West Branch Run [SEP] mouth of the watercourse
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West Branch Run


mouth. Its watershed has an area of . The elevation of West Branch Run near its mouth is above sea level. At its headwaters, the stream has an elevation of approximately above sea level. West Branch Run flows through a valley known as California Hollow in Pine Township, Columbia County. West Branch Run has high levels of dissolved oxygen. The watershed of West Branch Run has an area of . There are no roads along West Branch Run where it flows through California Hollow. The stream is one of only a few
12436560
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
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
Elk Run (West Branch Fishing Creek tributary)


Sugarloaf Township, Columbia County. It continues flowing south-southeast through the village of Elk Grove. After a short distance, the stream reaches its confluence with West Branch Fishing Creek. Elk Run joins West Branch Fishing Creek upstream of its mouth. Elk Run has three named tributaries: Gallows Run, Hog Run, and Long Run. Gallows Run joins Elk Run upstream of its mouth. Its watershed has an area of . Hog Run joins Elk Run upstream of its mouth. Its watershed has an area of . Long Run
16058390
Rough Run


mile, the stream turns southwest for several hundred feet. It then turns south-southeast for several hundred feet and reaches the slope. The stream reaches its confluence with West Branch Fishing Creek immediately afterwards. Rough Run joins West Branch Fishing Creek upstream of its mouth, only downstream of the mouth of Peterman Run. The elevation near the mouth of Rough Run is above sea level. The elevation of the stream's source is between . For most of its length, Rough Run is on a glacial till known as the Wisconsinan
15775831
Slip Run (West Branch Fishing Creek tributary)


turning south-southeast and entering a valley. Approximately a mile (two kilometers) further downstream, the stream reaches its confluence with West Branch Fishing Creek not far from Fishing Creek Road. Slip Run joins West Branch Fishing Creek upstream of its mouth. The elevation near the mouth of Slip Run is above sea level. However, the elevation of the stream's source is between above sea level. The stream is on the northern side of North Mountain. The geology in the vicinity of Slip Run has been affected by glaciation
8573683
Dobson Run


the right. It then turns in a generally north-northeasterly direction for several tenths of a mile before reaching its confluence with West Branch Mahantango Creek on the border between Juniata County and Snyder County. Dobson Run joins West Branch Mahantango Creek upstream of its mouth. The elevation near the mouth of Dobson Run is above sea level. The elevation of the stream's source is above sea level. The watershed of Dobson Run has an area of . The mouth of the stream is in the United States Geological Survey quadrangle of Dalmatia
20577001
White Deer Creek


US Route 15 and a few tenths of a mile later, reaches its confluence with the West Branch Susquehanna River. White Deer Creek joins the West Branch Susquehanna River upstream of its mouth. White Deer Creek has five named tributaries: Lick Run, Mile Run, Sand Spring Run, Cowbell Hollow, and Tunis Run. Lick Run joins White Deer Creek upstream of its mouth and drains an area of . Mile Run joins White Deer Creek upstream of its mouth and drains an area of . Sand Spring Run joins the creek upstream
430441
Quaker Run (West Branch Mahantango Creek tributary)


short distance further downstream, the stream reaches its confluence with West Branch Mahantango Creek near the border between Juniata County and Snyder County. Quaker Run joins West Branch Mahantango Creek upstream of its mouth. The elevation near the mouth of Quaker Run is above sea level. The elevation near the stream's source is . Quaker Run is mostly situated between Dresslers Ridge to the south and Graders Ridge to the north, in eastern Monroe Township. A series of gray shales exposed along Quaker Run and dipping 30 degrees southeast, has been observed
20850941
Laurel Run (West Branch Fishing Creek tributary)


abutment walls crosses the stream. Laurel Run begins in a valley in Davidson Township. It flows south for several hundred feet before turning southeast for a few tenths of a mile. The stream then turns south for a similar distance before turning southeast again and exiting the valley. It crosses Fishing Creek Road and a short distance later, reaches its confluence with West Branch Fishing Creek. Laurel Run joins West Branch Fishing Creek upstream of its mouth. The elevation near the mouth of Laurel Run is above sea level. The elevation of
17591582
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
Spring Run (West Branch Susquehanna River tributary)


West Branch Susquehanna River upstream of its mouth. 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. The elevation near the mouth of Spring Run is above sea level. The elevation of the stream's source is above sea level. The watershed of Spring Run has an area of . The stream is entirely within the United States Geological Survey quadrangle of Milton. Its mouth is located at Watsontown
16553285
Stewart Run (Octoraro Creek tributary)


before its confluence with West Branch Octoraro Creek. Stewart Run joins the West Branch Octoraro Creek upriver of its mouth. The elevation near the mouth of Stewart Run is above sea level. The elevation of the creek's source is between above sea level. The stream's watershed is part of the Piedmont region, characterized by rolling hills. The lower of the stream is designated a Scenic River. The watershed of Stewart Run has an area of . Its mouth is in the United States Geological Survey quadrangle of Kirkwood. Its source
20398761
West Branch Run


