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River Fowey : ウィキペディア英語版
River Fowey

The River Fowey ( ; (コーンウォール語:Fowi))〔(Place-names in the Standard Written Form (SWF) ) : (List of place-names agreed by the MAGA Signage Panel ). Cornish Language Partnership.〕 is a river in Cornwall, England, United Kingdom.
It rises at Fowey Well (originally (コーンウォール語:Fenten Fowi), meaning ''spring of the river Fowey'') about north-west of Brown Willy on Bodmin Moor, not far from one of its tributaries rising at Dozmary Pool and Colliford Lake, passes Lanhydrock House, Restormel Castle and Lostwithiel, then broadens at Milltown before joining the English Channel at Fowey. The estuary is called Uzell ((コーンウォール語:Usel), meaning ''howling place''). It is only navigable by larger craft for the last . There is a ferry between Fowey and Bodinnick. The first road crossing going upstream is in Lostwithiel. The river has seven tributaries, the largest being the River Lerryn. The section of the Fowey Valley between Doublebois and Bodmin Parkway railway station is known as the Glynn Valley ((コーンウォール語:Glyn), meaning ''deep wooded valley''). The valley is the route of both the A38 trunk road and the railway line (built by the Cornwall Railway in 1859). The railway line is carried on eight stone viaducts along this stretch (see Cornwall Railway viaducts).
==Geology and hydrology==
The upper reaches of the Fowey are mainly moorland giving way to woodland and farmland, predominantly livestock. This means that 63.6% of the catchment is grassland, with a further 18.3% woodland and 10.7% arable land. Of the remaining 7.5%, 2.6% is urban or built-up areas, 2.5% is mountain, heath and bog and the remainder is inland waters.
The catchment area of the River Fowey covers a total of 41,800 acres (65.3 sq. miles) consisting of kaolinised granite on Bodmin Moor, Devonian slates and grits, and valley gravels.〔 Data collected by the National Water Archive shows that average flow at the Restormel monitoring station is 4.78 cubic m/s and is affected by the reservoirs at Colliford and Sibleyback and by abstraction of water for public supply.〔

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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