Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
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Transcription
Sunday Sep 7-1904
I am again at the fault line near
the Benas Ldt. The line dips to the N. at
a high angle, and to the S. calls our land
and the ramp ldy. The strike of these li.
just around [illegible] to the south y the R.R.
quay in the Pind. Later I learn that the fault
line is a little more S. There is a Pinnt line just
to the S. if the vertical rocks at the R.R.
and it's the same Pinnt in Harrington.
Gore on the R.R. Pind quarry. These Pinnt li.
dip 80 N. and strike N, & E. The thickness is
about 200 feet across strike. The line on,
the border of the brwell help to the higher Bluean
Between lines the fault.
As I sit at Harrington Gore and look N
I see another Pinnt on the hill under him and
visited with hard sandstone. It dips 60 S.
Therefore it is the same Pinnt turn over, and
accordingly we have an arch here. I saw this
same fold in the Intermediate gerd. N
As the dip in all places is to the N
for all the li., Harrington Gore are the R.R.
lead me now the leading not one li.