At the end of the valley, it receives Shingle Run, its only named tributary, and abruptly turns south. After more than a mile, West Branch Run passes the Shoemaker Covered Bridge, crossing Pennsylvania Route 442 on the way, and turns southeast. It then crosses Pennsylvania Route 442 again and shortly afterwards reaches its confluence with Little Fishing Creek. West Branch Run joins Little Fishing Creek upstream of its mouth. The only named tributary of West Branch Run is Shingle Run. Shingle Run joins West Branch Run upstream of its
12436559
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
Glade Run


-northwest for several tenths of a mile before turning northwest and reentering Muncy Creek Township. It then gradually turns south-southwest. After several tenths of a mile, the stream turns northeast before turning west-southwest for a few tenths of a mile. It then reaches its confluence with the West Branch Susquehanna River. Glade Run joins the West Branch Susquehanna River upriver of its mouth. 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
17310246
Buffalo Creek (West Branch Susquehanna River tributary)


Buffalo Creek has six named tributaries: Little Buffalo Creek, Spruce Run, Beaver Run, Stony Run, Rapid Run, and North Branch Buffalo Creek. Little Buffalo Creek joins Buffalo Creek upstream of its mouth and its watershed has an area of , while Spruce Run joins Buffalo Creek upstream of its mouth and its watershed has an area of . Beaver Run joins Buffalo Creek upstream of its mouth and its watershed has an area of , while Stony Run joins Buffalo Creek upstream of its mouth and its watershed has an area of .
6459884
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
Black Run (West Branch Susquehanna River tributary)


the West Branch Susquehanna River upstream of its mouth. 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. The elevation near the mouth of Black Run is above sea level. The elevation of the stream's source is above sea level. Black Run was described as a
16774091
County Line Branch


, it receives the tributary Beaver Run. It then turns northeast into Anthony Township, where it picks up the tributary McKee Run. The stream then turns southeast and reaches its confluence with West Branch Chillisquaque Creek at the southern edge of Anthony Township. County Line Branch joins West Branch Chillisquaque Creek upstream of its mouth. Tributaries of County Line Branch include Beaver Run and McKee Run. The stream also has unnamed tributaries. The entirety of County Line Branch and the entirety of each of its tributaries is considered by the Pennsylvania Department of
8336563
Leiningers Run


another unnamed tributary from the left before turning east-northeast again. After several tenths of a mile, it receives one more unnamed tributary from the left before eventually turning southeast and reaching the end of its valley. A short distance further downstream, the stream reaches its confluence with West Branch Mahantango Creek at the border between Juniata County and Snyder County. Leiningers Run joins West Branch Mahantango Creek upstream of its mouth. The elevation near the mouth of Leiningers Run is above sea level. The elevation near the stream's source is
20643636
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
Dry Run (West Branch Susquehanna River tributary)


. A short distance further downstream, it reaches its confluence with the West Branch Susquehanna River. Dry Run joins the West Branch Susquehanna River upstream of its mouth. 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 . It has a 2 percent chance of reaching and a 1 percent chance of reaching . The peak
16553547
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
Bloody Run (West Branch Fishing Creek tributary)


before turning south-southwest. The stream then turns east-southeast for a few tenths of a mile and its valley deepens. It turns south-southeast and then south for approximately two miles (three kilometers) and its valley continues to deepen. The stream then leaves its valley and turns east-southeast for a few tenths of a mile, in the valley of West Branch Fishing Creek. It then reaches its confluence with West Branch Fishing Creek. Bloody Run joins West Branch Fishing Creek upstream of its mouth. The
16172427
Shingle Run (West Branch Run tributary)


its mouth. Shingle Run has a number of tributaries, which are smaller than the stream itself. However, none of them are named. The elevation near the mouth of Shingle Run is above sea level. The elevation of the stream's source is between and above sea level. At least one bridge crosses Shingle Run. It carries State Route 4028. The watershed of Shingle Run has an area of . Its watershed is part of the Lower North Branch Susquehanna River drainage basin. The stream is in the United States Geological
5564597
Lead Run


. Lead Run begins in on a plateau in eastern Davidson Township. It flows west-northwest for approximately before turning southwest and heading into a steep ravine, where it stays for more than a mile. Near its mouth, the stream leaves the ravine and turns south and then east. It then reaches its confluence with East Branch Fishing Creek. Lead Run joins East Branch Fishing Creek upstream of its mouth. Lead Run has no named tributaries. However, it does have a number of unnamed tributaries. The average discharge of
17306560
Lick Run (West Branch Susquehanna River tributary)


is Stone Run, which is geographically similar to Lick Run and joins it one mile upstream of the Baney Settlement. The daily load of manganese near the mouth of Fork Run is per day. The load of acidity near the mouth is per day and the daily load of alkalinity is . Immediately upstream of Flegals Run, the manganese load of Lick Run is per day. The daily loads of acidity and alkalinity at this location are and , respectively. Between Flegals Run and the mouth of Lick Run, the concentration of manganese
2163283
Sheshequin Path


