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The Mejillones Peninsula is thought to have one of the highest rates of tectonic uplift along the active convergent margin of northern Chile.
Opposing crustal motion between adjacent blocks is compatible with the formation of intervening normal faults and the hypothesis of ongoing extension of the forearc.
Comparisons with published data suggest a contemporaneous acceleration in uplift occurred throughout the Peninsula, with higher rates of mean uplift observed after 480 ka.
We proposed an efficient measurement strategy with respect to the radiocarbon calibration curve.
This method is also applicable for other deposits formed by any natural hazard if bulk peat is obtainable so it can contribute to better hazard assessment worldwide.