Blue Mountain Creek [SEP] mouth of the watercourse
[{"answer": "Macleay River", "provenance": [{"wikipedia_id": "40719283", "title": "Blue Mountain Creek", "start_paragraph_id": 1, "start_character": 0, "end_paragraph_id": 1, "end_character": 168, "bleu_score": 1.0, "meta": {}, "section": "Section::::Abstract."}]}]
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
Morro Creek


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


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


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


Merta (German: Merta Bach) is a creek in Šumperk District, Moravia, left right tributary of the Desná. Its length is 16,6 km and its drainage basin covers 74.5 km2. The mean annual discharge at its mouth is 1,20 m³/s. The Merta originates from southeast slope of Vřesník peak in High Ash Mountains, 1200 meters above sea level. Upper reaches have a character of mountain torrent flowing through steep meadows. Dead trees are in watercourse and banks keep its natural character. Then The Merta goes through villages of Vernířovice
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Santiago Creek


Santiago Creek is a major watercourse in Orange County in the U.S. state of California. About long, it drains most of the northern Santa Ana Mountains and is a tributary to the Santa Ana River. It is one of the longest watercourses entirely within the county. The creek shares its name with Santiago Peak, at the highest point in Orange County, on whose slopes its headwaters rise. The Santiago Creek watershed covers about in northern Orange County. The upper part of the creek is free-flowing, while the lower section
22063315
Bully Creek (Malheur River tributary)


the Northern Basin and Range and the Blue Mountains ecoregions, the watershed experiences an arid climate. Precipitation ranges from , with an average of . The highest elevation in the watershed is at Juniper Mountain, while the lowest is at the creek's mouth. Two hundred and five species of vertebrates have been identified within the Bully Creek watershed. Large mammals such as Rocky Mountain elk and mule deer, bobcats, beavers, otters, and raccoons inhabit the region. Twenty one species of fish have been spotted, but there are no
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Mouth of Wilson, Virginia


Mouth of Wilson is an unincorporated community, in Grayson County in the U.S. state of Virginia, just north of the North Carolina state line. The community lies in the Blue Ridge Highlands section of the Blue Ridge Mountains which are part of what is considered the 'Middle Appalachian Mountains' on the western banks of the New River, where the Big Wilson Creek empties its waters. The main road through the area is U.S. Route 58; other major roads include Virginia Route 16 and Virginia Route 93 (County Line Road).
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Bowmanville Creek


Bowmanville Creek is a watercourse in Durham County, that flows from its headwaters in the Oak Ridges Moraine to its mouth on Lake Ontario, at Bowmanville, Ontario. It borders Oshawa Creek, and Soper Creek, to the west and east, which have their headwaters in the Oak Ridges Moraine. Between Bowmanville Creek and Oshawa Creek, there are five smaller creeks, Farewell Creek, Robinson Creek, Tooley Creek, Darlington Creek and Westside Creek. Bowmanville Creek has been dammed in several places. About one km north of Lake Ontario
15222123
Burpengary Creek


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


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


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


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


Graham Creek is a perennial stream in Sonoma County, California, tributary to Sonoma Creek. Graham Creek rises in the northern Sonoma Mountains and flows generally northeasterly down the northeastern flank of Sonoma Mountain. Historically this watercourse was called Wild Water Creek, a name used in the time of author Jack London, some of whose work was inspired by the stream. Steelhead, "Oncorhynchus mykiss", have historically entered Graham Creek via Sonoma Creek for spawning. Stream surveys conducted from 1966 to 1986 indicated significant, but declining populations of anadromous
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Pooraka, South Australia


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


flowing into Fishing Creek Township and Stillwater. In Stillwater, Raven Creek empties into the creek from the northeast, above the mouth. About south, the creek turns and picks up Huntington Creek, and then flows past the communities of Zaners, Forks, and Pealertown. The mouth of Huntington Creek is above the mouth of Fishing Creek. Upon leaving Fishing Creek Township, about after picking up Huntington Creek, Fishing Creek flows southwest past Knob Mountain and into Orange Township. It passes near the northern edge of Knob Mountain downstream,
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Huntington Creek (Pennsylvania)


Jonestown, where it receives Pine Creek, its last named tributary. After flowing parallel to Huntington Mountain and Knob Mountain for a few miles, it reaches its confluence with Fishing Creek near the community of Forks. Huntington Creek joins Fishing Creek upstream of its mouth. Major tributaries of Huntington Creek include Kitchen Creek and Pine Creek. Kitchen Creek joins Huntington Creek upstream of its mouth; its watershed has an area of . Pine Creek joins Huntington Creek upstream of its mouth. Its watershed has an area of . The waters of Huntington
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Ashley County, Arkansas


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


and receives Benner Creek from the left and Digger Creek from the right. Slightly west of the mountain, about from the mouth, the river leaves Benton County, and enters Lincoln County. Passing Little Digger Mountain on the right, the river receives Fall Creek from the right, Cow Creek and Minotti Creek from the left, and Wolf Creek, Phillips Creek, Cedar Creek, and Butter Creek from the right as it passes Trenholm Saddle, a mountain gap at coordinates on the right about from the mouth. About later,
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Knob Mountain (Pennsylvania)


