Academic literature on the topic 'Pluvial lakes'

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Journal articles on the topic "Pluvial lakes"

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Reheis, Marith. "Highest Pluvial-Lake Shorelines and Pleistocene Climate of the Western Great Basin." Quaternary Research 52, no. 2 (September 1999): 196–205. http://dx.doi.org/10.1006/qres.1999.2064.

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Shoreline altitudes of several pluvial lakes in the western Great Basin of North America record successively smaller lakes from the early to the late Pleistocene. This decrease in lake size indicates a long-term drying trend in the regional climate that is not seen in global marine oxygen-isotope records. At +70 m above its late Pleistocene shoreline, Lake Lahontan in the early middle Pleistocene submerged some basins previously thought to have been isolated. Other basins known to contain records of older pluvial lakes that exceeded late Pleistocene levels include Columbus-Fish Lake (Lake Columbus-Rennie), Kobeh-Diamond (Lakes Jonathan and Diamond), Newark, Long (Lake Hubbs), and Clover. Very high stands of some of these lakes probably triggered overflows of previously internally drained basins, adding to the size of Lake Lahontan. Simple calculations based on differences in lake area suggest that the highest levels of these pluvial lakes required a regional increase in effective moisture by a factor of 1.2 to 3 relative to late Pleistocene pluvial amounts (assuming that effective moisture is directly proportional to the hydrologic index, or lake area/tributary basin area). These previously unknown lake levels reflect significant changes in climate, tectonics, and (or) drainage-basin configurations, and could have facilitated migration of aquatic species in the Great Basin.
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Waters, Michael R. "Late Quaternary Lacustrine History and Paleoclimatic Significance of Pluvial Lake Cochise, Southeastern Arizona." Quaternary Research 32, no. 1 (July 1989): 1–11. http://dx.doi.org/10.1016/0033-5894(89)90027-6.

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AbstractDuring the latest Quaternary, freshwater pluvial lakes intermittently formed in the topographically closed Willcox basin, Arizona. A lacustrine sequence of six separate high stands of Lake Cochise is documented by stratigraphic studies, 19 radiocarbon ages, and supplementary evidence. Two stands of pluvial Lake Cochise, older than 14,000 yr B.P., reached elevations above 1290 m. The prominent 1274-m shoreline of Lake Cochise, which circumscribes the basin, was largely created during a high stand between 13,750 and 13,400 yr B.P. During the Holocene, water filled the Willcox basin three times to an elevation slightly below the crest of the 1274-m shoreline. This occurred once during the early Holocene around or before 8900 yr B.P. and twice during the later part of the middle Holocene. Since the middle Holocene, only shallow ephemeral lakes have occupied the deflated central portion of ancient Lake Cochise, a depression known as the Willcox Playa. The lacustrine sequence of Lake Cochise provides an independent evaluation of late Quaternary paleoclimatic reconstructions for southern Arizona and the American Southwest.
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Orme, Antony R. "Pleistocene pluvial lakes of the American West: a short history of research." Geological Society, London, Special Publications 301, no. 1 (2008): 51–78. http://dx.doi.org/10.1144/sp301.4.

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Forman, Steven L., Richard P. Smith, William R. Hackett, Julie A. Tullis, and Paul A. McDaniel. "Timing of Late Quaternary Glaciations in the Western United States Based on the Age of Loess on the Eastern Snake River Plain, Idaho." Quaternary Research 40, no. 1 (July 1993): 30–37. http://dx.doi.org/10.1006/qres.1993.1053.

