Piner Creek [SEP] mouth of the watercourse
[{"answer": "Santa Rosa Creek", "provenance": [{"wikipedia_id": "9149896", "title": "Piner Creek", "start_paragraph_id": 1, "start_character": 131, "end_paragraph_id": 1, "end_character": 219, "bleu_score": 1.0, "meta": {}, "section": "Section::::Abstract."}]}]
Piner Creek


values scored by Colgan Creek. Most of the watercourse has been modified to accommodate urban development within Santa Rosa, and some alterations have been conducted to achieve higher levels of flood control. The dominant tree along the banks of Piner Creek is the coast live oak, "Quercus agrifolia"; within the streambed, a large number of cattail, "Typha latifolia", stands are observed. A considerable number of bird species are found along the stream banks of Piner Creek. Based upon benthic macroinvertebrate sampling in Piner Creek, a
10153678
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
10153674
Piner Creek


riprap lined channel, which has been modified in association with some alterations to lower Fountaingrove Lake. Thence Piner Creek flows northerly of an upscale modern office park before crossing under Redwood Highway and U.S. Highway 101. West of the U.S. 101 Freeway, Piner Creek winds through a retail and commercial/industrial area, before crossing under Piner Road near Coffey Lane; in this reach there is a large historic release to groundwater of solvent from manufacturing uses stemming back to the 1970s and 1980s. Water quality of Piner Creek is characterized by pH
10153672
Piner Creek


of the watershed is developed as residential use, and about one-sixth of the land is open space or used for recreation or agriculture. One of the early surviving architectural features of Sonoma County is within the Piner Creek catchment basin: A well preserved "Round Barn", constructed in 1899, a testament to the 19th century pasturage uses within this watershed. Piner Creek originates in the lower Mayacmas Mountains at Fountaingrove Lake. From its outlet at Fountaingrove Lake, Piner Creek flows down a relatively steep gradient, initially over a
10153671
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
Piner Creek


Rosa Plain, through which the middle and lower reaches of Piner Creek flow. Occasional basaltic outcrops are seen in the upper reach of Piner Creek, betraying the volcanic origin of the Mayacmas Mountains. The upper reach of Piner Creek watershed is characterized by presence of Goulding cobbly clay loam soil; this soil has slopes of up to 15 percent and is subject to moderate erosive potential. The actual soil depth is typically only about and may contain up to 25 percent cobblestones. Historic use of this soil has been for grazing. As
10153675
Piner Creek


as the floodplain formed. The upper soil surface of the Zamora material is grayish-brown hard, firm, sticky and plastic. Permeability is moderately slow and fertility is high for these lower reach soils, which has resulted in historic orchard use and present day vineyards. Formal habitat evaluation of Piner Creek has been conducted along with a number of other streams within the Laguna de Santa Rosa watershed. Habitat value of Piner Creek was found to be "Fair" compared to higher values scored by Matanzas Creek and Brush Creek and lower
10153677
Piner Creek


levels that are mildly basic, with upper reach pH levels about 8.5, declining to lower reach levels at 7.8 just above the discharge to Santa Rosa Creek. The headwaters soils are typically of pH about 6.9. Water quality of Piner Creek is generally low in turbidity, except for highest flow periods resulting from heavy rains; the water is free from odor. Springtime water temperatures are typically in the range of 60 to 65 degrees Fahrenheit (16 to 18 degrees Celsius). Piner Creek terminates at its confluence with Santa Rosa Creek
10153673
Piner Creek


Piner Creek is a stream in northeast Santa Rosa, California, United States () which originates as an outlet of Fountaingrove Lake. Piner Creek discharges to Santa Rosa Creek which in turn joins the Laguna de Santa Rosa. The upper reaches in the foothills of the Mayacamas Mountains are at elevations of 200 to 300 feet (60 to 90 meters), while the lower and middle reaches are located on the Santa Rosa Plain at elevations of between the 110- and 140-foot (33- and 43-meter) contours; therefore, these lower reaches
10153669
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
Piner Creek


have a gradient of about 1:250 toward the southwest. Geologic studies in the lower and middle reaches of Piner Creek indicate groundwater levels ranging from three to 15 feet (one to 5 meters) below the surface. Prior to extensive urban development of the middle and lower reaches, the landscape earlier bore extensive agricultural uses including plum orchards, which fruit was subsequently processed for prunes. The Piner Creek watershed consists of , approximately three-fourths of which lies within the municipal boundaries of the city of Santa Rosa. About one-third
10153670
Jackson Creek (Toronto)


