Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
Marathon, Texas, March 21-1924, Friday
With the old dilapidated Ford and the boy
Lauffen went about 18 miles northwest to the
junction of the Brad Canyon into the Lillian
canyon. Here on the southeast side of a four
mile ridge occurs some 25' or a thick reddish
limestone about 64' but thick of the Permian
(Basil formation) of Uddins Section #1-4.
Here occur large Permian Fusulinids,
some of which must be an inch long and nearly
one-quarter inch thick. Also some large Lob-
tidus but no Rickettsiaenia. One layer of
pelitic limestone in relation with Ammonites.
One can carve one's initials into the rock with
the hammer, but as they weather out the
oilicity, and as not good pencil marks they
are to be seen by the thousands. Looked about
5 hours to get them, and I think have a
representative lot.
One sees almost no other fossils.