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Dissertations / Theses on the topic 'Mountains – Arizona'

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Published: 4 June 2021

Last updated: 8 February 2022

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1

Warrick, Gregory David. "MOUNTAIN SHEEP FORAGING BEHAVIOR (ARIZONA)." Thesis, The University of Arizona, 1985. http://hdl.handle.net/10150/291298.

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2

Morgart, John R., Paul R. Krausman, William H. Brown, and Frank M. Whiting. "Chemical Analysis of Mountain Sheep Forage in the Virgin Mountains, Arizona." College of Agriculture, University of Arizona (Tucson, AZ), 1986. http://hdl.handle.net/10150/310778.

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3

Etchberger, Richard Carl 1957. "Mountain sheep habitat characteristics in the Pusch Ridge Wilderness, Arizona." Thesis, The University of Arizona, 1988. http://hdl.handle.net/10150/276839.

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Mountain sheep (Ovis canadensis mexicana) in the Pusch Ridge Wilderness (PRW), Santa Catalina Mountains, Arizona have abandoned historic habitat and now occupy 44 km². I used univariate analyses to quantify differences of physiographic and vegetational variables between abandoned habitat and habitat that is still used by mountain sheep. A discriminant function model characterized the magnitude of the differences between the 2 habitats. Habitat that supports mountain sheep has less human disturbance and is more open with more side oats grama (Bouteloua curtipendula), red brome (Bromus rubens),

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4

Avanesians, Patrick, Giancarlo A. Daroch, John Fleming, et al. "GEOPHYSICAL INVESTIGATION OF THE TUCSON MOUNTAINS." LASI Laboratory for Advanced Surface Imaging, The University of Arizona (Tucson, AZ), 2011. http://hdl.handle.net/10150/624628.

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Transient Electromagnetic (TEM), Controlled Source Audio Magnetotellurics (CSAMT), Gravity, and Magnetic data were collected in the Tucson Mountains during the Spring semester, 2011. The goal was to investigate the extent of a low-resistivity porous sedimentary layer and faults that may form potential traps located under the surface volcanic layers, as interpreted by Lipman 1993. The sedimentary layer under the volcanics has the potential to be used for either water resources or compressed air storage to store solar energy. The results from the TEM and CSAMT surveys broadly correlated with the

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5

Wallace, Mark Christopher. "Elk habitat use in the White Mountains, Arizona." Diss., The University of Arizona, 1991. http://hdl.handle.net/10150/185690.

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I identified the seasonal ranges and migration routes for Rocky mountain elk (Cervus elaphus nelsoni) that summered on the White Mountains Apache Reservation (reservation). I described elk distributions, movements, diets, and behaviors related to habitats in the White Mountains, Arizona from October 1983 to July 1986. I identified neonatal elk hiding habitats and how long they were used. Adult and neonatal elk were captured and radio collared. I determined movements and habitat use from direct observations of marked elk relocated by radio-telemetry. Yearly home ranges in this population were l

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6

Johnson, William Theodore. "Flora of the Pinaleno Mountains, Graham County, Arizona." University of Arizona (Tucson, AZ), 1988. http://hdl.handle.net/10150/609089.

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The Pinaleno Mountains lie between the San Simon and Sulphur Springs Valleys in southeastern Arizona. The Pinalenos are one of three mountain ranges in Graham County managed by the Coronado National Forest. Forest Service management of this range is currently at a crossroads. Either a strict preservation policy will prevail or the development of an astrophysical observatory will be allowed. The most notable features of the Pinalenos, the third highest range in Arizona, are the abundance of perennial streams and the significant elevational range of 2050 m (6,720 ft.) on the northeast slope. Rec

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7

Dueñez, Ricardo Luis 1954. "OAK FUELWOOD VOLUME ESTIMATION IN THE HUACHUCA MOUNTAINS OF ARIZONA (EMORY OAK)." Thesis, The University of Arizona, 1987. http://hdl.handle.net/10150/276409.

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8

Chon, Enrique, Matthew Gabriel, Sara Harders, et al. "Geophysical Surveys near Old Yuma Mine, Tucson Mountains, Arizona." LASI Laboratory for Advanced Surface Imaging, The University of Arizona (Tucson, AZ), 2016. http://hdl.handle.net/10150/624630.

