Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
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Transcription
Tuesday June 7-1910. Around Delingsine
Left Loris Town on a local at 7.13 A.M.
for Delingsjove Junction. This on the buesque-
hannot from Delingsjove.
First worked south along the railroad and came
across a series of siliceous limestones interbedded with some
[illegible] layers, in which are gathered Styliolina fuscella,
Ambrocelia, Leptrocoelia flabellitis, Cathaerda, and
[illegible]. Have taken there. Begun from about the upper soft.
Then walked south to a place 1/2 mile below the Junc-
tion where there is a cut in cavernous limestones. On the
south surface on the west side of the cut may be seen a
fair abundance of Chonetes opistali, Picipidolites casinota
[illegible], Leptrothyria perplana [cray], Spirifera sculptilis
cray and S. mediaalis.
The dip of all these beds is to the N.N.E. from the Junction
with a gentle amount of dip. The thickness is very great.
I began first
the Marcellus away some distance from the Grand gaps
dips at about 45 degrees but due to weathering gives the
impression of standing on edge. Here as elsewhere the lower
Marcellus has calcareous
concretions, some 6 feet long by 12 inches thick
and then in low sulfur [in pyrite] or decomposition