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Relevant bibliographies by topics / Lake Valley

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Academic literature on the topic 'Lake Valley'

Author: Grafiati

Published: 2 June 2025

Last updated: 31 July 2025

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Journal articles on the topic "Lake Valley"

1

Lyons, W. B., S. W. Tyler, R. A. Wharton, D. M. McKnight, and B. H. Vaughn. "A Late Holocene desiccation of Lake Hoare and Lake Fryxell, McMurdo Dry Valleys, Antarctica." Antarctic Science 10, no. 3 (1998): 247–56. http://dx.doi.org/10.1017/s0954102098000340.

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Stable isotope data from waters of lakes in the McMurdo Dry Valleys (MDV) of southern Victoria Land, Antarctica are presented in order to establish the climatic history of this region over the past two millennia. New data from Lake Fryxell and Lake Hoare in Toylor Valley, along with previously published data from Lake Vanda, Wright Valley and Lake Bonney, Taylor Valley are used to infer the recent climatic history of MDV. Lakes Vanda, Fryxell and Bonney appear to have lost their ice covers and evaporated to small, hypersaline ponds by 1000 to ~1200 yr BP. Lake Hoare either desiccated or did no

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Dugan, H. A., M. K. Obryk, and P. T. Doran. "Lake ice ablation rates from permanently ice-covered Antarctic lakes." Journal of Glaciology 59, no. 215 (2013): 491–98. http://dx.doi.org/10.3189/2013jog12j080.

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AbstractIn the McMurdo Dry Valleys of Antarctica, three large, permanently ice-covered, closed-basin lakes exist along the floor of Taylor Valley. Lake ice ablation (loss of ice mass) is calculated as the sum of sublimation and surface melt, and is the driver of ice-cover turnover in these systems. In Taylor Valley, both manual and automated lake ice ablation rates have been calculated from 2001 to 2011. Results indicate relatively consistent winter ablation of 0.07–0.21 m (0.2–0.7 mm w.e. d−1). Summer ablation of lake ice is more variable and ranges from 0.25 to 1.62 m (5–31 mm w.e. d−1) over

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Laiti, L., D. Zardi, M. de Franceschi, G. Rampanelli, and L. Giovannini. "Analysis of the diurnal development of a lake-valley circulation in the Alps based on airborne and surface measurements." Atmospheric Chemistry and Physics 14, no. 18 (2014): 9771–86. http://dx.doi.org/10.5194/acp-14-9771-2014.

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Abstract. This study investigates the thermal structures of the atmospheric boundary layer (ABL) and the near-surface wind field associated with a lake-valley circulation in the south-eastern Italian Alps – the so-called Ora del Garda. Two flights of an equipped motorglider allowed for the exploration of the diurnal evolution of this circulation, from the onset, on Lake Garda's shoreline, throughout its development along the Sarca Valley and Lakes Valley (Valle dei Laghi), to the outflow into the Adige Valley. At the same time, surface observations, both from a targeted field campaign and from

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Aguilar, Germán, Joseph Martinod, Matías Gallardo, and Christian Sue. "Chronology of the Bayo River valley deglaciation and implications for the Late Pleistocene Atlantic-to-Pacific drainage reversal of the General Carrera-Buenos Aires palaeolake, Patagonia-Chile." Andean Geology 50, no. 1 (2023): 1. http://dx.doi.org/10.5027/andgeov50n1-3460.

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We present a study on the glacial and paraglacial geomorphology of a Patagonian Cordillera Valley that is key to understanding evolution of the great lakes of Patagonia. 10Be cosmogenic nuclide exposure ages of ice-moulded surfaces from the Bayo River Valley confirm that the valley became ice-free before 13.4-14.2 ka. This valley constituted the first outlet of the Chelenko Lake, precursor of the General Carrera-Buenos Aires Lake (GCBAL), toward the Pacific Ocean. This age constrains the timing of the lake drainage reversal from the Atlantic Ocean to the Pacific Ocean. Alluvial fans and terrac

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Hall, B. L., G. H. Denton, and B. Overturf. "Glacial Lake Wright, a high-level Antarctic lake during the LGM and early Holocene." Antarctic Science 13, no. 1 (2001): 53–60. http://dx.doi.org/10.1017/s0954102001000086.

