Shamokin Creek [SEP] mouth of the watercourse
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Shamokin Creek


Run, Bennys Run, Locust Creek, and others. Little Shamokin Creek joins Shamokin Creek upstream of its mouth and drains an area of . Carbon Run joins Shamokin Creek upstream of its mouth and drains an area of . Coal Run joins Shamokin Creek upstream of its mouth and drains an area of . Bennys Run joins Shamokin Creek upstream of its mouth and drains an area of . Locust Creek joins Shamokin Creek upstream of its mouth and drains an area of . The entire length of Shamokin Creek is designated as impaired due to high
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Shamokin Creek


Shamokin Creek was dry near the confluence of North Branch Shamokin Creek, but near Quaker Run, its discharge was . In Shamokin, the discharge was and slightly further downstream, it was . Near its mouth, the creek's discharge was . The creek's discharge was considerably higher in March 2000, being near North Branch Shamokin Creek, near Quaker Run, at Shamokin (depending on the site), below Shamokin (again, depending on the site), and at Sunbury. The concentrations of manganese and iron in the
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Shamokin Creek


sluices formed by cobbles. There is a weir with a height of on the creek downstream of Shamokin. In the early 1900s, the average rate of precipitation in the watershed of Shamokin Creek was per year. The water temperature of the creek at Shamokin was measured to be in August 1999. The watershed of Shamokin Creek has an area of . The mouth of the creek is in the United States Geological Survey quadrangle of Sunbury. However, its source is in the quadrangle of Mount Carmel. The creek also passes through the
19053544
Little Shamokin Creek


confluence with Shamokin Creek. Little Shamokin Creek is located in the ridge-and-valley Appalachian Mountains. The headwaters of the creek are located higher than the mouth. The highest portions of the watershed are in the southeastern area, where Little Mountain is located. 90% of the rocks in the upper portion of the Little Shamokin Creek watershed are interbedded sedimentary rocks. The other 10% are sandstone. The main soil series in the Little Shamokin Creek watershed is the Berks-Weikert-Bedington series, which is a shaly
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North Branch Shamokin Creek


of . The mouth of the stream is in the United States Geological Survey quadrangle of Mount Carmel. However, its source is in the quadrangle of Ashland. Communities in the creek's watershed include the borough of Marion Heights and the census-designated place of Strong. In 2009, Northeastern ITS requested a permit to discharge stormwater into North Branch Shamokin Creek for construction purposes. When the Operation Scarlift report for Shamokin Creek was written, there were no raw sewage discharges into North Branch Shamokin Creek. North Branch Shamokin Creek was entered
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North Branch Shamokin Creek


Ridge. It then crosses Pennsylvania Route 54 and gradually turns west-southwest. Several tenths of a mile further downstream, the creek reaches its confluence with Shamokin Creek. North Branch Shamokin Creek joins Shamokin Creek upstream of its mouth. The entire length of North Branch Shamokin Creek is designated as an impaired waterbody and has poor water quality. The cause of the impairment is metals and the source is abandoned mine drainage. In addition to experiencing acidity and metal loading from acid mine drainage sources, the creek is also impacted by flow
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Shamokin Creek


elevation of the creek's source is between above sea level. Between Mount Carmel and Shamokin, the gradient of the creek is . Between Shamokin and the creek's mouth, this decreases to . The watershed of Shamokin Creek is in the Appalachian Mountains section of the Ridge and Valley physiographic province. The lower reaches of the watershed are in the Northern Shale Valleys and Slopes Ecoregion, while the upper reaches are in the Anthracite Coal Ecoregion. In the early 1900s, vast culm deposits along the creek's banks caused it to lack
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Shamokin Creek


south and receiving Little Shamokin Creek, its last named tributary, from the left. Several tenths of a mile further downstream, it flows west for several tenths of a mile, flowing along the border between Sunbury and Upper Augusta Township. The creek then turns southwest for several tenths of a mile and continues flowing along the border until it reaches its confluence with the Susquehanna River. Shamokin Creek joins the Susquehanna River upriver of its mouth. Shamokin Creek has eleven named direct tributaries, including Little Shamokin Creek, Carbon Run, Coal
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Plum Creek (Little Shamokin Creek tributary)


Creek joins Little Shamokin Creek upstream of its mouth. A total of of Plum Creek plus all of its unnamed tributaries are designated as impaired. The impairment comes from siltation, organic enrichment, and low levels of dissolved oxygen and are due to grazing; however, the remaining of the main stem are not designated as impaired. The elevation near the mouth of Plum Creek is above sea level. The elevation of the creek's source is between above sea level. Plum Creek is a small, perennial stream. The watershed of
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Locust Creek (Shamokin Creek tributary)


A few tenths of a mile further downstream, it reaches its confluence with Shamokin Creek. Locust Creek joins Shamokin Creek upstream of its mouth. Locust Creek has no named tributaries, but it has one unnamed tributary. This tributary is known as UNT #18656 and of it is an impaired waterbody. Locust Creek has poor water quality. The entire length of Locust Creek is designated as an impaired waterbody. The cause of the impairment is metals and the source is abandoned mine drainage. The acid mine drainage impacts to the creek
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Lick Creek (Shamokin Creek tributary)


right. The creek then turns north for a few tenths of a mile, entering a much broader valley and receiving an unnamed tributary from the left. The creek then turns east for more than a mile and receives two more unnamed tributaries from the left before turning north-northeast and then east. It then turns northeast for a short distance and crosses Pennsylvania Route 61 before reaching its confluence with Shamokin Creek. Lick Creek joins Shamokin Creek upstream of its mouth. Lick Creek has no named tributaries. However, it does have
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Furnace Run (Shamokin Creek tributary)


