To the Editor of the Geological Magazine

are also some beds which may turn out to be altered limestones; a,nd then, this group is really an old mountain-chain, having an anticlinal line, which (if the beds had not been broken through and broken up at the same time) would have given a ridge of many thousand feet high.These features, I think...

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Vydáno v:	Geological Magazine
Hlavní autor:	John Ward
Médium:	Článek
Jazyk:	angličtina
Vydáno:	Cambridge University Press 1865
Témata:	Geological Studies and Exploration Geological formations and processes Paleontology and Stratigraphy of Fossils Cambrian rocks anticline mountain chains stratigraphy
On-line přístup:	https://doi.org/10.1017/s001675680016193x
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