Sunbury) and west to the "Great Island" (at modern Lock Haven) and further west to Kittanning on the Allegheny River. The east branch followed Loyalsock Creek north from its mouth at the village of "Otstonwakin" (modern Montoursville) to Wallis Run, north there, then west to Lycoming Creek along either Murray Run to the village of Fields Station, or that and Slacks Run to the village of Bodines. The middle branch was about one mile (0.6 km) west of Loyalsock Creek and ran north along
5271117
Turkey Run (West Branch Susquehanna River tributary)


for a few tenths of a mile before turning south and passing through a small pond. After a few tenths of a mile, the stream turns southeast for several tenths of a mile, passing through another small pond, crossing Pennsylvania Route 405, and crossing railroad tracks. It then turns south-southwest for several tenths of a mile before reaching its confluence with the West Branch Susquehanna River. Turkey Run joins the West Branch Susquehanna River upstream of its mouth. Turkey Run is not designated as an impaired waterbody. The elevation
16832365
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
Big Run (West Branch Fishing Creek tributary)


southeast and almost immediately leaves the plateau and begins descending steeply through a deep and narrow valley. After several tenths of a mile, the stream gradually turns south. A short distance further downstream, it crosses Fishing Creek Road and reaches its confluence with West Branch Fishing Creek. Big Run joins West Branch Fishing Creek upstream of its mouth. Between June 2010 and April 2011, the water temperature of Big Run was measured four times during a study of the Fishing Creek watershed. The highest temperature, occurred on June 18, 2010
16410883
Buck Run (West Branch Brandywine Creek tributary)


enters Newlin Township, where it flows south-southeast for several miles until it reaches its confluence with Brandywine Creek. Buck Run joins Brandywine Creek upstream of its mouth. Buck Run has two named tributaries: Birch Run and Doe Run. Birch Run joins Buck Run upstream of its mouth. Its watershed has an area of . Doe Run joins Buck Run upstream of its mouth. Its watershed has an area of . The discharge of Buck Run ranges from 3.9 to 44 cubic feet per second, with an average of 20.3 cubic
8229619
Black Run (West Branch Susquehanna River tributary)


it was noted that there was a potential industrial site to the north of the stream. Black Run was entered into the Geographic Names Information System on August 2, 1979. Its identifier in the Geographic Names Information System is 1169731. In the late 1800s, a tannery discharged waste into Black Run. In 1990, a wastewater treatment plant was proposed; it was planned to be located near the mouth of Black Run and to discharge per day into the West Branch Susquehanna River. The drainage basin of Black Run is designated as
16774093
East Branch Fishing Creek


Branch and Big Run. It starts flowing southwards for approximately one mile before picking up Heberly Run, its longest tributary. Further on, it receives Lead Run and turns southwest towards Jamison City. Shortly after the turn, the creek receives Trout Run, one of its shortest named tributaries. In Jamison City, the creek receives Blackberry Run and several unnamed tributaries before flowing into West Branch Fishing Creek. The total elevation change between East Branch Fishing Creek's source and its mouth is . At one location, East Branch Fishing Creek
15548182
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
Muncy Creek


Susquehanna River. Muncy Creek joins the West Branch Susquehanna River is upstream of its mouth. Significant tributaries of Muncy Creek include Little Muncy Creek and Wolf Run. The watershed of Little Muncy Creek has an area of . This creek reaches its confluence with Muncy Creek upstream of its mouth. The watershed of Wolf Run has an area of . This stream reaches its confluence with Muncy Creek upstream of its mouth. Other large tributaries of the creek include Lewis Creek, Rock Run, and Sugar Run. The watersheds of these tributaries have
7061752
Quaker Run (West Branch Mahantango Creek tributary)


. Gray and brown boulders of conglomerate containing some iron and white quartz have also been observed in the vicinity of the stream. The watershed of Quaker Run has an area of . The stream is entirely within the United States Geological Survey quadrangle of Richfield. Its mouth is located near Richfield. Quaker Run is one of the main streams in Monroe Township, along with Stony Run and West Branch Mahantango Creek. The drainage basin of Quaker Run is designated as a Coldwater Fishery and a Migratory Fishery. The stream is situated near a
20850942
Limestone Run (Montour and Northumberland Counties, Pennsylvania)


254. At this point, the stream turns west, paralleling Limestone Ridge. It exits Limestone Township and enters the southern part of Turbot Township, Northumberland County. The stream continues west, parting from Limestone Ridge and crossing under Interstate 80 and then Pennsylvania Route 147 before entering the borough of Milton. It reaches its confluence with the West Branch Susquehanna River on the other side of Milton, near Milton State Park. Limestone Run joins the West Branch Susquehanna River upriver of its mouth. Limestone Run has no named tributaries. However
8584601
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
Garden Island (South Australia)


connected to a road system that runs from the above-mentioned bridge. An electric power transmission line crosses the island in an east-west direction to a termination point at the Torrens Island Power Station. Garden Island is one of the geographical features in what is now the Adelaide metropolitan area that was formed as a consequence of sea level rise at the start of the Holocene. Sea level rise had three consequences. Firstly, watercourses existing at the time were forced to create new mouths in new coastline. Secondly, currents arising
17998920
Buffalo Creek (West Branch Susquehanna River tributary)


picks up its tributary Stony Run before passing the community of Cameron and picking up Spruce Run. At this point, Buffalo Creek flows along the border between Buffalo Township and Kelly Township. Buffalo Creek then meanders in an eastward direction, passing near a quarry, the community of Kelly Point, and the Lewisburg Federal Penitentiary. After leaving Buffalo Township, the creek flows briefly along the border between Kelly Township and Lewisburg before discharging into the West Branch Susquehanna River. Buffalo Creek joins the West Branch Susquehanna River upriver of its mouth.
6459883
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
Chillisquaque Creek


