Twomile Run [SEP] mouth of the watercourse
[{"answer": "Kettle Creek", "provenance": [{"wikipedia_id": "42462145", "title": "Twomile Run", "start_paragraph_id": 1, "start_character": 0, "end_paragraph_id": 1, "end_character": 97, "bleu_score": 1.0, "meta": {}, "section": "Section::::Abstract."}]}]
Twomile Run


day. The pH of Twomile Run at its mouth ranged from 3.4 to 3.9 and the average pH at this location was 3.52 in 2007. However, by 2011, the pH upstream of Huling Branch had increased by 0.4 and the acidity concentration of Twomile Branch had halved. The alkalinity concentration in Twomile Run above Middle Branch Twomile Run is 0.37 milligrams per liter and the daily load is . The concentration of alkalinity in Twomile Run upstream of Pecking Patch Hollow is 1.03 milligrams per liter. The daily load is at this location.
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Twomile Run


Twomile Run is a tributary of Kettle Creek in Clinton County, Pennsylvania, in the United States. It is long. Tributaries of the stream include Huling Branch and Middle Branch Twomile Run. The stream flows through Leidy Township and Noyes Township. The stream's watershed has an area of approximately 9 square miles. Coal is mined in the watershed. Most of the acid mine drainage in Kettle Creek comes from Twomile Run. The discharge of Twomile Run at its mouth ranges from 200 to 10,000 gallons per minute. There are 2.1
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Kettle Creek (Pennsylvania)


per day. At the mouth of Twomile Run, the daily manganese load is and at the USGS stream gauge on Kettle Creek, the load is per day. At the USGS gauge on Kettle Creek, the daily load of aluminum is and at the mouth of Twomile Run it is per day. At the mouth of Butler Hollow, the aluminum load is per day. At the mouth of Kettle Creek itself, it is per day. The daily load of acidity at the creek's mouth is per day and at the
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Twomile Run


, it is per day. The load of aluminum above the swamp on Twomile Run is and the load is per day upstream of the stream's middle branch. Below Robbins Hollow, the load is per day and below KC121, the daily load is . Downstream of Huling Branch, the daily load is . The manganese concentration at the mouth of Twomile Run ranges from 2.1 to 11.7 milligrams per liter. The average concentration is 5.6 milligrams per liter. Upstream of Middle Branch Twomile Run, the concentration is 6.83 milligrams per liter
15498986
Kettle Creek (Pennsylvania)


Twomile Run enters it from the northeast. At the United States Geographical Survey stream gauge downstream of the Alvin R. Bush Dam, the load of iron in Kettle Creek is per day. The daily load of iron is at the mouth of the tributary Twomile Run. The load of iron is per day at the mouth of the tributary Butler Hollow. At the mouth of Kettle Creek, the load is per day. The daily load of manganese at the mouth of the creek is and at the mouth of Butler Hollow it is
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Twomile Run


Run at its mouth ranges from 291 micro-Siemens to 1091 micro-Siemens, with an average of 663 micro-Siemens. There are a number of surface mines and deep mine complexes in the Twomile Run watershed. Some of the deep mine complexes extend into adjacent watersheds. There are several rock formations in the Twomile Run watershed which are visible on the surface. These include the Huntley Mountain Formation, the Burgoon Sandstone, the Pottsville Group and the Allegheny Group. The Huntley Mountain Formation is from Devonian and Mississippian times and
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Kettle Creek (Pennsylvania)


mouth of Butler Hollow it is per day. The acidity load at the mouth of Twomile Run is per day and at the USGS gauge the load is per day. At the USGS gauging station on Kettle Creek, the concentration of iron is 0.15 milligrams per liter, the concentration of manganese is 0.04 milligrams per liter, and the concentration of aluminum is 0.14 milligrams per liter. The acidity concentration is 0.64 milligrams per liter and the concentration of alkalinity is 11.36 milligrams per liter. At the mouth of Twomile Run, the concentration
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Twomile Run


Wellsboro Anticline and to the south is the Hyner Dome. The Huling Branch valley is relatively straight and narrow. The elevation of Twomile Run at its source is , while the elevation at its mouth is . The first acid mine drainage discharge is at . The maximum elevation in the watershed is . The average basin slope is 8.32 degrees. At to white and orange metal precipitate forms on the banks of Twomile Run at its confluence with Kettle Creek because the waters of the former stream are acidic, while those of the latter are
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Twomile Run


the sampling site KC121, the discharge is 1893 gallons per minute and upstream of Huling Branch, the discharge is 2258 gallons per minute. The discharge at the mouth of Twomile Run ranges from 200 to 10,000 gallons per minute, which is between 0.6 and 2 percent of the discharge of Kettle Creek. Upstream of the swamp on the stream, the daily load of iron is and the load is per day upstream of Middle Branch Twomile Run. Downstream of Robbins Hollow, the daily iron load is per day and downstream of KC121
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Twomile Run


