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The Geology of the Country Between Applby, Ullswater, and Haweswater

The Geology of the Country Between Applby, Ullswater, and Haweswater

34799096
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Описание
Excerpt from The Geology of the Country Between Applby, Ullswater, and Haweswater: Explanation of Quarter-Sheet 102 S. New Series, Sheet 30

The original geological survey of the area represented in the map (Sheet 102 S.W.), to which the present Memoir is an explanation, was completed as far back as the year 1876, and was the work of Messrs. W. T. Aveline, T. McK. Hughes, J. R. Dakyns, R. H. Tiddeman, J. Clifton Ward, R. Russell, W. H. Dalton, J. G. Goodchild, G. H. Lightfoot, and E. J. Hebert, the mapping being under Mr. Aveline's superintendence. The map as it now appears was issued in 1893.

Of the officers above named seven have retired from the service and one is dead. Some delay has consequently arisen in the preparation of a description of the map. The present Memoir has been arranged mainly by Mr. Dakyns and Mr. Goodchild; the contributions of the different surveyors being indicated by their appended initials.

The sheets of the county maps on the scale of six inches to a mile included in the present one-inch map are Cumberland 57, 58, 65, 66; and Westmorland 3, 4, 5, 7, 8, 9, 12, 13, 14, 15, 19, 20, 21, 22.

The area embraced by the map extends from near the head of Ullswater on the west to Dufton and Appleby on the cast As it thus embraces the north-eastern part of the Lake District, including Haweswater, Bleawater, and Brothers Water, it possesses much geological interest in its copious development of the Borrowdale Volcanic Series. It contains also the northern edge of the Shap granite boss, and in its north-eastern corner a portion of the remarkably interesting inlier of the Silurian Series at the base of Cross Fell.

Around the hills of Lower Silurian Rocks the Carboniferous system is well developed.

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