Relevant bibliographies by topics / San Juan County (Utah)

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Academic literature on the topic 'San Juan County (Utah)'

Author: Grafiati
Published: 4 June 2021
Last updated: 3 March 2023

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Journal articles on the topic "San Juan County (Utah)"

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Haynes, Patrick E. "Mineralogy of the Jomac Mine San Juan County, Utah." Rocks & Minerals 75, no. 4 (July 2000): 240–48. http://dx.doi.org/10.1080/00357520009605651.

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Smith, Jordan W., Emily J. Wilkins, and Anna B. Miller. "Bears Ears National Monument and Outdoor Recreation in San Juan County, Utah." Society & Natural Resources 34, no. 7 (April 9, 2021): 966–79. http://dx.doi.org/10.1080/08941920.2021.1907867.

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Kampf, Anthony R., Travis A. Olds, Jakub Plášil, Joe Marty, and Samuel N. Perry. "Feynmanite, a new sodium uranyl sulfate mineral from Red Canyon, San Juan County, Utah, USA." Mineralogical Magazine 83, no. 02 (May 28, 2018): 153–60. http://dx.doi.org/10.1180/mgm.2018.117.

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AbstractThe new mineral feynmanite, Na(UO2)(SO4)(OH)·3.5H2O, was found in both the Blue Lizard and Markey mines, San Juan County, Utah, USA, where it occurs as a secondary phase on pyrite-rich asphaltum in association with chinleite-(Y), gypsum, goethite, natrojarosite, natrozippeite, plášilite, shumwayite (Blue Lizard) and wetherillite (Markey). The mineral is pale greenish yellow with a white streak and fluoresces bright greenish white under a 405 nm laser. Crystals are transparent with a vitreous lustre. It is brittle, with a Mohs hardness of ~2, irregular fracture and one perfect cleavage on {010}. The calculated density is 3.324 g cm–3. Crystals are thin needles or blades, flattened on {010} and elongate on [100], exhibiting the forms {010}, {001}, {101} and {10$\bar{1}$}, and are up to ~0.1 mm in length. Feynmanite is optically biaxial (–), with α = 1.534(2), β = 1.561(2) and γ = 1.571(2) (white light); 2Vmeas.= 62(2)°; no dispersion; and optical orientation:X=b,Y≈a,Z≈c. It is weakly pleochroic:X= colourless,Y= very pale green yellow andZ= pale green yellow (X<Y<Z). Electron microprobe analyses (WDS mode) provided (Na0.84Fe0.01)(U1.01O2)(S1.01O4)(OH)·3.5H2O. The five strongest powder X-ray diffraction lines are [dobsÅ(I)(hkl)]: 8.37(100)(010), 6.37(33)($\bar{1}$01,101), 5.07(27)($\bar{1}$11,111), 4.053(46)(004,021) and 3.578(34)(120). Feynmanite is monoclinic, has space groupP2/n,a= 6.927(3),b= 8.355(4),c= 16.210(7) Å, β = 90.543(4)°,V= 938.1(7) Å3andZ= 4. The structure of feynmanite (R1= 0.0371 for 1879Io> 2σI) contains edge-sharing pairs of pentagonal bipyramids that are linked by sharing corners with SO4groups, yielding a [(UO2)2(SO4)2(OH)2]2–sheet based on the phosphuranylite anion topology. The sheet is topologically identical to those in deliensite, johannite and plášilite. The dehydration of feynmanite to plášilite results in interlayer collapse involving geometric reconfiguration of the sheets and the ordering of Na.
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Chukanov, Nikita V., Dmitry Y. u. Pushcharovsky, Marco Pasero, Stefano Merlino, Anna V. Barinova, Steffen Mö ckel, Igor V. Pekov, Aleksandr E. Zadov, and Viktor T. Dubinchuk. "Larisaite, Na(H3O)(UO2)3(SeO3)2O2 4H2O, a new uranyl selenite mineral from Repete mine, San Juan County, Utah, U.S.A." European Journal of Mineralogy 16, no. 2 (March 29, 2004): 367–74. http://dx.doi.org/10.1127/0935-1221/2004/0016-0367.

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Davis, Thomas L., and Geoffrey M. Jackson. "Seismic stratigraphy study of algal mound reservoirs, Patterson and Nancy fields, Paradox basin, San Juan County, Utah." GEOPHYSICS 53, no. 7 (July 1988): 875–80. http://dx.doi.org/10.1190/1.1442524.

