Marine terrace staircases of western Iberia: Uplift rate patterns from rocky limestone coasts of central Portugal (Cape Raso - Abano beach and Cape Espichel)
ORCID
- Martin Stokes: 0000-0003-3788-4615
Abstract
The Western Iberian Peninsula is undergoing compressive tectonic reactivation, resulting in spatial and temporal variations of surface uplift. Uplift quantification can be undertaken in coastal settings using staircases of shore platforms developed onto rocky headlands. This study analyses two marine terrace staircases in central Portugal: Cape Raso - Abano beach and Cape Espichel. Geomorphic and stratigraphic analyses identified marine terraces/shore platforms developed below a culminant shore platform, four at Cape Raso and eleven at Cape Espichel. The terrace chronology was obtained by using ESR and pIRIR dating. Using the interactions between the elevation, age and global mean sea-level elevations, the marine terraces were correlated with Marine Isotope Stages (MIS). The shore platforms at the Cape Espichel are more elevated than the coeval references at the Cape Raso - Abano beach and this indicates differential uplift. Considering the culminant shore platform (3.7 Ma), for the Espichel W promontory the estimated long-term uplift rate is ∼0.03 m/ka, but for the Cape Raso is only ∼0.01 m/ka. Also, by using the shore platform considered as produced by the MIS 15 high stand (∼572 ka), the estimated uplift rate for the Espichel W promontory is ∼0.13 m/ka, but for the Cape Raso is ∼0.07 m/ka. The Espichel W promontory terrace staircase also allows to deduce that the estimated uplift rate was nearly constant during ∼600 ka to ∼200 ka ago (∼0.13–0.11 m/kA), but it after decreases (∼0.06–0.01 m/ka).
DOI Link
Publication Date
2025-02-28
Publication Title
Quaternary International
Volume
720
ISSN
1040-6182
Acceptance Date
2024-12-30
Deposit Date
2025-02-07
Embargo Period
2026-01-27
Funding
This work was funded by the Funda\u00E7\u00E3o para a Ci\u00EAncia e Tecnologia (FCT) I.P./MCTES, through national funds (PIDDC) with the projects: UIDB/MAR/04292/2020 ( https://doi.org/10.54499/UIDB/04292/2020 , https://doi.org/10.54499/UIDP/04292/2020 ) MARE - Marine and Environmental Sciences Centre; LA/P/0069/2020 ( https://doi.org/10.54499/LA/P/0069/2020 ) ARNET - Aquatic Research Network); UIDB/GEO/04683/2020 (ICT - Institute of Earth Sciences); and UIDB/04084/2020 (CEGOT - Centre of Studies in Geography and Spatial Planning); UIDB/50019/2020 ( https://doi.org/10.54499/UIDB/50019/2020 ), UIDP/50019/2020 ( https://doi.org/10.54499/UIDP/50019/2020 ) and LA/P/0068/2020 ( https://doi.org/10.54499/LA/P/0068/2020 ).
Additional Links
Keywords
ESR and OSL dating, Marine terrace, Pleistocene, Shore platform, Uplift, Western iberian margin
Creative Commons License

This work is licensed under a Creative Commons Attribution-NonCommercial-No Derivative Works 4.0 International License.
Recommended Citation
Stokes, M. (2025) 'Marine terrace staircases of western Iberia: Uplift rate patterns from rocky limestone coasts of central Portugal (Cape Raso - Abano beach and Cape Espichel)', Quaternary International, 720. Available at: 10.1016/j.quaint.2024.109657
This item is under embargo until 27 January 2026