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We report evidence of a large proglacial lake (Glacial Lake Wright) that existed in Wright Valley in the McMurdo Dry Valleys region of Antarctica at the last glacial maximum (LGM) and in the early Holocene. At its highstands, Glacial Lake Wright would have stretched 50 km and covered c. 210 km2. Chronology for lake-level changes comes from 30 AMS radiocarbon dates of lacustrine algae preserved in deltas, shorelines, and glaciolacustrine deposits that extend up to 480 m above present-day lakes. Emerging evidence suggests that Glacial Lake Wright was only one of a series of large lakes to occupy

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Fleisher, P. Jay. "Evidence of An Ice-Dammed Lake and Laurentide Readvance Upper Susquehanna Valley, New York State." Journal of Geography and Geology 14, no. 2 (2022): 52. http://dx.doi.org/10.5539/jgg.v14n2p52.

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Landforms and well logs document a system of ice-contact and proglacial lakes in the upper Susquehanna valley during Laurentide Ice Sheet retreat from the Appalachian Plateau, central New York State.&nbsp; Recessional moraines formed dams for all lakes, except a newly revealed &ldquo;Ancestral Goodyear Lake&rdquo; retained behind an ephemeral ice dam stranded at Colliersville.&nbsp; A prominent dead-ice sink currently occupies the valley floor at the dam site  Ancestral Goodyear Lake held a stable lake level at 1360 feet as represented by thick lake sediments perche

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Roshchyna, N. O., and B. O. Baranovski. "Hydrological and hydrobotanic typology of the lake of North-Steppe Dnieper region." Ecology and Noospherology 30, no. 2 (2019): 125–31. http://dx.doi.org/10.15421/031921.

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This article is devoted to the typology of lakes of the North-Steppe Dnieper. In developing the typology of lakes, the parameters were taken into account: landscape location, hydro-chemical and hydro-biological characteristics and the degree of their anthropogenic transformation. The data presented are based on the processing of stationary and route research materials from 1998 to 2018 on the lakes of river valleys: Dnieper, Samara, and Orel. Hydrological indicators are analyzed according to the literature, cartographic and archival data of the Dneprodiprovodkhoz Institute and the Biology Rese

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Oaks, Robert, Susanne Jänecke, Tammy Rittenour, Thad Erickson, and Michelle Nelson. "Implications and hydrographs for two Pre-Bonneville pluvial lakes and double geosols from 14 OSL-IRSL ages in Cache Valley, NE Bonneville Basin." Geosites 51 (January 14, 2024): 1–24. http://dx.doi.org/10.31711/ugap.v51i.142.

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In the northeastern Great Basin, USA, thirteen new optically stimulated luminescence (OSL) ages and one infrared stimulated luminescence (IRSL) age show that two deep pluvial lakes preceded the Bonneville lake cycle in Cache Valley during marine oxygen-isotope stages (MIS) 6 (123-191 ka) and 4 (56-71 ka), respectively. Our new data define quantitative hydrographs of the Little Valley and Cutler Dam lake cycles in both Cache Valley and the main Bonneville basin. In western Cache Valley, excavation of a faulted, east-plunging spit has sequentially exposed these deposits and overlying MIS 3 Field

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Doran, Peter T., Christopher P. McKay, Andrew G. Fountain, et al. "Hydrologic response to extreme warm and cold summers in the McMurdo Dry Valleys, East Antarctica." Antarctic Science 20, no. 5 (2008): 499–509. http://dx.doi.org/10.1017/s0954102008001272.

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AbstractThe meteorological characteristics and hydrological response of an extreme warm, and cold summer in the McMurdo Dry Valleys are compared. The driver behind the warmer summer conditions was the occurrence of down-valley winds, which were not present during the colder summer. Occurrence of the summer down-valley winds coincided with lower than typical mean sea level pressure in the Ross Sea region. There was no significant difference in the amount of solar radiation received during the two summers. Compared to the cold summer, glaciological and hydrological response to the warm summer in

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Stone, Michael S., Peter T. Doran, and Krista F. Myers. "Rethinking the Lake History of Taylor Valley, Antarctica During the Ross Sea I Glaciation." Geosciences 15, no. 1 (2025): 9. https://doi.org/10.3390/geosciences15010009.

