Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
Edgemont area with Garland Goff (cont. from p 56,
Ntbk 4, I-K 2)
has traced channel edge; it has a
Northwest trend. Sandstone is fine
to medium grained.
Base Fall River seen at E, F and G.
similar to that in Devils tower area,
Garland puts local channel sand
directly under what I call base,
in Fall River. This in same position
as Henry Bells "Gould" ss. - will call it
"Fuson sandst." here, it would be top
Lokote, one ore-bearing in Cevile mine
probably, in D.T. area.
Fall River - Fuson-Lokote contact.
Seen at E (picture) where it
resembles the "red, white, r blue" contact
of D.T. area. At some of road cuts
we crossed gouztion also evident,
this was in Robinson Flats area.
The Fe specks were present. At E
the contact was within 2 or 3 feet
of basal FR ss and a thin ss
bed was on it locally.
Where the "Fuson sandstone"
was present at F and H we
discussed its position relative to
the Fall River. At F there is no
weathered zone and Fall River sits
directly on the "Fuson SS".