were considered to be "poor" or "marginal" habitats by the Pennsylvania Department of Environmental Protection in 2001. The Pennsylvania Fish and Boat Commission assessed the mouth of the stream as 2 out of 10 on their habitability scale in the same year. Most of the land in the Twomile Run watershed is used for recreation. Deer hunting and bear hunting are often done in the area. There is also a series all-terrain vehicle trails known collectively as the Whiskey Springs ATV trail complex. These are located in the sub
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Twomile Run


to 11.7 milligrams per liter of manganese in the waters at this location. In 2007, the average pH at the mouth of the stream was 3.52, with a range of 3.4 to 3.9. By 2011, the stream's pH had increased slightly upstream of Huling Branch. Rock formations in the watershed include the Huntley Mountain Formation, the Burgoon Sandstone, the Allegheny Group, and the Pottsville Group. Twomile Run begins in Sproul State Forest in Leidy Township, Clinton County. The stream flows south and slightly east, leaving Sproul
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Twomile Run


State Forest and Leidy Township and then entering Noyes Township. Soon after entering Noyes Township, it receives the tributary Middle Branch Twomle Run and continues south. The Twomile Run valley begins to get deeper at this point. The stream turns southwest, then southeast, and then southwest again. Shortly after the final bend, it receives the tributary Huling Branch and not long afterwards enters Kettle Creek. Named tributaries of Twomile Run include Middle Branch Twomile Run and Huling Branch. Robbins Hollow joins Twomile Run downstream of Middle Branch Twomile Run.
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Twomile Run


Twomile Run, Huling Branch, and Middle Branch Twomile Run all have floodplains in their upper reaches. The first coal mines in the Twomile Run watershed were deep mines, but there are no surviving maps of them. Surface mining of the Lower Kittanning and Upper Kittanning coals began after World War Two, with the Lower Kittanning coal being mined to a depth of . By the 1970s, the surface mining had ended. Much of the coal mined in the entire Kettle Creek watershed was in the Twomile Run watershed. In the 1930s
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Twomile Run


the Pennsylvania Fish and Boat Commission observed two species of fish, white sucker and smallmouth bass in this location. Twomile Run has the highest potential fish biodiversity of all streams in the Kettle Creek watershed, with a Potential Species Richness of 232 to 241 in places. "Plecoptera", "Trichoptera", "Odonata", and "Coleoptera" have all been observed on Huling Branch. The stonefly and caddisfly populations on Middle Branch Twomile Run are increasing. The confluences of Middle Branch Twomile Run and Huling Branch with Twomile Run
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Twomile Run


Huling Branch has an unnamed tributary of its own and is significantly longer than Middle Branch Twomile Run, about the same length as Twomile Run. Other tributaries of Twomile Run include Pecking Patch Hollow and MackIntosh Hollow. The watershed of Twomile Run experiences significant acid mine drainage, with of the stream being affected by it. The acid mine drainage flows in the watershed have a pH of 2.5 to 3.5, an iron concentration of 20 to 50 milligrams per liter, and an aluminum concentration of 20 to 70 milligrams per liter. The
15498983
Twomile Run


There is no alkalinity downstream of Huling Branch. The sulfate load upstream of the swamp on Twomile Run is per day and upstream of Middle Branch Twomile Run, the daily load is . Downstream of Robbins Hollow and KC121, the sulfate load is and per day, respectively. Below Huling Branch, the load is per day. The sediment load in the Twomile Run watershed is per acre per year. The phosphorus and nitrogen loads are less than per acre per year and per acre per year, respectively. The conductivity of Twomile
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Twomile Run


and early 1940s, there was a Civilian Conservation Corps located in the Twomile Run watershed. A draft for an Operation Scarlift report was written in 1973 for Kettle Creek (which Twomile Run is a tributary of), but was never approved. A number of passive treatment systems were installed in the tributary Robbins Hollow in 2004 and nine have been installed in the main stem. Timber is produced in the watershed of Twomile Run. Some coal reserves remain in the watershed. Brook trout are found in the upper reaches of the tributary
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Twomile Run


Middle Branch Twomile Run, upstream of the acid mine drainage discharges in its watershed. There are brook trout above the acid mine drainage discharges on Twomile Run, but none below the discharges. The brook trout population is considered to be a "Class A population" and is increasing. The concentration of brook trout at one location on the tributary Huling Branch is per hectare and at another location the concentration is per hectare. The confluence of Twomile Run with Kettle Creek was completely devoid of fish in 1967, but by 1997,
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Twomile Run


acidity concentration in these flows ranges from 200 to 600 milligrams per liter. The stream is the only significant source of acid mine drainage to enter Kettle Creek on its eastern side. Thirty to fifty percent of the acid mine drainage in the Twomile Run watershed comes from baseflow. Above the swamp on Twomile Run, the discharge of the stream is 511 gallons per minute. Upstream of Middle Branch Twomile Run, the discharge is 618 gallons per minute and downstream of Robbins Hollow, the discharge is 1402 gallons per minute. Downstream of
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Kettle Creek (Pennsylvania)


of the mouth. At the southern edge of Leidy Township, Kettle Creek makes several meanders, crossing the border between Leidy Township and Noyes Township three times. The creek then meanders several miles through Noyes Township, passing strip mines and another gauging station. The creek's mouth is at the community of Westport, near Pennsylvania Route 120. Significant tributaries to Kettle Creek include Germania Branch, Little Kettle Creek, Cross Fork, Hammersley Fork, Trout Run, Beaverdam Run, Twomile Run and others. In the upper reaches of Kettle
10473366
Clavey River


