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sed12111-sup-0001-FigS1.tifimage/tif60044K

Figure S1. (A) Grain-size distributions of the matrix of different till layers (<2 mm). (B) Clast fabric plotted on a ternary diagram compared with data from other sites (in Benn, 1994). (C) Plot of S1/S3 eigenvalues for the Ballyhorsey clast fabric data, compared with data from other sites (Menzies & Shilts, 2002). (D) Schmidt equal-area projections of clast fabric data of the three different till layers observed at the base of the pit.

sed12111-sup-0002-FigS2.tifimage/tif37337K

Figure S2. Interpreted section 3. Photograph showing the erosive contact between the clay-rich diamicton (F1.1) and the massive and poorly sorted gravel (F3.1). Note the occurrence of clastic dykes sourced in F1.1 that propagates upwards.

sed12111-sup-0003-FigS3.tifimage/tif16223K

Figure S3. Interpreted section 4. Distal part of the wedge displaying mainly sandy deposits (F3.6) that are affected by intense deformation. The deformed zone is characterized by a 3 m wide depression bordered by step normal faults. This depression is surrounded by intense deformation structures including thrust faults (A), asymmetrical folds (B) and clastic dykes (C).

sed12111-sup-0004-FigS4.tifimage/tif12607K

Figure S4. Sedimentary logs 6 and 12. See Fig. 2 for their localizations.

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