| Sir Charles Lyell - 1854 - 870 str.
...he quarried into this ice, and proved the superposition of the lava for several hundred yards, so us completely to satisfy himself that nothing but the...so expensive, that there is no probability of the operations being renewed. On the first of December, 1828, I visited this spot, which is on the * Ferara.... | |
| George Dennis - 1864 - 828 str.
...a lava - current. With a large body of workmen he quarried into this ice, which was extremely hard, and proved the super-position of the lava for several...ice could account for the position of the glacier. " Wo may suppose," says Sir Charles Lyell, " that at the commencement of the eruption, a deep mass... | |
| George Dennis, John Murray (Firm) - 1864 - 664 str.
...workmen he quarried into this ice, which was extremely hard, and proved the super-position of the laya for several hundred yards, so as completely to satisfy...ice could account for the position of the glacier. " We may suppose," says Sir Charles Lyell, " that at the commencement of the eruption, a deep mass... | |
| Charles Knight - 1866 - 582 str.
...at the foot of the highest cone was part of a large and continuous glacier covered by a lava-current Having procured a large body of workmen, he quarried...ice could account for the position of the glacier." Besides the three natural divisions of the mountain before noticed, j£tn.i is divisible into seven... | |
| 1880 - 816 str.
...the foot of the highest cono was part of a large and continuous glacier covered by a lava-current. Having procured a large body of workmen, he quarried...ice could account for the position of the glacier" (in other words, the ice had not accumulated in a cavern of moderate extent accidentally formed beneath... | |
| 1879 - 948 str.
...the foot of the highest cone was part of a large and continuous glacier covered by a lava-current. Having procured a large body of workmen, he quarried...ice could account for the position of the glacier" (in other words, the ice had not accumulated in a cavern of moderate extent accidentally formed beneath... | |
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