Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
Mexico City Monday Sep. 10-1906.
In the morning attended the session of the
Congress. Some time was devoted to a discussion
of geological climates.
Ordnis was the first speaker as Chamberlin had
to leave the city. He offered no particularly new
views but indicated the old and new ideas of in-
terpreting geologic climates. He thought the old idea
of cooling earth had to be laid one side be-
cause of the Cambrian glacial period, and especially
because of the indication that there may have been
Precambrian glacial periods.
Last year he had seen the Dwyka conglomerate
of S. Africa and it indicates that this Permo-
Cretaceous glacial region had not been laid down
in a high country but that the land here had
totally been reduced to a low land. This region
was not far south of equator. A cooling climate
he did not think the probable explanation but
due to some oscillatory cause. He suggests a
cold climate with a summer snow fall.
Beetle suggested that as Loengly had shown
that the sun is a variable star may the glacial
climates etc due primarily to this cause.