Field Notebook: Nova Scotia 1914
Page 16
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?