Jackson Creek is a watercourse that flows into Lake Ontario near 10th Street, in the New Toronto neighbourhood of Etobicoke, a suburb of Toronto, Ontario, Canada. It is part of the Great Lakes Basin. Its headwaters were approximately five kilometers northwest—north of Bloor Street, near Highway 427. Portions of the watercourse remain above-ground today. The creek is named for Jackson Farm, the historical location of its mouth. Even though lost, for now, Jackson Creek is a strong candidate for day-lighting with
14363282
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
18572296
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
14371599
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
1358403
Piner Creek


the stream approaches the Santa Rosa Plain immediately east of U.S Highway 101, slopes diminish to a gradient of five to 15 percent and the predominant soil type is Felta very gravelly loam. This Felta soil is characterized by an upper surface grayish-brown color and texture of a fine, sticky and plastic nature. West of U.S. Highway 101, Piner Creek flows over the Santa Rosa Plain at gradients of less than two percent. Here the predominant soil type is Zamora silty clay loam, which has been deposited as an alluvial fan
10153676
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
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
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
13617662
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
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
6040227
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
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,
2484722
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
9459104
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
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
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
Santa Rosa, California


Moon, and the Sonoma Creek watershed known as the Sonoma Valley. The city's western edge lies in the Laguna de Santa Rosa catchment basin. The city is in the watershed of Santa Rosa Creek, which rises on Hood Mountain and discharges to the Laguna de Santa Rosa. Tributary basins to Santa Rosa Creek lying significantly in the city are Brush Creek, Matanzas Creek, and Piner Creek. Other water bodies within the city include Fountaingrove Lake, Lake Ralphine, and Santa Rosa Creek Reservoir. The prominent visual features east of
17475324
Sonoma County, California


, riparian forests, oak woodlands and grasslands... As the receiving water of a watershed where most of the county's human population lives, it is a landscape feature of critical importance to Sonoma County's water quality, flood control, and biodiversity. The Laguna's largest tributary is Santa Rosa Creek, which runs through Santa Rosa. Its major tributaries are Brush Creek, Mark West Creek, Matanzas Creek, Spring Creek and Piner Creek. Santa Rosa Creek was shown to be polluted in Sonoma county first flush results. The boundary
3667781
Santa Rosa Creek


of the middle and lower reach banks. A significant stream restoration project was created in the downtown Santa Rosa reach in the late 1990s, allowing steelhead and coho salmon to migrate to productive upstream spawning areas. Major tributaries to Santa Rosa Creek include Brush Creek, Piner Creek, Matanzas Creek and Colgan Creek. Annual precipitation in the Sonoma Creek watershed is about 24 to 38 inches (60 to 70 centimeters). Water quality sampling in the Railroad Square area of Santa Rosa indicate coliform bacteria standards are often exceeded. Archaeological data demonstrates
14774368
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
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
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
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
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
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
Keswick Creek


Keswick Creek and Glen Osmond Creek together form a watercourse flowing through the inner south-eastern, south-western and western suburbs of the Adelaide metropolitan area, in the Australian state of South Australia. The watercourse is part of the Patawalonga River catchment. The water course has been extensively altered since European settlement to manage stormwater flows and avoid flooding in the heavily populated urban areas through which it passes. The source of Glen Osmond Creek is in the south-eastern suburb of Glen Osmond, abutting the Adelaide Hills. Its original
19066323
Klamath River


of beaver from 1915–1917 on High Prairie Creek at the mouth of the Klamath River near Requa, California. Within a matter of years, the plentiful beavers in the Klamath Basin had been mostly wiped out. Beaver dams had previously been an important factor in stream habitat in the Klamath River watershed, helping to moderate the power of floods and creating extensive wetlands. The loss of the beaver dams resulted in detrimental consequences for watercourses in the basin, exacerbating the power of winter floods, and causing severe erosion. Trapping parties eventually moved
12430006
Mullum Mullum Creek


