MAN, ISLE OF (anc. Mona), a possession of the crown of England, in the Irish sea, 33 m. long by 12 broad in the broadest part. The area is 220 sq.m. Oval in general form its outline is very irregular, being indented with numerous bays and creeks. Its chief physical characteristic is the close juxtaposition of mountain, glen and sea, which has produced a great variety and beauty of scenery. The greater part of its surface is hilly. The hills (culminating point Snaefell 2,034 f t.), have a trend in the direction of the longer axis, but throw out radiating spurs, which frequently reach the coast line. The outline of the hills is smooth and rounded, the rocks, the Manx Slate series, being a group of slates, flags, grits and conglomerates which have suffered much from folding, crushing and cverthrusting.
No satisfactory fossils have yet been found in these rocks, but they are regarded provisionally as of Upper Cambrian age. The series is penetrated by masses of granite at Dhoon, Foxdale, etc. Streams have frequently rent steep-walled gulleys in the hill-sides, and the westerly winds have caused them to be tree less, except in some of the lower slopes. Rising almost directly from the sea, they present a much more imposing appearance than many hills of greater altitude. On the south-west, they descend precipitously into the sea, and unite with the cliffs to produce most striking coast scenery. The whole coast from Peel round by the Calf-of-Man, to near Ramsey, is distinguished by rugged gran deur. The Calf-of-Man is a precipitous island reaching an alti tude of 36o feet. From Ramsey round by the Point of Ayre to near Peel, extend low sandy cliffs, bordered by flat sandy shores.
The low-lying northern plain extends northward from the road between Ramsey and Ballough and is composed of Carboniferous (limestones, sandstones and conglomerates) and Triassic rocks entirely covered by glacial drift. This plain is relieved only by a low range of hills, the highest attaining an elevation of 27o feet. There is a small tract (8 sq.m.) of Carboniferous rocks in the neighbourhood of Castletown, which are of great economic im portance forming the only source of lime and also the best build ing stone in the island. The drainage of the island radiates from
around Snaefell. Narrow, winding glens studded with fir, syca more, and mountain ash, with patches of gorse, heather and fern, afford a striking contrast to the bare mountain tops. Traces of an older system of drainage are noticeable, especially in the cen tral depression between Douglas and Peel. There are no lakes.
The chief bays are, on the east coast, Ramsey, with an excellent anchorage, Laxey, Douglas, Derbyhaven, Castletown and Port St. Mary; and on the west coast Port Erin and Peel.