reach of the stream is designated as an impaired waterbody due to miscellaneous habitat alteration from habitat modifications not including hydromodification.
Further west the Seiont and Gwyrfai empty into the western end of the Menai Strait. A part of the east of the national park is within the upper Dee (Dyfrydwy) catchment and includes Bala Lake or Llyn Tegid, the largest natural waterbody in Wales. A fuller list of the rivers and tributaries within the area is found at List of rivers of Wales.
Bennys Run (also known as Buddys Run or Benny's Run) is a tributary of Shamokin Creek in Northumberland County, Pennsylvania, in the United States. It is approximately long and flows through Shamokin Township. The watershed of the stream has an area of . The stream is not designated as an impaired waterbody and it has a relatively high level of water quality.
Bennys Run is not designated as an impaired waterbody. The engineering department of the Pennsylvania Department of Transportation once received an NPDES permit to discharge stormwater into the stream for construction purposes. However, in 2005 and 2006, the Pennsylvania Department of Environmental Protection received complaints about untreated sewage discharge into the creek. The estimated flow of sewage into the stream was per day.
It is not designated as an impaired waterbody and is a freestone stream in its upper reaches. The topography of the watershed has been described as "rough and hilly". Numerous small lakes and swamps occur in the watershed of East Branch Tunkhannock Creek. These include Handsome Pond, Robinson Lake, Harding Pond, Tamarack Swamp, Tea Pond, two lakes named Mud Pond, Idlewild Lake, and Coterell Lake.
Studies conducted by DEQ, USGS, the City of Gresham, and other public agencies have identified DDT (dichloro-diphenyl-trichloroethane), dieldrin, polychlorinated biphenyls (PCB), chlordane, and polycyclic aromatic hydrocarbons (PAH) as carcinogenic pollutants of Johnson Creek. The creek has been classified as a "waterbody of concern" by the DEQ because of elevated levels of copper, chromium, and nickel in water and sediments. Generally, metal concentrations increase downstream.
There are about 2,000 families living in the southern bund. Even though some have toilets in the backyard, they conveniently direct the pipelines to the lake, causing extensive damage to the waterbody. The government's efforts to relocate the encroachers has not yielded satisfactory results. Corporation officials said they were trying to convince encroachers to get sewer connections by paying a nominal fee of Rs 100.
It is the sole hydrodynamic model listed in the model selection tool database for hydrodynamic and chemical fate models that can perform 1-D, 2-D, and 3-D time-variable modeling for most waterbody types, consider all state variables and include the near- and far-fields. GEMSS can also provide GUI’s, grid generation, and GIS linkage tools and has strong documentation.Fitzpatrick, J., et al.
San Diego Coastkeeper was launched in 1995 as San Diego Baykeeper in order to combat chronic pollution of San Diego Bay that transformed a once-thriving ecosystem into a highly toxic waterbody. Baykeeper became the 15th approved Waterkeeper program in the country. In 2005, San Diego Baykeeper became San Diego Coastkeeper, whose mission now encompasses protecting all of San Diego County’s bays, beaches, watersheds and ocean.
106 species of fish recorded in the lake consist of 61 genera, 17 families and 5 orders. The three lakes, also called the Slam Pe in the local Tày ethnic language, that form Ba Bể lake are called the Pé Lầm, Pé Lù, and Pé Lèng; all linked as one waterbody. The lake’s central part is contracted while its outer two parts are wider.
Horton Creek is a tributary of Tunkhannock Creek in Susquehanna County and Wyoming County, in Pennsylvania, in the United States. It is approximately long and flows through Brooklyn Township and Lathrop Township in Susquehanna County and Nicholson Township and Nicholson in Wyoming County. The watershed of the creek has an area of . The creek is not designated as an impaired waterbody and has no named tributaries.
To the west a long shoulder of land falls gradually between Nether Beck and Over Beck, narrowing as they converge toward the shore of Wastwater. In the middle of the plateau is Low Tarn, a large shallow waterbody lying in a flat basin. It drains via Brimfull Beck into Over Beck. This whole area is unfrequented with few paths amongst the grassy hillocks and low crags.
Spruce Run is not designated as an impaired waterbody. Even though the nearby Buffalo Creek headwaters, which are just across a mountain from Spruce Run, are affected by acid deposition, Spruce Run itself is not affected by it. However, it is still impacted by nutrient pollution and sediment. The sediment load of Spruce Run and its tributary Black Run was in 2000 and in 2008.
Beaver Run is as degraded as some impaired tributaries of Buffalo Creek. However, Beaver Run was not designated by the Pennsylvania Department of Environmental Protection as an impaired waterbody until 2008. A total of of the stream and its tributaries are impaired. Despite this, it is not a major contributor of degradation to the main stem of Buffalo Creek, due to its low discharge.
Leonard Creek (also known as Leonards Creek or Leonard's Creek) is a tributary of Bowman Creek in Luzerne County and Wyoming County, in Pennsylvania, in the United States. It is approximately long and flows through Dallas Township in Luzerne County and Monroe Township in Wyoming County. The watershed of the creek has an area of . The creek is not designated as an impaired waterbody.
Boile Run is not designated as an impaired waterbody. At least one person has a National Pollutant Discharge Elimination System to discharge sewage into an unnamed tributary of the stream from a single residence. The peak annual discharge of Boile Run at its mouth has a 10 percent chance of reaching . It has a 2 percent chance of reaching and a 1 percent chance of reaching .
Rausch Creek is designated as an impaired waterbody, with the cause of the impairment being metals and the probable source being abandoned mine drainage. Rausch Creek flows through a water gap, and several mountains are in the vicinity of the creek. The watershed of Rausch Creek experienced extensive deep mining in the early 20th century. There are still several active mining permits in the watershed.
Beaver Creek is a tributary of Buttermilk Creek in Lackawanna County and Wyoming County, in Pennsylvania, in the United States. It is approximately long and flows through West Abington Township in Lackawanna County and Overfield Township and Falls Township in Wyoming County. The watershed of the creek has an area of and contains Lake Winola. The creek is not designated as an impaired waterbody.
NY 414 southbound in Hector just past the NY 79 junction. This section of the route overlooks Seneca Lake (at right) as it heads downhill. The route initially heads east from Watkins Glen to skirt the southern edge of the lake, but turns north upon exiting the village and passing the southeastern tip of the waterbody. Just outside Watkins Glen, NY 414 comes to a fork.
Mill Run (also known as Osterhout Creek or Osterhouts Creek) is a tributary of the Susquehanna River in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through Tunkhannock Township and Overfield Township. The stream is not designated as an impaired waterbody. In its upper reaches, it flows through glacial drift, while in its lower reaches, it passes over a waterfall.
The entire length of West Branch Rausch Creek is designated as an impaired waterbody. The cause of the impairment is metals and the probable source is abandoned mine drainage. Despite being impacted by abandoned mine drainage, the creek is not impacted by sediment, unlike the nearby East Branch Rausch Creek. The average discharge of West Branch Rausch Creek near its mouth is per day.
Little Meshoppen Creek is a tributary of Meshoppen Creek in Susquehanna County and Wyoming County, in Pennsylvania, in the United States. It is approximately long and flows through Auburn Township in Susquehanna County and Messhoppen Township and Messhoppen in Wyoming County. The watershed of the creek has an area of . The creek is a Coldwater Fishery and Migratory Fishery and is not designated as an impaired waterbody.
Douglas Hollow is not designated as an impaired waterbody. At a site upstream of its mouth, Douglas Hollow was observed in 2001 to have a pH of 7.2 and an alkalinity concentration of . The water hardness was and the specific conductance was 136 umhos. In a measurement in August 2001, when the air temperature nearby was , the water temperature in the stream's lower reaches was .
Farr Hollow (also known as Farr Hollow Run) is a tributary of North Branch Mehoopany Creek in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through Windham Township and North Branch Township. The watershed of the stream has an area of . The stream is not designated as an impaired waterbody and flows through a mixture of forested and agricultural land.
Farr Hollow is not designated as an impaired waterbody. In 2001, measurements of pH near the source and mouth of Farr Hollow were 7.4 and 7.0, respectively. Measurements of alkalinity were , with the higher value in the upper reaches. The total water hardness of the stream was near the source and near the mouth, while the specific conductance at these locations was 266 and 135 umhos, respectively.
Nassawango Creek is a stream in the U.S. state of Maryland; it is the largest tributary of the Pocomoke River, located on the Delmarva Peninsula. Older variations on the same name include Nassanongo, Naseongo, Nassiongo, and Nassiungo, meaning "[ground] between [the streams]".Runkle, Stephen A. Native American Waterbody and Place Names within the Susquehanna River Basin and Surrounding Subbasins Publication 229. Susquehanna River Basin Commission, September 2003.
Cherry Ridge Run is a tributary of Mehoopany Creek in Luzerne County and Wyoming County, in Pennsylvania, in the United States. It is approximately long and flows through Fairmount Township in Luzerne County and Forkston Township in Wyoming County. The watershed of the stream has an area of . The stream is not designated as an impaired waterbody and has a pond known as Wild Fowl Pond.
In addition to height and climate, other factors are the layering of the rock, its gradient and aspect, the types of waterbody and the lines of dislocation. For hard rock massifs, rugged rock faces (e.g. in the Dolomites) and mighty scree slopes are typical. By contrast, flysch or slate forms gentler mountain shapes and kuppen or domed mountaintops, because the rock is not porous, but easily shaped.
