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Contributed by American Museum of Natural History Library.
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Transcription
Fri. Oct. 16. Load down the river trail as far
as the creek about 1/2 miles away. On way back went
down on beach where we made our first finding (it
was fairly low tide) to have a look at the geology & see
if I could find any fossils.
weathering product of recent time.
bedded, but scarcely consolidated
my fine sandstone
high tidal mark
low tidal marks
equally soft sandstones
with some shales where
beds have slight dip
to west.
As I read the picture there is
a slight break in sedimentation
where the beds lying horizontally come in contact with
the dipping beds. Both seem to be late Pleistocene or
Recent in age, non-fossiliferous, & to contain a good
deal of cross-bedding. Whether Lacustrine, marine or
aestuarine in origin I have not found out. Suspect
marine however.
The hills & ditch here [illegible] them
are merely the products of differential weathering of
horizontal strata of soft shale & sandstone.
Picked up the valves, still hinged together, if a
fresh water clam. Also what may be a fossil seed (but
fine) set in the sandstone left on the beach. (P.S. Not a foal)
The topmost layer of the diagram follows the contours
of the surface. It is mixed reddish-brown sand
clay, almost exactly similar to the subsoil I secured
at Lake Davienville.
Another interesting bit smoked out of tree this a.m. See
cat. # 3005.
Sat. Oct. 17. Put on a drive to get the handicart if
this place. Its tracks appear in muddy low places
close to the river. Setting bs steel traps for it!
Also went out for snelling again. Unsuccessful this
time treated at least a dozen trees.
Brien & Rand picked up some Emballonura bates, apparently
the same as at Black Rim, Palmer Junction & L. Davienville.
This form I shot a caseaway. He was just walking
about in the woods.