Kashinka Hollow [SEP] mouth of the watercourse
[{"answer": "East Branch Briar Creek", "provenance": [{"wikipedia_id": "43562721", "title": "Kashinka Hollow", "start_paragraph_id": 1, "start_character": 0, "end_paragraph_id": 1, "end_character": 113, "bleu_score": 1.0, "meta": {}, "section": "Section::::Abstract."}]}]
Kashinka Hollow


canopy coverage. Of ten sites in the Briar Creek watershed, this location has a priority rank of 1. Kashinka Hollow sometimes has high levels of lead and nitrates. The mouth of Kashinka Hollow has an elevation of above sea level. The source of the stream has an elevation of above sea level. The mouth of Kashinka Hollow lies over limestone, while the rest of the watershed's lower reaches lie on shale. Most of the watershed's middle and upper reaches lie over siltstone, but the uppermost reaches are on mudstone
15314344
Kashinka Hollow


Township. It flows west for several tenths of a mile before turning south and flowing into a valley for more than a mile. In the valley, the stream flows parallel to Kachinka Hollow Road. Upon exiting the valley, it continues south for a short distance before turning southwest near Martzville. The stream then turns south again and shortly afterwards reaches its confluence with East Branch Briar Creek. Kashinka Hollow joins East Branch Briar Creek upstream of its mouth. The discharge of Kashinka Hollow ranges from 0.12 to 41.2 cubic feet per second
15314341
East Branch Briar Creek


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


. The soil at one location on Kashinka Hollow is of the Watson Series. This soil series is a fairly well-drained and acidic silt loam. A number of other types of soil are also found in the stream's watershed. The watershed of Kashinka Hollow has an area of . The watershed is entirely in Briar Creek Township. Major roads in the stream's watershed include Evansville Road, Summer Hill Road, and Twin Church Road. Trout reproduce naturally along the entire length of Kashinka Hollow. The Run for the Diamonds
15314345
Kashinka Hollow


Kashinka Hollow is a tributary of East Branch Briar Creek in Columbia County, Pennsylvania, in the United States. It is approximately long and flows through Briar Creek Township. Its watershed has an area of . The median pH of the stream is 7.565. It has the lowest visual assessment score of any stream in the Briar Creek watershed. The stream's watershed lies over limestone, shale, siltstone, and mudstone. Trout inhabit Kashinka Hollow. Kashinka Hollow begins half a mile northwest of the community of Summer Hill in Briar Creek
15314340
Kashinka Hollow


is 34 parts per million and the maximum concentration is 86 parts per million. The median concentration is 43.5 parts per million. In a visual assessment by the Briar Creek Association for Watershed Solutions, Kashinka Hollow was given a score of 3.4 (the lowest in the Briar Creek watershed) on a scale of 1 to 10. It scored best (10 on a scale of 1 to 10) on fish barriers and it scored worst (1 on a scale of 1 to 10) on streambank stability, riparian buffering, and
15314343
Kashinka Hollow


. The median discharge is 2.325 cubic feet per second. The water temperature of the stream ranges from to , with a median of . The stream's highest temperature is the highest recorded water temperature of any stream in the watershed of Briar Creek. The electric conductance of the stream's waters ranges from 88 to 301 milli-siemens, with a median of 147 milli-siemens. The pH of Kashinka Hollow ranges between 7.14 and 8.73. The median pH of the stream is 7.565. The minimum concentration of total dissolved solids
15314342
Kashinka River


Kashinka () is a river in Kesovogorsky and Kashinsky Districts of Tver Oblast, Russia, a left tributary of the Volga River (joining the Volga at the Uglich Reservoir, near the town of Kalyazin). The length of the river is , and the area of its drainage basin is . The town of Kashin and the urban-type settlement of Kesova Gora are located along the Kashinka. The source of the Kashinka is in the swamps northwest of the village of Zadorye, at the border of Kesovogorsky and Bezhetsky Districts.
15600523
Kashinka River


It flows east, passes Kesova Gora, and in the village of Brylino turns south. It passes Kashin, where it makes a loop. The historical part of the town is located within the loop of the Kashinka. Further south, it becomes a part of the Uglich Reservoir. It joins the Volga in the village of Gorki. The drainage basin of the Kashinka includes the central part of Kashinsky District and the southern part of Kesovogorsky District, as well as minor areas in the east of bezhetsky District. The Kashinka River
15600524
Sugar Hollow Creek


its confluence with Bowman Creek. Sugar Hollow Creek joins Bowman Creek upstream of its mouth. Sugar Hollow Creek is not designated as an impaired waterbody. The concentration of alkalinity in Sugar Hollow Creek is . The elevation near the mouth of Sugar Hollow Creek is above sea level. The elevation of the creek's source is between above sea level. Sugar Hollow Creek flows through a valley known as Sugar Hollow. Near the mouth of Sugar Hollow Creek, the surficial geology mainly consists of Wisconsinan Outwash, but there is a thin strip
19896693
York Hollow


