Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
While changes run into on one lying oratus, lime
stone and then magnesia limestone. According
therein we have here a at firstly, and there-
fore due in the area of the meeting of the
mother sea with the Arctic or Gulf sea.
Cataract. Whirlpool sandstone at base.
days
Over it lies thin bedded fissile blue shales for
fath, then a zone of the same shale only a few mus
thousands of impure dolomite dividing the fauna I
collected some years ago, about 5 fath thick, followed
by once shale of the same characters for 19 feet.
Then 5 fath zone of thin bedded dolomitic limestone with a brief sandstone between the top, the limestone
limestone reflects onto Oreltonia and almost no shale
fartings. Lots of Lajula payments. Mayhara & cuneata.
Then once blue shales for 3 feet above
then sandstone and red shales of the Medina appear.
I would say the Ordovician therefor 32 feet above
the Whirlpool. It is due that the Medina sandstone,
There in our head here between the Cataract
and Ordovician. Then is best seen in the