Kline Hollow Run [SEP] mouth of the watercourse
[{"answer": "Devil Hole Run", "provenance": [{"wikipedia_id": "44255249", "title": "Kline Hollow Run", "start_paragraph_id": 1, "start_character": 0, "end_paragraph_id": 1, "end_character": 128, "bleu_score": 1.0, "meta": {}, "section": "Section::::Abstract."}]}]
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
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
Kline Hollow Run


important. The water temperature of Kline Hollow Run is cooled by nearby shrubbery. This causes the stream to have a relatively high concentration of dissolved oxygen. Kline Hollow Run was entered into the Geographic Names Information System on August 2, 1979. Its identifier in the Geographic Names Information System is 1178586. Kline Hollow Run is named after the Kline Family. Kline Hollow, the hollow through which the stream flows, has the same etymology. The Columbia County Natural Areas Inventory advises against extensive logging in the vicinity of Devil Hole Run
5855514
Kline Hollow Run


Kline Hollow Run is a tributary of Devil Hole Run in Lycoming County and Columbia County, in Pennsylvania, in the United States. It is approximately long and flows through Jordan Township in Lycoming County and Pine Township in Columbia County. The stream is mostly surrounded by forested land and it is part of a Locally Significant Area listed on the Columbia County Natural Areas Inventory. Plantlife common in the vicinity of the stream include hemlock trees and trout inhabit the stream itself. The stream is considered to be an Exceptional Value stream. Kline
5855510
Devil Hole Run


Devil Hole Run Road. It then exits its valley and turns southeast. A short distance further downstream, it reaches its confluence with Little Fishing Creek on the border between Pine Township and Greenwood Township. Kline Hollow Run, which joins Devil Hole Run in the latter stream's lower reaches, is the only named tributary of Devil Hole Run. The elevation near the mouth of Devil Hole Run is above sea level. The elevation of the stream's source is between and above sea level. The area that surrounds Devil Hole Run
5692702
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
Kline Hollow Run


Hollow Run begins in a valley in Jordan Township, Lycoming County, a short distance south of Richarts Grove. It flows south for a few hundred feet before turning southwest. The stream then turns south-southeast and passes through a pond. Several tenths of a mile further downstream, it exits Jordan Township and Lycoming County. Upon exiting Lycoming County, Kline Hollow Run enters Pine Township, Columbia County. It continues flowing south-southeast for more than a mile, receiving an unnamed tributary, before eventually gradually turning south.
5855511
Messers Run


tenths of a mile later, it exits Kline Township and enters East Union Township. In East Union Township, the stream turns northwest and receives the tributary Negro Hollow. It then turns northeast for a few hundred feet and passes near the Blue Head Reservoir. The stream then turns northwest and flows for slightly less than a mile until it reaches its confluence with Catawissa Creek. Messers Run joins Catawissa Creek upstream of its mouth. Messers Run has three tributaries, only one of which is named. The named tributary is known as
2192053
Kline Hollow Run


of Benton. Additionally, the stream is located in the northern part of Pine Township and is approximately one mile (two kilometers) west of the community of Derrs. The stream is within a large and mostly untouched block of forest. The only roads that are close to the stream are small private roads. Kline Hollow Run is part of a Locally Significant Area in Columbia County. The area's county priority rank is five on a scale of one to five, with one being the most important and five being the least
5855513
Messers Run


Negro Hollow and it flows through Delano Township, Kline Township, and East Union Township. The unnamed tributaries are known as "Trib 27610 To Messers Run" and "Trib 27609 To Messers Run". The former is entirely in Kline Township, while the latter flows through Delano Township and Kline Township. Messers Run is infertile and acidic upstream of the Lofty Reservoir. The stream has the potential to be affected by acid precipitation in this part of it. The stream also has these attributes from the Lofty Reservoir downstream to the
2192054
Negro Hollow


Negro Hollow (also known as Negro Hollow Run) is the only named tributary of Messers Run in Schuylkill County, Pennsylvania, in the United States. It is approximately long and flows through Delano Township, Kline Township, and East Union Township. The watershed of the stream has an area of . The stream is considered to be a High-Quality Coldwater Fishery and Class A Wild Trout Waters. Two species of fish inhabit the stream, including brook trout. The main rock formations in the stream's watershed are the Mauch
2638114
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
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
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
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
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
Devil Hole Run


