On the occurrence of a peat bed beneath deposits of drift in southwestern Ohio

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Abstract
V III.-On the Occurrence of a Peat bed beneath Deposits of Drift £n Southwestern Ohio.A BED of peat has lately been found one mile east of Ger• mantown, Montgomery county, Ohio, and twelve miles west of south from Dnyton-in the occurrence and connections of which there are sever:11 facts of unusual interest.It lies in, and directly above, the channel of Twin creek, a tributary of the Miami river.The general course of the creek is southeasterly, but just above the pOint where the peat bed is exposed, it has made a sudden change in direction from east to west of south.Its northern and eastern banks for t of a mile in each direction from the point of deflection, are precipitous walls of stratified clay and gravel, from 50 to 100 feet in thick•
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openalex_W2317256771 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors Edward Orton
Journal american journal of science
Year 1870
DOI
10.2475/ajs.s2-50.148.54
URL
https://ajsonline.org/article/62334.pdf
Keywords Keywords not found

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