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Journal articles on the topic 'Wyoming, history'

Author: Grafiati

Published: 4 June 2021

Last updated: 31 July 2024

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1

Curtiss, Catherine. "Building Up Wyoming: Depression-Era Federal Projects in Wyoming, 1929–1943." Western Historical Quarterly 45, no. 3 (August 2014): 353.1–353. http://dx.doi.org/10.1093/whq/45.3.353.

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2

Coombs, F. Alan, and Roger L. Williams. "Aven Nelson of Wyoming." Western Historical Quarterly 17, no. 1 (January 1986): 81. http://dx.doi.org/10.2307/968660.

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3

Smith, Melvin T., and Judith Hancock Sandoval. "Historic Ranches of Wyoming." Western Historical Quarterly 18, no. 4 (October 1987): 443. http://dx.doi.org/10.2307/969373.

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4

Guzmán, Gonzalo. "“Things change you know”: Schools as the Architects of the Mexican Race in Depression-Era Wyoming." History of Education Quarterly 61, no. 4 (November 2021): 392–422. http://dx.doi.org/10.1017/heq.2021.37.

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AbstractThis article examines the development of racially segregated Mexican rooms and Mexican schools in Wyoming during the Depression era. Working in concert with New Deal legislation, the segregation of Mexican children—regardless of US citizenship—in Wyoming was not just a matter of social practice and local custom, it became an expression of increased state and federal power that mirrored Jim Crow laws. Wyoming was not alone. The segregation of Mexicans also occurred in neighboring Colorado, Montana, and Nebraska. This article also discusses how, ultimately, public schools and schooling finalized the codification and institutionalization of Mexicans as a race of their own. In Wyoming, schools were the architects of the Mexican race. Furthermore, this unexplored area demonstrates that the segregation of Mexican children was not just a Southwest phenomenon but encompassed almost all of the US West.

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5

Minckley, T. A. "Postglacial vegetation history of southeastern Wyoming, U.S.A." Rocky Mountain Geology 49, no. 1 (March 1, 2014): 61–74. http://dx.doi.org/10.2113/gsrocky.49.1.61.

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6

Lageson, David. "Structural History of the Buffalo Fork Fault and Ancestral Washakie Range, Wyoming." UW National Parks Service Research Station Annual Reports 12 (January 1, 1988): 103–4. http://dx.doi.org/10.13001/uwnpsrc.1988.2713.

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The Buffalo Fork fault is an east-dipping, north-trending reverse\thrust fault which lies along the west side of the Washakie Range in northwestern Wyoming (Love, 1975). This fault was active during the Laramide Orogeny (60-55 million years ago), during which time it uplifted the Ancestral Washakie Range. The purpose of this on-going research project is to determine the displacement vector of the Buffalo Fork fault and to relate this to the regional kinematic pattern of Laramide deformation in northwestern Wyoming. Previous field work by the author (Lageson, 1987) has shown that other Laramide faults in northwestern Wyoming experienced significant components of oblique-slip, depending on their orientation. If a regional pattern of displacement can be determined from several faults, then it may be possible to reconstruct the crustal stress field during the Laramide Orogeny. This study of the Buffalo Fork fault is one step toward this greater goal.

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7

Smith, Duane A., A. Dudley Gardner, and Verla R. Flores. "Forgotten Frontier: A History of Wyoming Coal Mining." American Historical Review 96, no. 1 (February 1991): 268. http://dx.doi.org/10.2307/2164222.

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8

Hewitt, William L., A. Dudley Gardner, and Verla R. Flores. "Forgotten Frontier: A History of Wyoming Coal Mining." Journal of American History 77, no. 3 (December 1990): 1050. http://dx.doi.org/10.2307/2079085.

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9

Cole, Terrence, A. Dudley Gardner, Verla R. Flores, and Phyllis Smith. "Forgotten Frontier: A History of Wyoming Coal Mining." Western Historical Quarterly 22, no. 1 (February 1991): 76. http://dx.doi.org/10.2307/968731.

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10

Mocsary, George A., and Debora A. Person. "A Brief History of Public Carry in Wyoming." Wyoming Law Review 21, no. 2 (January 1, 2021): 341–68. http://dx.doi.org/10.59643/1942-9916.1450.

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11

Harlow, Mary, Lawrence Schmidt, and Paula Munoz. "Digitization of the Grand Teton National Park Herbarium." UW National Parks Service Research Station Annual Reports 29 (January 1, 2005): 27–29. http://dx.doi.org/10.13001/uwnpsrc.2005.3599.

