Range Creek [SEP] mouth of the watercourse
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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
Burpengary Creek


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


The Kindra Creek, a watercourse that is part of the Murrumbidgee catchment within the Murray–Darling basin, is located in the Riverina and South West Slopes regions of New South Wales, Australia. The Kindra Creek (technically a river) rises near Warre Warral trigonometry station southwest of , sourced by runoff from the Great Dividing Range. The creek flows generally southwest and then northwest before reaching its confluence with the Mimosa Creek to form Redbank Creek (itself a tributary of a series of watercourses that combine to form an old anabranch of
16669527
Wimmera River


Dividing Range below , between and , and flows generally north and west, through , , and , also forming the eastern boundary of the Little Desert National Park. It is joined by fourteen minor tributaries, including the Mackenzie River, before reaching its mouth at Lake Hindmarsh, near Jeparit. The river descends over its course. On the rare occasions that Lake Hindmarsh overflows, water flows via Outlet Creek to Lake Albacutya. In most years the Wimmera River's flow does not reach these terminal lakes, and the watercourse itself contracts
11861037
Panalatinga Creek


The Panalatinga Creek is an urban watercourse located in the southern suburbs of Adelaide in the Australian state of South Australia. Part of the Onkaparinga River catchment area that drains the western slopes of the Mount Lofty Ranges, the creek rises in the foothills in the southern Adelaide suburbs around Chandlers Hill through to Trott Park, South Australia and reaches its confluence with the Field River near the Southern Expressway. Now no more than a narrow suburban watercourse, Panalatinga Creek's earliest European recorded use was as the source of water for John Reynell's
6170452
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
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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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
Jackson Creek (Victoria)


The Jackson Creek (sometimes incorrectly spelled as Jacksons Creek) is a watercourse of the Port Phillip catchment, located in the outer northern suburbs of Melbourne, in the Australian state of Victoria. Formed by the confluence of the Distill, Gisborne and Slaty creeks that drain the southern parts of the Macedon Ranges, part of the Great Dividing Range through the Black Forest, the Jackson Creek rises northwest of , within the Rosslynne Reservoir. The creek flows east, then south, then south by east, joined by two minor tributaries before
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Little Catawissa Creek


's concentration of alkalinity ranges from and its pH ranges from 6.8 to 7.0. The concentration of water hardness in the creek's waters upstream of its mouth is . upstream of its mouth, the water hardness is and upstream of its mouth it is . The water hardness of the creek's waters upstream of its mouth is . At 1:00 P.M. on June 26, 1997, the air temperature in the vicinity of Little Catawissa Creek upstream of its mouth was . The water temperature of the creek at this place and time was .
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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
11853161
East Branch Rausch Creek


resource extraction. The average discharge of East Branch Rausch Creek near its mouth was measured to be per day. The pH of the creek near its mouth ranged from 4.5 to 6.8, with an average of 5.75. The concentration of alkalinity ranged from , with an average of . The iron concentration in East Branch Rausch Creek near its mouth was found to range from , with an average of . The manganese concentration ranged from . The concentration of aluminum ranged between , and averaged . The aluminum load requires a 95 percent reduction to
22040770
Deep Creek (Melbourne)


The Deep Creek is a watercourse of the Port Phillip catchment, located in the outer north western suburbs of Melbourne, in the Australian state of Victoria. Formed by the confluence of a number of smaller streams draining the north eastern slopes of the Macedon Ranges and the southern slopes of the Cobaw range, both ranges being constituent parts of the Great Dividing Range, the Deep Creek rises north of Mount Macedon, near Cobaw. The river flows generally east in a broad shallow valley, to the north of , before turning generally southwards
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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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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,
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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
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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Kolan River


then flows east and then finally north by east and reaches its mouth north of . The Kolan River is joined by nineteen tributaries including the main tributary, Gin-Gin Creek, a watercourse that is long. The lower reaches of the river are surrounded by sugar cane fields. The Mouth of Kolan River Regional Park is a protected area at the river mouth. The river descends over its course. Other water storage facilities that are supplied with water from the river include the Bucca Weir and the Kolan Barrage. "Macfadyena unguis
21876707
West Branch Rausch Creek


the creek is not impacted by sediment, unlike the nearby East Branch Rausch Creek. The average discharge of West Branch Rausch Creek near its mouth is per day. The pH of the creek has been measured to range from 6.1 to 6.5, with an average of 6.3. The alkalinity concentration ranged from , with an average of . The iron concentration in West Branch Rausch Creek near its mouth ranges from , with an average of . The concentration of manganese ranges from , with an average of . The aluminum concentration ranges between less
160943
Macumba Station


