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Journal articles on the topic 'Utah County (Utah) Provo (Utah) Utah'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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1

Kowallis, Bart, and Laura Wald. "Rock Canyon near Provo, Utah County: A Geologic Field Laboratory." Geosites 1 (March 12, 2020): 1–15. http://dx.doi.org/10.31711/geosites.v1i1.58.

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Rock Canyon near Provo, Utah is an ideal outdoor laboratory. The canyon has been known and explored for many years by scientists and students for its fascinating geology, biology, and botany. It is also a favorite location for rock climbers, hikers, and other outdoor enthusiasts. Facilities near the mouth of the canyon including parking, restrooms, a lecture amphitheater, and a covered pavilion with picnic tables provide an ideal location for visitors. Geology is the focal point of this beautiful canyon with a history that stretches from the Precambrian (about 700 million years ago) to the Wasatch fault and Lake Bonneville, which covered much of western Utah at its peak roughly 18,000 years ago. Excellent exposures of the rocks allow visitors to see features clearly and piece together the history of the canyon. The oldest rocks are glacial deposits of the Mineral Fork Tillite. The tillite is overlain by a thick section of Paleozoic rocks of Cambrian to Permian age, all of which have been deformed into an asymmetric, overturned fold formed during the Sevier orogeny, a roughly 140 to 50 million year old mountain building event. The upper reaches of the canyon were sculpted by glaciers during the Pleistocene and deposits of the Provo and Bonneville levels of Lake Bonneville are found at the mouth of the canyon, now cut by a recent alluvial fan. Also, at the mouth of the canyon are excellent exposures of features associated with the Wasatch fault.

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2

Pratiwi, Cekli S. "OPTIMIZING RESTORATIVE JUSTICE PROGRAM FOR THE BEST INTEREST OF THE CHILDREN IN REFORMING JUVENILE JUSTICE SYSTEM IN UTAH." Legality : Jurnal Ilmiah Hukum 27, no. 2 (November 6, 2019): 242. http://dx.doi.org/10.22219/jihl.v27i2.10172.

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This study examine first, to what extent the fully restorative justice system could be implemented in the Utah’s JJS and supported by the legislations so that the minor can enjoy a special protection while they still have the opportunity to participate actively with accountability in solving the problem without destroy their freedom and dignity and can bring more benefit to their best interest. Second, to what extent the right to legal counsel could help the minor to enjoy their constitutional rights as well as to seek a better solution of their problem. The research done by observing the review hearing, pre-trial, petition, trial at the Fourth Judicial District Courthouse Provo and the detention hearing at Slate Canyon Youth Center. The data is also collected from various secondary resources such as the Utah Statutes, the international and regional instruments. There is an opportunity for the JJS Utah county to shift from applying the partly to the fully RJP specially for truancy or misdemeanor cases and the right to access public defender should be automatically granted to the minors.

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3

Quist, Tanya M., C. Frank Williams, and M. L. Robinson. "Effects of Varying Water Quality on Growth and Appearance of Landscape Plants." Journal of Environmental Horticulture 17, no. 2 (June 1, 1999): 88–91. http://dx.doi.org/10.24266/0738-2898-17.2.88.

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Abstract Increasing demand for limited water supplies in populated arid regions over the next decade may require implementation of new water-use practices. Eliminating use of high-quality water for landscape irrigation by using low-quality water delivered through secondary systems is an ideal option for conserving potable water. However, irrigation of woody landscape plants using waters high in inorganic salts may adversely affect soil fertility, structure, plant growth and appearance. Twelve woody ornamentals commonly used in landscapes in Salt Lake County, Utah, were treated with three blends of Utah Lake and Provo River water to assess the quality of plants produced. Three irrigation treatments, designated high-, medium-, and low-quality water were blended to maintain sodium concentrations of 15, 80 and 120 mg/liter respectively. Soils irrigated with medium-and low-quality water developed significantly higher adjusted sodium absorption ratio (SAR) and salinity than soils irrigated with high quality water and the effect varied with time. Except for four species, medium-and low-quality water did not significantly lower scores for plant appearance. Results of this two-year study support development of secondary water systems and use of lower-quality water for landscape irrigation.

