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Geotechnical properties of the soils affected by piping near the Benson area, Cochise County, ArizonaBenites, Luis Alfredo, 1942- January 1968 (has links)
No description available.
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Geology of the Pickhandle Hills, San Bernadino Valley, Cochise County, ArizonaKelly, Richard James, 1941- January 1966 (has links)
No description available.
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Geology of the Eagle Peak-Hell's Gate area, Happy Valley quadrangle, Cochise County, ArizonaPlut, Frederick William, 1941- January 1968 (has links)
No description available.
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Fusulinid fauna of the Horquilla Limestone in the Gunnison Hills, Cochise County, ArizonaEstes, Wayne Shelton, 1928- January 1968 (has links)
No description available.
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Vegetation as an indicator of rock types in the northern Swisshelm Mountains, southeastern ArizonaBradbury, David E. (David Edwin), 1944- January 1969 (has links)
No description available.
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The geology of the Seven Dash Ranch area, Cochise County, ArizonaCook, Frederic Stearns, 1900-, Cook, Frederic Stearns, 1900- January 1938 (has links)
No description available.
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THE RELATIONSHIP BETWEEN IRRIGATED FARMLAND DECLINE AND PHYSICAL LANDSCAPE FACTORS: A SPATIAL ANALYSIS (SOUTHEASTERN ARIZONA)Towne, Douglas Clark, 1962- January 1986 (has links)
No description available.
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Lithofacies, depositional environments, and diagenesis of the Mural limestone (Lower Cretaceous), lee siding area, Cochise County, ArizonaMonreal, Rogelio January 1985 (has links)
No description available.
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Geology and ore deposits of the Dives and Gold Ridge groups, Dos Cabezas, ArizonaShields, James Culver, 1915-, Shields, James Culver, 1915- January 1940 (has links)
No description available.
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Geology, mineralization, and alteration of the Jhus Canyon area, Cochise County, ArizonaChakarun, John Douglas, 1945- January 1973 (has links)
The Jhus Canyon area, located on the northeastern flank of the Chiricahua Mountains, Cochise County, Arizona, contains rock units from Precambrian to Mid-Tertiary in age. Precambrian granite, Paleozoic and Early Cretaceous sedimentary rocks, and Late Cretaceous(?) andesitic lava flows have been intruded by a complex Mid-Tertiary stock. The youngest rocks present are Mid-to-Late Tertiary rhyolite dikes. The effects of hydrothermal alteration are conspicuous both within and adjacent to the stock. The igneous rocks of the stock display propylitic, argillic, and phyllic alteration. Sedimentary hosts were altered to skarn, hornfels, and marble. Silicification is prominent in both the igneous and sedimentary rock types. Pyrite is the most abundant sulfide mineral in the area, but minor amounts of chalcopyrite and molybdenite are also present. The existing level of erosion is believed to expose the most intense and extensive alteration and mineralization that developed. No ore deposit is thought to exist here, but molybdenum values from rock chip samples suggest that the southwestern lobe of the stock is worthy of closer examination, especially for skarn occurrences. Mineralization in the nearby Hilltop Mine area is not related to the Jhus Canyon Stock, and its ore potential must be evaluated independently.
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