. Furnace Run begins in a small lake in Coal Township, in the census-designated place of Fairview-Ferndale. It flows east-northeast for its entire length, almost immediately entering the census-designated place of Edgewood. Several tenths of a mile further downstream, the stream enters Shamokin and reaches its confluence with Shamokin Creek. Furnace Run joins Shamokin Creek upstream of its mouth. Furnace Run is designated as an impaired waterbody. The cause of the impairment is sedimentation and siltation. The source of the impairment is urban
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North Branch Shamokin Creek


was measured. The sulfate concentration ranged from and the chloride concentration ranged from . The elevation near the mouth of North Branch Shamokin Creek is above sea level. The elevation of the creek's source is between above sea level. In one reach, North Branch Shamokin Creek passes between two ridges known as Red Ridge and Green Ridge, or Jamies Ridge. There are occurrences of coal in the creek's watershed. One coal bed, where the creek flows between Red Ridge and Green Ridge, has a thickness of up to .
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Shamokin Creek


to Shamokin Creek as the worst stream in the Coal Region due to the mine water, culm deposits, and other problems. During this time period, the culm deposits were so extensive that it was one of the few creeks where it was commercially viable to recover coal from its streambed. The creek was black throughout its entire length and typically sluggish in its upper reaches, though it had fast reaches. However, it was clear at its headwaters. The elevation near the mouth of Shamokin Creek is above sea level. The
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Coal Run (Shamokin Creek tributary)


stream crosses Pennsylvania Route 61 and passes near the census-designated place of Ranshaw. The stream then flows in a west-northwesterly direction for several tenths of a mile, passing through the census-designated place of Marshalton before entering Shamokin. The stream then flows west for a few tenths of a mile until it reaches its confluence with Shamokin Creek. Coal Run joins Shamokin Creek upstream of its mouth. The entire length of Coal Run is designated as an impaired waterbody. The cause of the impairment is metals and the source
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Trout Run (Shamokin Creek tributary)


aquatic life. Trout Run begins in the Number Four Reservoir in Coal Township. It heads west-southwest for several tenths of a mile, flowing through a broad, deep valley between two ridges. The stream then turns west-northwest for a short distance before turning southwest. Several tenths of a mile further downstream, it reaches its confluence with Shamokin Creek. Trout Run joins Shamokin Creek upstream of its mouth. Trout Run is not designated as an impaired waterbody. The stream has a high level of water quality and no
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Quaker Run (Shamokin Creek tributary)


for a short distance and crosses Pennsylvania Route 61 before turning west-southwest for more than a mile and entering Mount Carmel Township and a valley. The stream then turns in a westerly direction for a few miles, entering Coal Township and then the census-designated place of Ranshaw. In Ranshaw, it crosses Pennsylvania Route 901 and reaches its confluence with Shamokin Creek. Quaker Run joins Shamokin Creek upstream of its mouth. Quaker Run has no named tributaries, but it does have one unnamed tributary. This tributary is designated as
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Shikellamy


maintain an outpost at Shamokin and served as an emissary between the Moravians and Madame Montour's village of Otstonwakin at the mouth of Loyalsock Creek and French Margaret's village at the mouth of Lycoming Creek. Shikellamy permitted the Moravians to stay at Shamokin because he believed that they had the Indians' best interest at heart. He knew that, unlike other white men, the Moravians had no interest in the Indians' furs and did not want to take their land, nor did the missionaries give Shikellamy's people any alcohol. Shikellamy
5398230
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
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Trout Run (Shamokin Creek tributary)


known as Brush Valley. A dam known as the Trout Run Dam Number 4 is located on Trout Run. As of 1980, it is in good condition. The watershed of Trout Run has an area of . The stream is entirely within the United States Geological Survey quadrangle of Shamokin. The watershed of Trout Run is in the central part of the Shamokin Creek drainage basin. It is roughly rectangular and longer than it is wide. The community of Uniontown is near the mouth of the stream. Trout Run mainly flows through
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Shamokin Creek


levels of metals from abandoned mine drainage. In addition to abandoned mine drainage, the creek is impacted by sewage, disruption of the area's natural hydrology, and probably nutrient pollution, sediment, and low levels of dissolved oxygen. Non-polluted streams in the creek's lower reaches dilute the pollution by more than doubling Shamokin Creek's discharge. However, impairments remain as far downstream as the creek's mouth in Sunbury. There are dozens of abandoned mine drainage discharges in the watershed's upper reaches. Some discharges lead into
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Bennys Run


above sea level. Bennys Run is a small and shallow stream situated in Irish Valley. It flows in a generally easterly direction. The watershed of Bennys Run has an area of . The mouth of the stream is in the United States Geological Survey quadrangle of Shamokin. However, its source is in the quadrangle of Trevorton. The watershed borders several other watersheds, including the Little Shamokin Creek watershed, the Lick Run watershed, and the lower Shamokin Creek watershed. A road known as Irish Valley Road runs alongside Bennys Run for
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Bennys Run


. Bennys Run begins in a pond in Shamokin Township. It flows northeast for a few tenths of a mile before turning east-northeast and flowing through a valley. Over the next few miles, the stream receives four unnamed tributaries from the left and one unnamed tributary from the right. It then turns north-northeast for a few tenths of a mile before crossing Pennsylvania Route 61 and reaching its confluence with Shamokin Creek. Bennys Run joins Shamokin Creek upstream of its mouth. Bennys Run is not designated as an impaired waterbody
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Carbon Run


Ferndale. The stream flows alongside Pennsylvania Route 125 for several tenths of a mile before turning north and entering Shamokin. Several tenths of a mile further downstream, it turns northwest and reaches its confluence with Shamokin Creek. Carbon Run joins Shamokin Creek upstream of its mouth. The entire length of Carbon Run is designated as an impaired waterbody. The cause of the impairment is metals other than mercury and the source of the impairment is abandoned mine drainage. Its two unnamed tributaries are also impaired. The stream is impacted by acid mine
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Plum Creek (Little Shamokin Creek tributary)


