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Rapid sea-level movements and noneruptive crustal deformations in the Phlegrean Fields caldera, Italy

2006; Geological Society of America; Volume: 34; Issue: 2 Linguagem: Inglês

10.1130/g21894.1

1943-2682

Christophe Morhange, Nick Marriner, Jacques Laborel, Micol Todesco, Christine Oberlin,

Methane Hydrates and Related Phenomena

Research Article| February 01, 2006 Rapid sea-level movements and noneruptive crustal deformations in the Phlegrean Fields caldera, Italy Christophe Morhange; Christophe Morhange 1CEREGE, CJB, Université Aix-Marseille, 29 avenue Robert Schuman, F-13621 Aix-en-Provence, France Search for other works by this author on: GSW Google Scholar Nick Marriner; Nick Marriner 1CEREGE, CJB, Université Aix-Marseille, 29 avenue Robert Schuman, F-13621 Aix-en-Provence, France Search for other works by this author on: GSW Google Scholar Jacques Laborel; Jacques Laborel 2Université de la Méditerranée, Faculté des Sciences de Luminy, F-13288 Marseille, France Search for other works by this author on: GSW Google Scholar Micol Todesco; Micol Todesco 3Istituto Nazionale di Geofisica e Vulcanologia, via D. Creti 12, I-40128 Bologna, Italy Search for other works by this author on: GSW Google Scholar Christine Oberlin Christine Oberlin 4Centre de Datation par le Radiocarbone, Université Lyon 1, F-69622 Villeurbanne, France Search for other works by this author on: GSW Google Scholar Geology (2006) 34 (2): 93–96. https://doi.org/10.1130/G21894.1 Article history received: 25 May 2005 rev-recd: 26 Sep 2005 accepted: 12 Oct 2005 first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Christophe Morhange, Nick Marriner, Jacques Laborel, Micol Todesco, Christine Oberlin; Rapid sea-level movements and noneruptive crustal deformations in the Phlegrean Fields caldera, Italy. Geology 2006;; 34 (2): 93–96. doi: https://doi.org/10.1130/G21894.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract The importance of Pozzuoli's archaeological ruins in linking sea-level change and Earth deformation with volcanic activity has been recognized since the nineteenth century. The pillars of the Roman market were used as a paleotide gauge by pioneer geologists such as Lyell. For the first time, we have radiocarbon dated biological indicators on these remains, showing three 7 m relative sea-level highstands during the fifth century A.D., the early Middle Ages, and before the 1538 eruption of Monte Nuovo. These repeated uplift and subsidence cycles, not always followed by volcanic activity, have important implications for the evaluation of volcanic hazard. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.