Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
May 1 - 1913 Thursday, Hancock.
Started out to walk from Hancock to Tonoloway
along the Western Maryland R.R. Checked my baggage
to Cumberland.
In the first cut east of Round Top, we see an arch in the
red lalins. The sandy dark red beds are full of long concre-
tions and those are arranged vertically. They are still places of definition
but concretions of lime gathered by a rising and sinking water
with the dryness and petrety of the zone,
tells that they are opposed to the weathering, percolating
water flows along these vertical grooves and changes the ferric
iron to the green ferrous form. About 50 feet we exposed
in the center of the arch one which are about 70 feet of this
kind with similar modular groups.
held red rocks. The grey beds here are all seen
cracked and splitting the dramatic character can be seen
sag through a bed just thick, The sun cracked zone is
any-thin at least 50 feet. Leperditia are
common here in the sun cracked beds. The cement has
followed over above the base of the red beds.
Opposite Lee Johns Run or at level 103 there is
fine exposure of Clinton shales with the regulation fossils.
Here are my large Beysichia, have taken a piece of the
Pennsylvanian limestone.