-south, which is rare for streams in the western Sierra, which generally flow from east to west. Shortly downstream, it receives Rock Creek from the left, then Trout Creek from the right, and is crossed by Forest Route 3N01 about above the mouth. It receives Twomile and Cottonwood Creeks from the right, then Reed Creek, its largest tributary, from the left about from the mouth. Between Twomile and Cottonwood Creeks there is a concrete bridge carrying Forest Route 1N04. The Clavey receives Bear Springs Creek and Quilty
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Twomile Run


alkaline. The velocity-depth of Twomile Run is low, but there is an adequate frequency of riffles in the stream. The right bank of the stream is somewhat unstable. Between 1992 and 2005, the annual precipitation ranged from to at the nearby Alvin R. Bush Dam. The average rate of precipitation was per year. The watershed of Twomile Run has an area of 9.15 square miles. There are of streams in the watershed, of which are affected by acid mine drainage. Most of the watershed is forested land.
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Twomile Run


the Burgoon Sandstone is from Mississippian times. The other two formations are both from the Pennsylvanian times. The Upper Kittanning and Lower Kittanning coal seams are found in hills with the Allegheny Group. The Pottsville Group also contains coal seams. The elevation of the Upper Kittanning coal seam in the watershed ranges from to in the ridge between Middle Branch Twomile Run and Huling Branch. The watershed of Twomile Run runs in approximately the same direction as the nearby Clearfield-McIntyre Syncline. To the north of the Clearfield-McIntyre Syncline is the
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Twomile Run


and the daily load is . Above Pecking Patch Hollow, the concentration of manganese is 6.43 milligrams per liter and the daily load is . Downstream of Huling Branch, the manganese concentration is 6.44 milligrams per liter and the load is per day. The daily load of acid above the swamp on Twomile Run is . The load of acid above Middle Branch Twomile Run is per day. Below Robbins Hollow, the daily load is ; below KC121, the load is per day. Downstream of Huling Branch, the daily load is per
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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
Kettle Creek (Pennsylvania)


Short Bend Run it was 431 milligrams per liter. Above Twomile Run on Kettle Creek, the sulfate concentration was 16 milligrams per liter and at the mouth it was 11 milligrams per liter. Upstream of the acid mine drainage, the sulfate concentration ranges from under 10 to 17 parts per million. In areas affected by acid mine drainage, the sulfate concentration ranges from 37 to 1375 parts per million. The chloride concentration in the waters of Kettle Creek and its tributaries is very low, ranging from under one to three parts per
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Twomile Run


However, there are some areas of grassland, parking areas, and roads. The watershed runs in a northeast-southwest direction. Most of the land in the watershed is owned by the Pennsylvania Department of Conservation and Natural Resources, the Bureau of Forestry, and Sproul State Forest. There are some agricultural lands in the watershed, most of which are in the vicinity of Huling Branch. Roads in the Twomile Run watershed include Two Mile Run Road. There are between 15 and 20 stream crossings in the stream's watershed.
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Kettle Creek (Pennsylvania)


. It is acidic due to a presence of pyrite and has a sulfur concentration of 1 to 5 percent. The Clearfield-McIntyre Syncline runs through the western lower part of the Kettle Creek watershed in a southwest-to-northeast direction. North of this syncline lies the Wellsboro Anticline. South of it lies the Hyner Dome. A set of fractures in the watershed causes the tributary Huling Branch to have a straight and narrow valley and for Kettle Creek itself to make a sharp 90-degree turn near the mouth of the tributary Twomile
10473383
Twomile Creek (Kanawha River)


Twomile Creek is a tributary of the Kanawha River, long, in West Virginia in the United States. Via the Kanawha and Ohio rivers, it is part of the watershed of the Mississippi River, draining an area of on the unglaciated portion of the Allegheny Plateau, in the city of Charleston and its vicinity. Twomile Creek is formed approximately east-northeast of the unincorporated community of Guthrie by the confluence of the Right Fork Twomile Creek, long, which rises approximately north-northwest of the unincorporated community of Elk Hills,
13756965
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
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
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
Nea-Nidelvvassdraget


