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B
A
Fig. 12.7 Aerial image of the barrier Schaabe; view is towards east and the Baltic is located on the
left side (for location, see Fig. 12.1 , no. 9). Two beach ridge systems are evident: an older system
( A ), which consists of short, low-lying ridges, bent into the former bay and a second system of
higher elevated dune ridges ( B ), which cut off the bay from the sea and show rapid progradation.
This system is covered by dense pine forest (Photo: R. Lampe 2007 )
A
C
B
Fig. 12.8 Aerial image of the eastern tip of the Zingst peninsula and the offshore sand flats and
islands; view is northwards (for location, see Fig. 12.1 , no. 6). The inlet is progressively truncated
by a spit ( A ) growing from west ( left ) to east ( right ). Sand flats ( B ) with incised flooding channels
spread between the islands. In the northern part of the offshore island, progradational beach ridges
( C ) are visible (Photo: R. Lampe 2007 )
 
 
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