Abstract. Wave-transported boulders represent important records of
storm and tsunami impact over geological timescales. Their use for hazard
assessment requires chronological information on their displacement that in
many cases cannot be achieved by established dating approaches. To fill this
gap, this study investigated, for the first time, the potential of optically
stimulated luminescence rock surface exposure dating (OSL-RSED) for
estimating cliff-detachment ages of wave-transported coastal boulders. The
approach was tested on calcarenite clasts at the Rabat coast, Morocco.
Calibration of the OSL-RSED model was based on samples with rock surfaces
exposed to sunlight for ∼ 2 years, and OSL exposure ages were
evaluated against age control deduced from satellite images. Our results
show that the dating precision is limited for all targeted boulders due to
the local source rock lithology which has low amounts of quartz and
feldspar. The dating accuracy may be affected by erosion rates on boulder
surfaces of 0.02–0.18 mm yr−1. Nevertheless, we propose a robust relative
chronology for boulders that are not affected by significant
post-depositional erosion and that share surface angles of inclination with
the calibration samples. The relative chronology indicates that (i) most
boulders were detached from the cliff by storm waves; (ii) these storms
lifted boulders with masses of up to ∼ 24 t; and (iii) the
role of storms in the formation of boulder deposits along the Rabat coast
is more significant than previously assumed. Although OSL-RSED cannot
provide reliable absolute exposure ages for the coastal boulders in this
study, the approach has large potential for boulder deposits composed of
rocks with larger amounts of quartz or feldspar and less susceptibility to
erosion.