Page 48 - MSc_thesis_R A Kil

(a) Homogeneous scour fill showing a large
quantity of bioclasts at the bottom. Erosion
by wind formed the protruding banks. Ruler
is four metres long.
(c) Tabular cross-stratification. Thickness of
each bed is ca. one metre.
(e) Large foresets forming a bed of approx.
eight metres thick in the Scala Cavallo cliff.
Figure 4.8 – Field examples of scour fills, tabular cross-stratification and large foresets.
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(b) Scour fill in the San Francesco quarry, in
the southern part of Favignana town. The
wall is two metres high.
(d) Bottom part of this section in Bue Marino
shows tabular cross stratification. Ruler of
approx. two metres for scale.
(f ) Situation in the northern part of Cala Az-
zurra, showing large foresets up to six metres
high.