by Gina Reinhart (who holds a 2/3 stake) a China's Shanghai CRED (which holds the remaining 1/3). The station contains a range of terrains including sandhills, mulga woodland, watercourses with redgums and areas of desert and gibber plain. Watercourses crossing the property include the Macumba River, Stevenson Creek and Alberga Creek, each having several waterholes some of which are almost permanent, except in times of prolonged drought. Willow Bore, which was sunk by the government prior to 1892, can provide per day, enough to
20712732
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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Nescopeck Creek


15 percent and in the northern line of hills, there is an area with a slope of over 15 percent. The elevation at Nescopeck Creek's mouth and along Nescopeck Creek for a few miles upstream is in the range of above sea level. The elevation of the creek's watershed north of the northernmost line of hills is in the range of . The central part of the Nescopeck Creek watershed, south of the northernmost line of hills, including the mouth of Black Creek, is also in this range. The area close
18926678
Tycannah Creek


The Tycannah Creek, a watercourse that is part of the Barwon catchment of the Murray-Darling basin, is located in the Orana region of New South Wales, Australia. The creek rises on the northern side of the Nandewar Range and flows into the Mehi River downstream from Moree. On its way to the Mehi River, it flows through the village of Terry Hie Hie. There are five main creeks which feed into Tycannah Creek which are Bald Hill Creek, Crossing Creek, Bowman Creek, Berrygil Creek and Brigalow Creek.
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Riddells Creek


Riddells Creek is a town in Victoria, Australia, located in the Shire of Macedon Ranges. It is located in between the cities of Bendigo and Melbourne. Riddells Creek is also the name of the main watercourse which flows through the township, and which is a tributary of Jacksons Creek to the south. The town is served by Riddells Creek railway station on the Bendigo line. At the , Riddells Creek had a population of 2976. Riddells Creek was originally settled by John Carre Riddell and Thomas Ferrier Hamilton in 1841, when
20002262
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
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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
17835729
Thomes Creek


Thomes Creek is a major watercourse on the west side of the Sacramento Valley in Northern California. The creek originates in the Coast Ranges and flows east for about to join the Sacramento River, at a point about northeast of Corning in Tehama County. Thomes Creek is a highly seasonal stream and drains a mostly rural watershed of some . There are no permanent dams on the creek, although there are some small diversions for agriculture and domestic water supply, and the overall water quality is considered good. The upper of Thomes Creek are
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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
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Yarriambiack Creek


The Yarriambiack Creek, an inland intermittent watercourse of the Wimmera catchment, is located in the Wimmera region of the Australian state of Victoria. Rising on the northern slopes of the Great Dividing Range, the Yarriambiack Creek flows generally north and drains into Lake Coorong, one of a series of ephemeral lakes, northeast of . The name of the creek is thought to derive from "Jarambuik", the name of a sub-group of the indigenous Wotjobaluk people; also once spelt Yarriambiac, Yarramberger and Yarrambeak. The Yarriambiack Creek is
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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
16777910
Thomson River (Queensland)


the Great Dividing Range, the northernmost headwaters of the river begin as Torrens Creek, inland from Charters Towers. The watercourse becomes the Thomson just north of the town of Muttaburra, where the channels of Landsborough Creek, Towerhill Creek and Cornish Creek meet. Aramac Creek joins the river from the east, south of Muttaburra and Maneroo Creek flows from the west, joining the Thomson south of Longreach. Just to the west of Longreach the river is crossed by the Landsborough Highway. The river continues in a south westerly direction, passing
17016365
Officer Creek


The Officer Creek, part of the Lake Eyre basin, is an ephemeral watercourse located in the Far North region in the Australian state of South Australia. The creek rises in the Musgrave Ranges and flows through the Aboriginal community of Kaltjiti in the Anangu Pitjantjatjara Yankunytjatjara Lands. With the Ammaroodinna and Currie Creeks, the creek empties into the Warburton River. Officer Creek is usually a dry sandy bed and only flows at times of very high rainfall. In September 1873 during his second trip into the South Australian interior, Ernest Giles and
18991160
Jacobs Creek (Australia)


