Figure 3.

Sediment exposed in Rogen ridge, Anåkröken, central Sweden. Distal is to the left in the photographs.

(a) Panoramic view of the cross-section (small car for scale), showing major erosional surfaces, boulder lag, and foreset bedding.

(b) Upper part of the exposure; the sediment is finer and better stratified than that below. Sand and silt in graded and cross laminae are common in this part of the section; see (d).

(c) Lower part of the exposure. Crudely bedded, angular boulders derived from the local shale bedrock in a multimodal matrix (gravel to silt). The boulders are imbricate with major planes dipping proximally (Shaw 1979).

(d) Interbedded poorly sorted gravel to silt with angular clasts and graded, fine sand and silt.