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The Ross Sea I glaciation, marked by the northward advance of the Ross Ice Sheet (RIS) in the Ross Sea, east Antarctica, corresponds with the last major expansion of the West Antarctic Ice Sheet during the last glacial period. During its advance, the RIS was grounded along the southern Victoria Land coast, completely blocking the mouths of several of the McMurdo Dry Valleys (MDVs). Several authors have proposed that very large paleolakes, proglacial to the RIS, existed in many of the MDVs. Studies of these large paleolakes have been key in the interpretation of the regional landscape, climate,

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Dissertations / Theses on the topic "Lake Valley"

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Carroll, Kelly Patrick. "Permeability of Lake Ice in the Taylor Valley, Antarctica: From Permeameter Design to Permeability Upscaling." Columbus, Ohio : Ohio State University, 2008. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=osu1206545662.

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Whittaker, Thomas E. "Lake-Level Fluctuations in the Fryxell Basin, Eastern Taylor Valley, Antarctica." Fogler Library, University of Maine, 2004. http://www.library.umaine.edu/theses/pdf/WhittakerTE2004.pdf.

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Yetman, Gregory George. "Spatial information and environmental decision making : the Windermere Valley, British Columbia." Thesis, McGill University, 1999. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=30231.

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Local participation in environmental decision making processes is a recognized need if the goals of sustainable development are to be met. Spatial information is an important part of environmental decision making, but so far, technical barriers have prevented effective public participation in spatial data management and analysis. These barriers need to be overcome if participants are to take part in a decision making process in a manner that is both fair and competent. The study was undertaken to quantify land cover change in a particular region and, through this exercise, to determine what th

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Rey, Kevin A. "Insights into the Early Transgressive History of Lake Bonneville from Stratigraphic Investigation of Pilot Valley Playa, UT/NV, USA." BYU ScholarsArchive, 2012. https://scholarsarchive.byu.edu/etd/3803.

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Multiple shallow sediment cores were obtained from Pilot Valley playa, a sub-basin located in the northwestern Bonneville basin. Analysis of stratigraphy, ostracodes, mineralogy, chemistry, total inorganic carbon (TIC), total organic carbon (TOC), and stable isotopes were performed to better place these sediments into proper context with respect to the Lake Bonneville cycle. Results showed Pilot Valley playa contains a nearly full sequence of Lake Bonneville deep-water marl in addition to sediments deposited before and after the Lake Bonneville cycle. Within the marl is a sequence of organic r

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Drake, Alexandra. "Mapping of Massive Ground Ice Using Ground Penetrating Radar Data in Taylor Valley, McMurdo Dry Valleys of Antarctica." Thesis, Uppsala universitet, Institutionen för geovetenskaper, 2015. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-260357.

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The distribution of massive ground ice in the ground in Taylor Valley of the McMurdo Dry Valleys, Antarctica, is quite unknown, and could provide answers to questions such as where the ice comes from, if it has been affected and removed by proglacial lakes and how landscapes underlain by massive ground ice responds to climate change. It could also be a source for atmospheric information in the past and hence a key in climate research. The main goal with this project was therefore to map the distribution of massive ground ice mainly in Taylor Valley, but also in the adjacent Salmon Valley and W

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Limbu, Sal Bir. "Estimating Upper Red Butte Watershed Contribution to Salt Lake Valley Water Resources." DigitalCommons@USU, 2019. https://digitalcommons.usu.edu/etd/7503.

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Water is crucial for domestic, agricultural, industrial, environmental, and hydropower uses. Once precipitation occurs, it eventually partitions into streamflow, evapotranspiration (ET), and groundwater recharge. Distribution of precipitation into these partitions is called a hydrologic budget. The hydrologic budget of any geographic area or watershed under different climate change conditions help water managers to make appropriate water management plans. Computer based hydrologic modeling software has been used extensively to solve many water resources problems including hydrologic budgets. H

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Lowry, John H. Jr. "Spatial Analysis of Urbanization in the Salt Lake Valley: An Urban Ecosystem Perspective." DigitalCommons@USU, 2010. https://digitalcommons.usu.edu/etd/746.