Jacobs Creek, formerly known as Jacob's Creek, is a small creek located in Mid North region of the Australian state of South Australia. Jacobs Creek rises in the Barossa Ranges and flows westward through the wine-producing region of the Barossa Valley, approximately north of Adelaide. The creek is only several kilometres long and eventually meets the North Para River at . The watercourse is studded with ancient and picturesque River Red Gums. It was first discovered (but not named) by Europeans in December 1837 by an expedition led Colonel
20214153
Mirrool Creek


The Mirrool Creek, a watercourse that is part of the Lachlan sub-catchment of the Murrumbidgee catchment within the Murray–Darling basin, is located in the Riverina region of New South Wales, Australia. The course of the Mirrool Creek is indefinite at various locations. The Mirrool Creek (technically a river) rises in the Ingalba Nature Reserve, about west by south of the town of , sourced by runoff from the Great Dividing Range. The creek flows generally north northwest, west, north by west, and west again
16669600
Peelwood Creek


The Peelwood Creek, a watercourse that is part of the Lachlan sub-catchment of the Murrumbidgee catchment within the Murray–Darling basin, is located in the South West Slopes region of New South Wales, Australia. The Peelwood Creek (technically a river) rises in remote country north of and , sourced by runoff from the Great Dividing Range. The creek flows generally north, then northeast, then northwest by west, before reaching its confluence with the Tuena Creek, itself a tributary of the Lachlan River, east of ,
16669672
Little Wapwallopen Creek


it reaches its confluence with the Susquehanna River. Little Wapwallopen Creek is approximately long. It joins the Susquehanna River upriver of its mouth. Little Wapwallopen Creek has numerous unnamed tributaries and two named tributaries: Nuangola Outlet and Pond Creek. Pond Creek joins Little Wapwallopen Creek upstream of its mouth. Its watershed has an area of . Nuangola Outlet joins Little Wapwallopen Creek upstream of its mouth. Its watershed has an area of . The discharge of Little Wapwallopen Creek near its mouth has been observed to range from . The turbidity level of
14488710
Carrizo Creek (Imperial County, California)


Valley then north through Carrizo Gorge and Carrizo Canyon, into Carrizo Valley where it is joined on the left by Vallecito Creek, as it turns east through the Carrizo Badlands where 3 miles east of the site of the old Carrizo Creek Station, at an elevation of 322 feet / 98 meters, it becomes Carrizo Wash. Carrizo Wash terminates at its confluence with San Felipe Creek at . Carrizo Creek, its wash and its tributary, Vallecito Creek, were the watercourses that carved the pathway from the Peninsular Ranges of Southern California through the
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Tennant Creek


watercourse of Tennant Creek in 1872. Two years later, the solid stone buildings of the Tennant Creek Telegraph Station that remain on the site today, were completed by the occupants of the station. This is one of the four remaining original telegraph stations in Australia. Tennant Creek was the site of Australia's last gold rush during the 1930s and at that time was the third-largest gold producer in Australia. The Tennant Creek Telegraph Station remained an isolated outpost until that time. Gold was discovered in the ranges three miles north
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Rocky Ponds Creek


The Rocky Ponds Creek, a watercourse that is part of the Murrumbidgee catchment within the Murray–Darling basin, is located in the South West Slopes region of New South Wales, Australia. The Rocky Ponds Creek (technically a river) rises below Rocky Ponds, approximately east of the town of , on the south western slopes of the Great Dividing Range. The creek flows generally west and then south before reaching its confluence with the Jugiong Creek (itself a tributary of the Murrumbidgee River) near the locality of Hidden Brook,
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Strawberry Creek


Strawberry Creek is the principal watercourse running through the city of Berkeley, California. Two forks rise in the Berkeley Hills of the California Coast Ranges, and form a confluence at the campus of the University of California, Berkeley. The creek then flows westward across the city to discharge into San Francisco Bay. The north fork has also been called "Blackberry Creek", a name which has also been applied to another small creek in Berkeley, a portion of which has been daylighted through Thousand Oaks School Park. The canyon in
20920214
Jerrawa Creek


