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Topographically, the boundaries of the Yorkshire Dales trace the flow of streams from the lowest points between it and the neighbouring regions of the Lake District, North Pennines, Forest of Bowland, South Pennines and North York Moors. Hills are grouped as topographically as possible, according to their 'parent Marilyn'.
Yorkshire is drained by several rivers. In western and central Yorkshire, the many rivers empty their waters into the River Ouse, which reaches the North Sea via the Humber Estuary. [1] The most northerly of the rivers in the Ouse system is the River Swale, which drains Swaledale before passing through Richmond and meandering across the Vale of ...
The Yorkshire Dales are a series of valleys, or dales, in the Pennines, an upland range in England. They are mostly located in the ceremonial county of North Yorkshire , but extend into Cumbria and Lancashire ; they are entirely within the historic boundaries of Yorkshire .
Teesdale and its side dales, historically in the North Riding of Yorkshire, and sometimes considered part of the Yorkshire Dales, [2] [3] are in the North Pennines AONB. On 1 August 2016, the area of the National Park was increased by nearly a quarter, with an extra 161 square miles (417 square kilometres) of upland landscape given protected ...
Articles about mountains and hills in Yorkshire, England. Subcategories. This category has the following 4 subcategories, out of 4 total. N ...
Black Hill, in the Peak District, is the highest hill in West Yorkshire, England.Its summit rises to an elevation of 582 m (1,909 ft) above sea level. [1] It is surpassed in height by only two other major summits in the Peak District (Kinder Scout and Bleaklow).
The mountains of Whernside (736 m or 2,415 ft), Ingleborough (723 m or 2,372 ft) and Pen-y-ghent (694 m or 2,277 ft) are collectively known as the Three Peaks.The peaks, which form part of the Pennine range, encircle the head of the valley of the River Ribble in the Yorkshire Dales National Park in the North of England.
The Geology of Yorkshire in northern England shows a very close relationship between the major topographical areas and the geological period in which their rocks were formed. The rocks of the Pennine chain of hills in the west are of Carboniferous origin whilst those of the central vale are Permo-Triassic.
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