Wind action in Maine

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Abstract
DRIFTING sands of the ordinary type are very common in Maine, especiall'y in the western half of the State.These sands are partly of marine, partly of fresh-water deposition.All of the hU'ge rivers of Maine, except the Penobscot, covered large areas with sand near where they emptied into the sea during the Champlain epoch, the sea of that period being, as is well known, somewhat more than 200 feet 9.bove its present level.For various reasons the drift of the Penobscot valley differed considerably from the valley-drift of any other large
Reference Key
openalex_W2326300239 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors Graham Stone
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Journal american journal of science
Year 1886
DOI
10.2475/ajs.s3-31.182.133
URL
https://ajsonline.org/article/64245.pdf
Keywords Keywords not found

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