The Jerrawa Creek, a watercourse that is part of the Lachlan sub-catchment of the Murrumbidgee catchment within the Murray–Darling basin, is located in the South West Slopes region of New South Wales, Australia. The Jerrawa Creek (technically a river) rises on the slopes of the Great Dividing Range northwest of near the localities of Dixon and Jerrawa, and flows generally east by north, then north by east before reaching its confluence with the Lachlan River north of the locality of . The course of the creek is approximately
16173081
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
Little Mehoopany Creek


upstream of its mouth. Little Mehoopany Creek is not designated as an impaired waterbody. There are zero miles of impaired streams in the creek's watershed. The average discharge of Little Mehoopany Creek is at a monitoring station near its mouth. The maximum time for water to flow from the headwaters to the mouth is 8 hours and 50 minutes. In a study of the creek's watershed by the Mehoopany Creek Watershed Association in the early 2000s, the water temperature of the creek at a fire company property ranged from . At a
19007952
Cranberry Creek (Stony Creek tributary)


if it is . The pH of Cranberry Creek near its mouth ranges from 4.8 to 5.6, with an average of 5.08. The discharge of Cranberry Creek near its mouth is 1502.67 gallons per minute. However, it has been known to run dry. The elevation near the mouth of Cranberry Creek is above sea level. The elevation of the creek's source is between and above sea level. A reservoir known as the Grape Run Reservoir is located on the upper reaches of Cranberry Creek. The creek also flows through the Hazleton
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Mehoopany Creek


others. North Fork Mehoopany Creek joins Mehoopany Creek upstream of its mouth and its watershed has an area of . Stony Brook joins Mehoopany Creek upstream of its mouth. The watershed of this brook has an area of . The average rate of precipitation in the watershed of Mehoopany Creek ranges from per year. Mehoopany Creek is acidic in early spring. The elevation near the mouth of Mehoopany Creek is above sea level. The elevation of the creek's source is between and . Its elevation decreases at a rate of per mile in its
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Sisters Creek, Tasmania


Sisters Creek is a locality and small rural community in the local government area of Waratah-Wynyard, in the North West region of Tasmania. It is located about north-west of the town of Wynyard. The Bass Highway passes through from east to west, and the watercourse named Sisters Creek flows through from south to north. The 2016 census determined a population of 134 for the state suburb of Sisters Creek. An 1851 map of Tasmania names a range of hills in the vicinity as the “Sisters”. The name
14533185
Rudall River


The Rudall River is an ephemeral river in the Pilbara region of Western Australia. The entire length of the river is located within the boundaries of the Karlamilyi National Park. The headwaters of the river lie below the Watrara Range near Island Hill and flows eastward until it discharges into Lake Dora. The river is unique in the region as it is a major watercourse with reliable water sources and many permanent pools. The river has a total of nine tributaries including; Watrara Creek, Rooney Creek, Poonemerlarra Creek and Dunn Creek. The
17312348
Arroyo Grande Creek


Arroyo Grande Creek is a major stream in San Luis Obispo County on the Central Coast of California. The creek flows in a southwesterly direction, from the Santa Lucia Range to the Pacific Ocean. It is a major source of water supply for southern San Luis Obispo County. The creek's name is derived from the Spanish for "large watercourse", and was sometimes called the "Roaring Grande" in the 19th century due to its propensity for flooding. The city of Arroyo Grande, established in 1867, was named after
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Mangrove Creek (New South Wales)


The Mangrove Creek, a perennial river that is part of the Hawkesbury-Nepean catchment, is located in the Central Coast region of New South Wales, Australia. The Mangrove Creek rises about southwest of Mount McQuiod below the Hunter Range, and flows generally south, joined by six minor tributaries, before reaching its confluence with the Hawkesbury River between Spencer and Wendoree Park. The river descends over its course. Although called a creek, the watercourse is designated as a river, and its headwaters are impounded by the Mangrove Creek Dam
16579101
Wiconisco Creek


concentration of alkalinity ranges from 3.2 to 70.17 milligrams per liter, depending on the site. The daily load ranges from . The elevation near the mouth of Wiconisco Creek is above sea level. The highest elevation in the watershed is above sea level. This occurs on Big Lick Mountain. From river mile 37.5 to the mouth, the elevation of the creek decreases at a rate of per mile. Some strainers are situated on Wiconisco Creek between Lykens and Loyalton. The creek flows through a gorge for several miles in its lower reaches
18094175
Briar Creek (Susquehanna River tributary)


mouth ranges from to , with a median of . Upstream of West Branch Briar Creek, the creek's pH ranges from to . The median is . Near the creek's headwaters, the pH ranges from to and has a median of . West Branch Briar Creek has a minimum pH of , a median pH of , and a maximum pH of . Not far from its headwaters, East Branch Briar Creek has a pH range of to and a median pH of . Near Briar Creek Reservoir, it has a pH range of
8710477
Congewai Creek