Mullum Mullum Creek is a creek in the outer eastern suburbs of Melbourne, Victoria, Australia. It is the main watercourse of the Mullum Mullum Valley, a tributary of the Yarra River and Yarra Valley. For tens of thousands of years it was used as a food and tool source sustainably by the Wurundjeri people, Indigenous Australians of the Kulin nation, who spoke variations of the Woiwurrung language group. It is one of the only watercourses lying within urban metropolitan Melbourne that is surrounded by native and regenerated bushland for almost its entire
11953195
Yarriambiack Creek


a distributary of the Wimmera River and leaves the river near Drung Drung, approximately east of . The watercourse flows northwards through and empties into Lake Coorong just east of . The flow of the watercourse is intermittent and depends almost entirely on the level of the Wimmera River. After not flowing for most of the previous 15 years, it flooded in September 2010 and January 2011. Water was released from the Wimmera River in 2012 and flowed through the creek and ended in Warracknabeal. There are a number of weirs built along the creek
600213
List of watercourses in the San Francisco Bay Area


These watercourses (rivers, creeks, sloughs, etc.) in the San Francisco Bay Area are grouped according to the bodies of water they flow into. Tributaries are listed under the watercourses they feed, sorted by the elevation of the confluence so that tributaries entering nearest the sea appear first. Numbers in parentheses are Geographic Names Information System feature ids. Watercourses which feed into the Pacific Ocean in Sonoma County north of Bodega Head, listed from north to south: Watercourses which feed into the Pacific Ocean in Sonoma County between the
12372266
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
14284171
Toronto waterway system


The Toronto waterway system comprises a series of natural and man-made watercourses in the Canadian city of Toronto. The city is dominated by a large river system spanning most of the city including the Don River, Etobicoke Creek, Highland Creek, the Humber River, Mimico Creek and the Rouge River. The city has many rivers that stretch all over the city and all end up draining into Lake Ontario. Of the various watercourses that drained Toronto, the Don River, the Humber River, and the Rouge River have headwaters in
14180437
Red River (Illinois)


The Red River is a tributary of Panther Creek in Woodford County, Illinois. Its headwaters are located southeast of Eureka, and after draining several townships it flows into Panther Creek in Palestine Township. Soon afterwards, Panther Creek itself flows into the Mackinaw River near Congerville. Via the Mackinaw River, the Red River of Illinois is part of the Illinois River and Mississippi River watershed. The Red River's drainage pattern is an unusual example of a watercourse officially designated as a river flowing into and feeding a larger watercourse that is officially
18195477
Sonoma Water


is thus different from County departments, which are created by the Board of Supervisors for administrative purposes, but are not separate legal entities. Sonoma Water was created as a special district in 1949 by the California Legislature to provide flood protection and water supply services. Providing flood protection is an important role in this community. The Water Agency has partnered with federal agencies to help build and manage a variety of flood protection projects, including Warm Springs Dam, Spring Lake, Coyote Valley Dam, Matanzas Creek Reservoir, Piner Creek Reservoir,
615624
Garonne


most distant point (along watercourses from the river mouth) in the drainage basin from which water runs. The Ratera-Saboredo cirque is the "most distant point (along watercourses from the river mouth) in the drainage basin from which water runs", and the source of the Garonne, according to the United States Geological Survey, the National Geographic Society, and the Smithsonian Institution convention upon determining a stream's source. The Garonne follows the Aran Valley northwards into France, flowing via Toulouse and Agen towards Bordeaux, where
1652483
Scotts Valley, California


discovered gold at Scott’s Bar. Approximately ten thousand years ago there was a lake in the lowest elevation of Scotts Valley, and Paleo Indians lived near its shores. The lake receded to form a peat bog. Later, around 2000 BC, Ohlone people occupied areas along the remaining creeks, spring and seep areas, along with permanent and seasonal drainages, and on flat ridges and terraces. Therefore, areas along watercourses are considered likely locations for prehistoric cultural resources. Several watercourses, including portions of Carbonera Creek, Bean Creek
17474387
List of watercourses in the Australian Capital Territory


This is a list of watercourses in the Australian Capital Territory. It includes all rivers, streams, brooks, creeks, gullies, anabranches, backwaters, and any other watercourses with a gazetted name. This list is complete with respect to the 1996 Gazetteer of Australia. Dubious names have been checked against the online 2004 data, and in all cases confirmed correct. However, if any watercourses have been gazetted or deleted since 1996, this list does not reflect these changes. Strictly speaking, Australian place names are gazetted in capital
16583214
List of watercourses in Western Australia


