Relevant bibliographies by topics / St. George Utah

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Academic literature on the topic 'St. George Utah'

Author: Grafiati
Published: 4 June 2021
Last updated: 6 February 2022

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Journal articles on the topic "St. George Utah"

1

Hunt, Larry E., and Larry M. Logue. "A Sermon in the Desert: Belief and Behavior in Early St. George, Utah." Journal of American History 77, no. 1 (June 1990): 312. http://dx.doi.org/10.2307/2078713.

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Pillis, Mario S. De, and Larry M. Logue. "A Sermon in the Desert: Belief and Behavior in Early St. George, Utah." American Historical Review 95, no. 1 (February 1990): 270. http://dx.doi.org/10.2307/2163155.

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Morse, Kathryn, and Larry M. Logue. "A Sermon in the Desert: Belief and Behavior in Early St. George, Utah." Western Historical Quarterly 21, no. 2 (May 1990): 244. http://dx.doi.org/10.2307/969868.

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4

Brooke, John L., and Larry M. Logue. "A Sermon in the Desert: Belief and Behavior in Early St. George, Utah." Journal of Interdisciplinary History 20, no. 2 (1989): 313. http://dx.doi.org/10.2307/204859.

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Goldberg, Robert A., and Larry M. Logue. "A Sermon in the Desert: Belief and Behavior in Early St. George, Utah." Journal of the Early Republic 8, no. 4 (1988): 469. http://dx.doi.org/10.2307/3123193.

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ALLISON, JAMES R., CATHRYN M. MEEGAN, and SHAWN SABRINA MURRAY. "ARCHAEOLOGY AND ARCHAEOBOTANY OF SOUTHERN PAIUTE HORTICULTURE IN THE ST. GEORGE BASIN, SOUTHWESTERN UTAH." KIVA 73, no. 4 (June 2008): 417–49. http://dx.doi.org/10.1179/kiv.2008.73.4.003.

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7

Unfer, Louis. "History of the Earth Sciences at Southeast Missouri State University." Earth Sciences History 4, no. 1 (January 1, 1985): 69–71. http://dx.doi.org/10.17704/eshi.4.1.f2160035u6854p28.

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The history of Southeast Missouri State University parallels that of other teacher education institutions. It started as Southeast Missouri Normal School in 1873 and reached university status in 1972. A department of Geology and Geography was established in 1909, becoming the Geography Department in 1915. In 1924, the sciences were combined into the Science Department. In 1960, this became the Division of Science and Mathematics and the Department of Earth Sciences was formed. An earth science major began in 1937, with separate geology and geography majors established in 1958. Recently the Department has developed more specialized, job-oriented programs in mining geology and in cartography. Since 1983 the Department has also operated a field camp, headquartered on the campus of Dixie College, St. George, Utah.
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VITKUS, ALLISON R., KAREN CHIN, JAMES I. KIRKLAND, ANDREW R. C. MILNER, EDWARD L. SIMPSON, and ERIC T. ELLISON. "UNUSUAL FOSSILIFEROUS CONCRETIONS FROM LACUSTRINE DEPOSITS IN THE LOWER JURASSIC MOENAVE FORMATION IN ST. GEORGE, UTAH, USA: IMPLICATIONS FOR ANCIENT FISH MASS MORTALITIES." PALAIOS 35, no. 2 (February 17, 2020): 77–93. http://dx.doi.org/10.2110/palo.2019.063.

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ABSTRACT Two types of unusual concretions with similar biotic contents but markedly different shapes and distributions were found in close stratigraphic proximity within the Lower Jurassic Whitmore Point Member of the Moenave Formation in St. George, Utah. Both types of concretions formed in lacustrine sediments and contain abundant ganoid fish scales, numerous ostracode carapaces, and apparent rip-up clasts. Elongate, cylindrical concretions developed in parallel and regularly spaced rows in one horizon, and comparatively flat and irregularly shaped and distributed concretions formed in an overlying layer only a few centimeters above. Microprobe and Raman analyses of concretion samples reveal abundant hematite in both concretions as well as groundmass minerals dominated by silica in the cylindrical concretions and dolomite in the flat concretions. The abundance of fish skeletal debris in concretions from two consecutive horizons may suggest recurring fish mass mortality in ancient Lake Dixie, the large lake that occupied the St. George area during the Early Jurassic. We propose a model for the formation of the concretions based on their shapes, distributions, and chemistry. In this model, accumulations of disarticulated fish debris were colonized and consolidated by microbial mats and shaped by oscillatory flow (in the case of the cylindrical concretions) or lack thereof (in the case of the flat concretions). Then, after burial, groundwater chemistry and possibly the metabolic activities of microorganisms led to the precipitation of minerals around and within the masses of fish material. Finally, diagenetic alteration changed the mineral makeups of the cylindrical and flat concretions into what they are today.
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Rose, Makae, Jerald D. Harris, and Andrew R. C. Milner. "A trace fossil made by a walking crayfish or crayfish-like arthropod from the Lower Jurassic Moenave Formation of southwestern Utah, USA." PeerJ 9 (January 26, 2021): e10640. http://dx.doi.org/10.7717/peerj.10640.

