Somerset by J. H. Wade;G. W. Wade
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page 11 of 283 (03%)
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re-appear as the islets of the Steep and Flat Holms. On their S.W. side
they descend into the plain with considerable abruptness; and when viewed from the lower parts of the county, present a hard sky-line, like some enormous earthwork. On the opposite side their aspect in general is far less impressive, and towards Bath they lose themselves in a confusion of elevations and declivities. The main ridge is an extended tableland, some 25 m. long, and in places 3 m. broad. It rises to its greatest heights at Blackdown (1067 ft.) and Masbury (958). Geologically, it consists of mountain limestone superimposed on old red sandstone, which here and there comes to the surface. Near Downhead there is an isolated outburst of igneous rock. The Mendips are honeycombed with caverns, the most notable being at Banwell, Harptree, and Burrington; and a large one has been recently discovered some 4 m. from Wells. At Cheddar their W. edge is broken by a remarkable gorge, in the sides of which caves also occur. The level of the tableland is indented with "swallet holes," the chief of which are the East Water Swallet and the Devil's Punch-Bowl. The _Quantocks_ are much less extensive, though their highest summits rise to a greater altitude. Like the Mendips, they turn their steepest flank westwards, the ascent on the E. being gradual; and on this side they are cut by a number of well-timbered and delightful combes. Few caves have been discovered in them, though there is one at Holwell near Asholt. W. of the Quantocks are the _Brendons_ and the highlands of _Exmoor_, the latter extending into Devon, though their highest point, Dunkery Beacon, is included in Somerset. Dunkery is 1707 ft. above the sea-level; and other conspicuous hills in this district are Lucott Hill (1516), Elworthy Barrow (1280), Selworthy Beacon (1014), and Grabbist Hill. The Quantocks, Brendons, and Exmoor consist of older rocks than the Mendips, belonging as they do to the Devonshire series of old red sandstones. Bordering the Brendons are found the red marls of the |
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