Hollow upstream of its mouth. Its watershed has an area of . The elevation near the mouth of York Hollow is above sea level. The elevation of the stream's source is between above sea level. The surficial geology in the vicinity of York Hollow mainly consists of alluvium and colluvium. However, there is also Illinoian Till and Illinoian Lag present, as well as bedrock. The surficial geology at its headwaters mainly consists of Illinoian Lag. The watershed of York Hollow has an area of . The stream's mouth is in
7466705
Cowbell Hollow


at the bottom of the mountain and reaching its confluence with White Deer Creek. Cowbell Hollow joins White Deer Creek upstream of its mouth. Cowbell Hollow is not designated as an impaired waterbody. The elevation near the mouth of Cowbell Hollow is above sea level. The elevation of the stream's source is above sea level. The watershed of Cowbell Hollow has an area of . The stream's valley is entirely within the United States Geological Survey quadrangle of Williamsport SE. The mouth of the stream is situated within of McKean Springs.
16500594
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
Bit mouthpiece


gag What it is: A mouthpiece (usually single jointed, but not always) that is hollow in the middle, making it very light. The mouthpiece is usually thicker than average. Action: The thick, hollow mouthpiece spreads out pressure, thought to make it less severe. However, this effect varies with the mouth structure of the individual horse. Some horses prefer a smaller diameter bit in their mouth because their mouths do not have room for the thick mouthpieces, and in such cases a hollow mouth bit may cause
15418113
Farr Hollow


Branch Mehoopany Creek watershed, including Farr Hollow, in 2001. Two locations were part of the study, one upstream of the mouth and another upstream of the mouth. In 2016, the Mehoopany Creek Watershed Association requested that the Pennsylvania Department of Environmental Protection undertake an evaluation of Farr Hollow, along with North Branch Mehoopany Creek and Little Mehoopany Creek. Wild trout naturally reproduce in Farr Hollow from its headwaters downstream to its mouth. The stream is classified as a Coldwater Fishery. However, in 2001, these wild brook trout populations
18396906
Bowman Hollow


the end of the valley. It then enters the floodplain of Mehoopany Creek and turns north for a short distance before reaching its confluence with Mehoopany Creek. Bowman Hollow joins Mehoopany Creek upstream of its mouth. The elevation near the mouth of Bowman Hollow is above sea level. The elevation near the stream's source is above sea level. The stream is located within a U-shaped hollow and is surrounded on three sides by cliffs. Bowman Hollow has a waterfall known as the Bowman Hollow Falls. The waterfall drops approximately into
14064520
Stranger Hollow


over the stream. Stranger Hollow begins on Catawissa Mountain in Beaver Township. It flows east for a few tenths of a mile and enters a valley. It eventually turns northeast for another few tenths of a mile before reaching its confluence with Catawissa Creek. Stranger Hollow joins Catawissa Creek upstream of its mouth. Stranger Hollow has no tributaries, named or unnamed. Stranger Hollow is considered to be impaired by atmospheric deposition due to pH. The pH of the stream is unknown. The elevation near the mouth of Stranger Hollow is above sea
20986991
Kesovogorsky District


of Kesova Gora. Population: 8,199 (2010 Census); The population of Kesova Gora accounts for 47.3% of the district's total population. The whole area of the district belongs to the drainage basin of the Volga. The areas in the north and the east of the district belong to the drainage basin of the Korozhechna River. The source of the Korozhechna lies in the northwestern part of the district. The rivers in the center and the west of the district drain into the Kashinka River. The Kashinka crosses the district
5970585
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
Fallow Hollow


a slightly longer distance before turning northwest and beginning to flow parallel to Ripple Brook Road. A short distance downstream, it reaches its confluence with Coles Creek. Fallow Hollow joins Coles Creek upstream of its mouth. The elevation near the mouth of Fallow Hollow is above sea level. The elevation at the source of the stream is between and . The watershed of Fallow Hollow has an area of . The entire length of the stream is on closed and private land. There are numerous types of habitats in the watershed of Fallow Hollow
18913853
Fox Hollow (Mehoopany Creek)


south for several hundred feet before turning southeast again for a few tenths of a mile. It then turns east-southeast for several hundred feet before reaching its confluence with Mehoopany Creek. Fox Hollow is approximately long. The stream joins Mehoopany Creek upstream of its mouth. The elevation near the mouth of Fox Hollow is above sea level. The elevation near the source of Fox Hollow is above sea level. Fox Hollow is located near a mountain known as Little Round Top. The watershed of Fox Hollow has an area of .
8133590
Hess Hollow


valley. After more than a mile, the stream turns southwest and then abruptly turns southeast, crossing Pennsylvania Route 487. Almost immediately afterwards, it reaches its confluence with Coles Creek. Hess Hollow joins Coles Creek upstream of its mouth. The elevation near the mouth of Hess Hollow is above sea level. The elevation of the stream's source is just over above sea level. Hess Hollow does some meandering. Fritz Hill is situated to the west of the hollow. There is a pond at the headwaters of the stream,
18973146
Tinker Hollow