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Seismic data from the Paradox basin, southeast Utah, exhibit amplitude anomalies associated with the presence of Pennsylvanian algal mound reservoirs. An experimental line over the Patterson and Nancy fields shows amplitude reductions corresponding to reservoir mound facies. Amplitude reduction is due to the lateral facies change from intermound evaporite‐dominated facies to the carbonate algal mound facies. Porosity in the mound facies accentuates the amplitude reduction but the influence of porosity is minor compared to the effect of the lateral lithologic change. Recurrent movement on basement faults during the Pennsylvanian may have controlled the location of these mounds.
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Kampf, Anthony R., Jakub Plášil, Travis A. Olds, Barbara P. Nash, and Joe Marty. "Uranoclite, a new uranyl chloride mineral from the Blue Lizard mine, San Juan County, Utah, USA." Mineralogical Magazine 85, no. 3 (March 31, 2020): 438–43. http://dx.doi.org/10.1180/mgm.2021.33.

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AbstractThe new mineral uranoclite (IMA2020-074), (UO2)2(OH)2Cl2(H2O)4, was found in the Blue Lizard mine, San Juan County, Utah, USA, where it occurs as tightly intergrown aggregates of irregular yellow crystals in a secondary assemblage with gypsum. The streak is very pale yellow and the fluorescence is bright green–white under 405 nm ultraviolet light. Crystals are translucent with vitreous lustre. The tenacity is brittle, the Mohs hardness is ~1½, the fracture is irregular. The mineral is soluble in H2O and has a calculated density of 4.038 g⋅cm–3. Electron microprobe analyses provided (UO2)2(OH)2.19Cl1.81(H2O)4. The six strongest powder X-ray diffraction lines are [dobs Å(I)(hkl)]: 8.85(38)(002), 5.340(100)(200, 110), 5.051(63)($\bar{2}$02), 4.421(83)(112, 004, 202), 3.781(38)($\bar{2}$12) and 3.586(57)(014, $\bar{2}$04). Uranoclite is monoclinic, P21/n, a = 10.763(8), b = 6.156(8), c = 17.798(8) Å, β = 95.656(15)°, V = 1173.5(18) Å3 and Z = 4. The structure is the same as that of synthetic (UO2)2(OH)2Cl2(H2O)4 in which the structural unit is a dimer consisting of two pentagonal bipyramids that share an equatorial OH–OH edge. The dimers are linked to one another only by hydrogen bonding. This is the second known uranyl mineral containing essential Cl and the first in which Cl coordinates to U6+.
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Kampf, Anthony R., Travis A. Olds, Jakub Plášil, Peter C. Burns, Radek Škoda, and Joe Marty. "Paramarkeyite, a new calcium–uranyl–carbonate mineral from the Markey mine, San Juan County, Utah, USA." Mineralogical Magazine 86, no. 1 (December 13, 2021): 27–36. http://dx.doi.org/10.1180/mgm.2021.100.

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AbstractThe new mineral paramarkeyite (IMA2021-024), Ca2(UO2)(CO3)3⋅5H2O, was found in the Markey mine, San Juan County, Utah, USA, where it occurs as a secondary phase on gypsum-coated asphaltum in association with andersonite, calcite, gypsum and natromarkeyite. Paramarkeyite crystals are transparent, pale green-yellow, striated tablets, up to 0.11 mm across. The mineral has white streak and vitreous lustre. It exhibits moderate bluish-white fluorescence (405 nm laser). It is very brittle with irregular, curved fracture and a Mohs hardness of 2½. It has an excellent {100} cleavage and probably two good cleavages on {010} and {001}. The measured density is 2.91(2) g cm–3. Optically, the mineral is biaxial (–) with α = 1.550(2), β = 1.556(2), γ = 1.558(2) (white light); 2V = 60(2)°; strong r > v dispersion; orientation: Y = b; nonpleochroic. The Raman spectrum exhibits bands consistent with UO22+, CO32– and O–H. Electron microprobe analysis provided the empirical formula (Ca1.83Na0.20Sr0.03)Σ2.05(UO2)(CO3)3⋅5H2O (+0.07 H). Paramarkeyite is monoclinic, P21/n, a = 17.9507(7), b = 18.1030(8), c = 18.3688(13) Å, β = 108.029(8)°, V = 5676.1(6) Å3 and Z = 16. The structure of paramarkeyite (R1 = 0.0647 for 6657 I > 2σI) contains uranyl tricarbonate clusters that are linked by Ca–O polyhedra to form heteropolyhedral layers. The structure of paramarkeyite is very similar to those of markeyite, natromarkeyite and pseudomarkeyite.
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Kampf, Anthony R., Jakub Plášil, Anatoly V. Kasatkin, Joe Marty, and Jiří Čejka. "Markeyite, a new calcium uranyl carbonate mineral from the Markey mine, San Juan County, Utah, USA." Mineralogical Magazine 82, no. 5 (May 21, 2018): 1089–100. http://dx.doi.org/10.1180/minmag.2017.081.085.

