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George Odell Bachman

Biographic Data

ID6400388
NAMEGeorge Odell Bachman
GIVEN NAMESGeorge Odell
FAMILY NAMEBachman
SIGNATUREBACHMAN G O
VERIFIEDNo
TOTAL WORKS7
TOTAL CITATIONS11
WORKS AS AUTHOR7
WORKS AS EDITOR0
FIRST PUBLICATION YEAR1953
LATEST PUBLICATION YEAR1985
H-INDEX2
  • Assessment of near-surface dissolution at and near the Waste Isolation Pilot Plant (Wipp), southeastern New Mexico

    George Odell Bachman•REPORT•1985

    The area at and near the WIPP site was examined for evidence of karst development on the geomorphic surface encompassing the site. Certain surficial depressions of initial concern were identified as blowouts in sand dune fields (shallow features unrelated to karstification). An ancient stream system active more than 500,000 yr ago contained more water than any system since. During that time (Gatuna, Middle Pleistocene), many karst features such a…

  • Geology of the Bear Peak area, Dona Ana County, New Mexico

    George Odell Bachman, Donald A Myers•REPORT•1969•References: 1

    The Bear Peak area, in south-central New Mexico at the south end of the San Andres Mountains, includes structural elements of both the westward-dipping San Andres Mountains and the Organ Mountain igneous mass.Rocks exposed in the area range in age from Precambrian to Recent.The Precambrian rocks include schist, quartzite, granite, and associated rocks.Paleozoic rocks, which make up much of the mountain mass, include the Bliss Sandstone of Late Ca…

  • Preliminary geologic map of the northeastern part of New Mexico

    George Odell Bachman, C H Dane•REPORT•1962•Cited by: 1

  • Preliminary geologic map of the southwestern part of New Mexico

    C H Dane, George Odell Bachman•REPORT•1961•Cited by: 6

  • Preliminary geologic map of the southeastern part of New Mexico

    C H Dane, George Odell Bachman•REPORT•1958

  • Preliminary geologic map of the northwestern part of New Mexico

    C H Dane, George Odell Bachman•REPORT•1957•Cited by: 3

  • Geology of a part of northwestern Mora County, New Mexico

    George Odell Bachman•REPORT•1953•Cited by: 1

  • Preliminary geologic map of the southwestern part of New Mexico

    C H Dane, George Odell Bachman•REPORT•1961•Cited by: 6

  • Preliminary geologic map of the northwestern part of New Mexico

    C H Dane, George Odell Bachman•REPORT•1957•Cited by: 3

  • Preliminary geologic map of the northeastern part of New Mexico

    George Odell Bachman, C H Dane•REPORT•1962•Cited by: 1

  • Geology of a part of northwestern Mora County, New Mexico

    George Odell Bachman•REPORT•1953•Cited by: 1

  • Geology of a part of northwestern Mora County, New Mexico

    George Odell Bachman•REPORT•1953•Cited by: 1

  • Preliminary geologic map of the northwestern part of New Mexico

    C H Dane, George Odell Bachman•REPORT•1957•Cited by: 3

  • Preliminary geologic map of the southeastern part of New Mexico

    C H Dane, George Odell Bachman•REPORT•1958

  • Preliminary geologic map of the southwestern part of New Mexico

    C H Dane, George Odell Bachman•REPORT•1961•Cited by: 6

  • Preliminary geologic map of the northeastern part of New Mexico

    George Odell Bachman, C H Dane•REPORT•1962•Cited by: 1

  • Geology of the Bear Peak area, Dona Ana County, New Mexico

    George Odell Bachman, Donald A Myers•REPORT•1969•References: 1

    The Bear Peak area, in south-central New Mexico at the south end of the San Andres Mountains, includes structural elements of both the westward-dipping San Andres Mountains and the Organ Mountain igneous mass.Rocks exposed in the area range in age from Precambrian to Recent.The Precambrian rocks include schist, quartzite, granite, and associated rocks.Paleozoic rocks, which make up much of the mountain mass, include the Bliss Sandstone of Late Ca…

  • Assessment of near-surface dissolution at and near the Waste Isolation Pilot Plant (Wipp), southeastern New Mexico

    George Odell Bachman•REPORT•1985

    The area at and near the WIPP site was examined for evidence of karst development on the geomorphic surface encompassing the site. Certain surficial depressions of initial concern were identified as blowouts in sand dune fields (shallow features unrelated to karstification). An ancient stream system active more than 500,000 yr ago contained more water than any system since. During that time (Gatuna, Middle Pleistocene), many karst features such a…

Archaeology (7 works) · Archaeology and Natural History (7 works) · Geography (7 works) · Geology (7 works) · Botany, Ecology, and Taxonomy Studies (6 works) · Cartography (4 works) · Geologic map (4 works) · Rangeland and Wildlife Management (4 works) · Geology and Paleoclimatology Research (3 works) · Geochemistry (2 works)

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