Nea-Nidelvvassdraget is a watercourse in the municipalities of Tydal, Selbu, Klæbu, and Trondheim in Trøndelag county, Norway. The total area of the watershed is and it runs for about from the source in the Sylan mountains to its mouth in Trondheimsfjorden. Trondheim Energiverk has fourteen power stations along the water course which are highly regulated, with a total production (in 2004) of . Development of the area had already begun in 1890 with the development of the Øvre Leirfoss power station. Important rivers in the Nea-Nidelvvassdraget
1382567
Cooum River


and Chinese coins on the banks of the river. In the late eighteenth century, Pachaiyappa Mudaliar, the renowned philanthropist, bathed in this river before offering prayers at the Komaleeswarar Temple in Komaleeswaranpet. Cooum River and the nearby Elambore River (or North River), which flows into the Cooum at its mouth, were running very close to each other near the former Central Jail area opposite Chennai Central. During floods, both the watercourses inundated the whole area. In the 1700s, the two rivers were linked by a cut to
18984612
Kettle Creek (Pennsylvania)


Bush Lake sub-watershed, with an average slope of 19.12 degrees. Other sub-watersheds with steep slopes include Spicewood Run (18.54 degrees), Walters Run (17.32 degrees), middle Kettle Creek (16.78 degrees), and Hammersley Fork (16.24 degrees). The least steep basin in the watershed is Twomile Run, with an average slope of 8.32 degrees. The watershed of Kettle Creek has an area of 244 square miles. It is located in Clinton, Potter, Cameron, and Tioga Counties. Forested land
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Kettle Creek (Pennsylvania)


grow on the tributary Bearfield Run. Mammal and bird diversity is high throughout the stream corridors in the Kettle Creek watershed. Reptile and amphibian diversity is the highest in the southern part of the stream corridors. Fish diversity is highest in the Twomile Run sub-watershed. Two wetlands can be found in the sub-watershed of John Summerson Branch Trout Run. One is a mixed graminoid swamp and the other is a broadleaf conifer swamp. Half of the trees in the Kettle Creek watershed are northern hardwood trees. The remainder includes
10473415
Sepik


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


definition of a river source specifically uses the most distant point (along watercourses from the river mouth) in the drainage basin from which water runs year-around (perennially), or, alternatively, as the furthest point from which water could possibly flow ephemerally. The latter definition includes sometimes-dry channels and removes any possible definitions that would have the river source "move around" from month to month depending on precipitation or ground water levels. This definition, from geographer Andrew Johnston of the Smithsonian Institution, is also used
20534038
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
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
Eider Canal


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


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


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


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


section of Watling Street between Hockliffe and Dunchurch (and thus serving this neighborhood) became a turnpike. A toll-gate, the "Twomile Ash Toll Gate" was located here, and it was from this that Milton Keynes Development Corporation took the district name. By the First Edition of the Ordnance Survey (1846-), a building is shown beside the road, called "Twomile Ash". A milestone can still be found on Watling Street (now called the V4). Immediately behind the two mile post are three
14097880
Course of the Rogue River (Oregon)


Next comes Illahe Campground, on the right bank at RM 33 (RK 53). Little Wildcat Rapids begins the next stretch. Below this, Lone Tree Creek enters from the right just before Old Diggins Rapids, below which Twomile Creek enters from the right just before Twomile Rapids. Next comes Walker Bar, where Walker Creek enters from the left, and below this Slide Creek enters from the right. At this point, NFD Road 33 crosses the river and continues along the left bank, while the Agness-Illahe Road
21723834
Josiah Gregg


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


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


Spencer Township is one of eleven townships in Jennings County, Indiana, United States. As of the 2010 census, its population was 2,326 and it contained 911 housing units. According to the 2010 census, the township has a total area of , of which (or 99.35%) is land and (or 0.65%) is water. The streams of Indian Creek, Little Mutton Creek, Powder Creek, Storm Creek, Tea Creek and Twomile Creek run through this township. The township contains eight cemeteries: Barkman, Hunt
21594677
Discovery Bay, Washington


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


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


In Scotland and northern England a Linn is a geographical water feature. In Scotland it describes where a watercourse has cut through a shelf of hard rock creating a narrow (usually), steep-sided cut though which the watercourse runs. Typically there is only one named Linn on any watercourse - although obviously - there may actually be more than one feature with the necessary attributes. The photograph of the Linn of Dee illustrates the attributes of a typical 'Linn'. In "Gordon (1925)" the author describing a
13483383
Swan Coastal Plain


of the soil results in the loss of much water. Much flow is lost, and some watercourses simply cease to flow, for example, Wungong Brook, Cardup Brook, and Manjedal Brook. Secondly, the sequence of north-to-south-oriented dunes create obstacles to further westerly flow. Many watercourses turn at right angles and flow south or north along the dune swales, and in some cases this allows multiple watercourses to coalesce. For example, on reaching the coastal plain, Ellen Brook runs south for around 30
21688450
South Rockhampton Cemetery


of the non-Judaeo-Christian section where the burial traditions of the Chinese, Aboriginal and other groups left no visible memorial. A watercourse runs from the southwest corner through the Church of England section to the eastern perimeter. Some headstones exist within overgrown areas of this watercourse, including the only surviving cast iron headstone. A sandstone ridge surfaces within the watercourse, and a headstone dated 1862 is thought to have been quarried from the sandstone on this site, as it has a different grain and colouring to the local Stanwell sandstone
5270178
Watercourse Distillery