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Examples of digitization projects in the history of science are understood to have lasting consequences for the intellectual history of their fields (Petersen, 2005; Roes 2001). Following this trend, herbarium collections around the world are beginning to be digitized with positive results for their institutions (Begnoche, 2002; Ong, 2002). Librarians, with their long history of making collections accessible, are participating in this trend (Foster, 2005). The University of Wyoming Libraries encourage Librarians to develop and maintain collections in a variety of subjects, and the Libraries are pursuing opportunities in digital collections. This project expands the University of Wyoming Libraries work in the digitizing of a unique collection of plant specimens.

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12

McIntosh, John. "The Second Jurassic Dinosaur Rush." Earth Sciences History 9, no. 1 (January 1, 1990): 22–27. http://dx.doi.org/10.17704/eshi.9.1.6282582245666570.

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The first great North American Dinosaur Rush, begun in 1877 and precipitated by the Marsh-Cope rivalry, was followed by an even greater second Dinosaur Rush, begun just before the turn of the century. The two major principals involved were H. F. Osborn of the American Museum of Natural History in New York and W. J. Holland of the Carnegie Museum in Pittsburgh, but a number of other institutions were also involved, among them the Field Museum in Chicago and parties from the Universities of Wyoming and Kansas. The old Marsh sites at Como Bluff, Wyoming and Garden Park, Colorado were reworked with great success, but many new quarries were also opened, among them, those in the Freezeout Hills and eastern slope of the Big Horn Mountains in Wyoming and the Grand Junction area in Colorado, but most importantly at the two greatest North American Jurassic dinosaur sites: The American Museum Bone Cabin Quarry in Wyoming and the Carnegie Museum Quarry at Dinosaur National Monument in Utah.

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13

Bonner, Robert E. "Buffalo Bill Cody and Wyoming Water Politics." Western Historical Quarterly 33, no. 4 (2002): 432. http://dx.doi.org/10.2307/4144767.

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14

Fairbanks, Robert B., and Robert W. Righter. "The Making of a Town: Wright, Wyoming." Western Historical Quarterly 17, no. 3 (July 1986): 362. http://dx.doi.org/10.2307/968914.

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15

Rankin, Charles E. "Teaching: Opportunity and Limitation for Wyoming Women." Western Historical Quarterly 21, no. 2 (May 1990): 147. http://dx.doi.org/10.2307/969839.

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16

Clark, John G., and Robert W. Righter. "The Making of a Town: Wright, Wyoming." Journal of American History 72, no. 4 (March 1986): 934. http://dx.doi.org/10.2307/1908904.

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17

Hewitt, William L. "The “Cowboyification” of Wyoming Agriculture." Agricultural History 76, no. 2 (April 1, 2002): 481–94. http://dx.doi.org/10.1215/00021482-76.2.481.

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18

Hewitt, William L. "The "Cowboyification" of Wyoming Agriculture." Agricultural History 76, no. 2 (April 2002): 481–94. http://dx.doi.org/10.1525/ah.2002.76.2.481.

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19

McDonald, James C., and Eileen E. Schell. "The Spirit and Influence of the Wyoming Resolution: Looking Back to Look Forward." College English 73, no. 4 (January 1, 2011): 360–78. http://dx.doi.org/10.58680/ce201113514.

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Drawing on their recent interviews with various scholars who were involved, the authors review the history of the highly significant Wyoming Resolution and analyze its subsequent impact on conditions for contingent faculty.

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20

Diggs, D. Teddy, and Deborah Hardy. "Wyoming University: The First 100 Years, 1886-1986." Western Historical Quarterly 18, no. 2 (April 1987): 224. http://dx.doi.org/10.2307/969612.

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21

Chamberlain, Kevin, B. Frost, and Carol Frost. "Precambrian Geological Evolution of the Teton Range, Western Wyoming." UW National Parks Service Research Station Annual Reports 23 (January 1, 1999): 85–87. http://dx.doi.org/10.13001/uwnpsrc.1999.3375.

