Clifton, Arizona (Laigler, U.S.G.S. Prof. Pap. 43, 1905). North of Bisbee, 120 miles, near the New Mexi. can line on San Francisco river and not far pa Pala river Pinal schist at base. Quartzite schists. Granite cuts the Pinal. Almost always undulati the Paleogric. A normal granite. Coronado quartzite, 200' There is a basal engl. 0-50' but often absent, rest quartzite. Strong red pind in maroon. Still from 2 miles north of Morenci. North of Morenci Canyon, on left, Ordovician on right, faulted down. West in Chase Creek, uplifted near Longfellow incline, has capped by Ord. 2 miles S.W. of Morenci the following section: White quartzite 50' Banded, pind & maroon quartzite m. Blopp. 162 Quartzitic engl. 10 Sandstone 3 Quartzitic engl. Petks up to 7 inch 8 Crazed sandstone at base 10 --- 243 Criths p.m. older rocks, thrusts outy Pinal. No granite pieces. Engl. "a fluviatile deposit gradually merging into marine conditions." A transgresion on an irregular surface. Just south of Longfellow incline in Chase Creek, in