Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
25.
Clay lens? comes in here, very silty, similar
to that at (23). Considerable SS over it, may
be below for Dakota clay. - Note - is lower split
main clay.
26.
1st Glen SS thick, due to coarse calcite in
lower 5 to 6', just above caltz zone is
coarse clay pellet zone - a local lens.
27,
Disconformity - lies between m wash covered
slope between 3rd SS and top Lytle SS,
a zone 5' to 8' wide. Lytle SS quite thin -
at least part cropping. No cyl, few scattered
pebbles. Local concent pebbles top surface.
Note on clay beds: - Main bed- after pinchout at (21)
not traceable but would guess horizon .
lies mostly E of crest. The clay that
comes in at (23) not identified- it split
of main bed it is very low in slope, yet
high for Dakota. Looks like clay that comes
in at (25), which is lower split. Main bed
comes in at (28); the lower split sends out
into gap, main bed crosses, lies between SS's
on other side.
28
Main bed === 4' t with basal bent, oval ripple
marked surface (picture)
Note on Dakota clay: If Dakota clay is in at all
it is at break in steep rock slope along
east base hogback- local silty beds
crop out in this position near gap.
No good Clay seen. Bed must be
within 10' ± Graneros contact.
Greneros contact not visible but
assumed near lost SS ledges cropping at
gap.