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Sandstone Shale Basalt Line Granite

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Just west of roll the railroad line bends southwestward toward the gila river, which is crossed at the north end of antelope hill, as shown in plate 33, b. this hill is composed of light-colored arkose and arkosic sandstone supposed to be of tertiary age, of which about 500 feet is exposed, dipping to the south at a low angle.

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