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AbstractThe most viable sources for ubiquitous loess deposits on the eastern Snake River Plain, Idaho are aggraded river valleys, active alluvial fans, and fluctuating pluvial lake margins associated with regional late Pleistocene glaciation of the northern Rocky Mountains. Stratigraphic studies on the Idaho National Engineering Laboratory document two distinct loess deposits, separated by a well-developed paleosol, resting on basaltic lava. Baked sediments beneath this lava yielded thermoluminescence (TL) age estimates of 108,000 ± 13,000 and 101,000 ± 7000 yr, and baked organic matter gave radiocarbon ages of >32,000 yr B.P., consistent with an earlier K/Ar age for the flow of 95,000 ± 25,000 yr. The overlying two loess deposits yielded TL age estimates of 74,000 ± 6000 and 28,000 ± 3000 yr. The available geochronology indicates that the latest period of loess deposition commenced ca. 40,000 to 35,000 yr ago and ceased approximately 10,000 yr ago, which is generally coincident with the inferred timing of regional Pinedale glaciation and pluvial lake expansion. We estimate that the penultimate loess depositional episode dates between 80,000 and 60,000 yr ago, which is significantly younger than previous age estimates of 140,000 to 150,000 yr based on stratigraphic position. We speculate that this period of loess deposition may correlate with documented early to middle Wisconsinan glaciation and a high stand of pluvial lakes in the Basin and Range province.
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Chernova, Elena N., Vladimir M. Shulkin, Eugenia V. Lysenko, Tatiana N. Lutsenko, and Anna G. Boldeskul. "Hydrochemical and biogeochemical features of freshwater and brackish lakes in eastern Sikhote-Alin." Izvestiya TINRO 178, no. 3 (September 30, 2014): 157–72. http://dx.doi.org/10.26428/1606-9919-2014-178-157-172.

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Concentration of major ions and trace metals dissolved and suspended in water and trace metals in plankton of freshwater (Vaskovskoye, Golubichnoye, Yaponskoye) and brackish (Dukhovskoye, Krugloye, Mramornoye, Blagodati) lakes of eastern Sikhote-Alin is determined in July 2011-2012. The Lakes Golubichnoye and Blagodati are included in the Sikhote-Alin State Natural Biosphere Reserve. Anions are detected by the liquid chromatography (Shimadzu LC-10AVP), cations and metals are analyzed by the atomic absorption spectrophotometry (AAS Shimadzu 6800), and carbon concentration is measured by the method of thermocatalytic oxidation with infrared registration (TOC-VCPN, Shimadzu). The freshwater lakes of eastern Sikhote-Alin are distinguished by heightened concentrations of chlorides, sulfates, and sodium as compared with lakes of East-European Plain, mainly because of aerial transfer of ions from the sea. The ions concentration in brackish lakes is determined by direct penetration of seawater. Difference of the heavy metals concentration between freshwater and brackish lakes is negligible, except the manganese with higher concentration in the freshwater lakes. Lakes with wetlands in their drainage area have high concentrations of dissolved organic carbon, iron and manganese, which are depended on water regime. Concentrations of trace metals in the lakes water are low because of its pluvial origin (rainwater transforms slightly in the process of filtration through effusive rocks), with exception of Lake Vaskovskoe located in the area of mining and processing the polymetallic and borosilicate ores, close to the lead smeltery in Rudnaya Pristan stopped in 2009: the lead concentration in the water of this lake is heightened, both in dissolved and suspended forms, though does not exceed the maximal permissible concentration for drinking water. Accumulation of metals by plankton is determined mainly by biological need of the plankton in these elements and practically doesn’t depend on their concentration in water.
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Honke, J. S., J. S. Pigati, J. Wilson, J. Bright, H. L. Goldstein, G. L. Skipp, M. C. Reheis, and J. C. Havens. "Late Quaternary paleohydrology of desert wetlands and pluvial lakes in the Soda Lake basin, central Mojave Desert, California (USA)." Quaternary Science Reviews 216 (July 2019): 89–106. http://dx.doi.org/10.1016/j.quascirev.2019.05.021.

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Reheis, Marith C., David M. Miller, John P. McGeehin, Joanna R. Redwine, Charles G. Oviatt, and Jordon Bright. "Directly dated MIS 3 Lake-Level Record from Lake Manix, Mojave Desert, California, USA." Quaternary Research 83, no. 1 (January 2015): 187–203. http://dx.doi.org/10.1016/j.yqres.2014.11.003.

