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 language | English |
|---|---|
| Pages (from-to) | 1621-1632 |
| Number of pages | 12 |
| Journal | Bulletin of the Geological Society of America |
| Volume | 112 |
| Issue number | 10 |
| DOIs | |
| Publication status | Published - 2000 |
Keywords
- Dating
- Glaciers
- Himalaya
- Last glacial maximum
- Monsoons
- Mount Everest
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