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4

Ausich, William I. "Lower Mississippian crinoid (Echinodermata) fauna from Utah County, Utah." Journal of Paleontology 77, no. 1 (January 2003): 139–45. http://dx.doi.org/10.1017/s0022336000043481.

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A low-diversity crinoid fauna is described from the Fitchville Formation, Lower Mississippian (Late Devonian to Early Mississippian) of Utah County, Utah. Based on the crinoid fauna, composed of Nunnacrinus olsoni new species, Paracosmetocrinus lundi new species, and Platycrinites sp., this fauna is interpreted as being from the Kinderhookian, Upper Fitchville Formation. This occurrence of Nunnacrinus extends the geographic and facies range of this genus in western North America and the geographic range of Paracosmetocrinus within western North America.

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5

AUSICH, WILLIAM I. "LOWER MISSISSIPPIAN CRINOID (ECHINODERMATA) FAUNA FROM UTAH COUNTY, UTAH." Journal of Paleontology 77, no. 1 (January 2003): 139–45. http://dx.doi.org/10.1666/0022-3360(2003)077<0139:lmceff>2.0.co;2.

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6

WITKIND, I. J. "Potential Geologic Hazards near the Thistle Landslide, Utah County, Utah." Environmental & Engineering Geoscience xxv, no. 1 (February 1, 1988): 83–94. http://dx.doi.org/10.2113/gseegeosci.xxv.1.83.

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7

Shupe, J. B., J. D. Brotherson, and S. R. Rushforth. "Patterns of vegetation surrounding springs in Goshen Bay, Utah County, Utah U.S.A." Hydrobiologia 139, no. 2 (August 1986): 97–107. http://dx.doi.org/10.1007/bf00028092.

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8

Christensen, M. J., J. W. Bown, and L. I. Lei. "The effect of income on selenium intake and status in Utah County, Utah." Journal of the American College of Nutrition 7, no. 2 (April 1988): 155–67. http://dx.doi.org/10.1080/07315724.1988.10720233.

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9

Boulter, Tyler, Solanda Moran, Victor Moxley, and Eugene C. Cole. "Investigation of Knowledge and Perception of Tuberculosis Among Hispanics in Utah County, Utah." Journal of Immigrant and Minority Health 19, no. 1 (November 23, 2015): 147–54. http://dx.doi.org/10.1007/s10903-015-0316-8.

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10

Sharifi-Mood, Mahyar, Daniel T. Gillins, Kevin W. Franke, Jasmyn N. Harper, Steven J. Bartlett, and Michael J. Olsen. "Probabilistic liquefaction-induced lateral spread hazard mapping and its application to Utah County, Utah." Engineering Geology 237 (April 2018): 76–91. http://dx.doi.org/10.1016/j.enggeo.2018.01.015.

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11

Peabody, Frederick. "Rare Plants of Bryce Canyon National Park, Utah." UW National Parks Service Research Station Annual Reports 15 (January 1, 1991): 61–63. http://dx.doi.org/10.13001/uwnpsrc.1991.2969.

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A literature survey has been completed in order to determine plant species that have been considered rare, and also plant species that are potentially rare. Dr. Stan Welsh of the Botany and Range Science Department of Brigham Young University (Provo, Utah) was contacted personally during the field season. His experience in the region has provided a list of additional species that are considered rare for the state of Utah and occur on specific sites near the National Park (Table 1). It is possible that these additional rare species may occur within the boundaries of the park.

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12

Ramsey, Gordon P. "2019 AAPT Award Citations at the Summer Meeting, Provo, Utah." American Journal of Physics 87, no. 9 (September 2019): 696–98. http://dx.doi.org/10.1119/1.5123356.

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13

Obeidi, Fida, and Delbert J. Eatough. "Continuous Measurement of Semivolatile Fine Particulate Mass in Provo, Utah." Aerosol Science and Technology 36, no. 2 (January 2002): 191–203. http://dx.doi.org/10.1080/027868202753504056.

