Muddy Branch [SEP] mouth of the watercourse
[{"answer": "Potomac River", "provenance": [{"wikipedia_id": "20685420", "title": "Muddy Branch", "start_paragraph_id": 3, "start_character": 0, "end_paragraph_id": 3, "end_character": 237, "bleu_score": 0.5268690054437961, "meta": {}, "section": "Section::::Course.\n"}]}]
Don River (Ontario)


The Don River is a watercourse in southern Ontario, that empties into Lake Ontario, at Toronto Harbour. Its mouth was just east of the street grid of the town of York, Upper Canada, the municipality that evolved into Toronto, Ontario. Of the various watercourses that drained Toronto, the Don, the Humber River, and the Rouge River have headwaters in the Oak Ridges Moraine. The Don is formed from two rivers, the East and West Branches, that meet about north of Lake Ontario while flowing southward into the
15180333
Muddy Run (West Branch Susquehanna River tributary)


the extreme western area of the watershed. The Hagerstown-Edom-Washington series is found in the eastern section of the watershed. The Leck Kill-Meckesville-Calvin soil series occurs in the southwestern and north-central areas of the watershed. The stream banks of Muddy Run are eroded in some locations. The elevation of the creek at its mouth is above sea level. The area of the Muddy Run watershed is approximately 11.4 square miles. 75% of the watershed is devoted to agriculture 15% is forested, and
3360547
Muddy Run (West Branch Susquehanna River tributary)


Pennsylvania Route 147 in the western part of the watershed, and a number of township roads throughout the watershed. The watershed occupies part of Milton Township, Turbot Township, Delaware Township in Northumberland County. It also occupies a small area of western Limestone Township, in Montour County. The first mill in Turbot Township was built on Muddy Run by Hawkins Boone some time before 1779. In 1785, Cornelius Waldron and his son Laffert arrived at the mouth of Muddy Run. Laffert Waldron later purchased a tract of farmland on the creek
3360549
California Wash (Nevada)


California Wash is an arroyo tributary to the Muddy River, in Clark County, Nevada. Its mouth is at its confluence with the Muddy River over a mile southwest of Moapa and a mile and a half west of Glendale, Nevada. Its source is at an elevation of 3320 feet at the southwestern end of the Muddy Mountains, at . From there it drains northeastward to its mouth on the Muddy River. California Wash was named for the "California Crossing" of the Muddy River at its mouth by the Mormon Road,
14497977
Lady Robinsons Beach


runway for the Sydney Airport. This runway was to jut out into Botany Bay at the position of the mouth of the Cooks River. It took several years to relocate the mouth of the river to its current position and to landfill the former mouth of the river. This relocating of the mouth of the river allowed for widening and deepening of the mouth of the river and the now adjacent mouth of the river's tributary, Muddy Creek. The widened and deepened mouth of Muddy Creek was renamed Kyeemagh Canal. One consequence of
7694315
Original Maryborough Town Site


Street and the site of Aldridge's inns drops down towards the creek. East of the creek's mouth is a concentration of bamboo, mature native trees and other exotic species, and a small stone and concrete jetty stands just upriver from the mouth of Muddy Creek, near the site of Furber's inn. Northwest of the mouth of Muddy Creek, the terrain rises from the river to a river terrace, where Furber Street is located. The river terrace is quite flat and is framed by Muddy Creek to the southeast,
6183270
Toronto waterway system


Bay Park East. The Source of the River is the Huber Spring Pond and the basin is 903 km . The Don River is a watercourse in southern Ontario, that empties into Lake Ontario, at Toronto Harbour. Its mouth was just east of the street grid of the town of York, Upper Canada, the municipality that evolved into Toronto, Ontario. The Don is formed from two rivers, the East and West Branches, that meet about 7 kilometres (4 mi) north of Lake Ontario while flowing southward into the
14180440
Narran River


Narran River, a watercourse of the Barwon catchment within the Murray–Darling basin, is located in the Southern Downs district of Queensland and Orana district of New South Wales, Australia. The river rises south west of Dirranbandi, as a branch of the Balonne River in Queensland, and flows generally to the south and south-west, before reaching its mouth at Narran Lake, between Brewarrina and Walgett in New South Wales; descending over its course. In March 2010 the Narran River flooded the Angledool Lake at Angledool and then
16332847
Garonne


most distant point (along watercourses from the river mouth) in the drainage basin from which water runs. The Ratera-Saboredo cirque is the "most distant point (along watercourses from the river mouth) in the drainage basin from which water runs", and the source of the Garonne, according to the United States Geological Survey, the National Geographic Society, and the Smithsonian Institution convention upon determining a stream's source. The Garonne follows the Aran Valley northwards into France, flowing via Toulouse and Agen towards Bordeaux, where
1652483
Muddy River (Washington)


Survey (USGS) stream gauge, on the left from the mouth. Muddy River enters the Lewis River about from the larger stream's mouth on the Columbia River. The USGS monitors the flow of Muddy River at a station upstream of the confluence with the Lewis River. The average flow of the river during 54 water years, including 1984–2011, is . The maximum flow recorded was on February 8, 1996, and the minimum flow was on December 5–7, 1929. The high flow in 1996 was associated with general flooding
14757778
Monkey River


Monkey River is a coastal watercourse in southern Belize that rises in the Maya Mountains and discharges to the Caribbean Sea near Monkey River Town. One of Belize's major rivers, Monkey River has northern headwaters which originate in the Cockscomb Basin Wildlife Sanctuary, where the Swasey Branch drains the East Basin of that wildlife sanctuary. Further south, the Bladen Branch watercourse drains the eastern slopes of the Maya Mountains including the ancient Mayan settlement areas of Lubaantun and Nim Li Punit. These two watercourses join to form the Monkey River approximately 16 kilometres
2619521
Oshawa Creek


Oshawa Creek is a watercourse that flows from its headwaters in the Oak Ridges Moraine to its mouth on Lake Ontario, at Oshawa, Ontario. It drains a watershed of . In its lowest reaches, in Oshawa, two tributaries, Goodman's Creek and Montgomery Creek, join the watercourse. To the west it borders Lynde Creek, which also has its headwaters in the Oak Ridges Moraine, and the shorter watercourses Pringle Creek and Corbett Creek. Bowmanville Creek, to the east, also has its headwaters in the Oak Ridges Moraine
15142259
Big Muddy River


