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Geology and geomorphology of the Cheria region

Abstract : The region of Chéria is characterized by the juxtaposition of large SW-NE oriented depressions bounded by low narrow djebel systems of uplifted Eocene limestones. A series of five such depressions constitute the region of contact between the High Constantine Plains and the Nemenchas sensu stricto. From west to eats they are : the Ounrhal depression, the Outa Guert-Outa Gassès depression, the Outa Zora-Outa Guibeur depression, the Chéria depression, and the Telidjène depression. Our work has been confined to the latter two.
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Submitted on : Tuesday, June 20, 2017 - 10:04:16 AM
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  • HAL Id : hal-01542749, version 1


Jean-Louis Ballais. Geology and geomorphology of the Cheria region. Libyca, Centre de recherches anthropologiques, préhistoriques et ethnographiques, 1975, pp.49-60. ⟨hal-01542749⟩



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