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Contributed by Yale Peabody Museum of Natural History.
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Transcription
Perce', Quebec, August 6 1929, Tuesday
Started our tope 8A.M. tr investigate the Priests road
tr locate on Clarke's Map of 1917 the various geological
formations, and tr take dips and strikes.
Crossing the front - Tron au chat - one soon saw that all
of Clarke's Hog is Ordovician like Perce' Rock. It stands very
vertical = dip 75° S-E, strike N.85° W, and is cut by pink
orthal. jdg mns near at right angles to the strike.
Where the Ordovian comes to the Priests road the dip is 70° S.E.
and strike N. 70° W. This strike leads into Tron au Chat puleh
where the Ordovician is outcrop by the Bonarentine. The Ordovician
or the road crosses a wide gneis. In the gutter saw a little
fluctuated Ord. outcrop.
Then follows the Bonarentine crop, about as Clarke has it,
only it appears to be continuous with the Bonarentine of the
Pic d'auron and in the criele.
It appears to lie nearly horizontal, and mostly
the pettles are of the Ordovician.
At the Grand Coupe the Bonarentine trace of St. Anne
comes down all the way to the stream. here crossing the road and
even below. How the strata appear to be horizontal all the way
to the top. At the mouth of this brook in the Richmondian and
I judge it comes up all the crees, and is outcrop by the Bon-
arentine and notes Clarke has it north a litt of the Heldetley in
2 morg; his notes should come up to enclose by the Bonar.