Congewai Creek, a watercourse of the Hunter River catchment, is located in the Hunter district of New South Wales, Australia. The Congewai Creek rises below Myall Range, about southeast of Quorrobolong trig station within the Watagans National Park. The river flows generally west by south, then north by west, then northwest by north, then west by north, then west southwest, and then south, joined by four tributaries including the Cedar Creek, before reaching its confluence with the Wollombi Brook near . The river descends over its course
6702099
Brown Hill Creek


Brown Hill Creek, also known as Willawilla in the Kaurna language, is a watercourse flowing from the Adelaide Hills through in the inner south suburbs of the Adelaide metropolitan area, in the Australian state of South Australia. It is part of the Patawalonga River catchment. The creek rises on the western slopes of the Mount Lofty Ranges near Crafers and flows generally in a west-north-west direction through the suburb of Brown Hill Creek, south of Brown Hill, a prominent hill rising immediately south-east of Mitcham village,
826658
Eight Mile Plains, Queensland


of the Aboriginal clan formerly occupying this area is uncertain. According to one source they are likely to have been the Chepara clan of Eight Mile Plains who spoke Turrbal. The Yerongpan of Oxley Creek who are said to have claimed the area from Brisbane to Ipswich. Another source claims they were the Yagarabal, who ranged from Brisbane to the Logan River and west to Moggill Creek. The Aborigines used a trail which later became Logan Road. This trail bisected many creeks including the Mimosa Creek and Bulimba Creek watercourse. Eight Mile Plains
9197951
Mouse Creek (Schwaben Creek tributary)


its mouth. No stream segment in the watershed of Mouse Creek is designated as an impaired waterbody. The headwaters reach of the creek was selected as the reference watershed for the Dalmatia Creek total maximum daily load. In 2001, the water temperature of Mouse Creek at Urban ranged from in two measurements. The discharge ranged from and the specific conductance ranged from 250 to 350 micro-siemens per centimeter at . The creek's pH was slightly alkaline, ranging from 7.7 to 8.4 and the water hardness ranged from . In 2001,
11344914
Nanticoke Creek


. At the creek's mouth, the pH was 6.8 in October 1999. The net alkalinity concentration was 40.0 milligrams per liter at the mine discharge in June, 3.70 milligrams per liter at the discharge in October, and 18.0 milligrams per liter at the mouth in October. During the 1970s, the acidity concentration of the creek's waters ranged from 18 to 365 parts per million on the main stem. The alkalinity concentration ranged from 0 to 3 parts per million. The specific conductance of the creek below the mine discharge was
8894245
East Branch Fishing Creek


pH occurs on Shanty Run. At two sites on East Branch Fishing Creek itself, the creek's pH is 5.34 (at its confluence with Lead Run) and 5.63 (at its mouth). The average amount of aluminum in the streams in the watershed ranges from 0.024 milligrams per liter to 0.366 milligrams per liter. The highest concentration occurs on Ore Run and the lowest concentration occurs on the mouth of East Branch Fishing Creek. One stream in the watershed, Big Run, has a pH range of less than 3 to
15548184
King Sound


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


creek near Dallas in several measurements ranged from . The elevation near the mouth of Abrahams Creek is above sea level. The elevation of the creek's source is between above sea level. The highest point in the watershed is on Bunker Hill, at slightly over above sea level. The lowest point in the watershed is at the creek's mouth. There are plains to the north of Abrahams Creek. Wetlands known as the Abrahams Creek Wetlands are in the vicinity of the creek. They consist of several ponds along the side of
6874738
Huntington Creek (Pennsylvania)


Creek increase the size of Fishing Creek by a factor of two. The average annual rate of precipitation in the watershed of Huntington Creek ranges between and . The elevation near the mouth of Huntington Creek is above sea level. The elevation of the creek's source is between and above sea level. Upstream of Kitchen Creek, its elevation decreases by per mile. Between Kitchen Creek and Pine Creek, the elevation decreases by per mile. Between Pine Creek and the mouth, the elevation decreases by per mile. The headwaters of Huntington
9589306
Warrior Creek (Pennsylvania)


at most measurements. During several measurements in 1973 and 1974, the water temperature of Warrior Creek ranged from at the outlet of a culvert on Middle Road. At the inlet of the culvert, the water temperature ranged from . At the outlet of the culvert on Middle Road, the creek's pH ranged from 4.50 to 7.40. At the inlet of the culvert, the pH ranged from 6.55 to 8.45. The elevation near the mouth of Warrior Creek is above sea level. The elevation of the creek's source is between
9475882
Hop Bottom Creek


