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Journal articles on the topic 'Absaroka Mountains'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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1

Malone, David, John Craddock, Jessica Welch, and Brady Foreman. "Detrital Zircon U-Pb geochronology and provenance of the Eocene Willwood Formation, Northern Absaroka Basin, Wyoming." Mountain Geologist 54, no. 2 (2017): 104–24. http://dx.doi.org/10.31582/rmag.mg.54.2.104.

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We report the results of U-Pb ages from detrital zircon populations in the lower Eocene synorogenic Willwood Formation in the northern Absaroka Basin, Wyoming. Zircons (n=229) were extracted from three sandstone beds and one ash layer in the Willwood Formation at the base of Jim Mountain in the North Fork Shoshone River Valley. K-S statistical analysis indicates that the three sandstones, which were sampled from the base, middle, and top of the formation, have identical age spectra, indicating that the sandstone provenance remained the same during the duration of Willwood deposition. The zirco

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2

Frison, George C., R. L. Andrews, J. M. Adovasio, R. C. Carlisle, and Robert Edgar. "A Late Paleoindian Animal Trapping Net from Northern Wyoming." American Antiquity 51, no. 2 (1986): 352–61. http://dx.doi.org/10.2307/279947.

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A net made of juniper (Juniperus sp.) bark cordage and designed for capturing animals the size of deer or mountain sheep has been radiocarbon dated to late Paleoindian times. It was recovered in the Absaroka Mountains of north-central Wyoming and provides insight into prehistoric animal procurement strategies that did not require the use of stone artifacts.

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3

Swenson, Jon E. "Compensatory Reproduction in an Introduced Mountain Goat Population in the Absaroka Mountains, Montana." Journal of Wildlife Management 49, no. 4 (1985): 837. http://dx.doi.org/10.2307/3801355.

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4

Eakin, Daniel. "Evidence for Shoshonean Bighorn Sheep Trapping and Early Historic Occupation in the Absaroka Mountains of Northwest Wyoming." UW National Parks Service Research Station Annual Reports 29 (January 1, 2005): 74–86. http://dx.doi.org/10.13001/uwnpsrc.2005.3617.

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This report briefly summarizes 2004-2005 archaeological investigations at five sites located on Boulder Ridge in northwest Wyoming's Absaroka Range. Archaeological investigations on Boulder Ridge began in the 1970s when Frison (1978:258-262) documented site 48PA781, the Boulder Ridge Animal Trap (Figure 1C). In July 2003, school documented several additional sites on Boulder Ridge, including 48PA2646, a previously unrecorded feature interpreted as remains of a bighorn sheep trap (Finley and Finley 2004).

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5

Ackert, jr., Robert P. "A rock glacier/debris‐covered glacier system at galena creek, absaroka mountains, wyoming." Geografiska Annaler: Series A, Physical Geography 80, no. 3-4 (1998): 267–76. http://dx.doi.org/10.1111/j.0435-3676.1998.00042.x.

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6

KUDO, A. M., and DAVID E. BROXTON. "High-potassium intrusive rocks of the Crandall ring-dike complex, Absaroka Mountains, Wyoming." Geological Society of America Bulletin 96, no. 4 (1985): 522. http://dx.doi.org/10.1130/0016-7606(1985)96<522:hirotc>2.0.co;2.

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7

Klaus, Marion, Robert E. Moore, and Ernest Vyse. "Microgeographic variation in allozymes and mitochondrial DNA of Microtus richardsoni, the water vole, in the Beartooth Mountains of Montana and Wyoming, U.S.A." Canadian Journal of Zoology 79, no. 7 (2001): 1286–95. http://dx.doi.org/10.1139/z01-082.

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Microtus richardsoni, the water vole, is listed as a sensitive species within region 2 of the USDA Forest Service. Because it is a sensitive species, the water vole's ability to disperse becomes an important management concern in terms of its population viability. Both allozyme and mitochondrial DNA analyses were used to study microgeographic population structure within a group of populations from four adjacent watersheds of the Beartooth Mountains of Montana and Wyoming. Of 31 protein loci examined, only ADH, EST-1, and SOD-1 were polymorphic. ADH and EST-1 were in HardyWeinberg equilibrium,

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8

Kruse, Carter G., Wayne A. Hubert, and Frank J. Rahel. "Geomorphic Influences on the Distribution of Yellowstone Cutthroat Trout in the Absaroka Mountains, Wyoming." Transactions of the American Fisheries Society 126, no. 3 (1997): 418–27. http://dx.doi.org/10.1577/1548-8659(1997)126<0418:giotdo>2.3.co;2.

