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The products of chalk weathering are dissolved in rainwater and are transported in stream flow. Chalk streams transport little suspended material (unlike most rivers), but are considered "mineral-rich" due to the dissolved calcium and carbonate ions. The surface water of chalk streams is commonly described as "gin clear".
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 River Dour is a chalk stream in the county of Kent, England. It flows from the villages of Temple Ewell and River between which is a neighbourhood served by a railway station, Kearsney. It is roughly 4 miles (6.4 km) long. It originally had a wide estuary on the site of modern Dover, although today it flows into the Dover Harbour through a ...
The Nailbourne near Bishopsbourne on 22 July 2006. Even when there is no water in the stream it is still a haven for wildlife. The Little Stour starts at the springs near Well Chapel, Bekesbourne, after the watercress beds the Nailbourne joins the Little Stour (when it is running) and then joins with the Great Stour at Plucks Gutter near West Stourmouth.
A bourne is an intermittent stream, flowing from a spring. Frequent in chalk and limestone country where the rock becomes saturated with winter rain, that slowly drains away until the rock becomes dry, when the stream ceases. [1] The word is from the Anglo-Saxon language of England.
The state of the upper Beane resulted in calls for the river's restoration. [6] The management plan for the river includes the objective that there is adequate flow along the length of the river to support a ‘good status’ chalk stream ecology (as defined by the European Union's Water Framework Directive).
Jon Hoefling, USA TODAY Updated December 7, 2024 at 2:11 AM With the new, expanded 12-team playoff this year, a conference championship has never been more important.
The River Allen starts as a winterbourne at Wyke Farm in Monkton Up Wimborne, on the chalk downland of Cranborne Chase.It flows roughly southwards on the dip slope of the downland through Wimborne St Giles, and is joined by the Gussage stream at Gussage All Saints and the Crichel stream south of Moor Crichel, before passing through Witchampton and Hinton Parva, where the landscape transitions ...