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ABSTRACTThe new mineral markeyite (IMA2016-090), Ca9(UO2)4(CO3)13·28H2O, was found in the Markey mine, San Juan County, Utah, USA, where it occurs as a secondary phase on asphaltum in association with calcite, gypsum and natrozippeite. The mineral is pale yellowish-green with white streak and fluoresces bright bluish white under a 405 nm laser. Crystals are transparent and have vitreous to pearly lustre. It is brittle, with Mohs hardness 1½ to 2, irregular fracture and three cleavages: perfect on {001}; good on {100} and {010}. The measured density is 2.68 g cm–3. Crystals are blades, flattened on {001} and elongate on [010], exhibiting the forms {100}, {010}, {001}, {110}, {101}, {011} and {111}. Markeyite is optically biaxial (–) with α = 1.538(2), β = 1.542(2) and γ = 1.545(2) (white light); the measured 2V is 81(2)°; the dispersion isr<v(weak); the optical orientation isX=c,Y=b,Z=a; and pleochroism isX= light greenish yellow,YandZ= light yellow (X>Y≈Z). Electron microprobe analyses (energy-dispersive spectroscopy mode) yielded CaO 18.60, UO342.90, CO221.30 (calc.) and H2O 18.78 (calc.), total 101.58 wt.% and the empirical formula Ca8.91(U1.01O2)4(CO3)13·28H2O. The six strongest powder X-ray diffraction lines are [dobsÅ(I)(hkl)]: 10.12(69)(001), 6.41(91)(220,121), 5.43(100)(221), 5.07(33)(301,002,131), 4.104(37)(401,141) and 3.984(34)(222). Markeyite is orthorhombic,Pmmn,a= 17.9688(13),b= 18.4705(6),c= 10.1136(4) Å,V= 3356.6(3) Å3andZ= 2. The structure of markeyite (R1= 0.0435 for 3427Fo> 4σF) contains uranyl tricarbonate clusters (UTC) that are linked by Ca–O polyhedra forming thick corrugated heteropolyhedral layers. Included within the layers is an additional disordered CO3group linking the Ca–O polyhedra. The layers are linked to one another and to interlayer H2O groups only via hydrogen bonds. The structure bears some similarities to that of liebigite.
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Kampf, Anthony R., Jakub Plášil, Travis A. Olds, Barbara P. Nash, and Joe Marty. "Ammoniozippeite, a New Uranyl Sulfate Mineral from the Blue Lizard Mine, San Juan County, Utah, and the Burro Mine, San Miguel County, Colorado, USA." Canadian Mineralogist 56, no. 3 (May 30, 2018): 235–45. http://dx.doi.org/10.3749/canmin.1800002.

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Olds, Travis A., Luke R. Sadergaski, Jakub Plášil, Anthony R. Kampf, Peter C. Burns, Ian M. Steele, Joe Marty, Shawn M. Carlson, and Owen P. Mills. "Leószilárdite, the first Na,Mg-containing uranyl carbonate from the Markey Mine, San Juan County, Utah, USA." Mineralogical Magazine 81, no. 5 (October 2017): 1039–50. http://dx.doi.org/10.1180/minmag.2016.080.149.

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AbstractLeószilárdite (IMA2015-128), Na6Mg(UO2)2(CO3)6·6H2O, was found in the Markey Mine, Red Canyon, White Canyon District, San Juan County, Utah, USA, in areas with abundant andersonite, natrozippeite, gypsum, anhydrite, and probable hydromagnesite along with other secondary uranium minerals bayleyite, čejkaite and johannite. The new mineral occurs as aggregates of pale yellow bladed crystals flattened on ﹛001﹜ and elongated along [010], individually reaching up to 0.2 mmlong. More commonly it occurs as pale yellow pearlescent masses to 2 mm consisting of very small plates. Leószilárdite fluoresces green under both longwave and shortwave ultraviolet light, and is translucent with a white streak, hardness of 2 (Mohs), and brittle tenacity with uneven fracture. The new mineral is readily soluble in room temperature H2O. Crystals have perfect cleavage along ﹛001﹜, and exhibit the forms ﹛110﹜,﹛001﹜,﹛100﹜,﹛101﹜ and ﹛101﹜. Optically, leószilárdite is biaxial (-), α= 1.504(1), β= 1.597(1), γ= 1.628(1) (white light); 2V (meas.) = 57(1)°, 2V (calc.) = 57.1°; dispersion r > v, slight. Pleochroism: X= colourless, Y and Z= light yellow; X<Y ≈ Z The average of six wavelength dispersive spectroscopic analyses provided Na2O 14.54, MgO 3.05, UO3 47.95, CO2 22.13, H2O 9.51, total 97.18 wt.%. The empirical formula is Na5.60Mg0.90U2O28C6H12.60, based on 28 O apfu. Leószilárdite is monoclinic, C2/m, a = 11.6093(21), b = 6.7843(13), c = 15.1058(28) Å, β = 91.378(3)°, V= 1189.4(4) Å3 and Z = 2. The crystal structure (R1 = 0.0387 for 1394 reflections with Iobs > 4σI), consists of uranyl tricarbonate anion clusters [(UO2)(CO3)3]4- held together in part by irregular chains of NaO5(H2O) polyhedra sub parallel to [010]. Individual uranyl tricarbonate clusters are also linked together by three-octahedron units consisting of two Na-centred octahedra that share the opposite faces of a Mg-centred octahedron at the centre (Na–Mg–Na), and have the composition Na2MgO12(H2O)4. The name of the new mineral honours the Hungarian-American physicist, inventor and biologist Dr. Leó Szilárd (1898–1964).
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Dissertations / Theses on the topic "San Juan County (Utah)"

