Geological Report On Warren County And The Neighboring Oil Regions
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Geological Report of Warren County and the Neighboring Oil Regions by John F. Carll Pdf
Excerpt from Geological Report of Warren County and the Neighboring Oil Regions: With Additional Oil Well Records A. E. Lehman, topographical geologist for the South Mountains in Cumber land and York Cos. 907 Walnut street, Philadelphia. H. C. Lewis, geologist for surface deposits; Germantown, Philadelphia. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at www.forgottenbooks.com 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.
Geological Report on Warren County and the Neighboring Oil Regions; with Additional Oil Well Records by John Franklin Carll Pdf
This historic book may have numerous typos and missing text. Purchasers can usually download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1883 edition. Excerpt: ...a half south-west of Lottsville, which I have called Miller's Cliff, the other on the south line of the township where the State road crosses it. The sub-Olean was positively identified only in the vicinity of Pike's Rocks, on the east, where it is a characteristic yellow, iron-stained sandstone. On the ridge holding Miller's cliff there is ample scope for it to appear, but I was unable to find an outcrop of it, or anything in the soil which might indicate its presence. This range of hills, however, has been so cleanly swept, rounded and drift covered by glacial action, that the rock may possibly be concealed. I have therefore colored the map as if it had been found. Nevertheless, it may be questioned whether there are not good grounds for inferring that the sub-Olean has been eroded here, and thus allowed the Olean conglomerate to bed upon lower rocks, which might partially account for its low elevation at Miller's as compared with the outliers east and south of that point: Elevation of Pike's Rocks near east side of the township, top--1980 A. T. ""Nuttall's" " south-east corner" "1955'" ""Drake's" on south line of ""1890'" 'i "Miller's cliff, "1880'" The latter view of the case seems warranted also, by the following facts: In the vicinity of Wrightsville, a massive flat-pebble sandstone or conglomerate, 15' to 20' thick, is plainly exposed in a number of places. Its top at Wrightsville is 1600' A. T. The base of Olean, here, judging by the surrounding outcrops, would be about 1910' A. T, --making an interval of 310' between the two rocks. The Wrightsville conglomerate is also exposed in several places around the ridge containing Miller's cliff, where it lies, ...
Report on the Coal Mines of the Monongahela River Region from the West Virginia State Line to Pittsburgh, Including the Mines on the Lower Youghiogheny River by J. Sutton Wall Pdf
The 12 heliotype plates are from photography by E.B. Harden (topographer of the survey) and are views of vernacular industrial architecture of coal tipples, priarily on rivers, and one of a compressed air locomotive.--David Hanson documentation.