Plum Creek has an area of . The mouth of the creek is in the United States Geological Survey quadrangle of Sunbury. However, its source is in the quadrangle of Trevorton. The headwaters of Plum Creek are south of Millers Crossroads Church. The creek's mouth is near Pennsylvania Route 890. Plum Creek has been used as a water supply for Sunbury. There are some reservoirs in the creek's watershed. Plum Creek was entered into the Geographic Names Information System on August 2, 1979. Its identifier in the Geographic Names
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Lick Creek (Shamokin Creek tributary)


a number of unnamed tributaries. At least one of these is intermittent. The elevation near the mouth of Lick Creek is above sea level. The elevation of the creek's source is between above sea level. Lick Creek is not impacted by mining. The creek has a relatively high level of water quality. All streams in the creek's watershed meet at least one designated use and none are impaired. The watershed of Lick Creek has an area of . The mouth of the creek is in the United States Geological Survey quadrangle
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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
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Winfield Creek


mouth of Winfield Creek is above sea level. The elevation of the creek's source is between above sea level. Winfield Creek joins the West Branch Susquehanna River on its right bank. Winfield Creek is a very small stream and flows through a limestone valley. The creek flows through a narrow valley, which is bordered by Shamokin Mountain on the north and highlands on the south. The watershed of Winfield Creek has an area of . The mouth of the creek is in the United States Geological Survey quadrangle of Northumberland. However,
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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
Anderson Creek (Pennsylvania)


their journey northwards towards freedom are collectively known as the Underground Railroad. In western Pennsylvania, routes began at the Maryland–Pennsylvania border and traveled through Bedford, Pennsylvania, where the route split and converged at the Great Shamokin Path at the mouth of Anderson Creek. From there, the route led to The Big Spring near Luthersburg, Pennsylvania, and thence on Meade's Path to the Venango Path, Lake Erie and onward to Canada. Quaker settlers living along the Great Shamokin Path in Clearfield County did what they could to assist
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Coal Run (Shamokin Creek tributary)


is in the Coal Region. In the early 1900s, fine culm was carried into Coal Run via waste water streams from collieries. However, there were no large culm deposits on the stream below the Hickory Ridge Colliery. Trash and sewage entered the stream at Shamokin. The watershed of Coal Run has an area of . The mouth of the stream is in the United States Geological Survey quadrangle of Shamokin. However, its source is in the quadrangle of Mount Carmel. The designated uses of Coal Run are coal water and migratory
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Millers Run


Ralpho Township. It enters a valley and flows west-southwest for several tenths of a mile before turning west. After a few tenths of a mile, it turns west-southwest. Several tenths of a mile further downstream, the stream turns northwest for more than a mile before turning west and flowing alongside Gilgers Ridge. After a few tenths of a mile, it turns south and then northwest before reaching its confluence with Shamokin Creek. Millers Run joins Shamokin Creek upstream of its mouth. Millers Run is an unimpaired waterbody
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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
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Shamokin Creek


main stem of Shamokin Creek for much of the creek's length. Shamokin Creek was entered into the Geographic Names Information System on August 2, 1979. Its identifier in the Geographic Names Information System is 1193324. The creek is also known as Great Shamokin Creek and Middle Branch Shamokin Creek. The former name appears in Thomas Francis Gordon's "A Gazetteer of the State of Pennsylvania", which was published in 1833. The latter name appears in a 1982 county highway map made by the Pennsylvania Department of Transportation. The creek
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Shamokin Creek


is named after a Delaware word for "Eel Creek". Many of the early settlers in the valley of Shamokin Creek were Scotch-Irish. The first mill in the current boundaries of Northumberland County was built on or near the creek in 1774. A road up the creek's valley was being laid out by 1775. The first coal in Shamokin was discovered in Shamokin Creek at what is now Spurzheim Street and Clay Street. Before the War of 1812, Abraham Cherry constructed a sawmill on Shamokin Creek. Some coal mining
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Shamokin Creek


Shamokin Creek (also known as Great Shamokin Creek or Middle Branch Shamokin Creek) is a tributary of the Susquehanna River in Northumberland County, Pennsylvania, in the United States. It is approximately long and flows through Mount Carmel, Mount Carmel Township, Coal Township, Shamokin, Ralpho Township, Shamokin Township, Snydertown, Upper Augusta Township, and Sunbury. The watershed of the creek has an area of . It experiences significant impacts by abandoned mine drainage and many abandoned mine drainage discharges are in its watershed. Various other impairments also
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North Branch Shamokin Creek


The creek passes through an axis perpendicular to coal strata in the area. There are underground mine complexes throughout the watershed of North Branch Shamokin Creek. The Mid Valley Discharge is in the creek's watershed. Half of its flow is lost to the nearby Mahanoy Creek watershed. Some loss in the watershed of North Branch Shamokin Creek also reappears in the watershed of Quaker Run. North Branch Shamokin Creek is coated with a layer of iron precipitate. It has a permeable streambed. The watershed of North Branch Shamokin Creek has an area
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List of tributaries of Shamokin Creek


Shamokin Creek is a 32.4-mile (52.1 km) long creek flowing through Northumberland County, Pennsylvania, in the United States, into the Susquehanna River. It has 12 named tributaries, including 11 direct tributaries and one sub-tributary. The tributaries include seven runs and five creeks. The longest are Little Shamokin Creek, Carbon Run, North Branch Shamokin Creek, Coal Run, and Millers Run. Many of the upper tributaries of Shamokin Creek are in the Western Middle Anthracite Coalfield and nearly all of the streams in this part of
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Zerbe Run


Run has an area of . The mouth of the stream is in the United States Geological Survey quadrangle of Sunbury. However, its source is in the quadrangle of Shamokin. The stream also passes through the quadrangle of Trevorton. The mouth of the stream is located within of Hunter. Zerbe Run is one of major streams in the watershed of Mahanoy Creek. Its watershed occupies a total of 8.3% of the Mahanoy Creek drainage basin. Most of the abandoned mine land in the watershed occurs to the south of the stream.
11868601
List of tributaries of Shamokin Creek


the watershed are impacted by mining, except for Furnace Run. Various mine drainage sites occur in the watersheds of all other streams in the upper Shamokin Creek watershed. None of the tributaries in the lower reaches of the Shamokin Creek watershed are affected by mining. Four tributaries of Shamokin CreekLick Creek, Millers Run, Bennys Run, and Trout Runare not designated as impaired waterbodies by the United States Environmental Protection Agency. Another five tributariesNorth Branch Shamokin Creek, Locust Creek, Quaker Run, Coal Run, and Carbon Run are impaired by
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Shamokin Creek