. The Big Muddy cuts through the Shawnee Hills south of Murphysboro near the confluence with its smaller tributary, Kinkaid Creek. From there, it runs southward roughly twenty miles and meets the Mississippi directly south of Grand Tower. Near its mouth, a small portion of the Big Muddy acts as the dividing line between Jackson and Union counties. Major tributaries of the Big Muddy include Beaucoup Creek, the Little Muddy River, Casey Creek, the Middle Fork of the Big Muddy and Crab Orchard Creek. Smaller tributaries include Town Creek,
21232635
Themiste hennahi


structure of six branching tentacles which surround the mouth. The collar (immediately behind the tentacles) is not reddish-purple as it is in "Themiste dyscrita", and the introvert is devoid of spines. "Themiste hennahi" is native to the tropical and subtropical eastern Pacific Ocean, its range including the western coast of the United States, and the coasts of Peru and Chile. It burrows into sandy, gravelly, silty and muddy substrates in the intertidal zone, including eelgrass beds, and conceals itself under loose rocks
4629490
Dufton


. Nor is it muddied by cattle, or by birds or wild animals, or by a branch fallen from a tree." The main activities in the village nowadays are linked to tourism and farming. Dufton was badly affected by the foot and mouth disease outbreak of 2001. Local farms were in the area which became known as "the Penrith spur" where the disease proved very hard to eradicate and where the final cases of the outbreak occurred. The practice of grazing sheep on communal pastureland above the village may have contributed
1375256
Muddy Run (Spruce Run tributary)


of its mouth. A total of of streams in the watershed of Muddy Run are designated as impaired waterbodies. The cause of the impairment is sedimentation/siltation and the source of the impairment is grazing-related agriculture. The total maximum daily load date is 2015. In addition to sediment, Muddy Run is also affected by "E. coli", nutrient pollution, and thermal radiation. In 2000, the load of sediment in Muddy Run was , while in 2008 it was . This equates to somewhere between . In the
9738240
Muddy Run (West Branch Susquehanna River tributary)


Muddy Run is a tributary of the West Branch Susquehanna River in Northumberland County, Pennsylvania, in the United States. It is in length. The creek is several miles northeast of the community of Milton. Main land uses include agricultural land and forest. The area of the creek's watershed is 11.4 square miles, most of which is agricultural land. Muddy Run is entirely within Turbot Township. Most of the rock in the watershed is shale. The most common soil series is the Berks-Weikert-Bedington series. Muddy
3360542
Winooski River


Branch are left-bank tributaries which enter from the south. The Lower Tributaries, smaller tributary streams nearer the mouth of the Winooski, include Mill Brook, Muddy Brook, Allen Brook and Alder Brook. The name "Winooski" comes from the Abenaki word "winoskik" meaning "at wild onion land," a reference to the leeks or wild onions that were once common along the river banks. The byname "Onion River" came into general usage in the late 18th and early 19th century, after Ira and Ethan
19225208
Kennet River (Victoria)


The Kennet River, now commonly spelt Kennett River, is a perennial river of the Corangamite catchment, located in The Otways region of the Australian state of Victoria. Formed by the confluence of the West and East branches of the river, the Kennet River rises in the Otway Ranges in southwest Victoria, below Muddy Saddle and flows generally east by south through the Port Campbell National Park before reaching its river mouth and emptying into Addis Bay within Bass Strait, northeast of Cape Otway at the locality of . From its highest point,
20706990
Muddy Run (Spruce Run tributary)


streambank erosion and came from other sources. In 2000, the total load of phosphorus in Muddy Run from row crops was and the load from groundwater was . The load from hay and pastures was , the load from low-density urban land was , came from unpaved roads, and came from septic systems. Other sources contributed . The elevation near the mouth of Muddy Run is above sea level. The elevation of the stream's source is between above sea level. A total of of streams in the watershed of Muddy Run
9738243
Muddy River (Washington)


the river leaves the national volcanic monument but remains in the national forest. At about the level, Clearwater Creek enters from the left. Turning south, the river descends less rapidly, passing under Forest Road 25 and then receiving Clear Creek from the left about from the mouth. At the road crossing, Muddy Creek Picnic Site is on the left. Below the confluence with Clear Creek, the river meanders through Cedar Flats, leaves the national forest slightly more than a mile from the mouth, and passes a United States Geological
14757777
Callville Wash


the southern slope of Muddy Peak (5387 ft / 1642 m) in the Muddy Mountains. Callville Wash originally had a tributary, originally known as West Fork Callville Wash, whose confluence with Callville Wash is now under Callville Bay. Following the creation of Lake Mead it now flows into Callville Bay, at and is known as West End Wash. Callville Wash was part of the original 1829 Armijo Route of the Old Spanish Trail along the Colorado River, between the mouth of the Virgin River and mouth of Las Vegas Wash. That trail
5659085
Sepik


May 1885. But the river, in fact, did not yet have a European name. It was thus termed "Kaiserin Augustafluß" by the explorer and scientist Otto Finsch, after the German Empress Augusta. The word 'Sipik' was first reported by A. Full as one of two names for the watercourse—the other being 'Abschima'—used by the natives living at the mouth of the river. A few years later, Leonhard Schultze applied the term 'Sepik' to the entire watercourse, and it took, although Schultze
9372594
North Creek (Toronto)


North Creek is a mostly buried watercourse that flows into Lake Ontario on the grounds of the former Lakeshore Psychiatric Hospital now in Colonel Samuel Smith Park. Its mouth was at Kipling Avenue. Its headwaters were near the present day intersection of the Queen Elizabeth Way and Browns Line. Almost all the creek had been buried by 1960, but part of the creek remains and mouth now flows in an easterly direction instead of southerly into Lake Ontario. The mouth of Etobicoke Creek was approximately 2.5 km to the west of the mouth of North
11160504
Muddy Run (Spruce Run tributary)


are flanked by fences, though this could eventually increase to . Stabilization occurs on only of streams, though this could increase to in the future. The watershed of Muddy Run has an area of . The mouth of the stream is in the United States Geological Survey quadrangle of Lewisburg. However, the source is in the quadrangle of Mifflinburg. The watershed makes up 3 percent of the watershed of Buffalo Creek. There are of streams in the watershed of Muddy Run, of which are in agricultural land. A total of 57
9738244
Buffalo Creek (West Branch Susquehanna River tributary)