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14

Smith, Justen O., and John L. Wesley. "4-H Donated Meat Program: A Model for Service." Journal of Youth Development 4, no. 1 (March 1, 2009): 132–36. http://dx.doi.org/10.5195/jyd.2009.281.

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Meat continues to be the most in-demand food item for the Utah Food Bank. To address this issue, the 4-H Donated Meat Program was started by a 4-H Club in Davis County, Utah. When Utah State University Extension Agents in Davis, Salt Lake, Weber, and Morgan Counties became involved in the program it expanded rapidly. The program was made possible through generous donations from corporations allowing for the purchase of market livestock exhibited by 4-H youth at county fair livestock sales. USDA certified processed meat was then donated to the Utah Food Bank for distribution to hungry families in the counties participating in the program. The program has grown rapidly. In 2005, two counties were involved with 3,000 pounds of meat donated to the food bank. By 2007, ten counties were involved with 70,000 pounds of meat donated. This program has become a model of service for hundreds of 4-H youth in Utah. This program may be duplicated in other states to meet the demand for meat at food banks across the nation.

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15

Anderson, Paul. "What you can discover on an ancient Cretaceous beach, a geosite in Emery County, Utah." Geosites 1 (December 31, 2019): 1–9. http://dx.doi.org/10.31711/geosites.v1i1.77.

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Utah was prime beach country in its central to eastern portion during the Middle to Late Cretaceous (70 to 92 million years ago). At this time, a long shallow sea extended from the Artic to the Gulf of Mexico and from central Utah east to beyond Kansas. Scores of ancient beach deposits that represent the shoreline along this seaway are exposed in the eastern half of Utah. This paper will guide you to one of these white sandy beaches that dominated central Utah during this time period. The site is located near a developed archeological site (Rochester panel, Smithsonian site number 42EM392). The Rochester panel is dissimilar to other Fremont culture images and likely dates between A.D. 500 to A.D. 700 (Loendorf, 1985). If you visit the panel please do not touch (oil from you skin damages the surface), deface, or climb on this precious resource.

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16

Ege, Carl. "Devils playground, Box Elder County." Geosites 1 (December 31, 2019): 1–7. http://dx.doi.org/10.31711/geosites.v1i1.79.

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Why take your kids to the neighborhood playground, when you can visit a playground that inspires their sense of geologic adventure? Devils Playground is not your ordinary community playground, but a wonderland of granitic rock weathered into fantastic forms and weird shapes. Occupying an assortment of Bureau of Land Management, state, and private land in the Bovine Mountains, Devils Playground is a relatively unknown geologic curiosity found in a remote corner of northwestern Utah. Devils Playground is situated in the physiographic region known as the Great Basin province that extends across western Utah, Nevada, and to the Sierra Nevada Mountains in eastern California. The area is composed mostly of granitic rocks of the Emigrant Pass intrusion. A combination of granitic rock, faulting, and weathering under a semiarid climate created favorable conditions for the creation of Devils Playground. Desert plants such as sagebrush,Utah juniper, pinyon pine, Mormon tea, and cheatgrass are common throughout the area.

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17

Wolff, Leonard, and Gerry Austin. "Orpiment from Barneys Canyon, Salt Lake County, Utah." Rocks & Minerals 80, no. 3 (May 2005): 194–96. http://dx.doi.org/10.3200/rmin.80.3.194-196.

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18

Harris, KaLynne, Lauren Vanderhooft, Lindsay Burt, Sheryll Vanderhooft, and Christopher Hull. "Tanning business practices in Salt Lake County, Utah." Journal of the American Academy of Dermatology 66, no. 3 (March 2012): 513–14. http://dx.doi.org/10.1016/j.jaad.2011.08.017.

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19

Hurlbut, David Dmitri. "The “Conversion” of Anthony Obinna to Mormonism: Elective Affinities, Socio-Economic Factors, and Religious Change in Postcolonial Southeastern Nigeria." Religions 11, no. 7 (July 15, 2020): 358. http://dx.doi.org/10.3390/rel11070358.

