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[[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