The center wetlands development on sandy accumulative forms of coastal zone of a sea
Abstract
On sandy accumulative forms of the Black Sea coastal zone was distinguished specific type of the landscape that was named as "center of wetland”. This type is forming in conditions of alongshore drift flow dissipation, under impact of abundant quantity of sediment, increased thickness of wave dredging layer, moderate inclination of submarine slope and intensive increase of the shoreline. The basic element of shore landscape is small lake that located between two after-storm beach-ridge with long up to 200-400 m and depth up to 1,5-3,5 m. Usually, this lakes are bordering by reed belt and characterized of salt water, impoverished flora and fauna, muddy sediment, nourishment of graund water, intensive dynamic. At the same time this lakes are include in complex landscape system of sandy accumulative coastal forms.
Downloads
Authors who publish with this journal agree to the following terms:
- Authors retain copyright and grant the journal right of first publication of this work under the terms of a license Creative Commons Attribution License 4.0 International (CC BY 4.0).
- Authors are able to enter into separate, additional contractual arrangements for the non-exclusive distribution of the journal's published version of the work (e.g., post it to an institutional repository or publish it in a book), with an acknowledgement of its initial publication in this journal.
- Authors are permitted and encouraged to post their work online (e.g., in institutional repositories or on their website) prior to and during the submission process, as it can lead to productive exchanges, as well as earlier and greater citation of published work.