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New invertebrate trace fossils from the Lower Jurassic Moenave Formation at the St. George Dinosaur Discovery Site at Johnson Farm (SGDS) continue to expand the ichnofauna at the site. A previously unstudied arthropod locomotory trace, SGDS 1290, comprises two widely spaced, thick, gently undulating paramedial impressions flanked externally by small, tapered to elongate tracks with a staggered to alternating arrangement. The specimen is not a variant of any existing ichnospecies, but bears a striking resemblance to modern, experimentally generated crayfish walking traces, suggesting a crayfish or crayfish-like maker for the fossil. Because of its uniqueness, we place it in a new ichnospecies, Siskemia eurypyge. It is the first fossil crayfish or crayfish-like locomotion trace ever recorded.
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Zatoń, Michał, Paul D. Taylor, and Olev Vinn. "Early Triassic (Spathian) post-extinction microconchids from western Pangea." Journal of Paleontology 87, no. 1 (January 2013): 159–65. http://dx.doi.org/10.1666/12-060r.1.

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A new microconchid tentaculitoid,Microconchus utahensisnew species, is described from the Lower Triassic (Spathian) Virgin Formation of two localities (Hurricane Cliffs and Beaver Dam Mountains) near St George, Utah. This small encrusting tubeworm, previously referred to erroneously asSpirorbis, has a laminated shell microstructure containing minute pores (punctae). The population from deeper water facies of the Beaver Dam Mountains is more abundant than that from Hurricane Cliffs and the tubes are significantly larger in size. Although represented by only one species (M. utahensis), microconchids are by far the most dominant component of the otherwise impoverished sclerobiont assemblage of the Virgin Formation, which also includes rare cemented bivalves and probable foraminifers. Whereas the remainder of the Virgin fauna is quite diverse, the low diversity of encrusters suggests a slow recovery from end-Permian mass extinctions. Indeed, more typically Mesozoic sclerobiont assemblages dominated by cyclostome bryozoans and serpulid polychaetes did not appear until the Late Triassic, probably Rhaetian.
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Dissertations / Theses on the topic "St. George Utah"

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Tatton, Bronson Ron. "Design Guidelines for the Historic Downtown of the City of St. George, Utah." DigitalCommons@USU, 2008. https://digitalcommons.usu.edu/etd/53.

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This document proposes historic preservation guidelines for the downtown area of the City of St. George, Utah. It grew from a summer internship with the city where I took inventory of the streetscape in the Historic Downtown and prepared recommendations in the form of a PowerPoint Presentation that was given to the city council. This paper summarizes the summer internship and introduces a more appropriate approach based on reflection of the internship. The new approach involves a thorough inventory of the historic character, in-depth research of the historic elements that contribute to the historic character, development of design guidelines and standards, reviews, and codification of the design guidelines and standards. The historic elements that contribute most to the city’s historic character are identified as 1) block and lot layout and building setbacks, 2) architecture, 3) irrigation ditches, 4) tree lined streets, and 5) other streetscape elements and site features. Through comprehensive research of old photography, literature, and existing conditions these historic elements are further defined. The historic elements are currently being specified in design guidelines and standards and reviewed by the city in preparation for possible codification. (173 pages)
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Shamo, Michael Lyle. "Making the Desert Blossom: Public Works in Washington County, Utah." BYU ScholarsArchive, 2010. https://scholarsarchive.byu.edu/etd/2555.

