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Asher P Schick

Biographic Data

ID4054655
NAMEAsher P Schick
GIVEN NAMESAsher P
FAMILY NAMESchick
SIGNATURESCHICK A P
AFFILIATIONSUniversity of Arizona
VERIFIEDNo
TOTAL WORKS3
TOTAL CITATIONS1
WORKS AS AUTHOR3
WORKS AS EDITOR0
FIRST PUBLICATION YEAR1964
LATEST PUBLICATION YEAR1984
H-INDEX1
  • Research Contributions to the Physical Geography of Israel

    C Vita-Finzi, Claudio Vita‐finzi et al.•ARTICLE•Geographical Journal•1984

  • Impact of Climatic Change on an Arid Watershed

    Open Access•William B Bull, Asher P Schick•ARTICLE•Quaternary Research•1979

    The Nahal Yael basin is underlain chiefly by schist, amphibolite, and granite. Thin (generally

  • Thorne Cave, Northeastern Utah

    Open Access•Harold E Malde, Asher P Schick•ARTICLE•American Antiquity•1964•Cited by: 1•References: 18

    Geologic interest in Thorne Cave stems from its link with valley alluvium along Cliff Creek, which accumulated to a height of 48 ft., continued to build up another 13 ft. while men lived here, and then reached 30 ft. higher - sealing in the signs of man. Mineralogic study shows that ground water then circulated through the cave deposits for a considerable time. The alluvium is correlated with the lower part of the Tsegi Formation of the Navajo co…

  • Thorne Cave, Northeastern Utah

    Open Access•Harold E Malde, Asher P Schick•ARTICLE•American Antiquity•1964•Cited by: 1•References: 18

    Geologic interest in Thorne Cave stems from its link with valley alluvium along Cliff Creek, which accumulated to a height of 48 ft., continued to build up another 13 ft. while men lived here, and then reached 30 ft. higher - sealing in the signs of man. Mineralogic study shows that ground water then circulated through the cave deposits for a considerable time. The alluvium is correlated with the lower part of the Tsegi Formation of the Navajo co…

  • Thorne Cave, Northeastern Utah

    Open Access•Harold E Malde, Asher P Schick•ARTICLE•American Antiquity•1964•Cited by: 1•References: 18

    Geologic interest in Thorne Cave stems from its link with valley alluvium along Cliff Creek, which accumulated to a height of 48 ft., continued to build up another 13 ft. while men lived here, and then reached 30 ft. higher - sealing in the signs of man. Mineralogic study shows that ground water then circulated through the cave deposits for a considerable time. The alluvium is correlated with the lower part of the Tsegi Formation of the Navajo co…

  • Impact of Climatic Change on an Arid Watershed

    Open Access•William B Bull, Asher P Schick•ARTICLE•Quaternary Research•1979

    The Nahal Yael basin is underlain chiefly by schist, amphibolite, and granite. Thin (generally

  • Research Contributions to the Physical Geography of Israel

    C Vita-Finzi, Claudio Vita‐finzi et al.•ARTICLE•Geographical Journal•1984

Geology (3 works) · Paleontology (3 works) · Alluvium (2 works) · Archaeology (2 works) · Geography (2 works) · Geology (2 works) · Geomorphology (2 works) · Hydrology and Sediment Transport Processes (2 works) · Paleontology (2 works) · Pleistocene (2 works)

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