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Hallin Fell (AW FEF 35) Traditional Cache

This cache has been archived.

Royal Oak: As the owner has not responded to my previous log requesting that they check this cache I am archiving it.

If you wish to email me please send your email via my profile (click on my name) and quote the cache name and number.

Regards

Royal Oak
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Hidden : 7/20/2006
Difficulty:
2.5 out of 5
Terrain:
2.5 out of 5

Size: Size:   small (small)

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Geocache Description:

Hallin Fell 388 m (1,273 ft) Hallin fell is a continuation of the ridge leading down from Steel Knotts, but the depression at The Coombs 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 Coombs.

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". 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.

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Additional Hints (Decrypt)

Npebff gur tenff sebz gur fhzzvg pnvea, njnl sebz gur ynxr, ner fbzr ebpxf. Ybbx va gurz. Ovatb!

Decryption Key

A|B|C|D|E|F|G|H|I|J|K|L|M
-------------------------
N|O|P|Q|R|S|T|U|V|W|X|Y|Z

(letter above equals below, and vice versa)