File:Geopanorama strada Supino - Santa Serena.jpg

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Italiano: Geopanorama strada Supino - Santa Serena. Il panorama mostra in linee bianche i limiti stratigrafici tra i calcari di diversa età oggi esposti e sedimentati nel corso del Mesozoico dal Giurassico superiore al Cretaceo (da circa 150 a 80 milioni di anni). La linea rossa invece corrisponde alla traccia della faglia la cui mezzafreccia indica il blocco ribassato e la ripetizione dei limiti stratigrafici. Il gradino generato è il prodotto dell'ultima e la più recente delle fasi tettoniche che hanno interessato l'Appennino di cui i Monti Volsci son parte: la distensione. Questa è legata all'assottigliamento della crosta terrestre un tempo in compressione. Nel corso soprattutto del Quaternario (ultimi 2 milioni di anni circa), la distensione dell'Appennino ha permesso la formazione del graben (fossa) della Ciociaria e l'innalzamento definitivo della catena.
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Author Luca Cardello

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current15:32, 2 June 2019Thumbnail for version as of 15:32, 2 June 20196,617 × 2,188 (2.84 MB)Luca Cardello (talk | contribs)Cross-wiki upload from it.wikipedia.org

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