Studies From the Geological Department

Cover Studies From the Geological Department
Studies From the Geological Department
William Shirley Bayley
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At one point it contains stratified gravel. On the west the terrace falls away in a steep bank of drift to the flood plain of the river, but on the south a second, lower, terrace of considerable extent occurs at an elevation 40 feet above the stream.
The 70 foot terrace is again seen opposite this point across Middle Fork as a narrow shelf on the bluflf where a tributary valley comes in from the west.
As before mentioned the point between Middle and Salt Forks and the knoll to the south represe
...nt a terrace from 60 to 70 feet above the river. A corresponding terrace may be seen on the bluffs at the south side of Salt Fork just west of its junction with Middle Fork. On the north side of the Vermilion in Sec.
15, T. 19 N., R. 12 W., just north of the knoll previously de- scribed occurs a marked terrace at 70 feet above the river, (PI.
Ill, Fig. 3) . In a road cut the following section is exposed : Sand and glacial gravel, water laid 2 feet Shale dieintegrated to a sticky clay 3% feet Clay shale On the south side of the river in Sec.


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