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This article analyzes the “conversion” of Anthony Uzodimma Obinna, an Igbo schoolteacher from the town of Aboh Mbaise in Imo State, and his extended family to Mormonism in southeastern Nigeria between the 1960s and the 1980s, from a historical perspective. I argue that the transition of Anthony Obinna and his family away from Catholicism to Mormonism can be explained by both the elective affinities that existed between Mormonism and indigenous Igbo culture, and socio-economic factors as well. This article bases its conclusions on a close reading of oral histories, personal papers, and correspondence housed at the LDS Church History Library in Salt Lake City, Utah and L. Tom Perry Special Collections at Harold B. Lee Library, Brigham Young University in Provo, Utah.

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20

Sharp, Aaron R., Perry G. Ridge, Matthew H. Bailey, Kevin L. Boehme, Maria C. Norton, JoAnn T. Tschanz, Ronald G. Munger, Christopher D. Corcoran, and John SK Kauwe. "Population substructure in Cache County, Utah: the Cache County study." BMC Bioinformatics 15, Suppl 7 (2014): S8. http://dx.doi.org/10.1186/1471-2105-15-s7-s8.

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21

Holmgren, Lyle N., and Chad R. Reid. "4-H & FFA Livestock Projects: Life Skills Gained and Knowledge Learned." Journal of Youth Development 2, no. 1 (June 1, 2007): 124–32. http://dx.doi.org/10.5195/jyd.2007.367.

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Junior Livestock shows are one of the most popular 4-H and FFA projects in Utah. Thousands of youth participate in these shows from every county in Utah. County extension agents and FFA advisors spend much time with livestock committees, leaders, parents, and youth engaged in livestock shows. Can public funds spent on salaries be justified for county 4-H extension agents and FFA advisors who work with junior livestock shows? To help answer this question, 413 youth involved in livestock shows in Utah were surveyed in 2001. Youth were asked to share skills learned from their livestock projects. Value statements along with specific content skills were measured in the survey. The results indicate that from their 4-H and FFA projects, youth learned to accept responsibility, follow instructions, gain self-confidence, follow instructions, “do the right thing” as well as a variety of other values and content skills.

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22

COOK, A. GAYLON. "Suckers of the Subgenus Pantosteus from Provo River and “Cottonwood Creek”, Utah." American Midland Naturalist 143, no. 2 (April 2000): 422–32. http://dx.doi.org/10.1674/0003-0031(2000)143[0422:sotspf]2.0.co;2.

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23

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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24

AGRELL, S. O., G. A. CHINNER, and P. D. ROWLEY. "The black skarns of Pine Canyon, Piute County, Utah." Geological Magazine 136, no. 4 (July 1999): 343–59. http://dx.doi.org/10.1017/s0016756899002800.

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A small micromonzonite pluton intruding Miocene extrusives of the Marysvale volcanic field of southern Utah has undergone a sequence of explosive brecciation, syenite veining, rheomorphism, calcium metasomatism and zeolitization. Skarn-like occurrences of magnetite and Al-spinel-rich feldspathoidal rocks within the outcrop are of two main types: (1) an olivine-bearing variety with occasional REE-rich minerals (zirconolite) occurs as veins and seams in desilicated latite screens and xeno-liths.; (2) an aluminous, corundum- and hibonite-bearing variety with accessory zirconolite, perovskite and armalcolite occurs mainly as fillings to the micromonzonite breccias. The chemically disparate types are interpreted as having initiated as propylitic, and argillic/alunitic, alterations of latite country rock in the early hydrothermal system of the pluton. Subsequent intrusion of the micromonzonite to higher levels has incorporated these products into the igneous complex, in which they have experienced varying degrees of nephelinization, pyrometamorphism, rheomorphism and veining.

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25

Pope, C. Arden, and F. Dean Miner. "Valuation of improved air quality in Utah County, USA." Environmental Management 12, no. 3 (May 1988): 381–89. http://dx.doi.org/10.1007/bf01867527.

