Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
K-Mananutten.
Magnitinsky hole mist.
dip 55 E.
Magnitisky S.S. Orems.
Magnitowsk S6, 41' N
Coral
Base of Mananutten
Strike N. 10 E.
Richnessy
Central.
Palat Fault. Shear out
Subsidence ent. →
dip S. 47° W.
At first the Massanutten sandstone much resem-bles the Martinsburg because much of it is derived from the beds above pieces of a clay shale for the Martinsburg sandstone or shale, I have however the former attains its regular character of spotted red and yellow whitish quartzite. It is always a much harder and more regularly bedded sandstone than that of the Martinsburg. The Massanutten is a sandstone or rather quartzite throughout. Some of the layers are made into stains and seams somewhat Clinton in ore.
Magnitinsky fault
Martinsbury
hole
to next Mananutten about 1000 feet
Mananutten
fault
hollows
Martinsburg shale
dip S.
Massanutten
dip 17° S.
hollows
1-7389