Solid rocks on the nearshore seabed – the distribution and potential impact on coastal processes in the Kołobrzeg region, the Southern Baltic

The Southern Baltic seabed is mainly composed of marine sediments situated on glacial and fluvioglacial deposits. In the Kołobrzeg region, however, solid rocks are located at the shallow subbottom. In order to determine the exact distribution of the rocks, some analyses of sonar images, underwater p...

Full description

Saved in:
Bibliographic Details
Published in:Oceanological and hydrobiological studies 2017-03, Vol.46 (1), p.62-73
Main Authors: Rudowski, Stanisław, Sitkiewicz, Patryk, Wróblewski, Radosław, Makurat, Katarzyna
Format: Article
Language:English
Subjects:
Abrasion
Bathymetric data
Coastal processes
Coasts
Distribution
dynamic layer
Erosion resistance
Geological structures
Geology
Geomorphology
Glacial deposits
Glacial drift
Jurassic
Jurassic sandstone and mudstone outcrops
Marine sediments
Morphology
Ocean floor
Oceanography
Offshore
Outcrops
Polish coast
Rock
Rocks
ROV TV
Sandstone
seafloor relief and geological structure
Sediment
Sediment samplers
Sediment samples
Sediments
Shoreline protection
side-scan sonar
Storms
sub-bottom profiling
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:The Southern Baltic seabed is mainly composed of marine sediments situated on glacial and fluvioglacial deposits. In the Kołobrzeg region, however, solid rocks are located at the shallow subbottom. In order to determine the exact distribution of the rocks, some analyses of sonar images, underwater photos, sediment samples, seismoacoustic profiles and bathymetric data have been performed. The outcrops of Jurassic sandstones and mudstones have been documented. The geological structure of the area is presented, while the fact that the present seafloor relief is determined by the shallow uneven top surface of the Jurassic rocks is emphasized. The seabed has been classified as rock platform-constrained. The seafloor is a sediment-poor abrasion platform, within which marine sandy sediments are transported, mainly toward offshore, on the firm, stiff or hard surface of glacial deposits and Jurassic solid rocks. This results in a lack of material for the reconstruction of the beach after storms. Many of the commonly used methods for studying the condition and changes of the coast cannot be used in this type of terrain due to the presence of a thin and discontinuous dynamic layer lying on the erosion-resistant rocks of the geomorphologically complex seafloor.
ISSN:1897-3191
1730-413X
1897-3191
DOI:10.1515/ohs-2017-0007