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To assist the United States Geological Survey with an on-going groundwater study around Old Yuma Mine in Tucson, Arizona, the University of Arizona GEN/GEOS 416/516 Field Studies in Geophysics class conducted geophysical surveys along two transects near the mine. Transect 1 was situated across the mine site; Transect 2 was located to the northeast in a nearby residential area. The methods used were gravity, magnetics, transient electromagnetics (TEM) and inductive electromagnetics (Geonics EM-31, and Geonics EM-34). The goal was to use these data to investigate the subsurface density, magnetic

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9

Daniel, Thomas F., and Mary L. Butterwick. "Flora of the South Mountains of South-central Arizona." University of Arizona (Tucson, AZ), 1992. http://hdl.handle.net/10150/609143.

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10

Chen, Daqin 1958. "Geotechnical characterization of an alluvial fanglomerate." Thesis, The University of Arizona, 1988. http://hdl.handle.net/10150/276713.

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The Department of Energy (DOE) has recently announced that the Superconducting Super Collider (SSC) will soon be built somewhere in the United States. Preliminary geophysical studies indicate that the Sierrita site 35 miles southwest of Tucson has geological conditions that would facilitate construction of the SSC. The Maricopa site southwest of Phoenix is also one of the two potential sites in Arizona. However, several additional geotechnical investigations were required to convincingly demonstrate the suitability of these two locations. The present research program identified the geotechnica

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11

Fleming, John B., Husna D. Hafit, Khaliza B. Khalid, et al. "Controlled Source Audio Magnetotelluric (CSAMT) Surveys in the Tucson Mountains." LASI Laboratory for Advanced Surface Imaging, The University of Arizona (Tucson, AZ), 2012. http://hdl.handle.net/10150/624629.

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Controlled Source Audio-Magnetotellurics (CSAMT) surveys were conducted in 2012 in the Tucson Mountains as a continuation of the 2010 and 2011 Laboratory for Advanced Subsurface Imaging (LASI) field studies in this area. This geologic setting was chosen for its high-resistivity impermeable volcanic layer overlaying porous sedimentary layers. This type of structure has potential for water resources and as a reservoir for compressed air energy storage (CAES). The data from 2,500 meters of CSAMT survey lines generated 900 meter-deep resistivity versus elevation cross-sections and six plan maps of

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12

HAVERLAND, RAYMOND LOUIS. "SOIL DEVELOPMENT ON A GRANITIC CATENA IN SOUTHEASTERN ARIZONA (WEATHERING)." Diss., The University of Arizona, 1987. http://hdl.handle.net/10150/184144.

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Chemical input-output analyses were used to evaluate the rate of rock weathering and soil development on a granitic inselberg of the Dragoon Mountains in southeastern Arizona. Soil genesis relationships were investigated through field and laboratory study of the soil profile, parent rock, microclimate and vegetation, on different catena positions and hillside aspects. Precipitation and runoff water qualities were determined, with increased summer acidity. Precipitation volume was estimated by extrapolating data from a nearby recording station. Runoff volume was estimated by the U.S.D.A.-S.C.S.

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13

Meyer, John William 1958. "First year coppice regeneration of Quercus emoryi and Quercus arizonica in the Huachuca Mountains, Arizona." Thesis, The University of Arizona, 1988. http://hdl.handle.net/10150/276734.

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Emory oak (Quercus emoryi) and Arizona white oak (Q. arizonica), currently being harvested for fuelwood in encinals of southern Arizona, usually regenerate through stump sprouting. Adjacent to a Huachuca Mountains fuelwood cutting area, 3 replications of four thinning treatments (25%, 50%, 75%, and 100% intensity) were established in January, 1986. Regeneration was assessed one year later by examining the effects of thinning intensity, partial or complete stem cluster cutting, and tree characteristics. Clearcutting greatly increased the proportion of stumps that sprout for Emory oak and increa

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14

Morgart, John Raymond. "Desert bighorn sheep forage relationships in the Virgin Mountains, Arizona." Diss., The University of Arizona, 1990. http://hdl.handle.net/10150/185076.

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Twelve desert bighorn sheep (Ovis canadensis nelsoni) were captured 12-14 November 1979 in the Black Mountains, western Arizona, and translocated to a 283 ha enclosure in the Virgin Mountains, northwestern Arizona. I studied habitat and foraging relationships of the population from November 1979 to December 1981. My objectives were to investigate productivity, group characteristics and habitat use, intraspecific comparisons of diet, diet overlap with cattle, forage availability and use, diet diversity, and plant quality. Seven and 8 females in the enclosure had lambs in 1980 and 1981, respecti

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15

Rondeau, Renee Jane 1956. "Flora and vegetation of the Tucson Mountains, Pima County, Arizona." Thesis, The University of Arizona, 1991. http://hdl.handle.net/10150/277880.