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Because urban areas comprise a variety of biotic (e.g. people, trees) and abiotic (e.g. streets, water) components that interact and are often interdependent upon one another, it is helpful to study urban areas as urban ecosystems. Our goal in Chapter 2 is to measure and quantify the spatial and demographic structure of the urbanized portion of Salt Lake County, Utah. We use 18 metrics from four broad categories (density, centrality, accessibility, and neighborhood mix) to measure urban form for three age-based residential neighborhood types. Using analysis of variance (ANOVA) we test for d

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Muiruri, Veronica Mwihaki. "Late Quaternary diatom and palynomorph stratigraphies and palaeoenvironments of the Koora Graben and Lake Magadi Basin, Kenya Rift Valley." HKBU Institutional Repository, 2017. https://repository.hkbu.edu.hk/etd_oa/461.

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Two sets of cores were recovered from the southern Kenya Rift (Koora and Magadi basins) through the Hominid Sites and Paleolakes Drilling Project and the Olorgesailie Drilling Project. These contain a detailed environmental Quaternary history with records of up to ~1 million years. This period correlates with much of the Olorgesailie Formation record of 1.2 Ma in the Olorgesailie Basin. The Magadi cores reached trachyte at ~ 194 and 133 m with this project focussed on the longer core, MAG14-2A, which includes limestone, zeolitic, laminated and massive clay and silt, massive mud, chert, trona,

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Steele, Erin M. "CORRELATION OF TERRACES IN THE CHAGRIN RIVER VALLEY WITH ANCESTRAL LEVELS OF LAKE ERIE, NORTHEASTERN OHIO." University of Akron / OhioLINK, 2007. http://rave.ohiolink.edu/etdc/view?acc_num=akron1197297354.

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Ambili, Anoop. "Lake sediments as climate and tectonic archives in the Indian summer monsoon domain." Phd thesis, Universität Potsdam, 2012. http://opus.kobv.de/ubp/volltexte/2013/6479/.

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The Indian summer monsoon (ISM) is one of the largest climate systems on earth and impacts the livelihood of nearly 40% of the world’s population. Despite dedicated efforts, a comprehensive picture of monsoon variability has proved elusive largely due to the absence of long term high resolution records, spatial inhomogeneity of the monsoon precipitation, and the complex forcing mechanisms (solar insolation, internal teleconnections for e.g., El Niño-Southern Oscillation, tropical-midlatitude interactions). My work aims to improve the understanding of monsoon variability through generation of l

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Books on the topic "Lake Valley"

1

Gregg, Kristen J. Lake Chelan Valley. Arcadia Pub., 2009.

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Gregg, Kristen J. Lake Chelan Valley. Arcadia Pub., 2009.

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Pistolesi, Andrea. Lake Powell, Monument Valley. Casa Editrice Bonechi, 1992.

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Lake Valley Rowletta History Book Society., ed. Combining communities: Lake Valley, Rowletta. Lake Valley Rowletta History Book Society, 1986.

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Benedict, James B. Archeology of the Coney Lake Valley. Center for Mountain Archeology, 1990.

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Leventhal, Joel S. Geochemistry of Mariano Lake-Lake Valley cores, McKinley County, New Mexico. U.S. G.P.O., 1990.

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Sims, Ray O. Loon Lake and Ash Valley revisited: A history of Ash Valley and Loon Lake in Douglas County, Oregon. R.O. Sims, 1998.

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Piercy, Frederick Hawkins. Route from Liverpool to Great Salt Lake Valley. Applewood Books, 1997.

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United States. Congress. Senate. Committee on Energy and Natural Resources. Trinity Lake: Report (to accompany H.R. 63). U.S. G.P.O., 1997.

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International, Conference on Salt Lakes (7th 1999 Death Valley National Park Calif and Nev ). Saline lakes: Publications from the Seventh International Conference on Salt Lakes, held in Death Valley National Park, California, U.S.A., September 1999. Kluwer Academic Publishers, 2001.

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Book chapters on the topic "Lake Valley"

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Renaut, Robin W., and Richard Bernhart Owen. "Lake Logipi and the Suguta Valley." In The Kenya Rift Lakes: Modern and Ancient. Springer Berlin Heidelberg, 2023. http://dx.doi.org/10.1007/978-3-642-25055-2_7.

