MENDIP HILLS
, a range in the See also:north of See also:Somersetshire, See also:England
.
Using the name in its widest application, the eastern boundary of the range may be taken to be formed by the upper valleys of the See also:rivers See also:Frome and Brue, and the depression between them
.
The range extends from these north-westward with a See also:major See also:axis of about 23 m., while the outliers of Wavering Down and Bleadon See also:- HILL
- HILL (0. Eng. hyll; cf. Low Ger. hull, Mid. Dutch hul, allied to Lat. celsus, high, collis, hill, &c.)
- HILL, A
- HILL, AARON (1685-175o)
- HILL, AMBROSE POWELL
- HILL, DANIEL HARVEY (1821-1889)
- HILL, DAVID BENNETT (1843–1910)
- HILL, GEORGE BIRKBECK NORMAN (1835-1903)
- HILL, JAMES J
- HILL, JOHN (c. 1716-1775)
- HILL, MATTHEW DAVENPORT (1792-1872)
- HILL, OCTAVIA (1838– )
- HILL, ROWLAND (1744–1833)
- HILL, SIR ROWLAND (1795-1879)
Hill continue it towards the See also:shore of the See also:Bristol Channel
.
The range is generally about 6 m. in width, and its See also:total See also:area about 130 sq. m
.
Its See also:south-western See also:face descends to the See also:low " See also:moors " or marshes drained by the See also:Axe and other streams, the small towns of Axbridge, See also:Cheddar and See also:Wells lying at the See also:foot of the hills
.
Towards the north-See also:east its limits are less clearly defined, for high ground, intersected by narrow vales, extends as far as the valley of the" See also:Avon
.
A depression, followed by the road between Radstock and Wells, strikes across the range about its centre; the See also:principal elevations See also:lie See also:west of this, and to the area thus defined the name of the Mendips is sometimes restricted
.
The See also:summit of the hills is a gently swelling See also:plateau, which reaches its extreme height in the north—io6S ft
.
The Mendips consist principally of Carboniferous See also:Limestone
.
See also:Fine cliffs and scars occur on the flanks of the plateau, as in the See also:gorge of Cheddar, and there is a wonderful See also:series of caverns, the result of See also:water See also:action
.
The See also:surface of the plateau is often broken by deep holes
(" swallets ") into which streams flow
.
Some of the caves, such as those at Cheddar, are easy of See also:access, and attract many visitors owing to the beauty of the stalactitic formations; others, of greater extent and grandeur, have only been explored, or partly explored, with See also:great difficulty
.
Some caves have yielded large quantities of See also:animal remains (hyaenas, bears and others) together with traces of prehistoric human occupation
.
Among such Wookey Hole, where the See also:river Axe issues from the foot of a cliff, may be mentioned
.
See also:Lead was worked among the Mendips at a very See also:early See also:period
.
Some of the See also:Roman workings, especially in the neighbourhood of See also:Charterhouse-on-Mendip, have yielded pigs of lead inscribed with the names of emperors of the 1st and 2nd centuries A.D., together with an abundance of smaller See also:objects
.
See E
.
See also:Baker and H
.
Balch, The Netherworld of Mendip (See also:Clifton, 1907)
.
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