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 ha), and (3) the Lohuche Stage (ca. 1-2 ha). The Periche Stage is coincident with Oxygen Isotope Stage 2; the Chhukung Stage represents a late glacial or early Holocene glacial advance; and the Lohuche Stage is a late Holocene glacial advance that predates the Little Ice Age.
| Original language | English |
|---|---|
| Volume | 112 |
| Publication status | Published - Oct 2000 |
Keywords
- dating
- glaciers
- Himalaya
- Last Glacial Maximum
- monsoons
- Mount Everest
- EQUILIBRIUM-LINE ALTITUDES
- YOUNGER-DRYAS
- ARABIAN SEA
- SUMMER MONSOON
- RONGBUK VALLEY
- LUMINESCENCE
- MORAINES
- CLIMATE
- QUARTZ
- TIBET