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History of education of Cochise CountyBlack, James Walter, 1912-, Black, James Walter, 1912- January 1940 (has links)
No description available.
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History of education of Cochise CountyBlack, James Walter, 1912- January 1940 (has links)
No description available.
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Ground-Water Flow and Interaction with Surface Water in San Bernardino Valley, Cochise County, Arizona and Sonora Mexico.Davis, OLaura Agnes January 1997 (has links) (PDF)
Thesis (M.S. - Hydrology and Water Resources)--University of Arizona, 1997. / Includes bibliographical references (leaves 311-317).
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The history of the lower San Pedro Valley in ArizonaMuffley, Bernard William, 1909- January 1938 (has links)
No description available.
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Application of Remote Sensing in Floodway DelineationClark, Robin B. 20 April 1974 (has links)
From the Proceedings of the 1974 Meetings of the Arizona Section - American Water Resources Assn. and the Hydrology Section - Arizona Academy of Science - April 19-20, 1974, Flagstaff, Arizona / Population pressures on the land resources of Arizona have led to the sale and development of areas subject to flooding and because of the inadequacy of land use controls, the area is open to various land speculation schemes and unplanned subdivision growth. A floodplain delineation project was conducted for the planning department of Cochise County, Arizona, in which imagery acquired by earth resources technology satellite (ERT-1) and by high-altitude aircraft was employed. Parameters of the analysis included soils and geomorphology, vegetation, hydrologic calculations, and historical data. Floodplain soils lack developed b horizons, as compared to older, more mature soils not subject to flooding. General soil maps can only be used as guidelines, but a detailed soil survey can add significantly to the accuracy of image interpretations. Erosion-affected soil tones in areas adjacent to active channels proved beneficial in that the heightened contrast served to enhance resolution of vegetation-type boundaries. Hydrologic calculations were done based on valley cross-sections surveyed at two-to-three mile intervals. The historic data input into the system of floodplain delineation is dependent on the location of high-water marks and on obtaining a record of the amount of rainfall which resulted in the high-water mark.
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