Pine Township, a few hundred feet from the border between Columbia County and Lycoming County. It flows south-southeast for a few tenths of a mile before turning south. After a few hundred feet, the stream turns south-southeast again, crossing Wolf House Hollow Road. Its valley becomes deeper as it continues downstream. After at least two miles (three kilometers), it receives its only named tributary, Kline Hollow Run. At this point, the stream turns south for a few tenths of a mile, crossing
5692701
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
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
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
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
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
Fowler Hollow Run


Fowler Hollow Run is a stream in Perry County, Pennsylvania, in the United States. It is part of the Susquehanna River watershed as it is a tributary of Shultz Creek, which is a tributary of Sherman Creek, which flows into the Susquehanna. The drainage basin for Fowler Hollow Run is 5.59 square miles (14.48 km²) and enters Shultz Creek 3.90 miles (6.28 km) from its mouth on Sherman Creek. It is 48.14 miles (77.47 km) along Sherman Creek to the lower Susquehanna River. The 6.2 mile
327857
Messers Run


Messers Run is a tributary of Catawissa Creek in Schuylkill County, Pennsylvania, in the United States. It is approximately long and flows through Kline Township and East Union Township. The only named tributary of the stream is Negro Hollow, but it has two unnamed tributaries. The creek has some alkalinity, but is slightly acidic. The main rock formations in the watershed of it are the Mauch Chunk Formation and the Pottsville Formation. The main soils in the watershed are the Leck Kill soil and the Hazleton soil. The watershed of
2192050
White Deer Creek


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


west-southwest and almost immediately enters Hartley Township. It continues flowing west-southwest for several tenths of a mile. The stream then turns west-northwest for a short distance before turning southwest. Several tenths of a mile further downstream, it reaches its confluence with Panther Run at The Hook. Slide Hollow joins Panther Run upstream of its mouth. The field pH of Slide Hollow was once measured to be 6.85, while the lab pH was measured to be 6.51. The concentration of aluminum in the stream was measured to
12118224
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
Messers Run


throughout the rest of the watershed. Messers Run is flanked by areas prone to flooding during a 100 year flood from the mouth of Negro Hollow upstream to its headwaters. Negro Hollow and its unnamed tributaries are also surrounded by areas prone to flooding during a 100-year flood for much of their length. Both of the unnamed tributaries of Messers Run are surrounded by such areas for the majority of their length. Messers Run has a width of upstream of the Lofty Reservoir. The gradient of the stream at this location is . Its width
2192060
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
The Devil's Nose


The Devil's Nose is a steep but small mountain ridge that spans from southwest to northeast between the Little Cacapon and Potomac rivers in northeastern Hampshire County, West Virginia. From its southern end near Neals Run on Johnsons Hollow, The Nose rises from the landscape curving along a bend in the Little Cacapon River. From Johnsons Hollow, The Nose continues northeast flanked to its west by a plain at the Little Cacapon's mouth into the Potomac, and to its east by The Nose Hollow and Neals Run-Paw Paw Road (
3114740
Shepman Run


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


a water supply as early as the early 1900s. Messers Run was surveyed once by the environmental services branch of the Pennsylvania Fish and Boat Commission. This survey was carried out by Young in November 1990. Messers Run is considered by the Pennsylvania Department of Environmental Protection to be a High-Quality Coldwater Fishery, as is its tributary Negro Hollow. Both Messers Run (from Lofty Reservoir downstream to Blue Head Reservoir) and Negro Hollow (between its headwaters and its mouth) are also considered by the Pennsylvania Fish and Boat Commission
2192066
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
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
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
10473370
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
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
Cox Run


its confluence with Little Muncy Creek. Cox Run joins Little Muncy Creek upstream of its mouth. Cox Run has no named tributaries. However, it does have two unnamed tributaries. The upper tributary is approximately long and the lower one is approximately long. The elevation near the mouth of Cox Run is above sea level. The elevation of the stream's source is above sea level. The stream flows through a valley known as Neufer Hollow. The watershed of Cox Run has an area of . The stream is entirely within the
17761048
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
Negro Hollow


in Delano Township, but significant portions are also in East Union Township and Mahanoy Township. A smaller part of the watershed is in Kline Township. The watershed is part of the Lower North Branch Susquehanna drainage basin. There is some land belonging to a Nature Conservancy Priority Forest Hub in the eastern part of the watershed of Negro Hollow. The lower reaches of the watershed are in Pennsylvania State Game Lands Number 308. Nearly all of the watershed is forested. Negro Hollow is in the United States Geological Survey quadrangle of Delano.
2638121
Phoronid


respiration. The tentacles are hollow, held upright by fluid pressure, and can be moved individually by muscles. The mouth is inside the base of the crown of tentacles but to one side. The gut runs from the mouth to one side of the stomach, in the bottom of the ampulla. The intestine runs from the stomach, up the other side the body, and exits at the anus, outside and a little below the crown of tentacles. The gut and intestine are both supported by two mesenteries (partitions that
17779206
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
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
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
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
Sica Hollow State Park