Distillers, who at that stage owned the Watercourse along with several other distilleries in the Republic of Ireland consolidated its operations in a new, purpose-built distillery in Midleton. The name of the distillery lives on in the name given by Irish Distillers to a subsidiary which runs the Jameson Experience at the former Jameson Bow Street Distillery in Dublin and the Old Midleton Distillery in Cork. The Watercourse Distillery was where Cork Dry Gin, the most popular brand of gin in Ireland was originally produced. In the 1960s, Cork Distilleries Company
9625744
Kettle Creek (Pennsylvania)


1983 to by 6.4. The tributaries Twomile Run, Huling Branch, and Middle Branch above the acid mine drainage have had their pH levels measured at 5.9, 5.7, and 5.5, respectively. The pH of the watershed ranges from 5.5 to 8.6. The alkalinity concentration of the waters of the creek ranged from 20 to 25 milligrams per liter in the 1950s and 1960s, but decreased to 11 to 15 milligrams per liter by 1993. Kettle Creek's level of specific conductivity ranges from 50 to 1500 micro-siemens. On
10473376
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
Somatosensory evoked potential


. Conversely, source modeling suggests that the evoked field distribution at a given moment may result from activities of multiple distributed sources that overlap in time. This model fits better with the parallel activation and the feedback controls that characterize the processing of somatosensory inputs at the cortical level. When recording SEPs, one usually seeks to study peripheral, spinal, brainstem, and early cortical SEPs during the same run. Electrodes placed on the scalp pick up both SEPs generated in the cortex and thalamocortical fibers (which are picked up as near-
10173556
Sep Lambert


though, against Scotland in 1920 and against the Irish Military and Scotland in 1921. In all matches for Ireland, Sep Lambert scored 342 runs at an average of 20.12, with a top score of 60 not out against Oxford University in May 1902, his only half-century for Ireland and also his top first-class score. He took ten catches and no stumpings. Sep Lambert came from a cricketing family. His brother Bob was one of Ireland's finest cricketers, and his nephew Ham also played cricket for Ireland
17780530
World Qualification Series (2009)


18 - Aug 23" 30th Anniversary of the Lacanau Pro and good conditions this year. Surf, concerts, events scheduled. Check out the video for a summary of the event http://vimeo.com/6994555 "Aug 25 - Aug 30" "Sep 01 - Sep 06" "Sep 01 - Sep 06" "Sep 04 - Sep 06" "Sep 09 - Sep 12" "Sep 10 - Sep 13" "Sep 08 - Sep 13" "Sep 15 - Sep 20" "Sep 16 - Sep 22" "Sep
1986943
2011 Scottish Conservative Party leadership election


MSP and Liz Smith MSP endorse Murdo Fraser. 30 Aug – Liz Smith is declared as Murdo Fraser's campaign manager. 1 Sep – Gavin Brown, formerly speculated as standing in the election, states that he will not run and lends his backing to Murdo Fraser. 2 Sep – Jackson Carlaw officially launches his leadership campaign in Glasgow. 4 Sep – Murdo Fraser makes the high-profile announcement that if elected leader, he would disband the Scottish Conservatives and seek to create a new centre-right party, autonomous but allied
10722173
List of 1982–83 NBA season transactions


1982 Oct 2, 1982 Oct 1, 1982 Sep 30, 1982 Sep 29, 1982 Sep 28, 1982 Sep 27, 1982 Sep 24, 1982 Sep 22, 1982 Sep 20, 1982 Sep 19, 1982 Sep 18, 1982 Sep 17, 1982 Sep 15, 1982 Sep 14, 1982 Sep 13, 1982 Sep 10, 1982 Sep 9, 1982 Sep 7, 1982 Sep 2, 1982 Sep 1, 1982 Aug 31, 1982 Aug 27, 1982 Aug 26, 1982 Aug 16, 1982 Aug 8,
557049
Bradford Township, Chickasaw County, Iowa


Bradford Township is one of twelve townships in Chickasaw County, Iowa, USA. As of the 2000 census, its population was 2,140. Bradford Township is named for Chief Bradford of the Chickasaw Indians. Bradford Township covers an area of and contains one incorporated settlement, Nashua. According to the USGS, it contains five cemeteries: Cagley, Greenwood, Oak Hill, Pearl Rock Catholic and Saint Michaels. The streams of Little Cedar River and Twomile Creek run through this township. Bradford Township contains two airports or landing strips: Clevelands
17170661
River Bourne, Addlestone


were caused by heavy rainfall and thunderstorms across the region that resulted in flooded homes and businesses, power cuts and road closures. This caused the rainfall to run across the land to local watercourses and low-lying areas. Two months' rainfall fell in one night and local watercourses were unable to cope with the run off so flooded adjacent land, buildings and roads. Concerns were express by residents to the parish council that the flooding in Chobham was exacerbated on a small scale by the use of Field 0081, Pennypot Lane,
13728728
Kettle Creek (Pennsylvania)