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26

Medina, Richard M., Kara Byrne, Simon Brewer, and Emily A. Nicolosi. "Housing inequalities: Eviction patterns in Salt Lake County, Utah." Cities 104 (September 2020): 102804. http://dx.doi.org/10.1016/j.cities.2020.102804.

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27

Benson, Alvin K., and Stephan T. Hash. "Integrated three-dimensional interpretation of major concealed faults beneath Mapleton, Utah County, Utah using gravity data, supported with magnetic data." Engineering Geology 51, no. 2 (December 1998): 109–30. http://dx.doi.org/10.1016/s0013-7952(98)00045-3.

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28

Rigby, J. Keith, and Paul Jamison. "Lithistid sponges from the Late Ordovician Fish Haven Dolomite, Bear River Range, Cache County, Utah." Journal of Paleontology 68, no. 4 (July 1994): 722–26. http://dx.doi.org/10.1017/s0022336000026160.

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The tricranoclad demosponge Hindia sphaeroidalis Duncan, 1879, is reported as a common silicified sponge in the basal dolomite of the Deep Lakes Member of the Upper Ordovician Fish Haven Formation of northeastern Utah for the first time. A small juvenile orchoclad anthaspidellid, Hudsonospongia? sp., is also the first of that family reported from Fish Haven beds and the Deep Lakes Member. Both taxa are from localities on the eastern slope of Mount Magog, north of Tony Grove Lake, in the Bear River Range, Cache County, east of Logan, Utah.

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29

Smith, Katelynn M., John H. McBride, Stephen T. Nelson, R. William Keach, Samuel M. Hudson, David G. Tingey, Kevin A. Rey, and Gregory T. Carling. "An integrated high-resolution geophysical and geologic visualization of a Lake Bonneville shoreline deposit (Utah, USA)." Interpretation 7, no. 2 (May 1, 2019): T265—T282. http://dx.doi.org/10.1190/int-2018-0116.1.

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Pilot Valley, located in the eastern Basin and Range, Western Utah, USA, contains numerous shorelines and depositional remnants of Late Pleistocene Lake Bonneville. These remnants present excellent ground-penetrating radar (GPR) targets due to their coherent stratification, low-clay, low-salinity, and low moisture content. Three-dimensional GPR imaging can resolve fine-scale stratigraphy of these deposits down to a few centimeters, and when combined with detailed outcrop characterization, it provides an in-depth look at the architecture of these deposits. On the western side of Pilot Valley, a well-preserved late Pleistocene gravel bar records shoreline depositional processes associated with the Provo (or just post-Provo) shoreline period. GPR data, measured stratigraphic sections, cores, paleontological sampling for paleoecology and radiocarbon dating, and mineralogical analysis permit a detailed reconstruction of the depositional environment of this well-exposed prograding gravel bar. Contrary to other described Bonneville shoreline deposits, calibrated radiocarbon ages ranging from 16.5 to 14.3 (ka, BP) indicate that the bar was stable and active during an overall regressive stage of the lake, as it dropped from the Provo shoreline (or just post-Provo level). Our study provides a model for an ancient pluvial lakeshore depositional environment in the Basin and Range province and suggests that stable, progradational bedforms common to the various stages of Lake Bonneville are likely not all associated with periods of shoreline stability, as is commonly assumed. The high-resolution GPR visualization demonstrates the high degree of compartmentalization possible for a potential subsurface reservoir target based on ancient shoreline sedimentary facies.

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30

Benson, Alvin K., Kelly L. Payne, and Melissa A. Stubben. "Mapping groundwater contamination using dc resistivity and VLF geophysical methods–A case study." GEOPHYSICS 62, no. 1 (January 1997): 80–86. http://dx.doi.org/10.1190/1.1444148.

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Geophysical methods can be helpful in mapping areas of contaminated soil and groundwater. Electrical resistivity and very low‐frequency electromagnetic induction (VLF) surveys were carried out at a site of shallow hydrocarbon contamination in Utah County, Utah. Previously installed monitoring wells facilitated analysis of water chemistry to enhance interpretation of the geophysical data. The electrical resistivity and VLF data correlate well, and vertical cross‐sections and contour maps generated from these data helped map the contaminant plume, which was delineated as an area of high interpreted resistivities.

