<abstract xmlns="http://www.w3.org/1999/xhtml"> Firths are geomoiphological and hydrological sites typical for flat, neutral coast of no tidal sea basins. There in the greatest extend is preserved the geological column of the correlative Pleistocene- Holocene sediments. They make possible to reveal the Quaternary evolution of the contact zone „land-sea“. Firths are one of the most reliable indicators for the Quaternary Earth crust movements.Along the Black Sea coast most widely are developed the firths in the north - west and the west periphery, where they form a classic firth type coast.This report examines the results of complex studies of Batova river firth, located (developed) on the North Bulgarian Black Sea coast.</abstract>

Firths are geomoiphological and hydrological sites typical for flat, neutral coast of no tidal sea basins. There in the greatest extend is preserved the geological column of the correlative Pleistocene- Holocene sediments. They make possible to reveal the Quaternary evolution of the contact zone „land-sea“. Firths are one of the most reliable indicators for the Quaternary Earth crust movements.Along the Black Sea coast most widely are developed the firths in the north - west and the west periphery, where they form a classic firth type coast.This report examines the results of complex studies of Batova river firth, located (developed) on the North Bulgarian Black Sea coast.

Geomorphology of outflow part Batova river valley

„Episkop Konstantin Preslavski” University of Shumen, Faculty of natural sciences, Department “Geography and methodology of teaching geography” Shumen, 9712 Universitetska Str. 115,

„Episkop Konstantin Preslavski” University of Shumen, Faculty of natural sciences, Department “Geography and methodology of teaching geography”Shumen, 9712 Universitetska Str. 115,

Acta Scientifica Naturalis

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 License.

{"article-title":"Geomorphology of outflow part Batova river valley"}

Firths are geomoiphological and hydrological sites typical for flat, neutral coast of no tidal sea basins. There in the greatest extend is preserved the...

Geomorphology of outflow part Batova river valley

Published Online: Feb 09, 2017

Page range: 94 - 99

Received: Oct 30, 2016

Accepted: Jan 11, 2017

DOI: https://doi.org/10.1515/asn-2017-0015

Keywords
firth (liman), coastline, neutral type of coast, Quaternary movements

© 2017

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 License.

Geomorphology of outflow part Batova river valley

Published Online: Feb 09, 2017

Page range: 94 - 99

Received: Oct 30, 2016

Accepted: Jan 11, 2017

DOI: https://doi.org/10.1515/asn-2017-0015

Keywordsfirth (liman), coastline, neutral type of coast, Quaternary movements

© 2017

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 License.

Keywords
firth (liman), coastline, neutral type of coast, Quaternary movements