, ospreys, Canada geese, herons, and mallard ducks have visited Kettle Creek Lake. Various birds of prey have also temporarily visited the watershed. Ring-necked pheasants and ruffed grouse live in the watershed. On Twomile Run above the acid mine drainage, a total of 19 macroinvertebrate taxa including 5 members of the orders Ephemeroptera and Plecoptera were observed in 1998. Below the acid mine drainage, there were only two taxa, neither of which belonged to Ephemeroptera or Plecoptera. Above the acid mine drainage on Middle Branch, ten
10473410
September 1941 lunar eclipse


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


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


Jerome "Jerry" White (born 1959) is an American politician and journalist, and is the Labor Editor reporting for the World Socialist Web Site. He is a member of the Socialist Equality Party of the United States, and was a member of its predecessor the Workers League, joining the movement in 1979. White ran as the SEP candidate for United States President in 1996 and 2008, and again in 2012 with running mate Phyllis Scherrer. White was again the SEP presidential nominee in the 2016 election. Jarome White was
2288073
The Beeps


Sapphire Stream S2/Ep45 Apr. 29 Wash Those Socks! S2/Ep46 Dec. 12 The Bumps SEASON 3: S3/Ep1 Aug. 30 Up Down Hill S3/Ep2 Aug. 31 Caravan S3/Ep3 Sep. 6 Secret Garden S3/Ep4 Sep. 7 Bounceflower Tea S3/Ep5 Sep. 13 The Whale S3/Ep6 Sep. 14 Soggy Sockroaches S3/Ep7 Sep. 20 Stinkroots S3/Ep8 Sep. 21 Sing-a-long-a-beeps S3/Ep9 Sep. 27 History Book S3/Ep10 Sep. 28 What Goes Splat? S3
14688027
Ayr


meaning "watercourse" or "strong river". This name was used before the establishment of the Julian calendar in reference to the River Ayr. The town was formerly known as 'Inverair' or 'Inverayr', meaning "mouth of the river Ayr", yet this was later abbreviated to 'Air', and then to 'Ayr'. Elements of the old name remain present within the Scottish Gaelic name for Ayr – "Inbhir Air". The areas surrounding modern day Ayr were known to have been occupied
10090348
Signal Transfer Point


. SEPs send signaling messages to other SEPs, but the messages are normally routed via the SEP's adjacent STPs. An STP's main function is to identify the best path for two SEPs to communicate. A typical application would be for two SEPs to agree on the use of a shared data path (e.g., using ISUP to initiate a voice call between a user on one SEP and a user on the second SEP). In this way, STPs route signaling messages (for starting, maintaining or finishing any kind of
21819468
Hobson's Conduit


Hobson's Conduit, also called Hobson's Brook, is a watercourse that was built from 1610 to 1614 by Thomas Hobson and others to bring fresh water into the city of Cambridge, England from springs at Nine Wells, a Local Nature Reserve (), near the village of Great Shelford. It is now a Scheduled Ancient Monument and historical relic. The watercourse currently runs overground until Cambridge University Botanic Garden and Brookside, where it is at its widest. At the corner of Lensfield Road stands a hexagonal monument to Hobson,
13766129
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
River Continuum Concept


to be more predictable as to the biological properties of the water. The concept was first developed in 1980 by Robin L. Vannote, with fellow researchers at the Stroud Water Research Center. The River Continuum Concept is based on the idea that a watercourse is an open ecosystem that is in constant interaction with the bank, and moving from source to mouth, constantly changing. Basis for this change in the overall system is due to the gradual change of physical environmental conditions such as the width, depth, water, flow characteristics,
15291764
Waswanipi River


of Chibougamau. A bridge spans the river at the village of Waswanipi. From its source, the course of the river flows over distributed as follows: The mouth of the Waswanipi River is located at: As early as XVIIIth century, the designation "Waswanipi" means a lake Waswanipi, two rivers and a Native American group. The river has already been referred to as "Olga River". A map of 1898 indicates "R. Waswanipi" for this watercourse. At the beginning of the XXth century, during a voyage
18069608
Beckfoot


