Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
101
Saw our Permian predicts of material. No has
Nitre any on this trail.
In the lower Lufai appear the large Perducts'
as seen in Starbury Hill near Pine.
Redwall - Lufai contact not once exposed, where
it was fairly clear the contact was an even one. Our
or projection of the Redwall into the Lufai as near
June.
The lower Lufai is the mostly shaly part of the for-
mination, primarily for 450 feet. Then for 375' foot the Lufai
has more and more benches of sandstone. Then a cliff
making or 25- foot thick. Then a shaly zone for
70 feet. Upper Lufai is decidedly thick bedded
sandstone for about 330 feet = Hermit. All of the
thick bedded sandstone tends to be more lens cus-
bbed. Saw well up in the Lufai this thick goes
(3-5 feet) of nodular limy beds, a short of intraforma-
tional conglomerate, a falling of calcareous petites, little
Saw last summer in Kora Desert with Belle.
The fresetting of the Coconino into the S, here
is very little in the reverse direction to N. Saw once
like this:
[illegible]
The sands have
angular and more
or less angular.