This is a list of watercourses in Western Australia. It includes all rivers, streams, brooks, creeks, gullies, anabranches, backwaters, and any other watercourses with a gazetted name. This list is complete with respect to the 1996 Gazetteer of Australia. Dubious names have been checked against the online 2004 data, and in all cases confirmed correct. However, if any watercourses have been gazetted or deleted since 1996, this list does not reflect these changes. Strictly speaking, Australian place names are gazetted in capital letters only
3278445
List of watercourses in Western Australia, A


This is part of a list of watercourses in Western Australia. It includes all rivers, streams, brooks, creeks, gullies, anabranches, backwaters, and any other watercourses with a gazetted name, in Western Australia. This list is complete with respect to the 1996 Gazetteer of Australia. Dubious names have been checked against the online 2004 data, and in all cases confirmed correct. However, if any watercourses have been gazetted or deleted since 1996, this list does not reflect these changes. Strictly speaking, Australian place names
3971223
List of watercourses in Western Australia, B


This is part of a list of watercourses in Western Australia. It includes all rivers, streams, brooks, creeks, gullies, anabranches, backwaters, and any other watercourses with a gazetted name, in Western Australia. This list is complete with respect to the 1996 Gazetteer of Australia. Dubious names have been checked against the online 2004 data, and in all cases confirmed correct. However, if any watercourses have been gazetted or deleted since 1996, this list does not reflect these changes. Strictly speaking, Australian place names
3971224
List of watercourses in Western Australia, C


This is part of a list of watercourses in Western Australia. It includes all rivers, streams, brooks, creeks, gullies, anabranches, backwaters, and any other watercourses with a gazetted name, in Western Australia. This list is complete with respect to the 1996 Gazetteer of Australia. Dubious names have been checked against the online 2004 data, and in all cases confirmed correct. However, if any watercourses have been gazetted or deleted since 1996, this list does not reflect these changes. Strictly speaking, Australian place names
3971225
List of watercourses in Western Australia, D


This is part of a list of watercourses in Western Australia. It includes all rivers, streams, brooks, creeks, gullies, anabranches, backwaters, and any other watercourses with a gazetted name, in Western Australia. This list is complete with respect to the 1996 Gazetteer of Australia. Dubious names have been checked against the online 2004 data, and in all cases confirmed correct. However, if any watercourses have been gazetted or deleted since 1996, this list does not reflect these changes. Strictly speaking, Australian place names
3971227
List of watercourses in Western Australia, M


This is part of a list of watercourses in Western Australia. It includes all rivers, streams, brooks, creeks, gullies, anabranches, backwaters, and any other watercourses with a gazetted name, in Western Australia. This list is complete with respect to the 1996 Gazetteer of Australia. Dubious names have been checked against the online 2004 data, and in all cases confirmed correct. However, if any watercourses have been gazetted or deleted since 1996, this list does not reflect these changes. Strictly speaking, Australian place names
3971251
List of watercourses in Western Australia, E–H


This is part of a list of watercourses in Western Australia. It includes all rivers, streams, brooks, creeks, gullies, anabranches, backwaters, and any other watercourses with a gazetted name, in Western Australia. This list is complete with respect to the 1996 Gazetteer of Australia. Dubious names have been checked against the online 2004 data, and in all cases confirmed correct. However, if any watercourses have been gazetted or deleted since 1996, this list does not reflect these changes. Strictly speaking, Australian place names
3971228
List of watercourses in Western Australia, I–L


This is part of a list of watercourses in Western Australia. It includes all rivers, streams, brooks, creeks, gullies, anabranches, backwaters, and any other watercourses with a gazetted name, in Western Australia. This list is complete with respect to the 1996 Gazetteer of Australia. Dubious names have been checked against the online 2004 data, and in all cases confirmed correct. However, if any watercourses have been gazetted or deleted since 1996, this list does not reflect these changes. Strictly speaking, Australian place names
3971235
List of watercourses in Western Australia, N–Q


