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" ... and exposed to the action of the external air, immediately cracks, becomes porous, and alters its form. As we proceeded downward this became more and more evident, and the same lava which at its original source flowed in perfect solution, undivided,... "
The Life and Remains of Edward Daniel Clarke: Professor of Mineralogy in the ... - Pągina 78
per William Otter - 1827 - 528 pągines
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The Edinburgh Review: Or Critical Journal, Volum 44

1826
...compose it, since any lava whatever, separated from its channel, at its very source, and exposed to the action of the external air, immediately cracks,...such a manner, that upon 'its arrival at the bottom of the mountain, the whole current resembled nothing so much as a rolling heap of unconnected cinders...
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The Life and Remains of the Rev. Edward Daniel Clarke, LL.D., Professor of ...

William Otter - 1824 - 670 pągines
...compose it, since any lava whatever, separated from its channel, at its very source, and exposed to the action of the external air, immediately cracks,...a little farther down, had its surface loaded with scoriae in such a manner, that upon its arrival at the bottom of the mountain, the whole current resembled...
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The Congregational magazine [formerly The London Christian instructor]., Volum 1

1825
...liquid state, and all equally in fusion. The appearance of the scoriae is to be attributed only to the action of the external air, immediately cracks,...and alters its form. As we proceeded downward, this brramc more anJ inore evident ; and the same lara which , at its original source, flowed in pcrfeci...
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Principles of Geology: Being an Inquiry how for the Former Changes ..., Volum 2

Sir Charles Lyell - 1835
...the materials which compose it ; since any lava whatever, separated from its channel, and exposed to the action of the external air, immediately cracks,...flowed in perfect solution, undivided, and free from encumbrances of any kind, a little farther down had its surface loaded with scoriae in such a manner,...
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Principles of Geology: Being an Inquiry how Far the Former Changes ..., Volum 2

Sir Charles Lyell - 1835 - 1782 pągines
...the materials which compose it, since any lava whatever, separated from its channel, and exposed to the action of the external air, immediately cracks,...became more and more evident; and the same lava which at-its original source flowed in perfect solution, undivided, and free from encumbrances of any kind,...
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Pompeii, Volum 1

William Clarke (architect.) - 1836
...the materials which compose it, since any lava whatever, separated from its channel and exposed to the action of the external air, immediately cracks,...flowed in perfect solution, undivided, and free from encumbrances of any kind, a little farther down had its surface loaded with scoriae in such a manner,...
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Pompeii [by W. Clarke].

William Clarke (architect.) - 1836
...the materials which compose it, since any lava whatever, separated from its channel and exposed to the action of the external air, immediately cracks,...flowed in perfect solution, undivided, and free from encumbrances of any kind, a little farther down had its surface loaded with scoriae in such a manner,...
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Principles of Geology: Being an Inquiry how Far the Former Changes ..., Volum 1

Sir Charles Lyell - 1837 - 546 pągines
...the materials which compose it, since any lava whatever, separated from its channel, and exposed to the action of the external air, immediately cracks,...more and more evident;. and the same lava which at iis original source flowed in perfect solution, undivided, and free from encumbrances of any kind,...
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The Saturday Magazine ...

1838
...compose it, since any lava whatever, separated from its channel, at its very source, and exposed to the action of the external air, immediately cracks,...becomes porous, and alters its form. As we proceeded downwards this became more and more evident, and the same lava which at its original source flowed...
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The Saturday Magazine, Volum 12

1838
...compose it, since any lava whatever, separated from its channel, at its very source, and exposed to the action of the external air, immediately cracks,...becomes porous, and alters its form. As we proceeded downwards this became more and more evident, and the same lava which at its original source flowed...
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