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The River Swale in Yorkshire, England, is a major tributary of the River Ure, which becomes the River Ouse, that empties into the North Sea via the Humber Estuary. The river gives its name to Swaledale, the valley through which it flows. The river and its valley are home to many types of flora and fauna typical to the Yorkshire Dales.
Below Richmond, the valley sides flatten out and the Swale flows across lowland farmland to meet the Ure just east of Boroughbridge at a point known as Swale Nab. The Ure becomes the Ouse, and eventually (on merging with the Trent) the Humber. From the north, Arkengarthdale and its river the Arkle Beck join Swaledale at Reeth.
The vale is the floodplain of the River Swale and its tributaries, including the Wiske and Cod Beck. The river enters the vale from Swaledale, in the north-west, then flows in a south-easterly direction before entering the Vale of York. The underlying geology of the landscape is sandstone and mudstone, with clays and silts in the south-west.
At these times the Swale was a gully from what had been a sea channel in very warm periods. Namely before the Strait of Dover had swept away so much swampy land, accentuated by sea levels being lower, even to beyond the end of the ice age, i.e. in the mid seventh millennium BC, the coasts of Essex and Kent stretched much further into the North Sea.
The River Swale has been known to be subject to flooding and is monitored closely by the Environment Agency. [6] Although Great Langton is located in a primary area for fishing, no local residents are in the trade. [7] The River Swale also attracts large numbers of duck into the village, commonly seen around
East Gill Force upper falls in Swaledale, North Yorkshire The lower part of East Gill Force as the Gill joins the River Swale. East Gill Force is a waterfall in Swaledale, 330 yards (300 m) east of the hamlet of Keld, in the Yorkshire Dales National Park, North Yorkshire, England. [1]
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This archetypal form of swale is a dug-out, sloped, often grassed or reeded "ditch" or "lull" in the landform. One option involves piling the soil onto a new bank on the still lower slope, in which case a bund or berm is formed, mitigating the natural (and often hardscape-increased ) risks to slopes below and to any linked watercourse from ...