This is part of a list of watercourses in Western Australia. It includes all rivers, streams, brooks, creeks, gullies, anabranches, backwaters, and any other watercourses with a gazetted name, in Western Australia. This list is complete with respect to the 1996 Gazetteer of Australia. Dubious names have been checked against the online 2004 data, and in all cases confirmed correct. However, if any watercourses have been gazetted or deleted since 1996, this list does not reflect these changes. Strictly speaking, Australian place names
3971252
List of watercourses in Western Australia, R–S


This is part of a list of watercourses in Western Australia. It includes all rivers, streams, brooks, creeks, gullies, anabranches, backwaters, and any other watercourses with a gazetted name, in Western Australia. This list is complete with respect to the 1996 Gazetteer of Australia. Dubious names have been checked against the online 2004 data, and in all cases confirmed correct. However, if any watercourses have been gazetted or deleted since 1996, this list does not reflect these changes. Strictly speaking, Australian place names
3971271
List of watercourses in Western Australia, T–V


This is part of a list of watercourses in Western Australia. It includes all rivers, streams, brooks, creeks, gullies, anabranches, backwaters, and any other watercourses with a gazetted name, in Western Australia. This list is complete with respect to the 1996 Gazetteer of Australia. Dubious names have been checked against the online 2004 data, and in all cases confirmed correct. However, if any watercourses have been gazetted or deleted since 1996, this list does not reflect these changes. Strictly speaking, Australian place names
3971274
List of watercourses in Western Australia, W–Z


This is part of a list of watercourses in Western Australia. It includes all rivers, streams, brooks, creeks, gullies, anabranches, backwaters, and any other watercourses with a gazetted name, in Western Australia. This list is complete with respect to the 1996 Gazetteer of Australia. Dubious names have been checked against the online 2004 data, and in all cases confirmed correct. However, if any watercourses have been gazetted or deleted since 1996, this list does not reflect these changes. Strictly speaking, Australian place names
3971313
List of watercourses in Western Australia, 0–9


This is part of a list of watercourses in Western Australia. It includes all rivers, streams, brooks, creeks, gullies, anabranches, backwaters, and any other watercourses with a gazetted name, in Western Australia. This list is complete with respect to the 1996 Gazetteer of Australia. Dubious names have been checked against the online 2004 data, and in all cases confirmed correct. However, if any watercourses have been gazetted or deleted since 1996, this list does not reflect these changes. Strictly speaking, Australian place names
5122628
Reedy Creek Conservation Park


brown stringybark woodland at its western boundary. The conservation park is the only part of the Reedy Creek watercourse which "ensures regeneration of the river red gums" because the rest of the watercourse is used for grazing. As of 1990, visitation consisted of use “mainly by local residents”. It was also considered to have “potential” for use as an educational resource by the Kangaroo Inn Area School which is located about west of the conservation park's southern boundary in the locality of Kangaroo Inn. The conservation park is
3369519
West Coast Piners


West Coast Piners were groups of men who worked on the West Coast of Tasmania, Australia, logging Huon pine. In most cases they used Strahan as their base, as it was the port from which the timber was shipped. The main eras of the Piners were the Sarah Island convict era (1821–33, 1846–47) and the period from the 1890s to the 1940s. Most of their activities were focused on the rivers (and their tributaries) that flow into Macquarie Harbour – the King River and the Gordon River The smaller
106690
List of rivers of California


of the Golden Gate; tributaries are listed from those entering nearest the bays to farthest). The Central Valley watershed feeding into Suisun Bay via the Sacramento–San Joaquin Delta is excluded; see the following section for the Sacramento and San Joaquin river systems. "For additional detail on Bay Area creeks, see List of watercourses in the San Francisco Bay Area." "For additional detail on Bay Area creeks, see List of watercourses in the San Francisco Bay Area." The Sacramento and San Joaquin River systems drain the
12430141
Piner High School


