Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
Fault line
State quarries
Barry Hill, Cambria
Public Park
Richmond dyes from Sanda Drive.
Coast Station area
Tracy hills. Cliff cliff
Eastward arm hills at millis.
Eclerminis
old formation.
Quartz Ridges
Old land surface ad when.
greatly altered by faulting.
This land surface may have
been uneven causing the
difference in the hills resting
upon the Tracyte. The
Eclerminis may
be ancient folding of the joint
in which quartzite
of the sea.
rising disturbed formation.
May the Eclerminis be of entirely charac.
ter, or at least of shale deposits?