Ackerly Creek is a tributary of South Branch Tunkhannock Creek in Lackawanna County, Pennsylvania, in the United States. It is approximately long and flows through South Abington Township, Waverly Township, Glenburn Township, Dalton, and La Plume Township. The creek has several unnamed tributaries and drains an area of nearly . Ackerly Creek is not designated as an impaired waterbody, but it is impacted by some water quality problems.
Lake Jean was historically rendered acidic by atmospheric deposition. In the summer of 1991, its pH was found to be 5.8, less than the minimum of 6.0 needed to attain its designated uses for aquatic life. The lake was listed as an impaired waterbody for this reason in 1996. By 2007, the pH had increased to 6.5 to 7.4, within Pennsylvania's criteria for pH.
Lake Maardu (; also known earlier as Lake Liivakandi) is a lake on the southern side of the town of Maardu, in northern Estonia. It has an area of , max. depth is and the lake is above sea-level. Lake Maardu was a natural waterbody before 1894 when the landowner of Maardu Manor Otto von Brevern dug a ditch () to the sea and the lake run empty.
After Parikshit was seated on the throne of Hastinapur and the Pandavas along with Draupadi had reached heaven, Subhadra and Uttarā went to the forests to live as hermits. It is believed they died of natural causes in the forest. Another version of the story is that Krishna, Subhadra and Arjun went to a waterbody. Krishna asked Arjun to push Subhadra into the pond.
Lake Clarrie Hall provides valuable public recreation including swimming, sailing, boating and freshwater fishing, including sports fishing for Australian bass. Boat access for electric outboard and paddle-powered craft is available at Crams Farm, at the southern end of the waterbody. Lake Clarrie Hall has been stocked with more than Australian bass fingerlings over the past 10 years. A fishing licence is required to fish in the lake.
Several pairs of the bird may forage in close proximity on a single waterbody. Large flocks form in winter and a flock of nearly 6000 was recorded at Chilka lake. This species feeds mainly at the surface of the water. Stomach analysis showed that they fed on small fishes Puntius, Mystus, Oryzias, molluscs, crustaceans, insect larvae as well as plant matter from species such as Ipomoea, Hydrilla and Ruppia.
North Branch Shamokin Creek (also known as Beaver Creek) is a tributary of Shamokin Creek in Columbia County and Northumberland County, Pennsylvania, United States. It is approximately long and flows through Conyngham Township in Columbia County and Mount Carmel Township in Northumberland County. The watershed of the creek has an area of . The entirety of the creek is designated as an impaired waterbody due to metals from abandoned mine drainage.
The Salamandre Lake is a freshwater body of the municipality of Eeyou Istchee Baie-James (municipality), in the administrative region of Nord-du-Québec, at Quebec, in Canada. The northern part of the lake is crossed to the West by the Broadback River. Forestry is the main economic activity of the sector. Recreational tourism activities come second with an upstream navigable waterbody including the Broadback River and the Nipukatasi River.
Green Creek is not designated as an impaired waterbody. The waters of Green Creek considerably increase the flow of Fishing Creek at Orange Township. In 1841, the creek was described as a "considerable stream" with water power of "no little magnitude". At a site in the upper reaches of Green Creek, where its watershed has an area of , the creek's average daily discharge was once measured to be .
"The water is totally contaminated and not conducive for boating. At present, stormwater drain works are in progress near the lake, which we hope will put an end to illegal discharge of sewage from residential areas. It could be dangerous for children to go on a boat ride on the contaminated waterbody," corporation commissioner D Karthikeyan told TOI. The ambitious programme of the corporation was conceived three years ago.
The Ching is classified by the Environment Agency as a Heavily Modified Waterbody, and when last studied, while in good condition on chemical standards, was deemed to be only of moderate ecological quality status, with multiple reasons for quality issues identified. In 2009, Thames Water announced a study aimed at reducing pollution of the river in its lower reaches caused by domestic waste water from sinks, showers, dishwashers, and washing machines.
It is a deep waterbody measuring wide at its northern end and over at its southern end. The inlet connects Lancaster Sound in the north with the Gulf of Boothia in the south. Davis Strait is a narrow and relatively shallow area connecting Baffin Bay in the north with the Labrador Sea in the south. It varies in width from to over , with the shallowest waters found along the Davis Sill.
The Totsu Wozhu which is situated in the southern part of the Phiru-shaki area is the largest amongst these but occupies merely around an acre of land. Other similar natural lakes are situated in the Sanis and Mekokla areas. The lake created by the Doyang dam is the biggest manmade waterbody in the district. There are no permanent waterfalls in the district though several are formed during the monsoons.
Reaches of Little Mahantango Creek are designated as an impaired waterbody. The cause of the impairment is sedimentation/siltation and the probable source is agriculture. The entirety of the creek and all of its unnamed tributaries and sub-tributaries are designated as impaired. In July 1998, the water temperature of Little Mahantango Creek near Pitman was once measured to be , while at Line Mountain, it was measured to be .
Its designated use is for aquatic life. Cherry Ridge Run is not designated as an impaired waterbody. As of 2011, it is one of five named streams in the Mehoopany Creek watershed that have not been assessed by the Pennsylvania Fish and Boat Commission. A pair of adult bald eagles have been observed at Wild Fowl Pond on Cherry Ridge Run, as well as four hooded mergansers and eight buffleheads.
Retrieved on 13 Jun 2013 Forebays have a number of functions. They are used in flood control to act as a buffer during flooding or storm surges, impounding water and releasing in a controlled way into the larger waterbody. They may be used upstream of reservoirs to trap sediment and debris (sometimes called a sediment forebaySediment Forebays at www.greenworks.tv. Accessed on 14 Jun 2013) in order to keep the reservoir clean.
Here, NY 220 turns southeast at Steere Road (unsigned NY 991A) and continues into Preston. Where NY 991A heads north to serve Bowman Lake State Park. Southern terminus of the NY 12 / NY 220 overlap in Oxford In Preston, the open fields return as NY 220 follows another waterbody, this time the slightly larger Mill Brook. The route crosses the stream just before entering the town of Oxford, where they split.
NGOs, including the Society for Protection of the Harbour, were formed to resist further attempts to reduce the size of the waterbody, with its chairman, Christine Loh, quoted as saying that the harbour "...is a precious national asset and we must preserve it for future generations. I believe an insightful and visionary chief executive would support our stance and work with us to protect the harbour".Harbourprotection. "Harbourprotection ." Love Harbour Day.
In 14 measurements between 1962 and 1978, the discharge of Polk Valley Run at Hellertown ranged from . All but three measurements were under . Between the early 1960s and the early 1980s, the peak annual discharge of the stream ranged from just over to nearly one year in the mid-1970s. A reach of Polk Valley Run is designated as an impaired waterbody due to siltation from agricultural activity.
There is also a small patch of Wisconsinan Ice-Stratified Drift in the middle reaches and a larger one near the headwaters. The surficial geology on the sides of the valley mainly consists of Wisconsinan Till, with a small lake above the headwaters and one patch of bedrock consisting of sandstone and shale on the Tinker Hill side of the valley. Tinker Hollow is not designated as an impaired waterbody.
Fidlers Run (also known as Fiddlers Run, Fidler Run, or Fidlers Creek) is a tributary of the Susquehanna River in Northumberland County, Pennsylvania, in the United States. It is approximately long and flows through Jackson Township and Lower Mahanoy Township. The watershed of the stream has an area of . The stream is not designated as an impaired waterbody, although a reaches of a few of its unnamed tributaries are.
Hoffer Creek is designated as an impaired waterbody. The cause of the impairment is sedimentation/siltation and a probable of the impairment is grazing-related agriculture. As of the early 2010s, the sediment load in Hoffer Creekincluding an adjacent unnamed tributary to the Susquehanna Riveris per year, or per day. This requires a 5 percent reduction to meet the creek's total maximum daily load for sediment: per day, or per year.
The creek is not designated as an impaired waterbody and is a relatively large stream, contributing a significant amount of water to Fishing Creek. A valley known as the Greenwood Valley is located in the vicinity of Green Creek. The creek's own valley was likely affected by glaciation during the Ice Age. Soil erosion is a significant concern in some areas of the watershed of Green Creek, especially in the Greenwood Valley.
The Schwarzer See is a lake on the German Baltic Sea island of Rügen. It belongs to the municipality of Sellin and is located in the Granitz Forest. The lake has an area of 23 hectares, a greatest depth of 15 metres and the elevation of its water surface above sea level is . The lake, which is poor in nutrients, is one of the very rare types of waterbody, a so-called kettle lake (Kesselsee).
East Branch Field Brook is not classified as an impaired waterbody. An Erosion and Sediment Control permit has been issued to Williams Field Services Company, LLC, for which one of the receiving streams is East Branch Field Brook. Chief Gathering, LLC once requested a permit to construct and maintain a pipeline for natural gas and a two timber mat bridges across the stream. One crossing would impact of the stream and the other would impact .
The stream order or waterbody order is a positive whole number used in geomorphology and hydrology to indicate the level of branching in a river system. There are various approachesKoschitzki, 2.3, pp. 12ff to the topological ordering of rivers or sections of rivers based on their distance from the source ("top down"Weishar, p. 30.) or from the confluence (the point where two rivers merge) or river mouth ("bottom up"Weishar, p.