Piner High School (PHS) is a Public high school in Santa Rosa, California, United States. It is part of the Santa Rosa High School District, which is itself part of Santa Rosa City Schools. Piner High School was built in 1966 in Santa Rosa, California. Initially it was surrounded by orchards, local farm land and pastures. By 1975 the City of Santa Rosa expanded to the back fence of the compound. In the late 1980s further expansion included more housing on two sides and Youth Community Park (
6898247
Piner High School


including an award winning skate park) across the street. Piner High School was opened with 10th, 11th, and 12th grades in the fall of 1966. The next year it became a four year high school, with the class of 1968 being the first graduating class of the school history. Prior to the first graduating class, William McCrossen, an adult, finished his high school education and was in fact the very first graduate of Piner High School. The class of 1975 was the last of the four year classes until
6898248
Cox's Cottage


flats on its eastern boundary. The block generally slopes from Mulgoa Road to the creek with a small rise of saddle near the road. The site features two small dams lcoated on the natural watercourse along the northern boundary which are fed by rain and not by a watercourse. Two areas of former vineyard terraces are still evident. Vegetation on the cleared lower flats and the flat area east of Mulgoa Road is mainly pasture species with agricultural weeds including St John's Wort and blackberry in places. Along Mulgoa Creek are remnant native trees
10283446
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
Etadunna, South Australia


passes through the locality from south to north while the watercourse of Cooper Creek passes from east to west across its northern end. Features associated with the Cooper Creek watercourse include the northern end of Lake Gregory which is located in the locality’s south-eastern corner. Places of cultural and natural heritage significance located within the locality include the Coongie Lakes wetland system, the Killalpaninna Mission site, the Lake Palankarinna Fossil Reserve and the ‘shipwreck’ of the barge, MV Tom Brennan. The principal land uses within the locality are primary
18300680
Shamokin Creek


Run, Bennys Run, Locust Creek, and others. Little Shamokin Creek joins Shamokin Creek upstream of its mouth and drains an area of . Carbon Run joins Shamokin Creek upstream of its mouth and drains an area of . Coal Run joins Shamokin Creek upstream of its mouth and drains an area of . Bennys Run joins Shamokin Creek upstream of its mouth and drains an area of . Locust Creek joins Shamokin Creek upstream of its mouth and drains an area of . The entire length of Shamokin Creek is designated as impaired due to high
19053532
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.
2916609
Fountaingrove Lake


Fountaingrove Lake is a reservoir in the city of Santa Rosa, California, United States. Formed by the Fountaingrove Dam, the lake is fed from the east by Piner Creek, which is also the lake's sole outlet. Fountaingrove Dam is an earthen dam built in 1953. It is high, long, and wide. In 1985, a private country club known as the Fountaingrove Golf and Athletic Club built a championship 18-hole golf course centered on Fountaingrove Lake. The golf course was designed by Ted Robinson Sr. The dam
8658489
Conewago Creek (west)


Creek. Instead, the rapids are the Conewago Falls beyond the creek's mouth in the Susquehanna River, which also give their name to the other Conewago Creek, whose mouth is on the east bank of the Susquehanna River in Dauphin and Lancaster counties, only north of the mouth of this Conewago Creek. Conewago Creek flows east , then northeast to its mouth. The source is in Franklin Township in Adams County, and the mouth is at the Susquehanna River at York Haven in York County. The Conewago Creek watershed has a
8513324
Chillisquaque Creek


Chillisquaque Creek, and Middle Branch Chillisquaque Creek. Beaver Run joins Chillisquaque Creek upstream of its mouth and its watershed has an area of . Mud Creek joins Chillisquaque Creek upstream of its mouth and its watershed has an area of . West Branch Chillisquaque Creek joins Chillisquaque Creek upstream of its mouth. East Branch Chillisquaque Creek joins Chillisquaque Creek upstream of its mouth, as does Middle Branch Chillisquaque Creek. Their watersheds have areas of and , respectively. Reaches of Chillisquaque Creek are designated as an impaired waterbody. Causes of impairment include sedimentation/
12695750
Nine Partners Creek


Creek upstream of its mouth. Nine Partners Creek has two named tributaries: Butler Creek and Leslie Creek. Butler Creek joins Nine Partners Creek upstream of its mouth, within of Harding Corners, and drains an area of . Leslie Creek joins Nine Partners Creek upstream of its mouth, within of Lenox, and drains an area of . The elevation near the mouth of Nine Partners Creek is above sea level. The elevation near the creek's source is above sea level. The surficial geology inside the valley of Nine Partners Creek in
2896281
Bonanza Creek


