Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
Sep 12 - 99 Tuesday
I have come about 3 miles west of the
University of Wyoming cabin and am sitting in
the rim of another Triassic amphitheatre.
The centre of the arch is cut out and above
I put the beds dip to the N. E. Looking down
the hole the beds are seen to dip to the W, S. W,
and S. To the south are higher hills and contain
both Jurassic and the same occurs to N. and E.
Directly W are the Shirley Dots, a
perend [illegible] North Dot like those at Bullwain
but is solely lies to the S. W.
The thickness of the red beds beneath the
Forego Out Limestone cannot be less than 400
foot and may exceed this. The White Trias
is visible on this hole as in the one beneath
Forego Out Dot.
The F.O. limestone in the cliff is about four
feet thick but some of it is washed away. Collected
a few more fossils from this zone.