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Timing of late quaternary glaciations South of Mount Everestin the Khumbu Himal, Nepal

  • B. W.M. Richards
  • , D. I. Benn*
  • , L. A. Owen
  • , E. J. Rhodes
  • , J. Q. Spencer
  • *Corresponding author for this work

    Research output: Contribution to journalArticlepeer-review

    Abstract

    Moraines south of Mount Everest in the Khumbu Himal were dated using optically stimulated luminescence. Clustering of ages and morphostratigraphy allowed three advances to be dated: (1) The Periche Glacial Stage (ca. 18-25 ka), (2) the Chhukung Glacial Stage (ca. 10 ka), and (3) the Lobuche Stage (ca. 1-2 ka). The Periche Stage is coincident with Oxygen Isotope Stage 2; the Chhukung Stage represents a late glacial or early Holocene glacial advance; and the Lobuche Stage is a late Holocene glacial advance that predates the Little Ice Age.

    Original languageEnglish
    Pages (from-to)1621-1632
    Number of pages12
    JournalBulletin of the Geological Society of America
    Volume112
    Issue number10
    DOIs
    Publication statusPublished - 2000

    Keywords

    • Dating
    • Glaciers
    • Himalaya
    • Last glacial maximum
    • Monsoons
    • Mount Everest

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