Shamokin Creek Restoration Alliance received more than $500,000 in grants from the United States Environmental Protection Agency to repair abandoned mine drainage sources in the watershed. A flood control project was carried out on Shamokin Creek in Mount Carmel in 2013. The main stem of Shamokin Creek is designated as a Warmwater Fishery and a Migratory Fishery. However, all of the creek's tributariesincluding unnamed ones are designated as Coldwater Fisheries and Migratory Fisheries. The main stem of Shamokin Creek is not inhabited by any aquatic life upstream of the tributary Carbon Run.
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Shamokin Creek


the watershed of Mahanoy Creek, which has some mine drainage discharges that flow back into the Shamokin Creek watershed. The pH of Shamokin Creek as far downstream as Sunbury can be as low as 4.2. The pH in the creek's upper reaches is 6.1 to 6.6, depending on the site and the time of year, while in Shamokin, it can range from 6.3 to 6.5; below Shamokin, it can range from 5.9 to 6.3; and at Sunbury, it can range from 4.0 to 6.5. In August 1999,
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Shamokin Creek


bridge known as the Shamokin Creek Bridge carries Pennsylvania Route 61 over Shamokin Creek in Sunbury. It is a through truss bridge that was built in 1933 and repaired in 1981. The bridge is open to traffic and has a length of . It has little historical significance. Shamokin Creek was the subject of an Operation Scarlift report in 1972. The Shamokin Creek Restoration Alliance was founded in 1996 with the purpose of "[encouraging] partnerships and develop[ing] incentives and methods to facilitate funding for reclamation of abandoned mine lands (AML)
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Little Shamokin Creek


. It was constructed in 1856 by Samuel Lantz. The first public road in the valley of Little Shamokin Creek was built in 1787. Plum Creek is one named tributary of Little Shamokin Creek. There are no other named tributaries of the creek, although there are several unnamed ones. In some of the agricultural areas of the Little Shamokin Creek watershed, there is very little riparian buffer. Livestock also have easy access to the creek in some areas. There are beef and pork farms located near the creek. The farms contribute
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Shamokin Creek


in Shamokin Creek watershed." In 1999, the Northumberland County Conservation District received a $52,830 to assess Shamokin Creek. In the same year, the Shamokin Creek Restoration Alliance received a $5000 grant from the Eastern Pennsylvania Coalition for Abandoned Mine Restoration. Various grants for passive treatment systems in the watershed were also given in 1999. In 2002, the Northumberland County Planning Commission received a $75,000 Growing Greener grant to eliminate sources of impairment in the watershed of Shamokin Creek. In 2003, the Northumberland County Conservation District and the
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Plum Creek (Little Shamokin Creek tributary)


Plum Creek is a tributary of Little Shamokin Creek in Northumberland County, Pennsylvania, in the United States. It is approximately long and flows through Shamokin Township and Rockefeller Township. The watershed of the creek has an area of . It is a small, perennial stream and its valley was substantially colonized by the early 19th century. A number of bridges have been constructed over the creek. Plum Creek begins in a small pond in Shamokin Township. It flows northwest for several tenths of a mile before turning west. The creek then
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Lick Creek (Shamokin Creek tributary)


Lick Creek is a tributary of Shamokin Creek in Northumberland County, Pennsylvania, in the United States. It is approximately long and flows through Shamokin Township. The watershed of the creek has an area of . The creek is not designated as impaired and its watershed is designated as a Coldwater Fishery and a Migratory Fishery. It supports some aquatic life. Lick Creek begins in a valley on a ridge in Shamokin Township. It flows east-northeast for several tenths of a mile before turning north and receiving an unnamed tributary from the
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Shamokin Creek


was being done at the creek by 1825. A dam was constructed on the creek in Shamokin in 1826 and John C. Byrd opened a stone coal quarry on the creek in the same year. The only canal boat on Shamokin Creek was launched in the early 1830s. In the early 1900s, the most significant industries in the watershed of Shamokin Creek were coal mining, foundries, iron works, nail production, agriculture, silk mills, and woolen mills. The creek was also used as water power for several small mills and
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Quaker Run (Shamokin Creek tributary)


, there was a quarry near the stream. Mine complexes also extend under the stream. The channel of Quaker Run is flanked by walls in Ranshaw. These walls are in a state of disrepair. The watershed of Quaker Run has an area of . The mouth of the stream is in the United States Geological Survey quadrangle of Shamokin. However, its source is in the quadrangle of Mount Carmel. The Wildlife for Everyone Endowment Foundation has carried out a restoration project on Quaker Run in Coal Township. This project has restored of
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Shamokin Creek


lined with iron in some reaches. The creek has high concentrations of nickel. In and around Shamokin, the aluminum concentration of Shamokin Creek ranges from , depending on the site. This equates to a daily load of . In the creek's middle reaches, the concentration decreases from ( per day) at site SC5 to ( per day) at site SC7 to ( per day) at Sunbury. In August 1999 and March 2000, the sulfate concentration in the upper reaches of Shamokin Creek ranged from , depending on the site
19053537
Shamokin Creek


quadrangles of Danville, Shamokin, Riverside, and Trevorton. The creek's watershed mainly occupies southern Columbia County and central Northumberland County. There are 14 municipalities in the watershed of Shamokin Creek, including 13 in Northumberland County and one in Columbia County. There are of streams in the watershed of Shamokin Creek. Of these, (27 percent) are impaired by abandoned mine drainage. In Mount Carmel, the creek is used to carry stormwater. Historically, it carried waste such as untreated sewage from both the community of Mount Carmel
19053545
Locust Creek (Shamokin Creek tributary)


. The concentrations of recoverable manganese and iron were , while the recoverable aluminum concentration was . In March 2000, the concentration of dissolved oxygen in Locust Creek was , but no carbon dioxide was observed. The nitrogen concentration was , while the phosphorus concentration was . The chloride and sulfate concentrations were . The ammonia concentration was less than and the nitrate concentration was less than . The elevation near the mouth of Locust Creek is above sea level. The elevation of the stream's source is between above sea level. There is a thick
14784340
Roaring Creek (Pennsylvania)


