T58 Sea-Level Indicators: New Interpretations and Constraints for Future Projections

Tuesday, 27 October 2020
10:00 AM - 12:00 PM
Meeting Rooms


SUBMERGENCE OF THE HELLENISTIC HARBOR AT AKKO, ISRAEL: IMPLICATIONS FOR SEA-LEVEL RECONSTRUCTIONS IN THE LEVANTINE BASIN

Paper number: T58-8
Program: Technical Sessions
Time: 11:30 AM – 11:40 AM


Authors


Abstract

With rising seas and impending inundation, a sound understanding of the factors controlling sea-level is imperative in order to accurately predict regional coastline changes. Such information can result from a variety of different sources, spanning from geological or biological markers of past sea-levels to archaeological indicators. This study utilizes a combination of such markers to better understand the causes for the submergence of the Hellenistic (3rd to 1st centuries BCE) harbor of Akko, located in the Eastern Mediterranean (northern Israel). Three possible reasons for the current sub-aerial position (1.1 to 1.2 meters below present sea-level) of these harbor remains were assessed: structural deterioration, eustatic sea-level rise, and vertical tectonic movements. The sloping surface of the harbor quay, as well as the harbor's construction on a cohesionless sediment fill indicate subsidence from structural deterioration. However, this deterioration only accounts for part of the elevational discrepancy. The remaining difference can be explained by comparison of the currently submerged harbor with other similarly dated submerged coastal structures in the Levant, which suggests a common sea-level rise of 1 to 2 meters. Together, these results show that an estimated ~1 meter of sea-level rise has occurred since the Hellenistic Period. Minor vertical displacements from tectonic activity cannot be ruled out and merit further investigation. This study emphasizes the complicated nature of sea-level, highlighting the importance of using proper construction methods for the coastal environment, as well as the inevitability of submergence with rising seas.

Geological Society of America Abstracts with Programs. Vol. 52, No. 6

doi: 10.1130/abs/2020AM-358013

© Copyright 2020 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.