Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
The Kxss didn't recognize the complicated
structure of the gap area. I believe there
"#143" unitank is on the same bed, faulted
into 2 portions. The N75-90°W faults
do this and the N-E faults tend to make
the units appear thicker than they are
normally.
I conclude that eastern most "upper"
Wolfcamp contains Tenney (Haymond)
& Dimple. The Dimple in very dark is,
the Tenney Haymond are quartzites.
The massive is out of the wolfcamp - seems
to grade laterally into bed 3, section 17,
but faulting may make the picture more
complicated.
This is look like the only answer to
the grouping of just even to place these
"upper" Wolfcamp beds in Section 17.
The conglomerate would suggest it
should fall & called here, but the
catalogues similar to the upper
Wolfcamp. The fossils suggest an
association that seems related to the
Widowmaker - level. Of those beds are
[illegible] slightly more coarse than the
upper Wolfcamp.
we are about 12 miles away & - There is
no typical couple of the Kxss before
we get into the salty portions. We
ride here. Problems!
It will pay to investigate the outcrops
in the canyon south by the Allen-
Panch. The "wolfcamp" may be
shoved there, but I really wonder!