2018
DOI: 10.1016/j.geomorph.2017.11.020
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Geomorphic evidence of Quaternary tectonics within an underlap fault zone of southern Apennines, Italy

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Cited by 26 publications
(10 citation statements)
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“…A complex geomorphic analysis may include computation of indices such as mountain front of water divide sinuosity, asymmetry, drainage basin elongation, relief ratio, hypsometry, normalized steepness, and concavity, integrated with geomorphological analysis (Giano et al, 2018). This study presents the most important geomorphic features that are often included in geographic education curriculum and also embedded in R algorithms: computation and mapping of slope steepness, aspect orientation, visualization hillshade and DEM elevation.…”
Section: Calculate Terrain Characteristics: Slope and Aspectmentioning
confidence: 99%
“…A complex geomorphic analysis may include computation of indices such as mountain front of water divide sinuosity, asymmetry, drainage basin elongation, relief ratio, hypsometry, normalized steepness, and concavity, integrated with geomorphological analysis (Giano et al, 2018). This study presents the most important geomorphic features that are often included in geographic education curriculum and also embedded in R algorithms: computation and mapping of slope steepness, aspect orientation, visualization hillshade and DEM elevation.…”
Section: Calculate Terrain Characteristics: Slope and Aspectmentioning
confidence: 99%
“…The average direction of the chain axis is approximately N150°, corresponding to the strike of both the main thrusts and younger coaxial normal faults. Extensional tectonics is still active along the axis of the chain deforming Pleistocene sediments [17][18][19][20][21][22]. Such a complex structural setting produced a mountain chain over 2000 m high and a regional divide oriented NW-SE that separates the drainage network towards south-west in the Tyrrhenian Sea, northeast in the Adriatic Sea, and east in the Ionian Sea.…”
Section: Geology and Geomorphology Of The Study Areamentioning
confidence: 99%
“…The most recent shortening occurred on the front range of the chain deforming the Pleistocene sediments and volcanics [29,31,32]. Moreover, extensional tectonics displacing the orogeny is still active along the axis of the Apennines chain [26][27][28][29][30][31][32][33][34][35][36][37][38][39]. The average direction of the chain axis is approximately N150 • , which corresponds to the strike of both the main thrusts and the coaxial normal faults.…”
Section: Regional Geology and Geomorphologymentioning
confidence: 99%
“…Many mountain tops of the axial belt correspond to the remnants of Pliocene-Pleistocene erosional land surfaces uplifted and dismembered by Quaternary faults [28]. The landscape of the axial zone includes block-faulted ridges and massifs, bounded by high-angle fault scarps retreated by slope-replacement processes [44] and displaced by active faults [38]. The intermontane basins filled with Pliocene-Quaternary fluvial and lacustrine deposits [36,45] are also present.…”
Section: Regional Geology and Geomorphologymentioning
confidence: 99%