The significant majority of the fish observed at both sites were adults. Miller Run has an extremely low concentration of benthic macroinvertebrates in all of its reaches. On a scale of 0 to 100, various sites on Miller Run had an IBI score of 14.47 to 25.82 (values below 63 indicate an impaired waterbody). The biodiversity levels of the macroinvertebrates are also very low; the Shannon Diversity Index scores range from 0.607 to 1.726.
South Branch Tunkhannock Creek is not designated as an impaired waterbody and has relatively good water quality. The topography of the watershed of South Branch Tunkhannock Creek has been described as "rough and hilly" and the underlying geology consists of interbedded sedimentary rock. There is a gorge with a depth of on the creek at one point. Major land uses in the watershed of South Branch Tunkhannock Creek include forested land and agricultural land.
Heleioporus albopunctatus has terrestrial egg deposition. Males excavate burrows up to 1 m deep in sandy substrates surrounding ephemeral waterbodies, and commence calling in autumn (March/April). Amplexus (mating) occurs in the burrow and females deposit a clutch of eggs embedded in foam, in a chamber at the base of the burrow. Eggs develop to mid-stage tadpoles within the eggs, but final development is dependent on winter rains filling the waterbody and flooding burrows.
The lake disappears by the summer, and is the only known example in Britain. Pant-y- Llyn turlough occupies a small depression on the northern perimeter of the South Wales Coalfield at Cernydd Carmel. This depression represents a glacial channel formed along the Betws Fault where displacement has brought Carboniferous Limestone into contact with older impervious Devonian rock. The hydrological regime of the waterbody is linked to local groundwater behaviour within the limestone.
Named after the Oneida word for bull thistle,Runkle, Stephen A. Native American Waterbody and Place Names within the Susquehanna River Basin and Surrounding Subbasins Publication 229. Susquehanna River Basin Commission, September 2003. in the 19th century the Chenango furnished a critical link in the canal system of the northeastern United States. The Chenango Canal, built from 1836–1837 between Utica and Binghamton, connected the Erie Canal in the north to the Susquehanna River.
This major tourist project was initiated in the early 1970s by the head of the county council of St. Wendel, Werner Zeyer, who later became the minister president of the Saarland. The long term aim was to strengthen the tourist infrastructure in the county of St. Wendel in order to raise the number of tourists. In addition, the new waterbody was intended to extend the local recreation facilities and improve the ecology.
Below these trees the river broadens into the oddly shaped Kentmere Tarn. A natural waterbody was drained in the 1830s to extend the available farmland, but the scheme failed and merely resulted in an area of marsh. It was later found that the tarnbed was rich in diatomite, a mineral used to produce thermal insulation. Extraction began in the 1930s and continued until 1971, producing the lines of the present man-made tarn.
The Kakkayur Temple pond is a major waterbody that serves for the bathing and washing needs of a majority of people in this village. The huge tank is also a training place for the local swimming team, some of whom are national level champions. The pond was renovated at a cost of 20 Lakh Rupees by the Residents in 2016 - The project was executed by an action committee presided by Sri. Sundareswaran Marar.
The lake is part of the Moates Lake System along with Moates Lake and Lake Gardner. All of these lakes were linked to form a large estuarine system during the last interglacial period approximately 120,000 years ago. The main waterbody covers a maximum area of but the associated wetlands cover an area closer to . The area south of the lake was drained with a channel being constructed to connect it with Gardner Creek.
Several designations of this body of water have been known since the beginning of the 20th century. The map of the province of Quebec (1911) by James White, accompanying the ninth report of the Geographical Survey of Canada, refers to this waterbody "L. Geikie", of unknown origin. The "Dictionary of Rivers and Lakes of the Province of Quebec" (edition of 1914) uses the designation "Lake Geikie" under the heading "Mill River" (today Théodat).
Fidlers Run is not designated as an impaired waterbody. Some of its unnamed tributaries are not designated as impaired waterbodies. However, reaches of some of the stream's unnamed tributaries are in fact designated as impaired, due to siltation from agriculture and grazing- related agriculture. At the downstream limit of the stretch of Fidlers Run that is on the border of Lower Mahanoy Township, the stream's peak annual discharge has a 10 percent chance of reaching .
European Council Directive 92/43/EEC of 21 May 1992 on the conservation of natural habitats and of wild fauna and flora. detection and assessment of invasive species; mapping and assessment of forest resources; assessment of forest vitality; landscape planning and management; detection and assessment of archaeological heritage; holistic assessment and restoration of aquatic ecosystems; mapping and assessment of waterbody depth and sediments; research of fish migration and natural reproduction; wildlife mapping and modelling; future satellite simulation.
The entire length of Coal Run is designated as an impaired waterbody. The cause of the impairment is metals and the source of the impairment is abandoned mine drainage. The stream is one of several in the watershed of Shamokin Creek to be impacted by abandoned mine drainage, although it is not seriously impacted. However, it is fairly consistently neutral or alkaline, with an average pH of 6.5, though its pH can be as low as 4.8.
Ponden Reservoir is an artificial upland lake in the Worth Valley, near Stanbury, West Yorkshire, England. Ponden was built as a compensation reservoir after the nearby Watersheddles Reservoir (upstream) was used to divert water away from the River Worth. Ponden was needed to regulate the flow of water down the river into the downstream mills in the valley. The reservoir is owned and managed by Yorkshire Water, and is used as a recreational waterbody by a sailing club.
In 1975, a young girl named Manjhri is married off to a small village in the middle of nowhere in the Rann of Kutch. There, she joins a group of women shackled by patriarchal mandates. Their only escape from the suppression is when they go out to fetch water at a distant waterbody every morning. Other than those few hours everyday, their lives are bound by the rules made by men which they have to abide by.
Travelling south from the Eskdale rim the tops are Kepple Crag, Great Whinscale, Crook Crag (1,538 ft), Green Crag and White How. The crest then turns west toward the Fell Road, passing over Great Worm Crag (1,400 ft), considered by some to be a separate fell. To the west of the summit ridge is Low Birker Pool, a tarn which feeds Birker Force. This shallow waterbody is contained by a low moraine and overlooked by Tarn Crag.
The principal tops are Ancrow Brow (1,820 ft), White Howe (1,738 ft), Lords Seat (1,719 ft) and Great Yarlside (1,950 ft). These ridges encompass the valleys of Bannisdale, Crookdale, Wet Sleddale, Borrowdale and Wasdale, the latter two of which should not be confused with their more famous Lakeland counterparts. To the north of the summit is a marshy depression, containing Greycrag Tarn. This is a series of small pools in the bed of a larger historic waterbody.
Moel Oernant is a high hill in the community of Trawsfynydd in the county of Gwynedd in North Wales. It has a number of western tops, the highest of which reaches a height of overlooking the waterbody known as Llyn Gelli-Gain and another at Frîdd Wen exceeds . To the south of the lake is the top of Pîg Idris which reaches 429m. The minor top of Y-Foel attains 430m to the northeast of Moel Oernant.
Nonetheless, repeated applications are necessary, and spraying floating leaves shows 40-50% control for a single season. Dichlobenil is more effective than glyphosate in controlling N. peltata. The application of the chemical in the spring during emergence coupled with mechanical removal of floating leaves and repeated dichlobenil applications has been successful. However, the producers of dichlobenil advise not to treat more than 20% of a waterbody and to not treat areas where flow exceeds 90m/hour.
In 2014, Waste Management of Pennsylvania, Inc. was issued an Erosion and Sediment Control Permit for which the receiving waterbody is Derr Run. In 2007, the US Gypsum Company was issued a permit to build, maintain, and operate a long natural gas pipeline crossing the stream in two places, as well as crossing other streams. However, one of the crossings of Derr Run was planned to involve no impact to the stream; the other was planned to impact .
Gladhouse Reservoir covers an area of meaning it is the largest freshwater area in the Lothians. It is a sizeable, rather shallow waterbody which contains two small islands, lying at an altitude of above sea level at the foot of the Moorfoot Hills. The dam and associated construction were made out of pink sandstone and was designed to contain up to "1700 million gallons". At the time this was regarded as a notable feat of engineering.
The pit blind can be a solid structure that is placed into a hole in the ground or on the bank of a waterbody. Since pit blinds rest below the top of the surrounding soil, some structural strength is required to prevent the soil from collapsing into the blind. Commercially available blinds can be made from fiberglass, polyethylene or even lightweight metals. Homemade blinds can also be constructed of wood, but typically cannot withstand the moisture of an underground habitat.
The southern perimeter is formed by Seathwaite Tarn and its attendant streams. The tarn was originally a much smaller waterbody, but was raised early in the 20th century to provide drinking water for the Barrow in Furness area. The dam is almost 400 yards long and is concrete cored with slate buttresses, the resulting depth of the tarn being around 80 ft. Water is not abstracted directly from the tarn, but flows some distance downriver to an off-take weir.
The Schwentine Oxbow Lake (Altarm der Schwentine) is a part of the Schwentine that has been designated as nature reserve since 1984.einzigartig – Naturführer durch Schleswig Holstein, Landesamt für Natur und Umwelt des Landes Schleswig- Holstein (editor), Wachholtz Verlag, Neumünster 2008, , p. 13 (in German) It received this conservation status because the waterbody has remained close to its natural state due to its steep river banks and is a habitat for a range of rare plants and animals. It covers an area of .
