Page:Field Notes of Junius Henderson, Notebook 2.pdf/27

 limestone is a conglomerate laid on an eroded surface. It is in a crushed zone, however, and the apparent nonconformity may be due to crushing. Below the conglomerate just mentioned are red thin bedded slightly calcareous sandstone dipping 10˚ N. 63˚ E., which is in turn underlaid by conglomerate unconformable on lower similar sandstones and then other conglomerates all slightly calcareous in places. Section at, top and bottom reversed. -Granite -Covered zone, 25 ft., perhaps weathered granite as at Very massive, hard, coarse conglomerate, dip 15˚ bearing N. 63˚ E. 8 ft. same conglomerate appearing at intervals above debris for 200 yds to E with rotten deep red conglomerate in upper 100 yds, of considerable thickness -Covered zone of 200 yds or more with 4 or 5 ft of hard gray limestone about midway -Pinkish gray calcareous sandstone, rather thin bedded.