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The following thesis is a study of how communities of Washington County, Utah developed within one of the most inhospitable deserts of the American West. A trend of reliance on public works programs during economic depressions, not only put people to work, but also provided an influx of outside aid to develop an infrastructure for future economic stability and growth. Each of these public works was carefully planned by leaders who not only saw the immediate impact these projects would have, but also future benefits they would confer. These communities also became dependent on acquiring outside investment capital from the Mormon Church, private companies and government agencies. This dependency required residents to cooperate not only with each other, but with these outside interests who now had a stake in the county's development. The construction of the Mormon Tabernacle and Temple in St. George during the 1870s made that community an important religious and cultural hub for the entire region. Large-scale irrigation and reclamation projects in the 1890s opened up new areas for agriculture and settlement. And in the 1920s and 1930s the development of Zion National Park and the construction of roads provided the infrastructure for one of the county's most important industries, tourism. Long after these projects' completion they still provided economic and cultural value to the communities they served. Some of these projects provided the infrastructural foundation that allowed Washington County communities to have greater security and control over their economic future. Over time the communities of southern Utah created dramatic reenactments and erected monuments of these very projects to celebrate and preserve the story of their construction. During the first decade of the twenty-first century Washington County has become one of the fastest growing areas in the country, and as a result public works programs continue to be important to support this growth.
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Vitkus, Allison Rebecca. "Unusual, fossiliferous concretions from the lower Jurassic Moenave formation in St. George, Utah, USA| Implications for ancient fish mass mortalities." Thesis, University of Colorado at Boulder, 2015. http://pqdtopen.proquest.com/#viewpdf?dispub=1600564.

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Two types of unusual concretions with similar contents but markedly different shapes and distributions were found in close stratigraphic proximity within the Whitmore Point Member of the Moenave Formation. Roughly cylindrical, elongate concretions were found in parallel and regularly spaced rows, and a layer of irregularly shaped and distributed fossiliferous concretions was discovered only a few centimeters above the cylindrical concretions. Both sets of concretions contain abundant hematite as well as enameloid fish scales. In addition, the concretions contain numerous ostracod carapaces and what appear to be rip-up clasts. Microprobe and Raman analyses of representative concretion samples reveal that the cylindrical concretions have a groundmass largely composed of silica while the irregular concretions have a groundmass largely composed of dolomite, and the ostracods within each type of concretion have been altered and match the chemistry of the surrounding groundmass. Evidence of multiple cement precipitation events is present within each concretion. These unusual concretions suggest mass fish mortality events in the large lake that occupied the St. George area in the early Jurassic.

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Esplin, Scott Clair. "Education in Transition: Church and State Relationships in Utah Education, 1888-1933." Diss., CLICK HERE for online access, 2006. http://contentdm.lib.byu.edu/ETD/image/etd1194.pdf.

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Books on the topic "St. George Utah"

1

A sermon in the desert: Belief and behavior in early St. George, Utah. Urbana: University of Illinois Press, 1988.

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2

Utah Geological Association. Field Conference. Thrusting and extensional structures and mineralization in the Beaver Dam Mountains, southwestern Utah: 1986 Annual Field Conference, Utah Geological Association, October 9, 10, 11, 1986, St. George, Utah. Edited by Griffen Dana T. 1943-, Phillips W. Revell, and Utah Geological Association. Salt Lake City, Utah: Utah Geological Association, 1986.

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3

Westfall, Deborah. Green Spring, an Anasazi and Southern Paiute encampment in the St. George Basin of Utah: The Washington City-Green Spring Archaeological Project. Salt Lake City, Utah: Utah State Office, Bureau of Land Management, 1987.

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Westfall, Deborah. Green Spring, an Anasazi and Southern Paiute encampment in the St. George Basin of Utah: The Washington City-Green Spring Archaeological Project. Salt Lake City, Utah: Utah State Office, Bureau of Land Management, 1987.

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Westfall, Deborah. Green Spring, an Anasazi and Southern Paiute encampment in the St. George Basin of Utah: The Washington City-Green Spring Archaeological Project. Salt Lake City, Utah: Utah State Office, Bureau of Land Management, 1987.

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Gottfried, Gerald J. Ecology, management, and restoration of piñon-juniper and ponderosa pine ecosystems: Combined proceedings of the 2005 St. George, Utah and 2006 Albuquerque, New Mexico workshops. Fort Collins, CO: United States Dept. of Agriculture, Forest Service, Rocky Mountain Research Station, 2008.

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7

Symposium, on Rock Art Conservation and Protection (1987 St George Utah). Preserving our rock art heritage: Proceedings from the Symposium on Rock Art Conservation and Protection, presented at the fourteenth annual conference of the American Rock Art Research Association, St. George, Utah, May 23-24, 1987. [San Miguel, Calif: The Association, 1989.