, before turning south and then west. For more than a mile, the creek flows through a valley between Montour Ridge and a smaller hill. Upon leaving the valley, the creek crosses Pennsylvania Route 147 and Pennsylvania Route 405 and heads in a southwesterly direction for several tenths of a mile before reaching its confluence with the West Branch Susquehanna River. Chillisquaque Creek joins the West Branch Susquehanna River upriver of its mouth. Chillisquaque Creek has five named direct tributaries: Beaver Run, Mud Creek, West Branch Chillisquaque Creek, East Branch
12695749
Black Run (West Branch Susquehanna River tributary)


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. It is a relatively small stream with its mouth located near Montgomery. The stream's watershed is designated as a Warmwater Fishery and a Migratory Fishery. Black Run begins to the east of
16774088
Elk Run (West Branch Fishing Creek tributary)


joins Elk Run upstream of its mouth. Its watershed has an area of . A total of of Elk Run and its unnamed tributaries are considered to be impaired. In Columbia County, of the stream is impaired. The cause of the impairment is atmospheric deposition. The elevation near the mouth of Elk Run is above sea level. The elevation of the stream's source is between . Elk Run has a high gradient and is a clearwater creek. The valley of Elk Run is mostly in the vicinity of Wisconsinan Ice-Contract
16058391
Painter Run


receives another unnamed tributary from the right. The stream then turns southeast for some distance and its valley continues to become deeper. It then receives another unnamed tributary from the left and turns southeast for approximately a mile, flowing alongside State Route 2003. It then gradually turns south-southeast and receives its only named tributary, Oxhorn Run, from the right. Several tenths of a mile further downstream, it reaches its confluence with West Branch Fishing Creek. Painter Run joins West Branch Fishing Creek upstream of its mouth. Painter Run
16233019
Shingle Mill Run


begins in a valley in Davidson Township. It flows east for approximately a mile and its valley becomes progressively deeper. The stream then turns east-southeast for several tenths of a mile. It then receives its first and only named tributary, Bearwallow Run. At this point, the stream turns east for nearly a mile before exiting its valley and reaching its confluence with West Branch Fishing Creek. Shingle Mill Run joins West Branch Fishing Creek upstream of its mouth. Shingle Mill Run has one named tributary, which is known as
16411465
Lick Run (West Branch Susquehanna River tributary)


occupies 8.8% of the watershed's area. The elevation of the headwaters of Lick Run is higher than the elevation of the stream's mouth. The mouth's elevation is above sea level. Although there is little stream flow at the headwaters of Lick Run, there is some slightly further downstream. There are numerous pools in this area of the stream as well. Downstream of the tributary Doctors Fork, there are riffles and pools in it. The summers in the Lick Run watershed are warm, but the winters are long
2163289
Valley View (Romney, West Virginia)


corporate limits of Romney on the east and south and the Yellow Banks on the west. As well as Valley View's tract, the Mayhew family owns agricultural land rich in alluvial soils along the South Branch Potomac River west of the house. The South Branch Valley Railroad bisects this farmland, crossing the South Branch Potomac River via a wooden trestle. Valley View Island, an island in the South Branch Potomac River just north of the mouth of Sulphur Spring Run, is approximately southwest of the Valley View house. Both the house
19910822
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
White Deer Hole Creek


here along the river and cross the creek just before its mouth; however, this track is not in service as of 2009. Pennsylvania Route 44 runs east-west roughly parallel to the creek between Elimsport and Allenwood. Township roads run along the eastern two-thirds of the creek, and smaller, more primitive roads follow it to its source. From the mouth of White Deer Hole Creek it is along the West Branch Susquehanna River to its confluence with the Susquehanna River at Northumberland. The elevation at the source is ,
10682717
Dry Run (West Branch Susquehanna River tributary)


