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Contributed by Yale Peabody Museum of Natural History.
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Transcription
carries the uranium at the Carlie
Mine) Locally one of the sands in
the clstn interval thickens and it
grows those above and below to
form a single unit of sandstone
est. by Max and Bob to be at least
150 to 165 ft. locally. This happens
in Black Gulch, lower half in the SE¼
sec. 34, T. 52 N., R. 66 W. Also is
clstn zone above Top Lkote SS but
not certain how much.
Unconsolidated clayey & sandy gravels
common feature of Lkote in this
zone, and they contain polished
pebbles as elsewhere. The top SS
is above these, the lower, larger
SS is both below and at least in
part equiv. to them. Locally lower
SS has brecc with soft beds –
usually fairly coarse or gravely
(See loc. A for good section of
coarse lower beds – and on up
into Fall River but top SS small
or absent)
Most unusual feature is the
consistency of thick cyltc sandst.
in this zone. Cgl at very base
typified by abundance black
chert pebbles
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