Most of the watershed is in Columbia County and smaller areas are in Montour County and Northumberland County. Only a very small area in the its upper reaches is in Schuylkill County. The watershed is in the Lower North Branch Susquehanna drainage basin. The creek's mouth is in the United States Geological Survey quadrangle of Danville. However, its source is in the quadrangle of Shumans. The creek also passes through the quadrangle of Catawissa. Other quadrangles that the watershed is in include Shamokin, Ashland, and Mount Carmel. The creek
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Little Shamokin Creek


They are the Berks-Weikert-Bedington series, the Leck Kill-Meckesville-Calvin series and the Hazelton-Dekalb-Buchanan series. Little Shamokin Creek is the only stream in the Shamokin Creek watershed where fish can survive, as of 1999. Little Shamokin Creek starts in eastern Northumberland County, several miles north of Trevorton. From its starting point, the creek flows west through the Irish Valley and eventually exits the valley. Upon reaching the Augustaville Church, it turns northwards. The creek continues northwards until it reaches its
1215871
Little Shamokin Creek


Little Shamokin Creek is a tributary of Shamokin Creek and a sub-tributary of the Susquehanna River in Northumberland County, Pennsylvania, in the United States. The watershed of the creek has an area of 37 square miles, spread out over Upper Augusta Township, Lower Augusta Township, Rockefeller Township, and Shamokin Township. The creek's watershed contains four rock formations. These are the Hamilton Group, the Spechty Kopf formation, the Irish Valley formation, and the Buddy Run formation. The watershed also contains three main soil types.
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Shamokin Creek


However, the creek supports six species of fish further downstream. In 2001, there were 169 individual fish from eight species in Shamokin Creek at Shamokin. The most common species were white suckers (74 individuals), creek chubs (48 individuals), and spotfin shiners (31 individuals). Other species included pumpkinseeds, (7 individuals), green sunfish (5 individuals), yellow bullhead (2 individuals), stonerollers, and rainbow trout (1 individual each). In Shamokin Creek at Sunbury, there were 112
19053556
Shamokin Creek


Creek had large populations of pike, sunfish, suckers, and eels. Many areas in the upper reaches of Shamokin Creek support little or no macroinvertebrate life due to metals coating the streambed. In August 1999, more than 500 coliform colonies per 100 milliliters were observed in the creek near Shamokin, of which 97 were "E. coli". A total of of Shamokin Creek are navigable by canoe during snowmelt or within two days of hard rain. The scenery is described as "Poor to Fair" in Edward Gertler's book
19053558
List of tributaries of Shamokin Creek


metals due to abandoned mine drainage. Furnace Run is impaired by channelization and habitat alteration, while Little Shamokin Creek and its tributary Plum Creek are impaired by siltation, organic enrichment, and low levels of dissolved oxygen. Although the main stem of Shamokin Creek is designated as a Warmwater Fishery, all of its tributaries are designated as Coldwater Fisheries. Some tributaries, such as North Branch Shamokin Creek and Quaker Run, lack fish life. However, several fish species have been observed in Carbon Run and downstream tributaries such as Trout Run
15194531
Bowmanville Creek


Bowmanville Creek is a watercourse in Durham County, that flows from its headwaters in the Oak Ridges Moraine to its mouth on Lake Ontario, at Bowmanville, Ontario. It borders Oshawa Creek, and Soper Creek, to the west and east, which have their headwaters in the Oak Ridges Moraine. Between Bowmanville Creek and Oshawa Creek, there are five smaller creeks, Farewell Creek, Robinson Creek, Tooley Creek, Darlington Creek and Westside Creek. Bowmanville Creek has been dammed in several places. About one km north of Lake Ontario
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Shamokin Creek


along the border of the census-designated place of Marshalton. After several tenths of a mile, it turns south-southwest before turning north-northwest and entering Shamokin. Several tenths of a mile after entering Shamokin, the creek receives the tributary Coal Run from the right and turns west-southwest. A few tenths of a mile further downstream, it crosses Pennsylvania Route 125 and receives Carbon Run and Furnace Run from the left and turns north, exiting Shamokin and reentering Coal Township. Upon entering Coal Township, Shamokin Creek
19053528
Shamokin Creek


. At Shamokin, it ranged from , and below Shamokin, it ranged from . The sulfate concentration in Sunbury ranged from . In August 1999 and March 2000, the nitrogen concentration in the upper reaches of Shamokin Creek ranged from , depending on the site. At Shamokin, it ranged from , and below Shamokin, it ranged from . The nitrogen concentration in Sunbury ranged from . The concentration of sodium was , while the phosphorus concentration was and the chloride concentration was . In 1917, the "Water Resources Inventory Report" referred
19053538
Larrys Creek


The lands of the West Branch Susquehanna River Valley were then chiefly occupied by the Munsee phratry of the Lenape (or Delaware), and were under the nominal control of the Five (later Six) Nations of the Iroquois. The Great Shamokin Path crossed the creek at a ford near its mouth; however, no trails of the indigenous peoples are recorded as having followed Larrys Creek north. On November 5, 1768, the British acquired the "New Purchase" from the Iroquois in the Treaty of Fort Stanwix, opening what
20558250
Little Shamokin Creek


to the stream's rating by the Department of Environmental Protection as "impaired". Water-penny beetles have also been observed in the creek, indicating that it is recovering from being biologically impaired. However, there is siltation in the creek, which damages the food chain there. Little Shamokin Creek is part of a trout fishery that also contains South Branch Roaring Creek, Mahantango Creek, and other streams. An area of 25.5 acres on the side of Little Shamokin Creek in Rockefeller Township was converted to a recreational area by
1215880
Burpengary Creek