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AbstractAn outcrop-based lake-level curve, constrained by ~ 70 calibrated 14C ages on Anodonta shells, indicates at least 8 highstands between 45 and 25 cal ka BP within 10 m of the 543-m upper threshold of Lake Manix in the Mojave Desert of southern California. Correlations of Manix highstands with ice, marine, and speleothem records suggest that at least the youngest three highstands coincide with Dansgaard–Oeschger (D–O) stadials and Heinrich events 3 and 4. The lake-level record is consistent with results from speleothem studies in the Southwest that indicate cool wet conditions during D–O stadials. Notably, highstands between 43 and 25 ka apparently occurred at times of generally low levels of pluvial lakes farther north as interpreted from core-based proxies. Mojave lakes may have been supported by tropical moisture sources during oxygen-isotope stage 3, perhaps controlled by southerly deflection of Pacific storm tracks due to weakening of the sea-surface temperature gradient in response to North Atlantic climate perturbations.
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García, Antonio Francisco, and Martin Stokes. "Late Pleistocene highstand and recession of a small, high-altitude pluvial lake, Jakes Valley, central Great Basin, USA." Quaternary Research 65, no. 1 (January 2006): 179–86. http://dx.doi.org/10.1016/j.yqres.2005.08.025.

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AbstractModels of factors controlling late Pleistocene pluvial lake-level fluctuations in the Great Basin are evaluated by dating lake levels in Jakes Valley. “Jakes Lake” rose to a highstand at 13,870 ± 50 14C Yr B.P., receded to a stillstand at 12,440 ± 50 14C yr B.P., and receded steadily to desiccation thereafter. The Jakes Lake highstand is roughly coincident with highstands of lakes Bonneville, Lahontan and Russell. The rise to highstand and recession of Jakes Lake were most likely controlled by a storm track steered by the polar jet stream. The final stillstand of Jakes Lake helps constrain timing of northward retreat of the polar jet stream during the Pleistocene–Holocene transition.
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Ibarra, Daniel E., Anne E. Egger, Karrie L. Weaver, Caroline R. Harris, and Kate Maher. "Rise and fall of late Pleistocene pluvial lakes in response to reduced evaporation and precipitation: Evidence from Lake Surprise, California." Geological Society of America Bulletin 126, no. 11-12 (June 2, 2014): 1387–415. http://dx.doi.org/10.1130/b31014.1.

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Negrini, Robert M., and Jonathan O. Davis. "Dating Late Pleistocene Pluvial Events and Tephras by Correlating Paleomagnetic Secular Variation Records from the Western Great Basin." Quaternary Research 38, no. 1 (July 1992): 46–59. http://dx.doi.org/10.1016/0033-5894(92)90029-i.

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AbstractPaleomagnetic records are used to correlate sedimentary sequences from pluvial Lakes Chewaucan and Russell in the western Great Basin. This correlation is the basis for age control in the relatively poorly dated sequence from Lake Chewaucan. The resulting chronology supports a lack of sedimentation in Lake Chewaucan during the interval 27,400 to 23,200 yr B.P., an assertion supported by the presence of a lag deposit at the corresponding stratigraphic horizon. Because the Lake Chewaucan outcrop (near Summer Lake, Oregon) is near the bottom of the lake basin, we conclude that Lake Chewaucan was at a lowstand during this time interval. The Chewaucan lowstand is coeval with the lowstand accompanying the Wizard's Beach Recession (isotope stage 3) previously seen in the geologic record from nearby pluvial Lake Lahontan. The ages of six tephra layers, including the Trego Hot Springs tephra, were also estimated using the paleomagnetic correlation. Together, the new age of the Trego Hot Springs tephra (21,800 yr B.P.) and the lake surface level prehistory of Lake Chewaucan imply a revised model for the lake surface level prehistory of Lake Lahontan. The revised model includes a longer duration for the Wizard's Beach Recession and the occurrence of a younger lowstand of short duration soon after the lowstand corresponding to the Wizard's Beach Recession.
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Dissertations / Theses on the topic "Pluvial lakes"

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Domínguez, Acosta Miguel. "The Pluvial Lake Palomas-Samalayuca Dune systems." To access this resource online via ProQuest Dissertations and Theses @ UTEP, 2009. http://0-proquest.umi.com.lib.utep.edu/login?COPT=REJTPTU0YmImSU5UPTAmVkVSPTI=&clientId=2515.