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9

Harlan, Stephen S., Lawrence W. Snee, and John W. Geissman. "40Ar/39Ar geochronology and paleomagnetism of Independence volcano, Absaroka Volcanic Supergroup, Beartooth Mountains, Montana." Canadian Journal of Earth Sciences 33, no. 12 (1996): 1648–54. http://dx.doi.org/10.1139/e96-125.

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Independence volcano is a major volcanic complex in the lower part of the Absaroka Volcanic Supergroup (AVS) of Montana and Wyoming. Recently reported Rb–Sr mineral dates from the complex give apparent ages of 91 and 84 Ma, whereas field relationships and the physical and compositional similarity of the rocks with other dated parts of the AVS indicate an Early to Middle Eocene age for eruption and deposition. To resolve the conflict between age assignments based on stratigraphic correlations and Rb–Sr dates, we report new paleomagnetic data and 40Ar/39Ar dates for Independence volcano. Paleoma

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10

Reckin, Rachel, and Lawrence C. Todd. "Social-boundary defence, mountain people and obsidian in the Absaroka and Beartooth mountains of the Greater Yellowstone Ecosystem, USA." Hunter Gatherer Research 3, no. 3 (2019): 429–58. http://dx.doi.org/10.3828/hgr.2017.21.

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11

Reider, Richard G., Gary A. Huckleberry, and George C. Frison. "Soil Evidence for Postglacial Forest-Grassland Fluctuation in the Absaroka Mountains of Northwestern Wyoming, U.S.A." Arctic and Alpine Research 20, no. 2 (1988): 188. http://dx.doi.org/10.2307/1551497.

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12

Nyblade, Andrew P., Peter N. Shive, and Kevin P. Furlong. "Rapid secular variation recorded in thick Eocene flows from the Absaroka Mountains of northwest Wyoming." Earth and Planetary Science Letters 81, no. 4 (1987): 419–24. http://dx.doi.org/10.1016/0012-821x(87)90128-2.

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13

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 m

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14

Klutsch, Jennifer G., Betsy A. Goodrich, and William R. Jacobi. "Post-fire regeneration dynamics in whitebark pine (Pinus albicaulis) forests in Wind River and Absaroka Mountains, Wyoming, USA." Journal of Forestry Research 26, no. 3 (2015): 719–33. http://dx.doi.org/10.1007/s11676-015-0064-6.

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15

Scheiber, Laura, and Amanda Burtt. "Archaeology and Social Geography in the Sunlight Basin, Wyoming." UW National Parks Service Research Station Annual Reports 37 (January 1, 2014): 85–96. http://dx.doi.org/10.13001/uwnpsrc.2014.4053.

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Painter Cave (48PA3288) is a dry rockshelter in the foothills of the Absaroka Mountains of northwestern Wyoming that has deeply stratified deposits. Archaeological materials were disturbed several decades ago by looters, who reportedly took a number of perishable Native American artifacts including moccasins and a cradle board, as well as numerous other unidentified objects. Preliminary assessment by Shoshone National Forest Service personnel in 2011 suggested that the site might still be partially intact. Indiana Universityâs Bighorn Archaeology project conducted a pilot study at Painter Ca

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16

Barrett, SW. "Fire Regimes on Andesitic Mountain Terrain in Northeastern Yellowstone-National-Park, Wyoming." International Journal of Wildland Fire 4, no. 2 (1994): 65. http://dx.doi.org/10.1071/wf9940065.

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A fire history investigation was conducted for three forest community types in the Absaroka Mountains of Yellowstone National Park, Wyoming. Master fire chronologies were based on fire-initiated age classes and tree fire scars. The area's major forest type, lodgepole pine (Pinus contorta Dougl. var. latifolia) ecosystems, revealed a predominant pattern of stand replacing fires with a 200 year mean interval-nearly half the length estimated in previous studies of lodgepole pine on less productive subalpine plateaus in YNP. High elevation whitebark pine (P. albicaulis Engelm.) forests had primari

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17

Gettings, M. E. "Multifractal magnetic susceptibility distribution models of hydrothermally altered rocks in the Needle Creek Igneous Center of the Absaroka Mountains, Wyoming." Nonlinear Processes in Geophysics 12, no. 5 (2005): 587–601. http://dx.doi.org/10.5194/npg-12-587-2005.

