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Chlorinated insecticide residues in the Santa Rita mountain areaLaubscher, James Albert, 1938- January 1968 (has links)
No description available.
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Geomorphology of the Box Canyon Drainage Basin, Santa Rita Mountains, Pima County, ArizonaVan Fleet, John Milton, 1948- January 1973 (has links)
No description available.
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Tactite alteration and its late stage replacement in the southern half of the Rosemont mining district, ArizonaMcNew, Gregory E. January 1981 (has links)
No description available.
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A gravity survey over late Quaternary fault scarps west of the Santa Rita Mountains, ArizonaTanbal, Khalid Mohamed, 1958- January 1987 (has links)
No description available.
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SOCIAL AND SPATIAL SYSTEMS IN A TEMPERATE NONBREEDING BIRD COMMUNITYSilliman, James January 1981 (has links)
Field work to determine possible causes of variation in avian social behavior in a nonbreeding community of 42 species was undertaken during two winter seasons in oak-juniper woodland of the Santa Rita mountains of southern Arizona. Transect observations are used to calculate monthly densities, frequency of social foraging, and size and composition of social groups for all species. Additional data taken to quantify the foraging logistics of 22 species includes foraging substrate, time spent at a foraging station, and distance travelled between foraging stations. These data are used to generate indices of logistic similarity and interspecific association for species pairs in order to test the hypothesis that species which are similar in their foraging logistics are more likely to associate than those which are not. Causes of solitary behavior and variation in intraspecific social behavior are also examined. Exclusively solitary foraging behavior is strongly associated with species that use sparse, unpredictable prey too small to share. These species, referred to as "extensive foragers," appear to be constrained from both intraspecific and interspecific association by being logistic mismatches with all but their closest competitors, with which the potential for interference competition is high. Evidence is presented to refute the hypothesis that solitary behavior is due to low vulnerability to predators. Species which are intraspecifically solitary tend to use evenly distributed resources, and gregarious species use patchy and abundant resources. Exceptions are most frequent among permanent residents, which may continue to maintain social and spacing systems used in the breeding season. Among gregarious species, permanent residents are more likely to maintain stable group sizes than winter residents. A correlation exists between similarity of foraging logistics and likelihood of interspecific association, but it is subject to considerable variance. Causes of this variance include the tendency of transient migrants not to associate with other species, and the tendency of certain species to form temporary associations, regardless of logistic similarities. Why some species form temporary ("opportunistic") associations while others do not remains unclear.
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Geochemistry of the Laramide igneous suite of the Santa Rita and Empire Mountains, southeastern ArizonaTrapp, Richard A. January 1987 (has links)
No description available.
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The geology and ore deposits of a portion of the Tyndall Mining District, Santa Cruz County, ArizonaWalchessen, Anne Aurelia January 1983 (has links)
No description available.
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A Paleocene Paleomagnetic Pole from the Gringo Gulch Volcanics, Santa Cruz County, ArizonaBarnes, Arthur E. January 1980 (has links)
Paleomagnetic data from 25 sites (5 samples per site) in andesite flows of the Gringo Gulch Volcanics in Santa Cruz County, Arizona, were analyzed to determine a lower Paleocene paleomagnetic pole. Alternating-field demagnetization to 500 oe peak field was sufficient to erase secondary viscous components. The mean direction of magnetization (inclination = -58.8°, declination = 167.5 °) was obtained by averaging the site mean directions of the 25 sites, which are all reversed. The resultant lower Paleocene pole position is at lat. 77.0 °N, 1on. 201.0 °E (dp = 1.2 °, dm = 1.7 °).
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