Buffalo Creek and all its tributaries in 2000 and 2008 was approximately per year. The pH and calcium carbonate concentration have both increased in the upper reaches of Buffalo Creek since September 2009, as has the water temperature. The phosphorus concentration at the point where Buffalo Flat Road passes over Buffalo Creek has increased by at least tenfold since September 2009. Parts of Coal Run, Rapid Run, Beaver Run, and Muddy Run are impaired or possibly impaired by agriculture. The elevation of the mouth of Buffalo Creek is between above sea level
6459894
Gewässerkennzahl


system of the regional Wasser- und Bodenverband (association for water and ground management). The numbers for a watercourse and its catchment area are thus identical. If a river has subsidiary watercourses, an additional figure is allocated to its index number for each further branch. So in theory even a rivulet could be allocated its own catchment. In practice, catchment numbering for water sources below the level of streams are not used. Catchment areas are thus distinguished by a number with up to a maximum of seven digits. Watercourse index numbers
11932339
Eider Canal


. Though the new canal's western end is farther south (at the mouth of the Elbe), much of the Eider Canal's watercourse was reused for the new waterway. Many sections were deepened, and some were straightened, cutting off bends that still exist as lakes. The new canal was opened by Kaiser Wilhelm II in 1895. In 1783, as part of the canal's development, three warehouses (called "packing houses" in German) were built along the watercourse: one at the Kiel-Holtenau lock
20050281
Jackson Creek (Toronto)


Jackson Creek is a watercourse that flows into Lake Ontario near 10th Street, in the New Toronto neighbourhood of Etobicoke, a suburb of Toronto, Ontario, Canada. It is part of the Great Lakes Basin. Its headwaters were approximately five kilometers northwest—north of Bloor Street, near Highway 427. Portions of the watercourse remain above-ground today. The creek is named for Jackson Farm, the historical location of its mouth. Even though lost, for now, Jackson Creek is a strong candidate for day-lighting with
14363282
Bonar Creek


Bonar Creek was a creek in Mimico, Ontario, Canada. It was a tributary of the still-existing Mimico Creek, a watercourse that empties into Lake Ontario. Bonar Creek joined Mimico Creek north of Lake Shore Boulevard, in the marsh at the mouth of the Mimico Creek. The creek is named for Irish immigrants Bill and Letitia Bonar who lived in a pumphouse near the waterway. Almost the entire creek has been buried, except for a short stretch where the former watercourse joined Mimico Creek, and that remaining portion has
20143285
Kampen, Overijssel


, the watercourse of the river IJssel was dredged several times, but the costs were relatively high and within a few years, the river silted up again. As the IJssel had several delta-like mouths here, the main route of the river shifted several times. In the 19th century, a new strategy was put in place to counter this problem: some watercourses were dammed to allow for more water at a higher speed through one or two main routes. This had the advantage that less sand and silt were deposited and
880447
Big Muddy Creek (Missouri River tributary)


past Plentywood, then south, forming the eastern border of Fort Peck Indian Reservation. It joins the Missouri west of Culbertson. It was explored in 1805 by the Lewis and Clark Expedition, who called it Martha's River in their journals and noticed on their return voyage in 1806 that it had changed its mouth on the Missouri. Along with the Milk River and the Poplar River, it is one of three waterways in Canada that drain into the Gulf of Mexico. Big Muddy Creek has also been known as: Big Muddy
5229781
Sheldrake River


these watercourses must meet standards that enable those uses. Class C watercourses also are suitable for primary and secondary contact recreation even though other factors may limit the use for that purpose. Water quality standards for Class C watercourses include limitations on fecal coliform, pH, total dissolved solids, and dissolved oxygen. Two principal tributaries enter the Mamaroneck River, one from the east and one from the west. The East Branch of the Mamaroneck River is the furthest upstream tributary along the Mamaroneck River and originates in north Harrison near the intersection of
6876631
Lothian


spelling) meaning "country of the fort of Lugus", the latter being a Celtic god of commerce. Alternatively it may take its name from a watercourse which flows through the region, now known as the Lothian Burn, the name of which comes from either the British "lutna" meaning "dark or muddy stream", "*lǭd", with a meaning associated with flooding (see Leeds), or "lǖch", meaning "bright, shining". A popular legend is that the name comes from
13668638
Kolan River


then flows east and then finally north by east and reaches its mouth north of . The Kolan River is joined by nineteen tributaries including the main tributary, Gin-Gin Creek, a watercourse that is long. The lower reaches of the river are surrounded by sugar cane fields. The Mouth of Kolan River Regional Park is a protected area at the river mouth. The river descends over its course. Other water storage facilities that are supplied with water from the river include the Bucca Weir and the Kolan Barrage. "Macfadyena unguis
21876707
Cispus River


as Walupt Creek. About from its mouth, the Cispus River receives Muddy Fork from the left. Muddy Fork starts from this junction, at Mount Adams' Lava Glacier and is named for the glacial debris and silt in the water which give the river a muddy appearance. The Cispus River flows through a heavily forested valley, much of the forest regrown after the Cispus Burn, which occurred the first decade of the 20th century and consumed most of the lower drainage. The rushing Canyon Creek enters the river originating high on the
12500641
Muddy Roots


The second annual Muddy Roots Spring Weekender was held from May 16, 2014 to May 17, 2014 in Nashville, Indiana at the Valley Branch Retreat. Dr. Ralph Stanley announced that he will be retiring at the end of 2014; his farewell tour included performing at the Muddy Roots Spring Weekender. The third annual Muddy Roots Europe festival was held from June 20, 2014 to June 22, 2014 at the Cowboy Up Steakhouse Saloon in Waardamme, Belgium. The fifth annual Muddy Roots Music Festival was held from August 29, 2014
2579487
Jebel Dair