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31

Sprinkel, Douglas, Mary Beth Bennis, Dale Gray, and Carole Gee. "Stratigraphic Setting of Fossil Log Sites in the Morrison Formation (Upper Jurassic) near Dinosaur National Monument, Uintah County, Utah, USA." Geology of the Intermountain West 6 (October 31, 2019): 61–76. http://dx.doi.org/10.31711/giw.v6.pp61-76.

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The outcrop belt of the Upper Jurassic Morrison Formation in the northeastern Uinta Basin and southeastern flank of the Uinta Mountains is particularly rich in dinosaurian and non-dinosaurian faunas, as well as in fossil plants. The discovery of several well-preserved, relatively intact, fossil logs at several locations in Rainbow Draw and one location in Miners Draw, both near Dinosaur National Monument (Utah), has provided an opportunity to study the local paleobotany, stratigraphy, and sedimentology of the Morrison Formation in northeastern Utah.

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32

Petersen, Morris S., Dieter Korn, and Jürgen Kullmann. "The Early Mississippian (Osagean) ammonoid Dzhaprakoceras (Cephalopoda) from Utah." Journal of Paleontology 74, no. 5 (September 2000): 853–57. http://dx.doi.org/10.1017/s0022336000033059.

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The Mississippian ammonoid genus Dzhaprakoceras Popov, 1965, well known in the eastern hemisphere, is reported from the Delle Member of the Deseret Limestone at Flux and Lakeside Mountains, Tooele County, Utah. This is the first report of the genus in western North America. The ammonoids, D. gordoni n. sp. and D. djaprakense (Librovitch, 1927) occur with mehli—Lower texanus Zone conodonts indicating a middle Osagean (earliest Viséan) age.

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33

Stokes, Wm Lee. "Alleged Human Footprint from Middle Cambrian Strata, Millard County, Utah." Journal of Geological Education 34, no. 3 (May 1986): 187–90. http://dx.doi.org/10.5408/0022-1368-34.3.187.

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34

Leavitt, Steven D., and Larry L. St Clair. "Lichens of the Boulder Mountain Plateau, Wayne County, Utah, USA." Evansia 25, no. 4 (December 2008): 85–89. http://dx.doi.org/10.1639/0747-9859-25.4.85.

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35

Call, David A., Richard M. Medina, and Alan W. Black. "Causes of Weather-Related Crashes in Salt Lake County, Utah." Professional Geographer 71, no. 2 (December 20, 2018): 253–64. http://dx.doi.org/10.1080/00330124.2018.1501713.

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36

Benson, Alvin K., and Andrew R. Floyd. "Application of gravity and magnetic methods to assess geological hazards and natural resource potential in the Mosida Hills, Utah County, Utah." GEOPHYSICS 65, no. 5 (September 2000): 1514–26. http://dx.doi.org/10.1190/1.1444840.

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Gravity and magnetic data were collected in the Mosida Hills, Utah County, Utah, at over 1100 stations covering an area of approximately 58 km2 (150 mi2) in order to help define the subsurface geology and assess potential geological hazards for urban planning in an area where the population is rapidly increasing. In addition, potential hydrocarbon traps and mineral ore bodies may be associated with some of the interpreted subsurface structures. Standard processing techniques were applied to the data to remove known variations unrelated to the geology of the area. The residual data were used to generate gravity and magnetic contour maps, isometric projections, profiles, and subsurface models. Ambiguities in the geological models were reduced by (1) incorporating data from previous geophysical surveys, surface mapping, and aeromagnetic data, (2) integrating the gravity and magnetic data from our survey, and (3) correlating the modeled cross sections. Gravity highs and coincident magnetic highs delineate mafic lava flows, gravity lows and magnetic highs reflect tuffs, and gravity highs and magnetic lows spatially correlate with carbonates. These correlations help identify the subsurface geology and lead to new insights about the formation of the associated valleys. At least eight new faults (or fault segments) were identified from the gravity data, whereas the magnetic data indicate the existence of at least three concealed and/or poorly exposed igneous bodies, as well as a large ash‐flow tuff. The presence of low‐angle faults suggests that folding or downwarping, in addition to faulting, played a role in the formation of the valleys in the Mosida Hills area. The interpreted location and nature of concealed faults and volcanic flows in the Mosida Hills area are being used by policy makers to help develop mitigation procedures to protect life and property.

