Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
August 19, Hankes Bay. North done continued.
average dip is 4S.30E. to the try core, where it appears to swing around
or the same layer continues to form the shore just the point at the
east edge of the try core. Within the next 300 yards we go down
through 10 feet of Cryptogon beds and 10-foot more of sandy li.
with some harded layers near the base, but the basal 3 feet shown
[To S. that is an argaceous li. and one or something]
is leary redded red li. Here the dip abruptly changes to 30d.
20 W, but whether by a fault or sharp flexure cannot be seen.
(= ? sometime)
Downrun the same red line is exposed on both side of this line.
Continuing down run in the section there's about 15 feet of reddist
li. Then 10 feet of thin redded fluit li. with interbedded dark
shales.
Within 70 yards we come down through the above 10 feet of
strata and then ascending to the red li. Within the next 70 yards,
Here there's clearly shown a sharp anticline and the red li.
plunges again to the southward.
Then follow an unexplored interval of about 150 yards or
where the leary redded quartzite is exposed, almost dipping
20 S.60 E., but within a few yards swinging to due E.