Dry Run has an area of . The mouth of the stream is in the United States Geological Survey quadrangle of Allenwood. However, its source is in the quadrangle of Milton. The mouth of the stream is located within of Watsontown. A Conrail railroad crosses Dry Run at one point. The area of the stream's watershed at this point is . According to the Warrior Run Pathways Partnership, Dry Run could benefit from improved stream and watershed management practices, including the installation of riparian buffers, installing fencing, management of waste
16553549
Turkey Run (West Branch Susquehanna River tributary)


near the mouth of Turkey Run is above sea level. The elevation of the stream's source is above sea level. Turkey Run was described as a "small stream" in an 1892 book of Lycoming County history. The stream is in a region known as the Black Hole Valley, along with Black Hole Creek. The watershed of Turkey Run has an area of . The stream is entirely within the United States Geological Survey quadrangle of Muncy. Its mouth is located within of Seagers. The designated use for Turkey Run is
16832366
Bean Run


south-southwest for several tenths of a mile as its valley deepens before receiving an unnamed tributary from the right. It then turns southeast for several tenths of a mile as its valley broadens. The stream then reaches its confluence with Bowman Creek. Bean Run joins Bowman Creek upstream of its mouth. Bean Run has no named tributaries, but it does have one unnamed tributary. This tributary is known as the west branch of Bean Run. Bean Run is not designated as an impaired waterbody. The elevation near the mouth of
2518801
Swanks Run


for several tenths of a mile, entering a small and narrow valley. It then receives an unnamed tributary from the left and turns southeast. Its valley becomes deeper as it flows downstream. After several tenths of a mile, the stream reaches its confluence with West Branch Fishing Creek. Swanks Run joins West Branch Fishing Creek upstream of its mouth. Swanks Run has no named tributaries. However, it does have one unnamed tributary, which is slightly less than half a mile long and flows in a north-to-south
16923751
Hemlock Run


It then turns southeast for a few tenths of a mile and receives an unnamed tributary from the left before turning south-southwest and then south-southeast. The stream enters a deep valley and receives another unnamed tributary from the right. Over the next several tenths of a mile, it gradually turns south and reaches its confluence with West Branch Fishing Creek. Hemlock Run joins West Branch Fishing Creek upstream of its mouth. Hemlock Run has no named tributaries. However, it does have three unnamed tributaries. The first tributary is
17137622
Hog Run


The stream then turns south-southwest for nearly a mile and the valley continues to deepen. It then turns south and then southwest. After a short distance, it reaches its confluence with Elk Run. Hog Run joins Elk Run upstream of its mouth. A total of of Hog Run is considered to be impaired. This is approximately 4.97 percent of all the impaired streams in the watersheds of East Branch Fishing Creek and West Branch Fishing Creek. The cause of the impairment is atmospheric deposition and metals. Hog Run does not
17936417
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
Cabin Run, Columbia County, Pennsylvania


to Cabin Run Road for several tenths of a mile. Upon leaving the valley, the stream crosses Fowlersville Road and turns southeast for a short distance before turning south again. After another few tenths of a mile, it reaches its confluence with West Branch Briar Creek. Cabin Run reaches its confluence with West Branch Briar Creek upstream of its mouth. The discharge of Cabin Run ranges from 0.17 to 15.7 cubic feet per second. The median discharge is 0.53 cubic feet per second. The water temperature of the stream ranges from to
15059680
Wolf Run (Muncy Creek tributary)


to parallel the West Branch Susquehanna River. Near the borough of Muncy, it reaches its confluence with Muncy Creek, very near to Muncy Creek's confluence with the West Branch Susquehanna River. Wolf Run joins Muncy Creek upstream of its mouth. Wolf Run experiences siltation and also experiences stream bank erosion. The annual load of sediment flowing through Wolf Run is . A load of of sediment per year comes from croplands, comes from stream banks, comes from forests, and comes from hay or pastures. per year comes from what
8410534
Birch Island Run


Island Run empties into the West Branch Susquehanna River at the border between Clinton County and Centre County, near a Conrail railroad. Named tributaries of Birch Island Run include Amos Branch and Little Birch Island Run. There are also a number of unnamed tributaries to the stream. The daily load of manganese in Birch Island Run is at the site BIR01, which is located at the confluence of Little Birch Island Run with Birch Island Run and at the site BIR02, which is located near the stream's mouth. The load of acidity
5089980
West Branch Fishing Creek


is long. The vast majority of the watershed is forested, with the only urban areas being the communities of Central and Elk Grove. There are a small number of residential areas and seasonal cabins in the watershed. The watershed of West Branch Fishing Creek contains a number of sub-watersheds. The largest of these is the watershed of Elk Run, which has an area of 7.49 square miles and joins the creek from its mouth. The second-largest sub-watershed is that of Painter Run. It has an area
1707619
Shingle Run (West Branch Run tributary)


Survey quadrangle of Lairdsville. Its mouth is in the southern part of Pine Township, Columbia County and is near the community of Pine Summit. Shingle Run was entered into the Geographic Names Information System on August 2, 1979. Its identifier in the Geographic Names Information System is 1187539. In the 19th century, the mouth of the stream was in a school district known as District No. 1. A proposal was once made to replace a bridge crossing Shingle Run and to place cement concrete paving in its streambed, among other
5564598
Warrior Run (West Branch Susquehanna River tributary)


of European habitation in the area. A historic Native American trail once ran from Northumberland to Muncy, passing by the mouth of Warrior Run and the Muncy Hills on the way. By the late 1800s, a public road occupied the course of this path. John Shikellamy, the oldest son of the Oneida chief Shikellamy, owned a hunting lodge at the mouth of Warrior Run. The lodge was known as the Warrior's Camp. Shikellamy himself lived in an area between Warrior Run and Chillisquaque Creek in around 1737. In May
7680077
Trout Run (East Branch Fishing Creek tributary)


plateau in Davidson Township. It flows west-northwest for a short distance before turning southwest and entering a valley, which it flows through for some distance. At the end of the valley, the stream turns southwest and then south. After a short distance, it reaches its confluence with East Branch Fishing Creek. Trout Run joins East Branch Fishing Creek upstream of its mouth. Trout Run has no named tributaries. It does, however, have at least one small unnamed tributary. The average discharge of Trout Run is 930
17356697
Eagle River (Michigan)