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The crystalline rocks that form the core of the Teton Range are part of the Wyoming Province, which is one of the oldest portions of North America. Study of the basement of the Tetons, coupled with the results of ongoing research in similar-aged rocks exposed elsewhere in Wyoming, will provide information on how the crust evolved in the early Earth in general and in the Wyoming province in particular. In 1999 the project involved two weeks of fieldwork in Grand Teton National Park and regions to the east, including the Gros Ventre Range, deep canyons of the Buffalo Fork River near Togwotee Pass, and outcrops of basement near Dubois, Wyoming. The main goals of the fieldwork were to complete the sampling of key units in Grand Teton National Park, and to determine whether or not the next nearest outcrops of basement (Gros Ventre, Togwotee Pass and Dubois regions) share the early geologic history preserved in the rocks of Teton National Park. This field work involved four faculty members from UW and a graduate student, who is doing the study as part of her MS thesis. Several months of laboratory analysis at UW have characterized the rocks through thin section, stained slabs, and whole rock geochemical and Nd, Sr, and Ph isotopic methods and produced preliminary U-Pb dates. The principal results from this year 's efforts are that the Teton basement rocks consist of large proportions of juvenile crust, the majority of the rocks formed over a relatively narrow time span from ~2.74 to 2.68 Ga, they were deformed at about 2.67 Ga, and that rocks exposed in the Buffalo Fork River to the east are shallow level equivalents to the deep rocks exposed in the Tetons. Based on these observations and measurements, we hypothesize that the basement rocks of the Tetons formed in an offÂshore, island arc setting between 2.74-2.68 Ga, and they were accreted to the Wyoming province at about 2.67 Ga. Post-tectonic intrusion of distinctive peraluminous granites in both the Teton's (Mt. Owens quartz monzonite) and elsewhere in the Wyoming province at 2.55 Ga strengthens our interpretation of a shared history after 2.67 Ga. If this model for the basement rocks in the Teton's holds up, it will be the first case of crustal growth by lateral accretion for the Archean Wyoming province, and one of the earliest examples of plate tectonics style crustal growth documented from anywhere in the world. Plate tectonic growth has dominated the Earth 's evolution from ~2.5 Ga to the present, but it is unclear whether or not analogous processes operated before 2.5 Ga.

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22

Harrington, Charles D. "A Revision in the Glacial History of Jackson Hole, Wyoming." Mountain Geologist 22, no. 1 (January 1, 1985): 28–32. http://dx.doi.org/10.31582/rmag.mg.22.1.28.

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Timbered Island, a ridge of till in the Jackson Hole lowland, was originally interpreted as an end moraine constructed by a piedmont glacier extending eastward from the Teton Range. Instead, a study of till fabric suggests that Timbered Island was deposited along the western margin of a large ice lobe extending south into the lowland. The marked similarity in the till fabric of Timbered Island and other moraines deposited by the intermontane glacier in the northern part of the lowland suggests that all were formed in a similar manner. Timbered island has survived because its trend was parallel to the direction of meltwater flow during subsequent glacial advances, whereas segments of the moraine normal to meltwater flow would more likely have been buried or removed.

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23

Hlebinsky, Ashley. "Report: The 2019 Kurt Swanson Bucholz Arsenals of History Symposium." Armax: The Journal of Contemporary Arms VII, no. 1 (2021): 95–96. http://dx.doi.org/10.52357/armax85251.

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In 2019, the third annual Kurt Swanson Bucholz Arsenals of History Symposium brought together firearms researchers from around the world in Cody, Wyoming. While the first two symposia had been developed specifically for academic scholars, public historians, and museum professionals, this third symposium set out to include one more group of stakeholders in the conversation: non-traditional researchers. Fittingly, the theme for the 2019 symposium was “Firearms, History & Museums in a Digital Era”.

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24

Frost, C. "The Late Archean history of the Wyoming province as recorded by granitic magmatism in the Wind River Range, Wyoming." Precambrian Research 89, no. 3-4 (June 1998): 145–73. http://dx.doi.org/10.1016/s0301-9268(97)00082-x.

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25

Emmons, David M., and Duane A. Smith. "Rocky Mountain West: Colorado, Wyoming, and Montana, 1859-1915." Western Historical Quarterly 24, no. 1 (February 1993): 94. http://dx.doi.org/10.2307/970032.

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26

Breithaupt, Brent. "Biography of William Harlow Reed: The Story of a Frontier Fossil Collector." Earth Sciences History 9, no. 1 (January 1, 1990): 6–13. http://dx.doi.org/10.17704/eshi.9.1.59584t2t2gl6r04t.

