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Jonathan O Davis

Biographic Data

ID5652967
NAMEJonathan O Davis
GIVEN NAMESJonathan
FAMILY NAMEO Davis
SIGNATUREDAVIS J O
AFFILIATIONSDesert Research Institute
VERIFIEDNo
TOTAL WORKS4
TOTAL CITATIONS0
WORKS AS AUTHOR4
WORKS AS EDITOR0
FIRST PUBLICATION YEAR1983
LATEST PUBLICATION YEAR1992
H-INDEX0
  • Dating Late Pleistocene Pluvial Events and Tephras by Correlating Paleomagnetic Secular Variation Records from the Western Great Basin

    Open Access•Robert M Negrini, Jonathan O Davis•ARTICLE•Quaternary Research•1992

    Paleomagnetic 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 stratigra…

  • Dating volcanic ash by thermoluminescence

    Open Access•Glenn W Berger, Jonathan O Davis•ARTICLE•Quaternary International•1992

  • Correlation of Late Quaternary Tephra Layers in a Long Pluvial Sequence near Summer Lake, Oregon

    Open Access•Jonathan O Davis•ARTICLE•Quaternary Research•1985

    Near Summer Lake in southern Oregon, 54 tephra beds of late Quaternary age are exposed in pluvial lake sediments of Lake Chewaucan. Seven of the tephra beds near the top can be correlated with tephra deposits younger than 117,000 yr at Mount St. Helens, Washington, at Crater Lake, Oregon, and in northwestern Nevada in the deposits of pluvial Lake Lahontan. However, most of the section at Summer Lake lies below the correlated units, and contains 3…

  • Level of Lake Lahontan during Deposition of the Trego Hot Springs Tephra about 23,400 years ago

    Open Access•Jonathan O Davis•ARTICLE•Quaternary Research•1983

    The Trego Hot Springs tephra bed is a silicic tephra about 23,400 yr old, found at several localities in pluvial lake sediments in northern Nevada, southern Oregon, and northeastern California. It has been characterized petrographically, by the major and minor element chemistry of its glass, and by its stratigraphic position with respect to other tephra layers. At a newly described locality on Squaw Creek, northwest of Gerlach, Nevada, at the nor…

No prominent works on this page.

  • Level of Lake Lahontan during Deposition of the Trego Hot Springs Tephra about 23,400 years ago

    Open Access•Jonathan O Davis•ARTICLE•Quaternary Research•1983

    The Trego Hot Springs tephra bed is a silicic tephra about 23,400 yr old, found at several localities in pluvial lake sediments in northern Nevada, southern Oregon, and northeastern California. It has been characterized petrographically, by the major and minor element chemistry of its glass, and by its stratigraphic position with respect to other tephra layers. At a newly described locality on Squaw Creek, northwest of Gerlach, Nevada, at the nor…

  • Correlation of Late Quaternary Tephra Layers in a Long Pluvial Sequence near Summer Lake, Oregon

    Open Access•Jonathan O Davis•ARTICLE•Quaternary Research•1985

    Near Summer Lake in southern Oregon, 54 tephra beds of late Quaternary age are exposed in pluvial lake sediments of Lake Chewaucan. Seven of the tephra beds near the top can be correlated with tephra deposits younger than 117,000 yr at Mount St. Helens, Washington, at Crater Lake, Oregon, and in northwestern Nevada in the deposits of pluvial Lake Lahontan. However, most of the section at Summer Lake lies below the correlated units, and contains 3…

  • Dating Late Pleistocene Pluvial Events and Tephras by Correlating Paleomagnetic Secular Variation Records from the Western Great Basin

    Open Access•Robert M Negrini, Jonathan O Davis•ARTICLE•Quaternary Research•1992

    Paleomagnetic 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 stratigra…

  • Dating volcanic ash by thermoluminescence

    Open Access•Glenn W Berger, Jonathan O Davis•ARTICLE•Quaternary International•1992

Geology and Paleoclimatology Research (4 works) · Pluvial (4 works) · Tephra (4 works) · Volcano (4 works) · Geochemistry (3 works) · Geology (3 works) · Geomorphology (3 works) · Paleontology (3 works) · Pleistocene (3 works) · Geological formations and processes (2 works)

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