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Late Pleistocene Glaciation of Mono Basin, California

Published online by Cambridge University Press:  20 January 2017

Marcus I. Bursik  and
Alan R. Gillespie
Marcus I. Bursik
Affiliation:
Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109
Alan R. Gillespie
Affiliation:
Remote Sensing Laboratory, University of Washington, Seattle, Washington 98195
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Abstract

Moraines in the canyons of Mono Basin are separable into relative-age groups on the basis of clast-sound velocities in exposed boulders, moraine morphology, and weathering features on boulder surfaces. Tioga, Tenaya, Tahoe, and Mono Basin moraine deposits each have distinct weathering characteristics and therefore constitute different relative-age groups. The Tioga glacial episode at June Lake may postdate ∼25,200(?)-yr-old basaltic lavas, and the Tenaya episode may have occurred ∼30,700 yr ago. A comparison of the glacial and lacustrine records of Mono Basin over the past 40,000 yr, based on new interpretations of radiometric ages, is consistent with the hypothesis that maximum glacial and maximum pluvial periods were not necessarily synchronous.

Type
Articles
Information
Quaternary Research , Volume 39 , Issue 1 , January 1993 , pp. 24 - 35
Copyright
University of Washington

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References

Bailey, R. A. (1989). “Geologic Map of the Long Valley Caldera, Mono-Inyo Craters Volcanic Chain, and Vicinity, Eastern California. U.S. Geological Survey Miscellaneous Investigations Series Map 1–1933.Google Scholar
Bard, E. Hamelin, B. Fairbanks, R. G., and Zindler, A. (1990). Calibration of the carbon timescale over the past 30,000 years using mass spectrometric U-Th ages from Barbados corals. Nature 345, 405–410.Google Scholar
Benson, L. V. Currey, D. R. Dorn, R. I. Lajoie, K. R. Oviatt, C. G. Robinson, S. W. Smith, G. I., and Stine, S. (1990). Chronology of expansion and contraction of four Great Basin lake systems during the past 35,000 years. Paleogeography, Paieoclimatology, Pa~ leoecology 78, 241–286.Google Scholar
Bierman, P., and Gillespie, A. R. (1991). Range fires: A significant factor in exposure-age determination and geomorphic surface evolu-tion. Geology 19, 641–644.Google Scholar
Birkeland, P. W. (1984). “Soils and Geomorphology.” Oxford Univ. Press, New York.Google Scholar
Birkeland, P. W., and Burke, R. M. (1988). Soil catena chronose-quences on eastern Sierra Nevada moraines, California U.S.A. Arctic and Alpine Research 20, 473–484.CrossRefGoogle Scholar
Birman, J. H. (1964). “Glacial Geology across the Crest of the Sierra Nevada, California.” Geological Society of America Special Paper 75.CrossRefGoogle Scholar
Blackwelder, E. (1931). Pleistocene glaciation in the Sierra Nevada and Basin Ranges. Geological Society of America Bulletin 42, 865–922.CrossRefGoogle Scholar
Burke, R. M., and Birkeland, P. W. (1979). Reevaluation of multipa-rameter relative dating techniques and their application to the glacial sequence along the eastern escarpment of the Sierra Nevada, Cali-fornia. Quaternary Research 11, 21–51.CrossRefGoogle Scholar
Bursik, M. I. (1988). “Late Quaternary Volcano-Tectonic Evolution of the Mono Basin, Eastern California.” Unpublished Ph.D. dissertation, California Institute of Technology.Google Scholar
Bursik, M. I. (1991). Relative dating of moraines based on landform degradation, Lee Vining Canyon, California. Quaternary Research 35, 451–455.CrossRefGoogle Scholar
Bursik, M., and Sieh, K. (1989). Range front faulting and volcanism in the Mono Basin, eastern California. Journal of Geophysical Research 94, 15587–15609.Google Scholar
Chesterman, C. W., and Gray, C. H. Jr. (1975). “Geology of the Bodie Quadrangle, Mono County, California.” California Division of Mines and Geology, Map Sheet 21.Google Scholar
Clark, M. M. (1976). Evidence for rapid destruction of latest Pleistocene glaciers of the Sierra Nevada, California. Geological Society of America Abstracts with Programs, Corditteran Section 8, 361–362.Google Scholar
Clark, M. M. (1979). Range-front faulting: Cause of the difference in height between Mono Basin and Tahoe moraines at Walker Creek. In “Field Guide to Relative Dating Methods Applied to Glacial Deposits in the Third and Fourth Recesses and along the Eastern Sierra Nevada, California, with Supplementary Notes on Other Sierra Nevada Localities. Field Trip Guidebook for Friends of the Pleistocene Pacific Cell” (Burke, R. M. and Birkeland, P. W., Eds.), pp. 54–57.Google Scholar
Conca, J. L., and Rossman, G. R. (1982). Case hardening of sandstone. Geology 10, 520–523.Google Scholar
Crook, R. (1986). Relative dating of Quaternary deposits based on p-wave velocities in weathered granitic clasts. Quaternary Research 25, 281–292.Google Scholar