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Clement, Susanne M. "Modeling the Pluvial Lakes of the Great Basin During the Last Glacial Maximum." Kent State University / OhioLINK, 2005. http://rave.ohiolink.edu/etdc/view?acc_num=kent1120066079.

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Gudefin, Julia. "Le statut juridique de l'eau à l'épreuve des exigences environnementales." Thesis, Lyon 3, 2013. http://www.theses.fr/2013LYO30068.

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Que l’on soit un simple promeneur ou un fin observateur, l’eau est présente partout. Pourtant, l’atout qu’elle représente pour les activités anthropiques cache souvent sa réalité environnementale, celle de son cycle. Ce constat se reflète dans l’appréhension juridique de l’eau laquelle est conçue comme un bien ou une chose. Cette qualification l’assigne donc à un statut juridique dont les manifestations révèlent la fonction utilitariste de la ressource. Or, l’émergence des problématiques environnementales confronte le statut juridique de l’eau à sa réalité physique. Ainsi, le droit et les exigences environnementales s’influencent réciproquement pour générer des règles protectrices de l’eau et des représentations juridiques du cycle hydrologique qui engendrent des évolutions du statut. Dès lors, ce dernier s’émancipe des catégories juridiques traditionnelles issues du droit des biens et s’habille d’une finalité protectrice dont les règles et les concepts, qui s’attachent à la fonction écologique de l’eau et à la réalité environnementale du cycle hydrologique, lui façonnent une autre condition juridique
Along a simple stroll or through fine observations, you will always find water, wherever you go. However, the asset this resource represents for anthropogenic activities often hides its environmental reality, the one of its cycle. This is reflected in the legal definition of water which conceives it as property. This latter qualification assigns it to a judicial status which reveals the utilitarian function of the resource. Yet, the emergence of the environmental issues confronts water’s legal status to its tangible reality. Thus, the conflict between the law and water’s environmental demands makes way for protective regulations. Along with the hydrologic cycle’s legal representation, they both influence the evolution of water’s status. Consequently, the latter goes beyond property law traditional legal categories and arms itself with a protective purpose. Its rules and concepts are tied to the ecological function of water and to the environmental reality of the hydrologic cycle which shape yet another judicial condition for the water
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Books on the topic "Pluvial lakes"

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Martens, Diane C. Reproductive ecology of the piping plover at Chaplin Lake, Saskatchewan. Edmonton: Canadian Wildlife Service, 2008.

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Friends of the Pleistocene. Pacific Cell and Geological Survey (U.S.), eds. Old, very high pluvial lake levels in the Lahontan basin, Nevada: Evidence from the Walker Lake basin : contributions to the guidebook, 1996 field trip, Pacific Cell, Friends of the Pleistocene. [Reston, Va.?]: U.S. Dept. of the Interior, U.S. Geological Survey, 1996.

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1956-, Clark Peter U., and Lea Peter D, eds. The Last interglacial-glacial transition in North America. Boulder, Colo: Geological Society of America, 1992.

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U, Clark Peter, Lea Peter D, and Geological Society of America, eds. The Last interglacial-glacialtransition in North America. Boulder, Colo: Geological Society of America, 1992.

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Pluvis, lac disparu: Du retrait glaciaire à l'aménagement hydroélectrique : études paléoécologiques. [Genève, Suisse]: Muséum d'histoire naturelle de Genève, 1990.