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Haney, Michael J. "Ungulate Damage to Safflower in San Juan County, Utah." DigitalCommons@USU, 2011. https://digitalcommons.usu.edu/etd/1037.

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In Utah, farmers are concerned that ungulates are damaging safflower (Carthamus tinctorius) fields. I examined elk (Cervus elaphus) and mule deer (Odocoileus hemionus) damage to safflower production in San Juan County, Utah during 2009 and 2010. Data on damaged safflower plants were collected within 28 fields, totaling 1,581 ha (13 fields totaling 963 ha during 2009; 15 fields totaling 618 ha during 2010). I compared 3 methods to assess losses: ungulate-proof exclosures, adjacent plant compensation method, and counting the number of damaged plants in 50-m transects (safflower count method). Exclosures were of limited use because they could not be erected until farmers stopped using cultivating their fields. Hence, this method did not account for ungulate damage to young plants. The adjacent plant compensation method assessed yields within 1 m of a randomly-selected damaged plant to account for any compensatory growth of neighboring plants but this method proved inaccurate because ungulate herbivory was concentrated so that a browsed plant was often surrounded by other browsed plants so no compensatory growth by surrounding plants occurred. The most accurate method was the safflower count method which determined the number of damaged plants within a field and then multiplied this number by the decrease in yield from an average damaged plant. I used this method to examine 981,000 plants for damage. Deer and elk damaged or killed 7.2% of safflower plants during 2009 and 1.4% of plants during 2010. Overall yield reduction was 2.9% during 2009 and 0.6% in 2010. The total value of safflower loss within all surveyed fields in 2009 was $9,023 for a loss of $9.42 / ha. The loss of value within surveyed fields in 2010 was $2,330, or $3.77 / ha. The best model for predicting ungulate damage in 2009 included distance to canyon from field edge and the percent of a field bordered by a fallow field, while the best model for 2010 included distance to canyon from field edge and the percent of a field bordered by a wheat field. Safflower farmers were surveyed in the spring of 2010 to compare perceived losses in their fields during 2009 to those measured in this study. Farmers believed that damage by deer and elk reduced their yields by 20% with most damage caused by elk (x¯ =12% by elk, 7% by deer, 1% by other wildlife). On average, perceptions of damage were 5.2 times higher than the actual levels I measured during 2009. This was not surprising because farmers usually surveyed their field from the field’s edge and ungulate damage was concentrated along the edge of the fields.
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Banis, David. "The Wilderness Problem: A Narrative of Contested Landscapes in San Juan County, Utah." PDXScholar, 2004. https://pdxscholar.library.pdx.edu/open_access_etds/1972.

