Relevant bibliographies by topics / Ruby Mountains

Academic literature on the topic 'Ruby Mountains'

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Published: 10 December 2022
Last updated: 29 January 2023

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Journal articles on the topic "Ruby Mountains"

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Rickart, Eric A., Rebecca J. Rowe, Shannen L. Robson, Lois F. Alexander, and Duke S. Rogers. "Shrews of the Ruby Mountains, Northeastern Nevada." Southwestern Naturalist 56, no. 1 (March 2011): 95–102. http://dx.doi.org/10.1894/rts-08.1.

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Kissin, Alexander J. "Ruby and Sapphire from the Southern Ural Mountains, Russia." Gems & Gemology 30, no. 4 (January 1, 1994): 243–52. http://dx.doi.org/10.5741/gems.30.4.243.

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Wanket, James A., David B. Wahl, and Jennifer E. Kusler. "Preliminary pollen record from Echo Lake, Ruby Mountains, Nevada." Quaternary International 387 (November 2015): 149. http://dx.doi.org/10.1016/j.quaint.2015.01.185.

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Schaefer, Vincent J. "Is something happening to our supply of Supercooled Clouds?" Journal of Weather Modification 10, no. 1 (April 3, 2018): 1–3. http://dx.doi.org/10.54782/jwm.v10i1.580.

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On October 19, 1977, on a flight from Albany, New York to Reno, Nevada, I spent most of the trip on the sunny side of the jet aircraft watching the world go by.... The flight route from Chicago to Reno went past Cheyenne, Elk Mountain, Flaming Gorge Reservoir, just north of the Bingham Copper Pit, and then across the Bonneville Salt Flats into Nevada. Much of the region west of Chicago was cloudless but shortly afterwe crossed the Nevada state line,the first batch of cumulus clouds appeared as we approached the Ruby Mountains. Proceeding west southwest, convective clouds increased in concentration until they obscured the ground. The sky above our plane was cloudless and therewere no middle clouds.....
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Dewez, Véronique, and Marie-Anne Geurts. "Analyses minéralogiques multivariées de sédiments du Wisconsinien supérieur au sud-ouest du Yukon." Canadian Journal of Earth Sciences 33, no. 1 (January 1, 1996): 42–51. http://dx.doi.org/10.1139/e96-005.

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For this study, 84 samples of glacial and juxtaglacial sediments were collected in valleys of the Ruby Range and Aishihik Basin (southwestern Yukon). Analyses were conducted to quantify the heavy minerals in the sand fraction and to assess the petrography of the gravel fraction. A cluster analysis performed on the heavy mineral results showed five groups of deposits, three of which are related to local glaciers inside the Ruby Range, the other two being related to regional ice lobes of Kluane and Aishihik, respectively. The three groups of local sediments correspond to the three lithologies of the Ruby Range, i.e., the granitic batholith, the schists, and the alaskite. The sediments from the regional ice lobes are characterized by highly diversified mineralogy and petrography and the relative abundance of minerals from the Saint Elias Mountains, the main source of the ice lobes. A correspondance factor analysis performed on the heavy mineral results organizes samples and minerals into a triangular cloud, the three vertices corresponding to biotite, carbonate, and titanite–garnet. These are the key elements of local glaciers, Kluane ice lobe, and Aishihik ice lobe, respectively. Finally, the study shows the extension of Kluane lobe in one valley of the Ruby Range, the ice flow pattern in another valley, as well as a transfluence from Kluane lobe inside the Range.
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Colgan, Joseph P., Keith A. Howard, Robert J. Fleck, and Joseph L. Wooden. "Rapid middle Miocene extension and unroofing of the southern Ruby Mountains, Nevada." Tectonics 29, no. 6 (December 2010): n/a. http://dx.doi.org/10.1029/2009tc002655.

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Thompson, Robert S. "Late Quaternary Environments in Ruby Valley, Nevada." Quaternary Research 37, no. 1 (January 1992): 1–15. http://dx.doi.org/10.1016/0033-5894(92)90002-z.