. The watershed of Tinker Hollow has an area of . The stream is entirely within the United States Geological Survey quadrangle of Clifford. Its mouth is located near Burdick Corners. A lake known as Coterell Lake is at the headwaters of an unnamed tributary to Tinker Hollow. It has an area of approximately . Wild trout naturally reproduce in Tinker Hollow from its headwaters downstream to its mouth. The designated use of the stream is aquatic life. The valley of Tinker Hollow was entered into the Geographic Names Information System on August 2,
7206612
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
10473368
Rogers Hollow


west-northwest for more than a mile, reaching the end of its valley and crossing Pennsylvania Route 87. The stream then turns west-northwest along the base of Mehoopany Mountain, gradually turning north-northwest over the next few tenths of a mile before reaching its confluence with Mehoopany Creek. Rogers Hollow is approximately long. The stream joins Mehoopany Creek upstream of its mouth. The elevation near the mouth of Rogers Hollow is above sea level, while the elevation near the mouth of the valley is above sea level. The
9590105
Battle of Newtown


the Chemung River, was a mile long at its crest, which rose above the road at its base leading into Newtown. The slope of the hill was covered with pine and dense growth of shrub oak. Hoffman Hollow, a marshy area of small hillocks and thick stands of trees, was just to the east of the hill. A small watercourse, called Baldwin Creek, ran through the hollow and emptied into the Chemung River (referred to as the Cayuga branch in Sullivan's reports). The creek followed the hill
5894220
Broad Hollow Run


-northeast and north for a few tenths of a mile. In this reach, the valley of the stream becomes much shallower on one side. The stream then turns north-northeast again. Several tenths of a mile further downstream, it enters the valley of Bowman Creek and reaches its confluence with Bowman Creek. Broad Hollow Run joins Bowman Creek upstream of its mouth. The elevation near the mouth of Broad Hollow Run is above sea level. The elevation near the source of Broad Hollow Run is between above sea level.
1534342
Thurston Hollow


a mile, passing through a pond, receiving an unnamed tributary from the left, and enters a valley. The stream then turns nearly due north for several tenths of a mile and passes through another pond before turning east-northeast. Several hundred feet further downstream, it reaches its confluence with Moneypenny Creek. Thurston Hollow joins Moneypenny Creek upstream of its mouth. Thurston Hollow is not designated as an impaired waterbody. The elevation near the mouth of Thurston Hollow is above sea level. The elevation of the stream's source is
18895355
Benson Hollow


a valley to the west of Cedar Ledge in Eaton Township. It flows south-southeast for a few tenths of a mile before turning east-southeast. Several tenths of a mile further downstream, the stream reaches its confluence with Bowman Creek. Benson Hollow joins Bowman Creek upstream of its mouth. Benson Hollow is not designated as an impaired waterbody. The elevation near the mouth of Benson Hollow is above sea level. The elevation of the stream's source is between above sea level. During the Ice Age, glacial meltwater
19545975
Pothole (landform)


The Earth scientists, who study rivers and streams, define a pothole as a smooth, bowl-shaped or cylindrical hollow, generally deeper than wide, found carved into the rocky bed of a watercourse. Other names used for riverine potholes are pot, (stream) kettle, giant's kettle, evorsion, hollow, rock mill, churn hole, eddy mill, and kolk. Although somewhat related to a pothole in origin, a plunge pool (or plunge basin or waterfall lake) is the deep depression in a stream
16988440
Farr Hollow


Township. It flows southeast and then south for a few tenths of a mile before entering North Branch Township. Here, the stream flows south-southeast through a progressively narrowing valley between Douglas Hill and Cedar Hill. After a few miles, it reaches its confluence with North Branch Mehoopany Creek. Farr Hollow joins North Branch Mehoopany Creek upstream of its mouth. Farr Hollow is not designated as an impaired waterbody. In 2001, measurements of pH near the source and mouth of Farr Hollow were 7.4 and 7.0, respectively. Measurements
18396901
Douglas Hollow


The stream passes through a small unnamed pond and flows south for several tenths of a mile before turning south-southeast for several tenths of a mile. It then turns south and crosses Pennsylvania Route 87 before reaching its confluence with North Branch Mehoopany Creek. Douglas Hollow joins North Branch Mehoopany Creek upstream of its mouth. Douglas Hollow is not designated as an impaired waterbody. At a site upstream of its mouth, Douglas Hollow was observed in 2001 to have a pH of 7.2 and an alkalinity concentration of . The water hardness was
18397569
Tinker Hollow


for a few tenths of a mile before turning north-northwest, receiving an unnamed tributary from the right and continuing to flow northwest. Several tenths of a mile further downstream, the stream reaches the end of its valley and reaches its confluence with Little Creek. Tinker Hollow is approximately long. The stream joins Little Creek upstream of its mouth. The elevation near the mouth of Tinker Hollow is above sea level. The elevation near the stream's source is above sea level. The surficial geology alongside Tinker Hollow in its lower
7206610
Karnes Hollow


short distance before turning north-northeast for several tenths of a mile. The stream then turns northeast for several tenths of a mile, entering Benton Township. It then turns east and reaches its confluence with Fishing Creek a few hundred feet further downstream. Karnes Hollow joins Fishing Creek upstream of its mouth. The elevation near the mouth of Karnes Hollow is above sea level. The elevation of the stream's source is between above sea level. Along most of the length of Karnes Hollow, the surficial geology features colluvium. However
8791624
Pescadero Creek