A small muddy reservoir can be seen near the northwest corner of the photograph, and sand dunes to the northwest. With the exception of Jebel Dair, most of the region is fairly flat. It is hot and semiarid, and marginally suited for subsistence agriculture, as well as for commercial crops of peanuts, sesame, and gum arabic. Drainage patterns dominate the landscape in central Sudan west of the White Nile River. Several major wadis, intermittently flowing watercourses, merge west and northwest of the mountain. The sand dunes nearby
19011328
Waterways, Oxford


Trap Grounds is a delightfully muddy wetland full of wildlife. The wetland is fed by the watercourse that runs through the estate from the 'lake' that was originally one of the North Oxford clay pits. The estate was built between 2000 and 2006, on the site of the British Motor Corporation's former Osberton Radiator Factory. There is a Waterways Residents Association (WRA) which represents everyone living on the estate, The Waterways Management Company (WMC) manages most of the public areas and leasehold properties on the Estate and represents
8702318
Sternotherus odoratus


A wild common musk turtle often will not hesitate to bite if harassed. Because its neck can extend as far as its hind feet, caution is required when handling one. "S. odoratus" turtle is found in a variety of wetland habitats and littoral zones, particularly shallow watercourses with a slow current and muddy bottom. Although it is more aquatic than some turtles, it is also capable of climbing, and may be seen basking on fallen trees and woody debris. Fallen trees and coarse woody debris are known to be important
18357455
Zuiderzee Works


after six months of continuous pumping. "Drained" in this context does not mean the land was wholly dry; extensive pools of shallow water still littered the muddy landscape. To make the soil usable it had to be further drained by a network of drainage canals. Small ditches were dug leading to larger watercourses, which in turn transported their water to the main drainage canals. These canals, dredged when the polder was still filled with water, conducted surplus water to the pumping stations. The resulting dehydration caused the former seabed
18784632
Montgomery, New York


second largest developed park in Orange County, is named after a sympathizer to the British during the American Revolution. The Wallkill River is the town's major watercourse, flowing through it from south to north past both the villages Montgomery and Walden, also partially serving as its border with Hamptonburgh. Two of its tributaries flow through Montgomery as well. The Muddy Kill, located entirely within the town, drains the area below the Comfort Hills in west central Montgomery. Tin Brook, the Wallkill's only major eastern tributary, rises just
17104610
Josiah Gregg


the mouth of a watercourse which they called the Little River. After exploring slightly to the north, they turned south along the coast and camped at Trinidad. Leaving Trinidad, they crossed a large river, but the fed-up members of the exploring party did not wish to wait for Gregg to determine the latitude of the mouth, and so pushed off without him. When he caught up with the group, his temper flared, and they named the river Mad River due to the outburst. On 20 December 1849,
19632321
King Sound


King Sound is a large gulf in northern Western Australia. It expands from the mouth of the Fitzroy River, one of Australia's largest watercourses, and opens to the Indian Ocean. It is about 120 km long, and averages about 50 km in width. The port town of Derby lies near the mouth of the Fitzroy River on the eastern shore of King Sound. King Sound has the highest tides in Australia, and amongst the highest in the world, reaching a maximum tidal range of 11.8 metres at Derby. The
309139
List of rivers of England


example is the River Tyne (MS), the confluence of the South Tyne (Rs) and the North Tyne (Ls) near Hexham. Those few watercourses (mainly in the Thames catchment) which branch off a major channel and then rejoin it or another watercourse further downstream are known as distributaries or anabranches and are labelled (d). The list is (or at least will be when completed) essentially a list of the main rivers of England (as defined by the Environment Agency) and which includes those named
19643300
Cephalocarida


elongated body. They have a large head, the hind edge of which covers the first thoracic segment. They have no eyes, presumably because of their muddy natural habitat. The second pair of antennae is located behind the mouth; in all other crustaceans the antennae are in front of the mouth at the adult stage, and only their larvae have antennae that have the same location as adult cephalocaridans. The mouth is located behind the large upper lip, flanked by mandibles. The first pair of maxillae is very small, and
18984782
Callville, Nevada


in St. George, he employed Hamblin and son, Cannon and Whitmore. Their travels included leaving the mouth of the Muddy River, traveling down the Virgin River for , continuing through Echo Wash for , before heading southwestward for to the Colorado River, a mile below the mouth of the narrows of Boulder Canyon and above the mouth of Black Canyon, where they located a black rocky point, which was considered a suitable spot for the construction of a warehouse, above high-water mark. It was located just below the confluence
3346567
Otoineppu, Hokkaido


In Ainu language, Otoineppu means "muddy river mouth". The name is probably a reference to muddy appearance of the water at the confluence of the Teshio River and one of its many tributaries, the Otoineppu River. Otoineppu is a landlocked village at the north of Hokkaido. The village sits at the northern tip of the Nayoro Basin, and is flanked by the Kitami Mountains to the east and the Teshio Mountains to the west. The town covers , measures from east to west and from north to south. The village
3732704
Discovery Bay, Washington


Peninsula of Washington state. The bay enters the Strait of Juan de Fuca between the Miller and Quimper peninsulas. The bay's mouth is just south of Protection Island, a small federally protected nature preserve. Discovery Bay is in length, and wide at its mouth. Its primary inlet is Snow Creek at the south end of the bay, and other small watercourses feed the bay on its east and west sides. The community of Discovery Bay is an area near the intersection of U.S. Route 101 and State Route 20, at
9005206
Goat Rock Beach


, especially in the pupping season. The Russian River, with its mouth at the north end of Goat Rock Beach, is Sonoma County's largest watercourse, both in flow rate and lineal extent. Immediately beyond the Russian River discharge to the Pacific Ocean is the coastal town of Jenner. North of the mouth of the Russian River is Jenner Beach. Goat Rock protrudes into the Pacific at the south end of Goat Rock Beach. Visitors can access the base of Goat Rock via a low lying isthmus of land which has been
9690212
River Tolka


to the tidal part of the Tolka, or its estuary, but have been confused by the merging of natural watercourses and city drainage lines. There are at least four such watercourses, including the multi-branched water sometimes called the "Grace Park Stream", another sometimes "Middle Arch Stream" and the Marino Stream. The Wad River system, coming from north Ballymun, interconnects with the Tolka, most notably via a link with the Claremont Stream, and with the Wad River Diversion, which flows along Ballymun Road and
14636429
Rijkevoort


living at the altitude of the monastery. About 2000, the last sisters, who all reached a high age, left for Tienray. Their sober monastery building is still in Rijkevoort. The Sint Anthonisloop, a channeled side branch of the Lage Raam, runs through the center of the village. The Lage Raam flows south of the village. These watercourses take care of the drainage of the former trout areas, all of which are mined to the agricultural area on a few strips of trees along the watercourses. Football club Toxandria
16606129
Gwydir River


