“…Many macro landforms, such as volcanoes, mountains, hills, plains, and fans, and sub-classified landforms, such as high mountains, low plains, tablelands, and rough low hills, can be achieved through a designed classifier or object-based image analysis approach based on topographic variables derived from DEMs (Camargo et al, 2012; Drăguţ and Eisank, 2012; Iwahashi and Pike, 2007; Jasiewicz et al, 2014; Manfré et al, 2015; Prima et al, 2006; Saadat et al, 2008; Stepinski and Bagaria, 2009; Vannametee et al, 2014). In the aforementioned classifications, topographic variables, such as slope, curvature, local relief, roughness, etc., are calculated through neighborhood analysis, which only reflects the local topographic surface parameters and fails to reveal terrain structural features in the macro scale.…”