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Wilderness preservation has been at the center of debates about public land policy for almost half a century, and nowhere has the controversy been more intractable than in Utah. Despite its vast expanses of unsetded and undeveloped red rock desert, managed primarily by the Bureau of Land Management (BLM), Utah has less designated wilderness than in any other state in the West. In this study, I focus on San Juan County in southeast Utah to study the conflict over the designation of wilderness. The controversy pits local residents and state politicians against state and national environmental groups, with the BLM shifting positions in between. I analyze and interpret the wilderness debate from three different perspectives. The fIrst explores the history of the Utah wilderness debate from the first BLM wilderness inventory in the 1970's through its re-inventory in the 1990's. I examine the influence of national, regional, and local forces such as institutional change within the BLM, in-fIghting among Utah-based environmental interest groups, and the sagebrush rebellion and county supremacy movements. The second perspective incorporates the spatial analytical techniques of geographical information systems to provide a relatively objective view of landscape characteristics used to defIne wilderness. I interpret the landscape as a continuum of varying degrees of wildness, a product of inherent naturalness and the influences of human impacts. Lastly, I examine the personal views of the meaning of wilderness through the words of actual participants in the debate. In an analysis of the statements of both county residents as well as the Southern Utah Wilderness Alliance, I explore the mental images and ideas that influence the ways in which people value and understand the desert environment.
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Prather, Phoebe R. "Factors Affecting Gunnison Sage-Grouse (Centrocercus minimus) Conservation in San Juan County, Utah." DigitalCommons@USU, 2010. https://digitalcommons.usu.edu/etd/827.

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Due to loss of habitat, Gunnison sage-grouse (Centrocercus minimus) currently occupy 8.5% of their presumed historical range. One population survives in Utah, occurring in San Juan County. The Gunnison Sage-grouse Rangewide Conservation Plan and the San Juan County Gunnison Sage-grouse Conservation Plan recommended management strategies to address identified conservation threats to the Utah population. I addressed three conservation strategies identified in the plans: 1) creation and enhancement of brood-rearing areas; 2) assessment of habitat conditions within the Gunnison Sage-grouse Conservation Area; and 3) prevention or reduction of perching events by avian predators on distribution line power poles. From 2007-2009, I addressed the conservation strategy of creating mesic brood-rearing areas in Conservation Reserve Program fields and native sagebrush areas by evaluating the role of irrigation and dormant season cattle grazing on habitat. Vegetation and arthropod diversity in irrigated versus non-irrigated plots did not differ (p>0.01). Conservation Reserve Program plots exhibited greater arthropod abundance and cover of perennial grass than the native sagebrush plots, but lower diversity of perennial grasses and abundance and diversity of forbs (p<0.01). The second conservation strategy I addressed was the completion of an assessment of habitat conditions within the Gunnison Sage-grouse Conservation Area. I measured vegetation conditions within habitat occupied and unoccupied by Gunnison sage-grouse. Cover and height of grasses exceeded guidelines for occupied and unoccupied habitats. Forb cover was below recommended guidelines in occupied habitat. Sagebrush cover was below guidelines for winter habitat. Habitat restoration efforts should focus on retaining existing sagebrush cover and establishment of sagebrush, forb, and grass cover within Conservation Reserve Program fields. The third conservation strategy I evaluated was the retrofitting of distribution line power poles with perch deterrents to discourage avian predators from perching. I evaluated the efficacy of five perch deterrents. The perch deterrents did not mitigate potential avian predators from perching. A deterrent designed for insulators, in combination with physical deterrents we tested, has potential to prevent perching. These studies provided a sound first step that can be built upon by the Monticello/Dove Creek Local Working Group to improve habitat conditions, reduce the threat of avian predation, and plan future conservation activities within the Conservation Area.
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Sureda, Maite 1966. "Small mammal abundance within Mexican spotted owl home ranges in the Manti-LaSal National Forest, San Juan County, Utah." Thesis, The University of Arizona, 1996. http://hdl.handle.net/10150/278552.

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Ecologists suspect that owls select specific areas based on prey availability. My objective was to determine and compare distributions and abundances of Mexican spotted owl prey species' within different vegetation types in the canyons and mesas of the Manti-LaSal National Forest in Utah. I conducted live-trapping during summer and fall, 1994-95. Woodrat species (Neotoma spp.) are the Mexican spotted owls primary prey species as determined by percent biomass. Peromyscus spp. are also important in terms of frequency. Woodrats were only captured in the canyons and were primarily captured within the pinyon (Pinus spp.) - juniper (Juniperus spp.) vegetation type. The Mexican spotted owls in southeastern Utah spend >75% of their time within the canyons and forage within pinyon-juniper stands in the canyons. Maintaining the present state of pinyon-juniper stands within the canyons may benefit Mexican spotted owl populations in the Manti-LaSal National Forest.
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Mandurino, Sally Timmins. "The impact of the physical and cultural geography of southeastern Utah on Latter-day settlement." Diss., CLICK HERE for online access, 1998. http://patriot.lib.byu.edu/u?/MTGM,33227.

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Orchard, Kenneth Lynn. "Paleoflood hydrology of the San Juan River, southeastern Utah, USA." Thesis, The University of Arizona, 2001. http://etd.library.arizona.edu/etd/GetFileServlet?file=file:///data1/pdf/etd/azu_etd_hy0025_m_sip1_w.pdf&type=application/pdf.