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William Harlow Reed was born in Hartford, Connecticut in 1848. His adventurous spirit led him to the Rocky Mountain West to take positions guiding, hunting game, and fighting Indians. In 1877, while working as a foreman for the Union Pacific Railroad at Como, Wyoming, he accidentally discovered large bones on the nearby ridge. These specimens, reported to O.C. Marsh at Yale University, heralded him into a career in vertebrate paleontology that he would pursue for the next 38 years. Although frustrated by certain aspects of field work and lack of recognition as a field paleontologist, he was a diligent and loyal collector for Marsh. He gave this same dedication in later years to W. C. Knight at the University of Wyoming and W. J. Holland at the Carnegie Museum. Although not formally educated in the sciences, Reed's desire to learn, interest in natural phenomena, and association with the notable paleontologists of his time, allowed him to gain a background in geology and paleontology. After more than 25 years of significant discoveries of dinosaurs, ichthyosaurs, plesiosaurs, pterosaurs, mammals, and cycads in Wyoming, Reed was given the position as curator of the museum and instructor in geology at the University of Wyoming in 1904. He held this position until his death in 1915.

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27

Brown, Sabrina R., Ashley Baysinger, Peter M. Brown, Justin L. Cheek, Jeffrey M. Diez, Christopher M. Gentry, Thomas A. Grant, et al. "Fire History Across Forest Types in the Southern Beartooth Mountains, Wyoming." Tree-Ring Research 76, no. 1 (January 21, 2020): 27. http://dx.doi.org/10.3959/trr2018-11.

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28

Duebendorfer, E. M., and R. S. Houston. "Kinematic history of the Cheyenne belt, Medicine Bow Mountains, southeastern Wyoming." Geology 14, no. 2 (1986): 171. http://dx.doi.org/10.1130/0091-7613(1986)14<171:khotcb>2.0.co;2.

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29

Barrett, Stephen, and Stephen Arno. "Fire History of the Lamar River Drainage, Yellowstone National Park, Wyoming." UW National Parks Service Research Station Annual Reports 13 (January 1, 1989): 169–73. http://dx.doi.org/10.13001/uwnpsrc.1989.2821.

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This study's goal is to document the fire history of the Lamar River drainage, southeast of Soda Butte Creek in the Absaroka Mountains of northeastern Yellowstone National Park (YNP). Elsewhere in YNP investigators have documented very long-interval fire regimes for lodgepole pine forests occurring on rhyolitic derived soils (Romme 1982, Romme and Despain 1989) and short-interval fire regimes for the Douglas-fir/grassland types (Houston 1973). No fire regime information was available for lodgepole pine forests on andesitic derived soils, such as in the Lamar drainage. This study will provide managers with a more complete understanding of YNP natural fire history, and the data will supplement the park's Geographic Information System (GIS) data base. Moreover, most of the study area was severely burned in 1988 and historical tree ring data soon will be lost to attrition of potential sample trees.

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30

Nicholas, Liza. "Wyoming as America: Celebrations, A Museum, and Yale." American Quarterly 54, no. 3 (2002): 437–65. http://dx.doi.org/10.1353/aq.2002.0029.

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31

Tranel, Lisa, Summer Brown, and James Spotila. "Uplift and Denudation of the Teton Range, Wyoming." UW National Parks Service Research Station Annual Reports 31 (January 1, 2008): 145–49. http://dx.doi.org/10.13001/uwnpsrc.2008.3731.

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Our research group is interested in understanding the development of the dramatic relief of the Teton Range. In similar settings worldwide, relief has been examined as product of uplift and denudation. Therefore, we are combining tectonic and geomorphic studies to identify the progression of erosional processes from glacial to interglacial climates and also to refine the uplift history. By integrating these fields, we hope to gain a better understanding of the evolution of the Teton landscape.

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32

Harlow, Mary, and Lawrence Schmidt. "Digitization of the Grand Teton National Park Herbarium, 2006-2007." UW National Parks Service Research Station Annual Reports 30 (January 1, 2006): 42–45. http://dx.doi.org/10.13001/uwnpsrc.2006.3641.

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Examples of digitization projects in the history of science are understood to have lasting consequences for the intellectual history of their fields (Petersen, 2005; Roes 2001). Following this trend, herbarium collections around the world are beginning to be digitized with positive results for their institutions (Begnoche, 2002; Ong, 2002). Librarians, with their long history of making collections accessible, are participating in this trend (Foster, 2005). This project expands the University of Wyoming Libraries work in the digitizing of a unique collection of plant specimens.