" controlled the area from Bean Hollow Creek southward to Año Nuevo Creek and inland to Butano Ridge. The "Oljon" controlled from the lower San Gregorio Creek drainage southward to Bean Hollow Creek, including the lower Pescadero and Butano drainages. The "Cotogen" held the land in and around Purisima Creek. When the Portolà Expedition traveled on horseback along the immediate coast on October 24, 1769, Padre Juan Crespí wrote, "Only in the watercourses are any trees to be seen; elsewhere we saw nothing but grass, and
10016814
Hill 60, Port Kembla


is now largely re-shaped by the formation of a wetland area and "frog hollow". This landscaping has disturbed Aboriginal shell deposits adjacent to this feature. A small sandy beach between MM Beach and Boilers Point contains Aboriginal shell deposits at the interface of the beach and the toe of slope below the watercourse and "frog hollow". Other Aboriginal shell deposits are located at the interface of the upper elevations of the rock walls around Boilers Point and the soil deposits on the Point itself. Some of these have been exposed
752153
Deep Hollow (West Branch Fishing Creek tributary)


and its valley becomes much deeper. The stream then turns south-southwest for a few tenths of a mile. It then turns south-southeast again, crossing Fishing Creek Road and reaching its confluence with West Branch Fishing Creek. Deep Hollow joins West Branch Fishing Creek upstream of its mouth. The elevation near the mouth of Deep Hollow is above sea level. The elevation near the stream's source is just over above sea level. Nearly all of the surficial geology in the valley of Deep Hollow is on bedrock consisting of
7342865
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
Farr Hollow


of alkalinity were , with the higher value in the upper reaches. The total water hardness of the stream was near the source and near the mouth, while the specific conductance at these locations was 266 and 135 umhos, respectively. In August 2001, when the air temperature nearby was , the water temperature of the stream was in its lower reaches and in its upper reaches. The elevation near the mouth of Far Hollow is above sea level. The elevation near the stream's source is above sea level. Farr Hollow is
18396902
Sugar Hollow Creek


of alluvium along the creek itself. Slightly further upstream, some Wisconsinan Till is present. During the Ice Age, glacial meltwater from the valley of Sugar Hollow Creek helped to create a large delta in the valley of Bowman Creek. This delta has since been divided by stream action. There are two "deeply notched" cols at the headwaters of the creek. There is an abandoned and semi-reclaimed pit at the mouth of the creek's valley. The watershed of Sugar Hollow Creek has an area of . The mouth
19896694
Negro Hollow


concentration of alkalinity in the stream is 4 milligrams per liter. The total concentration of water hardness is 7 milligrams per liter. At 12:20 P.M. on July 22, 1997, the air temperature in the vicinity of Negro Hollow upstream of its mouth was . The water temperature of the stream at this time and location was . The specific conductivity of the stream's waters is 20 micromhos. The elevation near the mouth of Negro Hollow is above sea level. The elevation of the stream's source is approximately above sea level. The
2638117
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
Soldier Hollow (Utah)


Soldier Hollow is a small hollow in the Wasatch Range that is located within the Wasatch Mountain State Park in northwestern Wasatch County, Utah, United States. The hollow was formerly a Native American encampment and was later used by a group of Army surveyors in the 1850s. While the hollow is fairly small, it is most notable for the Soldier Hollow winter sports venue that is located at the mouth of the hollow (and that was named after the hollow). The venue was created for the 2002 Winter Olympics and hosted the
11331650
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
Davis Hollow


The stream then turns southwest for a few tenths of a mile, leaving the valley and entering a plain. It then turns southwest and crosses Pennsylvania Route 487 after several tenths of a mile. At this point, it turns south-southwest and reaches its confluence with Fishing Creek a short distance further downstream. Davis Hollow joins Fishing Creek upstream of its mouth. The elevation near the mouth of Davis Hollow is above sea level. The elevation of the stream's source is between above sea level. There are two patches of
8791309
Bee Sellers Hollow


sandstone and shale. The valley of Karnes Hollow is in the watershed of Bee Sellers Hollow. Bee Sellers Hollow is not considered to be impaired. The watershed of Bee Sellers Hollow has an area of . The mouth of the stream's valley is in the United States Geological Survey quadrangle of Stillwater. However, its source is in the quadrangle of Benton. Bee Sellers Hollow is mainly located in the western part of the borough of Stillwater. The stream is entirely within that borough. The valley of Bee Sellers Hollow was entered
8997584
Bee Sellers Hollow