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Raby, Kim Scarlet. "Use of water quality data for land management decisions: A case study in San Juan County, Colorado." Diss., Connect to online resource, 2005. http://wwwlib.umi.com/cr/colorado/fullcit?p1427772.

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Bergolc, Melanie L. "The Coleopteran Fauna of Sultan Creek-Molas Lake Area with Special Emphasis on Carabidae and how the Geological Bedrock Influences Biodiversity and Community Structure in the San Juan Mountains, San Juan County, Colorado." Bowling Green State University / OhioLINK, 2009. http://rave.ohiolink.edu/etdc/view?acc_num=bgsu1245610254.

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Eckersley, Jaclyn Marie. "The Beef Basin Occupation as an Extension of the Northern San Region: An In-Depth Analysis of the Ceramics in Beef Basin, Utah." BYU ScholarsArchive, 2018. https://scholarsarchive.byu.edu/etd/7061.

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This paper is a summary of the methods and key results of my analysis of 7,997 sherds from 14 sites in Beef Basin, Utah. I discuss physical attributes of the collection, the results of mean ceramic dating, the results of neutron activation analysis, and the results of refiring a sample of nips in an oxidizing atmosphere. I briefly summarize the architecture at each site , as well as possible Fremont cultural material found in and near Beef Basin. I conclude that Beef Basin was likely occupied in the early Pueblo III period and that the occupation was sudden and brief. I determined that paste color can be used as a general indicator of clay procurement locale north of the Abajo Mountains, just as it is in the Comb Ridge vicinity (Glowacki et al. 2015), that there was ceramic production in Beef Basin using local materials, and that the people of Beef Basin had similar connections as, or connections with the east of the Comb Ridge area, as evinced by similar sources for light-paste ceramics found in both areas.
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Gournay, Jonas Paul. "Phylloid algal bioherms and ooid grainstones : characterization of reservoir facies utilizing subsurface data from the Aneth Platform and outcrop data along the San Juan River, Paradox Basin, southeastern Utah /." Digital version accessible at:, 1999. http://wwwlib.umi.com/cr/utexas/main.

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Books on the topic "San Juan County (Utah)"

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San Juan County Historical Society (Utah), ed. Early San Juan County. Charleston, S.C: Arcadia Pub., 2008.

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Tate, LaVerne. Early San Juan County. Charleston, S.C: Arcadia Pub., 2008.

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Avery, Charles. Bedrock aquifers of eastern San Juan County, Utah. Salt Lake City, Utah: U.S. Dept. of the Interior, Geological Survey, 1985.

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United States. Soil Conservation Service., United States. Bureau of Land Management., and Utah Agricultural Experiment Station, eds. Soil survey of San Juan County, Utah, central part. [Washington, D.C.?]: The Service, 1993.

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Weir, Gordon Whitney. Geologic map of the Hatch Rock quadrangle, San Juan County, Utah. Reston, VA: U.S. Geological Survey, 1994.

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Rosalie, Goldman, ed. My Canyonlands. [Moab, Utah]: Canyon Country Publications, 1997.

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Turk, Toni Richard. Rooted in San Juan: A genealogical study of burials in San Juan County, Utah, 1879-1995. [Blanding, Utah]: T.R. Turk, 1995.

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D, Agenbroad Larry, ed. Anasazi subsistence and settlement on White Mesa, San Juan County, Utah. Lanham, Md: University Press of America, 1985.

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Shumway, Helen Nielson. The first forty years: A history of San Juan High School, 1914-1955. [Blanding, Utah?]: C. Harvey, 1994.

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1929-, Poole F. G., ed. Mineral resources of the Mancos Mesa Wilderness Study Area, San Juan County, Utah. [Washington, D.C.]: U.S. G.P.O., 1989.

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Book chapters on the topic "San Juan County (Utah)"

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Wondolleck, Julia M., and Steven L. Yaffee. "Influencing Management from the Bottom Up in Port Orford, Oregon, and San Juan County, Washington." In Marine Ecosystem-Based Management in Practice, 131–52. Washington, DC: Island Press/Center for Resource Economics, 2017. http://dx.doi.org/10.5822/978-1-61091-800-8_6.

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Tillman, R. W. "TOCITO SANDSTONE CORE, HORSESHOE FIELD, SAN JUAN COUNTY, NEW MEXICO." In Shelf Sands and Sandstone Reservoirs, 559–76. SEPM (Society for Sedimentary Geology), 1985. http://dx.doi.org/10.2110/scn.85.13.0559.

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"Columbian Mammoth and Ancient Bison: Paleoindian Petroglyphs along the San Juan River near Bluff, Utah, USA." In Evolution, Cognition, and the History of Religion: A New Synthesis, 562–99. BRILL, 2018. http://dx.doi.org/10.1163/9789004385375_039.