The Eagle River is a stream on the Keweenaw Peninsula of the U.S. state of Michigan. The river flows into Lake Superior in the community of Eagle River. Most of the river lies within Houghton Township. The main branch of the river is formed at the confluence of its East Branch and its West Branch at the community of Phoenix, about two miles southeast of its mouth, and parallels M-26 from Phoenix into Eagle River. The east and west branches each run along the south side of the Cliff Range to meet in Phoenix
12834123
Oxhorn Run


of the West Branch Fishing Creek and East Branch Fishing Creek watersheds. The entirety of Oxhorn Run does not attain the stream standards of the Pennsylvania Department of Environmental Protection. The stream is the only non-attaining stream in the watershed of Painter Run. The elevation near the mouth of Oxhorn Run is above sea level. The elevation of the stream's source is between above sea level. A glacial or resedimented till known as the Wisconsinan Till occurs in numerous places throughout the watershed of Oxhorn Run. In the stream's lower
17937372
Aro Valley


Much of Wellington consists of the remnants of an old peneplain, a flat expanse that rose from the sea about 20 million years ago. This land was heavily dissected by watercourses from that time and today the tops of the hills around Wellington indicate the general height of that eroded peneplain. During this time massive faults appeared that are still active today. 1 km to the west of Aro Valley is the Wellington Fault running north-east along the foot of the Tinakori Hills and beyond. A series of splinter faults branch off from
14820846
Duboistown, Pennsylvania


and moved west to Clearfield County. He became quite wealthy and the city of DuBois was named in his honor. The town built by the DuBois brothers and established as a borough in 1878 is by no means the beginning of the history of Duboistown. It is situated at the mouth of Mosquito Run on the banks of the West Branch Susquehanna River. A tribe of Susquehannock Indians had what appears to have been a fairly major settlement at the mouth of the creek. The early European settlers found the remains of an Indian village
8712012
Long Run (Elk Run tributary)


atmospheric deposition and metals. A total of of the stream and its unnamed tributaries have this impairment. This is approximately 10.5 percent of all the impaired streams in the watersheds of West Branch Fishing Creek and East Branch Fishing Creek. Long Run does not attain the stream standards of the Pennsylvania Department of Environmental Protection. None of its four unnamed tributaries attain the standards either. The elevation near the mouth of Long Run is above sea level. The elevation of the stream's source is between above sea level. Most of the valley
17751374
Buffalo Creek (West Branch Susquehanna River tributary)


Rapid Run joins Buffalo Creek upstream of its mouth and its watershed has an area of , while North Branch Buffalo Creek joins Buffalo Creek upstream of its mouth and its watershed has an area of . The pH of the waters of Buffalo Creek at three sites ranges from 5.0 to 6.7. Out of six times that the pH of the waters of the creek was measured in the springs and summers of 2010 and 2012, the lowest pH, 5.0, occurred at the location BC-6 on July 27, 2012. The highest pH,
6459885
Portishead Railway


The Portishead Railway is a branch line railway running from Portishead in Somerset to the main line immediately west of Bristol, England. It was constructed by the "Bristol & Portishead Pier and Railway Company", but it was always operated by its main line neighbour, and was more usually thought of as "the Portishead branch" or "the Portishead railway". It opened as a broad gauge () line to connect new docks at Portbury, at the west side of the mouth of the River Avon, with the railway
6153451
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
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
Shepman Run


. The elevation of the stream's source is above sea level. The stream flows through a valley known as Tommy Hollow. A bridge known as the Eichenlaub bridge crosses Shepman Run in Moreland Township, off Tom Hill Hollow Road (on the road's west side). The bridge has a length of . The watershed of Shepman Run has an area of . The stream is entirely within the United States Geological Survey quadrangle of Hughesville. Its mouth is located near Clarketown. Shepman Run is in the Lower West Branch Susquehanna sub
18760434
Warrior Run (West Branch Susquehanna River tributary)


1769, a lot of 609 acres, including the present-day community of Watsontown, was surveyed at the mouth of Warrior Run. Captain Daniel Piper came to own this land. European Settlers arrived at the stream, four miles (seven kilometers) upstream of the mouth, in 1772, making them the first European settlers in that area. These settlers included Jacob Freeland, John Vincent, Peter Vincent, and Cornelius Vincent. Fort Freeland was built on the site in 1775 to protect the settlers from the Indians. It
7680078
Laurel Fork (North Fork South Branch Potomac River tributary)