Knob Mountain. The settlers that arrived in this year primarily traveled from New Jersey to the mouth of Fishing Creek via Berwick and from the mouth of Fishing Creek up the creek's valley to near Knob Mountain. Such settlement was, at the time, the northernmost non-native settlement in the Fishing Creek watershed. A community at the base of the mountain was built in 1822. An Indian path once passed over the mountain near its eastern terminus. The Susquehanna and Tioga Turnpike once crossed over Knob Mountain. A township border
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Sierra Pelona Mountains


. Three major tributaries of the Santa Clara River and numerous minor watercourses and washes drain the range: Castaic Creek, San Francisquito Creek, and Bouquet Creek. Three sag ponds nestle within the narrow valley that divides the mountains from the Antelope Valley: Hughes Lake, Munz Lakes, and Elizabeth Lake. The Native population of California in the Sierra Pelona and Santa Susana Mountains included the Tataviam and Serrano people. They traded with the Tongva and Chumash to the south and west, until the Spanish colonization of the Americas relocated them from
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San Rafael Creek


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


Mountain between Frackville and the creek's mouth. Little Mahanoy Creek flows through a valley between Ashland Mountain and Broad Mountain. The valley is very steep and narrow near the creek's headwaters, but becomes broader further downstream, being close to wide at the mouth. The creek lies over a layer of red shale. Below the shale is a layer of hard and compact sandstone, which has some black, carbon-containing matter in it. Little Mahanoy Creek is one of the only tributaries of Mahanoy Creek that is not affected
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Ruggs, Oregon


, are relics of Pleistocene glacial periods. Ruggs lies along Rhea Creek, a tributary of Willow Creek in the Blue Mountains east of the Cascades. These creeks eventually converge and flow north into the Columbia Gorge at Heppner Junction, a Union Pacific station located on the left bank at the mouth of Willow Creek at Columbia River Mile (RM) 252. Newspaper records suggest that the Ruggs area at one point had its own post office known as "Midway" on the aforementioned Wright family's property. Ruggs has no elected officials
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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
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
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San Rafael Wilderness


. Most of the wilderness lies between the crests of two parallel mountain ranges, the San Rafael Mountains and Sierra Madre Mountains, and includes the drainages of two watercourses: the Sisquoc River and Manzana Creek. Both flow to the northwest, eventually joining together and draining into the ocean near Santa Maria. Elevations within the wilderness vary from at the confluence of Manzana Creek and the Sisquoc River on the western boundary, to over at Big Pine Mountain, the highest point in Santa Barbara County. Dividing the drainages of the Manzana and
1392319
Lindy Creek


Lindy Creek begins in a pond on Bald Mountain in Ransom Township, not far from the border between Ransom Township and Newton Township. The creek flows south down the mountain for several tenths of a mile before turning southeast and continuing to flow down the mountain. After several tenths of a mile, it enters Scranton and crosses Interstate 476. Several tenths of a mile further downstream, the creek reaches its confluence with Keyser Creek. Lindy Creek joins Keyser Creek upstream of its mouth. At its mouth, the peak annual discharge of
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Kugruk River


size. The eastern fork is called Taylor Creek, while the western retains the name Kugruk River. Taylor Creek rises to the southeast of Midnight Mountain, and flows west to its junction with the Kugruk River. It occupies a valley about deep, cut in the plateau on which Midnight Mountain stands. The bed rock at the mouth of Taylor Creek is a dark schist similar to that of Midnight Mountain, while immediately south of that mountain, at a point about f miles from the mouth of Taylor Creek, there are exposures
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Little Catawissa Creek


T435 and the creek's mouth, its width is . The gradient of the creek upstream of T431 is . The gradient between T431 and T435 is and the gradient between T435 and the mouth of the creek is meters per kilometer. There is a flooded strip mine in the western part of the watershed of Little Catawissa Creek. The headwaters of the creek are on a mountain known as Big Mountain. The creek is a freestone stream. The watershed of Little Catawissa Creek has an area of . Most of the watershed is in
1368388
Catasauqua Creek


Catasauqua Creek is a ENE–SSW oriented creek draining (straight line distance) from springs of the Blue Mountain barrier ridge several miles below the Lehigh Gap in the ridge-and-valley Appalachians located upriver & opposite from Allentown in Lehigh and Northampton counties in Pennsylvania. The mouth of the creek outlets directly opposite West Catasauqua, Pennsylvania just below the Race Street bridge across the Lehigh, the latest of the several successor structures built to replace the original wooden bridge built in 1839-1840 to carry heavy wagons of iron ore to
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Dandenong (disambiguation)


The name Dandenong is derived from the Woiwurrung language of the Wurundjeri people, that was applied to the watercourse now known as Dandenong Creek. The name as appropriated to extend beyond its actual meaning and is now applied to two settlements, a mountain summit and the Dandenong Ranges mountain range. The creek however, originates in the mountain range, so this connection is more understandable. It is not known where the name "Dandenong" came from nor what it means, or even its correct spelling, other variations include; "Tanjenong
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San Pietro (creek)


