Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
August 7-1918, Wednesday
Parson Pond.
A dark but clearing morning. With middle tide at 9.30
we start with the boat cruise along the north shore as far in as we
can get. At 10 we are actually started and at 11.30 a.m., we are at the
very head of Parsons Pond at the foot of the mountains and in front of a
small river known as Middle Brook. There is another one to the
[illegible]
South known as South Brook and yet another one about half a mile
to the East known as East Brook.
As we go up the Pond one nowhere sees any cliffs and the shores
are marshy and swampy to the very edge of the water. The shore
with its smooth granite boulders are nearly everywhere swampy and lie
in the marshy shore. A once unpromising place to work out the
gologic sequence is hardly possible. The inner part of the Pond is
deep enough at all times for one boat, but the outer two miles one
boat can go from middle to deep tide. The present opening has
been made artificially dug and is a precarious place to get
in and out of for a boat drawing 3 feet more of water. Steam
might be done at high tide in calm water.
As we near the head of the Pond it becomes plain that all of the
mountains flanking it and extending to the south and north are made
up of bedded rock. One great precipitous cliff can be seen from the
sea or the village of Parson Pond to be of strata dipping to the south-
[illegible]
East. The southeastern and eastern shore are all of Portlandic age and
apparently are of marble. On the southeastern side about 1/2 mile to
the south of Middle Brook there is a precipitous cliff and other