Procesy aktywizujące degradację wybrzeża klifowego Zalewu Puckiego

Leszek Zaleszkiewicz, Dorota Koszka-Maroń


Activation processes of degradation of cliff coast of Puck Lagoon.
S u m m a r y. The western cliff coast of Puck Lagoon has a lentgh of 7900 m. Its development proceeds as a result of processes of desintegration, denudation and marine erosion. The mass movement getting on depends on kind of sediment, geometry of slope and plant cover. Earth fall and talus accumulation prevail. As an effect of this processes, the cliff retreats in the form of small wastes.

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