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


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


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


The nickel and selenium concentrations are less than , respectively, while the boron concentration is less than . The creek's strontium concentration is . The mouth of Muncy Creek has an elevation of slightly less than , while the source of the creek has an elevation of between and . The headwaters of the creek are more than higher than its mouth. The headwaters of Muncy Creek are mountainous and are situated on the Allegheny Plateau. The southern edge of the Allegheny Mountain runs from the creek west as far as Lock Haven or Pine Creek
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E-card


an announcement sent with a link to the card's location at the E-card site. Between Sep 1996 and Thanksgiving 1997, a paper greeting card company named Blue Mountain developed E-cards on its web site. Blue Mountain grew quickly by allowing visitors to create greetings for others to use. Blue Mountain further expanded when Microsoft promoted its service on its free Hotmail service. This affiliation ceased and Blue Mountain sued Microsoft in Nov 1998 for putting email card announcements from it and other E-card companies in the junk folder
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Wissahickon Creek


a multi-use trail approved for mountain bikers with permits. The blue blazed trail has been designated a hiking trail only. All trails in the Andorra Natural Area are prohibited to all bicycles. Devil's Pool is an attraction best reached from Valley Green by crossing the stream and taking the footpath on the eastern bank, going downstream to the mouth of the Cresheim Creek. As the ravine widens into the Cresheim, the waters gather in a basin surrounded on either side by rocky outcroppings before flowing into the Wissahickon Creek. Legend
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Campbell Creek, Queensland


Campbell Creek is a locality in the North Burnett Region, Queensland, Australia. In the , Campbell Creek had a population of 7 people. The locality takes its name from the Campbell Creek watercourse which has its source is more mountainous area (up to ) in the south of the locality and flows northward toward the lower flatter land ( in the north of the locality. Barambah Creek forms the north-western boundary of the suburb and the two creeks have their confluence on the locality's northern boundary (). A short
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Hans Yost Creek


near the mouth of Hans Yost Creek is above sea level. The elevation near the creek's source is above sea level. Part of a steep valley between Broad Mountain and Mahantango Mountain is drained by Hans Yost Creek. The creek flows through the Southern Anthracite Coal Field. The watershed of Hans Yost Creek has an area of . The creek is entirely within the United States Geological Survey quadrangle of Tremont. Its mouth is located within of Weishample. The headwaters of Hans Yost Creek flow through forested land and are difficult to access
21109443
Blue Creek Valley


Valley is narrow, only 5-8 mi wide, small feeder creeks feed the region from the four cardinal directions. Blue Creek Reservoir is located in the center-south of the valley, with Blue Creek Spring located 2 mi northeast, the main feed to the reservoir. The outlet of Blue Creek Reservoir trends south past Howell, Utah, into agricultural land. A peak associated with the north of the Promontory Mountains ends the valley's south, at the mountain range foothills. The mountain, Engineer Mountain, , and
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Rock Flat Creek


The Rock Flat Creek, a watercourse that is part of the Murrumbidgee catchment within the Murray–Darling basin, is located in the Monaro region of New South Wales, Australia. The Rock Flat Creek (technically a river) rises below One Tree Hill, on the lower slopes of the Snowy Mountains, part of the Great Dividing Range. The creek flows generally north by west before reaching its confluence with the Cooma Creek just upstream from that creek's confluence to form the Numeralla River (itself a tributary of the Murrumbidgee River
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McKay Creek National Wildlife Refuge


McKay Creek National Wildlife Refuge is a United States National Wildlife Refuge located between plains and the Blue Mountains of Eastern Oregon. The refuge provides habitat for rare and endangered species and breeding and migratory birds. The lack of other local wetland habitats elevates the importance of this refuge as a home to a variety of wildlife and plant species in an arid environment. McKay Creek National Wildlife Refuge, dam and reservoir are named for Dr. William C. McKay, an early pioneer in the Pendleton, Oregon, area. McKay settled near the mouth
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Carbonera Creek


Carbonera Creek is a watercourse in Santa Cruz County, California, that eventually flows to the San Lorenzo River. The stream rises in the rugged Santa Cruz Mountains and flows in a generally southwesterly direction. The city of Scotts Valley is situated within the watershed of Carbonera Creek and its main tributary to the north, Bean Creek. Carbonera Creek joins Branciforte Creek near the 500 block of Market Street in Santa Cruz. Branciforte Creek discharges to the San Lorenzo River, which empties into the Pacific Ocean at Monterey Bay at Santa Cruz.
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San Mateo Creek (San Francisco Bay Area)


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


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


Boulder Creek is a locality in the Rockhampton Region, Queensland, Australia. In the , Boulder Creek had a population of 12 people. The Dee River forms the eastern boundary of the locality. The terrain is mountainous with named peaks of Mount Victoria at and Mount Battery at . The land is mostly undeveloped. The watercourse Boulder Creek (after which the locality is presumably named) rises in the north of the locality and flows to the south-east of the locality where it becomes a tributary to the Dee River within the
21513013
Branciforte Creek


