Over the Coniston Limestone beds, the Stockdale Shale's are also reasonably soft and simply eroded so that a major topographic break takes place at the junction of the Borrowdale Volcanic Series and the Silurian rocks. Valleys like Kentmere and Long Sled dale , which run through both types of rock, show contrasting scenery in their distinct sections.luxury themed boutique hotels in the lake district Whereas their reduced elements have a soft landscape with comparatively smooth green slopes and only occasional bare rock outcrops, the upper portions are a wilderness of crags, rocky buttresses and huge screes.
The geological boundary is equally distinct on the west side of Coniston Water, close to Coniston itself . Towering above the town are the slopes culminating in the Previous Man, all formed of volcanic beds. Closer at hand, by the side of Yew dale Beck, prolonged ribs oflava run down the hill�side and rocky buttresses like Long Crag depart no doubt of the presence of the Borrowdale Volcanic Series. The vale of Yew dale Beck and the softer outlines of the country to the east come as an abrupt change as soon as the Silurian strata is reached. The very same discontinuity in landscape types is apparent to the southwest of Coniston along the approximate line of the prehistoric Walna Scar Street by the side of Mealy Beck.
To the south and east of this boundary, the Silurian nation stretches away in a series of plateau at different heights. A prominent surface occurs at about 800 ft and shows up effectively to the east of Coniston Water. Elsewhere, at a reduced degree, a a lot more broken and hummocky topography has created. In which challenging grit bands occur they often give rise to a series of rocky knolls, several of which have been smoothed by the passage of ice. In in between are small walled fields interspersed with rough pasture in the more unwell drained hollows. This is the kind of landscape which is effectively noticed on either side of the major street between Staveley and Windermere and also in the location all around Below barrow, in which even the contours of the Ordnance Survey map carry out the broken character of the countryside.
In the Beneath barrow location it is the Kirkby Moor Flags, the uppermost beds of the Silurian succession, which are largely accountable. These exact same beds also outcrop to the east of Kendal exactly where they kind Hay Fell, crowned by the crags of Benson Knott . Yet another bed of wide�spread occurrence is the Bannisdale Slates which forms considerably of the region all around Windermere. This formation is above 5 thousand feet thick and is characterized by alternating bands of sandy mudstone and tough grit, providing it a stepped appear�ance which is readily recognizable in the area.
Very good views are lacking in the location largely simply because numerous elements are now covered with conifer plantations. On the steep edges of the hills deciduous woodland is far more widespread as along the eastern shores of Coniston Water. This is one particular of the unspoilt parts of the Lake District, and in spring, when the shafts of sunlight penetrate the trees and when gaps enable occasional glimpses of Coniston Previous Guy across the lake, the drive through the woods is unsurpassed.
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