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Book chapters on the topic "Pluvial lakes"

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Merlin, Mark D., Patrick D. Nunn, John C. Kraft, Donald L. Forbes, Ian Shennan, E. Robert Thieler, Cheryl J. Hapke, et al. "Pluvial Lake Shore Deposits." In Encyclopedia of Coastal Science, 773–78. Dordrecht: Springer Netherlands, 2005. http://dx.doi.org/10.1007/1-4020-3880-1_248.

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Warnke, Detlef A., and Hillert Ibbeken. "Pluvial Lake Shore Deposits." In Encyclopedia of Earth Sciences Series, 1–7. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-48657-4_248-2.

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Warnke, Detlef A., and Hillert Ibbeken. "Pluvial Lake Shore Deposits." In Encyclopedia of Earth Sciences Series, 1381–87. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-319-93806-6_248.

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Erol, Oğuz. "Geomorphologic Arguments for Mid- to Late Holocene Environmental Change in Central Anatolian (Pluvial) Lake Basins." In Third Millennium BC Climate Change and Old World Collapse, 321–50. Berlin, Heidelberg: Springer Berlin Heidelberg, 1997. http://dx.doi.org/10.1007/978-3-642-60616-8_12.

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"Western Pluvial Lakes Tradition." In Encyclopedic Dictionary of Archaeology, 1479. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-58292-0_230073.

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Knott, Jeffrey R., Elmira Wan, Alan L. Deino, Mitch Casteel, Marith C. Reheis, Fred M. Phillips, Laura Walkup, Kyle McCarty, David N. Manoukian, and Ernest Nunez. "Errata: Lake Andrei: A Pliocene pluvial lake in Eureka Valley, eastern California." 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(08e).

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ABSTRACT This paper has no abstract. Errata Knott, J.R., Wan, E., Deino, A.L., Casteel, M., Reheis, M.C., Phillips, F.M., Walkup, L., McCarty, K., Manoukian, D.N., and Nunez, E., Jr., 2019, Lake Andrei: A Pliocene pluvial lake in Eureka Valley, eastern California, in Starratt, S.W., and Rosen, M.R., eds., From Saline to Freshwater: The Diversity of Western Lakes in Space and Time: Geological Society of America Special Paper 536, p. 125–142, https://doi.org/10.1130/2018.2536(08). In the original online version of Chapter 8 published on 31 January 2019, a sentence in the top left paragraph on p. 127 read, “We informally named two of these tuffs the 3.509 ± 0.009 Ma tuff of Last Chance and the 3.506 ± 0.010 Ma tuff of Hanging Rock Canyon.” As shown in the current online PDF, that sentence should read, “We informally named two of these tuffs the 3.509 ± 0.009 Ma tuff of Hanging Rock Canyon and the 3.506 ± 0.010 Ma tuff of Last Chance.”
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Knott, Jeffrey R., Elmira Wan, Alan L. Deino, Mitch Casteel, Marith C. Reheis, Fred M. Phillips, Laura Walkup, Kyle McCarty, David N. Manoukian, and Ernest Nunez. "Lake Andrei: A Pliocene pluvial lake in Eureka Valley, eastern California." 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(08).

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Redwine, Joanna R., R. M. Burke, M. C. Reheis, R. J. Bowers, J. Bright, D. S. Kaufman, and R. M. Forester. "Middle and late Pleistocene pluvial history of Newark Valley, central Nevada, USA." In From Saline to Freshwater: The Diversity of Western Lakes in Space and Time. Geological Society of America, 2019. http://dx.doi.org/10.1130/2019.2536(18).

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Rhodes, Dallas D., Robert M. Negrini, J. Ramon Arrowsmith, Peter E. Wigand, Steven L. Forman, Manuel R. Palacios-Fest, and Owen K. Davis. "Geomorphic and sedimentologic evidence for pluvial Lake Carrizo, San Luis Obispo County, California." In From Saline to Freshwater: The Diversity of Western Lakes in Space and Time. Geological Society of America, 2019. http://dx.doi.org/10.1130/2019.2536(16).