Branciforte Creek is a long watercourse in Santa Cruz County, California, United States. Branciforte Creek rises on the western slopes of the Santa Cruz Mountains and discharges to the San Lorenzo River, which in turn empties into the Pacific Ocean. Within the State of California Branciforte Creek is classified within the Central Coast Basin. As of the year 2002, the State of California has designated Branciforte Creek as impaired with respect to turbidity and pathogens. The Branciforte watershed consists of , approximately 70 percent of which is covered with mixed evergreen forest
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Wrights Creek, Queensland


Wrights Creek is a locality in the Cairns Region, Queensland, Australia. In the , Wrights Creek had a population of 156 people. The locality is mostly low-lying flat land (approx 10 metres above sea level) with a small area of mountainous area in the south-west of the locality rising to an unnamed peak of 200 metres above sea level. The Trinity Inlet (aka Smith Creek) is the northern boundary of the locality while Wrights Creek (the watercourse from which the locality takes its name) and
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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
Tijeras Canyon Creek


Tijeras Canyon Creek is a watercourse in northeast Orange County, California and a tributary of Arroyo Trabuco. It originates in the foothills of the Santa Ana Mountains, and flows southwest through the suburban city of Rancho Santa Margarita for several miles as an underground culvert. Below State Route 241 it becomes a free-flowing creek, traveling through Cañada Vista Park and Tijeras Creek Golf Club before joining with Trabuco Creek in O'Neill Regional Park. Due to its relatively natural condition, the lower Tijeras Creek provides habitat for the threatened arroyo chub,
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Plamondon Creek


surrounded by mountains. The mouth of this head lake is located at: From the mouth of the head lake, the course of Plamondon Creek flows entirely in forest zone on according to the following segments: The mouth of Plamondon Creek is located at: The mouth of Plamondon Creek meets with Plamondon Bay (Gouin Reservoir). From there, the current flows over until Gouin Dam, according to the following segments: From this dam, the current flows along the Saint-Maurice River to Trois-Rivières. The term "
8861780
Blue Creek Valley


Blue Creek Valley is an long valley located in northeast Box Elder County, Utah. It is endorheic with the Blue Creek Reservoir its lowpoint located south in the valley's center. The valley is nestled between three mountainous regions. The West Hills and Blue Spring Hills border it east and southeast. The south abuts the north of the Promontory Mountains, and the west is formed by a small north-south range, the North Promontory Mountains The north of the valley borders the south of Idaho's Pocatello Valley. Because Blue Creek
18522926
Temescal Creek (Riverside County)


Temescal Creek (shown on federal maps as Temescal Wash) is an approximately watercourse in Riverside County, in the U.S. state of California. Flowing primarily in a northwestern direction, it connects Lake Elsinore with the Santa Ana River. It drains the eastern slopes of the Santa Ana Mountains on its left and on its right the western slopes of the Temescal Mountains along its length. With a drainage basin of about , it is the largest tributary of the Santa Ana River, hydrologically connecting the San Jacinto River and Lake Elsinore watersheds to
18077492
Ngatjan


River (Waraker Creek being the principal watercourse within the southern part of the locality). The locality is mountainous terrain ranging from 20 metres above sea level (in the Suez Creek valley) through to peaks such as Mount Mirinjo (390 metres), Cooroo Peak (430 metres) and Chalmynia Mountain (400 metres). The land in the locality is undeveloped and entirely contained within the Wooroonooran National Park (part of the Wet Tropics World Heritage Area). The only road through Ngatjan is the Cooroo Lands Road which traverses
9977319
Pomponio Creek


Pomponio Creek is a westward flowing stream in San Mateo County, California that originates on the western slope of the Santa Cruz Mountains and flows into the Pacific Ocean at Pomponio State Beach. Pomponio Creek is named for Ponponio Lupugeyun (also known as José Pomponio Lupugeym), a resistance fighter against the California mission system who had a mountain hideout at the headwaters of Pomponio Creek. A dam forms Pomponio Reservoir is located at about upstream from the mouth. A 15 foot high bedrock waterfall located about upstream from the creek mouth is an
10016792
San Diego Creek


century, the watershed was used for agriculture. Increased runoff from farmlands resulted in extensive erosion, which led to the creation of a stream channel that ran northwestwards into the Santa Ana River channel and thence the Upper Newport Bay. As siltation problems plagued the bay, the Bitter Point Dam was constructed to divert the Santa Ana River to its present mouth at Huntington Beach, leaving the Cienega/San Diego Creek as the main watercourse flowing into the bay. To support irrigation, farmers drilled numerous wells to tap the region's abundant
17239627
Nesquehoning Mountain


down a narrow undeveloped section to its confluence with the Lehigh River. The heavily forested, relatively steep slopes of Broad and Nesquehoning Mountains characterize the land within the watershed. While US 209 and PA 93 both climb watercourse ravines on opposite sides of the valley, the Nesquehoning route is very steep and was not anything more than a mule road before the systematic attempt to create a U.S. highway was put through alongside the creek. The Nesquehoning Creek valley consists of some residential and industrial development. Urban development is concentrated in the Borough of
977835
Little Mahantango Creek