The Gwydir River further splits into two anabranch west of Moree - the Lower Gwydir or "Big Leather Watercourse" is the southern channel, and the "Gingham Channel" is the northern branch. The Gingham Channel flows west and becomes undefined in wetlands and floodplains around west of Moree. Only in larger flood events does it then join with the Ballone Creek before it flows into the Barwon River. The Big Leather Watercourse then also loses definition in wetlands and floodplains to the west and only larger floods joins with the Barwon River to
17325263
Halpin Covered Bridge


The Halpin Covered Bridge, also called the High Covered Bridge, is a wooden covered bridge carrying Halpin Bridge Road across the Muddy Branch of the New Haven River in Middlebury, Vermont. It was listed on the National Register of Historic Places in 1974. The Halpin Covered Bridge is located in a rural area of northern Middlebury, near or on the border with neighboring New Haven on Halpin Bridge Road, a dead-end road off Halpin Road. The bridge spans a gorge carrying the Muddy Branch of the New Haven River,
10296507
Solenette


more specific habitat requirements than other widespread Atlantic flatfish such as the European plaice, common sole, and common dab. It is concentrated in waters moderately influenced by estuary outflows, at a salinity of 29-33 ppt, and is absent from the mouths of the largest estuaries where the salinity is lower. The solenette is often found on or half-buried in muddy or muddy-sandy substrates. The smallest of the soles in European waters, the solenette usually measures long and attains a maximum length of . It has an
12355666
Virgin chub


are with extremely faint lines. It is restricted to the Virgin River in Arizona, Nevada, and Utah. Another sizable population is found in the upper and middle reaches of the Muddy River in Nevada. The Arizona range of the Virgin chub is restricted to the Virgin River within Mohave County. In its native habitat, it occurs only in the mainstream of the Virgin and Muddy Rivers (Water within these rivers are generally somewhat warm, turbid, and saline), and very rarely in the immediate mouths of its major tributaries
3131168
Sumer


seen as the union of fresh and salt water; as male Abzu, and female Tiamat. The products of that union, Lahm and Lahmu, "the muddy ones", were titles given to the gate keepers of the E-Abzu temple of Enki, in Eridu, the first Sumerian city. Describing the way that muddy islands emerge from the confluence of fresh and salty water at the mouth of the Euphrates, where the river deposited its load of silt, a second hieros gamos supposedly created Anshar and Kishar, the
5423111
The 40th Anniversary Henry Cow Box Set


Legend" (1973), while "Ottawa Song" is part of a longer suite Frith composed for the Ottawa Company, the rest of which never survived, except for fragments that appeared in "Muddy Mouse" and "Muddy Mouth" on Wyatt's solo album, "Ruth Is Stranger Than Richard" (1975). This performance of "Ottawa Song" also appears (by accident) on "", but without the introductory bassoon solo. "Gloria Gloom" is from Matching Mole's second album, "
6742497
East Branch Tunkhannock Creek


Creek joins East Branch Tunkhannock Creek upstream of its mouth, near Elkdale, and drains an area of . Tinker Creek joins East Branch Tunkhannock Creek upstream of its mouth, within of Elkdale, and drains an area of . Dundaff Creek joins East Branch Tunkhannock Creek upstream of its mouth, within of Clifford, and drains an area of . Idlewild Creek joins East Branch Tunkhannock Creek upstream of its mouth, within of Royal, and drains an area of . East Branch Tunkhannock Creek is not designated as an impaired waterbody. The water
2591517
Special Operations Volunteer Force


, although a military one, was controlled by the Special Branch. It was formed from surrendered communist insurgents. The goal was to put the guerrilla's experience to work for the British. SEP/CEP volunteers to the SOVF committed to serving for 18 months. They were paid at the same rate as the junior police officers and were based in the same police compounds from which other government forces operated. SEP/CEP volunteers were formed into platoons and placed under the command of a British police officer. At the start of
17929996
Coronel, Chile


Coronel is a Chilean city and commune, located in the Concepción Province of the eighth region of Bio Bío. The city of Coronel is located in a sandy platform that goes from the mouth of the Biobío River to the Arauco Gulf bay, a muddy landscape, full of forests, typical of the region. This muddy, forested landscape enclosed by high mountains was what the first Spanish conquistadors and settlers found when arriving. Vegetation and forests covered most of the area except very close to the coast. This type of landscape is
13950320
Muddy Boggy Creek


timber. Near the source, the Muddy Boggy passes through the Arbuckle Mountains, and has a gradient of about . By the time it flows through the Cretaceous area, the gradient is only . It then flows through the Ouachita Mountains. Clear Boggy Creek has a gradient of about near its source and near its mouth. The river basin is about long by wide. The drainage area is , and includes parts of Coal, Pontotoc, Hughes, Pittsburg, Atoka, Johnson, Bryan, Pushmataha, and Choctaw counties. Muriel
16641970
Strzelecki Creek


The Strzelecki Creek, part of the Lake Eyre basin, is an ephemeral watercourse located in the Australian state of South Australia. The Strzelecki is a distributary of Cooper Creek and branches off near the town of Innamincka and flows in a southerly direction thought the Strzelecki Desert for about towards Lake Blanche. While being feed by the Cooper Creek, it does have its own catchment and can flow independently after ‘heavy localised storms.’ Flows on ‘exceptional’ occasions can reach Lakes Blanche, Callabonna, Frome and Gregory. Its watercourse
15890487
Wapous River


the upper part of this watercourse. This road branch connects with route 212 which bypasses the Gouin Reservoir by the north-east and connects the village of Obedjiwan, Quebec and La Tuque. The surface of the Wapous River is usually frozen from mid-November to the end of April, however, safe ice circulation is generally from early December to late March. Formerly, this watercourse has been designated "Black Castor River". The toponym "Wapous River" was formalized on December 5, 1968 at the Commission de toponymie
2153243
List of islands within the Murray River in South Australia