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33

Humstone, Mary, Hilery Walker, and Helis Sikk. "Jenny Lake Lodge and Cabins, Determination of Eligibility for the National Register of Historic Places." UW National Parks Service Research Station Annual Reports 32 (January 1, 2009): 27–35. http://dx.doi.org/10.13001/uwnpsrc.2009.3741.

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During summer 2009, the University of Wyoming American Studies Program conducted an intensive historic building and landscape survey of the Jenny Lake Lodge in Grand Teton National Park (Figure 1). The oldest of Grand Teton Lodge Companyâs visitor accommodations, Jenny Lake Lodge has a long and varied history that spans the period from early 20th century dude ranching to contemporary automobile tourism, and that is closely entwined with the history of Grand Teton National Park itself.

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34

Grund, Brigid Sky, and Snehalata V. Huzurbazar. "RADIOCARBON DATING OF TECHNOLOGICAL TRANSITIONS: THE LATE HOLOCENE SHIFT FROM ATLATL TO BOW IN NORTHWESTERN SUBARCTIC CANADA – ERRATUM." American Antiquity 83, no. 1 (January 2018): 184. http://dx.doi.org/10.1017/aaq.2017.72.

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The author affiliations appearing in Grund and Huzurbazar (2017) contain errors. The correct affiliations for the authors are as follows: Brigid Sky Grund ▪ Anthropology Department, University of Wyoming, Department 3431, 1000 E. University Avenue, Laramie, Wyoming 82071-2001.Snehalata V. Huzurbazar ▪ Department of Biostatistics, West Virginia University, P.O. Box 9190, One Medical Center Drive, Morgantown WV 26506, USA.Additionally, the sentence on page 5 reading, “Catastrophic melting events create palimpsest the upper layers of ice (Meulendyk et al. 2012), potentially introducing taphonomic bias” inadvertently omitted two words. The correct sentence is “Catastrophic melting events create a palimpsest in the upper layers of ice, potentially introducing taphonomic bias.”The publisher apologizes for these errors.

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35

Zellman, Mark, Glenn Thackray, Amie Staley, Harrison Colandrea, Nick Patton, and Dan O'Connell. "Geophysical and Geomorphological Analysis of the Teton Fault, Wyoming." UW National Parks Service Research Station Annual Reports 38 (January 1, 2015): 8–15. http://dx.doi.org/10.13001/uwnpsrc.2015.4079.

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This investigation applied geophysical and geomorphological analyses of the Teton Fault to assess its geometry, history, and influences on landscape evolution. This project builds on results from a preceding geophysical study completed one year ago (Thackray et al. 2014), a recent study of fault scarp morphology (Thackray and Staley, in review), and years of previous studies of the fault by many practitioners.

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36

Buhlmann, Arndt L., Patricia Cavell, Ronald A. Burwash, Robert A. Creaser, and Robert W. Luth. "Minette bodies and cognate mica-clinopyroxenite xenoliths from the Milk River area, southern Alberta: records of a complex history of the northernmost part of the Archean Wyoming craton." Canadian Journal of Earth Sciences 37, no. 11 (November 1, 2000): 1629–50. http://dx.doi.org/10.1139/e00-058.

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Minettes exposed in southern Alberta near the Milk River are the northern outliers of the Eocene Sweet Grass Hills igneous complex of the Montana alkalic igneous province. These minettes often contain coarse-grained xenoliths of phlogopite + clinopyroxene ± apatite. The parent magmas of the minettes were generated at pressures [Formula: see text]17 kbar in equilibrium with clinopyroxene + phlogopite ± olivine. Fractional crystallization and mixing provided a spectrum of evolved minettes and cumulates, the latter of which were sampled by subsequent minette magmas as xenoliths. Two xenoliths were dated at 49.0 ± 0.8 Ma and 52 ± 1.7 Ma. The host dyke of the latter xenolith gave an age of 50 ± 0.3 Ma. The minettes and their xenoliths have overlapping values of 87Sr/86Sri, εNdT, 206Pb/204Pb, 207Pb/204Pb, and 208Pb/204Pb, similar to those of alkaline igneous rocks from farther south in the Montana alkalic igneous province. The Sweet Grass Hills lie north of the Great Falls Tectonic Zone, previously interpreted as a Proterozoic suture zone separating the Archean Medicine Hat block from the Archean Wyoming craton to the south. Geochemical data for the Milk River minettes provide evidence for a history of the mantle underneath the Medicine Hat block, similar to that found previously for mantle-derived rocks of the Wyoming craton, including a significant Proterozoic mantle enrichment event. Given this similarity, we suggest that the Wyoming craton extends into southern Alberta, and that the Great Falls Tectonic Zone does not represent a Proterozoic suture of two Archean blocks.

