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Contributed by Yale Peabody Museum of Natural History.
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Transcription
all shales in about 10 fut mine, due me see the same
fauna that occur below the Catagoga bed.
I can come in shales with many thin limestones for 10
fut and then again to blue shales with almost no
limestone. Drill goes on upward the shales pre-
dominating by far, and the argillaceous limestone many.
One sees no diagnostic Richmond faunna until the second
Catagoga zone and here only
on this layer.
I did not go higher up in the
section today. See July 24 for remainder.
The lower Catagoga zone and the Virable
bed below are the same collected at the Clay Cliff.
Here as here the R. alternata come in higher and
then continue upward. In Gottmans Brook or
far as I can make out there is no sharp
introduction of the Richmond fauna and
hardly any of this fauna is present until we get
to the second Catagoga zone. Even then
and most of it is above that bed.
The Richmond fauna is near striking, I suppose
because now all the strata are blue mud.
I do draw line much to the south with the
Clay Cliff towards the open marine creatures.
On the basis of the barometer measurement
of Collingwood mountain which is about 810
fut from the lake level to the base of the