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On notera la différence d'´ epaisseur des dépôts molassiques sur les deux profils : la base de la formation Isnotú (Miocène moyen) estàest`està 3.5 s (TWT) sur le profil du flanc NW, alors que la base du Miocène estàest`està 1.3 s (TWT) sur le profil du flanc SE, 1997. ,
Plusieurs séismes historiques ontétéontété attribués ` a la faille, Mérida en 1812 (intensité X) et La Grita en 1932 (intensité IX) (Audemard, p.36, 1997. ,
Carte du bassin montrant sa forme rhomboédrique se développant entre deux branches de la faille de Boconó Le bassin est entaillé par le rio Chamá le long de sa bordure méridionale et par plusieurs quebradas (Qda) orientées N-S. (B) Vue en perspective du bassinàbassin`bassinà partir d'un MNT SRTM. Le bassin forme une dépression dont l'altitude est comprise entre 600 et 1000 m. Il est surplombé par des sommets qui atteignent plus de 2500 m, p.41 ,
En haut : Les facettes triangulaires du bord sud du bassin sont soulignées par la forte incision desrivì eres (Image Landsat Mister SID drapée sur un MNT SRTM) En bas : Photographie d'une facette triangulaire ,