Rapid Run is a tributary of Buffalo Creek in Centre County and Union County in Pennsylvania, in the United States. It is approximately long and flows through Miles Township in Centre County and Hartley Township, Lewis Township, West Buffalo Township, and Buffalo Township in Union County. The watershed of the stream has an area of . Some streams in the watershed are impacted by nutrients, sediment, E. coli, and thermal radiation and one unnamed tributary is designated as an impaired waterbody.
Red-backed shrike, male - one of the species that occur in the nature reserve The Schwentine Oxbow Lake () is an area around part of the River Schwentine between Raisdorf and Klausdorf that was designated a nature reserve in 1984.Landesamt Schleswig Holstein, p. 13 It received this conservation status because the waterbody has remained close to its natural state due to its steep river banks and is a habitat for a range of rare plants and animals. It covers an area of .
West Branch Rausch Creek was entered into the Geographic Names Information System on August 2, 1979. Its identifier in the Geographic Names Information System is 1190927. A concrete slab bridge carrying Bear Valley Road was constructed across West Branch Rausch Creek in 1973 and is long. In 1996, two companiesWenrich Coal Co. and D. and F. Deep Mine Coal Co.applied for renewal of permits for existing anthracite deep mine operations for which the receiving waterbody was West Branch Rausch Creek.
Lindell Beach is a rural farming community in the Columbia Valley of the Lower Mainland region of the province of British Columbia, Canada, lying south of the City of Chilliwack.BC Names entry "Lindell Beach (community)" It is located at the south end of Cultus Lake which is the main waterbody in the Columbia Valley, and just north of the boundary of the United States. From 2014 to 2019 the area has seen a significant increase in population due to several gated community developments.
Cronin and Kennedy, p.45 The HRFA was growing and many members now spread its message to communities and public officials. Richie Garrett, HRFA's president, was a local grave-digger from Ossining, NY who had grown up along the Croton River, fishing and living by means of this waterbody. By his involvement in the HRFA, he grew as an activist by writing letters and presenting slide shows of fish kills and pollution at venues from garden club meetings to Knights of Columbus halls.
East of Barneveld, a village in eastern Oneida County, NY 365 is a rural connector road that runs along the Hinckley Reservoir, a waterbody that extends into Herkimer County and Adirondack Park. Modern NY 365 was originally designated as part of several routes in the 1930 renumbering of state highways in New York. One of these was New York State Route 287, which extended from Barneveld to Ohio via Prospect. NY 365 itself was assigned in 1932, utilizing its current alignment from Verona to Barneveld.
Lake Alamosa is a former lake in Colorado. It existed from the Pliocene to the middle Pleistocene in the San Luis Valley, fed by glacial meltwater from surrounding mountain ranges. Water levels waxed and waned with the glacial stages until at highstand the lake reached an elevation of and probably a surface of over , but only sparse remains of the former waterbody are visible today. The existence of the lake was postulated in the early 19th century and eventually proven in the early 20th century.
The National Art Gallery arranges painting exhibitions at the Old Government House, the former residence of the Governor General. A collection of historical importance can be seen at the National Archives which is open to the public. The Botanical Gardens of the National Art Gallery is popular for afternoon strolls, and is noted for its orchids and shrubs. It houses a herbarium, a lily studded waterbody, walkways, and the Watapamu village, representing a typical village of the islands, which is named after the water pump located nearby.
Greenburn itself bears a tarn, or more correctly the remains of a reservoir. A natural waterbody was dammed in the early 18th century to provide water for the Greenburn Mine. The 250 yard long barrage has now been breached to leave a collection of pools and bogs.Blair, Don: Exploring Lakeland Tarns: Lakeland Manor Press (2003): The mines in question, also known as New Coniston Mine, were worked for copper from 1845 until substantially abandoned in 1865, the shafts reaching a depth of 700 ft below ground.
The American Mediterranean Sea is a name for the combined watershed of the Mississippi River Basin and the waterbody of the Caribbean Sea and the Gulf of Mexico.Sverdrup, H. U., M. W. Johnson and R. H. Fleming; The Oceans Their Physics, Chemistry, and General Biology, Prentis-Hall, 1942, pp. 15, 35 and 637-643 The name is not recognized by the USGS, the International Hydrographic Organization or other international hydrological bodies. The American Mediterranean has a surface area of 4.319 million km2 and an average depth of .
NY 338 began at an intersection with NY 40 in South Argyle, a hamlet within the town of Argyle. The highway headed eastward, passing over hills and intersecting with several local roadways. As NY 338 approached Cossayuna Lake and entered the town of Greenwich, it intersected with CR 48, the primary roadway along the western edge of the lake. NY 338 continued east along the southern extents of the waterbody to the lakeside hamlet of Cossayuna, then turned south toward the hamlet of East Greenwich.
The toponym "Troilus lake" evokes the work of life of Troilus de La Roche de Mesgouez (around 1540-1606), viceroy "so-called Terres-Neuves". His title of lieutenant-general "of the countries of Canada, Newfoundland, Labrador and Norembegue", received in 1598, conferred him the property of the country and the monopoly of the trade. Troilus is the name of the godfather of La Roche, Troilus de Mondragon, Spanish colonel. In 1945, the Quebec Geography Commission attributed the name of Troilus to this waterbody, previously designated Lake Seven.
Fox Sagar Lake, also Jeedimetla Cheruvu or Kolla Cheruvu, is a manmade lake and was the largest waterbody in Secunderabad. It was once spread over an area of . As of today, due to encroachment, it only occupies surface area of over . . The lake which is located Jeedimetla near Kompally was built in 1897 and as per some sources the lake still occupies a surface area of and some sources claim that it is the second biggest lake in Hyderabad and was a popular spot for picnics..
Direct developing eggs of Raorchestes jayarami. thumb Raorchestes jayarami, also known as Jayaram's Bush Frog, is a species of frog from the subfamily rhacophoridae found in Valparai in the Western Ghats of Tamil Nadu in India. Individuals of this species from the genus Raorchestes have morphs that range from plain green to variations with splotches and dots of darker greens and in some cases yellow. Anuran's from the genus Raorchestes, show direct- development while allows them to be independent from a waterbody for the development of tadpoles.
Rausch Creek is designated as an impaired waterbody throughout its entire length. The cause of the impairment is metals and the probable source is abandoned mine drainage. The creek is a major contributor of abandoned mine drainage to Pine Creek, the largest tributary of Mahantango Creek. The iron load in the creek requires a 92 percent reduction to meet the creek's total maximum daily load requirements, while the manganese load requires a 78 percent reduction and the aluminum load requires an 83 percent reduction.
To the west long and gentle slopes run down from the summit of Dow Crag toward the Duddon, while further north on this flank is Seathwaite Tarn. The ground here also begins in a shallow descent, but turns steep above the tarn in a line of minor crags. Seathwaite Tarn is a reservoir in a side valley of the Duddon system. This was originally a much smaller waterbody, but was dammed early in the 20th century to provide drinking water for the Barrow in Furness area.
A subsequent archaeological investigation at the discovery site in the same year returned further helmet pieces. Analysis of remains during the 1940s determined that the wooden tray was of ash, and that there may have been a feather trim to the helmet. The first technical report on the helmets was published by Norling-Christensen in 1946. It is thought that the Brøns Mose was a lake in the Bronze Age, and an extension of the modern Løged Sø waterbody - making the helmets a likely bog votive offering.
A reach of East Branch Saucon Creek is designated as an impaired waterbody. The cause of impairment is unknown, and probable sources include industrial point source discharge and urban runoff/storm sewers. The sediment load in East Branch Saucon Creek has been found to be 3861 tons per year at the creek's mouth and 2289 tons per year further upstream, at the Northampton Sportsman's Club. Two sites in the upper reaches of the creek's watershed had sediment loads of 511 and 108 tons per year.
The Steinhuder Meer Nature Park lies south of Nienburg/Weser, west of Neustadt am Rübenberge, northwest of Wunstorf, north of Hagenburg and Sachsenhagen and east of Rehburg-Loccum, parts of these parishes lying within the nature park itself. In the centre of the nature park is northwest Germany's biggest inland waterbody, Lake Steinhude (Steinhuder Meer). In the north of the nature park is the hillocky forest of Grinderwald, in the east is the bog of Totes Moor, its southwestern fringes are bordered by the Rehburg Hills and, in the northwest is the Schneerener Moor.
The Kouga River originates near Uniondale, Eastern Cape, South Africa, and flows eastward, where it joins the Groot River to form the Gamtoos just past the Kouga Dam. Its main tributary is the Baviaanskloof River, which joins its left bank before the dam.Fish to Tsitsikamma WMA 15 The Kouga is part of the Gamtoos river system which is formed by the Groot and the Baviaanskloof River.Catchment L, the Gamtoos River System The Kouga Mountains to the north the river, Kouga Municipality and Kou-Kamma Municipality are named after this waterbody.
The waterbody is surrounded to the south and east by rocky outcrops (known locally as the stony rises) which were formed by lava flows from Mount Porndon to the south-west and Mount Warrion to the east. The Red Rock volcanic complex overlooks the south east shore at Alvie. The Mount Warrion flows caused the lake to form by blocking drainage to the east. As is typical of lakes in the area, the eastern flanks of the lake consist of lunettes formed by wind borne sediments blown from the lake during periods with dry climates.
