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Haut Atlas occidental - Columbia University

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CIRCUIT C11 : HAUT ATLAS OCCIDENTAL<br />

FIG. 3.8 : Localisation des arrêts dans les structures salifères.<br />

FIG. 3.8 : Location of stops in the salt structures.<br />

47<br />

FIG. 3.9 : Le pli à noyau salifère<br />

du J. Amsittene.-A : Vue vers le<br />

nord-est depuis la route nationale<br />

N1.- B : Vue du cœur de l’anticlinal<br />

d’Amsittene aux salines<br />

d’Arich Ouzla. Au premier plan,<br />

les calcaires d’Arich Ouzla, premiers<br />

dépôts marins jurassiques<br />

du <strong>Haut</strong> <strong>Atlas</strong> <strong>occidental</strong>, remontés<br />

en partie par le diapirisme.<br />

FIG. 3.9 : The J. Amsittene fold,<br />

with salt core.-A : View to the<br />

north-east from the Agadir-Essaouira.highway.-<br />

B : View of the<br />

core of the Amsittene anticline at<br />

the Arich Ouzla salina. Front<br />

view, first Jurassic marine deposits<br />

of the Western High <strong>Atlas</strong>,<br />

uplifted through diapirism.

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