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AbstractPalynological data from sediment cores from the Ruby Marshes provide a record of environmental and climatic changes over the last 40,000 yr. The modern marsh waters are fresh, but no deeper than ∼3 m. A shallow saline lake occupied this basin during the middle Wisconsin, followed by fresh and perhaps deep waters by 18,000 to 15,000 yr B.P. No sediments were recovered for the period between 15,000 and 11,000 yr B.P., possibly due to lake desiccation. By 10,800 yr B.P. a fresh-water lake was again present, and deeper-than-modern conditions lasted until 6800 yr B.P. The middle Holocene was characterized by very shallow water, and perhaps complete desiccation. The marsh system deepened after 4700 yr B.P., and fresh-water conditions persisted until modern times. Vegetation changes in Ruby Valley were more gradual than those seen in the paleolimno-logical record. Sagebrush steppe was more widespread than at present through the late Pleistocene and early Holocene, giving way somewhat to expanded shadscale vegetation between 8500 and 6800 yr B.P. Shadscale steppe contracted by 4000 yr B.P., but had greater than modern coverage until 1000 to 500 yr ago. Pinyon-juniper woodland was established in the southern Ruby Mountains by 4700 yr B.P.
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MacCready, Tyler, Arthur W. Snoke, James E. Wright, and Keith A. Howard. "Mid-crustal flow during Tertiary extension in the Ruby Mountains core complex, Nevada." Geological Society of America Bulletin 109, no. 12 (December 1997): 1576–94. http://dx.doi.org/10.1130/0016-7606(1997)109<1576:mcfdte>2.3.co;2.

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Wahl, David, Scott Starratt, Lysanna Anderson, Jennifer Kusler, Christopher Fuller, Elmira Wan, and Holly Olson. "A 7700 year record of paleoenvironmental change from Favre Lake, Ruby Mountains, Nevada." Quaternary International 387 (November 2015): 148–49. http://dx.doi.org/10.1016/j.quaint.2015.01.184.

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Lee, Sang-Yun, Calvin G. Barnes, Arthur W. Snoke, Keith A. Howard, and Carol D. Frost. "Petrogenesis of Mesozoic, Peraluminous Granites in the Lamoille Canyon Area, Ruby Mountains, Nevada, USA." Journal of Petrology 44, no. 4 (April 1, 2003): 713–32. http://dx.doi.org/10.1093/petrology/44.4.713.

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Abstract Two groups of closely associated, peraluminous, two-mica granitic gneiss were identified in the area. The older, sparsely distributed unit is equigranular (EG) with initial εNd ∼ − 8·8 and initial 87Sr/86Sr ∼0·7098. Its age is uncertain. The younger unit is Late Cretaceous (∼80 Ma), pegmatitic, and sillimanite-bearing (KPG), with εNd from −15·8 to −17·3 and initial 87Sr/86Sr from 0·7157 to 0·7198. The concentrations of Fe, Mg, Na, Ca, Sr, V, Zr, Zn and Hf are higher, and K, Rb and Th are lower in the EG. Major- and trace-element models indicate that the KPG was derived by muscovite dehydration melting (&lt;35 km depth) of Neoproterozoic metapelitic rocks that are widespread in the eastern Great Basin. The models are broadly consistent with anatexis of crust tectonically thickened during the Sevier orogeny; no mantle mass or heat contribution was necessary. As such, this unit represents one crustal end-member of regional Late Cretaceous peraluminous granites. The EG was produced by biotite dehydration melting at greater depths, with garnet stable in the residue. The source of the EG was probably Paleoproterozoic metagraywacke. Because EG magmatism probably pre-dated Late Cretaceous crustal thickening, it required heat input from the mantle or from mantle-derived magma.
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Dissertations / Theses on the topic "Ruby Mountains"

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Nelson, Jennifer. "Geology, Geochemistry, and Geochronology of the Nathrop Volcanics: A Comprehensive Look at the History and Formation of Ruby and Sugarloaf Mountains." Bowling Green State University / OhioLINK, 2021. http://rave.ohiolink.edu/etdc/view?acc_num=bgsu1626900507074039.

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Satarugsa, Peangta 1960. "Cenozoic tectonic evolution of the Ruby Mountains metamorphic core complex and adjacent basins: Results from normal-incidence and wide-angle multicomponent seismic data." Diss., The University of Arizona, 1997. http://hdl.handle.net/10150/282541.

