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High Tove
High Tove is a fell in the English Lake District, close to the geographical centre of the Cumbrian hills. It forms part of the watershed between the Derwentwater and Thirlmere catchments, a ridge running broadly north-south.
==Topography==
Sitting astride the spine of the Central Fells, High Tove is an outlier of High Seat. It is separated from its taller northern neighbour by the Peewits, an extremely boggy depression. The ridge moves on south across further upland marsh towards Ullscarf, passing over the three rocky (and dry) outcrops of Middle Crag, Shivery Knott and Watendlath Fell (summit unnamed on Ordnance Survey maps). Armboth Fell lies to the south east of High Tove, connected to the ridge by a broad heathery saddle.
High Tove covers around one and a half miles of the north-south ridge, which is approximately a mile in width. It is bounded on the west by Watendlath Gill and its main feeder, Blea Tarn Gill. These flow to Watendlath Tarn, a popular beauty spot. The tarn is available for private fishing, being well stocked with trout. It holds a wide selection of flora, including water lilies and is at least 50 ft deep.〔Don Blair: ''Exploring Lakeland Tarns'': Lakeland Manor Press (2003): ISBN 0-9543904-1-5〕 Fisher and Launchy Gills provide the eastern boundaries of High Tove, flowing north and south around Armboth Fell respectively. Both are feeders of Thirlmere.
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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