Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
I advise employees, the pieces are of
all sizes from very small ones to three 3 to 4
and even 6 inches across. Sometimes these
cylinders are badly squeezed and drawn
out. They are the ochrestone where the pellets
are much thinner and more elongated. See
my sample.
These flat pellet conglomerate have the
pellets usually of limestone, and one wonders
when the limestone were came from some such
formations are not to be seen. Are they probably
the semi-crumbled limestone of a year or two
of accumulation not far diaforetically attuned
to dolomite before entire cement in the dolomite?
Extra get thought me for aug li at Shipgate Forky.
The gravel conglomerate seen not far from
Senjia Center are most interesting because
of the quantity of pellets, their large size, and
the little dolomitic parts that find them
together. Some of the blocks are 8 feet long
and the others divisions may be 6 and 4 feet.
They consist of three kinds of dolomites, of the
older formations. However one sees no flumar
sand rock, nor brown white quartzite, and nor