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I compiled the first vascular flora of the Tucson Mountains of southeastern Arizona, part of the Arizona Upland subdivision of the Sonoran Desert. The study area consisted of over 40,000 hectares, with two principal biotic communities: desertscrub and desert-grassland. Over 300 km of trails, ridges, washes, canyons, and peaks were surveyed in a three year period, covering all elevations and habitats. This was supplemented by examination of herbarium records. The area is unusually rich compared to other regional floras in the state of Arizona, including a vascular flora of 605 specific and infr

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16

Field, John Jacob. "Surficial processes, channel change, and geological methods of flood-hazard assessment on fluvially dominated alluvial fans in Arizona." Diss., The University of Arizona, 1994. http://hdl.handle.net/10150/186649.

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A combination of geological and hydraulic techniques represents the most sensible approach to flood hazard analysis on alluvial fans. Hydraulic models efficiently yield predictions of flood depths and velocities, but the assumptions on which the models are based do not lead to accurate portrayals of natural fan processes. Geomorphological mapping, facies, mapping, and hydraulic reconstructions of past floods provide data on the location, types, and magnitude of flood hazards, respectively. Geological reconstructions of past floods should be compared with the results of hydraulic modeling befor

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17

Trapp, Richard A. "Geochemistry of the Laramide igneous suite of the Santa Rita and Empire Mountains, southeastern Arizona." Thesis, The University of Arizona, 1987. http://hdl.handle.net/10150/558080.

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18

Glynn, Mary Eileen 1960. "Geotechnical investigations of two potential sites for the proposed Arizona superconducting super collider." Thesis, The University of Arizona, 1987. http://hdl.handle.net/10150/276641.

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Two sites around the Maricopa and Sierrita Mountains respectively were investigated to provide supporting data for the State of Arizona proposal to the Department of Energy to construct a Superconducting Super Collider (SSC) facility. The main feature of the facility is a 53 mile racetrack shaped tunnel. The proposed Maricopa SSC tunnel passes through three main types of rock--approximately 35 miles of indurated fanglomerates, 10 miles of granodiorites and 8 miles of volcanic and sedimentary rocks. The proposed Sierrita SSC tunnel also passes through three main rock types--approximately 19 mil

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19

Grubensky, Michael J. "Structure, geochemistry, and volcanic history of mid-Tertiary rocks in the Kofa Region, southwestern Arizona." Thesis, The University of Arizona, 1987. http://hdl.handle.net/10150/558071.

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20

Schwartz, Kerry Lisa 1962, and Kerry Lisa 1962 Schwartz. "A geohydrologic investigation of volcanic rocks using the gravity survey method: Galiuro Mountains, Graham, Pinal and Cochise Counties, Arizona." Thesis, The University of Arizona, 1990. http://hdl.handle.net/10150/558129.

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21

Haile, Abdi Barre 1956. "Possible water pollution sources in Sabino Creek, Santa Catalina Mountains, Arizona." Thesis, The University of Arizona, 1987. http://hdl.handle.net/10150/191949.

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Sabino Canyon is an important source of recreation for the Tucson Area. Human activities near the creek have caused pollution problems. This was especially noticeable in the Summerhaven area, where during 1970's a malfunctioning sewage treatment plant was discharging into Sabino Creek. During 1982, a new treatment facility was constructed with zero discharge into the creek. In the Lower Sabin° Creek recreation area, no sampling has been done since then. Thus, this research was designed to assess the extent of stream's pollution and to identify possible water pollution sources and to investigat

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22

Allen, George B. "Economic Geology of the Big Horn Mountains of West-Central Arizona." Thesis, The University of Arizona, 1985. http://hdl.handle.net/10150/244099.