Mahantango Creek near Pitman was once measured to be , while at Line Mountain, it was measured to be . The instantaneous discharge of the creek was near Pitman and at Line Mountain. The specific conductance was 199 micro-siemens per centimeter at near Pitman and 188 micro-siemens per centimeter at at Line Mountain. The concentration of nitrogen in nitrate in the creek was near Pitman and at Line Mountain. The elevation near the mouth of Little Mahantango Creek is above sea level. The elevation near the creek's source is above
295648
Kitchen Creek (Pennsylvania)


joins Huntington Creek upstream of its mouth. The elevation near the mouth of Kitchen Creek is above sea level. Lakes, swamps, and mountains are present at the headwaters of Kitchen Creek. The topography of the creek's watershed is described as "rough and hilly" in a 1921 book. The channel of Kitchen Creek is sinuous. The creek flows through rock formations made of sandstone and shale. There is a gorge and waterfall system on the creek. This system is known as the Kitchen Creek Ravines. The Kitchen Creek
5082192
Uvas Creek


its name from the 1842 Rancho Las Uvas Mexican land grant. The Spanish name for grapes, "uvas", is preserved in a number of place names, all apparently referring to the abundance of wild grapes ("Vitis californica") along the area's main watercourses. "Carnadero" probably means "butchering place". The Uvas Creek watershed drains the eastern slope of the Santa Cruz Mountains in southern Santa Clara County. On the upper section of the creek is Uvas Canyon County Park. Here, portions of the
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Blue Mountain Creek


The Blue Mountain Creek, an intermittent stream that is part of the Macleay River catchment, is located in the Northern Tablelands region of New South Wales, Australia. Blue Mountain Creek rises on the eastern slopes of Blue Mountain, north northeast of Walcha and south southeast of Uralla, within the Great Dividing Range. The river flows generally east, joined by two minor tributaries before reaching its confluence with the Macleay River in remote country within the Oxley Wild Rivers National Park, upstream of the confluence of the Macleay and Chandler rivers.
4401976
Ithan Creek


of its mouth. The elevation near the mouth of Ithan Creek is above sea level. The elevation of the creek's source is above sea level. Ithan Creek is within the Piedmont Uplands physiographic province. The Piedmont Uplands section has generally old, hard upland rocks that eroded from the Appalachian Mountains. The rocks in the watershed date to the Precambrian Era and Lower Paleozoic Era. The surficial geology mainly consist of felsic gneiss and mafic gneiss formations, with small amounts of serpentinite near the mouth of the creek. Silvery mica schist
11928480
Little Mahanoy Creek


a steep narrow valley between Ashland Mountain and Broad Mountain, which abruptly widens out a short distance downstream. The creek then flows on the northern edge of Broad Mountain to the borough of Gordon, where it picks up Rattling Run before flowing into Mahanoy Creek. Rattling Run flows into Little Mahanoy Creek in Gordon, not far from Little Mahanoy Creek's mouth. It rises from springs on the slopes of Broad Mountain. The watershed of Little Mahanoy Creek has an area of . Areas in the watershed include the southern side of Ashland
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Piner Creek


, which watercourse discharges to the Laguna de Santa Rosa; the Laguna de Santa Rosa ultimately forms a confluence with the Russian River, which flows into the Pacific Ocean. As recently as the Miocene period, twelve million years ago, the entire watershed of Piner Creek was on the floor of the Pacific Ocean. After significant volcanic uplift and tectonic movement, the headwaters region of the Mayacmas Mountains emerged above the ocean. Piner Creek was one of the drainages that began to drain the new landmass, in formation of the eventual Santa
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Grassy Island Creek


the mouth of Grassy Island Creek is above sea level. The elevation of the creek's source is between above sea level. Grassy Island Creek is in the Appalachian Mountain section of the ridge and valley pysiographic province. The geography of the creek's watershed consists of long, steep ridges with valleys in between. This is similar to the geography of the Lackawanna River watershed as a whole, but on a smaller scale. The headwaters of Grassy Island Creek are in mountain springs in the Moosic Mountains. In some reaches, the
21350165
Deep Creek (Mahantango Creek tributary)


. This makes the creek's watershed one of the few areas where the watershed of Mahantango Creek extend south of Mahantango Mountain. The watershed of Deep Creek has an area of . The mouth of the creek is in the United States Geological Survey quadrangle of Pillow. However, its source is in the quadrangle of Lykens. The creek also passes through the quadrangle of Klingerstown. Its mouth is located at Pillow. The main land use in the upper reaches of the watershed of Deep Creek is agricultural land. However, there are
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Silver Creek (Harney County, Oregon)


