ORCID
- Boulton, Sarah: 0000-0002-8251-0025
Abstract
Tidal notches are a generally accepted sea level indicator that, when different from mean sea level, witness tectonic activity at or near coastlines. However, how to infer related information is controversial since tectonic uplift from a single seismic event is not likely to exceed several decimetres. High resolution laser scanning offers the availability of close-up views on exposures and to detect evidence for multiple sea level indicators in between major emergence. Statistically representative profiles along exposure were analysed in order to prove for already described tidal notches and to highlight similar shapes in consistent geometries along coastal cliffs of Perachora Peninsula.
DOI
10.12681/bgsg.11748
Publication Date
2016-01-01
Publication Title
Bulletin of the Geological Society of Greece
Volume
50
Issue
1
First Page
468
Last Page
468
ISSN
0438-9557
Embargo Period
2022-06-22
Organisational Unit
School of Geography, Earth and Environmental Sciences
Recommended Citation
Schneiderwind, S., Kázmér, M., Boulton, S., Papanikolaou, I., & Reicherter, K. (2016) 'GEOMETRY OF HOLOCENE TIDAL NOTCHES – SEA LEVEL MARKERS AT PERACHORA PENINSULA, GULF OF CORINTH, GREECE', Bulletin of the Geological Society of Greece, 50(1), pp. 468-468. Available at: https://doi.org/10.12681/bgsg.11748
