Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
The succeeding 18 feet consists of grayish
sandy shale with layers of fine grained
gray or yellow sandstone an inch thick.
Above is 40 feet of purplish-black shale
like that at the base, succeeded by 15 feet
of drab clay. About 110 feet above the
base is a bed of friable fine-grained,
achre-stained sandstone 18 inches thick,
overlain by a few feet of light brown
clay. The uppermost 25 feet consists
of paper-thin layers of purplish-black
shale with gypsum filled cracks. The
member attains its maximum thickness
near Colorado City where it is 145
feet thick, but in the southern part
of the quadrangle it is much thinner
and in places measures less than 10
feet.
Dakota - Shows Dry Creek Canyon member present
in Bear Creek section - which must
be good'.
Richardson (1915) - Recognizes Purgatoire and its
members in Perry Park. Does not separate
members as 'exposure' too poor. Glencairn
equivalent apparently chiefly shale as
at type.
Stose, (1912)
Purgatoire formation. - The Purgatoire formation,
(p. 3) which is composed largely of sandstone,
was formerly regarded as part
of the Dakota sandstone and is so
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