Geomorphology of the thakkhola-muktinath region, central nepal, and its late quaternary history
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概要
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Glacial and mass-movement landforms, river terraces, and the sediments forming these landforms were surveyed in the field, and the origin, relative chronology and crustal movement were discussed in the upper basin of the Kali Gandaki River. Large scale land-slides and glacial deposits around Larjung played an important role for making up the geomorphology of the Thakkhola basin: These landslides made a distinct basin-form and the glacier deposits dammed up the Kali Gandaki and then formed the Paleo Marpha Lake, in which the Marpha Formation accumulated. These occurred in the Pre-Last Interglacial period. The Marpha Formation was entrenched and filled with fluvioglacial materials in the Early and Late Substages of the Last Glacial.
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