Fig. 4From: A record of deglaciation-related shifting of the proximal zone of a sandur — a case study from the Gwda sandur, NW Poland (MIS 2)Sedimentary details of glaciofluvial succession in the Stobno study site. a Stobno study site succession with marked three sedimentary units; b Wavy-laminated sandy fines (FSw) and climbing ripple cross-laminated sands (Src) of low-energy parts of braided river system; c Trough cross-stratified sands (St) and gravelly sands (SGt) of the uppermost part indicate megaripples in the deepest parts of the braided river channels; d Sediments deposited by high-energy flows in braided channelsBack to article page