Burpengary Creek is a watercourse in Moreton Bay Region, Queensland, Australia. It has a total catchment area of 7,960 hectares. It is about 40 kilometres north of Brisbane, The Burpengary Creek catchment forms part of the larger Deception Bay catchment and encompasses two distinctive creeks–Little Burpengary Creek (6,360ha) and Burpengary Creek (6, 360ha). These creeks flow into Deception Bay just south of the mouth of Caboolture River, which is itself south of Bribie Island. Burpengary Creek begins in the D’Aguilar Ranges at a
18572296
Little Shamokin Creek


sandstone near the creek. There is severe erosion on the banks of much of Little Shamokin Creek. The creek is also home to a fishing hole that is approximately deep. This is experiencing erosion as well. The waters of Little Shamokin Creek have low levels of dissolved oxygen. The average annual rainfall in the watershed is . There is an average of of runoff in the watershed annually. The creek takes in 22,675.426 pounds of sediment per day and per day of phosphorus. As of 1913, the Sunbury Water Company, which
1215875
Lick Creek (Shamokin Creek tributary)


of Shamokin. However, its source is in the quadrangle of Trevorton. The watershed of Lick Creek is in the lower part of the Shamokin Creek drainage basin and in the middle of the latter watershed's northern part. Lick Creek was entered into the Geographic Names Information System on August 2, 1979. Its identifier in the Geographic Names Information System is 1179280. The drainage basin of Lick Creek is designated as a Coldwater Fishery and a Migratory Fishery. Some aquatic life exists in the creek and it historically contained a healthy aquatic
13536057
Lock Haven, Pennsylvania


. Four Indian trails, the Great Island Path, the Great Shamokin Path, the Bald Eagle Creek Path, and the Sinnemahoning Path, crossed the island, and a fifth, Logan's Path, met Bald Eagle Creek Path a few miles upstream near the mouth of Fishing Creek. During the French and Indian War (1754–63), colonial militiamen on the Kittanning Expedition destroyed Munsee property on the Great Island and along the West Branch. By 1763, the Munsee had abandoned their island villages and other villages in the area.
8179848
Gerritsen Creek


Gerritsen Creek is a short watercourse in Brooklyn, New York City that empties into Jamaica Bay. The creek currently starts near Avenue U, but its original headwaters lay eight streets farther north. That part of the creek was buried in a storm sewer in 1920. The creek's mouth and much of its remaining length is part of a nature conservation area called Marine Park. The creek has been described as one of the "fingers" that formed the original shoreline of Jamaica Bay. The creek lies just beyond the maximum extent
14371599
Bakers Creek, Queensland


"eucalypt tree". In turn, the surrounding neighbourhood and also the school are named Dundula. The land in Bakers Creek is flat and low-lying (under 10 metres above sea level) and is well-watered by the watercourse Bakers Creek which flows into the Coral Sea. To the north of mouth of the creek is the Bakers Creek Conservation Park. The land is predominantly used for growing sugarcane and there is a network of cane tramways to deliver the harvested sugarcane to the local sugar mills. The locality was
20975915
North Branch Shamokin Creek


North Branch Shamokin Creek (also known as Beaver Creek) is a tributary of Shamokin Creek in Columbia County and Northumberland County, Pennsylvania, United States. It is approximately long and flows through Conyngham Township in Columbia County and Mount Carmel Township in Northumberland County. The watershed of the creek has an area of . The entirety of the creek is designated as an impaired waterbody due to metals from abandoned mine drainage. It is acidic, but its pH has been increasing. Underground mine complexes occur within the watershed. The creek has
14862082
Shamokin Creek


upper reaches of Shamokin Creek are , while the daily loads are . Closer to Shamokin, the iron concentration ranges from , depending on the site, while the manganese concentration ranges from . The daily loads are for iron and for manganese. Downstream of Shamokin, the iron concentration steadily decreases from at site SC5 to at site SC8 at Sunbury. These values equate to daily loads of . The manganese concentration decreases less dramatically, from ( per day) at SC5 to ( per day) at Sunbury. The creek's streambed is
19053536
North Branch Shamokin Creek


the early 1900s, the old channel of the creek was occupied by rocks and culm banks. The drainage basin of North Branch Shamokin Creek is designated as a Coldwater Fishery and a Migratory Fishery. In 1999, electrofishing in the creek failed to turn up any fish life. It is not stocked by the Pennsylvania Fish and Boat Commission. The creek also lacks any macroinvertebrates and is incapable of supporting aquatic life due to its acidity. Algae flourishes in a deep mine discharge in the watershed of North Branch Shamokin Creek due to a
14862094
Little Shamokin Creek


5's capacity was 26,670,000 gallons. It was located on the east bank of the creek. The watershed of little Shamokin Creek has an area of 37 square miles. 65% of the watershed is made up of forests. These include tree farms and groups of deciduous trees. 30% of the watershed is agricultural land. 2% of the watershed is urban or developed land in general. Pennsylvania Route 890 is a major route in the Little Shamokin Creek watershed. The creek and its tributaries are also accessible via a number
1215877
Shamokin Creek


mining was being done in the watershed of Shamokin Creek by the early 1800s. In the early 1900s, coal mining, foundries, iron works, nail production, agriculture, silk mills, and woolen mills were the main industries in the watershed. In the 1990s and 2000s, many grants for restoring the creek have been received by various organizations. The main stem of Shamokin Creek is designated as a Warmwater Fishery and a Migratory Fishery. The creek is devoid of fish life in its upper reaches, but several fish species have
19053525
North Branch Shamokin Creek


a permeable streambed and experiences flow loss. A colliery historically discharged waste water into North Branch Shamokin Creek. A number of bridges have been constructed over the creek. Its drainage basin is designated as a Coldwater Fishery and a Migratory Fishery. However, the creek is incapable of supporting aquatic life, including fish and macroinvertebrates. North Branch Shamokin Creek begins in a valley near Big Mountain, in the census-designated place of Wilburton Number Two, in Conyngham Township, Columbia County. The creek flows west-southwest through the valley
14862083
White Deer Hole Creek


