Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
Garlends interpretation is that this
is a channel sand originating in
the [illegible] Fall River, whereas I
interp. as a "Fuson", or post-Fuson
sand truncated by Fall River
plane of contact. At F the
top surface is plane , but neither
interp. can be eliminated. At H,
however, the "Fuson SS" is still
present but not completely
occupying "Fuson" interval, and
we found the weathered zone
with red clays tone beneath it
resting on "Fuson" SS. I think
this relationship favors my
interp. espec. since Garland has
mapped the SS in detail & shown
it to be same as at F.
Suspect that the "contact" of
Fall River & Fuson-Lekote will be
found to hold in the Southern
Hills , but that it may be
complicated to find locally
because of Fall River (in my sense)
channeling and more widespread
presence of the "Fuson SS"
Saw contact in Henry Bells'
Flint Hill quad. but had difficulty
with it where his "Gould" SS
was present. Here the gray
2.