National Forest, intersecting the tributary streams of (from south to north) Bearwallow Run, Lost Run, Knotmaul Run, Christian Run, Slabcamp Run, Locust Spring Run, Buck Run, and Cold Spring Run. Approximately northeast of Newman Run and Secondary Route 642, Laurel Fork enters Pendleton County, West Virginia. Upon entering the state of West Virginia, Laurel Fork enters the Monongahela National Forest and takes an eastwardly turn. The stream flows approximately east, collecting the tributary waters of Sams Run, before reaching its mouth.
13533184
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
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
Overpeck Creek


the English Neighborhood. The creek lay along the main land route west of the Hudson and provided a consistently difficult barrier for transportation in the area until the construction of modern roads and bridges in the 19th century. Development of the region was facilitated by the New Jersey Midland Railway, the West Shore Railroad, and the Erie Railroad's Northern Branch, latter of which partially runs parallel to the creek. Restoration of rail service is the object of the Northern Branch Corridor Project. Although the creek is theoretically navigable, the mouth of
3041118
Larrys Creek


First Fork has its source in Cummings Township and flows south-southeast into Mifflin Township. from its mouth Larrys Creek receives Canoe Run. Both these tributaries enter on the right bank. Larrys Creek then enters Piatt Township, flowing east around a ridge and through the village of Larryville where it receives Seeley Run on the left bank, from the mouth. It next flows back southwest, then south to the hamlet of Larrys Creek and finally into the West Branch Susquehanna River, east of the borough of Jersey Shore, at an
20558227
Warrior Run (West Branch Susquehanna River tributary)


was a stockaded log house with half an acre of land inside the walls. The fort provided visibility for approximately a mile upstream and downstream. It was destroyed on July 28, 1779 by 100 British troops under the command of John McDonald and 200 Indians commanded by Hiokoto, a Seneca chief. Hawkins Boone, a relative of Daniel Boone, built Fort Boone at the mouth of the stream. Fort Meninger was also located there. John Watson had the idea to build a community at the mouth of Warrior Run, which he
7680079
West Branch Rausch Creek


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. The pH of the creek has been measured to range from 6.1 to 6.5, with an average of 6.3. The alkalinity concentration ranged from , with an average of . The iron concentration in West Branch Rausch Creek near its mouth ranges from , with an average of . The concentration of manganese ranges from , with an average of . The aluminum concentration ranges between less
160943
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
West Branch Lackawanna River


Lake Creek, its only named tributary, from the right after several tenths of a mile. A few tenths of a mile further downstream, it enters Stillwater Lake and reaches its confluence with the Lackawanna River. The West Branch Lackawanna River joins the Lackawanna River upriver of its mouth. The West Branch Lackawanna River has one named tributary, which is known as Fiddle Lake Creek. Fiddle Lake Creek joins the West Branch Lackawanna River upriver of its mouth. Its watershed has an area of . Other unnamed tributaries include "Unnamed trib
2427511
Tresfjorden


Tresfjorden () is a fjord in Vestnes Municipality in Møre og Romsdal county, Norway. The long fjord branches off of the main Romsdal Fjord, and it is one of the two main fjords that cut into the municipality. The village of Vestnes sits at the mouth of the fjord (on the west side) and the village of Vikebukt sits at the mouth of the fjord (on the east side). The village of Tresfjord is located at the southern end of the fjord. European route E39 runs along the northwest
5277279
Slip Run (West Branch Fishing Creek tributary)


and the Wisconsinan Terminus crosses its watershed. There are a number of arcuate till ridges in the vicinity of Slip Run. Conglomerate erratics also occur to the west of the stream's valley. The surficial geology at the mouth of Slip Run consists of alluvium and Boulder Colluvium, which contains numerous boulders made of sandstone, conglomerate, and quartz. Further upstream, the surficial geology features bedrock consisting of sandstone and shale, with Boulder Colluvium occurring on a nearby upland. A large patch of Wisconsinan Till Moraine occurs along the upper reaches
8573684
Osa Fjord


The Osa Fjord () is a branch of the Eid Fjord and the Hardanger Fjord fully located within the municipality of Ulvik in Norway. The fjord is long, with a maximum depth of at its mouth, and it runs northeast from its mouth between Bruravik and Bagnsnes to the head of the fjord at the small village of Osa. On the west side, the Ulvik Fjord extends to the north to the municipal center of Ulvik. The outermost part of the Osa Fjord is also known as the Bagns Fjord (),
16243234
East Branch Fishing Creek


pH occurs on Shanty Run. At two sites on East Branch Fishing Creek itself, the creek's pH is 5.34 (at its confluence with Lead Run) and 5.63 (at its mouth). The average amount of aluminum in the streams in the watershed ranges from 0.024 milligrams per liter to 0.366 milligrams per liter. The highest concentration occurs on Ore Run and the lowest concentration occurs on the mouth of East Branch Fishing Creek. One stream in the watershed, Big Run, has a pH range of less than 3 to
15548184
Lick Run (West Branch Susquehanna River tributary)


