Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
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Transcription
Feb 15-1924, Friday. Slate area
Started out south of [illegible] and after going
20 miles due south are in the Precal
Crownitis where the Apache series, the Perm-
ian and Carboniferous are well exposed.
Over the Pinal schist with its granite and
diorite comes the Apache series. First is the
Scarnm conglomerate. This I did not see. It is
very much like the Barnes conglomerate to be
described later. The Scarnm is a variety in
thickness from a few feet up to 30 to 40. At
because it is a coarse conglomerate but with
pieces of the Pinal schist and appears to be of
local rocks. It appears to grade up into
guanzites and into the Pioneer shale.
I saw much of the Pioneer sandy
shale. It is a "dark reddish-brown, often
less arenaceous shale composed layers of
fine calcic detritus with little or
calcareous material." Where more sandy,
it is distinctly but irregularly laminated.