scholarly journals Catastrophic rock avalanches in a glaciated valley of the High Atlas, Morocco: 10Be exposure ages reveal a 4.5 ka seismic event

2014 ◽  
Vol 126 (7-8) ◽  
pp. 1093-1104 ◽  
Author(s):  
P. D. Hughes ◽  
D. Fink ◽  
W. J. Fletcher ◽  
G. Hannah
Keyword(s):  
Seismic Event ◽  
High Atlas ◽  
Rock Avalanches ◽  
Glaciated Valley ◽  
Exposure Ages

scholarly journals Timing of Pleistocene glaciations in the High Atlas, Morocco: New 10Be and 36Cl exposure ages

2018 ◽  
Vol 180 ◽  
pp. 193-213 ◽  
Author(s):  
Philip D. Hughes ◽  
David Fink ◽  
Ángel Rodés ◽  
Cassandra R. Fenton ◽  
Toshiyuki Fujioka
Keyword(s):  
Pleistocene Glaciations ◽  
High Atlas ◽  
Exposure Ages

A catastrophic Late Pleistocene debris flow sourced in the glaciated High Atlas of Morocco

2020 ◽  
Author(s):  
Madeleine Hann ◽  
Jamie Woodward ◽  
Philip Hughes ◽  
Edward Rhodes
Keyword(s):  
Debris Flow ◽  
Late Pleistocene ◽  
Landscape Change ◽  
Source Area ◽  
Luminescence Dating ◽  
Catastrophic Events ◽  
High Atlas ◽  
Mountain Environments ◽  
Tectonically Active ◽  
Exposure Ages

<p>Catastrophic events such as debris flows and big floods are important agents of landscape change in steepland mountain environments. These events can be prominent in paraglacial settings as well as those that are tectonically active.   Since such catastrophic events pose  a significant natural hazard in deglaciating modern settings (e.g. Haeberli et al. 2017), it is useful to better understand analogous events in the recent geological past.<br><br>The Tamatert Valley, near the village of Imlil, on the northern slopes of Jebel Toubkal (4167 m a.s.l.) in the High Atlas, holds a valuable record of Quaternary landscape change.  The steepland Tamatert Valley was glaciated during the Pleistocene (Hughes et al. 2018)  and lies on the major Tizi n’Test Fault Zone.<br><br>More than 200 well rounded basalt mega-boulders (>2m b axis) have been mapped in the Tamatert Valley catchment (9 km2). Many of the boulders are larger than 5 m (b axis). The mega-boulders are found in the active channel of the Tamatert River, stranded above the modern channel, and embedded in valley-fill deposits. A preliminary chronological framework, combining cosmogenic exposure and luminescence dating, points to deposition of these boulders in the Late Pleistocene. The boulders are porphyritic basalt and lithologically distinct from the local diorite/granite bedrock.  They were transported by a catastrophic flood or debris flow over a distance of more than 3 km from the glaciated basalt source area.<br><br>Serendipitously, a debris flow producing a similarly extensive deposit of boulders (up to 3 m b axis) occurred in the neighbouring Mizane Valley in September 2019. Mapping of this modern deposit allows direct comparison with the Late Pleistocene event. Together, these provide valuable insights into the geomorphological significance of high magnitude, large boulder transit events in glaciated, steepland river catchments in the High Atlas. <br><br>Haeberli, W., Schaub, Y. & Huggel, C. 2017. Increasing risks related to landslides from degrading permafrost into new lakes in de-glaciating mountain ranges. Geomorphology, 293, 405–417<br>Hughes, P.D., Fink, D., Rodés, Á., Fenton, C.R. & Fujioka, T. 2018. Timing of Pleistocene glaciations in the High Atlas, Morocco: New10Be and36Cl exposure ages. Quaternary Science Reviews, 180, 193–213</p>

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