Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
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Transcription
Had to pass my large box this afternoon
as the boat is here to -monus morning about 7.
I heard from a mechanic late this afternoon
that farther around Great Point than I got this
morning that "fine shell" occurs as good as any
I have. This may be an important clue for Wal-
lause points but I fear has no such value.
The geologist of gov gives a point locality at Indian
Point fully two miles east of Great Point.
On the steamer the next morning I noticed
that the limestone seen on West Point continues west
nearly as far as we arrived at Ellis's camp. From the steamer
their color (redish) and general character seems to be
that of the Chalco limestone seen at Chase an
Basem. The strike of these beds is that of the shore
the reason why no other beds came, just before
coming to the Carib. conglomerate a short distance of
stale appears also belonging to the Silurian.
It seems that all the low lying land has a bed
Carb. conglomerate from P. Daniel to Bleach Cope. Of course
at Pierce it lies as much as 1200 feet above the tide,