the pH upstream of Flegals Run ranges from 5.0 to 5.6. Near the mouth of Lick Run, the pH is between 5.4 and 5.9. The lowest pH in the entire watershed is at a site on Flegals Run, where it ranges from 4.0 to 4.2. In Fall 2004, the pH of Lick Run was observed to be 4.1. In the upper reaches of Lick Run, its pH is lowest in the spring and highest in the summer. The watershed of Lick Run is located in the Pittsburgh Low Plateaus Section of
2163287
South Branch Towanda Creek


passes through New Albany, where it receives the tributaries Beaver Run and Ladds Creek. Continuing roughly north, the creek passes by Hatch Mountain and enters Monroe Township. In Monroe Township, it receives the tributaries Fenner Run, Saterlee Run, and Kent Run. It passes Nichols Point, Marcy Point, and Kellogg Mountain. A few miles downstream, the creek reaches its confluence with Towanda Creek near the community of Monroeton. South Branch Towanda Creek joins Towanda Creek upstream of its mouth. The elevation near the mouth of South Branch
6039362
Buck Run (West Branch Brandywine Creek tributary)


vicinity of the stream. The average annual rate of precipitation in the watershed of Buck Run ranges from . The watershed of Buck Run has an area of . There are of streams in the watershed of Buck Run. The watershed occupies portions of 11 municipalities. The mouth of the stream is in the United States Geological Survey quadrangle of Coatesville. However, its source is in the United States Geological Survey quadrangle of Parkesburg. In the early 1900s, the predominant land use in the watershed of Buck Run was agriculture. Buck Run
8229624
Petite Rivière de Jacmel


The Petite Rivière de Jacmel is a watercourse running in Haiti through the Sud-Est department and the arrondissement of Jacmel. The Petite Rivière de Jacmel takes its source in the foothills of the mountain range called "Chaîne de la Selle", and set in Hispaniola's Tiburon Peninsula. Over approximately 10 kilometers long, the river then runs Eastwards, to meet South with the Caribbean Sea at the level of its mouth in the bay of the port-city of Jacmel. Along its path in the mountain, the river turns
2380076
Skipsfjorden, Torsken


Skipsfjorden is a branch of the Torskenfjorden in Torsken Municipality on the western coast of the large island of Senja in Troms county, Norway. The mouth of the fjord lies between Selneset on the west and Galgeneset on the east. The fjord runs about in a roughly eastwards direction to Skipsfjordbotn. The village of Torsken is located at Selneset at the mouth of the fjord. The mountain Skipstinden lies on the north side of the fjord and it climbs steeply to above sea level although its highest peak ( above sea level) lies a
21289111
Turtle Creek (West Branch Susquehanna River tributary)


Run, and the West Branch Susquehanna River. Turtle Creek was entered into the Geographic Names Information System on August 2, 1979. Its identifier in the Geographic Names Information System is 1189973. The creek received its name some time before 1769. Samuel Maclay carried out a survey in the vicinity of Turtle Creek in early March 1769. Several more surveys were done near the creek in that year. John Wilson had settled near the mouth of the creek by the fall of that year. In 1770, William Speddy settled approximately of
10059595
Bloody Run (West Branch Fishing Creek tributary)


elevation near the mouth of Bloody Run is above sea level. The elevation of the stream's source is between above sea level. There are riffles on Bloody run. A glacial till known as the Wisconsinan Bouldery Till can be found in the lower reaches of Bloody Run and in its valley. The stream's upper reaches are in the vicinity of a glacial till known as the Wisconsinan Till. In the stream's middle reaches and on the edges of its valley, there is bedrock consisting of shale and sandstone. The watershed
16172428
Painter Run


aquatic life. It attains the Pennsylvania Department of Environmental Protection's standards. However, its tributary Oxhorn Run does not meet the standards and is considered by the Pennsylvania Department of Environmental Protection to be impaired. The elevation near the mouth of Painter Run is above sea level. The elevation of the stream's source is between above sea level. Painter Run is in a narrow valley between two mountains. There is also a ridge to the north of the stream. Another ridge lies between the stream and West Branch Fishing Creek.
16233022
Nordvestfjord


by Charcot Land, and to the southwest by Hinksland, Th. Sørensen Land and Renland. The Nordvestfjord winds its way roughly in a NW/SE direction. Its largest branch is the Flyver Fjord, which runs in a roughly west/east direction and joins the southwestern shore about midway through the fjord. The fjord is fed by several glaciers. The Daugaard-Jensen Glacier is at the fjord's head flowing from the southwest and producing masses of icebergs. The mouth is located close to the mouth of Ofjord, between
19104887
History of Lycoming County, Pennsylvania


. He became quite wealthy and the city of DuBois was named in his honor. The town built by the DuBois brothers is by no means the beginning of the history of Duboistown. It is situated at the mouth of Mosquito Run on the banks of the West Branch Susquehanna River. A tribe of Susquehannock Indians had what appears to have been a fairly major settlement at the mouth of the creek. The early European settlers found the remains of an Indian village there. Arhaeologic evidence of earthenware, soapstone ware, pestles, hatchets
5049668