Field Operations of the Bureau of Soils

Cover Field Operations of the Bureau of Soils
Field Operations of the Bureau of Soils
United States Bureau of Soils
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Only glimpses of the other formations are had occasionally in gullies and cuts.
The second or Iowa invasion of the ice was the source of the present soils. The drift from this glacier is only found in the western fourth of the area, where it occurs as the elongated lobes of small hills, the first entering at Farley and reaching to Epworth, the second entering in northern Whitewater Township and reaching to Bernard, and the third following the North Fork of Maquoketa River and one of its tributa
...ries from Cascade to a point a few miles south of Garry Owen.
All three have a southeast direction. They are mainly indicated by a series of sandy loams, with occasional large and small erratic bowlders scattered about on the surface. Reaching out from the border of the Iowa drift is a continuous sheet of finely divided and homogeneous material lying unconformably over the formations mentioned. It is largely a silt, and contains no particles coarser than fine sand. Because of certain peculiarities it has been termed loess, and is correlated with vast areas of the same material that extend through the Mississippi Valley from southern Ix)uisiana and Mississippi to Canada.


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