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Toubkal Massif

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Major faults in the <b>Toubkal</b> <b>Massif</b> showing relationship with rock slope fai...
Published: 01 July 2014
Figure 1. Major faults in the Toubkal Massif showing relationship with rock slope failure deposits in the Assif n’Imserdane valley and at Lac d’Ifni. Redrawn from Delcaillau et al. (2011) with permission of Elsevier.
Series: Geological Society, London, Special Publications
Published: 01 January 2017
EISBN: 9781862399655
... moraine unit was formed by a small niche glacier that was present as recently as the mid-twentieth century. The Pleistocene glaciers are likely to have been associated with wetter conditions than today and colder air temperatures. Combined with ice in neighbouring areas, such as the Toubkal massif, the SW...
Series: GSA Special Papers
Published: 01 January 2007
DOI: 10.1130/2007.2423(02)
... sampling has been performed for the volcanic products of the lower basaltic pile and also of the Early Cambrian strata, in the Agoundis-Ounein region. Detailed investigations of the structural relationships between the basaltic pile and the underlying rhyolitic complex have been done in the Toubkal massif...
Journal Article
Journal: GSA Bulletin
Published: 01 July 2014
GSA Bulletin (2014) 126 (7-8): 1093-1104.
...Figure 1. Major faults in the Toubkal Massif showing relationship with rock slope failure deposits in the Assif n’Imserdane valley and at Lac d’Ifni. Redrawn from Delcaillau et al. (2011) with permission of Elsevier. ...
FIGURES | View All (12)
Series: Geological Society, London, Special Publications
Published: 01 January 2017
EISBN: 9781862399655
... glaciers tens of kilometres long. Other massifs sustained only small-scale ice masses, although this was the exception rather than the norm. Glaciers still exist today and there is evidence that small glaciers were a common sight in many regions during the Little Ice Age. The Mediterranean mountains...
Series: Geological Society, London, Special Publications
Published: 01 January 2008
DOI: 10.1144/SP297.15
EISBN: 9781862395459
... of the Agoundis–Ounein and Toubkal formation of Adoudounian type; ( IV ) Anti-Atlas region of the other Adoudounian formations. 2, outcrops of Late Ediacaran to Middle Cambrian volcanic rocks, in addition to the Ifri–Azegour and Ouzaga–Tizzirt areas: A, Agoundis-Ounein and Toubkal; B, Djbel Boho; C, Waoufengha...
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Series: Geological Society, London, Special Publications
Published: 01 January 2003
DOI: 10.1144/GSL.SP.2003.207.4
EISBN: 9781862394551
... a pulse of minor, but regionally extensive, inversion which reworked earlier normal faults. The inversion is most important at the edges of the Illizi and Murzuk basins ( Echikh 1998 ). Basin inversion occurred along the eastern edge of the Hoggar Massif and across the Gargaf Arch. In the Murzuk Basin...
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