On the Structure of Lavas Which Have Consolidated on Steep Slopes; With Remarks on the Mode of Origin of Mount Etna, and on the Theory of "Craters of Elevation"

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On the Structure of Lavas Which Have Consolidated on Steep Slopes; With Remarks on the Mode of Origin of Mount Etna, and on the Theory of "Craters of Elevation"
Citation	Lyell C. Philos. Trans. R. Soc. Lond. 1858; 148: 703-904.
Copyright	(Copyright © 1858, Royal Society)
DOI	unavailable
PMID	unavailable
Abstract	[Abstract unavailable]

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