Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
From these narrations although imperfect
it is evident that the Brindon series appears
at the end of Logans section and not in it
as many have assumed. Further as the strata
of Black Point dips in the reverse direction from
those to the north of Downing Creek and with
the same strike and low inclination that we
have at Mill Cure the apex of a flat an-
ticline. Logans just syncline therefore here
comes to an end and passes over into a
just arch. The rocks of Black Point in
all probability are somewhere in the upper
part of Logans divisions & further north the
topmost beds that have the limestone enplo-
ments. This matter can easily be worked
out by Bell who will do or during the
summer.
What the relation of the Brindon series
is to the Jogging series we do not yet
know but it will in all probability turn
out to be one of angular unconformity.
Tomorrow are go by rail to Oorakatu
and then by carriage south to Hardledge
which is at the peninsula opposite Joggins
Mines.