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McKnight, D. M., G. R. Aiken, E. D. Andrews, E. C. Bowles, and R. A. Harnish. "Dissolved organic material in dry valley lakes: A comparison of Lake Fryxell, Lake Hoare and Lake Vanda." In Physical and Biogeochemical Processes in Antarctic Lakes. American Geophysical Union, 1993. http://dx.doi.org/10.1029/ar059p0119.

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Cooke, Philippa, Peter Maguire, Russ Evans, and Nicholas Laffoley. "Seismicity near Lake Bogoria in the Kenya Rift valley." In Properties and Processes of Earth' Lower Crust. American Geophysical Union, 1989. http://dx.doi.org/10.1029/gm051p0175.

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Gophen, Moshe. "Hula Valley and Lake Kinneret Interrelationships: Future Management Proposition of Lake Agmon-Hula System." In Springer Geography. Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-23412-5_8.

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Zerkal, Oleg V., Sergey S. Chernomorets, Viktoriia A. Iudina, et al. "The Modern Activity of the Buzulgan Landslide and Its Influence on the Debris Flow Hazard for the Tyrnyauz Town (Northern Caucasus, Russia)." In Progress in Landslide Research and Technology, Volume 2 Issue 1, 2023. Springer Nature Switzerland, 2023. http://dx.doi.org/10.1007/978-3-031-39012-8_10.

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AbstractThe valley of the Gerkhozhan-Su River (a tributary of the Baksan River) in the Norther Caucasus is one of the most debris flow-prone areas in Russia. Large-scale debris flows here have occurred in 1937, 1960, 1961, 1962, 1977, 1999, 2000, 2002, 2011, 2017. The Tyrnyauz town is located in the impact zone of the debris flows. A significant impact on the debris flow hazard in the Gerkhozhan-Su River valley is exerted by the Buzulgan landslide, which was formed on the right side of the valley with a height of about 350 m and an average steepness of 23–25°. The area where the Buzulgan lands

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Nichols, Robert L. "Geology of Lake Vanda, Wright Valley, South Victoria Land, Antarctica." In Antarctic Research: The Matthew Fontaine Maury Memorial Symposium. American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm007p0047.

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Matanzima, Joshua. "The People of the Zambezi Valley: Interactions between Migrants and Locals in and Around Lake Kariba." In The Materiality of Lake Kariba. Springer Nature Singapore, 2024. http://dx.doi.org/10.1007/978-981-99-9573-8_3.

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Kiver, Eugene P., Dale F. Stradling, and Victor R. Baker. "The Spokane Valley and northern Columbia Plateau." In Glacial Lake Missoula and the Channeled Scabland Missoula, Montana to Portland, Oregon, July 20–26, 1989. American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft310p0023.

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Hanson, Larry G., and Victor R. Baker. "The Columbia Valley and Columbia River Gorge." In Glacial Lake Missoula and the Channeled Scabland Missoula, Montana to Portland, Oregon, July 20–26, 1989. American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft310p0063.

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Matsushima, Dai, Ulgiichimeg Ganzorig, and Ochirbat Batkhishig. "Preliminary Results of Estimating Erodibility and Erosivity over the Lake Valley, Mongolia." In Proceedings of the Fourth International Conference on Environmental Science and Technology (EST 2023). Atlantis Press International BV, 2023. http://dx.doi.org/10.2991/978-94-6463-278-1_22.

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Conference papers on the topic "Lake Valley"

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Hansen, Greg. "‘Clearing the Hurdles’ - A Look at the South Valley Sewer District, Jordan Basin WRF Membrane Basins Rehabilitation Project." In Coatings+ 2019. SSPC, 2019. https://doi.org/10.5006/s2019-00023.

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The South Valley Sewer District, located outside of Salt Lake City, Utah, experienced severe degradation of the concrete substrate the Membrane Basins at the Jordan Basin WRF. The Bowen Collins & Associates designed facility initially opened for service in July of 2012. By 2017 the facility was showing significant effects of concrete deterioration from chemical attack, caused by citric acid and sodium hypochlorite used as a part of the cleaning procedures in the membrane basins. This paper explains the background that led to the rehabilitation required; the team work employed by the engine

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Panin, A. V., N. E. Zaretskaya, D. V. Baranov, and A. O. Utkina. "The Pleistocene ice-dammed lakes in the Vychegda River valley." In Всероссийская конференция и полевой симпозиум. ФИЦ КНЦ РАН, 2024. http://dx.doi.org/10.37614/978.5.91137.520.1.020.

