Seafloor character of the Roman Rock area in False Bay, South Africa

This is a Preprint and has not been peer reviewed. The published version of this Preprint is available: https://doi.org/10.31223/X5B719. This is version 3 of this Preprint.

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Authors

Andrew Terhorst, John Rogers

Abstract

Context: This study investigates the seafloor character of a 12 km2 area off Simon’s Town in False Bay, South Africa.



Aims: The goal was to map the seafloor geology around Roman Rock Lighthouse, focusing on sedimentology.


Methods: Side-scan sonar and single-beam echosounder were used, complemented by sediment sampling and diver observations for ground-truthing. Sediment samples were analysed for texture and composition.


Key Results: Six patterns of reflectivity (acoustic facies) were identified, including granite outcrops, wave ripples, and patches of gravelly and quartzose sands. Sediment analysis showed a mix of calcareous and quartzose components, with calcareous material dominating the gravel fraction near granite outcrops.


Conclusions: The Roman Rock seafloor reflects a complex depositional environment shaped by biogenic activity and wave-induced sediment transport.


Implications: This research lays the groundwork for future geological studies in False Bay, particularly around wave-induced sediment dynamics.

DOI

https://doi.org/10.31223/X5B719

Subjects

Geology, Sedimentology

Keywords

False Bay; South Africa; seafloor mapping; side-scan sonar; diver observations

Dates

Published: 2024-10-04 01:18

Last Updated: 2025-02-27 06:54

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License

CC BY Attribution 4.0 International

Additional Metadata

Conflict of interest statement:
N/A