Great Spirit, to reply. Soon Wakantanka sent his messenger, Thunderer. Thunderer's eyes flashed. His dark wings beat the air, and he brought a cloud that rained over the Hollow. Madness seized Hand. He tried to run, but vines encircled his ankles. The water filled his screaming mouth. Thunderer's talons ripped out his eyes so he would never see the Happy Hunting Ground. Of all the people in the Hollow, only a raven-haired maiden called Fawn was saved from the rising water. She
1634265
White Deer Creek


of its mouth and drains an area of . Cowbell Hollow joins the creek upstream of its mouth and its watershed has an area of , making it the smallest named tributary by that measure. Tunis Run joins White Deer Creek upstream of its mouth and drains an area of . Some reaches of White Deer Creek are not designated as impaired waterbodies. However, a several miles in the creek's watershed are impaired. In one reach, the creek is impaired by habitat alterations due to hydromodification; in the other impaired reach, it
430442
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
Bryozoa


), which is closed by muscles and opened by fluid pressure. In one class, a hollow lobe called the "epistome" overhands the mouth. The gut is U-shaped, running from the mouth, in the center of the lophophore, down into the animal's interior and then back to the anus, which is located on the invert, outside and usually below the lophophore. A network of strands of mesothelium called "funiculi" ("little ropes") connects the mesothelium covering the gut with that lining
3074750
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
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
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
Larrys Creek


, and Canoe Run. The Second Fork is the largest tributary, with a watershed of or 28.0% of the total watershed. The First Fork is next largest, with a watershed of or 19.8% of the total. Roaring Run accounts for 5.7% of the total watershed with and other tributaries are less than 5% of the total. Starting at the mouth, the tributaries of Larrys Creek are: Seeley Run, Canoe Run, First Fork Larrys Creek, Second Fork Larrys Creek, Mash Run, "Pond Hollow
20558238
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
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
Phoronid


run the length of the body) connected to the body wall, and another mesentery connects the gut to the intestine. The body is divided into coeloms, compartments lined with mesothelium. The main body cavity, under the crown of tentacles, is called the metacoelom, and the tentacles and their base share the mesocoelom. Above the mouth is the epistome, a hollow lid which can close the mouth. The cavity in the epistome is sometimes called the protocoelom, although other authors disagree that it is a coelom and Ruppert,
17779207
Steve Kline (left-handed pitcher)


cog in both postseasons for the Cardinals. In fact, in 2001, Kline was called upon to close out both Cardinals victories in their 5 game Division Series loss to the Diamondbacks, and he responded with 2 saves in those clutch situations. Kline's overall effectiveness against left-handed batters was again highlighted on August 12, 2002, despite the fact that in that game he gave up a home run to left-handed slugger Brian Giles. It was noted that the home run was the first Kline had allowed to a
15689351
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
Kettle Creek (Pennsylvania)


liter and the manganese concentration is 0.07 milligrams per liter. Aluminum occurs in concentrations of 0.15 milligrams per liter at the mouth of the creek. The concentration of acidity and alkalinity are 1.65 and 11.17 milligrams per liter, respectively. In 2006, the concentration of sulfates at several points on Kettle Creek was measured. Upstream of Slide Hollow, it was seven milligrams per liter and in Slide Hollow, it was 910 milligrams per liter. The sulfate concentration of Kettle Creek upstream of Short Bend Run was 8 milligrams per liter. In
10473372
Negro Hollow


Chunk Formation and the Pottsville Formation and the main soils are the Leck Kill soil and the Hezleton soil. The stream has one unnamed tributary. Negro Hollow begins on a mountain known as Bears Head in Delano Township. It flows northwest for several tenths of a mile, entering a valley. The stream then receives an unnamed tributary and turns north for several hundred feet, flowing through another valley. It enters Kline Township and turns north-northeast for several tenths of a mile, entering East Union Township. The stream then turns
2638115
Harveys Creek