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The Big Horn Mountains are a geologically complex range that extends over 500 square km in west-central Arizona. Three major lithologic terranes outcrop: (1) Proterozoic amphibolite, phyllite, schists, gneiss, and granite; (2) Mesozoic monzonite to diorite intrusives; and (3) Cenozoic mafic to silicic volcanic rocks and clastic rocks. The entire area is in the upper plate of a detachment fault and, consequently, contains many low- to high-angle normal faults. Each lithologic terrane has its associated mineral occurrences. The Big Horn district is exclusively hosted in the pre- Tertiary terrane

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23

Gottfried, Gerald J., and Daniel G. Neary. "Hydrology of the Upper Parker Creek Watershed, Sierra Ancha Mountains, Arizona." Arizona-Nevada Academy of Science, 2002. http://hdl.handle.net/10150/296587.

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24

Christopherson, John Ostler 1956. "Effects of prescribed fire on fuel accumulation rates and selected soil nutrients." Thesis, The University of Arizona, 1989. http://hdl.handle.net/10150/277123.

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Fuel accumulation rate and total soil nitrogen, phosphorus, and sulfur following prescribed fires were studied. Three prescribed fires were conducted in S.E. Arizona ponderosa pine stands during the summers of 1979, 1980, and 1981. Samples of forest floor and larger diameter fuel and soil from the surface 1.5 inches and 1.5 to 3.0 inch layers were collected in the summer of 1981. Forest floor and total fuel accumulation averaged 5.4 to 6.7 and 6.3 to 8.9 tons/acre/year, respectively. Total nitrogen, phosphorus, and sulfur in the surface three inches of mineral soil were not significantly affec

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25

Young, David Paul. "The history of deformation and fluid phenomena in the top of the wilderness suite, Santa Catalina Mountains, Pima County, Arizona." Thesis, The University of Arizona, 1988. http://hdl.handle.net/10150/558089.

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26

Cunningham, William Dickson 1960. "Superposed thrusting in the northern Granite Wash Mountains, La Paz County, Arizona." Thesis, The University of Arizona, 1986. http://hdl.handle.net/10150/558059.

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27

Danzer, Shelley Rae 1951. "Fire history and stand structure in the Huachuca Mountains of Southeastern Arizona." Thesis, The University of Arizona, 1998. http://hdl.handle.net/10150/278665.

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Historically, wildfires in mixed conifer forests of Southwestern sky islands were frequent events. Dendrochronological methods were used to reconstruct fire regimes and stand age structures in the Huachuca Mountains of Southeastern Arizona. Pre-settlement (i.e., before ca. 1870) fire intervals ranged from 4 to 10 years, with many fires spreading over the entire sample area. Stand age distributions show an increase in more shade-tolerant tree species. Although ponderosa pine is still the dominant overstory tree species, recent recruitment is predominantly southwestern white pine and Douglas-fir

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28

Clements, Brooke Philip 1958. "Precious metal vein mineralization in the Bradshaw Mountains region, Yavapai County, Arizona." Thesis, The University of Arizona, 1991. http://hdl.handle.net/10150/558146.

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29

Krausman, Paul R., Leonard L. Ordway, Frank M. Whiting, and William H. Brown. "Nutritional Composition of Desert Mule Deer Forage in the Picacho Mountains, Arizona." University of Arizona (Tucson, AZ), 1990. http://hdl.handle.net/10150/609115.

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Nineteen forage species used by Desert Mule Deer (Odocoileus hemionus crooki) in the Picacho Mountains, Arizona were collected bimonthly in 1983 and analyzed for dry matter, protein fiber, lignin, ether extract, ash, cellulose, cell solubles, and hemicellulose. Results of the analyses are presented as a reference source for wildlife biologists, range managers, and others working with desert ecosystems.

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30

Seegmiller, Rick F., Paul R. Krausman, William H. Brown, and Frank M. Whiting. "Nutritional Composition of Desert Bighorn Sheep Forage in the Harquahala Mountains, Arizona." University of Arizona (Tucson, AZ), 1990. http://hdl.handle.net/10150/609139.

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Samples of 32 plant species (24 woody and succulent species, 5 grasses, 3 forbs) used by Desert Bighorn Sheep (Ovis canadensis mexicana) in the Harquahala Mountains, Arizona were collected bimonthly in 1982. All samples were analyzed for dry matter, protein, acid detergent fiber, neutral detergent fiber, lignin, cellulose, cell solubles, hemicellulose, ether extract, and ash. Woody and succulent plants had the highest protein levels (x̄ = 9.3% in September and October to 11.1% in January and February) followed by forbs and grass, respectively. Nutritional data are presented in tabular form as

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31

Riggs, Nancy Rosalind 1956. "Stratigraphy, structure, and mineralization of the Pajarito Mountains, Santa Cruz County, Arizona." Thesis, The University of Arizona, 1985. http://hdl.handle.net/10150/558036.