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37

Kipfmueller, Kurt F., and William L. Baker. "A fire history of a subalpine forest in south-eastern Wyoming, USA." Journal of Biogeography 27, no. 1 (January 2000): 71–85. http://dx.doi.org/10.1046/j.1365-2699.2000.00364.x.

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38

Tranel, Lisa, and James Spotila. "Relief History and Coupling of Erosional Processes in the Teton Range, Wyoming." UW National Parks Service Research Station Annual Reports 30 (January 1, 2006): 158–63. http://dx.doi.org/10.13001/uwnpsrc.2006.3683.

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Erosional processes influence topographic relief in mountain landscapes, but the spatial variation between differential processes and influence on tectonic uplift is poorly understood. Deep canyons and adjacent high peaks distinguish the Teton Mountains from nearby ranges, making it an ideal location to study how glacial, fluvial, and hillslope erosion interact to maintain high topographic relief. The purpose of this study is to quantify erosion rates of individual geomorphic processes in this complex system using a variety of techniques to see how each process contributes to landscape evolution in this mountain range.

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39

Alexander, Klint W. "The University of Wyoming College of Law at 100: A Brief History." Wyoming Law Review 21, no. 2 (January 1, 2021): 211–46. http://dx.doi.org/10.59643/1942-9916.1446.

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40

Kikut, Patrick. "University of Wyoming Outdoor Studio Art Class." UW National Parks Service Research Station Annual Reports 35 (January 1, 2012): 172–73. http://dx.doi.org/10.13001/uwnpsrc.2012.3961.

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Since its inception as a Summer Innovative Course in 2000, the Department of Art Summer Outdoor Studio class has been exceptionally grateful for the opportunity to stay and work at the AMK Research Station as part of the three week summer intensive. For art students, the dramatic setting and accommodation are inspiring and it is a highlight of the experience. From the AMK Ranch, students have full access to the Teton NP, Yellowstone NP as well as the National Wildlife Museum in Jackson. Art students also appreciate the interaction with students from different disciplines in the sciences and often those conversations have direct impact on the creative work studentâs produce during their stay. The AMK staff and in particular Professor Hank Harlow have offered us incredible hospitality and generosity. Professor Harlowâs knowledge of the geology, biology, and history of Teton National Park is invaluable to this course. Also, his enthusiasm for art and scientific research is infectious. Our stay at the AMK always culminates in an exhibition of student and faculty creative work, hosted by Hank Harlow, UW NPS Research Station Director.

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41

Foster, Mark S., and Duane A. Smith. "Rocky Mountain West: Colorado, Wyoming, and Montana, 1859-1915." American Historical Review 98, no. 3 (June 1993): 950. http://dx.doi.org/10.2307/2167711.

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42

Knobloch, Frieda. "Creating the Cowboy State: Culture and Underdevelopment in Wyoming since 1867." Western Historical Quarterly 32, no. 2 (2001): 201. http://dx.doi.org/10.2307/3650773.

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43

Humstone, Mary, and Sarah Schill. "AMK Ranch Cultural Landscape Study Grand Teton National Park." UW National Parks Service Research Station Annual Reports 29 (January 1, 2005): 30–38. http://dx.doi.org/10.13001/uwnpsrc.2005.3601.

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During summer, 2005, the University of Wyoming American Studies Program conducted an intensive cultural landscape survey and analysis at the AMK Ranch. Research Scientist Mary Humstone, working with graduate assistant Sarah Schill, documented the historic buildings and landscape features that tell the history of the Sargents Bay peninsula. The team updated the existing National Register of Historic Places nomination to include detailed building and landscape descriptions and a comprehensive history. The following report is excerpted from the National Register nomination.

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44

Thackray, Glenn D., and Mark Zellman. "Paleoseismic study of the Northern Teton Fault, Wyoming." UW National Parks Service Research Station Annual Reports 40 (December 15, 2017): 1–6. http://dx.doi.org/10.13001/uwnpsrc.2017.5539.

