Typical features of steep mountain streams are alternating channel-spanning steps and pools (Church & Zimmermann, 2007;Comiti & Mao, 2012;. Isolated step-pool units form in streams with bed slope higher than 3%-4% .Step-pool sequences, that is, consecutive step-pool units, are expected in streams with bed slope exceeding ∼7% (Chin, 1999; Church & Zimmermann, 2007;Comiti & Mao, 2012;Whittaker & Jaeggi, 1982). The prerequisites for step formation are heterogeneous and widely graded bed material being mobile during step-forming conditions, high flood events (i.e., high bed shear stresses), and low sediment supply (