ranged from . The sulfate and chloride concentrations in the creek's filtered water ranged from and . The concentration of nitrate in the creek's filtered waters ranged from . The elevation near the mouth of Hop Bottom Creek is above sea level. The elevation of the creek's source is between above sea level. Hop Bottom Creek is a relatively small stream that meanders through a deep valley. In its upper reaches, it has a clean channel. At the outlet of Heart Lake, the creek's channel is wide and deep.
8480802
Raven Creek


Slightly more than a mile downstream, it reaches its confluence with Fishing Creek. Raven Creek joins Fishing Creek upstream of its mouth. East Branch Raven Creek is the main tributary of Raven Creek. It is long. The elevation near the mouth of Raven Creek is above sea level. The elevation of the creek's source ranges from . The watershed of Raven Creek has an area of . Two covered bridges historically crossed Raven Creek: the Joe Ash Covered Bridge and the McHenry's Mill or Paperdale Covered Bridge. The former was
18814056
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
14845636
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
Antelope Creek (Little Butte Creek)


Antelope Creek is a tributary of Little Butte Creek in the U.S. state of Oregon. It begins in the foothills of the Cascade Range southeast of Medford and flows generally northwest to meet the larger creek downstream of Eagle Point and about by water from Little Butte Creek's mouth on the Rogue River. The creek passes under Oregon Route 62 (Crater Lake Highway) between Eagle Point and White City, slightly before entering Little Butte Creek. Named tributaries of Antelope Creek from source to mouth are Yankee Creek, Quarter Branch, and Dry
8896527
Briar Creek (Susquehanna River tributary)


to cubic feet per second (cfs), with a median of cfs. Just upstream of West Branch Briar Creek's confluence with the creek, the discharge ranges from to cfs, with a median of cfs. Near the mouth of the creek, the discharge ranges from to cfs. There is a median discharge of cfs at this point. On East Branch Briar Creek about two miles from its headwaters, the discharge ranges from to with a median discharge of cfs. Near Briar Creek Reservoir, East Branch Briar Creek's
8710474
Creasy Creek


It is known as Reilly Creek. Reilly Creek has its own tributary, which is known as Mill Creek. The pH of the waters of Creasy Creek ranges from 6.9 to 7.2, making it the only headwater tributary of Nescopeck Creek to have alkaline waters. The total concentration of alkalinity is between 12 and 24 milligrams per liter. The concentration of water hardness ranges between 15 and 24 milligrams per liter. The specific conductance of the creek's waters ranges from 49 to 74 micromohs. The elevation near the mouth of Creasy Creek
6737777
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
Cottonwood Creek (San Luis Creek)


Cottonwood Creek, originally Arroyo Alamos, a tributary stream of San Luis Creek, in Merced County, California. Its mouth, before the San Luis Dam was built across the course of San Luis Creek, originally was at its confluence with San Luis Creek at at approximately 250 feet / 76 meters. Today its mouth is located in the foothills of the Diablo Range, where Cottonwood Creek enters the north side of San Luis Reservoir at an elevation 548 feet / 167 meters. The source of the creek is at at an elevation
2435783
Small's Creek


Small's Creek was one of the three watercourses that flowed into Small's Pond, a small body of water of several acres in area, located near the intersection of Queen Street and Kingston Road, in Toronto, Ontario. There is a small plain between the shore of Lake Ontario and the bluffs which marked the shore of the larger Glacial Lake Iroquois, Bedrock was shallow on the plain. Smalls Creek, Tomlin's Creek, the other watercourse that drains into Smalls Pond, and Ashbridge's Creek to the east were all
7103201
Tangascootack Creek


in the 1800s to be found near the mouth of Tangascootack Creek, as well as in other locations. This bed ranged from to thick and contained iron pyrite as well. It was at least underground. An 1854 report estimated that there were of workable coal near Tangascootack Creek. The Tangascootack Creek watershed consists chiefly of valleys and rolling and broken hills. The creek's river channel is relatively sinuous. It is mostly sandstone and shale with some coal. The slope of the creek is per mile, and its mouth's elevation
20735555
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
Pine Creek (Solomon Creek tributary)


