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Titlebook: Landscapes and Landforms of Italy; Mauro Soldati,Mauro Marchetti Book 2017 Springer International Publishing AG 2017 Alps.Apennines.Island

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Lake Garda: An Outstanding Archive of Quaternary Geomorphological Evolutiony sediments with the archaeological heritage of human frequentation of the area, furnishing a very helpful tool for investigating the paleoclimatic evolution of this region as well as for investigating neotectonic activity.
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Landscapes of Northern Lombardy: From the Glacial Scenery of Upper Valtellina to the Prealpine Lacusdforms—have been selected to illustrate how different landscapes may originate from geomorphological modelling of different lithotypes in different morphogenetic systems. These eight sites are exemplary cases in which significant evidence of past and current climatic and structural conditions characterising this region is exhibited.
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Morphological Regions of Italydscape—even though often strongly diversified within themselves—which resulted from both the conditioning of the geological structure and the predominance of given exogenous processes, in relation to climatic conditions.
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The Glaciers of the Valle d’Aosta and Piemonte Regions: Records of Present and Past Environmental anare analysed for their specific scientific, environmental, cultural and economic importance. The distinctive dynamic nature of the glacial landscape is illustrated by examples of active glacial landforms and related slope instability, whose sensitivity to climate changes can increase hazards and risks.
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The Adamello-Presanella and Brenta Massifs, Central Alps: Contrasting High-Mountain Landscapes and Lface and surface karst landscapes have also developed. Owing to its extraordinary interest and geological-geomorphological value, these massifs are included in the European Geoparks Network and in the World Global UNESCO Network of Geoparks.
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The Dolomite Landscape of the Alta Badia (Northeastern Alps): A Remarkable Record of Geological and ene glaciers profoundly shaped the valleys and, at their retreat, periglacial and gravity-induced processes had a major role in slope modelling. Landslides have affected the valleys since the Lateglacial leaving a clear inprint on the landscape, as well as Man in recent times.
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