Geoscience Reference
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some places showing low mounds inherited from the buried moraine topography,
and extends over the depth range of 35-80 m.
The Baltic bottom topography features the first- and second-order morphostruc-
tural elements, i.e. geological structures formed by endogenous processes. The
first-order morphostructure covers the entire central and southern part of the Baltic
and is represented by the NW margin of the Russian plate (the Baltic syneclise).
Fig. 10.2
Digital model of the sea bottom slopes. Expected tectonic scarp locations are shown