of a mile before turning east-southeast. Several tenths of a mile further downstream, the stream flows away from Beecellar Road and leaves its valley. It then turns south-southeast for several tenths of a mile, crossing Kline Road. After this, it turns east-southeast for a few hundred feet, crossing Pennsylvania Route 487 and reaching its confluence with Fishing Creek near the southern border of Stillwater. Bee Sellers Hollow joins Fishing Creek upstream of its mouth. The elevation near the mouth of Bee Sellers Hollow is above
8997582
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
Bear Hollow Creek


Hollow Creek begins in a small pond near Bear Hollow Road in Lake Township. It flows south-southeast alongside Bear Hollow Road in a valley known as Bear Hollow for approximately a mile. The creek then turns southeast and continues flowing alongside Bear Hollow Road as its valley broadens. After approximately a mile, it reaches its confluence with Harveys Creek. The elevation near the mouth of Bear Hollow Creek is above sea level. The elevation of the creek's source is between above sea level. Bear Hollow, the valley of Bear
1694346
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
Panther Run


across from Dogback Mountain. Panther Run joins North Branch Buffalo Creek upstream of its mouth. Panther Run has one named tributary, which is known as Slide Hollow. Slide Hollow joins Panther Run upstream of its mouth and its watershed has an area of . The elevation near the mouth of Panther Run is above sea level. The elevation of the stream's source is between above sea level. The headwaters of Panther Run are in a spring on the forest floor. The stream is a "sizable stream" in some reaches.
12117899
Beartrap Hollow


Hollow in its lower reaches. The elevation near the mouth of Beartrap Hollow is above sea level. The elevation near the stream's source is above sea level. The headwaters of Beartrap Hollow are on a ridge known as South White Deer Ridge. The ridge is relatively steep in the stream's upper reaches, but becomes less steep towards the lower reaches of the stream. It flows down into the broad valley of White Deer Hole Creek. Beartrap Hollow is in the Ridge and Valley Freestone region. Beartrap Hollow is not designated
16714703
Negro Hollow


east-northeast for a few tenths of a mile and reaches its confluence with Messers Run near the Blue Head Reservoir. Negro Hollow joins Messers Run upstream of its mouth. Negro Hollow has no named tributaries. However it has one unnamed tributary. It is known as "Trib 27607 To "Negro Hollow"". This tributary flows through Mahanoy Township and Delano Township. Negro Hollow is an infertile and acidic stream. It has the potential to be affected by acid precipitation. The pH of Negro Hollow is 6.6. The
2638116
Kline Hollow Run


The stream's valley deepens as it flows south for more than a mile, passing by Huckleberry Ridge. Near the southern edge of Huckleberry Ridge, the stream reaches its confluence with Devil Hole Run. The elevation near the mouth of Kline Hollow Run is above sea level. The elevation of the stream's source is between and . Kline Hollow Run is surrounded by a hollow known as Kline Hollow. Stormwater runoff from a sawmill discharges into the stream as of 2001. Kline Hollow Run is in the United States Geological Survey quadrangle
5855512
Green Creek (Fishing Creek tributary)


heads in a southerly direction for several tenths of a mile before turning west-southwest. Several tenths of a mile further downstream, the creek abruptly turns south-southeast and almost immediately reaches its confluence with Fishing Creek. Green Creek joins Fishing Creek upstream of the latter creek's mouth. Green Creek has three named tributaries: Mud Run, Rickard Hollow, and Little Green Creek. Mud Run joins Green Creek upstream of its mouth and drains an area of . Rickard Hollow joins Green Creek upstream of its mouth and drains an
20730587
Laurel Run (Mill Creek tributary)


of a mile. Laurel Run joins Mill Creek upstream of its mouth. Laurel Run has one named tributary, which is known as Deep Hollow. Deep Hollow joins Laurel Run upstream of its mouth. Its watershed has an area of . The peak annual discharge of Laurel Run at its mouth has a 10 percent chance of reaching per second. It has a 2 percent chance of reaching per second and a 1 percent chance of reaching per second. The peak annual discharge has a 0.2 percent chance of reaching per second. The
4811184
Little Creek (East Branch Tunkhannock Creek tributary)


approximately long. The creek joins East Branch Tunkhannock Creek upstream of its mouth. Little Creek has one unofficially named tributary: Tinker Hollow, which is named for the valley through which it flows. Tinker Hollow joins Little Creek upstream of its mouth, near Burdick Corners, and drains an area of . The elevation near the mouth of Little Creek is above sea level. The elevation near the creek's source is above sea level. The surficial geology along the lower reaches of Little Creek mainly consists of alluvium, though there is
7103467
Rickard Hollow