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32

Horton, Scott Patterson 1951. "Effects of prescribed burning on breeding birds in a ponderosa pine forest, southeastern Arizona." Thesis, The University of Arizona, 1987. http://hdl.handle.net/10150/276570.

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A moderately intense, broadcast, understory, prescribed burn in 3 previously unburned ponderosa pine stands in southeastern Arizona felled or consumed 50% of all ponderosa pine snags ≥ 15 cm dbh. Large moderately decayed snags were most susceptible to burning. Large snags in the early stages of decay were preferred as nest sites by cavity-nesting birds. Numbers of live woody plants were reduced by 40%, mortality was greatest among shrubs and small trees. Canopy volume was reduced by 19%, the greatest impact was below 5 m. No species of cavity-nesting birds, or birds that associated with unders

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33

Gottfried, Gerald J., Peter F. Ffolliott, Daniel G. Neary, and John H. Yazzie. "Precipitation Patters on the Cascabel Watersheds, Peloncillo Mountains, New Mexico." Arizona-Nevada Academy of Science, 2011. http://hdl.handle.net/10150/296991.

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34

Zauderer, Jeffrey. "Riparian Habitats of the Southeast Sierrita Mountains: Vanished Perennial Habitats." Arizona-Nevada Academy of Science, 1989. http://hdl.handle.net/10150/296427.

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From the Proceedings of the 1989 Meetings of the Arizona Section - American Water Resources Association and the Hydrology Section - Arizona-Nevada Academy of Science - April 15, 1989, University of Nevada, Las Vegas, Nevada

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35

Duncan, John Towner 1960. "The geology and mineralization of the Northern Plomosa District, La Paz County, Arizona." Thesis, The University of Arizona, 1990. http://hdl.handle.net/10150/558125.

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36

Hall, Dwight Lyman 1953. "Stratigraphy and sedimentary petrology of the Mesozoic rocks of the Waterman Mountains, Pima County, Arizona." Thesis, The University of Arizona, 1985. http://hdl.handle.net/10150/558034.

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37

Davis, James Paulin Tilton 1954. "Hydrological considerations in locating the proposed Superconducting Supercollider in the Sierrita Mountains, Arizona." Thesis, The University of Arizona, 1989. http://hdl.handle.net/10150/277074.

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The Sierrita Mountains were investigated as a site for the proposed Superconducting Supercollider, which was to be housed in a ring-shaped tunnel more than 80 km (50 miles) in circumference. Geostatistical techniques including kriging were used to interpolate the potentiometric surface of the ground water and quantify its uncertainty along the proposed ring alignment to assess potential dewatering problems, based on the sparse water-level information available. Potential water supplies for the Superconducting Supercollider complex include local and imported good-quality ground water, poorer qu

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38

Carpenter, Michael C. "Earth-fissure movements associated with fluctuations in ground-water levels near the Picacho mountains, south-central Arizona, 1980-84." Diss., The University of Arizona, 1993. http://etd.library.arizona.edu/etd/GetFileServlet?file=file:///data1/pdf/etd/azu_e9791_1990_411_sip1_w.pdf&type=application/pdf.

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39

Beatty, Barbara. "Correlation of Some Mid-Mesozoic Redbeds and Quartz Sandstones in the Santa Rita Mountains, Mustang Mountains, and Canelo Hills, Southeastern Arizona." Thesis, The University of Arizona, 1987. http://hdl.handle.net/10150/249291.

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Mid-Mesozoic redbeds in the Santa Rita Mountains, Mustang Mountains, and Canelo Hills are lithologically and petrographically correlative. Quartz sandstone overlying the redbeds in the Mustang Mountains and Canelo Hills is also lithologically and petrographically correlative. The sediments were deposited during one or more breaks in volcanism associated with a continental magmatic arc that was active in southern Arizona during Triassic (?) and Jurassic time. The exact timing of sedimentation cannot be determined without more accurate dating of volcanics associated with the redbed strata. Redbe

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40

Yeats, Kenneth James, and Kenneth James Yeats. "Geology and structure of the northern Dome Rock Mountains, La Paz County, Arizona." Thesis, The University of Arizona, 1985. http://hdl.handle.net/10150/558016.