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37

Smith, Derald G., and Harry M. Jol. "Ground-penetrating radar investigation of a Lake Bonneville deita, Provo level, Brigham City, Utah." Geology 20, no. 12 (1992): 1083. http://dx.doi.org/10.1130/0091-7613(1992)020<1083:gprioa>2.3.co;2.

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38

Dayvault, Richard. "“Red Wood” from the Yellow Cat Area of Grand County, Utah." Rocks & Minerals 75, no. 4 (July 2000): 258–67. http://dx.doi.org/10.1080/00357520009605654.

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39

Shumway, J. Matthew, and Richard H. Jackson. "Place Making, Hazardous Waste, And The Development Of Tooele County, Utah*." Geographical Review 98, no. 4 (October 1, 2008): 433–55. http://dx.doi.org/10.1111/j.1931-0846.2008.tb00311.x.

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40

HYLLAND, M. D., and M. LOWE. "Regional Landslide-Hazard Evaluation Using Landslide Slopes, Western Wasatch County, Utah." Environmental & Engineering Geoscience III, no. 1 (March 1, 1997): 31–43. http://dx.doi.org/10.2113/gseegeosci.iii.1.31.

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41

Cesbron, Fabien P., and Sidney A. Williams. "Tooeleite, a new mineral from the U.S. Mine, Tooele County, Utah." Mineralogical Magazine 56, no. 382 (March 1992): 71–73. http://dx.doi.org/10.1180/minmag.1992.056.382.09.

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AbstractThe new mineral tooeleite occurs with pyrite, arsenopyrite, scorodite, and jarosite at the U.S. Mine, Tooele Country, Utah. Analysis by electron microprobe gave Fe2O3 43.56%, As2O5 38.61%, SO3 7.24%, and H2O by the Penfield method 9.80%. For this analysis, the suggested formula is Fe8-2x3+[(AS1-xSx)O4]6(OH)6.5H20; x is about 0.2.Crystals are orthorhombic, perhaps Pbcm or Pbc21, with a = 6.416, b 19.45, c = 8.941 Å. The strongest diffraction lines are [d in Å, (hkl), (I)] 9.75 (020) (10); 3.208 (200,132) (9); 3.047 (061,220) (5); 4.476 ({002) (4) and 2.680 (240,113) (4). The mineral is optically negative with a small 2V; α = 1.94, β = 2.05, γ = 2.06. Hardness = 3, Dmeas = 4.23, Dcalc = 4.15 g/cm3 for Z = 2.

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42

Draper, Thomas W., Thomas B. Holman, Whitney White, and Shannon Grandy. "Adult Attachment and Declining Birthrates." Psychological Reports 100, no. 1 (February 2007): 19–23. http://dx.doi.org/10.2466/pr0.100.1.19-23.

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Attachment scores for 658 young adults living in the USA were obtained using the Experiences in Close Relationships scale. The participants came from a subsample of the RELATE data set, who had also filled out the adult attachment measure. Those young adults living in Utah County, Utah, an area of the country with a higher than normal birthrate (88% members of the Church of Jesus Christ of Latter-day Saints), also had higher than average adult attachment scores. While the methodology was not sufficient to assess causal direction nor eliminate the possibility of unidentified influences, an undiscussed psychological factor, adult attachment, may play a role in the numerical declines observed among nonimmigrant communities in the USA and Europe.