The Dobbe, a bog kolk in the Ewiges Meer Nature Reserve A bog pond () is a waterbody in the middle of a raised or kettle bog, formerly also in percolating mires (Durchströmungsmooren). It is also called a bog eye, raised bog kolk, bog kolk or just kolk. Bog ponds owe their existence to the growth of the bog body and are thus of biogenic origin. Brown bog ponds are surrounded by peat and receive their water exclusively from precipitation or from the large rain storage capacity of raised bogs.
This is due to fact that most natural lakes in Germany are glacial or volcanic in origin, and Franconia escaped both influences in recent earth history. Among the largest waterbodies are reservoirs, which are mostly used as water reserves for the relatively dry landscapes of Franconia. These includes the waters of the Franconian Lake District, which was established in the 1970s and is also a tourist attraction. The heart of these lakes is the Großer Brombachsee, which has an area of 8.7 km² and is thus the largest waterbody in Franconia by surface area.
Bill Birkett, Complete Lakeland Fells, Collins Willow (1994), Drainage from the western slopes flows via Sharp Knott Gill and Fother Gill to Cogra Moss. This is a reservoir sitting in the deep valley between Blake Fell and Knock Murton, a reed rimmed waterbody held back by a substantial dam at the western end. Also known as Arlecdon Reservoir, it has a depth of around 30 feet.Blair, Don: Exploring Lakeland Tarns: Lakeland Manor Press (2003): The waters from this flank of the fell join the River Marron and ultimately the Derwent.
North Branch Shamokin Creek along Route 54 in Mount Carmel Township, PA. The entire length of North Branch Shamokin Creek is designated as an impaired waterbody and has poor water quality. The cause of the impairment is metals and the source is abandoned mine drainage. In addition to experiencing acidity and metal loading from acid mine drainage sources, the creek is also impacted by flow loss. The flow loss causes it to be an ephemeral stream. Between 1999 and 2003, the creek's discharge was measured four times to be between near Mount Carmel.
Oak Bay has a unique pool and manmade estuary caused by the creation of a causeway on Route 170. As a result, the easternmost section of the waterbody was split from Passamaquody Bay, connected only by four culverts which prevent the water from completely emptying during tidal changes. This pool is also fed by a small freshwater river on its northeastern border and thus experiences only a relatively minor height difference. Located in the centre of the bay is Spoon Island, so named because of its resemblance to an overturned spoon.
Had the lake been properly maintained, it could have been a major source of drinking water. The rapid pace of real estate development in the last two decades resulted in the shrinking of the waterbody from 265 acres to 55 acres now. The government allocated 53 acres to the Tamil Nadu Housing Board and 34 acres to the Tamil Nadu Slum Clearance Board for housing development. The encroachers on Erikkarai Street in Gandhi Nagar, who don't have sewage connections, are contributing to the pollution of the lake, locals said.
This runs parallel to the ridge and is the main feeder of Seathwaite Tarn, a reservoir in a side valley of the Duddon system. This was originally a much smaller waterbody, but was dammed early in the 20th century to provide drinking water for the Barrow-in-Furness area. The dam is almost 400 yards long and is concrete cored with slate buttresses, the resulting depth of the tarn being around 80 ft. Water is not abstracted directly from the tarn, but flows some distance downriver to an off-take weir.
Bowman Creek (also known as Bowmans Creek or Bowman's Creek) is a tributary of the Susquehanna River in Luzerne County and Wyoming County, in Pennsylvania, in the United States. It is approximately long and flows through Ross Township and Lake Township in Luzerne County and Noxen Township, Monroe Township, and Eaton Township in Wyoming County. The watershed of the creek has an area of . The creek is not designated as an impaired waterbody and its pH is close to neutral, although it has experienced some problems with acid rain.
The north-east ridge to Beda Fell is also well defined, a fair path traversing a series of rocky knolls before the final rise to the summit, named Beda Head. Southward from Angletarn Pikes is Angle Tarn itself. This indented waterbody is about a quarter of a mile long with an island in the middle and forms a picturesque foreground for views of the Pikes. The tarn sits in a hollow on the centre of the ridge, issuing westwards through a break in the parapet via the ravine of Angletarn Beck.
This aquatic sill is a submarine ridge below sea level extending from Baffin Island in the west to Greenland in the east. Unlike Baffin Bay and the Labrador Sea, Davis Strait is bounded by volcanic passive margins. Paleogene volcanic rocks are exposed on both sides of the strait: the Disko-Svartenhuk area of West Greenland in the east and near Cape Dyer on Baffin Island in the west. Hudson Strait–Evans Strait–Foxe Channel is a waterbody connecting Hudson Bay and Foxe Basin in the west-northwest with the Labrador Sea in the south-southeast.
The pheasant-tailed jacana's main sources of food are insects, molluscs, and other invertebrates picked from the floating vegetation or the water's surface. The forage by walking on vegetation and also by swimming in water, somewhat like phalaropes (Hoffmann claims that they wade in deeper water but never swim). They also ingest filamentous algae, seeds and plant material but this may be purely accidental. Flocks of as many as 50 to 100 can be found on a waterbody and they can become very tame and habituated to human presence.
The reservoir is jointly managed by the Bureau of Reclamation and the McKay Creek National Wildlife Refuge for irrigation water and a habitat for a variety wildlife including osprey, bald eagles, and an abundance of waterfowl. Fishing is permitted between March thorough September.Featured Waterbody - McKay Reservoir Oregon Department of Fish and Wildlife. Accessed 5 Jan 2009 McKay’s shallow water marshes and wetlands are also productive for warmwater fish such as rainbow trout, crappie, largemouth bass, sunfish, and yellow perch, as well as brown bullhead catfish, and lesser numbers of largemouth and smallmouth bass.
Location of the Grabow Bodden coast near Nisdorf The Grabow is a bodden - a lagoon-like waterbody - off the Baltic Sea south of the Zingst and Großer Werder peninsulas and the island group of Kleiner Werder.Die General Karte No. 1 - Schwerin-Rostock-Rügen, 1:200,000 scale, Mairs Geographische Verlag/Falk Verlag, Ostfildern, 2008. It lies on the coast of the German state of Mecklenburg-Vorpommern between Stralsund and Barth and forms the eastern part of the Darss-Zingst Bodden Chain. Its northern part belongs to the Western Pomerania Lagoon Area National Park.
To create the Amselsee in Saxon Switzerland, in 1934 a stream, the Grünbach (or Amselgrundbach), the main waterbody in the Amselgrund valley, was impounded by the municipality of Rathen just above its confluence with the Wehlgrund that joins from the rights 1934. The dam is around five metres high. At 127 m above sea level the curved, narrow, roughly 550 m long trout pond is used in summer for boat rides (using slot machines!) as well as for fish breeding and also provides flood prevention. Round trips have been possible since 1969.
Between Tarn Crag and Foule Crag is Sharp Edge, an aptly named arête which provides one of the most famous scrambles in the area. Hiker and author Alfred Wainwright noted that: ‘The crest itself is sharp enough for shaving (the former name was razor edge) and can be traversed only à cheval at some risk of damage to tender parts.’ Sharp Edge Scales Tarn, beneath Sharp Edge on Blencathra Below Tarn Crags is Scales Tarn, an almost circular waterbody filling a corrie. The bed plunges steeply to about and plants and fish are scarce.
USACE, Civil Works Regulatory Program – CWA Guidance to Implement the U.S. Supreme Court Decision for the Rapanos and Carabell Cases However, because authority under the Act is limited to protecting only navigable waters, jurisdiction over these smaller creeks is not absolute and may require just compensation to property owners when invoked to protect downstream waters. Finally, a water-body is presumed non-navigable with the burden of proof on the party claiming it is navigable. The U.S. Forest Service considers a waterbody not navigable until is adjudicated otherwise. see Whitewater v.
Even among organizations and researchers who distinguish lakes from ponds by size alone, there is no universally recognised standard for the maximum size of a pond. The international Ramsar wetland convention sets the upper limit for pond size as . Researchers for the British charity Pond Conservation (now called Freshwater Habitats Trust) have defined a pond to be 'a man-made or natural waterbody that is between and in area, which holds water for four months of the year or more.' Other European biologists have set the upper size limit at .
The architectural combination of a wada-type residence, a ghat on a waterbody, and a temple was typical of the Peshwa era. However, most of these palatial structures fell into disuse and disrepair after the lands and estates of the owners were taken away by the government after India became a republic in 1947. The Nana Phadnavis Wada on the bank of the river Krishna at Menavali is one of the very rare places where such a combination is preserved intact. The Nana Phadnavis wada is a large structure with six quadrangles, or courtyards, and a perimeter-protection wall.
The town of Rice Lake is located northeast of the center of Barron County and surrounds the city of Rice Lake on the west, north, and east. The waterbody of Rice Lake is located primarily in the city but extends north into the town. A few small arms of the lake at its south end also extend east into the town. The Red Cedar River enters the town near its northeast corner, flows southwest into Rice Lake (the lake and the city), then continues southward from the lake, forming a boundary between the city and the town.
The Reißeck, also Großes Reißeck ("Great Reisseck") is, at 2,965 metres above the Adriatic (9,728 ft), the highest peak of the Reißeck Group in the High Tauern of Carinthia, Austria. The range forms the southern part of the larger Ankogel Group with its highest summit, the Hochalmspitze, separated by the col of Mallnitzer Scharte at . The mountain also gives its name to the Reißeck municipality, located to the south in the Möll valley. The name Reißeck is derived from an old waterbody name, something like Reisach = "mountain stream" or "torrent", which became the Middle High German rîs = "the falling one".
