Fig. 12.

The Novorybnoye site (Fig. 1; sediment logs are in Fig. 20 in Fig. 17 in [1]). (A) Overview of the river cliff at Novorybnoye (looking east). The boundary between the Cretaceous sand (unit A) and overlying Quaternary sediment succession (unit B) is market by hatched line, as well as position of logged sub-sections (Nov 1a-e) and main sections (Nov 2 and Nov 3). (B) Glaciomarine unit B (Nov 1b, ∼13.5 m); massive, mollusc-bearing clayey silt with ice-rafted drop stones. (C) Unit C (Nov 1c, 14–15 m); shear laminated sand with intraclasts (boudins) from the unit B sediments; a glaciotectonite. (D) Unit E and F at site Nov 2; marine clayey silt overlain by shallow marine sand, in turn overlain by glaciomarine clayey silt with ice-rafted drop stones.