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United States. Congress. House. Committee on Transportation and Infrastructure. Subcommittee on Aviation., ed. Joint oversight field hearing on national park overflights : joint oversight hearing before the Subcommittee on National Parks and Public Lands of the Committee on Resources, and Subcommittee on Aviation of the Committee on Transportation and Infrastructure, House of Representatives, One Hundred Fifth Congress, first session, November 17, 1997, St. George, Utah. Washington: U.S. G.P.O., 1998.

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Alder, Douglas D., Blaine M. Yorgason, and Richard A. Schmutz. All That Was Promised: The St. George Temple and the Unfolding of the Restoration. Deseret Book, 2013.

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Geologic map of the St. George Basin, Utah, (Washington Co.). Utah Geological Survey, 1986. http://dx.doi.org/10.34191/m-99.

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Book chapters on the topic "St. George Utah"

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Woods, Aaron R., and Ryan P. Harrod. "A Line in the Sand." In Bioarchaeology of Frontiers and Borderlands, 212–30. University Press of Florida, 2019. http://dx.doi.org/10.5744/florida/9781683400844.003.0010.

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This chapter features a bioarchaeological examination of traumatic injuries and pathological conditions on human skeletal remains from the Fremont and Virgin Branch Puebloan cultures of the pre-contact American Great Basin and Southwest. This study indicates that there were differences across the borders of these regions, which share a boundary along the southern portions of Utah and Nevada. The Fremont and Puebloan borders considered in this chapter include the boundary between Parowan Valley and the St. George Basin, and the Canyons of the Escalante River and the Kaiparowits Plateau, all in the state of Utah. Additional Ancestral Puebloan bioarchaeological data will be discussed from southern Nevada to help illustrate differences between Fremont and Ancestral Puebloan skeletons. The skeletal evidence allows us to infer that the borders between the Fremont and Virgin Branch Puebloans and the Fremont and the Kayenta Puebloans were very distinct, and results demonstrated that there was a much higher rate of trauma and pathology among the Fremont.
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Shroff, Gautam. "Correct." In The Intelligent Web. Oxford University Press, 2013. http://dx.doi.org/10.1093/oso/9780199646715.003.0011.

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Last summer I took my family on a driving holiday in the American south-western desert covering many national parks. While driving along some of the long tracts of razor-straight highways, such as between Las Vegas and St George, Utah, I often fought drowsiness, not because of lack of sleep, but from the sheer monotony. A familiar experience for many, no doubt. Hardly any conscious thought is needed during such drives. It must be one’s ‘System’, as per Kahneman, which is most certainly doing what ever work is needed. Nevertheless, sleep is not an option. In spite of all the marvellous features embedded in the modern car, the ability to drive itself is, sadly, still missing. The cruise control button helps a bit, allowing one’s feet torelax as the car’s speed remains on an even keel. But the eyes and mind must remain awake and alert. When, if ever, one wonders, will cars with a ‘drive’ button become as common as those with an automatic transmission? Is driving along a perfectly straight stretch of highway really that difficult? After all, we all know that a modern jetliner can fly on autopilot, allowing even a single pilot to read a novel while ‘flying’ the aircraft on a long transcontinental flight. In fact, the jetliner would fly itself perfectly even if the pilot dozed off for many minutes or even hours. We insist that at least one pilot be awake and alert only for our own peace of mind, so as to be able to adequately respond to any emergency situation that might arise. First of all, the ubiquitous autopilot is itself quite a complex piece of equipment. Even to get a plane to fly perfectly straight along a desired heading at a fixed altitude takes a lot of work. The reason, as you must have guessed, is that nature, in the guise of the air on which our jetliner rides, can be quite unpredictable. Wind speeds and directions change continuously, even ever so slightly, requiring constant adjustments to the plane’s engine power, ailerons, flaps, and rudder. In the absence of such adjustments, our jetliner would most certainly veer off course, or lose or gain speed, even dangerously enough to trigger a powered dive or a stall.
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Reports on the topic "St. George Utah"

1

Lum, P. K., and K. K. Honda. Processed seismic motion records from St. George, Utah earthquake of September 2, 1992, recorded at seismic stations in southern Nevada. Office of Scientific and Technical Information (OSTI), April 1993. http://dx.doi.org/10.2172/10173644.

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