Note on the age of the Green Mountains

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Abstract
t The conform ability between the TaC'ollic schists and the adjoining limestone I have observed at varions 10eaUties in Vermont, Ma~sachllsetts, Connecticut and New York.part of the localities on the west side of the range and the rest on the east; and between the same limestone and the schists (inclnding mica schists and gneiss) and quartzyte to the easLwal'd also at several localities in Vermont, Massachusetts and Connecticut, so that the fact cannot rightly be questioned.The discoveries of fossils near Newburgh, west of the Hudson, by Whitfield and Dwight, are additional evidence as to the relation of the rocks.
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openalex_W2325590025 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors J. D. Dana
Journal american journal of science
Year 1880
DOI
10.2475/ajs.s3-19.111.191
URL
https://doi.org/10.2475/ajs.s3-19.111.191
Keywords Keywords not found

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