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Although chalk streams are generally watercourses originating from chalk hills, including winterbournes, streams, and rivers, the term chalk stream is used even for larger rivers, which would normally be considered too large for the term stream. The Somme in northern France is a chalk stream on a larger scale.
Map of the Scioto River watershed. The Scioto River (/ s aɪ ˈ oʊ t ə / sy-OH-tə) is a river in central and southern Ohio more than 231 miles (372 km) in length. [4] It rises in Hardin County just north of Roundhead, Ohio, flows through Columbus, Ohio, where it collects its largest tributary, the Olentangy River, flows south into Appalachian Ohio, and meets the Ohio River at Portsmouth.
The Columbus and Franklin County Metro Parks system was created in 1945 after a study was commissioned by the Columbus and Franklin County planning commissioners. The study endorsed the development of a metro park system with the area's rivers and streams as idea land for the parks modeled after the Cleveland Metroparks. The parks would also ...
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Big Walnut Creek was named for black walnut trees which once grew in old-growth forests near the stream. [5] According to the Geographic Names Information System, the Big Walnut Creek has also been known as: [6] Big Belly Creek; Big Bellys Creek; Big Lick Creek; Gahanna River; Hayes Ditch; Walnut Creek; Whingwy Mahoni Sepung; Menkwi Mhoani Siipunk
The River Purwell is a chalk stream in Hertfordshire, England. The entire course of the stream is near Hitchin. Its source is springs which rise out of the chalk bedrock at St Ippolyts, forming Ippollitts Brook. [1] It is known as the Purwell by the time it reaches Ninesprings on the border of the parishes of Great Wymondley and Hitchin.
The River Chess is a chalk stream that rises near Chesham in the Chiltern Hills, and flows for 11 miles (18 km) through Buckinghamshire and Hertfordshire to its confluence with the River Colne in Rickmansworth. The Chess, along with the Colne and Gade, gives rise to the name of the district of Three Rivers.
The Gypsey Race rises in the Great Wold Valley [4] through a series of springs and flows intermittently between Duggleby and West Lutton where it runs underground in the chalk aquifer before re-surfacing in Rudston. It has been known during very wet conditions for the stream to re-appear at Wold Newton [5] some 4.3 miles (7 km) north-west of ...