List of islands within the Murray River in South Australia is a list of islands located within the watercourse of the Murray River within the Australian state of South Australia from the mouth of the river at Encounter Bay in the south to the borders with the states of New South Wales and Victoria in the east including the following lakes located adjacent to the river's mouth - Coorong, Lake Albert and Lake Alexandrina. The following list includes islands (listed from west to east) in the Coorong as well as the following two channels connecting
14223286
Branchburg, New Jersey


Neshanic Station (ZIP Code 08853) and North Branch (ZIP Code 08876), North Branch Depot and Woodfern. The township is bordered on the west by Readington Township in Hunterdon County; on the north by Bedminster Township and on the south by Bridgewater Township and Hillsborough Township. The main watercourses are the Lamington River on the north, the North Branch of the Raritan River on the east and the South Branch of the Raritan River on the east and south. These rivers along with small streams and brooks are excellent for fishermen
4588088
Marys River (Oregon)


mouth, it flows under Route 20 for the third time, immediately receives Woods Creek from the right and turns southeast. It soon passes under Oregon Route 34 at the unincorporated community of Flynn, where it receives Greasy Creek from the right. Marys River then flows southeast by Philomath, which lies to its left (north), receives Newton Creek from the left, and passes a United States Geological Survey (USGS) stream gauge at from the mouth. At about from the mouth, the river receives Muddy Creek from the
13071551
World Qualification Series (2009)


18 - Aug 23" 30th Anniversary of the Lacanau Pro and good conditions this year. Surf, concerts, events scheduled. Check out the video for a summary of the event http://vimeo.com/6994555 "Aug 25 - Aug 30" "Sep 01 - Sep 06" "Sep 01 - Sep 06" "Sep 04 - Sep 06" "Sep 09 - Sep 12" "Sep 10 - Sep 13" "Sep 08 - Sep 13" "Sep 15 - Sep 20" "Sep 16 - Sep 22" "Sep
1986943
Nine Mile Run (New Jersey)


to access in most places. There are many roads that cross this stream, so accessing it is not a problem. The stream has varying terrain. Upstream, it is a fast flowing small stream with a generally rocky streambed. By Beekman Road, it slows down while still retaining a rocky bottom. Past Bennington Parkway, it gradually becomes more muddy and wide. Near its mouth at Cortelyous Lane, it is very muddy, slow, and wide. Some sides have steep banks. The banks are composed of shale in
13987481
Muddy Fork (Oregon)


course lies within the Mount Hood National Forest and Clackamas County. Falling between source and mouth, the stream's average loss of elevation is about . Flowing generally west from the glacier, it passes south of McNeil Point, which is on the stream's right. It then flows between Yocum Ridge, which is to the left, and Bald Mountain to the right before being crossed by the Pacific Crest Trail near the eastern end of Old Maid Flat. The Sandy River enters Old Maid Flat to the left of Muddy Fork,
17959029
Name of Toronto


disparaging Muddy York, used during the settlement's early growth. At the time, there were no sewers or storm drains, and the streets were unpaved. During rainfall, water would accumulate on the dirt roads, transforming them into often impassable muddy avenues. A more disparaging nickname used by the early residents was Little York, referring to its establishment as a collection of twelve log homes at the mouth of the Don River surrounded by wilderness, and used in comparison to New York City in the United States and York in England
7759042
Maryland Route 28


East of MD 112, MD 28 curves northeast and expands to a four-lane divided highway before passing Quince Orchard High School and intersecting MD 124 (Quince Orchard Road) at the southwest corner of the city of Gaithersburg. MD 28 continues southeast along the southern edge of Gaithersburg and passes by the new urbanist development Kentlands. The highway crosses Muddy Branch parallel to a pair of spurs on the south designated MD 899 (American Way). After the state highway expands to six lanes and intersects Muddy Branch Road, the old
12782076
Maryland Route 119


119 with I-370, I-270, MD 200, and the Shady Grove station along Washington Metro's Red Line. At the county highway, MD 119 enters the city of Gaithersburg and temporarily expands to six lanes until its intersection with Muddy Branch Road. The highway crosses Muddy Branch and passes along the edge of the New Urbanist community of Kentlands before intersecting MD 124 (Quince Orchard Road). MD 119 leaves the city of Gaithersburg and passes through Seneca Creek State Park. The highway does not provide access to the state park;
2793846
Warabandi system


number of rotational distributaries with carrying a full amount of water supply for ensuring every farmer gets enough water supply and equitable as the branch canals deliver water to watercourses after bringing into distributaries. The streams form tertiary distribution with full amount since the water from distributaries was supplied. Besides, the delivery of the water can't fulfill the demand since the volume of the watercourses are limited, so, the proceed of the delivery will continue about seven days to ensure every farmer receives the water. After seven days, which finished a period
16473840
Dugway Brook Watershed


northwesterly direction, then passing through Cleveland Heights, East Cleveland, and the City of Cleveland, where the two branches merge at a point just south of what is now Interstate 90. Dugway Brook then cuts northerly through the shoreline suburb of Bratenahl as a single watercourse, and finally discharges into Lake Erie. Dugway Brook is now an almost entirely enclosed culverted watercourse, running in its natural channel under and alongside streets and city parks built around it. The brook appears to have been culverted early in the 20th century, partly because
20228589
List of 1982–83 NBA season transactions