Silver Creek is an stream of Oregon which drains a portion of the endorheic Harney Basin to Harney Lake. Arising in the Blue Mountains, it flows generally southeast, although much of the stream is intermittent. The Silver Creek Volcanic Field is associated with the creek's watershed. From its headwaters in the southern Blue Mountains, Silver Creek flows south through the Ochoco National Forest and is feed by tributaries and, at the base of the mountains, large springs feed the creek. The creek meanders through a broad alluvial plain and turns
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Deep Creek (Mojave River tributary)


at a waterfall along Deep Creek. The creek continues north, at the bottom of a deep gorge through mountainous wilderness, receiving Holcomb Creek and Coxey Creek from the right before turning west, forming a canyon between the San Bernardino Mountains and Ord Mountains. The Deep Creek Hot Springs are located along the stream where it turns to the west. The Pacific Crest Trail follows the Deep Creek canyon for , from the confluence of Hooks Creek to the mouth. Deep Creek ends at its confluence with the West Fork Mojave River forming the
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Deep Creek (Mahantango Creek tributary)


, it reaches its confluence with Mahantango Creek. Deep Creek joins Mahantango Creek upstream of its mouth. Deep Creek is not designated as an impaired waterbody as of 2004. However, the Dauphin County conservation District has observed that nitrate concentrations in the creek are among the highest in Dauphin County. It is also likely that sediment loads are relatively high. The elevation near the mouth of Deep Creek is above sea level. The elevation near the creek's source is above sea level. Deep Creek cuts through Mahantango Mountain on its course
20939085
Huntsville Creek


for a few miles. It then receives Browns Creek, its only named tributary, from the right. At this point, the creek turns east-northeast and flows alongside Larksville Mountain for several tenths of a mile. It then flows east-southeast for a few tenths of a mile until it reaches its confluence with Toby Creek. Huntsville Creek joins Toby Creek upstream of its mouth. Huntsville Creek has one named tributary, which is known as Browns Creek. Browns Creek joins Huntsville Creek upstream of its mouth. Its watershed
4343187
Limpia Creek


Limpia Creek, originally known as the Rio Limpia, is a stream that heads in Jeff Davis County, Texas and its mouth is in Pecos County, Texas. Limpa is the Spanish word for "clear or clean water". The creek has its head in the Davis Mountains at an elevation of 7,160 feet, at location on the northeast slope of Mount Livermore. The creek flows 42 miles down Limpia Canyon past Fort Davis and Wild Rose Pass to the canyon mouth, where it turns eastward to its mouth at its confluence
3545113
South Branch Bowman Creek


part of the watershed of Kitchen Creek. There used to be a glacial lake in the valley of South Branch Bowman Creek. The watershed of South Branch Bowman Creek has an area of . The mouth of the creek is in the United States Geological Survey quadrangle of Sweet Valley. However, its source is in the quadrangle of Red Rock. The mouth of the creek is located at Mountain Springs. Most of the length of South Branch Bowman Creek is in Ricketts Glen State Park, but its lower reaches (including Mount Springs
2709780
Newport Creek


in 1913. The watershed of Newport Creek is in the Allegheny Mountain section of the ridge and valley geological region. The creek's headwaters are or higher in elevation than the mouth. The lowest elevation in the watershed is at the creek's confluence with the Susquehanna River and the highest elevation is on Penobscot Mountain. Little Wilkes-Barre Mountain is found in the southern part of the watershed. Most of the Newport Creek watershed is in the Northern Anthracite Coal Field. There are glaciofluvial deposits from the pleistocene epoch in parts of
12281879
Winfield Creek


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


lake (length: ; altitude: ) surrounded by mountains. The mouth of this lake is located in the eastern part of the township of Perrier, a few tens of meters from the eastern limit of the township of Lagacé. This mouth is at: From the mouth of the head lake, the course of the "De la Rencontre Creek" flows entirely in forest zone on according to the following segments: Upper part of the course of the "De la Rencontre Creek" (segment of ) altitude: ),
9080839
Icicle Creek


Washington. These high mountains are known as the Stuart Range. The range contains a number of glaciers, notably Colchuck Glacier, Sherpa Glacier, and Stuart Glacier. Eightmile Campground is located on Icicle Creek just below the mouth of Eightmile Creek. Below Eightmile Creek Icicle Creek is joined from the south by Rat Creek, which flows from the northern slopes of Cannon Mountain, Enchantment Peaks, Prusik Peak, and The Temple. There are numerous mountain lakes in this region. Just above river mile 5 Icicle Creek is joined from the
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Naples Creek


Naples Creek is a stream in San Mateo County, California, United States that rises on the western slopes of the Santa Cruz Mountains and discharges to the Pacific Ocean. The specific point of discharge is onto Naples Beach, a unit of the Half Moon Bay State Beach. This watercourse runs through the city of Half Moon Bay, which municipality has planning jurisdiction over the creekside area within its city boundaries. In the Open Space Element of Half Moon Bay's General Plan, Naples Creek is designated to have significant wetland and riparian
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Arroyo Seco (Salinas River tributary)


