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The travertine of Carvanno(Brescia)-The lithofacies of travertine of the Carvanno area aredescribed in detail.These deposits form the core of《Morphological Units》located at different altitudes andformed in different times during the Pleistocene.The deposition of the travertine is probably,from the evi-dence of morphological and morphostructural analyses,connected with the circulation of thermomineral wa-ters rising through tectonic contacts on the right of the Degagna Valley.Their subsequent levelling to terracesis due to variations in the base level of the rivers,connected with tectonic movements.
The travertine of Carvanno (Brescia) -The lithofacies of travertine of the Carvanno area aredescribed in detail.These deposits form the core of “Morphological Units” located at different altitudes and formed in different times during the Pleistocene. The deposition of the travertine is probably, from the evi-dence of morphological and morphostructural analyzes, connected with the circulation of thermomineral wa-ters rising through tectonic contacts on the right of the Degagna Valley. Their subsequent leveling to terracesis due to variations in the base level of the rivers, connected with tectonic movements.