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We investigated the earthquake history of the northern portion of the Teton fault by excavating two trenches across a fault scarp near the eastern shore of Jackson Lake, near Steamboat Mountain. We identified the primary stratigraphy of the trenches, logged the trenches in detail, and collected samples for dating analyses. The trenches exposed faulted glacial sediments and overlying hill slope colluvium and alluvial sediments. Interpretation of the trench stratigraphy is ongoing. Samples are currently being analyzed using radiocarbon and luminescence dating techniques to determine the ages of the sediments and constrain the timing of fault rupture. We hosted several visitors at the trench site, including professionals and students, and introduced two interns to the process of fault trenching and documentation. Featured photo from Figure 3 in report.

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45

Kikut, Patrick. "University of Wyoming Outdoor Studio Art Class." UW National Parks Service Research Station Annual Reports 36 (January 1, 2013): 185–86. http://dx.doi.org/10.13001/uwnpsrc.2013.4023.

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Since its inception as a Summer Innovative Course in 2000, the Department of Art Summer Outdoor Studio class has been exceptionally grateful for the opportunity to stay and work at the AMK Research Station as part of the three week summer intensive course. For art students, the dramatic setting and accommodation are inspiring and it is a highlight of the experience. From the AMK Ranch, students have full access to Grand Teton NP, Yellowstone NP as well as the National Wildlife Museum in Jackson. Last year we scheduled a docent tour of the Wildlife museum and attended an informative lecture on Native Art in the National Parks at the Coulter Bay Visitors Center. Art students appreciate the interaction with student researchers from different science disciplines. Often those conversations have direct impact on the creative work students produce during their stay. The AMK staff and, in particular, Professor Hank Harlow have offered us incredible hospitality and generosity. Professor Harlowâs knowledge of the geology, biology, and history of Grand Teton National Park is invaluable to this course. Also, his enthusiasm for art and scientific research is infectious. Our stay at the AMK always culminates in an exhibition of student and faculty creative work, hosted by Hank Harlow, UW NPS Research Station Director.

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Bowers, Nancy E., and Kevin R. Chamberlain. "Precambrian history of the eastern Ferris Mountains and Bear Mountain, south-central Wyoming Province." Canadian Journal of Earth Sciences 43, no. 10 (October 1, 2006): 1467–87. http://dx.doi.org/10.1139/e06-091.

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The eastern Ferris Mountains and Bear Mountain area of south-central Wyoming contain a complex assemblage of Archean and Proterozoic rock units, including a metasedimentary and metavolcanic supracrustal sequence named the Spanish Mine metamorphic suite, three granitic plutons (Turkey Creek, Ferris Mountains, Bear Mountain), and at least three sets of mafic dikes. The Spanish Mine metamorphic suite was deposited, intruded by mafic sills and (or) dikes, and underwent amphibolite-grade metamorphism and folding just prior to, or synkinematic with, the intrusion of the Turkey Creek metaplutonic suite, U–Pb dated at 2733.5 ± 2 Ma. A second set of mafic dikes intruded the Turkey Creek metaplutonic suite prior to mylonitic shearing and late-stage folding along the Miners Canyon shear zone. These events were followed by intrusion of the Ferris Mountains plutonic suite at ~2717 Ma. The emplacement of the yet undated granite of Bear Mountain records the last phase of Neoarchean magmatism. The timing of magmatism and deformation support a model that the Ferris Mountains basement rocks formed in an arc terrane distinct from the older Wyoming craton and were accreted to the province in the Neoarchean. Intrusion of a third mafic dike set is dated at 2113 ± 15 Ma and may date the silicified, epidote-rich zones that crosscut all of the Archean rock units. Lead isotopic compositions of galena within the Spanish Mine metamorphic suite indicate additional Proterozoic activity and mineralization.

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Morris, Christo, Thomas A. Monaco, and Craig W. Rigby. "Variable Impacts of Imazapic Rate on Downy Brome (Bromus tectorum) and Seeded Species in Two Rangeland Communities." Invasive Plant Science and Management 2, no. 2 (April 2009): 110–19. http://dx.doi.org/10.1614/ipsm-08-104.1.

