Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
62
July 17 - 1918. Wednesday. Dominion Q. to Bluff Head.
The first day in Newfoundland.
Before morning. We walked two hours at the Campyge bed about
1/2 mile southwest of the Dominion Quarries, but about one degree entire
trilobite.
The boat went to Port au Port from rail and gasoline. We had an
early lunch and left our third camp at noon in the soft shore and
Bluff Head.
As we got toward the east side are here a fine area of the Osts
boundary of the land, it is plain that the limestone strikes once and once into
the sea by the strike of the strike on the Ont. Then
the land as are for meander. This is probably the reason why one does not
see the li in Hunter Arm. Further more as we go north we get into grayw
dolomite.
At 2:30 P.M. are we within 1/2 mile of Bluff Head and so ashore,
we begin with some marked beds of red shale and olive green sandstone
and are so conglomerate like those noted on July 11. It's the continuation of
the section then uncompleted, soon all is interbedded coarse sandstones
with finer
conglomerates
like those below.
and arkose conglomerates in one place there is a 10 foot bed of conglomerate
the fragments of which are
made up of the formation itself, ranging from coarse sandstone and
shaly sandstone. The boulders are well rounded and range up in size
Another thinning gray ones with a patch of Conglomerate.
to 18 rocks across. That is 700 to 800 feet of these sandstone. Then a
vertical standing
little of red shale and dark blue shale interbedded with the sandstone,
Then a valley and a gravel fill, it is about 1/4 mile across this core to other.
the arches can again expand, here are small marked red shales with zones of
then fiddler sandstones. Then a very much crushed zone of the olive-green
sandstone with large masses of limestone. The latter are broken for an extent
and maybe of the Pabandonion.