A description of the "Bernardston series" of metamorphic upper Devonian rocks

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Abstract
Desoription of the Region.-Theterrace sands of the Oonnecticut river are narrow upon its western side where the river crosses the State line, and they continue with little increase of width for foul' miles southwesterly, and then, as they enter Bernardston, their boundar'y upon the older rocks turns abruptly west, and rnns for seven miles a little south of west, past the village of Bernardston, and along the north line of Greenfield.Bernardston village stands just in the.middle of this line, and at the mouth of a narrow valley, up which a lobe of the alluvial sands reaches northwardl'y for neal;ly two miles.On the west, this valley is bounded b'y the high ridge of West Mountain, made up of the contorted argillite which stretches in a narrow band far north, across Vel'mont, and disappears below the river * The introductory part of this paper, giving a history of previous investigations in the region, is here omitted.The publications mentioned in it, which are of chief interest in this connection, are: Prof.
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Authors B. K. Emerson
Journal american journal of science
Year 1890
DOI
10.2475/ajs.s3-40.238.264
URL
https://ajsonline.org/article/64358.pdf
Keywords Keywords not found

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