Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
Saturday Sep 2 - 1933.
Wea. SUN. NOV. 7, 1909 Ther.
The so called ridge of Mallett begins at
about 200 feet east of the Russell quarry. The
ascent is up over the dip slope here as in the
Russell quarry, about 200 E. The gray-white
very sandy [round grains] and marip[ose]
dolomite occupies the entire ridge to the low ground in the near where the
dip is about 50 E. The thickness can be esti-
mated from the topographic map. [about 330']
Beneath and to the NW lies another series
of streaked red gray and darker gray sandy (even
coarser grained) dolomite. These do not belong
to the