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Egger, Anne E., Daniel E. Ibarra, Ray Weldon, Robert M. Langridge, Brian Marion, and Jennifer Hall. "Influence of pluvial lake cycles on earthquake recurrence in the northwestern Basin and Range, USA." 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(07).

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Conference papers on the topic "Pluvial lakes"

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Lechler, Alex R., Katharine Huntington, Dan O. Breecker, Mark R. Sweeney, and Andrew J. Schauer. "CARBONATE CLUMPED ISOTOPE RECORD OF LGM-HOLOCENE CLIMATE CHANGE ACROSS THE PACIFIC NORTHWEST US: INSIGHTS FROM LOESS-PALEOSOLS AND PLUVIAL LAKES." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-303031.

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Ramirez, Adam E., Jeffrey R. Knott, Jeffrey S. Pigati, Jordon Bright, and Jeffrey C. Nekola. "PLUVIAL LAKE DEPOSITS OF DEEP SPRINGS VALLEY, CALIFORNIA." In 112th Annual GSA Cordilleran Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016cd-274420.

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Knott, Jeffrey R., Elmira Wan, Alan Deino, Mitch Casteel, Marith C. Reheis, Fred M. Phillips, Laura C. Walkup, Kyle R. McCarty, David Manoukian, and Ernest Nunez. "LAKE ANDREI: A PLIOCENE PLUVIAL LAKE IN EUREKA VALLEY, EASTERN CALIFORNIA." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-321363.

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Wriston, Teresa A., and Geoffrey M. Smith. "THE LATE PLEISTOCENE TO HOLOCENE ARCHAEOLOGY AND LAKE LEVELS OF PLUVIAL LAKE WARNER, OREGON." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-287174.

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Dickey, Hank, Matthew E. Kirby, Ed Knell, William T. Anderson, Stephanie Hernandez, Sophia Obarr, Jen Leidelmeijer, Jan Taylor, and Eyrica Arriola. "USING LAKE SEDIMENTS TO INFER LATE-GLACIAL HYDROLOGIC CONDITIONS OF PLUVIAL LAKE MOJAVE, CALIFORNIA." In 116th Annual GSA Cordilleran Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020cd-347676.

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Ibarra, Daniel E., Jessica L. Oster, Matthew J. Winnick, Andrea J. Ritch, C. Page Chamberlain, and Kate Maher. "CLIMATOLOGICAL DRIVERS OF PLIO-PLEISTOCENE PLUVIAL LAKE DISTRIBUTIONS IN WESTERN NORTH AMERICA." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-277562.

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McNeely, Cameron Jean, Stephen C. Kuehn, James K. Frye, and Jared W. Rose. "USING VOLCANIC ASH TO CONSTRAIN THE HISTORY OF GLACIAL-INTERGLACIAL LAKE LEVEL CHANGES AT SUMMER LAKE, PLUVIAL LAKE CHEWAUCAN, OREGON." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-320968.

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Munroe, Jeffrey S. "GROUND PENETRATING RADAR INVESTIGATION OF PLEISTOCENE SHORELINES OF PLUVIAL LAKE CLOVER, ELKO COUNTY, NEVADA." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-340587.

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Belanger, Bryce K., William H. Amidon, Benjamin Laabs, and Jeffrey S. Munroe. "MODELING CLIMATE CONSTRAINTS ON THE FORMATION OF PLUVIAL LAKE BONNEVILLE IN THE GREAT BASIN, USA." In 54th Annual GSA Northeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019ne-328050.

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Egger, Anne E., Ray J. Weldon, Robert M. Langridge, Daniel E. Ibarra, Brian Marion, and Jennifer Hall. "THE INFLUENCE OF PLUVIAL LAKE CYCLES ON EARTHQUAKE RECURRENCE IN THE NORTHWESTERN BASIN AND RANGE EXTENSIONAL PROVINCE." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-283557.

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