. Rickard Hollow has no named tributaries. However, it does have two unnamed tributaries. The elevation near the mouth of Rickard Hollow is above sea level. The elevation of the stream's source is between and above sea level. The stream is close to the Greenwood Valley and to another valley known as Davis Hollow. The Greenwood Township Municipal Authority has a permit to discharge sewage into Rickard Hollow. It is waived by the United States Department of Environmental Protection. This is considered to be a minor discharge, with a discharge
5968634
Davis Hollow


Hollow, the Wisconsinan glacial terminus descends over the course of ( per mile). The watershed of Davis Hollow has an area of . The mouth of the stream is in the United States Geological Survey quadrangle of Benton. However, its source is in the quadrangle of Stillwater. Davis Hollow was entered into the Geographic Names Information System on August 2, 1979. Its identifier in the Geographic Names Information System is 1172989. Davis Hollow is an unnamed stream that takes the name of the valley it flows through. The valley is
8791311
York Hollow


It flows southeast for more than a mile alongside Pennsylvania Route 239 before crossing the highway and turning east. It then receives the tributary Schultz Hollow from the left and turns southeast for several tenths of a mile, entering Sugarloaf Township. The stream then receives an unnamed tributary from the right. A few tenths of a mile further downstream, it reaches its confluence with West Creek. York Hollow joins West Creek upstream of its mouth. York Hollow has one named tributary, which is known as Schultz Hollow. Schultz Hollow joins York
7466704
Slide Hollow


Geological Survey quadrangle of Hartleton. The valley of Slide Hollow was entered into the Geographic Names Information System on August 2, 1979. Its identifier in the Geographic Names Information System is 1187806. Slide Hollow is an unofficially named stream that is named after the valley through which it flows. The stream is also known as Slide Hollow Run. Wild trout naturally reproduce in Slide Hollow from its headwaters downstream to its mouth. In the 1930s, the stream was known to be a good brook trout stream. It was also stocked with
12118228
Doubleup Hollow


Doubleup Hollow is a valley in the Black Mountains in Beaver and Iron County, Utah. Its mouth lies at an elevation of 6,450 feet / 1,966 meters. It heads at , at an elevation of 7,680 feet, in Beaver County. Doubleup Hollow is named for the practice that the Forty-niners and Mormon pioneers made of doubling up their wagon teams of oxen or mules to pull their wagons over the steep ridge between Doubleup Hollow and California Hollow where the Mormon Road ran between Greenville, Utah and Muley Point, over the
14241045
Yellow-tailed black cockatoo


. Hollows can be deep and wide, with a base of woodchips. A chance felling of a eucalypt known to have been used as a nesting tree near Scottsdale in northeastern Tasmania allowed accurate measurements to be made, yielding a hollow measuring high by wide at the mouth, and at least deep, in a tree which measured in diameter below the hollow. Both the male and female prepare the hollow for breeding, which involves peeling or scraping off wood shavings from the inside the hollow to prepare bedding for the eggs. Gum
797712
Octocorallia


tentacles and mouth, projecting about the surface. The mouth is slit-like, with a single ciliated groove, or "siphonoglyph", at one side to help control water flow. It opens into a tubular pharynx that projects down into a gastrovascular cavity that occupies the hollow interior. The pharynx is surrounded by eight radial partitions, or mesenteries, that divide the upper part of the gastrovascular cavity into chambers, one of which connects to the hollow space inside each tentacle. The gonads are located near the base of each
10487213
Vézère


should not be confused in the Dordogne with the Upper Vézère, or Auvézère, a tributary of the "L'Isle", 10 kilometers east of Périgueux. The name Vézère comes, according to some scholars, from the ancient hydronym Vizara or Izara, formed by two contiguous Ligurian roots. The first, "viz" or "iz", and the second "ara". "Viz" or "Iz" means a "hollow Valley", and "ara" means a "watercourse", the word "Vézère
292044
Hypostomus


wood; however, many species may be found among rocks in piedmont to mountain streams with moderate to swift flow. Members of this genus may be found over a range of substrates such mud, detritus, gravel, and sand. Many species spawn in hollows dug into mud banks or within hollow logs. As in all loricariids, these species have a suckermouth. They use their mouth as well as the pectoral, pelvic and caudal fin areas, to interact with the rocky river-bottom. The comb-toothed inferior mouth
11116433
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
Long Hollow (Catawissa Creek tributary)


air temperature in the vicinity of Long Hollow was . The water temperature of the stream at that time was . The elevation near the mouth of Long Hollow is above sea level. The elevation of the stream's source is between and . The lower reaches of Long Hollow are on rock of the Mauch Chunk Formation and the upper reaches are on rock of the Pocono Formation. The stream's unnamed tributary is on rock of the Spechty Kopf Formation and the Buddys Run Member of the Catskill Formation. The main soils in the watershed
20791855
Hammersley Fork