-southwest for several tenths of a mile, crossing Pennsylvania Route 309. The creek then turns northwest, passing through a small pond and then reaching its confluence with Solomon Creek after a few tenths of a mile. Pine Creek joins Solomon Creek upstream of its mouth. The water temperature of Pine Creek ranges from . No iron has been recorded in the creek. Its pH ranges from 5.5 to 6.5, the concentration of acidity ranges from 17.1 to 51.3 milligrams per liter, and the concentration of alkalinity is 17.1 milligrams per liter
3686343
You Yangs


yet sparse in their imagery — unquestionably of the Australian bush. The nearest settlements include; Two watercourses pass through or by the ranges: Hovells Creek originates in the western parts of the ranges, while Little River flows around the ranges to the north and east. Contrary to popular belief, the You Yangs are not the remains of a volcano. They are an inselberg or monadnock, and the granite that forms them was originally a mass of magma that had worked its way up into the surrounding sedimentary rocks during the Devonian period
17618721
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
Jamison Valley


northern escarpment is deeply serrated, having been carved up by watercourses over millions of years. Watercourses include Jamison Creek, Valley of the Waters Creek, Gordons Creek, Leura Falls Creek, Kedumba River and Causeway Creek. There are also numerous waterfalls, including Wentworth Falls, Empress Falls, Vera Falls, Gordon Falls, Leura Falls and Katoomba Falls. In this part of the valley there was formerly a sewage treatment plant, not far below the northern escarpment. It was serviced by a dirt road that went up to Kings Tableland
16356216
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
Corn Creek (Millard County)


Corn Creek, also called Kanosh Creek, is a stream in Millard County, Utah. Its mouth is located in the Pahvant Valley. Its source is at the confluence of East Fork Corn Creek and West Fork Corn Creek in the Pahvant Range. The location near the mouth of Corn Creek was originally a stopping place known as "Willow Flats" for the early travelers on the Mormon Road. On January 17, 1851, George A. Smith, leader of Mormon colonists who were on their way to establish the colony at Parowan
11503316
Little Wapwallopen Creek


. The Berwick Axis, which is also known as the Montour Axis, crosses the Susquehanna River half a mile downstream of the mouth of Little Wapwallopen Creek. There is concealed Marcellus shale near the creek in Hollenback Township. The water temperature of Little Wapwallopen Creek near Wapwallopen was measured several times during the 1970s. The values ranged from in May 1971 to in September 1972. The watershed of Little Wapwallopen Creek has an area of . The mouth of the creek is in the United States Geological Survey quadrangle of Berwick. However,
14488718
Leggetts Creek


to its mouth, a distance of . It is stocked with trout and also is inhabited by some non-game species. The drainage basin of the creek upstream of Summit Lake Creek is a Coldwater Fishery and a Migratory Fishery. From Summit Lake Creek downstream to its mouth, the drainage basin is a Trout Stocked Fishery and a Migratory Fishery. In a 2013 fishery survey of the creek, nine brown trout were observed. Their lengths ranged from 84 to 316 millimeters, with an average of 139 millimeters. The vast majority
17082200
Esk–Hampton Road


formerly 85) from Toowoomba to the Leichhardt Highway, and the southern section of the Leichhardt Highway (also National Route A39) to Goondiwindi. From a historical perspective the Esk–Hampton Road consists of three sections of approximately equal length. The eastern section, from Esk to the foothills of the Great Dividing Range, was developed along Redbank Creek (the watercourse) to provide access to stands of timber, and to a sawmill that was located at Redbank Creek (the locality). Subsequently, it serviced farms that were established
10806569
Bladensburg National Park


Bladensburg is a national park in Shire of Winton, Queensland, Australia. The park is 1152 km northwest of Brisbane, and just south of the town of Winton. Birds common to the area include the painted firetail, rufous-crowned emu-wren and rufous-throated honeyeater. The park features grassland plains, river flats, sandstone ranges and flat-topped mesas. The main watercourse in the park is the often dry Surprise Creek. During floods the creek becomes a braided channel. The landscape to the south of the
14585826
Amador Valley


Amador Valley is a valley in eastern Alameda County, California and is the location of the cities of Dublin and Pleasanton. The valley is bounded by the foothills of the Diablo Range on the north and south, Pleasanton Ridge to the west, and Livermore Valley to the east. Watercourses draining the Amador Valley include South San Ramon Creek, Tassajara Creek, Arroyo Mocho, Arroyo Valle and Arroyo de la Laguna. From prehistoric times much of the eastern part of the Amador Valley consisted of a lake known as Tulare Lake. With
18474659
Buffalo Creek (West Branch Susquehanna River tributary)