Bonanza Creek is a watercourse in Yukon Territory, Canada. It runs for about from King Solomon's Dome to the Klondike River. In the last years of the 19th century and the early 20th century, Bonanza Creek was the centre of the Klondike Gold Rush, which attracted tens of thousands of prospectors to the creek and the area surrounding it. Prior to 1896 the creek was known as Rabbit Creek. Its name was changed by miners in honour of the millions of dollars in gold found in and around the creek. During
20584747
East Branch Tunkhannock Creek


Creek joins East Branch Tunkhannock Creek upstream of its mouth, near Elkdale, and drains an area of . Tinker Creek joins East Branch Tunkhannock Creek upstream of its mouth, within of Elkdale, and drains an area of . Dundaff Creek joins East Branch Tunkhannock Creek upstream of its mouth, within of Clifford, and drains an area of . Idlewild Creek joins East Branch Tunkhannock Creek upstream of its mouth, within of Royal, and drains an area of . East Branch Tunkhannock Creek is not designated as an impaired waterbody. The water
2591517
Obrh


Obrh Creek () is a losing stream that originates and terminates in the Lož Karst Field in the Municipality of Loška Dolina. It is a watercourse in the Ljubljanica watershed. It is created by the confluence of Little Obrh Creek () and Big Obrh Creek (); the latter is fed by two tributaries: Brežiček Creek and Viševek Brežiček Creek (). The confluence, at which point it is simply named "Obrh", lies west of the village of Pudob. In the northwest, limestone part of the karst
11274489
Counter's Creek


watercourse, connecting to the Thames with boat moorings and is shown on modern maps as Chelsea Creek; this part of Fulham is sometimes known by the toponym "Sands End". The upper reaches have been variously known as Billingswell Ditch, Pools Creek and Counters Creek. In the Middle Ages, the creek was known as Billingwell Dyche, derived from 'Billing's spring or stream'. It formed the boundary between the parishes of Kensington and Fulham. By the eighteenth century the creek had become known as Counter's Creek,
14486433
Big Creek (Lake Erie)


Big Creek is a watercourse in Norfolk County, Ontario. It is approximately long. It empties into Lake Erie, at Port Rowan, at Long Point. Its watershed covers , alternately . The largest municipality it flows through is Delhi, Ontario. North Creek joins it there. Venison Creek joins downstream of Walsingham. The creek is the largest watershed in the Long Point Region. Small dams riddle the watershed. Three of the larger reservoirs are the Teeterville Reservoir on Big Creek, the Lehman Reservoir on North Creek, and the
15141747
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
Ashbridge's Creek


Ashbridge's Creek was a watercourse that flowed in Ashbridge's Bay, between the Don River and Highland Creek. Its headwaters were north of Greenwood and Danforth avenues, making it about long. The creek was buried, and converted to a sewer, in 1909, together with nearby Smalls Creek, and Tomlin's Creek, shortly after their communities they ran through were annexed by the growing city of Toronto. Portions of a fence the Ashbridge family erected along the creek, to keep their cattle from polluting it, survive to the
7103010
Payne's Creek


Payne's Creek is a natural watercourse in Tehama County, California. The creek was apparently originally called Paines Creek according to an 1879 land survey map of the area. The town of Paynes Creek was named after the creek. The creek most likely was named after James S. Payne, the proprietor of a local sawmill. The Payne's Creek watershed contains forested reaches, and also provides habitat for numerous understory flora and fauna. An example wildflower found in the watershed is the poppy "Calochortus luteus", which is at its
11820188
Eastern Creek (New South Wales)


Eastern Creek, a watercourse that is part of the Hawkesbury-Nepean catchment, is located in Greater Western Sydney, New South Wales, Australia. Eastern Creek rises in the western suburbs of Sydney, below Sugarloaf Ridge about west by north of . The creek flows generally north, joined by the Reedy, Angus, Bungarribee, Breakfast, Burdekin, Quakers, and Bells creeks, before reaching its confluence with South Creek, in the suburb of . The creek descends over its course. Eastern Creek is transversed by the M4 Western
19059770
Darby Creek (Pennsylvania)


and numerous others. Muckinipattis Creek joins Darby Creek upstream of its mouth and its watershed has an area of . Cobbs Creek joins Darby Creek upstream of its mouth and its watershed has an area of . Ithan Creek joins Darby Creek upstream of its mouth and its watershed has an area of . Little Darby Creek joins Darby Creek upstream of its mouth and its watershed has an area of . For most of its length, Darby Creek has a low level of water quality. However, in some reaches of the watershed, especially the
775335
Birch Creek (Yukon River tributary)


