Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
layer. The section is thus
Wticia
Trenton
10 foot mine.
Boulder bed 4-5 ft.
locally Disconformity
Blue Trenton
11 fath.
wave layer 8-10 inches
sometimes 30 inch.
30 fath to track.
If mine the 70 foot mine
to low water mark.
Thin the boulder bed of Barlow
On close inspection it is seen that the
Boulder bed is the channel of last bottom of the Wticia
sediments. The whole was rolled about, of mud
and many of the round trees rounded are then
are packed together. The contact with the Blue
Trenton is very sharp, the lower Trenton is smoother,
even bedded, blue-mud limestone, while the Wticia
begins yellowish-grey, granular with considerable
clayey material. During the boulder bed or foot
away we saw this:-