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Church, Stanley E., Robert J. Owen, Paul von Guerard, Philip L. Verplanck, Briant A. Kimball, and Douglas B. Yager. "The effects of acidic mine drainage from historical mines in the Animas River watershed, San Juan County, Colorado—What is being done and what can be done to improve water quality?" In Understanding and Responding to Hazardous Substances at Mine Sites in the Western United States. Geological Society of America, 2007. http://dx.doi.org/10.1130/2007.4017(04).

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deBuys, William. "Sand Canyon: Vanishing Acts." In A Great Aridness. Oxford University Press, 2011. http://dx.doi.org/10.1093/oso/9780199778928.003.0008.

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In the southwest the specter of climate change invites a long look into the deep past. For anyone who hunts for insights about the nature of the region and the trick of making peace with its aridity, the ubiquitous signs of vanished communities beckon irresistibly—in the ruins of Chaco Canyon, the empty cliff dwellings of Mesa Verde, and the mounded rubble of abandoned villages scattered near and far. The “lessons” they offer, however, are not always as clear as we would like them to be. Cautionary tales about the truths and errors of distant centuries can be easy to spin but surprisingly hard to reconcile to the complexity of the archaeological record, which is never static. As with any domain of science, the story told by the archaeology of the Southwest is always emerging, always gaining in heft and detail. When I went looking for someone who could help me read it, the trail I took led to the head of a rugged canyon, choked with piñon and juniper, in the far southwest of Colorado. “There’s a kiva, there’s a kiva, there’s a kiva,” says archaeologist Mark Varien, who is vice president of programs at the Crow Canyon Archaeological Center, outside Cortez. He points in succession to three circular depressions amid the rubble, signatures of the remains of subterranean rooms that once housed much of the life of the pueblo. Rough blocks of sandstone outline the space the kivas occupied, their roofs having long ago caved in. Wind has filled their cavities with the dust and litter of centuries. Now they bloom with cliff rose and sagebrush. We stand just behind the kivas on a mound of half-buried building stones, which are canted at every angle—the remains of masonry rooms. To either side lie the mounds of more room blocks, their rear walls forming the perimeter of the pueblo, and the pueblo itself wrapping around the cleft of a rocky draw. The draw leads south and widens into Sand Canyon, a dry tributary of McElmo Creek, which flows west out of Colorado and joins the San Juan River not far away in Utah.
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Conference papers on the topic "San Juan County (Utah)"

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Hultquist, Arne David, and Chris Shope. "PRELIMINARY WATER QUALITY DATA IN THE SAN JUAN RIVER IN SAN JUAN COUNTY, UTAH FOLLOWING THE GOLD KING MINE SPILL." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-304294.

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Jackson, G. M., and T. L. Davis. "Seismic-stratigraphic study and analysis of a test line, Patterson Field Area, San Juan County, Paradox Basin, Utah." In 1985 SEG Technical Program Expanded Abstracts. SEG, 1985. http://dx.doi.org/10.1190/1.1892644.

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Mercier, John M. "Coal mining in the western San Juan Basin, San Juan County, New Mexico." In 61st Annual Fall Field Conference. New Mexico Geological Society, 2010. http://dx.doi.org/10.56577/ffc-61.173.

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Chenoweth, William L., and Virginia T. McLemore. "Uranium in the Sanostee district, San Juan County, New Mexico." In 61st Annual Fall Field Conference. New Mexico Geological Society, 2010. http://dx.doi.org/10.56577/ffc-61.213.

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Sealey, Paul L., and Spencer G. Lucas. "Ammonite Zones in the Southeastern San Juan Basin, Sandoval County, New Mexico." In 2016 New Mexico Geological Society Annual Spring Meeting. Socorro, NM: New Mexico Geological Society, 2016. http://dx.doi.org/10.56577/sm-2016.403.

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Lange, Steven. "Evaluating the effectiveness of Sunnyside Gold Corporation’s reclamation, San Juan County, Colorado, USA." In 13th International Conference on Mine Closure. Australian Centre for Geomechanics, Perth, 2019. http://dx.doi.org/10.36487/acg_rep/1915_99_lange.

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Steelquist, Aaron T., Gustav Seixas, and George E. Hilley. "FLUVIAL INCISION RATES OF THE SAN JUAN RIVER USING IN-SITU 10-BE, MEXICAN HAT, UTAH." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-304091.

