Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
Just E. of the Barite, there is a road to the
N. and over by the Barite river. Marked N.
The reason why the Lignite lies so near
farther is because the land is low and
all is mowed into lower or older strata.
Bring up the Kings Road See me
shaly rock that may not be in place. It's in
it dips 80° S. & strikes N. 75° E. This
is just at the end of Barite,
Farther N. on Kings road See a
rock nearly horizontal. Dip slightly No. It
may not be in place.
On King farther W. marked me and the
dip is 30° S.W. Strike N. 130 E. There now
and there and seems to dip into the Barite Camp.
It rolls like Tournum, having due the
trails. The hills are all high to the N.W.
Then left the Kings Road and
to the south of it saw a thin outcrop
of Red Lignite Eridophyllum. It may
be the same zone seen along the railway.
The mining. The private road down on