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“Landscapes in tectonically active areas result from a complex integration of the effects of vertical and horizontal motions of crustal rocks and erosion or deposition by surface processes. In a sense, many landscapes can be thought of as resulting from competition among those processes acting to elevate the Earth's surface and those that tend to lower it” (Burbank and Anderson, 2001). Extracting information from deforming landscapes with an integrative approach is the main subject of tectonic geomorphology. The landscape features have different dimensional scales that correspond to different tectonic implications. The major landforms (from continent scale to orogen scale; 107-104 km) and the intermediate ones (from mountain belt scale to ridge and valley scale; 104-10 km) result from the interaction of both endogenic and exogenic processes, with a dominancy of one over the other at different places and times, while the minor ones (at single landform scale; 10-10-2 km) are related to tectonics (tectonic landforms) or to erosion processes (i.e. fluvial, slope, glacial landforms) as defined since the beginning of the history of tectonic geomorphology (Gerasimov, 1946; Cailleux and Tricart, 1956; Mescerjakov, 1968; Ollier, 1981, 1999; Morisawa and Hack, 1985; Panizza and Castaldini, 1987; Ascione and Cinque, 1999; Burbank and Pinter, 1999; Burbank and Anderson, 2001; Peulvast and Vanney, 2001; Scheidegger, 2004). At intermediate to small scale, mountain belts, and related piedmont, are one of the main subjects of tectonic geomorphology. At this scale, drainage basins are the key features in the landscape. Basins consist of river channels, hill slopes, crests of interfluves and drainage divides that define the shape of the catchment. Some of these elements will respond more rapidly to changes imposed on them than others, according to the combination of many factors such as lithology, local tectonics, rock uplift/subsidence and climate changes (Morisawa and Hack, 1985; Kühni and Pfiffner, 2001; Twidale, 2004). In tectonically active landscapes, changes in the incision/aggradation behaviour of the rivers are associated with the variations in climate and tectonics (Schumm, 1969; Bull, 1991; Merrits et al., 1994; Ascione and Cinque, 1999; Burbank and Pinter, 1999; Pazzaglia and

Two Tectonic Geomorphology Studies on the Landscape and Drainage Network of Chain and Piedmont Areas of the Abruzzi Region (Central Apennines, Italy)