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43

Bush, Michael. "Born in Zanzibar, Computerized in Provo, Utah: A Systematic Instructional Design Approach for Swahili CALL." CALICO Journal 27, no. 3 (May 31, 2010): 505–16. http://dx.doi.org/10.11139/cj.27.3.505-516.

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44

Novilla, M. Lelinneth B., James D. Johnston, John D. Beard, Lucas L. Pettit, Siena F. Davis, and Claire E. Johnson. "Radon Awareness and Policy Perspectives on Testing and Mitigation." Atmosphere 12, no. 8 (August 8, 2021): 1016. http://dx.doi.org/10.3390/atmos12081016.

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One in three homes in Utah (USA) contains dangerous levels of radon. Except for a radon mitigation certification law, Utah’s radon laws are nonexistent. To determine public perception of state policies on radon testing and mitigation, a social cognitive theory-based 52-item questionnaire was administered to residents (N = 307) who visited the Utah County Health Department (UCHD) during the study period. Respondents were divided into an Environmental Health Group (n = 110), who purchased a radon kit, and Vital Records Control Group (n = 197), who filed/obtained birth/death certificates at UCHD. Ninety percent responded they had never tested their homes for radon, and 99% were not aware of state policies regarding radon. Support for various radon policies was significantly associated with older age (odds ratios (OR): 0.37–0.52), being female (OR: 2.60–7.79), lower annual family income (OR: 2.27), and theoretical constructs of behavioral modeling (OR: 2.31–2.55) and risk perception (OR: 2.55–3.71). To increase awareness, testing, and remediation, respondents suggested increasing public education/awareness, requiring testing in homes, businesses, and public buildings, and increasing access to testing. Multi-sectoral radon risk reduction programs could incorporate behavioral modeling and risk perception as components to create a radon testing and mitigation culture in Utah.

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45

LACHMAR, T. E., K. K. BRADBURY, and J. P. EVANS. "Structure and Hydrogeology of Deformed Sedimentary Bedrock Aquifers, Western Summit County, Utah." Environmental & Engineering Geoscience 8, no. 3 (August 1, 2002): 219–36. http://dx.doi.org/10.2113/8.3.219.

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46

Gay, Christopher, Laura Shane-McWhorter, Kathy Williams, and Mary Bishop Stone. "Physician Prescribing of Anorexigenics for Weight Loss in Salt Lake County, Utah." Pharmacotherapy 20, no. 8 (August 2000): 967–73. http://dx.doi.org/10.1592/phco.20.11.967.35267.

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47

Loring, Michael W., and John P. Workman. "The Relationship between Land Ownership and Range Condition in Rich County, Utah." Journal of Range Management 40, no. 4 (July 1987): 290. http://dx.doi.org/10.2307/3898721.

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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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49

Refsnider, Kurt A., Benjamin J. C. Laabs, and David M. Mickelson. "Glacial Geology and Equilibrium Line Altitude Reconstructions for the Provo River Drainage, Uinta Mountains, Utah, U.S.A." Arctic, Antarctic, and Alpine Research 39, no. 4 (November 2007): 529–36. http://dx.doi.org/10.1657/1523-0430(06-060)[refsnider]2.0.co;2.

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50

Leary, P. C., and T. L. Henyey. "Anisotropy and fracture zones about a geothermal well from P‐wave velocity profiles." GEOPHYSICS 50, no. 1 (January 1985): 25–36. http://dx.doi.org/10.1190/1.1441833.

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The feasibility of locating fracture zones and estimating their crack parameters was examined using an “areal well shoot” method centered on Utah State Geothermal Well 9‐1, Beaver County, Utah. High‐resolution traveltime measurements were made between a borehole sensor and an array of shotpoints distributed radially and azimuthally about the well. The directional dependence of velocity in the vicinity of the well was investigated by comparing traveltimes from different azimuths. Velocity anisotropy was detected; this condition is consistent with, but not required by, the existence of fractures in the basement rock having orientations subparallel to the latest episode of local faulting. The interpretation is complicated by a variable thickness of overburden around the well. Traveltime delays also suggest the presence of a low‐angle fracture zone intersecting the well at a depth of ∼1 500 ft.

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