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Geomorphological map of the Val Miller and the Baitone area(Adamello Group).Magmatic intru-sive rocks(Western Adamello Tonalite,diorite and gabrodiorite,with related dykes)outcrop in this region.Contact metamorphic rocks are also known from the Baitone area.The present physionomy of the valley is related to various morpbogenetic agents.Those that acted for a longertime and more deeply are the glacial and periglacial ones.Typical erosional and depositional glacial forms arepresent all over the region.On the basis of morphological,stratigraphical,textural observations and of theweathering of the deposits as well as the degree of lichenization and the soil development,the Authors tried todifferenziate the various glacial deposits.The last century moraines and those of the Late Pleistocene are easyto distinguish.Landforms related to periglacial environments such as rock-glaciers,protalus ramparts,avalan-che tracks and cones have been recognized.Recent debris-flow lobes are present in the Malga Valley restingon stabilized debris and dejection cones.
Geomorphological maps of the Val Miller and the Baitone area (Adamello Group). Magmatic intru-sive rocks (Western Adamello Tonalite, diorite and gabrodiorite, with related dykes) outcrop in this region. Contact metamorphic rocks are also known from the Baitone area. present physionomy of the valley is related to various morpbogenetic agents. Those that acted for a longertime and more deeply are the glacial and periglacial ones. Tipical erosional and depositional glacial forms are present all over the region. On the basis of morphological, stratigraphical, textural observations and of the weathering of the deposits as well as the degree of lichenization and the soil development, the Authors tried todifferenziate the various glacial deposits. The last century moraines and those of the Late Pleistocene are easy to distinguish. Landforms related to periglacial environments such as rock- glaciers, protalus ramparts, avalan-che tracks and cones have been recognized. Recover debris-flow lobes are present in the M alga Valley restingon stabilized debris and dejection cones.