Justice Kennedy wrote an opinion concurring with the judgment of the court. While he agreed that the cases should be vacated and remanded, he believed that a wetland or non- navigable waterbody falls within the scope of the Clean Water Act's jurisdiction if it bears a "significant nexus" to a traditional navigable waterway. Using some of the Court's language in SWANCC, Justice Kennedy argued the CWA defines navigable waters as a water or wetland that possesses a significant nexus to waters that are navigable in fact.The Supreme Court, 2005 Term — Leading Cases: Federal Jurisdiction over Navigable Waters, 120 351, 351 (2006).
Chignik Lake is located at . It is on the southeast side of the Alaska Peninsula and comprises all of Chignik Lake the waterbody, as well as land to the northeast and southeast of the lake and land to the south of the Chignik River, the lake's outlet. According to the United States Census Bureau, the CDP has a total area of , of which are land and , or 46.27%, are water. In 2009 the Marines of 4th Combat Engineer Battalion, 4th Marine Division, began work on an inter-village road system linking Chignik Lake to Chignik Lagoon.Sgt.
The local body had even engaged a consultant, shortlisted by experts from Anna University, Public Works Department and the agriculture department. The consultant gave a detailed plan in October last on how to beautify the lake. This included removal of encroachments in Gandhi Nagar and Ambedkar Nagar, fencing of the entire waterbody, provision of three decks for walking, viewing and fishing and a boating jetty. The consultant also suggested plantation of African grass, reed and bamboo along the middle deck and flowering plants and trees like bottlebrush, bougainvillea, royal palms and areca nut betel palms along the upper deck.
St Georges Basin is a coastal waterbody located immediately adjacent to the Tasman Sea of the South Pacific Ocean, north of the town of Sussex Inlet and east of the town of St Georges Basin. The basin is fed by Wandandian Creek and Tomerong Creek and its primary outflow is to the Tasman Sea via the Sussex Inlet. The basin covers a catchment area of and contains approximately of water over an estimated surface area of ; and at an average depth of . Located with the basin are six artificial reefs that range up to in depth.
Leiopotherapon unicolor occurs in a wide range water conditions, it can be found in running to still waters with turbidity ranging from clear to almost opaque as well as being able to tolerate a wide range of salinities and showing the ability to live in a wide range of temperatures. Among the waterbodies it can be found include intermittent waters, and these waters are where it is most numerous. It also inhabits lakes, dams, rivers, billabongs, bore drains, wells and waterholes. In the interior of Australia this species may be found in any temporary waterbody, even wheel ruts flooded after rains.
This species is purported to appear in odd places following so called "rain of fish", as they are often observed scattered on the ground in the aftermath of heavy downpours. However, the fish have been transported to these places by flooding. This hardy species can survive dry periods by aestivation in the least amount of moisture in the bottom of a temporary waterbody. It is an omnivorous species which has a diet of consisting largely of aquatic and terrestrial insects, crustaceans and some molluscs, however it will also prey on small fish and consume a small amount of algae and aquatic weeds.
Riparian rights include such things as the right to access for swimming, boating and fishing; the right to wharf out to a point of navigability; the right to erect structures such as docks, piers, and boat lifts; the right to use the water for domestic purposes; the right to accretions caused by water level fluctuations; the right to exclusive use if the waterbody is non-navigable. Riparian rights also depend upon "reasonable use" as it relates to other riparian owners to ensure that the rights of one riparian owner are weighed fairly and equitably with the rights of adjacent riparian owners.
Immatures have only traces of white on the front These birds are usually seen singly or in pairs as they forage slowly along the edge of a waterbody mainly on the ground but sometimes clambering up low vegetation. The tail is held up and jerked as they walk. They probe with their bill in mud or shallow water, also picking up food by sight. They mainly eat insects (large numbers of beetles have been recorded), small fish (which are often carefully washed in water), aquatic invertebrates and grains or seeds such as those of Pithecolobium dulce.
Barren Island remained sparsely inhabited before the 19th century, mainly because of its relative isolation from the rest of the city. From the 1850s to the mid-1930s, the island was developed as an industrial complex with fish rendering plants and other industries, and also as an ethnically diverse community of up to 1,500 residents. Between the mid-19th century and 1934, the island housed industrial plants that processed the carcasses of the city's dead horses, converting them into a variety of industrial products. This activity led to the still-extant waterbody on the island's western shore becoming nicknamed "Dead Horse Bay".
An ephemeral waterbody is a wetland, spring, stream, river, pond or lake that only exists for a short period following precipitation or snowmelt. They are not the same as intermittent or seasonal waterbodies, which exist for longer periods, but not all year round. Examples of ephemeral streams are the Luni river in Rajasthan, India, Ugab River in Southern Africa, and a number of small ephemeral watercourses that drain Talak in northern Niger. Other notable ephemeral rivers include the Todd River and Sandover River in Central Australia as well as the Son River, Batha River and the Trabancos River.
To the west of the Hawse is the valley of Tarn Head Beck, the main feeder of Seathwaite Tarn, a reservoir in a side valley of the Duddon system. This was originally a much smaller waterbody, but was dammed early in the 20th century to provide drinking water for the Barrow-in-Furness area. The dam is almost 400 yards long and is concrete cored with slate buttresses, the resulting depth of the tarn being around 80 ft. Water is not abstracted directly from the tarn, but flows some distance downriver to an off-take weir.
Farther north, NY 10 passes directly between the Stoner Lakes, a pair of small water bodies separated by only NY 10, just south of where it crosses into Hamilton County. For most of its run through the county, NY 10 parallels a waterbody, namely the west branch of the Sacandaga River to where the Piseco Outlet flows into it, then the Piseco Outlet north to Big Bay near the community of Higgins Bay. NY 10 terminates soon after at an intersection with NY 8 south of Piseco Lake, west of Spy Lake, and southwest of Higgins Bay.
The route proceeds west into the town of Owasco and the hamlet of the same name within, the first community of any significant size along the route since it left Moravia. It heads westward through the center of the community before reentering rural surroundings and coming within view of Owasco Lake. The route curves northward at the waterbody and follows the eastern shore of Owasco Lake toward Auburn. Southeast of Auburn, NY 38A crosses a small stream and serves the Lakeview Golf and Country Club and the Owasco Country Club as it curves westward around the northern end of the lake.
Lake Verret is natural lake located in Assumption, Parish, Louisiana, US. The lake is west of Napoleonville, Louisiana, south of Pierre Part, part of the Atchafalaya River Basin of the Lower Mississippi River Region, with of watershed that includes () in Ascension Parish () in Assumption Parish and () in Iberville Parish.LWF: Lake Verret: Part VI -A Waterbody Management Plan Series Lake Verret, Grassy Lake, and Lake Palourde Lake History & Management Issues (pp. 5-6)- Retrieved 2017-11-23 Lake Verret is named after the first Spanish commandant Nicolas Verret. A historical monument was placed in front of the Assumption Parish Courthouse.
Johad in Haryanvi language and Rajasthani language are also called sarovar, taal and talab in Hindi language, and water pond or lake in English. A similar structure to a johads, called a khadin, consists of a very low and long earthen bund in the Jaisalmer district. Over 4,500 working johads in Alwar district and surrounding districts Rajasthan were revived by the NGO Tarun Bharat Sangh by Rajendra Singh. Haryana formed the Haryana State Waterbody Management Board to rejuvenate and manage 14,000 ponds in the state, including the development of 60 lakes in Delhi NCR falling within the state.
From below Eppendorf to its mouth the waterbody has cut a roughly 100 metre deep valley into the terrain. Between the Lößnitz valley and the former halt of Metzdorf on the Hetzdorf and Großwaltersdorf narrow gauge railway, the river meanders markedly in a relatively wide and visibly waterlogged river meadow. The adjoining section to the mouth, on the other hand has a significantly steeper gradient and only a narrow floodplain.c.f. Roughly 400 metres above its confluence with the Flöha and southwest of Görbersdorf, the Kleine Lößnitz empties into it from the right at 465 metres above sea level .c.f.
Livestock stalls and barns are at the rear of the plot (in Austria called the Hintaus) and may be linked by a farm track that runs around the village forming an outer ring. There is often a village pond on the anger and sometimes a stream flows through it which may not be easy to recognise today where the groundwater level has changed. The waterbody may well be the reason the anger was chosen. Originally there were no buildings on the anger, but in the course of time other community facilities were often built on it, such as the village church, village school or a smithy.
The lake and Mt. Tsukuba viewed from the east is the second-largest lake in Japan, located 60 km to the north-east of Tokyo. Hokusai In a narrower sense and officially, Lake Kasumigaura refers to a waterbody with an area of 167.63 km2. In a wider sense, Lake Kasumigaura can also refer to a group of contiguous lakes, which includes Lake Kasumigaura proper, hereby referred to as Nishiura (西浦), and two smaller lakes, Kitaura (北浦; 35.16 km2) and Sotonasakaura (外浪逆浦; 5.85 km2), and also encompasses the rivers connecting them. In this case the total area is 220 km2.
