[563] Mém. pour servir, &c. tom. iv. p. 116.
[564] See Prof. J. D. Forbes, Phil. Trans. 1846, p. 155, on Velocity of Lava.
[565] Ferrara, Descriz. dell' Etna, p. 108.
[566] Ferrara, Descriz. dell' Etna. Palermo, 1818.
[567] This view is taken from a sketch made by Mr. James Bridges, corrected after comparison with several sketches of my own.
[568] Scrope on Volcanoes, p. 153.
[569] This drawing is part of a panoramic sketch which I made from the summit of the cone, December 1, 1828, when every part of Etna was free from clouds except the Val del Bove. The small cone, and the crater nearest the foreground, were among those formed during the eruptions of 1810 and 1811.
[570] Scrope on Volcanoes, p. 102.
[571] Ferara, Descriz. dell' Etna, p. 116.
[572] Mr. Nasmyth, the inventor of the steam-hammer, has lately illustrated, by a very striking experiment, the non-conductibility of a thin layer of dry sand and clay. Into a caldron of iron one-fourth of an inch thick, lined with sand and clay five-eighths of an inch thick, he poured eight tons of melted iron at a white heat. After the fused metal had been twenty minutes in the caldron the palm of the hand could be applied to the outside without inconvenience, and after forty minutes there was not heat enough to singe writing-paper. This fact may help us to explain how strata in contact with dikes, or beds of fused matter, have sometimes escaped without perceptible alteration by heat.