ORCID Identifier(s)

ORCID 0000-0001-8390-052X, ORCID 0000-0002-7385-8679, ORCID 0000-0003-4978-4582, ORCID 0000-0001-9144-3031, ORCID 0000-0003-2482-0081

Document Type

Dataset

DOI

https://doi.org/10.32855/dataset.2026.02.051

Production/Collection Date

2026

Production/Collection Location

Arlington, TX

Depositor

Nathan Brown

Deposit Date

9-8-2026

Data Type

Experimental data. TXT, PDF and XLSX are the data file formats.

Abstract

Southern Italy preserves a well-studied record of deformation and uplift related to migrating oblique collision, trench retreat, and tearing of subducted ocean slabs. However, the surface expression of these processes is incompletely understood due to a lack of reliable ages for marine terraces >200 m above sea level (masl). Here we use luminescence methods to date shallow marine sands from terraces ~ 100 to 1,000 masl in southern Calabria and interpolate the results with regional surface mapping. Burial ages overlap across the full range of sampled elevations with a weighted mean of 118.8 ± 8.7 thousand years before present (ka). Calculated uplift rates vary from 12 mm yr-1 and throw rates on active normal faults are 0.8–4.2 mm yr-1. We infer that rapid post-120 ka uplift is an ongoing isostatic response to an active tear in the Ionian slab, consistent with recent geophysical observations and predictions of geodynamic models. These results have important implications for assessment of geohazards in southern Calabria and northeast Sicily, one of the highest seismic risk areas in the Mediterranean region.

Disciplines

Earth Sciences | Geology

Publication Date

2026

Language

English

Faculty Mentor of Honors Project

N/A

License

Creative Commons Attribution 4.0 International License
This work is licensed under a Creative Commons Attribution 4.0 International License.

Included in

Geology Commons

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