Al on g th e west ern coa st of Lake of Garda there are morphological and sedimentological evidences of Late Glacial and Holocen e coastlines . One of these (earlier than early Neolithic in date) lies at an altitude of 3-3,8 m above the present medium level of th e lake in the southern Benacus (South of Salo) and at 4-5 m of elevation in the northern zone. A set of ancient, supposed, wave-cut notches can be seen near Manerba between 23 and 60 m above the lake level. During the Holocene the western and southern zones of Lake Garda should have been interested by differentiated areal movements representing the continuation of tectonic activities already developed during the early -middle Pleistocene.
|Autori interni:||BARONI, CARLO|
|Titolo:||Note sulla paleogeografia olocenica della costa occidentale del Lago di Garda. Notes on the Holocene palaeogeography of th e western coast of Lake Garda.|
|Anno del prodotto:||1985|
|Appare nelle tipologie:||1.1 Articolo in rivista|