, crossed North White Deer Ridge and passed west through the Nippenose valley, then turned north and crossed Bald Eagle Mountain via McElhattan Creek and ran along the south bank of the river to the Great Island (near the present day city of Lock Haven). The stretch from the mouth of the creek to the Nippenose valley is approximately followed by Route 44. From the Great Island, the Great Shamokin Path continued further west to the modern boroughs of Clearfield and Kittanning, the last on the Allegheny River. Culbertson's Path followed
10682736
Shamokin Creek


south of Big Mountain, iron precipitate lines the creek for much of its length. The channel of Shamokin Creek is sinuous and flows through rock formations consisting of sandstone, shale, and extensive anthracite deposits. There are some culm deposits along the creek. The creek flows between stone walls in Shamokin. The upper of the watershed, upstream of Big Mountain, are in the Western Middle Anthracite Field, in the Coal Region. There are 34 coal veins in the watershed and nearly all have been either deep-mined or strip
19053542
Shamokin Creek


-mined. The creek passes through rock of the Hamilton Formation near Paxinos. The creek's valley is partly carved from Marcellus black slate. Red shale of the Mauch Chunk Formation also occurs in the watershed. Shamokin Creek flows almost entirely through rapids in from Shamokin downstream for . Most of these rapids are easily navigable by canoe, but there is one difficult and bouldery rapid near the Glen Burn Colliery. Eventually, the whitewater on the creek becomes less prevalent. By Paxinos, the rapids have almost disappeared, save for some
19053543
Shamokin Creek


and less than 1 percent agricultural land. In the early 1900s, there were marshes on the creek below Shamokin. Most of the land along the upper reaches of Shamokin Creek is commercial and industrial, with trash lining the streambanks. Further downstream, the creek flows through a broad floodplain, but remains impacted by development and has culm lining its cobble bars. Downstream of Snydertown, the landscape through which the creek flows is no longer impacted by development or mining and consists of forests and agricultural land. Pennsylvania Route 61 follows the
19053547
Kororoit Creek


The Kororoit Creek is a watercourse of the Port Phillip catchment, rising in the outer north western suburbs of Melbourne, in the Australian state of Victoria. The Kororoit Creek rises below Mount Kororoit, northeast of in the north western outer suburbs of Melbourne. The creek's headwaters are north of at approximately above sea level in ordovician geology. The creek flows generally south by east and passes over the volcanic lava plain of western Melbourne to its mouth at sea level, north of and emptying into Altona Bay within Port Phillip. The
1358403
Pooraka, South Australia


Pooraka (postcode 5095) is a suburb in Adelaide, South Australia. It is 12 kilometres north of the central business district. Pooraka was originally a subdivision of section 97 of the Hundred of Yatala, the latter spanning from Grand Junction Road, at Gepps Cross, to a point north of Montague Road. It was originally known as Dry Creek after the local watercourse (Dry Creek), which is now the name of a modern industrial locality west of Pooraka, at the creek's mouth (Dry Creek, South Australia
20070537
Shamokin Creek


a defined channel until Snydertown. The topography of the watershed of Shamokin Creek is "broken and mountainous". The lower reaches of the watershed mainly consist of rolling hills. The creek cuts through Big Mountain and Little Mountain immediately north of Shamokin. Locust Mountain and Mahanoy Mountain are on the southern border of the watershed's upper reaches. Broad alluvial flats occur in the lower reaches of the watershed. Mine spoil and pits occur in the upper reaches. Although mining only occurred in the upper third of the creek's watershed,
19053541
Shamokin Creek


was used as a water supply for the Pennsylvania Railroad. The Roaring Creek Water Company also used some of its tributaries as water supplies. Major settlements in the watershed of Shamokin Creek in the early 1900s included Shamokin, Mount Carmel, and Sunbury. Their populations were 19,588, 17,532, and 13,770, respectively. The main railroads in the watershed at this time were the Pennsylvania Railroad, the Philadelphia and Reading Railroad (both of which followed the creek for much of its length), and the Lehigh Valley Railroad (which crossed
19053551
Ashley County, Arkansas


northwestern boundary of the county before emptying into the Ouachita River, which serves as the southwestern boundary. The Port of Crossett is positioned just south of the Saline River's mouth. Within the county, Bearhouse Creek, Chemin-a-haut Bayou, Fountain Creek, Flat Creek, Mill Creek, and Overflow Creek are important watercourses. Ashley County contains Overflow National Wildlife Refuge, part of the Felsenthal National Wildlife Refuge, and four Wildlife Management Areas (WMAs) under Arkansas Game and Fish Commission jurisdiction. Beryl Anthony Lower Ouachita
11853161
Shamokin Creek


affect parts of the creek's watershed. Shamokin Creek is in the Appalachian Mountains section of the Ridge and Valley physiographic province. Rock formations consisting of sandstone, shale, and anthracite deposits occur in the watershed. The main land uses in the watershed of Shamokin Creek are forested land and agricultural land, with barren land and urban land making up only a few percent of the watershed. However, in the upper , forested land and mine spoils dominate, urban land is less prevalent, and agricultural land is virtually nonexistent. Coal
19053524
San Rafael Creek


San Rafael Creek is a watercourse in Marin County, California, United States that discharges to San Rafael Bay, a small embayment of the San Francisco Bay. The mouth of San Rafael Creek is a channelized estuary through an industrial area. San Rafael Creek has a designation under Federal Law Section 303(d) as impaired by diazinon, the principal pollutant causing impairment designations for streams discharging to San Pablo Bay, which is the northern arm of San Francisco Bay. In September 2007, the organization Save The Bay designated San Rafael Creek as
13617662
Dora Creek


Dora River is a watercourse that is located in the Upper Central Coast/Lower Hunter regions of New South Wales, Australia. Dora Creek River rises below Watagan Mountains west of Martinsville, and flows generally southeast by south, joined by two minor tributaries, before reaching its river mouth within Lake Macquarie, near the town of Dora Creek. The river descends over its course. The merged flows of Dora Creek together with Lake Macquarie reaches the Tasman Sea of the South Pacific Ocean at Swansea. The F3 Freeway crosses the creek,
2471331
Little Shamokin Creek


the extreme south of the watershed. The Hamilton Group is a rock formation that exists in all of the northern portion of the Little Shamokin Creek watershed. Immediately south of this formation in the watershed is a band of the Spechty Kopf formation. South of the Spechty Kopf formation is a band of members of the Irish Valley formation. In the extreme southern area of the watershed is a band of members of the Buddy Run formation. A rock formation known as the Oriskany chert stops at Little Shamokin Creek. There is also Oriskany
1215874
Refugio Creek


