Search results
Results from the WOW.Com Content Network
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 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 ...
Chalgrove Brook is a chalk stream located in South Oxfordshire, England. [1]It is a left tributary of the River Thame.It rises in a number of natural springs at the foot of the Chiltern Hills near Watlington, and flows in a northwesterly direction for approximately 7 miles (11 km) through Cuxham, Chalgrove, and Stadhampton, before emptying into the Thame near Chiselhampton.
Other examples include the Alkham Valley near Dover, and the Hartley Bottom and Fawkham valleys near Dartford in north Kent. [1] There are many examples of limestone dry valleys in the Peak District and the Yorkshire Wolds. A notable example is the valley of the River Manifold which is dry, except in spate, from Wetton south for several miles.
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 ...
A wide variety of river and stream channel types exist in limnology, the study of inland waters.All these can be divided into two groups by using the water-flow gradient as either low gradient channels for streams or rivers with less than two percent (2%) flow gradient, or high gradient channels for those with greater than a 2% gradient.
An extensive Neolithic ritual complex, the main elements of which are four large cursus monuments and a henge, is situated near the eastern end of the Great Wold Valley. More than 1,400 Bronze Age round barrows, comprising one or more burials and accompanied by items of grave goods, are known to exist on the Yorkshire Wolds.