Recent history of the Eastern Eliki Fault, Gulf of Corinth: geomorphology, palaeoseismology and impact on palaeoenvironments
Recent history of the Eastern Eliki Fault, Gulf of Corinth: geomorphology, palaeoseismology and impact on palaeoenvironments
The Eliki fault system dominates the landscape of the southwestern shore of the Gulf of Corinth, where rapid extension rates result in frequent earthquakes. These include an event in 373 BC that destroyed the city of Helike and a recent event in 1861. Uplifted Late Pleistocene marine terraces within the Eastern Eliki Fault footwall suggest revised slip rates of ~3–5 mm yr1, contributing ~2–3 mm yr1 geological extension to a net geodetic extension of ~10–15 mm yr1 across this part of the rift. Palaeoseismological trenches indicate two and possibly three earthquakes on the Eastern Eliki Fault in the last 1500 yr, including the 1861 earthquake. One trench (EET1A) reveals displaced stratigraphy, but the main fault trace is thought to lie further south beneath the Old National Road. Trench EET1A reveals liquefied sediments associated with an event between AD 1460 and the present, which may be the 1861 event, and displacement during a second event in the interval AD 440–1410 or AD 1270–1640. A third earlier event identified by liquefaction occurred on the Eliki or a nearby fault in AD 440–1410. Using the 1861 and second event (most likely AD 1270–1640), the interval between recent earthquakes is ~200–600 yr. Suitable trench sites are rare in this region, compounded by human activity over several thousand years. Borehole and trench data indicate that the Kerynites river frequently flowed eastwards along the Eastern Eliki Fault during the last 20–40 kyr, possibly influenced by tectonic tilting from the Eliki and Aigion fault systems and natural channel avulsion.
154-166
McNeill, L.C.
1fe6a1e0-ca1a-4b6f-8469-309d0f9de0cf
Collier, R.E.L.
4568b663-a810-44d7-8712-41a6fe1dd40a
De Martini, P.M.
57c595e9-91b0-4f7f-ad62-1697d0fe1b23
Pantosti, D.
1bc3054b-dbaf-4c47-b77b-e2fdb02ba469
D'Addezio, G.
aca702e5-d2ff-4212-acee-ae1fbfc75b51
2005
McNeill, L.C.
1fe6a1e0-ca1a-4b6f-8469-309d0f9de0cf
Collier, R.E.L.
4568b663-a810-44d7-8712-41a6fe1dd40a
De Martini, P.M.
57c595e9-91b0-4f7f-ad62-1697d0fe1b23
Pantosti, D.
1bc3054b-dbaf-4c47-b77b-e2fdb02ba469
D'Addezio, G.
aca702e5-d2ff-4212-acee-ae1fbfc75b51
McNeill, L.C., Collier, R.E.L., De Martini, P.M., Pantosti, D. and D'Addezio, G.
(2005)
Recent history of the Eastern Eliki Fault, Gulf of Corinth: geomorphology, palaeoseismology and impact on palaeoenvironments.
Geophysical Journal International, 161 (1), .
(doi:10.1111/j.1365-246X.2005.02559.x).
Abstract
The Eliki fault system dominates the landscape of the southwestern shore of the Gulf of Corinth, where rapid extension rates result in frequent earthquakes. These include an event in 373 BC that destroyed the city of Helike and a recent event in 1861. Uplifted Late Pleistocene marine terraces within the Eastern Eliki Fault footwall suggest revised slip rates of ~3–5 mm yr1, contributing ~2–3 mm yr1 geological extension to a net geodetic extension of ~10–15 mm yr1 across this part of the rift. Palaeoseismological trenches indicate two and possibly three earthquakes on the Eastern Eliki Fault in the last 1500 yr, including the 1861 earthquake. One trench (EET1A) reveals displaced stratigraphy, but the main fault trace is thought to lie further south beneath the Old National Road. Trench EET1A reveals liquefied sediments associated with an event between AD 1460 and the present, which may be the 1861 event, and displacement during a second event in the interval AD 440–1410 or AD 1270–1640. A third earlier event identified by liquefaction occurred on the Eliki or a nearby fault in AD 440–1410. Using the 1861 and second event (most likely AD 1270–1640), the interval between recent earthquakes is ~200–600 yr. Suitable trench sites are rare in this region, compounded by human activity over several thousand years. Borehole and trench data indicate that the Kerynites river frequently flowed eastwards along the Eastern Eliki Fault during the last 20–40 kyr, possibly influenced by tectonic tilting from the Eliki and Aigion fault systems and natural channel avulsion.
This record has no associated files available for download.
More information
Published date: 2005
Identifiers
Local EPrints ID: 15587
URI: http://eprints.soton.ac.uk/id/eprint/15587
ISSN: 0956-540X
PURE UUID: 1e9db632-ae72-4fc9-bd81-16f1ab9b9c51
Catalogue record
Date deposited: 29 Apr 2005
Last modified: 16 Mar 2024 03:20
Export record
Altmetrics
Contributors
Author:
R.E.L. Collier
Author:
P.M. De Martini
Author:
D. Pantosti
Author:
G. D'Addezio
Download statistics
Downloads from ePrints over the past year. Other digital versions may also be available to download e.g. from the publisher's website.
View more statistics