Open Access

Fig. 1


Download original image

Geographical and geological map of the studied region (Dubourdieu, 1956). The morsott profiles studied are located in a sedimentary basin, consisting mainly of the Cretaceous formations covered by fluvio-lacustrine deposits of quaternary age. These quaternary deposits come from several phases of alterations and erosions, these different phases produced a coarse and fine material, and which was deposited on the slopes and plains forming a cover for the old lands.

Current usage metrics show cumulative count of Article Views (full-text article views including HTML views, PDF and ePub downloads, according to the available data) and Abstracts Views on Vision4Press platform.

Data correspond to usage on the plateform after 2015. The current usage metrics is available 48-96 hours after online publication and is updated daily on week days.

Initial download of the metrics may take a while.