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Based on lithostratigraphic studies of sections and borehole cores, 14C and OSL dating, it is shown that alluvial and aeolian sedimentation took place in the middle and lower Vychegda valley throughout the Late Pleistocene, and the valley was not occupied by either glacier or proglacial lakes. The MIS 2 proglacial lake was locally distributed in the Northern Dvina valley. Reversal runoff through the Vychegda-Kama watershed could occur only at the end of MIS 6, when the middle and lower Vychegda was covered by ice sheet and a proglacial lake existed in the Keltma spillway crossing the watershed

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Knott, Jeffrey R., Elmira Wan, Alan Deino, et al. "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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Soule, Ralph, and Nikos Tzetos. "Lower Klamath Lake Valley Terramagnetic Survey: Interpretation." In Symposium on the Application of Geophysics to Engineering and Environmental Problems 2003. Environment and Engineering Geophysical Society, 2003. http://dx.doi.org/10.4133/1.2923125.

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Soule, Ralph, and Nikos Tzetos. "Lower Klamath Lake Valley terramagnetic survey: Interpretation." In SEG Technical Program Expanded Abstracts 2002. Society of Exploration Geophysicists, 2002. http://dx.doi.org/10.1190/1.1817380.

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Soule, Ralph, and Nikos Tzetos. "Lower Klamath Lake Valley Terramagnetic Survey: Interpretation." In 16th EEGS Symposium on the Application of Geophysics to Engineering and Environmental Problems. European Association of Geoscientists & Engineers, 2003. http://dx.doi.org/10.3997/2214-4609-pdb.190.pot04.

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Hooton, Jr., LeRoy W., and Charles H. Call, Jr. "Water Development in the Salt Lake Valley." In Water Resources and Environment History Sessions at Environmental and Water Reources Institute Annual Meeting 2004. American Society of Civil Engineers, 2004. http://dx.doi.org/10.1061/40738(140)10.

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Stokoe, Kenneth, Bradley Wilder, Brent Rosenblad, Ivan Wong, and James Bay. "SASW Testing in the Salt Lake Valley, UT." In Symposium on the Application of Geophysics to Engineering and Environmental Problems 2011. Environment and Engineering Geophysical Society, 2011. http://dx.doi.org/10.4133/1.3614140.

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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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McKean, Adam P., and Zachary W. Anderson. "NEW GEOLOGIC MAPPING OF THE SALT LAKE VALLEY." In 72nd Annual GSA Rocky Mountain Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020rm-346342.

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Reports on the topic "Lake Valley"

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Clark, Donald L., Stefan M. Kirby, and Charles G. Oviatt. Geologic Map of the Rush Valley 30' X 60' Quadrangle, Tooele, Utah, and Salt Lake Counties, Utah. Utah Geological Survey, 2023. http://dx.doi.org/10.34191/m-294dm.

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The Rush Valley 30' x 60' quadrangle extends southwest and west from the greater Salt Lake City–Provo metropolitan area with land use varied between public, military, Indian reservation, and private. This 1:62,500-scale geologic map will aid the proper management of land, water, and other resources. The map area lies within the eastern Basin and Range Province. Mountain ranges are composed of unexposed basement rocks overlain by exposed Neoproterozoic through Triassic rocks that are about 10.4 miles (16.8 km) thick, and by numerous Tertiary sedimentary and volcanic units (~47 to 20 Ma). The in

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McKean, Adam P., and Zachary W. Anderson. Interim Geologic Map of the Salt Lake City North Quadrangle, Salt Lake and Davis Counties, Utah. Utah Geological Survey, 2024. http://dx.doi.org/10.34191/ofr-768dm.

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The Salt Lake City North 7.5′ quadrangle is located in Salt Lake and Davis Counties from downtown Salt Lake City on the east to the Salt Lake International Airport on the west and extends north into Davis County to include the southern parts of the City of Bountiful and City of Woods Cross. The southern boundary of the quadrangle is at approximately 900 South Street in Salt Lake City. The quadrangle contains downtown Salt Lake City, the State Capitol building, the City of North Salt Lake, agricultural land, a number of oil refineries, a part of the Farmington Bay Waterfowl Management Area, and

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Taite, S. P. Deformation in the Parsnip River Valley, McLeod Lake map area, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127460.