Crook, R., and Gillespie, A. R. (1986). Weathering rates in granitic boulders measured by p-wave speeds. In “Rates of Chemical Weathering of Rocks and Minerals” (Colman, S. M. and Dethier, D. P., Eds.), pp. 395–417. Academic Press, Orlando, FL.Google Scholar
Dorn, R. I. Turrin, B. D. Jull, A. J. T. Linick, T. W., and Donahue, D. J. (1987). Radiocarbon and cation-ration ages for rock varnish on Tioga and Tahoe morainal boulders of Pine Creek, eastern Sierra Nevada, Calif., and their paleoclimatic implications. Quaternary Research 28, 38–49.Google Scholar
Edwards, R. L. Chen, J. H., and Wasserburg, G. J. (1987). 238U-234U-230Th-232Th systematics and the precise measurement of time over the past 500,000 years. Earth and Planetary Science Letters 81, 175–192.Google Scholar
Gillespie, A. R. (1982). “Quaternary Glaciation and Tectonism in the Southeastern Sierra Nevada, Inyo County, California.” Unpublished Ph.D. dissertation, California Institute of Technology.Google Scholar
Gillespie, A. R. (1984). Evidence for both Wisconsin and Illinoian ages for the Tahoe glaciation, Sierra Nevada, California. Geological Society of America Abstracts with Programs 16, 519.Google Scholar
Holm, R. F. (1987). Significance of agglutinate mounds on lava flows associated with monogenetic cones: An example at Sunset Crater, northern Arizona. Geological Society of America Bulletin 99, 319–324.2.0.CO;2>CrossRefGoogle Scholar
Huber, N. K., and Rinehart, C. D. (1965). “Geologic Map of the Devils Postpile Quadrangle, Sierra Nevada, California.” U.S. Geological Survey Map GQ-437.Google Scholar
Jones, J. G. (1970). Intraglarial volcanoes of the Laugarvatn region, southwest Iceland, II. Journal of Geology 78, 127–140.CrossRefGoogle Scholar
Kelleher, P. C. (1986). “The Mono Craters-Mono Lake Islands Volcanic Complex: Evidence for Several Magma Types, Magma Mixing, and a Heterogeneous Source Region.” Unpublished M.S. thesis, University of California, Santa Cruz.Google Scholar
Kesseli, J. E. (1941). Studies in the Pleistocene of the Sierra Nevada, California. University of California Publications in Geography 6, 315–362.Google Scholar
Kistler, R. W. (1966). “Geologic Map of the Mono Craters Quadrangle, Mono and Tuolomne Counties, California.” U.S. Geological Survey Quadrangle Map GQ-462.Google Scholar
Lachmar, T. E. (1977). “Glacial Geology of Lundy, Virginia, and Green Canyons, Mono County, California.” Unpublished M.S. thesis, Purdue University.Google Scholar
Lajoie, K. R. (1968). “Late Quaternary Stratigraphy and Geologic History of Mono Basin, Eastern California.” Unpublished Ph.D. dissertation, University of California, Berkeley.Google Scholar
Lajoie, K. R., and Robinson, S. W. (1982). Late Quaternary glacio-lacustrine chronology, Mono Basin, California. Geological Society of America Abstracts with Programs 14, 179.Google Scholar
Mathieson, S. A. (1984). Comparison of glacial sequences between the Yuba-Feather Divide, northern Sierra Nevada and Mono Basin, central Sierra Nevada, California: Evidence for an lllinoian Tahoe glaci-ation. Geological Society of America Abstracts with Programs 16, 320.Google Scholar
Matthes, F. E. (1930). “Geologic History of the Yosemite Valley.” U.S. Geological Survey Professional Paper 160.Google Scholar
McGee, W. J. (1885). On the meridional deflection of ice streams. American Journal of Science 29, 386–392.CrossRefGoogle Scholar
Mustoe, G. E. (1982). The origin of honeycomb weathering. Geological Society of America Bulletin 93, 108–115.2.0.CO;2>CrossRefGoogle Scholar
Phillips, F. M. Zreda, M. G. Smith, S. S. Elmore, D. Kubik, P. W., and Sharma, P. (1990). Cosmogenic chlorine-36 chronology for glacial deposits at Bloody Canyon, eastern Sierra Nevada. Science 248, 1529–1532.CrossRefGoogle ScholarPubMed
Putnam, W. C. (1949). Quaternary geology of the June Lake district, California. Geological Society of America Bulletin 60, 1281–1302.Google Scholar
Putnam, W. C, (1950). Moraine and shoreline relationships at Mono Lake, California. Geological Society of America Bulletin 61, 115–122.Google Scholar
Russell, I. C. (1889). Quaternary history of the Mono Valley, California. In “U.S. Geological Survey Eighth Annual Report,” pp. 267–394. (Reprinted by Artemisia Press, Lee Vining, CA, 1984.) Google Scholar
Sharp, R. P. (1968). Sherwin Till-Bishop Tuff geological relationships, Sierra Nevada, California. Geological Society of America Bulletin 79, 351–364.Google Scholar
Sharp, R. P. (1969). Semiquantitative differentiation of glacial moraines near Convict Lake, Sierra Nevada, California. Journal of Geology 77, 68–91.Google Scholar
Sharp, R. P., and Birman, J. H. (1963). Additions to the classical sequence of Pleistocene glaciations, Sierra Nevada, California. Geological Society of America Bulletin 74, 1079–1086.Google Scholar