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Abstract. Magnetic susceptibility was measured for 700 samples of drill core from thirteen drill holes in the porphyry copper-molybdenum deposit of the Stinkingwater mining district in the Absaroka Mountains, Wyoming. The magnetic susceptibility measurements, chemical analyses, and alteration class provided a database for study of magnetic susceptibility in these altered rocks. The distribution of the magnetic susceptibilities for all samples is multi-modal, with overlapping peaked distributions for samples in the propylitic and phyllic alteration class, a tail of higher susceptibilities for p

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18

MEEN, JAMES K., and DAVID H. EGGLER. "Petrology and geochemistry of the Cretaceous Independence volcanic suite, Absaroka Mountains, Montana: Clues to the composition of the Archean sub-Montanan mantle." Geological Society of America Bulletin 98, no. 2 (1987): 238. http://dx.doi.org/10.1130/0016-7606(1987)98<238:pagotc>2.0.co;2.

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19

Anderson, Ian, David H. Malone, and John Craddock. "Preliminary detrital zircon U-Pb Geochronology of the Wasatch Formation, Powder River Basin, Wyoming." Mountain Geologist 56, no. 3 (2019): 247–66. http://dx.doi.org/10.31582/rmag.mg.56.3.247.

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The lower Eocene Wasatch Formation is more than 1500 m thick in the Powder River Basin of Wyoming. The Wasatch is a Laramide synorgenic deposit that consists of paludal and lacustrine mudstone, fluvial sandstone, and coal. U-Pb geochronologic data on detrital zircons were gathered for a sandstone unit in the middle part of the succession. The Wasatch was collected along Interstate 90 just west of the Powder River, which is about 50 km east of the Bighorn Mountain front. The sandstone is lenticular in geometry and consists of arkosic arenite and wacke. The detrital zircon age spectrum ranged (n

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20

Gray, S., S. Jackson, K. Taylor, C. Palmer, and C. Fastie. "Tree-Ring Based Reconstructions of Paleo-Precipitation Regimes in the Eastern Yellowstone Region." UW National Parks Service Research Station Annual Reports 24 (January 1, 2000): 144–48. http://dx.doi.org/10.13001/uwnpsrc.2000.3431.

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There are few other regions where the influence of climate on basic ecosystem attributes has been as well documented as the Greater Yellowstone Ecosystem (GYE). Research has shown that elk, bison, and grizzly bear populations in the GYE are tightly linked to annual climate variation (Meagher 1976, Picton 1978). Authors have shown that the distribution of vegetation types in Grand Teton and Yellowstone National Parks is influenced by the seasonality of precipitation (Despain 1987, 1990). Natural disturbances, especially fires and insect outbreaks, are also known to coincide with specific climat

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21

Lindsay, C. R., and T. C. Feeley. "Magmagenesis at the Eocene Electric Peak–Sepulcher Mountain complex, Absaroka Volcanic Province, USA." Lithos 67, no. 1-2 (2003): 53–76. http://dx.doi.org/10.1016/s0024-4937(02)00252-9.

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22

Kuhn, Bernadette, and Joe Stevens. "Lichen Species Diversity Yellowstone National Park Gloria Site." UW National Parks Service Research Station Annual Reports 34 (January 1, 2011): 169–74. http://dx.doi.org/10.13001/uwnpsrc.2011.3891.

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Alpine ecosystems are important monitoring targets for examining climate-induced changes of vegetation cover, species composition, and species migration. In 2011, we installed alpine monitoring sites in Yellowstone National Park for the Rocky Mountain Inventory and Monitoring Network. The site was established using the protocol developed by the Global Observation Research Initiative in Alpine Environments [GLORIA] (Grabher et al. 2000). Here, we present a summary of the lichen species diversity documented within these monitoring plots, as well as the summary of field work completed for the GLO

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23

Lillegraven, Jason A. "Stratigraphic relationships along the monoclinal eastern base of Bald Ridge and northwestern edge of Wyoming’s Bighorn Basin, U.S.A." Rocky Mountain Geology 54, no. 2 (2019): 47–95. http://dx.doi.org/10.24872/rmgjournal.54.2.47.

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ABSTRACT This geologic study is focused on a less than 5 square-mile (ca. 13 km2) tract of public land in northwestern Wyoming, 8 miles (12.9 km) south-southwest of the small town of Clark in Park County. The study area is south of Clarks Fork of Yellowstone River along the eastern base of the topographic feature called Bald Ridge, also known structurally as Dead Indian monocline. Since the Middle Eocene, the study area has been along the northwestern margin of the Bighorn Basin. Prior to that time, the study area existed near the west–east center of the basin. Bald Ridge became elevated late

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24

Peter N. Shive, Kent A. Sundell. "Magnetostratigraphic Correlation of Eocene Rocks from the Absaroka Mountains, Wyoming: ABSTRACT." AAPG Bulletin 70 (1986). http://dx.doi.org/10.1306/94886907-1704-11d7-8645000102c1865d.

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