East Fork Harveys Creek. Bear Hollow Creek joins Harveys Creek in the latter creek's upper reaches. Paint Spring Run joins Harveys Creek upstream of its mouth. Its watershed has an area of . Pikes Creek joins Harveys Creek upstream of its mouth. Its watershed has an area of . East Fork Harveys Creek joins Harveys Creek upstream of its mouth. Its watershed has an area of . High levels of nutrients have been observed in the waters of Harveys Creek and the tributary East Fork Harveys Creek. Harveys Creek has been described as
669020
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
Pomatrum


, with a prominent mouth circlet. It has faint transverse divisions towards the front, but is otherwise smooth. The mouth circlet consists of about 30 plates divided into inner and outer regions. The anterior section has five structures on each side, which are interpreted as gills. A dark region running close to the ventral and posterior margins is interpreted as an endostyle. The condition of the anterior portion of the fossils suggests that it was thin-walled, i.e., that the anterior portion was largely hollow. The posterior part of
13053012
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
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.
15498988
Hand percussion


ridges on its body. Often known as Guiro, rhythms are created by running a thin stick up and down the ridges at different speeds. Gourds or bamboo have traditionally been used as they have a resonant hollow body and can easily be cut with ridges. A common type from Asia is a carved wooden frog which has ridges cut on its back and its mouth and belly hollowed out. Cowbells originate from the bells tied around the necks of livestock. They are any type of hand held bell tapped with fingers, wood or
17971663
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
Richard S. Kline


Friends"; producer Gary Cox also joined Kline briefly, but soon left to work for Reg Grundy Productions, while Ron Greenberg became an independent producer once again. With Kline running his own company, "Break the Bank" (completely unrelated to the earlier game) premiered in the fall of 1985, with Gene Rayburn as host. By year's end, Rayburn was let go due to conflict with Kline over the show's format and replaced by Joe Farago. After that, Kline tried again with "Strike it Rich
18086688
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
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
Hammersley Fork


Diversity Inventory Biological Diversity Area. The Pennsylvania Department of Environmental Protection also classifies the watershed as an exceptional-value area. From the mouth of Hammersley Fork to upstream of the mouth, the canopy cover ranges from 0 to 50 percent. Much of the creek, however, has a significant riparian buffer. The canopy coverage of the section of Hammersley Fork between Dry Hollow and Bunnell Run is 62 percent on average. However, the lower part of this section has 86 percent canopy coverage. The upper part of the stretch of
17509669
Where Troy Once Stood


old man of the sea, and at its mouth two projecting headlands sheer to seaward, but sloping down on the side toward the harbour... Wilkens believes that Havana's topography greatly resembles the description of Telepylos:"The harbour, about which on both sides a sheer cliff runs continuously, and projecting headlands opposite to one another stretch out at the mouth, and the entrance is narrow, ..., and the ships were moored within the hollow harbour, for therein no wave ever swelled, great or small, but all about was a bright
8605293
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
Devil Hole Run


is known as Devil's Hole Hollow. Devil Hole Run is located in the United States Geological Survey quadrangle of Benton. The mouth of the stream is at the community of Cole's Mill and is located near the community of Derrs. The stream is within a large and mostly untouched block of forest. The only roads that are close to the stream are small private roads. Devil Hole Run is part of a Locally Significant Area in Columbia County. The area's county priority rank is five on a scale of one to
5692703
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
Tiny Kline


. Two years later, they married. When he died during a ride, she took over and learned acrobatic tricks, including the "aerial iron jaw act", where she would be suspended by the mouth on a long glide wire. In 1961, Walt Disney began a search for a flying Tinker Bell to wow crowds at Disneyland. Kline was hired to glide down a wire connecting the Matterhorn to Sleeping Beauty's Castle. She retired from playing Tinker Bell in 1964. Tiny was scheduled to return as Tinker Bell that
19754069
Hammersley Fork


south, passing by Susquehannock State Forest. The stream continues south for some distance and crosses Pennsylvania Route 144. Immediately after crossing Pennsylvania Route 144, the stream reaches its confluence with Kettle Creek. Hammersley Fork joins Kettle Creek upstream of its mouth. The concentration of alkalinity in Hammersley Fork ranges from . Particles in the stream include coarse sand and fine gravel. The stream experiences relatively high water temperatures and in July 2003, its temperature between Dry Hollow and Bunnell Run ranges from . Between Dry Hollow and Nelson Branch, the temperature
17509658
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
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