Excerpt from The Silurian System, Founded on Geological Researches in the Counties of Salop, Hereford, Radnor, Montgomery, Caermarthen, Brecon, Pembroke, Monmouth, Gloucester, Worcester, and Stafford, Vol. 2 of 2: With Descriptions of the Coal-Fields and Overlying Formations Respecting the Irish case, it may be stated that Mr. James de C. Sowerby, whose authority is much cited in the memoir of Weaver, is of Opinion that all the fossils therein enumerated, p. 21, as belonging to the transition limestone of Cork and ...
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Excerpt from The Silurian System, Founded on Geological Researches in the Counties of Salop, Hereford, Radnor, Montgomery, Caermarthen, Brecon, Pembroke, Monmouth, Gloucester, Worcester, and Stafford, Vol. 2 of 2: With Descriptions of the Coal-Fields and Overlying Formations Respecting the Irish case, it may be stated that Mr. James de C. Sowerby, whose authority is much cited in the memoir of Weaver, is of Opinion that all the fossils therein enumerated, p. 21, as belonging to the transition limestone of Cork and neighbourhood, are, with one exception, characteristic fossils of the carboniferous limestone of England and Ireland and therefore that they are of the same geological age as those which, in another part of the memoir, are described as exclusively belonging to the carboniferous strata. Judging from the printed lists, Professor Phillips also thinks that the Cork limestone fossils are carboniferous. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at ... This book is a reproduction of an important historical work. Forgotten Books uses state-of-the-art technology to digitally reconstruct the work, preserving the original format whilst repairing imperfections present in the aged copy. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in our edition. We do, however, repair the vast majority of imperfections successfully; any imperfections that remain are intentionally left to preserve the state of such historical works.
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