Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
166
upon this
The dolostone are saccharial on weathered surface,
the sole climbs about mid-size. Occasional
molds of juvenicide or brachiopod but
not preserved well enough for identification.
A few horizons seem uplifted, but
no apparent fossils. The lower carbonat
is more a dolomite with considerable
amounts silt & clay. This joins
perhaps 600' at Brooks Ranch.
Drive past Allison Ranch to outlying K and
walked over to the Raymond outcrop just to the
NE. Here the Raymond dips about 30° SW,
Strike N40W
without much apparent folding or faulting
just nice even beds. These sandstones
have incised & flow-cast marks and
much slump wrinkles—quite a mess.
The