Viewing page 45 of 77

This transcription has been completed. Contact us with corrections.

[[blank]]
[[end page]]
[[start page]]
bed of conglomerate of small pebbles was superposed on the limestones.
[[line]]
Aug 2/95
West of the stream the limestones and shales are again seen forming a low arch, westward from which they are surmounted by a regular series of beds which have a purplish or reddish gray tint from a distance and being of varying hardness rise in a series of benches to a summit about 2000 ft high.  The harder beds are limestone without fossils, the softer ones a caleareous shale which crumbles into small angular fragments making long uniform talus slopes.  The limestones contain many mostly lenticular or spheroidal whitish concretions which affect