The glaciated catchments of the High Atlas Mountains of Morocco hold a valuable record of Quaternary river behaviour and environmental change. The Tamatert Valley is a small (< 10 km2) headwater tributary of the Rheraya River on the northern slopes of Jebel Toubkal (4167 m a.s.l.), joining the Mizane Valley at the village of Imlil. The geomorphology of the region is defined by steep sided valleys filled by deeply incised alluvial fans. Luminescence dating (feldspar-IRSL, n = 8) of alluvial sediments in the Tamatert Valley, combined with assessment of the morpho-stratigraphy, suggest net river aggradation during the late Pleistocene (~40-10 ka) and incision during the Holocene (
Date of Award | 1 Aug 2022 |
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Original language | English |
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Awarding Institution | - The University of Manchester
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Supervisor | Jamie Woodward (Supervisor) & Philip Hughes (Supervisor) |
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- Flood
- Mediterranean
- Luminescence
- River
- Geomorphology
- High Atlas
- Morocco
- Quaternary
- Debris flow
Records of Quaternary River Behaviour in Glaciated Catchments of the High Atlas Mountains, Morocco
Hann, M. (Author). 1 Aug 2022
Student thesis: Phd