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Mitchell, Corey, Linda Allison, Corey Mitchell, and Linda Allison. Desert tortoise inventory at Lake Mead National Recreation Area: 2022 line distance sampling surveys. National Park Service, 2024. http://dx.doi.org/10.36967/2304840.

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The Mojave desert tortoise (Gopherus agassizii) inhabits the Mojave and Colorado Deserts in the southwestern United States. The Lake Mead National Recreation Area (NRA) spans the Colorado River corridor in Arizona and Nevada and sits at an ecologically important intersection of the listed and unlisted Mojave tortoise populations. A large portion of the Lake Mead NRA contains suitable desert tortoise habitat, but no contemporary estimates of population densities exist for different areas of the recreation area. Three of the long-term range-wide monitoring strata overlap the Lake Mead NRA: Eldor

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Kerr, D. E. Reconnaissance surficial geology, Beechey Lake, Nunavut, NTS 76-G. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329669.

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Preliminary mapping studies of Beechey Lake map area, through aerial photograph interpretation and limited legacy data, improve our understanding of surficial sediments and glacial history. The area is dominated by glacially and meltwater-scoured bedrock, hummocky moraine, till of varying thickness occasionally streamlined, and thin ridged till. Glacial lake sediments are predominantly in river valley lowlands. Glaciolacustrine delta and raised beach elevations range from 410 m to 230 m and 440 m to 290 m, respectively. Glaciofluvial deposits consist of eskers, ice-contact mounds, proglacial o

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Benson, James R. An Archaeological Reconnaissance of the Over-the-Horizon Radar Project Transmitter Site, Buffalo Flat, Christmas Lake Valley, Lake County, Oregon. Defense Technical Information Center, 1986. http://dx.doi.org/10.21236/ada196559.

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Cross, Julian. Glacial Meltwater Modeling to Simulate Lake Water Budget (1996-2013) in Taylor Valley, Antarctica. Portland State University Library, 2000. http://dx.doi.org/10.15760/etd.7237.

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Hylland, Michael D., Adam I. Hiscock, Greg N. McDonald, et al. Paleoseismic Investigation of the Taylorsville Fault at the Airport East Site, West Valley Fault Zone, Salt Lake County, Utah. Utah Geological Survey, 2022. http://dx.doi.org/10.34191/ss-169.

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The West Valley fault zone (WVFZ) and Salt Lake City segment (SLCS) of the Wasatch fault zone comprise Holoceneactive normal faults that bound an intrabasin graben in northern Salt Lake Valley, Utah. Both fault zones have evidence of recurrent Holocene surface-faulting earthquakes. A topic of recent research is the seismogenic relation of the antithetic (subsidiary) WVFZ to the Wasatch fault zone—specifically, to what degree are WVFZ earthquakes independent of slip on the SLCS, or other adjacent segments, of the Wasatch fault zone. To improve paleoseismic data for the WVFZ and better understan

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Hylland, Michael D., Adam I. Hiscock, Greg N. McDonald, et al. Paleoseismic Investigation of the Taylorsville Fault at the Airport East Site, West Valley Fault Zone, Salt Lake County, Utah. Utah Geological Survey, 2022. http://dx.doi.org/10.34191/ss-169.

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Abstract:

The West Valley fault zone (WVFZ) and Salt Lake City segment (SLCS) of the Wasatch fault zone comprise Holoceneactive normal faults that bound an intrabasin graben in northern Salt Lake Valley, Utah. Both fault zones have evidence of recurrent Holocene surface-faulting earthquakes. A topic of recent research is the seismogenic relation of the antithetic (subsidiary) WVFZ to the Wasatch fault zone—specifically, to what degree are WVFZ earthquakes independent of slip on the SLCS, or other adjacent segments, of the Wasatch fault zone. To improve paleoseismic data for the WVFZ and better understan

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Medioli, B. E. Geochemical, grain size, mineralogical and chronological data from three shallow cores in the Red River Valley (Horseshoe Lake, Lake Louise, Manitoba and Salt Lake, North Dakota). Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2001. http://dx.doi.org/10.4095/212741.

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