“…As a consequence of continuous erosional processes, previously significant and extensive surfaces degraded into surface peaks, therefore, those eroded peaks can indicate the altitudinal position of paleosurface remnants (Bugya, 2009; Ebert, Hättestrand, Hall, & Alm, 2011; Rowberry, 2012; Soares & Riffel, 2006) (Figure 1). Several methods have been developed to detect surface peaks (Deng & Wilson, 2008; Kirmse & Ferranti, 2017; Podobnikar, 2012; Torres, Fraternali, Milani, & Frajberg, 2020). However, the Geomorphons algorithm can provide a fast, adjustable, and open‐source method for peak detection.…”