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the idle theory that all this heat may be produced by the chemical action of water on beds of sulphates or phosphates just below the surface. The temperature of the water should be sufficient to show that it comes from great depths. The writer was unable, from want of a thermometer, to verify the temperatures of the various springs in the Devil's Canon, but was told that they average 201 deg., and as most of them were boiling, it appeared not to be far from the truth. Since Arago discovered, in 1821, that the deepest artesian wells were the hottest, it has been observed that the hottest springs are the purest; and from their geological surroundings, many are proved to come from great depths. The Aguas Calientes de las Trincheras, near Puerto Cabello, issue from _granite_, at a temperature of 206 deg.; the Aguas de Comaugillas, near Guanaxuato, from _basalt_, at 205 deg.. To more fully establish the volcanic origin of the phenomena of California and Central America, if such a thing were necessary, it can, however, be shown that similar phenomena are found around the crater of a volcano in _actual eruption_. A graphic account of 'White Island,' in the South Pacific, from the pen of Captain Cracroft, R. N., who visited it with the Governor of New Zealand, in H. M. S. Niger, speaks of boiling springs, 'geysers,' and steam-escapes, in connection with a very remarkable active volcano. As very few are acquainted with this singular island, his description of his visit is given in full: 'Sunday, _January_ 15, 1862. 'This morning we were well inside the Bay of Plenty, and as the wind declined to a calm, I got steam up, and stood for White Island, on which there is a volcano in active operation. The white cloud of smoke that always hovers over it was in sight before eight o'clock, in shape like a huge palm tree, and at eleven o'clock, H. E., the governor, gladly accompanied me ashore, with all the officers of the ship that could be spared from duty. 'As we approached the island, its aspect was of the most singular and forbidding description. Except on its northern face, to which the sulphurous vapor does not appear to reach, it is utterly destitute of vegetation: here and there are a few patches of underwood; but in every other direction the island is bald, bleak, and furrowed into countless deep-worn ravines. The ce
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