Salinas Valley is actually a fairly large perennial stream. The common name, Arroyo Seco River or Arroyo Seco Creek, is actually a tautology because the name contains two mentions of "watercourse", thus "Arroyo Seco River" literally translates to "dry streambed river". The river rises in several unnamed forks in the Santa Lucia Mountains of the Coast Ranges near the Pacific Ocean. It flows generally north, cutting into a steep gorge, receiving Lost Valley Creek and Tassajara Creek both from the left. After the confluence with
5785003
Black Creek (Lehigh River tributary)


from the Lehigh River at the 19th century settlement of Lausanne Landing climbed the steep south slopes of Broad Mountain and followed a chain of watercourses to Nescopeck opposite Shickshinny, PA on the main Susquehanna branch. Initially, in 1830, the Beaver Meadow mining operations sent coal out by pack mules, but then capitalized the railway, when the technology was emergent and untried. Consequently, the creek hosted the first operating steam locomotives employed as mobile traction engines in the United States. Black Creek joins the Lehigh River near the community of Rockport
7762371
Virginia State Route 20


the watercourse and the highway passes through a gap between Green Mountain and Carters Mountain, which are part of the Southwest Mountains. The state highway follows the west side of the latter mountain to the community of Mill Creek, where the highway expands to a four-lane divided highway at its intersection with SR 53 (Thomas Jefferson Parkway). SR 53 provides access to Thomas Jefferson and James Monroe's respective estates of Monticello and Ash Lawn–Highland. SR 20 passes the entrance to Piedmont Virginia Community College just south of its
10727492
Sloan Creek (Washington)


Sloan Creek is the largest tributary of the North Fork Sauk River, entering the river about above the mouth of Lost Creek. Its only major tributary is Cadet Creek, which enters the creek about above its mouth. According to Fred Beckey, Cadet Creek is larger than Sloan Creek and could be equally considered the head of the Sauk River as the North Fork itself. Sloan Creek begins at the outlet of Blue Lake, which is located a slight 0.4 miles west of the unnamed lake that is the source of the North Fork
21169584
Ritner Creek


Ritner Creek is a tributary of the Luckiamute River in Polk County in the U.S. state of Oregon. The creek begins near Bald Mountain in the Central Oregon Coast Range and flows generally southeast to meet the Luckiamute southwest of Pedee and north of Kings Valley. The confluence is upstream of the Luckiamute's mouth on the Willamette River. Named tributaries of Ritner Creek from source to mouth are Sheythe, Love, Clayton, and Kinsey creeks. Ritner Creek passes under Oregon Route 223 just before entering the river. The Ritner Creek Bridge,
3601339
Buffalo Creek (West Branch Susquehanna River tributary)


. The elevation of the creek's source is between above sea level. Between upstream of its mouth and it mouth, a distance of the creek's gradient is . Between Mifflinburg and Lewisburg, the gradient is . The topography of the creek's watershed is mountainous in its upper reaches. However, in its lower reaches, the creek flows through a wide valley bordered by steep ridges. The creek's channel is sinuous and flows through rock formations consisting of sandstone and limestone, with some iron ore. All of the creek
6459895
Black Creek (Nescopeck Creek tributary)


manganese load is per day. The daily acidity load is . The elevation near the mouth of Black Creek is above sea level. Elevation at the source is between and . From its source to downstream, Black Creek's elevation decreases at a rate of per mile. For the next , elevation decreases at a rate of per mile. From there to the mouth, elevation falls at a rate of per mile. Black Creek's topography is described in a 1921 book as "mountainous". The upper part of the creek
7762296
Vrbas (river)


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


The South Fork Umatilla River is a tributary of the Umatilla River in Umatilla County in the U.S. state of Oregon. Its headwaters lie in the Umatilla National Forest in the Blue Mountains of northeastern Oregon near Pileup Saddle and Black Mountain. The South Fork flows generally north between Goodman Ridge and Bobsled Ridge to meet the North Fork Umatilla River near Graves Butte. Together the forks form the main stem Umatilla. Named tributaries of the South Fork from source to mouth are Shimmiehorn, Thomas, and Buck creeks, which all enter from the
12352307
Blue Jay Creek (Lake Huron tributary)


Blue Jay Creek is a river on Manitoulin Island in Central Manitoulin and Tehkummah townships, Manitoulin District in northeastern Ontario, Canada and a tributary of Lake Huron. Blue Jay Creek begins at a spring, about east of the community of Sandfield on Lake Manitou in Central Manitoulin township, and at an elevation of . It flows south under Ontario Highway 542 and then to the east of the community of Tehkummah in Tehkummah township. The creek heads southwest, takes in the right tributary Black Creek and reaches its mouth at Michael's Bay
6330380
Pine Creek (Mahantango Creek tributary)


Valley. This valley is situated between Mahantango Mountain and Broad Mountain. The tributary Deep Creek is also in Hegins Valley, being separated from Pine Creek by a low ridge within the valley. Pine Creek also flows through a water gap in Mahantango Mountain near its mouth. The main rock types in the watershed of Pine Creek are interbedded sedimentary rock and sandstone. The soils in the watershed are well-drained and permeable. The Lykens Valley coal seam, which is part of the Pottsville Formation, is found in the watershed's
10588482
Briar Creek (Susquehanna River tributary)