) of Fort Yukon. The coordinates of the mouth of the Upper Mouth are . Lower Mouth Birch Creek flows southwest from Birch Creek to enter Lower Birch Creek Slough southwest of Fort Yukon. An anabranch of the Yukon River, the slough flows southwest roughly parallel to the main stem for . The coordinates for the mouth of Lower Mouth Birch Creek are . The Bureau of Land Management (BLM) oversees of Birch Creek declared "wild" in 1980 as part of the National Wild and Scenic Rivers System. People floating the stream
11300976
Kettle Creek (Pennsylvania)


per day. At the mouth of Twomile Run, the daily manganese load is and at the USGS stream gauge on Kettle Creek, the load is per day. At the USGS gauge on Kettle Creek, the daily load of aluminum is and at the mouth of Twomile Run it is per day. At the mouth of Butler Hollow, the aluminum load is per day. At the mouth of Kettle Creek itself, it is per day. The daily load of acidity at the creek's mouth is per day and at the
10473369
Žlebe


only to the area at the highest part of the valley. The settlement spreads across Tertiary hills and low slopes of dolomite hills separated by ravines with creeks. Zakonjščica Creek is the main watercourse, with its source below Jetrbenk Hill (), and it empties into Mavelščica Creek at Seničica. Tributaries of Zakonjščica Creek include Potočnica Creek (with its source at the Potočnik farm) and Učak Creek (with its source at the Učak farm). Zlebe was attested in written sources in 1427 as "Slepach". The name is
19348460
Sepik


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


The Mouth of Baffle Creek Conservation Parks are a series of two protected conservation parks located adjacent to the mouth of the Baffle Creek, on the central coastal region of Queensland, Australia. The parks are within the Great Barrier Reef Marine Park coastal region. Baffle Creek is one of Queensland's few remaining undisturbed coastal rivers, and the creek’s estuary mouth is protected by Mouth of Baffle Creek Regional Park. This small coastal remnant features sandy beaches backed by low, open, eucalypt and she-oak woodlands with a camping area
22083687
Breakfast Creek (Blacktown, New South Wales)


Breakfast Creek, an urban watercourse that is part of the Hawkesbury-Nepean catchment, is located in Greater Western Sydney, New South Wales, Australia. Breakfast Creek rises in the western suburbs of Sydney in , near Cavanaugh Reserve, and flows generally north-west by west, joined by the Turner, Wallar and Ashlar creeks, before reaching its confluence with Eastern Creek, in the suburb of . The course of the creek is approximately . In 2005, the Breakfast Creek catchment area was rated the third highest polluting catchment out
19137780
Reedy Creek (Blacktown, Sydney)


Reedy Creek, an urban watercourse that is part of the Hawkesbury-Nepean catchment, is located in Greater Western Sydney, New South Wales, Australia. Reedy Creek rises in the western suburbs of Sydney about north-west of the Melville trigonometry station in the Memorial Park located in the suburb of . The creek flows generally north-east by north before reaching its confluence with Eastern Creek, in the suburb of , west of Sydney Motorsport Park. The course of the creek is approximately . In 2005, the Reedy Creek catchment
19138590
Devlins Creek


Devlins Creek, an urban watercourse that is part of the Parramatta River catchment, is located in Northern Suburbs region of Sydney, Australia. Devlins Creek rises about south south-west of the suburb of ; with its headwaters forming the watershed boundary between the Hornsby Plateau and the Cumberland Plain. The creek flows generally east before reaching its confluence with Terrys Creek to form the Lane Cove River, north-east of the suburb of , in Lane Cove National Park. The course of the creek is approximately . Devlins Creek is transversed
19296436
Little Cataraqui Creek


The Little Cataraqui Creek is a watercourse, much of which is a semi-urban wetland, that empties into Lake Ontario within the municipality of Kingston, Ontario, Canada. Further inland, just north of Highway 401, the creek has been dammed to form a reservoir that is part of the Little Cataraqui Creek Conservation Area. The adjective "little" distinguishes the creek from the (Greater) Cataraqui River 4.5 kilometers to the east, which forms the beginning of the Rideau Canal. Depending on the season, the creek is
18499309