ranged from . The sediment load in Hammersley Fork is per year. The nitrogen load is per year, while the phosphorus load is less than half a pound per acre per year. Between the mouth of Dry Hollow and the mouth of Bunnell Run, the waters of Hammersley Fork are a Rosgen type F and a Rosgen type C stream. The upper part of the stretch of the stream between Dry Hollow and Nelson Branch is a Rosgen type C stream. The middle part of the stretch is a Rosgen type B stream and
17509659
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
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
10473369
Dutch Hollow Lake


by Branigar Lake Properties of Wisconsin. Fish varieties were initially stocked into Dutch Hollow Lake. Now the lake has a balance of Northern Pike, Walleye, Large Mouth Bass, Yellow Perch, Crappie, Bluegill, and other Sunfish. Dutch Hollow Lake (Lat. 43 degrees/Long. 90 degrees) has an elevation of 951 feet (290 m). It is northwest of the city of Reedsburg, with the city of Wisconsin Dells thirty minutes away. The lake is and in depth. Dutch Hollow Lake is a
11267322
Broad Hollow Run


The surficial geology near the mouth of Broad Hollow Run consists of alluvium (which contains stratified sand, silt, gravel, and some boulders) and a till known as Wisconsinan Till. Further upstream, the surficial geology consists of Wisconsinan Till and alluvial fan, some of which is underlain by glacial lake clays. The surficial geology at the headwaters consists entirely of Wisconsinan Till. Broad Hollow Run is in the vicinity of the North Mountain region. The watershed of Broad Hollow Run has an area of . The stream is entirely within
1534343
Beartrap Hollow


as an impaired waterbody. The watershed of Beartrap Hollow has an area of . The stream is entirely within the United States Geological Survey quadrangle of Williamsport SE. Its mouth is located near Elmsport. Beartrap Hollow is being considered by the Pennsylvania Fish and Boat Commission for wild trout designation. The valley of Beartrap Hollow was entered into the Geographic Names Information System on August 2, 1979. Its identifier in the Geographic Names Information System is 1168978. The stream does not have a name of its own, but instead takes its name
16714704
Kline Hollow Run


. Wild trout naturally reproduce in Kline Hollow Run between its headwaters and its mouth. The stream is considered to be an Exceptional Value stream. It is on the Pennsylvania Fish and Boat Commission's list of wild trout streams. Hemlock trees are one of the dominant tree species in the vicinity of Kline Hollow Run. There are also small and herbaceous openings along the stream. These openings are likely to contain wet meadows, with various sedges, shrubs, and wetland plants. The area surrounding Kline Hollow Run is described as a
5855515
Soldier Hollow


featuring mountain biking and golfing in the summer. On May 1, 2016, the venue operation contract transferred from the Soldier Hollow Legacy Foundation to the Utah Olympic Legacy Foundation, which owns and operates several Olympic and Paralympic legacy venues elsewhere in the state. Soldier Hollow is located in the southeastern-most part of Wasatch Mountain State Park, a nature preserve created in 1961, which became a state park in 1968. The venue received its name from the hollow at the mouth of which it is located. Prior to becoming a
9103368
Rogers Hollow


elevation near the creek's source is above sea level. The valley of Rogers Hollow is relatively broad for its length. The mountains that border it on three sides form a U-shaped boundary. The watershed of Rogers Hollow has an area of . The stream is entirely within the United States Geological Survey quadrangle of Meshoppen. Its mouth is located near Forkston. The entirety of Rogers Hollow is classified as a Coldwater Fishery. It is one of only three named direct tributaries of Mehoopany Creek to have this classification. The valley
9590106
East Branch Raven Creek


as Stine Hollow. Stine Hollow joins East Branch Raven Creek upstream of its mouth. The stream's watershed has an area of . The average daily discharge of East Branch Raven Creek is estimated to be 3.63 cubic feet per second. The elevation near the mouth of East Branch Raven Creek is above sea level. The elevation of the creek's source is between above sea level. The percentage of runs, riffles, and pools have been measured on a section of East Branch Raven Creek that is long. A total of 47
15202418
Combe


A combe (; also spelled coombe or coomb and, in place names, comb) can refer either to a steep, narrow valley, or to a small valley or large hollow on the side of a hill; in any case, it is often understood simply to mean a small valley through which a watercourse "does not" run. The word "combe" derives from Old English "cumb", of the same meaning, and is unrelated to the English word "comb". It derives ultimately from the same
2056533
Long Hollow (Catawissa Creek tributary)


Long Hollow begins on Catawissa Mountain in Roaring Creek Township. It flows east for a few tenths of a mile. The stream then enters Beaver Township. It continues east and after a sort distance, the stream receives an unnamed tributary. It then continues roughly east for considerably more than a mile in a deep valley. At the end of the valley, the stream reaches its confluence with Catawissa Creek. Long Hollow joins Catawissa Creek upstream of its mouth. Long Hollow has one unnamed tributary. It is known as "Trib
20791853
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
West Branch Run


