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- W2078609894 abstract "Part I.—§ 1. Introduction. A recent visit to the Southern States of North America induces me to lay before the Society some observations on the physical aspect of a peculiarly interesting region traversed by the Tennessee River in the State of the same name and the bordering districts. The geological structure of this district has been ably described by Professor James M. Safford, the State Geologist. The region is now in process of being re-surveyed topographically and geologically under the direction of Major Powell, U.S. Geological Survey, to whom I am much indebted for kind assistance in procuring maps and information. In the present communication I do not propose to enter at any length into the geological structure of the district here described, but only to single out the most striking features connected with its physical structure, and to endeavour to show how they can be accounted for upon those principles of interpretation which, after many years of discussion and research, are generally adopted amongst geologists. Amongst others we shall have to explain the formation of table-lands, and of the erosion of the gorge by which a great river, the Tennessee, traverses a mountain-plateau in pursuing its way towards the ocean, instead of taking a much more direct course. § 2. Physical Features. 1. The Valley of East Tennessee .—The physical features of East Tennessee are, when viewed on a large scale, extremely simple, and are a faithful index to the geological structure. Along its eastern margin, where Tennessee joins North" @default.
- W2078609894 created "2016-06-24" @default.
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- W2078609894 date "1891-02-01" @default.
- W2078609894 modified "2023-09-27" @default.
- W2078609894 title "On the Physical Geology of Tennessee and Adjoining Districts in the United States of America" @default.
- W2078609894 doi "https://doi.org/10.1144/gsl.jgs.1891.047.01-04.09" @default.
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