Dynamics of the Caspian seashore in the Caucasus region under the condition of sea level rise
Abstract
On the Caspian seashore there are no evidences of the cliff abrasion and scouring of the accumulative (in classical sense) forms despite the recent sea level rise. The cause of such anomalous development is discussed and prognostic estimations of future destructive coastal processes are given.
About the Authors
L. A. Zhindarev
Московский государственный университет имени М.В.Ломоносова, Географический факультет
Russian Federation
Russian Federation
L. G. Nikiforov
Московский государственный университет имени М.В.Ломоносова, Географический факультет
Russian Federation
Russian Federation
G. I. Rychagov
Московский государственный университет имени М.В.Ломоносова, Географический факультет
Russian Federation
Russian Federation
Review
For citations:
Zhindarev L.A., Nikiforov L.G., Rychagov G.I. Dynamics of the Caspian seashore in the Caucasus region under the condition of sea level rise. Geomorfologiya. 2000;(1):82-88.
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