Abstract
300MW Baspa II is India's largest private hydroelectric facility, located at the Baspa River which is an important left-hand tributary to the Sutlej River in the NW Himalaya (India). In this valley the Sangla palaeo-lake has been dammed around 8200yr BP behind a rock-avalanche dam and Baspa II is located exactly on top of this palaeo-lake. This special location represents a very rare possibility to evaluate the short-term, river load and hydrological parameters measured during the planning and operational stages of Baspa II with the long-term parameters gained from the palaeo-lake sediments from the catchment. Sedimentological and geomorphological investigations of the lacustrine sediments have been used to reconstruct environmental changes during >2500years of its existence. The Mid-Holocene erosion rates of the Baspa catchment estimated from the volume and duration of deposition of the exposed lake sediments are at 0.7-1.0mmyr -1, almost identical with the modern erosion rates calculated from river gauge data from Baspa II. Several charcoal layers and charcoal pieces from the uppermost palaeo-lake levels around 5000calyr BP might be related to woodland clearance and they possibly represent one of the oldest evidences for human presence in the Baspa Valley during Neolithic time.
| Original language | English |
|---|---|
| Pages (from-to) | 157-172 |
| Number of pages | 16 |
| Journal | Journal of Asian Earth Sciences |
| Volume | 90 |
| Early online date | 26 Apr 2014 |
| DOIs | |
| Publication status | Published - 15 Aug 2014 |
Austrian Fields of Science 2012
- 105117 Palaeobotany
- 105101 General geology
- 601021 Prehistory
- 105404 Geomorphology
Keywords
- Erosion
- Lake sediments
- Landslide-dammed lake
- Palynology
- River load
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