Creek has two named tributaries: East Branch Briar Creek and West Branch Briar Creek. East Branch Briar Creek joins Briar Creek upstream of its mouth. It watershed has an area of . West Branch Briar Creek joins Briar Creek upstream of its mouth. Its watershed has an area of . The Briar Creek watershed falls into two of Pennsylvania's ten climate divisions: Division 1 (Pocono Mountains) and Division 5 (Central Susquehanna). The discharge of Briar Creek about two miles (three kilometers) downstream of its headwaters ranges from
8710473
Beaver Run (Catawissa Creek tributary)


McCauley Mountain and Buck Mountain, eventually turns northwest and then southwest less than a mile later. A short distance downstream, it turns west and crosses Pennsylvania Route 339, then reaches its confluence with Catawissa Creek. Beaver Run joins Catawissa Creek upstream of its mouth. While Beaver Run has no named tributaries, it has two numbered tributaries: Trib 27552 and Trib 27553. The elevation near the mouth of Beaver Run is above sea level. The elevation of the stream's source is just over above sea level. Beaver Run is
19375267
Joyce Kilmer-Slickrock Wilderness


are located high in the Unicoi Mountains, on opposite slopes of Bob Stratton Bald, a grassy bald overlooking the southwest corner of the Joyce Kilmer-Slickrock Wilderness. Slickrock Creek rises on Stratton's northwestern slope and flows northeastward to its mouth along the Cheoah River. Little Santeetlah rises on Stratton's southeastern slope and flows southeastward to its mouth along Santeetlah Creek. The Joyce Kilmer Memorial Forest along Little Santeetlah Creek is a rare example of an old growth cove hardwood forest, an extremely diverse forest type unique to the Appalachian Mountains.
5916079
Willow Creek (Columbia River)


Willow Creek is a long tributary of the Columbia River, located in the U.S. state of Oregon. It drains of Morrow and Gilliam counties. Arising in the Blue Mountains, it flows generally northwest to its confluence with the Columbia River upstream of Arlington. Willow Creek's headwaters are located near Arbuckle Mountain in the Blue Mountains, southeast of Heppner. It flows north, then west, receiving the North Fork on the right and Skinners Fork on the left. Willow Creek Lake is formed by the tall Willow Creek Dam just upstream
18670510
Rice Canyon Creek


Rice Canyon Creek is a tributary creek or arroyo of Temescal Creek in Riverside County, California. Rice Canyon Creek has its source at the head of Rice Canyon at an elevation of 3440 feet in the Santa Ana Mountains at east of the 4313 foot peak on the north south divide of the range. It is a wash that runs down from the canyon mouth at 1631 feet to its mouth at its confluence with Temescal Creek near Alberhill, California at an elevation of 1220 feet. Rice Canyon Creek has a tributary, Bishop Canyon
18446548
Reyburn Creek


reaching the community of Muhlenburg. The creek then turns south-southeast for a few miles, flowing alongside Reyburn Road. Eventually, it turns south for more than a mile and receives an unnamed tributary from the left. The creek then turns southwest and flows alongside Shickshinny Mountain for more than a mile until it reaches its confluence with Shickshinny Creek in the village of Koonsville, in Union Township. Reyburn Creek joins Shickshinny Creek upstream of its mouth. The peak annual discharge of Reyburn Creek at its mouth has a 10 percent chance
19651804
Lees Creek (Lackawanna River tributary)


mouth. Lees Creek is not designated as an impaired stream. The creek is in "good condition" for most of its length. It experiences some flow loss upstream of US Business Route 6, but is still a perennial stream as far as the culvert that carries it under that highway. It eventually loses its flow completely. The elevation near the mouth of Lees Creek is above sea level. The elevation of the creek's source is between above sea level. The headwaters of Lees Creek are on wetlands on West Mountain
260961
Moonbeam Creek (British Columbia)


Moonbeam Creek is a stream in Thompson-Nicola Regional District in the Interior region of British Columbia, Canada. It is in the Pacific Ocean drainage basin and is a left tributary of the North Thompson River. The nearest communities to the mouth of the creek on British Columbia Highway 5 are Blue River south and Valemount north; the mouth of the creek is just downstream of confluence of the North Thompson River and the Albreda River, where the North Thompson River turns 90° right and heads south. The creek begins at an
4538801
Rausch Creek (Pine Creek tributary)


while the effluent concentration ranged from less than to . The elevation near the mouth of Rausch Creek is above sea level. The elevation near the creek's source is above sea level. Rausch Creek flows through a water gap known as Kohlers Gap (or Bear Gap), where it is flanked by steep slopes. A number of abandoned deep mine openings occur in this reach. The tributary East Branch Rausch Creek flows between Big Lick Mountain and Good Springs Mountain, while the tributary West Branch Rausch Creek flows between Big Lick Mountain
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