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|  | Page 65:- lowest vallies, the highest point is 3000 feet above Wast Water.
 The lower of these points, lying to the south-west, is a bulky 
mountain - the proper Scawfell; the higher rising from a narrower 
base, has been called the Pikes. For want of a designation 
sufficiently explicit, strangers have sometimes been mistakenly 
directed to the secondary point; and to cross the deep chasm of 
Mickle Door, by which they are separated, is a work of 
considerable difficulty; although the direct distance does not 
exceed three quarters of a mile. Latterly however, it seems by 
common consent, the highest point is called Scawfell-Pikes; and 
since the erection of the large pile and staff upon it in 1826, 
there is no danger of mistaking the place.
 
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| geology 
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|  | Excepting some tufts of moss, very little vegetation is to be 
seen upon these summits. They are chiefly composed of rocks, and 
large blocks of stone piled one upon another; and their 
weather-worn surfaces prove that they have long remained in their 
present state. The prevailing rock is a kind of indurated slate, 
in layers of finer and coarser materials, which gives to the 
surface a ribbed or furrowed appearance; the finer parts are 
compact and hard as flint: and here the lichen 
geographicus appears in peculiar beauty. Scawfell-Pikes may be ascended on foot from any of the adjacent 
vales, but most conveniently from Borrowdale; yet the distance 
from a place of en-
 
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|  | gazetteer links 
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|   | -- "Mickle Door" -- Mickledor | 
 
 
|   | -- "Scawfell" -- Sca Fell | 
 
 
|   | -- "Scawfell Pike" -- Scafell Pike | 
 
 
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