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2- La strada di casa. Dove ogni minimo cambiamento risuona con fragore di tuono. 3- Le cicale e le colline. 4- Trovare una vecchia bicicletta e rimetterla a posto. Sapendo che è testimone di anni in cui provincial vallegrande economia domestica neanche c'eri. 5- Il primo bagno al mare. 6- Sentire la bimba che canta le stesse filastrocche che imparavamo anche noi all'asilo. 7- Mangiare le primule in montagna.

These evolutionary stages are preserved in the different catchments of the study area. Small coastal catchments show a provincial vallegrande economia domestica mostly affected by linear incision (also documented by orographic features and high hypsometric values), and preserve the first stages of hillslope evolution (1, 2 lower part on the Main Map). Large catchments (i. Feltrino and Vallegrande) were primarily affected by linear incision and secondarily enlarged by non-linear geomorphic processes, related to large landslide and hillslope processes (also documented by orographic features and moderately high hypsometric integral values with concave-convex shaped curves), and show later hillslope evolutionary stages (3, 4 lower part on the Main Map). Generally, local geomorphological processes were induced by Middle Pleistocene ‚ Holocene uplift processes and climate and sea-level change, which occurred after the late Early Pleistocene emergence of the western Adriatic area and the subsequent evolution of the Adriatic piedmont into a subaerial environment. This serenata a vallegrande 2014 world evolution could be considered representative of hilly regions developed on uplifted soft bedrock lithologies (clay-sand-conglomerate) within mid-latitude climate conditions, such vedova allegra trucco sposa the whole Adriatic piedmont of the Apennines chain. In conclusion, at a local scale, the detailed mapping of near-surface deposits and landforms contributes to understanding of the causes, mechanisms, and consequences of landform change also with a view to assisting engineering geomorphological problems.

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