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


The Hilton Brook or Sutton Brook is a tributary of the River Dove in Derbyshire, England, and is 26 kilometres (16 miles) long. Like many watercourses in the area, it has multiple names, often being named locally after the village it flows past. The source of the brook is to the north of Hulland village, where it is known as the Hulland-Hollow brook, it flows south to become the Spinneyford brook, this changes to the Brailsford brook, after the confluence with the Bradley brook. It
21790442
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
Bear Hollow Creek


Company. The creek's water made up one thirtieth of the company's water supply. Wild trout naturally reproduce in Bear Hollow Creek from its headwaters downstream to its mouth. Bear Hollow is listed on the Luzerne County Natural Areas Inventory. The hollow contains an eastern hemlock forest and has a very high level of amphibian biodiversity. Amphibian species that inhabit the area include northern red salamander, northern dusky salamander, redback salamander, red-spotted newt, spotted salamander, and spring peeper. Insect species such as Comet Darner, Lance
1694349
The Dell, Leamington Spa


The Dell is a small park in the Milverton area of Leamington Spa, Warwickshire, England. Although it is not well known nationally (like The Jephson Gardens) or regionally (like Newbold Comyn), it is a well used and popular park amongst Leamingtonians themselves. The park takes its name from the fact that it is situated in a small sunken hollow, or dell. Up until the 1820s, the Dell was simply part of the course of a local watercourse, the Bins Brook. As the town grew, however
823085
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
Slide Hollow


concentrations above the detection limit was hafnium (). However, the concentration of lead was and the uranium concentration was . The silicon concentration was . However, the arsenic concentration was only and the antimony concentration was . The concentration of bromine was , while the iodine concentration was . The elevation near the mouth of Slide Hollow is above sea level. The elevation of the stream's source is between above sea level. The watershed of Slide Hollow has an area of . The stream and its valley are entirely within the United States
12118227
Bushells Building


agency of the Government of New South Wales. It was added to the New South Wales State Heritage Register on 10 May 2002. The land that was to become the site of the Bushells building formed part of a locale known as Frog Hollow, and area of simple terraces and cottages. The suggestion of a watercourse in the early plans may explain the nickname, which appears to be given to many marshy localities in Sydney and other towns in Australia. From the vicinity of the intersection of Grosvenor and Cumberland Streets originated a small
12989906
The Coombe, Dublin


The Coombe () is a historic street in the south inner city of Dublin, Ireland. It was originally a hollow or valley where a tributary of the River Poddle, the Coombe Stream or Commons Water, ran. The name is sometimes used for the broader area around, in which the Poddle and its related watercourses featured strongly. In the late 17th century economic development started in order to house the clothiers who were moving into this then suburban area. Woolen manufacture was set up by settlers from England, while many French
14274528
Bowen Park, Brisbane


1863 as a park for public pleasure in inner-city Brisbane, an area under pressure to accommodate increased urban development and consolidation. The Queensland Government granted land to the Queensland Acclimatisation Society (QAS) in two parcels in 1863 and 1866, this site was then well out of town on the edge of development and had been worked as a brickfield. Part of this land lay along the watercourse of York's Hollow and the remainder was remnant bushland and brickworks. The site was not ideal for establishing a garden, the soil
20059887
Moksha River


flow of water is observed below the confluence of the hollow from the holy spring, where a small extension of the channel also forms. A true watercourse flows towards Vision in a poorly developed channel. In some places, the banks collapse in the face of the knocking out of them groundwater flowing into the channel. The bottom of the lowland where the stream flows is swamped. Along the banks of the stream, shrubs of willows, thickets of broadleaf cattails, reeds of forest and some other moisture-loving plants grow in
3515994
Słupsk


's area is covered by forests, while is used for agricultural purposes. Słupsk is rich in natural water bodies. There are more than twenty ponds, mostly former meanders of the Słupia, within the city limits. There are also several streams, irrigation canals (generally unused and abandoned) and a leat. Except in the city centre, all these watercourses are unregulated. There is generally little human influence on landform features visible within the city limits. However, in the northwestern part of the city there is a huge hollow
38124
Buffalo National River


mussels, and aquatic plants. The Buffalo National River is a popular camping, canoeing, and fishing destination. Visitors may bring their own canoes or rent from several independent concessioners. Camping is generally allowed throughout the park with the following exceptions: the Hemmed-in-Hollow area, on Big Bluff, in historical structures, on private property within the park, or within of any trail or watercourse. Camping is, however, permitted on gravel bars and sand bars along the river. In addition, the National Park Service
7190398
Elegant parrot


is found in two disjunct regions, one across southwestern Australia from Moora in the north to Merredin and Esperance in the east, and in southeastern South Australia (including Kangaroo Island) north to Marree, and east into western Victoria. Breeding season is anywhere from July to November or after rainfall, with one or occasionally two broods raised depending on rainfall. A hollow higher than above the ground in a tree, usually a eucalypt along a watercourse or stringybark forest, is utilised for nesting, and a clutch of four to six
8338405