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Seismic studies in the area of the Ruby Mountains metamorphic core complex and adjacent basins of northeast Nevada provide new evidence for Cenozoic tectonic evolution of the Ruby Mountains. Results from interpretation of industry seismic data show that (1) asymmetric basins flanking the Ruby Mountains were created by normal faults beginning in the late Eocene-early Oligocene; (2) the metamorphic core complex detachment fault system was cut by the normal fault system; and (3) total subsidences of Huntington and Lamoille basins, and Ruby basins are ∼4.5 and ∼5.0 km. Analysis of crustal-scale 3-component normal-incidence to wide-angle seismic data shows that (1) the crust along the eastern flank of the Ruby Mountains can be divided into three layers corresponding to the upper, middle and lower crust; (2) upper crustal rocks likely consist of metaquartzite, schist, granite gneiss, and granite-granodiorite with P-wave velocities (Vp) of 5.80-6.25 km/s, S-wave velocities (Vs) of 3.20-3.72 km/s, Poisson's ratios (sigma) of 0.22-0.25, and anisotropy of 0.6-2.5%; (3) possible middle crustal rocks are paragranulite, felsic granulite, felsic amphibolite gneiss, granite-granodiorite, and mica-quartz schist with Vp of 6.35-6.45 km/s, Vs of 3.70-3.75 km/s, and σ of 0.24; (4) lower crustal rocks most likely consist of granulite- rather than amphibolite-facies rocks with Vp of 6.60-6.80 km/s, Vs of 3.85-3.92 km/s, σ of 0.24-0.25, and anisotropy of less than 3%; (4) depth to the Moho varies irregularly between 30.5 and 33.5. Interpretation of these results suggests that (1) Cenozoic extension of the Ruby Mountains and adjacent basins began by late Eocene-early Oligocene; (2) depth to Moho does not reflect local surface relief on the eastern flank of the Ruby Mountains and adjacent basin; (3) fluid-filled fractures and mafic large-scale underplating are unlikely in the lower crust; (4) the present seismic velocities of highly extended core complex crust and normally extended Basin and Range crust are similar; and (5) orientations of fast shear waves near the surface and in the upper crust are parallel to sub-parallel to the regional maximum horizontal compressive stress in the Nevada part of the Basin and Range province.
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Knight, John A. II. "Quantifying Climate Change Over the Early Cretaceous Ruby Ranch Member of the Cedar Mountain Formation, East-Central Utah." Thesis, The University of Texas at San Antonio, 2018. http://pqdtopen.proquest.com/#viewpdf?dispub=10813710.

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The age of the Ruby Ranch Member (RRM) of the Cedar Mountain Formation in East-Central Utah was recently constrained using carbon isotope chemostratigraphy to span known excursions associated with the late Aptian. The RRM is characterized by calcrete horizons that are thought to occur across the C10 carbon isotope excursion. Along with carbonate stable isotope analyses and the region’s paleo-position in a depositional basin on the leeward rain shadow of the Sevier Orogenic belt, this interval is hypothesized to coincide with an aridification event. Our research objective is to quantify the extent of this aridity using clumped isotope paleothermometry (n = 7) and paleoprecipitation proxies (n = 51) for samples collected across the C10 chemostratigraphic interval. Two weathering indices, CIA-K and CALMAG, were applied to data obtained using X-ray fluorescence spectrometry. Using these proxies, we determined mean annual precipitation across the RRM at its type section. Precipitation values ( n = 27) obtained through CIA-K for identified paleosol horizons ranged between 795 and 1275 mm/year, and through CALMAG ranged between 735 and 1042 mm/year. Precipitation values decreased through the C10 interval which may indicate increased aridity. Clumped isotopes provided ?47 values ranging from 0.647 to 0.693‰. Paleotemperature measurements (n = 4) from accepted carbonate samples were between 27.9 and 46.3 °C. Isotopic compositions of water calculated from carbonates ranged between -4.4‰ and -1.9‰ VSMOW. Precipitation values and temperatures were not lowest during the C10 interval. Temperatures peaked at the end of the C10 interval and decreased afterward, indicating a potential for cooler, more arid conditions. These results suggest that carbon cycle changes during the mid-Cretaceous may have influenced paleoclimate conditions experienced in terrestrial settings.

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Emery, William Daniel. "Geology and Eruptive History of the Late Oligocene Nathrop Volcanics, Central Colorado Volcanic Field." Bowling Green State University / OhioLINK, 2011. http://rave.ohiolink.edu/etdc/view?acc_num=bgsu1299733477.

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Sorensen, Amanda Elizabeth MacKay. "Geologic mapping of exhumed, mid-Cretaceous paleochannel complexes near Castle Dale, Emery County, Utah: On the correlative relationship between the Dakota Sandstone and the Mussentuchit Member of the Cedar Mountain Formation." BYU ScholarsArchive, 2011. https://scholarsarchive.byu.edu/etd/2727.