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Hunt-Foster, R. K., T. E. Williamson, and N. R. Longrich. "Attempted relocation of the 1941 University of Oklahoma Pentaceratops Quarry, San Juan County, New Mexico (abs.)." In 2010 New Mexico Geological Society Annual Spring Meeting. Socorro, NM: New Mexico Geological Society, 2010. http://dx.doi.org/10.56577/sm-2010.661.

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Sealey, Paul L., and Spencer G. Lucas. "Paleontology, stratigraphy and biostratigraphy of the upper Cretaceous Lewis Shale near Waterflow, San Juan County, New Mexico." In 48th Annual Fall Field Conference. New Mexico Geological Society, 1997. http://dx.doi.org/10.56577/ffc-48.233.

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Newton, Brad Talon, Ethan Mamer, and Stacy Timmons. "Geochemistry of the Animas River Alluvial Aquifer After the Gold King Mine Spill, San Juan County, New Mexico." In 2018 New Mexico Geological Society Annual Spring Meeting. Socorro, NM: New Mexico Geological Society, 2018. http://dx.doi.org/10.56577/sm-2018.802.

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Reports on the topic "San Juan County (Utah)"

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Thomas C. Chidsey Jr. PRODUCTION ANALYSIS: CHEROKEE AND BUG FIELDS, SAN JUAN COUNTY, UTAH. Office of Scientific and Technical Information (OSTI), December 2003. http://dx.doi.org/10.2172/835836.

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Thomas C. Chidsey Jr and David E. Eby. THIN SECTION DESCRIPTIONS: CHEROKEE AND BUG FIELDS, SAN JUAN COUNTY, UTAH. Office of Scientific and Technical Information (OSTI), December 2003. http://dx.doi.org/10.2172/835954.

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Thomas C. Chidsey Jr and David E. Eby. CAPILLARY PRESSURE/MERCURY INJECTION ANALYSIS: CHEROKEE AND BUG FIELDS, SAN JUAN COUNTY, UTAH. Office of Scientific and Technical Information (OSTI), December 2003. http://dx.doi.org/10.2172/835960.

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Banis, David. The Wilderness Problem: A Narrative of Contested Landscapes in San Juan County, Utah. Portland State University Library, January 2000. http://dx.doi.org/10.15760/etd.1971.

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Thomas C. Chidsey Jr, David E. Eby, and Louis H. Taylor. SCANNING ELECTRON MICROSCOPY AND PORE CASTING: CHEROKEE AND BUG FIELDS, SAN JUAN COUNTY, UTAH. Office of Scientific and Technical Information (OSTI), December 2003. http://dx.doi.org/10.2172/835956.

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David E. Eby, Thomas C. Chidsey Jr, Kevin McClure, Craig D. Morgan, and Stephen T. Nelson. CARBON AND OXYGEN ISOTOPIC ANALYSIS: BUG, CHEROKEE, AND PATTERSON CANYON FIELDS, SAN JUAN COUNTY, UTAH. Office of Scientific and Technical Information (OSTI), December 2003. http://dx.doi.org/10.2172/835831.

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Thomas C. Chidsey Jr, David E. Eby, and Laura L. Wray. POROSITY/PERMEABILITY CROSS-PLOTS: CHEROKEE AND BUG FIELDS, SAN JUAN COUNTY, UTAH, AND LITTLE UTE AND SLEEPING UTE FIELDS, MONTEZUMA COUNTY, COLORADO. Office of Scientific and Technical Information (OSTI), December 2003. http://dx.doi.org/10.2172/835843.

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Thomas C. Chidsey Jr, David E. Eby, and Laura L. Wray. GEOPHYSICAL WELL LOG/CORE DESCRIPTIONS, CHEROKEE AND BUG FIELDS, SAN JUAN COUNTY, UTAH, AND LITTLE UTE AND SLEEPING UTE FIELDS, MONTEZUMA COUNTY, COLORADO. Office of Scientific and Technical Information (OSTI), December 2003. http://dx.doi.org/10.2172/835830.

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Thomas C. Chidsey Jr, Craig D. Morgan, Kevin McClure, David E. Eby, and Laura L. Wray. CROSS SECTIONS AND FIELD MAPS: CHEROKEE AND BUG FIELDS, SAN JUAN COUNTY, UTAH, AND LITTLE UTE AND SLEEPING UTE FIELDS, MONTEZUMA COUNTY, COLORADO. Office of Scientific and Technical Information (OSTI), December 2003. http://dx.doi.org/10.2172/835844.

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Doelling, Hellmut H., and Grant C. Willis. Geologic map of the Smoky Mountain 30' x 60' quadrangle, Kane and San Juan Counties, Utah, and Coconino County, Arizona. Utah Geological Survey, May 2006. http://dx.doi.org/10.34191/m-213.

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