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 |  ÇáÕÝÍÉ ÇáÑÆíÓíÉ  |  ãÜä äÜßÜæä ¿  |  ÌíÜæáÌíÜÇ ÇáÌÒÇÆÑ  |  ÝÜÖÜÇÁ ÇáãÓÜÊÜËÜãÜÑ  |  ÇáÊÑæíÌ ÈÇáãæÇÞÚ ÇáãäÌãí  |  ÇáäÔÇØÇÊ ÇáãäÌãíÉ  |  ÃÍÜÏÇË ÇáÓÜÇÚÜÉ  |
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        ÃÍÜÏÇË åÜÇãÜÉ

ÌíÜæáÌíÜÇ ÇáÌÒÇÆÑ

ÌíæáæÌíÇ ãäØÞÉ ÅÞáÇÈ

             
 
The solid mass of Eglab is the field of the formations of Superior Réguibat Complex. It primarily granitic and volcanic, is covered in the south by the sedimentary formations with Hank. One distinguishes, of West in East:

• the Western zone Chegga-Iguidi,field of the residual formations of the basic system (series and granites of Chegga);

• the central zone Aftout-Eglab field of Aftout Pluto surmounted by the series of the Souss Wadi where no witness of the basic metamorphic system appears;

• the zone Is Chenachane-erg Chech where terms of the basic system reappear within Aftout Pluto.


 
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