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Numerous well-preserved, exhumed paleochannels in the Morrison, Cedar Mountain and Dakota Sandstone formations are exposed east of Castle Dale, Utah. These channels consist primarily of point bar complexes and scattered, low sinuosity channels. To determine the vertical and lateral relationships of these channels within the Cedar Mountain and Dakota Sandstone formations, a 1:24,000 scale geologic map covering ~140 km2 was created showing the fluvial sandstones. In the study area the Cedar Mountain Formation consists, from bottom to top, of 2.5-10 m of Buckhorn Conglomerate Member equivalent units, ~80 m of the Ruby Ranch Member, and ~30 m of the Mussentuchit Member. The Dakota Sandstone consists of conglomeratic to sandy, meandering channel fills within the Mussentuchit Member. The Ruby Ranch-Mussentuchit member contact is diagnosed as the top of a laterally extensive, ~10 meter thick, maroon paleosol with calcrete horizons and root traces. When deeply weathered the contact is discernable as a shift from maroon mudstone to a pale green-white, silty mudstone. Like the balance of the Mussentuchit Member overbank deposits, the white-green mudstone is rich in smectitic clays. In the southern one-third of the mapped area, Ruby Ranch Member sandstones are thin, discontinuous channel segments surrounded by floodplain deposits. In the middle to northern area, point bar complexes dominate, some of which are laterally amalgamated. Flow direction data from four meander complexes and a low sinuosity channel indicate an average northeast flow. Dakota Sandstone channels all of which are within the Mussentuchit Member also flowed to the northeast but point bar complexes are both more numerous and more laterally continuous than in the Ruby Ranch Member, indicating deposition in an area with less accommodation space than during Ruby Ranch Member time. The data indicate the Dakota Sandstone consists exclusively of fluvial sandstones encased within the Mussentuchit Member of the Cedar Mountain Formation. Therefore, these units are coeval and simply different facies of the same depositional system. Consequently the Mussentuchit Member is considered a member facies of the Dakota Formation.
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Bonnaventure, Philip P. "Validation of the Basal Temperature of Snow (BTS) method to map permafrost in complex mountainous terrain, Ruby Range, Yukon Territory and Haines Summit, British Columbia." Thesis, University of Ottawa (Canada), 2006. http://hdl.handle.net/10393/27335.

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This study is the second attempt to use the Basal Temperature of Snow (BTS) method to map permafrost in mountainous regions of northwestern Canada. It differs from the first study which took place in Wolf Creek in terms of (1) the methodology used to evaluate BTS, (2) the strategy used to avoid spatial autocorrelation in residuals, and (3) the climatic regions investigated. Two study areas, part of the Ruby Range (61° 12' N, 138° 19' W) and Haines Summit (59° 37' N, 136° 27' W) were selected for BTS sampling based on differing climatic conditions and previous knowledge of permafrost elevations from active rock glaciers. A total of 30 BTS measurements were made in the Ruby Range in the winter of 2006 and a total of 77 BTS values were obtained in the Haines Summit area during 2005 and 2006. From these results, modeled BTS surfaces were created using elevation and potential incoming solar radiation as independent variables in a multiple linear regression. At Haines Summit, potential incoming solar radiation was not significant in the model and thus was dropped. The surface of modeled BTS was then combined with a physical validation of permafrost presence completed during the late-summer of 2005 in a logistic regression. The modeled results produced permafrost probability maps for both study areas. Based on modeled results, permafrost underlies an estimated 282 km2 or 66% of the Ruby Range study area and 23--236 km 2 or 43--44% of the Haines Summit study area. An attempt was made to use the linear model derived in the Ruby Range at Haines Summit in order to examine the possibility of expanding predictions into new areas. Although the results produced similar total amounts of permafrost, the spatial distribution differed: permafrost probabilities were reduced at high elevations while lower elevation sites exhibited increased probabilities. The results of the model transfer illustrate the importance of the pit data in determining the total amount of permafrost, while knowledge of BTS ranges contributes to the spatial distribution of permafrost. With further study it is likely that generic models can be derived for areas of similar climate.
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Hernandez, Brett M. "Physical Volcanology, Kinematics, Paleomagnetism, and Anisotropy of Magnetic Susceptibility of the Nathrop Volcanics, Colorado." Bowling Green State University / OhioLINK, 2014. http://rave.ohiolink.edu/etdc/view?acc_num=bgsu1400251995.

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Sigvardson, Malin E. "The Constitution of Movement in Rudy Wiebe's Fiction : A Phenomenological Study of Three Mennonite Novels." Doctoral thesis, Stockholm : Department of English, Stockholm University, 2006. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-1299.

