North Lancashire By J E Marr
North Lancashire By J E Marr
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The clints just mentioned are flat or fairly flat surfaces of limestone with fissures or "grikes" produced by the widening of the vertical joints by acidulated rain-water. The water is capable of dissolving the limestone, and the bare flat or gently-sloping limestone surfaces are therefore often traversed by two sets of fissures at right angles to each other, penetrating for many feet or even yards from the surface. The sides of these are often honeycombed by the solvent action of the rain assi...sted by the vegetation that may grow abundantly within. Such clints are seen on the higher parts of the two fells mentioned above.
The massive well-jointed Millstone Grit, when found on fell-tops and to some extent on fell-sides, produces steep scarps like those seen on the top of Clougha and other parts of the fells lying south-east of Lancaster, but the abundant growth of peat often covering glacial ac- cumulations of these fells has prevented the extensive development of such scarps, and the Millstone Grit tract of these high uplands is chiefly marked by somewhat c X!
What to read after North Lancashire By J E Marr?
You can find similar books in the "Read Also" column, or choose other free books by Marr, John Edward, 1857-1938 to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
The clints just mentioned are flat or fairly flat surfaces of limestone with fissures or "grikes" produced by the widening of the vertical joints by acidulated rain-water. The water is capable of dissolving the limestone, and the bare flat or gently-sloping limestone surfaces are therefore often traversed by two sets of fissures at right angles to each other, penetrating for many feet or even yards from the surface. The sides of these are often honeycombed by the solvent action of the rain assi...sted by the vegetation that may grow abundantly within. Such clints are seen on the higher parts of the two fells mentioned above.
The massive well-jointed Millstone Grit, when found on fell-tops and to some extent on fell-sides, produces steep scarps like those seen on the top of Clougha and other parts of the fells lying south-east of Lancaster, but the abundant growth of peat often covering glacial ac- cumulations of these fells has prevented the extensive development of such scarps, and the Millstone Grit tract of these high uplands is chiefly marked by somewhat c X!
What to read after North Lancashire By J E Marr?
You can find similar books in the "Read Also" column, or choose other free books by Marr, John Edward, 1857-1938 to read onlineMoreLess
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