1982 Oct 2, 1982 Oct 1, 1982 Sep 30, 1982 Sep 29, 1982 Sep 28, 1982 Sep 27, 1982 Sep 24, 1982 Sep 22, 1982 Sep 20, 1982 Sep 19, 1982 Sep 18, 1982 Sep 17, 1982 Sep 15, 1982 Sep 14, 1982 Sep 13, 1982 Sep 10, 1982 Sep 9, 1982 Sep 7, 1982 Sep 2, 1982 Sep 1, 1982 Aug 31, 1982 Aug 27, 1982 Aug 26, 1982 Aug 16, 1982 Aug 8,
557049
Muddy Run (West Branch Susquehanna River tributary)


of the watershed, is the only entity permitted to discharge sediment in the Muddy Run watershed. There is a total daily load of of sediment. comes from cropland, comes from the banks of streams, and comes from land used for hay or pastures. A total of comes from developed land, comes from forests, and comes from wetlands. The average annual amount of precipitation between the early 1990s and the early 2010s was . The average amount of annual runoff during the same time period was . In the Muddy Run watershed
3360544
Kymi (river)


about inland of the Gulf of Finland. The eastern branch splits into the Korkeakoski and Koivukoski branches, the latter branch dividing again to form two mouths (Langinkoski and Huumanhaara). The Korkeakoski branch has only one river mouth. The western branch divides into Ahvenkoski and Klåsarö branches, each with one mouth. The westernmost Ahvenkoski branch of the river served as a border between Sweden and Russia from 1743 to 1809. The parts of Finland east of the river were later called Old Finland. Old Finland was incorporated in the Grand Duchy
19353265
Muddy Run (West Branch Susquehanna River tributary)


Run begins in a valley in eastern Turbot Township, near the Paradise Church. The creek heads westward before turning south and then southwest. It crosses under Interstate 80 and turns due west again. After some distance, the creek crosses under Pennsylvania Route 147 and turns northwest past a country club. North of the country club, it turns abruptly north and then west again, crossing under Pennsylvania Route 405 and entering the West Branch Susquehanna River. Muddy Run's main tributaries are unnamed. The Hoeganaes Corporation, in the northwestern part
3360543
Double Branch


Double Branch is a stream in Bates County in the U.S. state of Missouri. It is a tributary to the Marais des Cygnes River. The stream headwaters arise just north of Missouri Route 52 about six miles east-southeast of Butler and the stream flows under Route 52 to the south-southwest. The stream joins the Marais des Cygnes River at the "He Bend" four miles northeast of Rich Hill. The headwaters are at and the confluence is at . Double Branch was named for the fact its watercourse has two branches
11745409
Muddy Kill


Muddy Kill is a tributary of the Wallkill River that runs entirely through the town of Montgomery in Orange County, New York, United States. It rises from a small pond just over a mile (1.7 km) west of the village of Walden, flowing first southwesterly then roughly due south to empty into the Wallkill just upstream from the village of Montgomery. Its course takes it mostly through areas cleared for agriculture, although not all are presently cultivated. Near its mouth it passes through a large horse farm, and then once
5438398
Missouri River


I never saw anything more terrific," Jolliet wrote, "a tangle of entire trees from the mouth of the Pekistanoui [Missouri] with such impetuosity that one could not attempt to cross it without great danger. The commotion was such that the water was made muddy by it and could not clear itself." They recorded "Pekitanoui" or "Pekistanoui" as the local name for the Missouri. However, the party never explored the Missouri beyond its mouth, nor did they linger in the area. In addition,
19833441
Ruth Is Stranger Than Richard


Fred Frith collaboration "Muddy Mouth"—with a series of brief, nonsensical interludes featuring only sparse piano accompaniment and some very strange high-pitched yelping vocals under the collective title "Muddy Mouse". "Ruth Is Stranger Than Richard" was released in May 1975. Unlike its predecessor "Rock Bottom", it received a mixed critical and public response; not counting 1982's "Nothing Can Stop Us" (which brought together a series of previously released single A and B sides, most of which were cover versions), "
16513218
Chillisquaque Creek


Chillisquaque Creek, and Middle Branch Chillisquaque Creek. Beaver Run joins Chillisquaque Creek upstream of its mouth and its watershed has an area of . Mud Creek joins Chillisquaque Creek upstream of its mouth and its watershed has an area of . West Branch Chillisquaque Creek joins Chillisquaque Creek upstream of its mouth. East Branch Chillisquaque Creek joins Chillisquaque Creek upstream of its mouth, as does Middle Branch Chillisquaque Creek. Their watersheds have areas of and , respectively. Reaches of Chillisquaque Creek are designated as an impaired waterbody. Causes of impairment include sedimentation/
12695750
Waihao River


The Waihao River is a natural watercourse in the Canterbury region of New Zealand's South Island. It flows into the Wainono Lagoon near Studholme. Its headwaters are in the Hunter Hills, foothills of the Southern Alps, and its catchment area is . The catchment receives approximately of rain annually. In its upper reaches, the river has two branches, the North Branch and South Branch, which join together at Waihao Forks. The river is well defined, but when it nears the coast, it becomes a braided river and has
81642
Raccoon Branch Wilderness


peaks on Dickey Ridge, High Point (4,019 feet) and Dicky Knob (3,606 feet)). There is a 300 foot high rock slide area on the eastern boundary, now stabilized with small pines beginning to grow. The wilderness includes the full watershed of Raccoon Branch and Scott Branch, tributaries of Dickey Creek. Other small streams, including Scott Branch, Shanty Branch, Muddy Branch, Slabtree Branch, Mullins Branch, Russell Hollow and Wildcat Branch, all flow from the wilderness in different directions to eventually reach the Holston
6853353
North Branch Buffalo Creek


the right. It then turns southeast for several tenths of a mile before reaching its confluence with Buffalo Creek. North Branch Buffalo Creek joins Buffalo Creek upstream of its mouth. North Branch Buffalo Creek has two named tributaries: Coal Run and Panther Run. Coal Run joins North Branch Buffalo Creek upstream of its mouth and its watershed has an area of . Panther Run joins North Branch Buffalo Creek upstream of its mouth and its watershed has an area of . Some stream reaches in the watershed of North Branch Buffalo Creek are designated as
11397642
Amazon River


conservative measurement excluding the Pará river estuary, from the mouth of the Araguari River to Ponta do Navio on the northern coast of Marajó, would still give the mouth of the Amazon a width of over . If only the river's main channel is considered, between the islands of Curuá (state of Amapá) and Jurupari (state of Pará), the width falls to about . The plume generated by the river's discharge covers up to 1.3 million square kilometres and is responsible for muddy bottoms influencing a wide area of the
1593115
Barbeled houndshark


