<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

Publicado en línea: 09 feb 2017

Páginas: 94 - 99

Recibido: 30 oct 2016

Aceptado: 11 ene 2017

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

Palabras clave
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

Publicado en línea: 09 feb 2017

Páginas: 94 - 99

Recibido: 30 oct 2016

Aceptado: 11 ene 2017

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

Palabras clavefirth (liman), coastline, neutral type of coast, Quaternary movements

© 2017

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

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