NY 430 begins at the Pennsylvania state line in rural western Chautauqua County as a continuation of PA 430, which begins roughly to the west in Erie. The route proceeds eastward as a county-maintained, state- numbered highway through the westernmost portion of the town of Mina to the hamlet of Findley Lake, a small community located at the northern tip of the lake of the same name. Here, the New York State Department of Transportation assumes maintenance of the route at a junction with NY 426. NY 430 briefly overlaps with NY 426 through the community and past the northern tip of the waterbody that gives the hamlet its name.
A GEMSS application requires two types of data: (1) spatial data (primarily the waterbody shoreline and bathymetry, but also locations, elevations, and configurations of man-made structures) and (2) temporal data (time-varying boundary condition data defining tidal elevation, inflow rate and temperature, inflow constituent concentration, outflow rate, and meteorological data. All deterministic models, including GEMSS, require uninterrupted time-varying boundary condition data. There can be no long gaps in the datasets and all required datasets must be available during the span of the proposed simulation period. For input to the model, the spatial data is encoded primarily in two input files: the control and bathymetry files.
It is able to swim in waterbody or in air The relatively harmless nature of the Chinese alligator is believed to have been an influence for the helpful nature of the dragon. The fact that the alligator ends its brumation when the rainy season begins and returns to its burrows when the rainwater in rivers recedes, as well as the fact that it lives in bodies of water, may be the reason for the dragon's portrayal as a water- related mythological creature. Alligator drums may have been used to simulate the species' vocalizations during the mating season, which humans associated with the dragon's "power of summoning rainclouds".
Unimpaired runoff, also known as full natural flow, is a hydrology term for the natural runoff of a watershed or waterbody that would have occurred under current land use but without dams or diversions. Flow readings from river gauges are influenced by upstream diversions, impoundments, and many other alternations of the land that drains into a watershed or of alternatives of a river channel itself. Engineers estimate unimpaired or natural runoff by estimating all of the effects of human "impairments" to flow and then removing these effects. Since these calculations involve many assumptions, they tend to be more accurate for either smaller watersheds or when expressed as longer period averages.
The SSSI includes ten former gravel pits, part of the Small River Lea, a further waterbody, Hall Marsh Scrape, which was constructed specifically for use by waterfowl. Also included in the site are areas of marsh, grassland, ruderal herbs, scrubland and woodland. The pits which include North Metropolitan Pit known as Northmetpit was excavated in the 1940s to Hooks Marsh Lake which was dug in the 1970s and cover a span of over 40 years. The site are of national importance for the wintering gadwall and the wintering northern shoveler and of regional importance for wintering coot and locally important for wintering snipe and the bittern.
It is not clear in what way the western lake or lakes – there are now 2 main areas of bogland, which may correspond to former lake basins – were connected to the remaining waterbody. One bog is immediately adjacent to the lake's western end, the other is halfway between that and the island's northwest tip. Canals have been cut into the bogs, for punting, rowing and motor boats transporting people and produce. There is some removal of peat and sediments to stem the lake's ongoing infilling; in addition it seems that in recent times, the lake's level is slowly rising again so that the eastern bog's area has receded somewhat.
The tower sits on a landscaped parcel at the northeast corner of the intersection of Kehui South Road and Tianchen Road, a wide pedestrian promenade. The surrounding terrain is level, consisting mostly of urban open space such as planted parkland or open plazas. To the east is a long curving artificial waterbody that bounds the Olympic Green neighborhood in that direction; on the other side the first block is either more open space or large buildings such as the China Science and Technology Museum, after which denser urban development and taller buildings begin. On the west similar medium-rises begin after two large blocks.
We felt that the template is ideal for our video and hence we paid for it." Baahubali's first poster was released in early May 2015. The poster, which showed an infant being lifted from a waterbody by a woman's hand, was criticised for its lack of originality; Deccan Chronicle noted its similarities to the poster of the 1998 American film Simon Birch, commenting, "The Baahubali poster shows a woman's hand raising an infant from a river; the Hollywood film's poster shows an infant being raised by two hands from water. The image seems to be the same with one difference, the Baahubali poster's baby is seen in typical Indian attire.
Port Ludlow, the community, is located on the eastern edge of Jefferson County at , on the northwest side of Port Ludlow, the waterbody, located at . The original settlement of Port Ludlow is in the northern part of the CDP, with new development reaching south of the Port Ludlow inlet. The CDP also includes the communities of Mats Mats (to the north), Swansonville (to the northwest), and Beaver Valley (on the western edge). Washington State Route 19 forms the western edge of the CDP, leading north to Port Hadlock and having its southern terminus at Washington State Route 104 at the southwest corner of the Port Ludlow CDP.
In recent years, the lake has been heavily encroached upon, particularly near the Chetpet railway station. There have been many plans to rejuvenate Chetpet lake since the mid-1990s, including developing a boat club, an aquarium, seafood stall and fish court besides a walkway around the waterbody. The last attempt to save the lake was in 2005, when the state environment department identified it along with 12 other lakes of Greater Chennai area for an eco-restoration project. The CPR Environmental Education Centre conducted a detailed survey, and based on that, the state government appointed the Tamil Nadu Urban Infrastructure Finance Services Limited to prepare a project report.
Rose Lake is an unincorporated community on the Yellowhead Highway in the Bulkley Valley region of northwestern British Columbia, Canada.BC Names entry "Rose Lake (community)" Its name is derived from the nearby waterbody Rose Lake.BC Names entry "Rose Lake (lake)" The community and the lake are along the northern mainline of the Canadian National Railway just northeast of Bulkley Lake. The area of Rose Lake is notable in the field of montane prominence, as it is the location of the divide between the Fraser and Skeena River basins such that the locality forms the prominence col for Mount Waddington, the highest peak completely within British Columbia.
Taj Lake Palace in Udaipur, India The technical distinction between a pond and a lake has not been universally standardized. Limnologists and freshwater biologists have proposed formal definitions for pond, in part to include 'bodies of water where light penetrates to the bottom of the waterbody,' 'bodies of water shallow enough for rooted water plants to grow throughout,' and 'bodies of water which lack wave action on the shoreline.' Each of these definitions has met with resistance or disapproval, as the defining characteristics are each difficult to measure or verify. Accordingly, some organizations and researchers have settled on technical definitions of pond and lake that rely on size alone.
Hathni Kund in Yamunanagar district, Karna Lake at Karnal,Page 153, Tourism: Theory, Planning, and Practice, By K.K. Karma, Krishnan K. Kamra, Published 1997, Indus Publishing, ancient Surajkund in Faridabad, and Tilyar Lake in Rohtak.Page 149, India: A Travel Guide, By B.R. Kishore, published 2001, Diamond Pocket Books (P) Limited, The Haryana State Waterbody Management Board is responsible for rejuvenation of 14,000 Johads of Haryana and up to 60 lakes in National Capital Region falling within the Haryana state."Haryana to develop 50-60 small lakes, water bodies in NCR: Manohar Lal Khattar" , Indian Express, 1 November 2017."Haryana to constitute pond management authority " , Business Standard, 1 November 2017.
The St. Joseph Channel is a strait in Algoma District, Northwestern Ontario, Canada and Chippewa County, Michigan, United States. Shows the outline of the channel highlighted on a topographic map. It is in the Great Lakes Basin and connects the St. Marys River flowing through the Middle Neebish Channel between Neebish Island and Sugar Island at the northwest and Lake George/ East Neebish Channel between Sugar Island and the Ontario mainland at the north, with the North Channel between St. Joseph Island and the Ontario mainland at the east, and with the Munuscong Channel between Neebish Island and St. Joseph Island at the southwest. All of these waterbody elements are part of Lake Huron.
Chuhi Mal Ka Talaab (literally "Chuhi Mal's water tank"), is a rectangular ancient water tank built by a rich salt trader and Nagarseth (city chief) "Seth Chuhi Mal" in the 18th-19th century, comprises a covered and arcaded gateway, four ghats on all four flanks with steps leading to the waterbody, 8 single-story octagonal-shaped chhatris of red sandstone built on burjis (pylon or bastion), and two historic temples on its bank. The tank is fed by a channel from Agra Canal flowing nearby.Magnificent masonry tanks of yore near Nalhar road behind Yasin degree college on the outskirts of Nuh city. The pond has an ancient cenotaph (chhatri) of red stone and having beautiful carvings.
Eastbound on NY 157A in Berne between Warner Lake and Thompson Lake NY 157A begins at a rural intersection with NY 157 in the southeastern portion of the town of Knox. Although it is signed as an east–west route, it heads generally southwestward at first, following the two- lane Warners Lake Road through a forested yet populated area just south of NY 157\. The homes and forests give way to open fields soon afterward, and the rolling terrain follows NY 157A into the adjacent town of Berne. Here, the number of homes alongside the highway rises as it approaches Warner Lake, a small waterbody northwest of the hamlet of East Berne.
It is probable that dispersal of Tarebia granifera from one waterbody or river catchment to another occurs passively via birds, notably waterfowl, which eat them and void them later, perhaps in another habitat. Evidence for this comes from the finding of many small Tarebia granifera 5–7 mm in height and still containing the soft parts in unidentified bird droppings from the bank of the Mhlali River, South Africa. Even though the shell of Tarebia granifera is thick, most of these juveniles had been partially crushed with only a few still intact. Both the intact and damaged specimens could have been alive when passed and perhaps survived had they been deposited in water.