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Books on the topic "Ruby Mountains"

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C, White Michael. 50 classic hikes in Nevada: From the Ruby Mountains to Red Rock Canyon. Reno: University of Nevada Press, 2006.

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William, Drexler John, Epis Rudy C. 1930-, and Larson Edwin E. 1931-, eds. Cenozoic volcanism in the southern Rocky Mountains updated: A tribute to Rudy C. Epis. Golden, CO: Colorado School of Mines, 1988.

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Nevada. Department of Wildlife. Conservation agreement and strategy, Columbia spotted frog (Rana luteiventris), Great Basin population, Nevada: Northeastern subpopulations, Jarbdidge-Independence and Ruby Mountain. [Nev.?]: Columbia Spotted Frog Technical Team, 2003.

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Tragedy on the mountain: A quadriplegic's journey from paralysis to Paralympics. [United States]: Createspace, 2012.

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Hyslop, Larry. Ruby Mountains Visitor Guide. Gray Jay Press, 2004.

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Geological Survey (U.S.), ed. Lineaments and their association with metal deposits, Ruby Mountains, Montana. [Reston, Va.?]: Dept. of the Interior, U.S. Geological Survey, 1985.

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G, Tysdal Russell, ed. Mineral resources of the Ruby Mountains Wilderness Study Area, Madison County, Montana. Washington: U.S. G.P.O., 1987.

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White, Michael C. 50 Classic Hikes in Nevada: From the Ruby Mountains to Red Rock Canyon. University of Nevada Press, 2006.

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Smith, Kevin J. Petrology and Origin of Precambrian Metamorphic Rocks in the Eastern Ruby Mountains Southwestern Montana: M. S. Thesis University of Montana. Lulu Press, Inc., 2021.

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Stryhas, Bart Andrew. Progressive refolding in high strain regimes: An application to the Maggia Nappe, Ticino, Switzerland and the Lamoille Canyon Nappe, Ruby Mountains, Nevada. 1988.

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Book chapters on the topic "Ruby Mountains"

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Kistler, R. W., E. D. Ghent, and J. R. O'neil. "Petrogenesis of Garnet Two-Mica Granites in the Ruby Mountains, Nevada." In 1989, Granites and Rhyolites, 10591–606. Washington, DC: American Geophysical Union, 2013. http://dx.doi.org/10.1002/9781118782057.ch27.

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Snoke, A. W., A. J. McGrew, P. A. Valasek, and S. B. Smithson. "A Crustal Cross-Section for a Terrain of Superimposed Shortening and Extension: Ruby Mountains-East Humboldt Range Metamorphic Core Complex, Nevada." In Exposed Cross-Sections of the Continental Crust, 103–35. Dordrecht: Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-009-0675-4_5.

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Echeverría, Javier, Narel Y. Paniagua-Zambrana, and Rainer W. Bussmann. "Grindelia boliviana Rusby Grindelia tarapacana Phil. Asteraceae." In Ethnobotany of Mountain Regions, 1–2. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-319-77093-2_133-1.

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Echeverría, Javier, Narel Y. Paniagua-Zambrana, and Rainer W. Bussmann. "Grindelia boliviana Rusby Grindelia tarapacana Phil. Asteraceae." In Ethnobotany of Mountain Regions, 919–20. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-28933-1_133.

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Paniagua-Zambrana, Narel Y., and Rainer W. Bussmann. "Clusia lechleri Rusby Clusia minor L. Clusia pachamamae Zenteno Ruiz & A. Fuentes Clusia sp. Clusiaceae." In Ethnobotany of Mountain Regions, 1–6. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-319-77093-2_75-1.

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Paniagua-Zambrana, Narel Y., and Rainer W. Bussmann. "Clusia lechleri Rusby Clusia minor L. Clusia pachamamae Zenteno Ruiz & A. Fuentes Clusia sp. Clusiaceae." In Ethnobotany of Mountain Regions, 577–82. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-28933-1_75.

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Munroe, Jeffrey S., Matthew F. Bigl, Annika E. Silverman, and Benjamin J. C. Laabs. "Records of late Quaternary environmental change from high-elevation lakes in the Ruby Mountains and East Humboldt Range, Nevada." In From Saline to Freshwater: The Diversity of Western Lakes in Space and Time. Geological Society of America, 2019. http://dx.doi.org/10.1130/2018.2536(03).

