Geology Reference
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Figure 12.4. Late-Pleistocene composite wedge cast formed within loess and lying beneath a fossil
soil horizon, Miechow Plateau, southwestern Poland. The upper, inner (sand) wedge is formed by
primary infi lling; the lower (pseudomorph) wedge shows evidence of secondary infi lling.
Figure 12.5. Oblique air photograph showing traces of a random orthogonal thermal-contraction
crack network, as revealed in crop marking, near Vessige, south-western Sweden. Photograph and
caption information are supplied courtesy of Professor H. Svensson.
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