Cheviot Hills

Definition and stakes

Jean F. Terry,  Northumberland Yesterday and To-day

“ Yet the two are linked by the same stream, which begins life as a brawling Cheviot burn, having for its fellows the head waters of the Rede, the Coquet, and the Till, with the scores of little dancing rills that feed them.
Nowhere in this land of swelling hills and grassy fields can one get out of either sight or sound of running water. Every little dip in the hills has its watercourse, every vale its broader stream, and the pleasant sound of their murmurings and sweet babbling fills in the background of every remembrance of days spent upon the green slopes of the Cheviots.
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Source: Gutenberg

Portrait of James Geikie James Geikie,  Fragments of Earth Lore: Sketches & Addresses Geological and Geographical

“ The solid rocks which enter into the composition of the Cheviots consist mainly of (1) hard grey and blue rocks, called greywacké by geologists, with which are associated blue and grey shale; (2) various old igneous rocks; and (3) sandstones, red and white, interbedded with which occur occasional dark shales. Now, before we can make any endeavour towards reconstructing in outline the physical geography of the Cheviot Hills during past ages, it is necessary that we should discover the order in which the rock-masses just referred to have been amassed. ”
Source: Gutenberg

Portrait of Ann Ward Radcliffe Ann Ward Radcliffe,  A Journey Made in the Summer of 1794…

“ All the intervening country, speckled with towns and villages, is spread beneath the eye, and, nearly eighty miles to the eastward, part of the Cheviot-hills are traced, a dark line, binding the distance and marking the separation between earth and sky. On the plains towards Carlisle, the nearer ridges of Cross-fell are seen to commence, and thence stretch their barren steeps thirty miles towards the east, where they disappear among the Stainmore-hills and the huge moorlands of Yorkshire, that close up the long landscape of the vale of Eden. ”
Source: Gutenberg

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