-futr", meaning "the mouth of a stream". Beck is a local word in Cumbrian dialect for a stream. Such a beck empties into the Solway Firth at the southern end of the hamlet, and it is this watercourse which gives the settlement its name. There are two known recorded variant spellings: Beck and Beckfoote. The area around Beckfoot was fortified during Roman times, as a series of milefortlets were constructed to guard the coast beyond the western end of Hadrian's Wall. The remains of milefortlets 14
19486679
Maceió


international flights. The city is home to the Federal University of Alagoas. The name "Maceió" has origin in the term tupi maçayó or maçaio-k, that means "what it covers the swamp". The Aurélio Dictionary says that the term "maceió" means a temporary and cyclic lagoon that is located at the edge of the sea at the mouth of a watercourse small enough to be interrupted by a silicate bar until the high tide opens the way temporarily cyclically related to the season, river flow, lunar seasons
9117059
River Adur


the English Channel at Shoreham-by-Sea. The mouth of the Adur is now two miles (3 km) from the town centre of Shoreham due to longshore drift. The Baybridge Canal uses part of the Adur's watercourse. The name "Adur" is a relatively recent (probably 1612s) invention, based on the name of the Roman fort Portus Adurni which was mistakenly believed to be at Shoreham. The river had previously been known as the "Bramber", and was also recorded as the "Sore"
9660167
Signal Transfer Point


calls originated by the SEPs' attached users) while avoiding disabled intermediary STPs. A signaling message typically never goes directly from a given SEP to the destination SEP: the message would normally have to pass through the initiating SEP's adjacent STP so that it can be routed to the destination SEP. In some applications, however, SEPs might be directly connected with signaling links; this would typically be done to enhance robustness or performance between two critical SEPs. Such mesh network configurations are also common in Europe, where STPs have not
21819469
Ordinary watercourse


have permissive power to carry out flood defence works at their discretion. This implies that a residual responsibility to maintain ordinary watercourses, and to report any issues with them to lead local flood authorities, (county councils or unitary authorities) rests in tort with riparian owners, that is owners of land adjoining such watercourses. Such watercourses were historically defined as non-navigable watercourses however their designation has changed to those watercourses not included on a 'main rivers map' and whose bed is not owned by an authority. Critical Ordinary Watercourses
11832706
Batmania


#12 (Sep 1965) about "The Silent Legend Behind the Batman!", namely Finger. Describing Kane's hiring of Finger and likely becoming the first source to state that Finger "put words in the mouth of the Guardian of Gotham," Bails attributed the status of co-creator of Batman to Finger. This led to a "lengthy retort" from Bob Kane himself appearing in the "Batmania" fanzine, "written just days after seeing the Bails piece," but unprinted until the 1967 "Batmania
6291360
Ordinary watercourse


An ordinary watercourse is one of the two types of watercourse in statutory language in England and Wales. Ordinary watercourses include every river, stream, ditch, drain, cut, dyke, sluice, sewer (other than a public sewer) and passage through which water flows and which does not form part of a main river. An internal drainage board where relevant, or lead local authority has permissive powers to carry out flood defence works for ordinary watercourses at their discretion. An ordinary watercourse is one of the two types of watercourse
11832704
Großer Zschand


The Großer Zschand is the longest dry valley in Saxon Switzerland and runs for about 6 km from the Neumann Mill in the Kirnitzsch valley to the "Roßmaulwiese" meadown in Bohemian Switzerland. The Großer Zschand has no permanent watercourse; during times of snowmelt or after heavy rain, individual, locally limited watercourses and small marshy areas are formed. The Großer Zschand was used in the days before the development of Saxon Switzerland as a trade route between Bohemia and Saxony. At Zeughaus there used to be a customs post. Until the present
5414112
List of rivers of County Dublin


There are more than 130 named rivers and streams in County Dublin, Ireland, which comprises the city of Dublin and the surrounding administrative counties. The rivers and streams are listed in one table, with systems such as the Liffey (and that of its major sub-system, the Dodder), Broadmeadow, Tolka and Shanganagh identified within the table. The name of each watercourse, the location of its mouth or confluence point and whether, for tributaries, they enter their parent on the right or left bank, is noted
10510129
Sableuse River


The Sableuse River is a watercourse in the Matapedia Valley, in administrative region of Bas-Saint-Laurent, in Quebec, Canada. Its origin lies in the Sableuse ponds in Saint-Vianney while its mouth lies in the Sableuse River Bay on Lake Matapedia. This river flows into the regional county municipalities (RCM): This course river of the Matapedia Valley is descending towards the Southwest; it passes through the territory of Sainte-Paule and Matapedia Lake (at the Eastern boundary of the territory of Sayabec). The
13244144
Tartigou River


The Tartigou River is a watercourse over long in the Matapedia Valley in Quebec, Canada. Its origin lies in the Bon-Dieu Lake in Saint-Moïse, while its mouth is on the Saint Lawrence in Baie-des-Sables. The name "Tartigou" comes from a transcription of the Mi'kmaq word "tlagatigotj". "Tartig" means "river of the little colony" or "little river of the colony." The Tartigou River takes its water from the Matapedia Valley in the Bas-Saint-Laurent
13244322
Arnschwang


preserved. In Arnschwang there were numerous of the very rare subterranean stables, the so-called "Schrazellöcher". Village-fountain sculptored by the local sculptor "Toni Scheubeck" on the occasion of the 1200-Jubilee year in 1995. Made of "Fürstensteiner" granite, the water channels polished, thereby brighter active; the remaining surfaces shaded. Source place and mouth of the watercourse in the fountain are marked with the annual figures 795 and 1995. It is 2-storey, long-stretched building. We will see the remains of
13442713
Marne (estuary)


