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Contributed by Yale Peabody Museum of Natural History.
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Transcription
July 18th Thursday.
Trifles easy and write letters.
Left Martinsburg at 3.17 and arriving at
Cumberland at 9. Stopping at Sandons.
Noble and Reeds at Mrs. Roberts,
July 19th Friday.
Cumberland, Md.
Collected all morning up to 1.30 at East Valley.
The section begins in the lower Martins shales and some
limestone [illegible] about 75 feet thick. The fossils collected are
amalgam for the upper ten feet, a few are marked as
from lower layers, there are from about the middle.)
Then follows a series of heavy bedded limestone with
some Charnia for 30 feet. One limestone of the
same nature contains for 25 feet abundantly in
Favosites & Phyphyllum and Stromatolites.
All of these beds are Martinsburg. Apparently nothing
30 feet thick
Above is coral gone but Reeds and Noble
found it of the field and rejected an area across
limestone with sandstone. Can not determine
the origin. In talking to Gordon of this horizon he thinks
it should go with the Ordovician, above has some [illegible],
Then follows the Lower Ordovician.