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Hallin Fell
Hallin Fell is a hill in the English Lake District surrounded on three sides by Ullswater.
==Topography==
The fell is a continuation of the ridge leading down from Steel Knotts, but the depression at The Hause is so profound that Hallin Fell appears totally independent in almost any view. This is born out by its status as a Marilyn, despite being diminutive amongst Lakeland fells.
Hallin Fell stands like a plug in the outlet of the Martindale valley system. The outflows of Rampsgill, Bannerdale and Boredale are deflected west around the fell, eventually finding the shore of Ullswater at Sandwick. Fusedale and the little valley above Howtown drain around the east of the fell to meet the Lake at Howtown Wyke. The southern boundaries of the fell are therefore easily defined by these watercourses and the Howtown to Sandwick road with its ferocious hairpin climb to The Hause.
The fell is circular in plan with smooth slopes to the south and west. Wainwright famously claimed that the southern side could be "ascended comfortably in bare feet".〔Alfred Wainwright:''A Pictorial Guide to the Lakeland Fells'', Book 2: ISBN 0-7112-2455-2〕 There is rougher ground on the other sides and Hallin Fell's northernmost extremity — Geordie's Crag — projects into the lake, separating Ullswater's middle and lower reaches.
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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