The Marneslenk (Dutch), or Marneslinke (Frisian), or Marne estuary, was a former estuary in western Friesland south of Harlingen, now reclaimed to be farmland. It formed around the year 300 AD, when rising sea levels also enlarged the Almere lake to the southwest, and formed the Middelzee to the east. The Marneslenk had its mouth on the Vlie and stretched southeasterly to the area of Tirns and then headed east to the Middelzee. Between 1100 and 1300 AD the watercourse was reclaimed and turned into fields by
13962934
Sully, Vale of Glamorgan


equivalent. It has been suggested that "Abersili" would be a more appropriate Welsh name, and an unofficial referendum has shown significant support for that view amongst residents. But it is unclear whether the name "Abersili" has ever been in common use; the earliest known example is by Iolo Morganwg, a notoriously untrustworthy source. Furthermore, "Abersili" means 'the mouth of the river Sili', but Sully Brook (assuming that that is the watercourse in question) does not reach the sea at Sully, but
16569567
List of rivers of Europe


) The choice of the source obviously has an impact. Here we attempt to list the most distant source. When that involves a tributary nearer the mouth of the river, the length of the nominal river is listed as well, if it meets the above criteria. 3) Rivers flowing into estuaries have an arbitrary end. Its channel through an estuary is usually included in the length when it is exposed at low tide. 4) The length of a watercourse through a reservoir or lake is open for interpretation. For this
19519261
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
Roi Et Province


(101) and the provincial name was written accordingly. Later, people took "๑๐๑" to mean 'one hundred and one' and have since then called it "Roi Et". Most of the province is covered by plains about 130–160 meters above sea level, drained by the Chi River. In the north are the hills of the Phu Phan mountain range. The Yang River is the major watercourse. In the south is the Mun River, which also forms the boundary with Surin. At the mouth of the
7190138
ChromeSkull: Laid to Rest 2


shown in Hollywood conversing with Spann, who assures him that they will find Jess. In a post-credits scene, the FBI is shown questioning ChromeSkull's pregnant wife, who is unaware of her husband's crimes, convinced that his long absences are due to his job. After the truth is revealed to her, the horrified Mrs. Cromeans grabs an agent's gun, and shoots herself in the mouth. The film was released Direct-to-Video on DVD and Blu-ray by Image Entertainment on Sep 20,
13219348
The Beeps


/Ep20 Sep. 19 Bouncy Bouncy Beep Beep S2/Ep21 Sep. 19 Big Beepday Bash S2/Ep22 Sep. 20 Yuk Says No S2/Ep23 Sep. 24 Wheely Helpful S2/Ep24 Sep. 25 Teeny Beep Takes Off S2/Ep25 Sep. 26 Carnival S2/Ep26 Sep. 27 Peas and Beeps S2/Ep27 Apr. 25 Stuck on You! S2/Ep28 Dec. 9 Hole Lot of Trouble S2/Ep29 Dec. 15 A Little Adventure S2/Ep30 Dec. 16 The Lost Houses S2/Ep31 May 1 Bounceberry Pie S2/Ep32 Dec. 23
14688025
Jadro


The Jadro is a watercourse in Dalmatia, Croatia that discharges to the Adriatic Sea. The upper reaches of the Jadro River, as well as its source, Jadro Spring, are protected as an ichthyological nature reserve, partly due to the presence of an endemic species of soft-mouthed trout. The headwaters of the Jadro River were the original water supply for the ancient city comprised by Diocletian's Palace (now an area within the present day city of Split). Contemporary studies indicate favourable water quality levels of the river near
12127374
Inveruglas


flowing down from Loch Sloy. The name of this watercourse is a curious back-formation, since Inveruglas means "the mouth of the Douglas". It may have acquired this name to differentiate it from the Douglas Water a few miles further south. Inveruglas Isle lies in Inveruglas Bay, an inlet of Loch Lomond. The Loch Lomond and Cowal Way starts and finishes at Inveruglas, this long distance waymarked footpath, will take you to Portavadie in the Cowal Peninsula on the east shore of Loch Fyne, 57miles of walking later
12281889
Vrbas (river)


the river Sava. The Vrbas river appears at the southern slope of the Vranica mountain near the town of Gornji Vakuf, at around above sea level and it drains central part of the northern slopes of the Dinaric mountain massif. It empties into the Sava river at around above sea level. Total length of the main watercourse is around . Average annual rainfall is around 800 l/m at the mouth of the Vrbas to the Sava river and up to 1500 l/m in the southern part of the basin. Characteristic mean
12890336
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