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Weaver, Stewart A. "7. To the ends of the earth." In Exploration: A Very Short Introduction, 100–113. Oxford University Press, 2015. http://dx.doi.org/10.1093/actrade/9780199946952.003.0007.

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With the filling of the large space on the map that was Tibet and High Asia, explorers turned to smaller spaces or else they turned to those untouched extremities where there was no map—the Arctic and the Antarctic. ‘To the ends of the earth ’ first describes the search for the North Pole in the Arctic. It was Americans Frederick Cook and Robert Peary who laid their competing claims to 90° north, but the race to the South Pole was between Robert Scott and Roald Amundsen. It was Amundsen who succeeded. The two next terrestrial prizes were the world's highest mountain, Mount Everest, and Rub' al Khali, the “Empty Quarter” of southeastern Arabia.
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Conference papers on the topic "Ruby Mountains"

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Nolt-Caraway, Sarah Ann, and Ryan C. Porter. "MAPPING CRUSTAL DEFORMATION USING SEISMIC ANISOTROPY, RUBY MOUNTAINS, NEVADA." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-340503.

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Levy, Drew, and Andrew Zuza. "THERMOMECHANICAL EVOLUTION OF THE RUBY MOUNTAINS-EAST HUMBOLDT RANGE MYLONITIC SHEAR ZONE." In Cordilleran Section-117th Annual Meeting-2021. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021cd-363345.

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Sackett, Hannah, Benjamin J. C. Laabs, Jeffrey S. Munroe, and Samantha W. Eckes. "CLIMATE CHANGE DURING DEGLACIATION OF THE OVERLAND CREEK VALLEY, RUBY MOUNTAINS, NEVADA, U.S.A." In 51st Annual Northeastern GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016ne-272821.

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Mueller, Carlton, James R. Metcalf, and Allen J. McGrew. "THERMOCHRONOLOGIC CONSTRAINTS ON THE COOLING AND EXHUMATION OF THE NORTHERN RUBY MOUNTAINS, NEVADA." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-337836.

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Zuza, Andrew, Seth Dee, Drew Levy, and Joel DesOrmeau. "GENERAL SHEAR STRAIN IN THE RUBY MOUNTAINS-EAST HUMBOLDT RANGE METAMORPHIC CORE COMPLEX." In Cordilleran Section-117th Annual Meeting-2021. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021cd-363135.

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Reimers, Alexander, and Benjamin Laabs. "CLIMATE CHANGE DURING DEGLACIATION INFERRED FROM NUMERICAL GLACIER MODELING IN THE RUBY MOUNTAINS, NEVADA." In 52nd Annual North-Central GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018nc-313256.

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Griffin, Kayla M., and Willis E. Hames. "RAPID AND DIACHRONOUS COOLING OF THE RUBY MOUNTAINS METAMORPHIC CORE COMPLEX THAT PREDATED THE YELLOWSTONE HOTSPOT." In 67th Annual Southeastern GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018se-312956.

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Lambert, Kimberly A., Jessica Campbell, and Michael A. Krol. "GEOCHEMICAL STUDY OF THE TIMBER HILL BASALT AND ADJACENT BASALT PLUGS WITHIN THE BLACKTAIL AND RUBY MOUNTAINS, SOUTHWEST MONTANA." In 72nd Annual GSA Rocky Mountain Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020rm-346715.

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Griffin, Kayla M., and Willis Hames. "THE PRE-MIOCENE REGIONAL EXHUMATION HISTORY OF DEEP CRUST EXPOSED IN THE RUBY MOUNTAINS METAMORPHIC CORE COMPLEX, NEVADA." In 66th Annual GSA Southeastern Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017se-290844.

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Camilleri, Phyllis A., Jack E. Deibert, and Michael E. Perkins. "THE ROLE OF THE ~ 16 -5 MA KNOLL- EAST HUMBOLDT-RUBY MOUNTAINS FAULT SYSTEM IN THE EVOLUTION OF THE RUBY–EAST HUMBOLDT-WOOD HILLS METAMORPHIC CORE COMPLEX, NORTHEAST NEVADA." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-277274.

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Reports on the topic "Ruby Mountains"

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Edwards, B. R., and A. Bye. Preliminary results of field mapping, GIS spatial analysis, and major-element geochemistry, Ruby Mountain volcano, Atlin volcanic district, northwestern British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2003. http://dx.doi.org/10.4095/214027.

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Mineral resources of the Ruby Mountains Wilderness Study Area, Madison County, Montana. US Geological Survey, 1987. http://dx.doi.org/10.3133/b1724a.

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