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<p>. The paper presents researches that were conducted in Czarna Orawa River catchment, situated within the Tatra and Beskidy Mountains. Czarna Orawa River channel is segmental meandering system with the index of tortuosity up to 1.6. The aim of the article is to characterize gravels which were transported from the Tatra Mountains and their role in valley bottom formation.</p>
</abstract>

. The paper presents researches that were conducted in Czarna Orawa River catchment, situated within the Tatra and Beskidy Mountains. Czarna Orawa River channel is segmental meandering system with the index of tortuosity up to 1.6. The aim of the article is to characterize gravels which were transported from the Tatra Mountains and their role in valley bottom formation.

Formation and role of neogene sediments from Tatra mountains in the shaping of Czarna Orawa river alluvial plain

Quaestiones Geographicae

. The paper presents researches that were conducted in Czarna Orawa River catchment, situated within the Tatra and Beskidy Mountains. Czarna Orawa River...

Formation and role of neogene sediments from Tatra mountains in the shaping of Czarna Orawa river alluvial plain

Published Online: Oct 21, 2012

Page range: 41 - 46

DOI: https://doi.org/10.2478/v10117-012-0003-y

This content is open access.