A FACILITY OF THE                                                        RESEARCH INFRASTRUCTURE

Tinerhir

The site consists of a small basaltic unit that expands within a large valley. The “flood basalt” originates in a fault along the northern slope of the valley and occurs at the top of a dissected plateau. The unit is a prominent feature along the large valley west of Tinerhir and its colour contrasts with the predominant calcareous lithologies.

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