Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
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Transcription
Than farther south to where the road
comes Bris d'Arc creek and Rees lo-
cality number 41. Here are some about 3
furl of a fossiliferous erguina layer of
grind stems. The fossils collected are all
of the uppermost 2 to 3 feet and have
specific determinations: S. munchisoni,
Threcharius oralis and other Upper Cretaceous
backshores, but the list not true. They
are good only for design determination.
Overlying the fiddle erguina occurs 2 to
3 feet of what appeared to me not to be a
clay but material like the Camden
novacalite. It had no fossils. It is probably
down a residual chalk. The middle of the Bris d'Arc
is given as 30 feet. The next may be [illegible] and.
Than a little farther south are collected
on a farm
a small fauna out of the dogamne lime-
stone, here 2 to 3 feet thick. These fossils
were determined at T.I.C returned to
Mayan. They are in Section 11, 2 R, 6 E,