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41

Fox, Kevin Bryant 1964. "Fawning habitat of desert mule deer in the Belmont and Bighorn mountains, Arizona." Thesis, The University of Arizona, 1992. http://hdl.handle.net/10150/278208.

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I monitored female desert mule deer (Odocoileus hemionus crooki) (n = 7) with radio telemetry in the Belmont and Bighorn mountains, Arizona, 1991. I examined habitat use, size of seasonal ranges, predation by coyotes, and behavior, and I identified fawning and fawn rearing habitat. Female desert mule deer preferred the montane vegetation associations and avoided creosote flats (Larrea tridentata) during fawning. Size of seasonal ranges were smaller in the 2 weeks postpartum (X = 3.75 km2 than in the 2 weeks prior to fawning (X = 6.71 km2 Activity during the first or last 4 hours of daylight di

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42

Reis, Jonathan Hunter. "Jurassic and Cretaceous tectonic evolution of the southeast Castle Dome Mountains, southwest Arizona." [Ames, Iowa : Iowa State University], 2009.

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43

Janecke, Susanne Ursula 1959. "Structural geology and tectonic history of the Geesaman Wash area, Santa Catalina Mountains, Arizona." Thesis, The University of Arizona, 1986. http://hdl.handle.net/10150/558061.

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44

Khanchoul, Kamel 1959. "THE RELATIONSHIP BETWEEN LITHOLOGY AND SLOPE FORM IN THE TUCSON MOUNTAINS, PIMA COUNTY, ARIZONA." Thesis, The University of Arizona, 1987. http://hdl.handle.net/10150/276500.

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The relationship between lithology and slope morphology is investigated at eight sites on granitic, andesitic, and sedimentary rock slopes in the Tucson Mountains. Several methods are used in the study. Topographic profiles are constructed. Skewness indices of the slope shapes, maximum and minimum slope angles, and slope lengths of the different slope profiles are computed and compared with each other. Debris size analysis is done to better determine hillfront/piedmont junctions. Slope surface regularities of the three lithological slopes are analysed and compared. The results show that the gr

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45

Neary, Daniel G., and Gerald J. Gottfried. "Geomorphology of Small Watersheds in an Oak Encinal in the Peloncillo Mountains." Arizona-Nevada Academy of Science, 2004. http://hdl.handle.net/10150/296608.

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46

Hauck, Wayne Russell. "Correlation and geochemical zonation of the mid-Tertiary volcanic and intrusive rocks in the Santa Teresa and northern Galiuro Mountains, Arizona." Thesis, The University of Arizona, 1985. http://hdl.handle.net/10150/558033.

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47

Rusden, Sally Anne 1954. "Management of the community economic base as a strategy for economic development." Thesis, The University of Arizona, 1988. http://hdl.handle.net/10150/276924.

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Application of economic base analysis at a multi-level scale illustrates the usefulness of this approach to tracking and measuring the economic flows and linkages between three defined areas. A census survey of employers in six rural communities of the White Mountain Region of Arizona is used to collect employment and sales data at a high level of specificity. These data serve as the basis for bifurcation of basic and nonbasic components necessary for estimating the multiplier. Measurement of these data determine the extent of economic dependence and spatial interaction which exist between com

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48

Zanga, Ambroise 1956. "Sampling efficiency evaluation in Emory oak woodlands of southeastern Arizona." Thesis, The University of Arizona, 1989. http://hdl.handle.net/10150/291343.

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A forest inventory was made by a two-man team in the Emory oak (Quercus emoryi) woodlands, near the Huachuca Mountains, in southeastern Arizona. Two plot sizes, 1/10th, and 1/25th hectare, and three basal area factors, 2, 4 and 6 (square meters per hectare) were used. Tree tally time was recorded, but the travelling time between plots was not recorded. Total number of trees, total basal area, and total volume of trees per hectare were measured, summarized, and analyzed. Significant differences were noted between plot sampling and point sampling. Results suggested that with plot sampling, 1/25t

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49

Mark, Roger Alan. "Structural and sedimentary geology of the area north of Hot Springs Canyon, southern Galiuro Mountains, Cochise County, Arizona." Thesis, The University of Arizona, 1985. http://hdl.handle.net/10150/558025.

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50

Goodlin, Thomas Charles. "Stratigraphic and structural relations of the area south of Hot Springs Canyon, Galiuro Mountains, Arizona." Thesis, The University of Arizona, 1985. http://hdl.handle.net/10150/558023.

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