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AbstractThe herbicide imazapic is registered for use on rangelands and provides effective short-term control of certain invasive annual grasses. However, details about optimal application rates for downy brome and susceptibility of simultaneously seeded species are lacking. Thus, we investigated downy brome and seeded species responses to variable rates of imazapic (0, 35, 70, 105, and 140 g ai/ha) in two plant communities (salt desert shrub and Wyoming big sagebrush). In autumn 2003, plots were treated with imazapic and seeded with one of five perennial plant materials (Siberian wheatgrass [‘Vavilov’ and the experimental source Kazak]; prostrate kochia [‘Immigrant’ and the experimental source 6X], and Russian wildrye [‘Bozoisky II’]). Downy brome cover and seeded species establishment were evaluated in spring 2004 and 2006. Downy brome cover in 2004 decreased with increasing imazapic rate at both sites, although more so at the Wyoming big sagebrush site. In 2006, no difference in downy brome cover existed among herbicide rates at the Wyoming big sagebrush site. At the salt desert shrub site, the high rate of imazapic reduced downy brome cover by about 25% compared to untreated plots. ‘Vavilov’ Siberian wheatgrass was the only seeded species with lower downy brome cover in 2006 than 2004. Seeded species establishment increased with imazapic rate in the salt desert shrub community, but in the Wyoming big sagebrush community it peaked at intermediate rates and declined at higher rates. Variation in downy brome control and seeded species establishment might have been associated with differences in precipitation, soil organic matter, and disturbance history between sites. Overall, imazapic was useful for helping establish desirable perennial species, but unless downy brome is reduced below a critical threshold, favorable precipitation can return sites to pretreatment levels within two years.

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Humstone, Mary. "Elk Ranch Determination of Eligibility for the National Register of Historic Places." UW National Parks Service Research Station Annual Reports 33 (January 1, 2011): 37–46. http://dx.doi.org/10.13001/uwnpsrc.2011.3779.

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During summer 2010, the University of Wyoming American Studies Program conducted an intensive cultural landscape survey and historical analysis of the Elk Ranch in Grand Teton National Park. Led by Research Scientist Mary Humstone, students documented the ranch landscape and remaining buildings. They conducted research in local archives to uncover the history of the ranch and determine its significance in the history of Jackson Hole and Grand Teton National Park. The team determined that the property is eligible for the National Register of Historic Places, with significance in agriculture and conservation.

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Young, Michael K. "Mobility of brown trout in south-central Wyoming streams." Canadian Journal of Zoology 72, no. 12 (December 1, 1994): 2078–83. http://dx.doi.org/10.1139/z94-278.

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Stream-resident brown trout (Salmo trutta) have often been considered to have small home ranges. To test this hypothesis, positions of adult brown trout in two streams were monitored from mid-June to early December 1991 and from late September 1992 to early June 1993 by using radiotelemetry. Thirty-seven of the 54 brown trout that were relocated at least once had home ranges greater than 50 m, trout larger than 340 mm moved more than did smaller brown trout, and movement of all fish tended to be greater in autumn. Different movement patterns of large and small fish imply the existence of two life-history strategies.

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Matson, Roger, and Jack Magathan. "Hanna of Wyoming—The Rockies’ Deepest Basin." Mountain Geologist 54, no. 4 (November 2017): 265–93. http://dx.doi.org/10.31582/rmag.mg.54.4.265.

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The Hanna Basin is one of the world’s deeper intracratonic depressions. It contains exceptionally thick sequences of mature, hydrocarbon-rich Paleozoic through Eocene rocks and has the requisite structural and depositional history to be a significant petroleum province. The Tertiary Hanna and Ferris formations consist of up to 20,000 ft of organic-rich lacustrine shale, shaly mudstone, coal, and fluvial sandstone. The Upper Cretaceous Medicine Bow, Lewis, and Mesaverde formations consist of up to 10,000 ft of marine and nonmarine organic-rich shale enclosing multiple stacked beds of hydrocarbon-bearing sandstone. Significant shows of oil and gas in Upper Cretaceous and Paleocene rocks occur in the basin. Structural prospecting should be most fruitful around the edges where Laramide flank structures were created by out-of-the-basin thrust faults resulting from deformation of the basin’s unique 50-mile wide by 9-mile deep sediment package. Strata along the northern margin of the basin were compressed into conventional anticlinal folds by southward forces emanating from Emigrant Trail-Granite Mountains overthrusting. Oil and gas from Pennsylvanian to Upper Cretaceous aged rocks have been found in such structures near the Hanna Basin. Only seven wells have successfully probed the deeper part of the Hanna Basin (not including Anadarko’s #172 Durante lost hole, Sec. 17, T22N, R82W, lost in 2004, hopelessly stuck at 19,700 ft, unlogged and untested). Two of these wells tested gas at commercial rates from Upper Cretaceous rocks at depths of 10,000 to 12,000 ft. Sparse drilling along the Hanna Basin’s flanks has also revealed structures from 3,000 to 7,000 feet deep which yielded significant shows of oil and gas.

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