By Julian W. Connolly
(Studies in Russian and Slavic literatures, cultures and historical past)
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Let us now turn our attention to the internal or geological structure of Cornwall. E. W. On the same ridge, but rather parallel than continuous thereto, is the great granitic group of Dartmoor in Devon, the whole of which is sometimes called the Ocrynian Range. The granitic patch of Dartmoor is by far the most extensive, being nearly twenty miles in diameter; that of Launceston is ten miles in length by six or seven in breadth at its widest part; and its most elevated hills, Rough-tor and Brown-Willy, do not much exceed 1,300 feet in height.
Agnes was taxed to the four shillings in the pound land-tax, Qth William and Mary, 1696, 1371. 5s. The present church of St. Agnes was of old only a small free chapel dedicated to her, without endowment, till the same was augmented and rebuilt, of three roofs, as it now stands, by charitable collections, and the proper charge and cost of the inhabitants thereof, in 1484; consecrated and dedicated to the honour of Almighty God, in the name of St. Agnes, as a daughter church to Peransand, by Dr. * St.
Murchison having investigated the deep-seated rocks in Wales, and in the adjacent districts, have finally traced the carboniferous series under the Severn, and so far west as the level ridge of land, extending from near Launceston to the sea coast between St. Gennys and Botreaux Castle, along which plane the escarpment manifests itself in a very conspicuous manner. While these discoveries may be considered as in progress, a Cornish gentleman, but one whose genius does honour to the nation, Mr. Robert Weare Fox, has deduced from galvanic action on metals, on their oxides, on their sulphurets, and on their saline solutions in water, the only theory that has yet accounted for the various phenomena observed in metallic lodes; and extending still further his investigations to the recently discovered connection between electric energies and terrestrial magnetism, Mr.