The waterbody as seen from Karpagam Bridge, Karpagam Avenue Tamil Nadu Urban Infrastructure Financial Services Limited has been charged with engaging consultants to develop a master plan and invite bidders for development of the park. The Adyar Creek Trust has been set up by the government of Tamil Nadu to co-ordinate the execution of the project. The Adyar Poonga Trust has been rechristened as Chennai Rivers Restoration Trust (CRRT). The Chief Secretary to the Government of Tamil Nadu is the chairman for the trust and the secretaries in the Finance Department, Municipal Administration and Water Supplies, Highways Department, Public Works Department, Environment and Forest Department, and the Commissioner, Corporation of Chennai are the trustees.
It remains on an almost northerly course for the next half- mile, flowing through a narrow wooded corridor between fields, to where U.S. Route 9 crosses. The Saw Kill bends to the northwest past this bridge, and toughly 2,000 feet (600 m) from US 9, it turns to the west and then southwest, still in a forested corridor through worked agricultural land. alt=A waterbody with streaks of green algal growth reflecting some of the clouds in the sky above. On a distant shore there are trees As it reaches the Mill Road bridge, the Saw Kill widens into a lake, at elevation, created by a dam southwest of the crossing, that extends 1,500 feet (500 m) to the northwest as well.
Owen, H.W. & Morgan, R. 2007 'Dictionary of the Place-names of Wales' Gomer Press, Ceredigion The southern part of the Grwyne Fechan valley in the Black Mountains The Gwryne Fawr rises at Blaen Grwyne Fawr on the southern slopes of Rhos Dirion in the Black Mountains and follows a southeastward course for several miles, its flow interrupted by the presence of Grwyne Fawr Reservoir, the only waterbody within this range of hills. Some way below the reservoir, Mynydd Du Forest clothes the sides of the valley. Though a public road penetrates the valley as far as the north end of the forest, the valley is very sparsely populated. It is only approaching the hamlet of Partrishow that the valley takes on a farmed appearance.
Almost 200 km long and 8000 km2 in area, the Canadian portion of the Okanagan watershed is approximately 2/3 the size of Vancouver Island. Okanagan Lake dominates the basin which contains many small lakes and watercourses. The Okanagan Valley was carved out by glaciers, and when the ice retreated approximately 10,000 years ago, the Canadian portion of the basin was filled with one huge waterbody, Lake Penticton. The Valley was scoured to something like its current state when an ice dam at the southern end of Lake Penticton melted, emptying most of the valley. The Canadian Environmental Grantmakers’ Network considers the Okanagan Basin to be the most arid watershed in Canada, with an urgent need for effective water management.
However, the creek largely has good water quality. It is not designated as an impaired waterbody. Near Factoryville, the average annual discharge of South Branch Tunkhannock Creek is . The maximum flow time from the headwaters of the creek to this point is 21 hours and 57 minutes. The average monthly recharge of the creek at Montdale, in terms of percentage of the total annual recharge of the creek, ranges from 1.8 percent in August to 19.2 percent in March. In 1976, the water temperature of the creek near Tunkhannock ranged from . In the 1960s and/or 1970s, the turbidity of South Branch Tunkhannock Creek near Tunkhannock ranged from 4 to 22 Jackson Turbidity Units. The specific conductance of the creek ranged from 70 to 200 micro-siemens per centimeter.
NJDEP identifies that "runoff from land surfaces was found to comprise a substantial portion of the phosphorus load", citing that large communities of geese that reside within the lake communities along Neepaulakating Creek and the nearby Clove Brook also contribute phosphorus to the creek. Clove Acres Lake is identified as being eutrophic in that phosphorus loading has stimulated excessive growth of algae and aquatic plants resulting in an accelerating aging of the lake, sedimentation and excessive loading of silt and organic matter, fluctuating oxygen saturation and depletion, and that these factors can impact the creek through a potential loss of biodiversity. The creek is further impaired to a lesser extant by other pollutants including fecal coliform and arsenic.U.S. Environmental Protection Agency, Watershed Assessment, Tracking & Environmental Results: 2012 Waterbody Report for Papakating Creek (below Pellettown).
Toxic encephalopathy is a neurologic disorder caused by exposure to neurotoxic organic solvents such as toluene, following exposure to heavy metals such as manganese, as a side effect of melarsoprol treatment for African trypanosomiasis, or exposure to extreme concentrations of any natural toxin such as cyanotoxins found in shellfish or freshwater cyanobacteria crusts. Toxic encephalopathy can occur following acute or chronic exposure to neurotoxicants, which includes all natural toxins. Exposure to toxic substances can lead to a variety of symptoms, characterized by an altered mental status, memory loss, and visual problems. Toxic encephalopathy can be caused by various chemicals, some of which are commonly used in everyday life, or cyanotoxins which are bio-accumulated from harmful algal blooms (HABs) which have settled on the benthic layer of a waterbody.
These water bodies have contributed to the economic development through fisheries in the landlocked state of Haryana. Haryana ranks second in India in terms of the average annual fish production per unit area in the country with 7000 kg per hectare average annual fish production.[harfish.gov.in/development-fisheries.htm Haryana fisheries annual production average, July 2016] Fish production has increased from 600 tonnes in 1966-67 at the time of formation of Haryana to 121000 tonnes of fish during the year 2015-16, providing a livelihood to over 30000 families in fisheries sector. On 1 November 2017, Chief Minister of Haryana Manohar Lal Khattar announced that Government of Haryana will form the Haryana State Waterbody Management Board to rejuvenate and manage 14,000 ponds in Haryana by digging the silt out every year.
NY 23 westbound after its brief concurrency with US 9 in Livingston Once across the bridge and into Columbia County, the highway encounters NY 9G near the Olana State Historic Site in western Greenport. The two highways briefly overlap until NY 9G continues north with NY 23B to follow NY 23's old course into and through the city of Hudson. NY 23 continues to the southeast, bypassing Hudson well to the south and serving Columbia–Greene Community College, located in an otherwise forested area of Greenport. After , the route meets US 9 at an isolated junction due south of Hudson. US 9 and NY 23 overlap for across more open but still largely undeveloped areas to a small, unnamed community on the western edge of Bell Pond, a small waterbody in the northeast corner of the town of Livingston.
"If there is a city in the United States which has need of quarantine laws, it is New Orleans", Justice Samuel Freeman Miller, a physician prior to his legal career, wrote for the Court. He noted that despite being a hundred miles (160 km) upriver from the Gulf of Mexico, it was the largest and busiest port on that waterbody. Many of the ships that came to New Orleans from the Gulf often came from warmer countries to the south, where tropical diseases were common, and past epidemics of yellow fever and cholera in the Mississippi Valley had all been identified as having spread from the city.Morgan's, at 459 Illustration of bodies of lynched Italian immigrants after 1891 incident Around that time Italian immigrants began arriving in New Orleans in great numbers; eventually the city would be home to more of them than any other in the South.
View of the Brocken over the site of the old Brocken Pond The Brocken Pond () is the name of a waterbody that was created in 1744 in the County of Wernigerode below the summit of the Brocken, the highest mountain in the Harz mountains of Germany. It is located in the present-day district of Harz. In a letter dated 12 August 1744 and written at the Brocken by Count Henry Ernest of Stolberg-Wernigerode to his father, Christian Ernest in Wernigerode, he reports amongst other things: that yesterday evening, about 1½ hours from the famous Brocken Pond, we even made a start on staking out some peat houses ... so that they can be timbered this autumn, started up in the winter [and in the spring ...] can be sorted out. Today we will continue staking them out, including two stone houses, specifically for the purpose of the workers.
The park has a lake and an island with a footbridge, an open- air amphitheatre (Nazrul Mancha), a sports stadium (Rabindra Sarobar Stadium), a children's park and the rowing clubs of Calcutta Rowing Club, Bengal Rowing Club and Lake Club. A view of Rabindra Sarobar in South Kolkata Lush green grass along the lake at New Town Eco Park The Central Park is a large urban park in the centre of the Salt Lake township in Kolkata Metropolitan Area, with a lake in the middle and information technology and government offices along its fringes. Eco Park (officially Prakriti Tirtha), located in New Town in Kolkata Metropolitan Area, is situated on a plot and is surrounded by a waterbody with an island called Ekanto in the middle. The park has been divided into three broad parts; (1) ecological zones like wetlands, grasslands, and urban forest, (2) theme gardens and open spaces, and (3) urban recreational spaces.
In Madurai, Pennycuick's statue has been installed at the state PWD office and his photographs are found adorning walls in peoples homes and shops. In 2002, his great grandson was honoured in Madurai, a function that was attended by thousands of people. The dam created a reservoir in a remote gorge of the Periyar river situated 3,000 feet above the sea in dense and malarial jungle, and from the northerly arm of this manmade waterbody, the water flowed first through a deep cutting for about a mile and then through a tunnel, 5704 feet in length and later through another cutting on the other side of the watershed and into a natural ravine and so onto the Vaigai River which has been partly built up for a length of 86 miles, finally discharging 2000 cusecs of water for the arid rain shadow regions of present-day Theni, Dindigul District, Madurai District, Sivaganga District and Ramanathapuram districts of Tamil Nadu, then under British rule as part of Madras Province (Sandes, 1935). The Periyar project, as it was then known, was widely considered well into the 20th century as "one of the most extraordinary feats of engineering ever performed by man".

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