Rapid Run joins Buffalo Creek upstream of its mouth and its watershed has an area of , while North Branch Buffalo Creek joins Buffalo Creek upstream of its mouth and its watershed has an area of . The pH of the waters of Buffalo Creek at three sites ranges from 5.0 to 6.7. Out of six times that the pH of the waters of the creek was measured in the springs and summers of 2010 and 2012, the lowest pH, 5.0, occurred at the location BC-6 on July 27, 2012. The highest pH,
6459885
Burke, Wills, King and Yandruwandha National Heritage Place


he travelled past the Flinders Ranges to discover a horseshoe of impassable salt lakes: LakeTorrens, Lake Eyre, Lake Blanche, Lake Callabonna and Lake Frome. Eyre's expedition coincided with a dry period; from the aptly named "Mount Hopeless" he described inland South Australia as a "dreary waste". In 1844 Charles Sturt followed Eyre and discovered the Strzelecki Creek which he named after his colleague, Paul Edmond de Strzelecki, and the main watercourses which fed Lake Eyre: Cooper Creek, Eyre Creek and the Georgina River.
9736654
Catawissa Creek


, Dark Run, and Little Catawissa Creek, but before picking up Tomhicken Creek, Catawissa Creek's pH ranges from 3.2 to 6.4 and averages 4.96. After the confluence with Tomhicken Creek, Catawissa Creek's pH ranges from 4.7 to 5.4. Despite the presence of acid mine drainage in Catawissa Creek, its waters are largely clear. From Catawissa Creek's source to Mainville, the creek's river valley is steep and narrow, and from Mainville to the creek's mouth, the river valley is more rolling. Interbedded sedimentary rock
2424877
Hull Creek (Lackawanna River tributary)


modern course, but at that point turned to the south instead of flowing along its present course. In a 2013 study, the water temperature of Hull Creek was found to range from . The average temperature was . The minimum and maximum temperatures were out of the ideal range, but the average temperature was in the ideal range. The watershed of Hull Creek has an area of . The part of the watershed that is upstream of the border between Blakely and Scott Township has an area of . The mouth of the creek is
19419778
Strzelecki Creek


The Strzelecki Creek, part of the Lake Eyre basin, is an ephemeral watercourse located in the Australian state of South Australia. The Strzelecki is a distributary of Cooper Creek and branches off near the town of Innamincka and flows in a southerly direction thought the Strzelecki Desert for about towards Lake Blanche. While being feed by the Cooper Creek, it does have its own catchment and can flow independently after ‘heavy localised storms.’ Flows on ‘exceptional’ occasions can reach Lakes Blanche, Callabonna, Frome and Gregory. Its watercourse
15890487
Sugar Run Creek


-siemens per centimeter at and 163 micro-siemens per centimeter at . The concentration of dissolved oxygen in the waters of Sugar Run Creek is 10.0 milligrams per liter and the concentration of carbon dioxide ranges from 1.2 to 1.8 milligrams per liter. The pH of the creek's waters ranges between 7.0 and 7.7. The concentration of bicarbonate in the creek ranges between 7.0 and 53 milligrams per liter and the concentration of carbonate is 0.0 milligrams per liter. The elevation near the mouth of Sugar Run Creek is above sea level. Trout
1441250
Briar Creek (Susquehanna River tributary)


studied location in the drainage basin. Near its mouth, the temperature ranges from . The median temperature is . On West Branch Briar Creek, the temperature is a minimum of , a median of , and a maximum of . Two miles downstream of East Branch Briar Creek's headwaters, the median temperature is and the range is . Near Briar Creek Reservoir, the water temperature has a minimum of , a maximum of , and a median of . Briar Creek is slightly alkaline on average. The pH of the creek near its
8710476
Millstream Chichester National Park


Millstream Chichester National Park is a national park in the Pilbara region of Western Australia, located north of the state capital, Perth. The park is made up of the old Millstream Station, which is on the Millstream Creek, just before it joins Fortescue River, one of the few permanent watercourses in the area and the Chichester Range. The area is homeland of the Yinjibarndi people. Millstream Creek was named by the explorer Francis Thomas Gregory in 1861. He reported the favourable grazing prospects. The first pastoral lease was taken up
13625908
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