Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
Sunday August 14-1932
Wea. TUES. MAY 25, 1909 Ther.
A fine cool Sunday morning, and I appear
Typical litter. At 11 A.M. Scam off in a Bus
for Swanton.
After lunch went E. to the "Chazy" exposure beside the
E-W road to Highgate Center. It is the Algoma Phillipsburg
series, has alternating granite and dol. that have flown
manure
over one into another. The dip is high from 50°-60°
or more to the E. The dol. are much torn due to pluge.
It is on the Chazy and primarily not the Phillipsburg marble, but
other marble beds in the same series.
Just at the N.W. of the Minisquari ****** Staradbridge
manure
River (Miss. River) we
find exposure of the Phillipsburg blue-white marble dipping
E. about 25 degrees. The line is angled for high.
I saw the same marble at the N.
Minisquinibridge in Swanton where all the trails are
and the dams run the falls.
South E of the River the banks are made of the Devonian;
and grey east of the old damm trail one has a good
display of the Devonian dipping E at 20 to 25 degrees. This
cap. I move to dip.
is east of the old Swanton Marble quarry, After going about
4 or 1/3 mile The Parker Shale comes in, and it can
be followed east along the telegraph line for another
1/3 mile. Towards the top is a dol. some and primarily
the same as at the top of the Parker Chible. The