The barbeled houndshark ("Leptocharias smithii") is a species of ground shark and the only member of the family Leptochariidae. This demersal species is found in the coastal waters of the eastern Atlantic Ocean from Mauritania to Angola, at depths of . It favors muddy habitats, particularly around river mouths. The barbeled houndshark is characterized by a very slender body, nasal barbels, long furrows at the corners of the mouth, and sexually dimorphic teeth. Its maximum known length is . Likely strong-swimming and opportunistic, the barbeled
7264457
West Branch Little Muncy Creek


. West Branch Little Muncy Creek joins Little Muncy Creek upstream of its mouth. West Branch Little Muncy Creek has one named tributary, which is known as West Creek. West Creek joins West Branch Little Muncy Creek upstream of its mouth, near Biggerstown, and drains an area of . The elevation near the mouth of West Branch Little Muncy Creek is above sea level. The elevation of the creek's source is above sea level. The surficial geology alongside West Branch Little Muncy Creek in its lower reaches mainly consists of alluvium.
3601654
September 1941 lunar eclipse


A partial lunar eclipse took place on Friday, September 5, 1941. It was a shallow partial lunar eclipse, with less than 10% of the Moon covered in Earth's shadow. Aug 31, 1941 = Sunday Sep 1, 1941 = Monday Sep 2, 1941 = Tuesday Sep 3, 1941 = Wednesday Sep 4, 1941 = Thursday Sep 5, 1941 = Friday Sep 6, 1941 = Saturday Sep 7, 1941 = Sunday Sep 8, 1941 = Monday Sep 9, 1941 = Tuesday Sep 10, 1941
5363349
Stone's Ferry, Nevada


Stone's Ferry is a former Mormon settlement and ferry crossing of the Colorado River between Nevada and Arizona, in Clark County, Nevada, United States. It was variously located during its history from the mouth of the Virgin River to 6 miles below the mouth of the Virgin River, opposite the Detrital Valley which provided an easy path into and out of the canyon of the Colorado River from the south and to and from the north through the Virgin and Muddy Valleys to Nevada and Utah. Subsequently, it was moved up river
22179365
Witch (righteye flounder)


Glyptocephalus cynoglossus, known in English by a variety of common names including the witch, witch flounder, pole flounder, craig fluke, Torbay sole and grey sole, is a species of flatfish from the family Pleuronectidae. It occurs on both sides of the North Atlantic Ocean on muddy sea beds in quite deep water. In northern Europe it has some importance in fisheries as a food fish. "Glyptocephalus cynoglossus" is a right-eyed flatfish with a small mouth which reaches the forward edge of the lower eye. The mouth
608331
Peterman Run


West Branch Fishing Creek. Peterman Run joins West Branch Fishing Creek upstream of its mouth, only upstream of the mouth of Rough Run. A total of of Peterman Run is considered to be impaired due to atmospheric deposition and metals. The impaired waters of the stream comprise approximately 4.01 percent of the total impaired waters in Sullivan County within the watersheds of West Branch Fishing Creek and East Branch Fishing Creek. The elevation near the mouth of Peterman Run is above sea level. The elevation of the stream's source is between above sea
15935990
Sheldrake River


Park in Mamaroneck Village business district. The East Branch of the Sheldrake River originates in Scarsdale and flows south through the Bonnie-Briar Country Club to meet the east tributary at Fenimore Road. Below Fenimore Road, the east branch flows through Rockland Avenue to meet the Sheldrake River below Valley Stream Road. The Sheldrake River and east branch have been classified by the New York State Department of Environmental Conservation as Class C. According to this state water quality classification, Class C watercourses should be suitable for fishing and fish propagation and discharges to
6876630
USS Vesuvius (1806)


New York area until the spring 1809, when she again sailed for New Orleans. Embarking upon duties to suppress slave traders and pirates operating out of the trackless bayous, "Vesuvius" cruised off the mouth of the muddy Mississippi River and into the Gulf of Mexico, alert for any sign of illegal activity. The crew's vigilance was rewarded in February 1810 when, under the command of Lieutenant Benjamin F. Read, "Vesuvius" gave chase to a pirate vessel off the mouth of the Mississippi and captured "Duc de Montebello
21678112
Roaring Run (Bowman Creek tributary)


Branch Roaring Run. Newton Run joins Roaring Run upstream of its mouth and drains an area of . South Branch Roaring Run joins Roaring Run upstream of its mouth and drains an area of . The alkalinity of Roaring Run upstream of the tributary South Branch Roaring Run is . Downstream of South Branch Roaring Run, the concentration increases to . The elevation near the mouth of Roaring Run is above sea level. The elevation of the stream's source is between above sea level. In its lower reaches, Roaring Run flows through a band
21918061
Humber


. The estuary appears in some Latin sources as (A name used by Edmund Spenser in "The Faerie Queene"). This is possibly a Latinisation of the Celtic form (Welsh for river mouth or estuary), but is erroneously given as a name for both the Humber and The Ouse as one continuous watercourse. Both and may record an older Indo-European word for water or river, (as in the ‘Five Rivers’ of the Punjab). An alternative derivation may be from the Latin verb meaning black
14140060
Ctenophora


as a stomach; and a system of internal canals. These branch through the mesoglea to the most active parts of the animal: the mouth and pharynx; the roots of the tentacles, if present; all along the underside of each comb row; and four branches round the sensory complex at the far end from the mouth – two of these four branches terminate in anal pores. The inner surface of the cavity is lined with an epithelium, the gastrodermis. The mouth and pharynx have both cilia and well-developed muscles
15997597
East Branch Briar Creek


turn west and passes along the outskirts of Berwick. After less than a mile, it enters the community of Briar Creek. Shortly afterwards, the creek reaches its confluence with Briar Creek. East Branch Briar Creek joins Briar Creek upstream of its mouth. Tributaries of East Branch Briar Creek include Kashinka Hollow and Glen Brook. Kashinka Hollow joins East Branch Briar Creek upstream of its mouth. Its watershed has an area of . Glen Brook joins the creek upstream of its mouth. Its watershed has an area of . The discharge of
13991811