Refugio Creek (pronounced from Spanish "refugio" meaning: shelter) is a watercourse running through the Refugio Valley from the hills of western Contra Costa County, California. It runs from the hills to its mouth at San Pablo Bay through the city of Hercules and unincorporated areas, including the town of Rodeo. The creek passes through a dense suburban area in addition to Refugio Valley Park. The creek is almost entirely at the surface level and unaltered although its riparian habitat is largely destroyed in the more developed areas. "Refugio
21988878
Morro Creek


Morro Creek is a coastal stream in San Luis Obispo County, in the central region of the U.S. state of California. The watercourse flows from the Santa Lucia Mountains to discharge into the Pacific Ocean, at its mouth on Estero Bay, near the city of Morro Bay. The creek is in the coastal sage and chaparral section of the California chaparral and woodlands Ecoregion. Historically this watershed had habitats containing considerable amounts of chaparral, and scarce Oak woodlands, and Grey Pine ("Pinus sabiniana") trees. The lower reaches
6040227
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
Pennsylvania Route 61


the Shamokin Creek, at which point it enters Shamokin Township. The route winds north through more woodland with some commercial areas, with the Shamokin Valley Railroad and the Shamokin Creek to the east. PA 61 curves northwest and intersects the southern terminus of PA 487 in the community of Paxinos. From here, the road curves west runs to the north of the residential community of Sunfftown before narrowing to a two-lane undivided road and heading through woodland. The route continues west through woodland with some farm fields and homes, running
6496860
San Pietro (creek)


The San Pietro or Evigno is a stream of Liguria (Italy). The creek is formed close to the village of Evigno (comune of Diano Arentino) from the union of several streams descending the south-eastern slopes of monte Torre (990 m). Going SSW, a direction the creek wil keep till to its mouth, it reaches Diano San Pietro where it gets from the left rio Beste, its main tributary. San Pietro watercourse marks for a long stretch the border between the comuni of Diano Castello (West
11272029
Moonee Ponds Creek


Catchment Management Authority. In 2002 the downstream end of the creek was realigned, to accommodate development of Victoria Dock at the Port of Melbourne. Moving the confluence with the Yarra River about 600 metres upstream, the creek mouth once located at the east end of Appleton Dock was removed, with a new watercourse dug leading directly south parallel with the Bolte Bridge approach spans. The realignment created a buffer zone between the port and the Melbourne Docklands residential and commercial areas. While realigning waterways is not a preferred option for Melbourne Water,
2484722
Patawalonga River


before European settlement, a tidal estuary. The river is serviced by a catchment area that exists in metropolitan Adelaide, with its mouth at the suburb of Glenelg. The Patawalonga serves as an outlet for the Keswick and Brownhill creeks and the Sturt River (also known as Sturt Creek), the latter being a former natural creek comprising for a significant part of its length now as a large concrete storm-drain. The catchment includes the Cowandilla-Mile End drainage network, the construction of which has replaced numerous small natural watercourses
9459104
Shamokin Creek


. It continues flowing north for several miles though a valley and alongside Pennsylvania Route 61, receiving Bennys Run from the left, Millers Run from the right, and Lick Run from the left. More than a mile after receiving Lick Run, Shamokin Creek turns in a westerly direction for many miles. In this reach, it flows through a much broader and deeper valley. It passes through Shamokin Township and Snydertown before entering Upper Augusta Township. Here, the creek flows in a west-southwesterly direction for several miles before turning
19053530
Locust Creek (Shamokin Creek tributary)


Locust Creek is a tributary of Shamokin Creek in Northumberland County, Pennsylvania, in the United States. It is approximately long and flows through East Cameron Township and Mount Carmel Township. The watershed of the creek has an area of . The stream is designated as impaired due to metals from abandoned mine drainage. It also experiences a low pH. The creek flows through a water gap in Locust Mountain. Prominent land uses in its watershed include refuse areas and forested land. The creek's watershed is designated as a Coldwater Fishery and a
14784335
San Mateo Creek (San Francisco Bay Area)


it is partly intermittent and altered, to San Francisco Bay about 1.1 km (0.7 mi) west of the mouth of Seal Slough. This watercourse lies entirely within San Mateo County and flows generally eastward to discharge into San Francisco Bay. San Mateo Creek once hosted coho salmon ("Oncorhynchus kisutch") as evidenced by specimens collected by Professor Alexander Agassiz of Harvard University in the 1850s and 1860s. He also collected steelhead trout ("Oncorhynchus mykiss") from the creek. Historical records indicate that Chinook salmon ("Oncorhynchus
4303207
Little Shamokin Creek


provides water to Sunbury, got its water from Little Shamokin Creek. A dam with five reservoirs was created on the creek, east of Sunbury. Reservoir Number 1's capacity was 2,750,000 gallons. Reservoir Number 2's capacity was 2,180,000 gallons. It was located on the east bank of the creek. Reservoir Number 3's capacity was 1,900,000 gallons. It was also located on the east bank of the creek. Reservoir Number 4's capacity was 16,510,000 gallons. It was located on the east bank of the creek. Reservoir Number
1215876
Plum Creek (Little Shamokin Creek tributary)


built in 1939 and repaired in 1997. It is long and is located southwest of Stonington. Another bridge of the same type was built over the creek southwest of Stonington in 1939 and repaired in 1994. This bridge carries State Route 4013 and is long. A prestressed box beam or girders bridge with a length of was constructed across the creek northwest of Seven Points in 1989 and carries T-684. The name "Plum Creek" was erroneously given to another stream in the stream system of Little Shamokin Creek in a 1952 United States
13318763