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The Geology Of The Head Of Chesapeake Bay (1888) (Paperback)
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The Geology Of The Head Of Chesapeake Bay (1888) (Paperback)
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General Books publication date: 2009 Original publication date:
1888 Original Publisher: Govt. Print. Off. Subjects: Geology
Science / Earth Sciences / General Science / Earth Sciences /
Geology Notes: This is a black and white OCR reprint of the
original. It has no illustrations and there may be typos or missing
text. When you buy the General Books edition of this book you get
free trial access to Million-Books.com where you can select from
more than a million books for free. Excerpt: M-oee.] WESTERXJrOST
EXPOSURES. 565 EXPOSURES IN THE PIEDMONT PLATEAU. 1. Lapidam Creek.
-- A number of natural and artificial sections, fairly representing
the geology of the Piedmont plateau, flanking the south side of the
Susquehanna, occur along this creek. Generalizing these, it may be
said that the terrane is granite and associated horn- blendic and
rarely chloritic schists, vertical or dipping south-southeast at
high angles, with occasional veins of quartz. The superficial
deposit on summits and slopes is a red. residuary clay, derived
from the decay of the crystalline rocks, reaching a maximum
observed thickness of ten or twelve feet. The upper valleys and
ravines are lined with alluvium of maximum observed depths of five
to eight feet, although where probably thickest its bottom was not
seen. The alluvium is largely formed of red, clayey materials
washed down from the slopes and in general is more or less sandy.
Both the residuary clays and the alluvium contain occasionally
angular pebbles or bowlders of local rocks, but absolutely no
erratic material occurs at any altitude. The summits of knolls and
ridges generally expose obdurate rock: vein quartz, exceptionally
siliceous horn- blendic schist, etc. 2. Quarry Point. -- Here a
prominent salient, perhaps 200 feet high, is formed of compact,
somewhat siliceous, hornblendic schist, dipping south-southeast 75
to 80. The same obdurate stratum finds a general topographic
expression in a ridge extending north-northeast f...
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