The fault at Rondout [New York]

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1879
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Abstract
MATHER gives a section,* from between Glasco and Great Falls of Esopus Creek, in which the Hudson River slates and the Lower Helderberg limestones are unconformably superposed, and the latter present the form of a ruptured and eroded anticlinal.He gives also, Plate 8, fig.7, a rough and unsatisfactory section of "High Rock," situated opposite Rhinebeck, between the junction of the Wallkill and the Hudson.In this section the Lower Helderberg limestones are represented in an almost erect position, resting unconformably upon Hudson River grits.Mr. J.G. Lindsley, the agent of the Cement Co. at Rondout, read an interesting papert before the Poughkeepsie Society of Natural Science on Feb. 26, 1879, which contains the results of local studies for which he has had excellent opportunities.In the summer of 1878, T made several hasty visits to the highly instructive locality at Rondout, and obtained the following data, some of which, as well as the inferences from them, are not given in Mr. Lindsley's paper.The southeast base of
Reference Key
openalex_W2313467896 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors T. N. Dale, S. T. Barrett
Journal american journal of science
Year 1879
DOI
10.2475/ajs.s3-18.106.293
URL
https://doi.org/10.2475/ajs.s3-18.106.293
Keywords Keywords not found

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