A third occurrence of peridotite in central New York

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Abstract
IN view of the interest attaching to the demonstl'ation by Professor G. H. Williams, of the igneous llature* of the socalled serpentine of Syracuse, N. Y., any further occurrence of similar rocks in this region seems worthy of note.A recent paperi' describes several dikes near Ithaca, N. Y., consisting of a rock closely related to the Syracuse peridotite.In both of these localities the dikes are associated with nearly horizontal, undisturbed strata, differing in this respect from the rock described in the present paper.This rock occurs in the form of a narl"Ow dike in a fault plane at the village of Manheim 01' East Oreek, seven miles east of Little Falls, N. Y.The dike is mentioned by Vanl1xem in his description of the
Reference Key
openalex_W2318325944 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors Charles Smyth
Journal american journal of science
Year 1892
DOI
10.2475/ajs.s3-43.256.322
URL
https://doi.org/10.2475/ajs.s3-43.256.322
Keywords Keywords not found

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