Fig. 17c
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Agrandissement du second cadre rouge. Dans l’amont du système, une perte s’est formée (PR) par capture d’un ruisseau aérien dans un fantôme de roche vidé. L’érosion élimine de plus en plus d’altérite. La circulation s’est amorcée, qui évoluera vers une connexion perte-résurgence, laquelle évoluera ensuite sur un mode fluviatile. Un affaissement s’amorce avec basculement des arbres et soutirage de la formation de couverture (AF).
Enlargement of the second red box. In the upstream of the system, a swallow hole has captured a surface river (PR) in an emptied ghostrock. The erosion brings more and more residual alterite. The underground flow has been initiated to a connection swallow hole – resurgence. After the erosion of the alterite, we obtain a speleological connection by an underground river. A collapse begins with a destabilization of trees and decanting of the overburden formation (AF).
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