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Topographical areas of Yorkshire
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Topographical areas of Yorkshire : ウィキペディア英語版
Topographical areas of Yorkshire
(詳細はNorth York Moors in the north-east of the county are Jurassic in age while the Yorkshire Wolds to the south east are Cretaceous chalk uplands. The plain of Holderness and the Humberhead levels both owe their present form to the Quaternary ice ages.
Much of Yorkshire presents heavily glaciated scenery as few places escaped the great ice sheets as they advanced during the last ice age.
== Drainage ==

Western and central Yorkshire are largely drained by rivers which empty their waters into the River Ouse which reaches the North Sea via the Humber Estuary. The most northerly of the rivers in the Ouse system is the Swale, which drains Swaledale before passing through Richmond and meandering across the Vale of Mowbray. Next, draining Wensleydale, is the River Ure, which joins the Swale east of Boroughbridge. The River Nidd rises on the edge of the Yorkshire Dales National Park and flows along Nidderdale before reaching the Vale of York. The Ouse is the name given to the river after its confluence with the Ure at Ouse Gill Beck. The River Wharfe, which drains Wharfedale, joins the Ouse upstream of Cawood. The Rivers Aire and Calder are more southerly contributors to the River Ouse and the most southerly Yorkshire tributary is the River Don, which flows northwards to join the main river at Goole.
In the far north of the county the River Tees flows easteards through Teesdale and empties its waters into the North Sea downstream of Middlesbrough. The smaller River Esk flows from west to east at the northern foot of the North York Moors to reach the sea at Whitby.
The River Derwent rises on the North York Moors, flows south then westwards through the Vale of Pickering then turns south again to drain the eastern part of the Vale of York. It empties into the River Ouse at Barmby on the Marsh. To the east of the Yorkshire Wolds the River Hull flows southwards to join the Humber Estuary at Kingston upon Hull. The western Pennines are served by the River Ribble which drains westwards into the Irish Sea close to Lytham St Anne’s.〔 Philips Motoring Atlas:Britain. Philips, London 2005〕

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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