“…Worldwide, these procedures have been widely applied to tectonically active regions, such as the Himalayan Arc (SEEBER; GORNITZ, 1983), Nicoya Peninsula in Costa Rica (HARE;GARDNER, 1984), Mexican Volcanic Belt (RAMÍREZ-HERRERA, 1998), South and Southern Spain (SILVA et al, 2003;EL HAMDOUNI et al, 2008;PEDRERA et al, 2009;PÉREZ-PEÑA et al, 2010). In Brazil, the morphometry of fluvial systems is one of the most common themes in fluvial geomorphology (BARROS; REIS, 2019) and the previously referenced techniques have largely been applied to investigate the correlation between geological features and the physiography of river valleys (ETCHEBEHERE et al, 2006;ROSSETTI et al, 2008;ROSSETTI, 2011;FUJITA et al, 2011;FURRIER, 2017). Moreover, morphometric and geomorphic indices were trained in Brazil in assessments of development of drainage systems and discrimination of ductile and brittle tectonics (ALVES et al, 2014), progress and growth of river catchments FURRIER, 2011), changes in river profiles (BARBOSA et al, 2013), identification and demarcation of morphotectonic features (CAMOLEZI et al, 2012), litho-structural and tectonic zoning (CHERÉM et al, 2011), and effective detection of neotectonics FURRIER, 2014;ROSSETTI, 2017).…”