Search results for "Relative sea level change"

showing 4 items of 4 documents

Vertical movements in NE Sicily and its offshore: Outcome of tectonic uplift during the last 125 ky

2013

New data in the coastal area between Acquedolci and Patti (northeastern Sicily, Italy) have been collected to calculate vertical tectonic rates in a key sector between the Kabilian-Calabrian and the Sicilian-Maghrebian chain. The comparison among marine geology data (multibeam and seismic reflection profiles) on the continental shelf-slope system and the radiocarbon ages on geomorphological markers collected during a coastal survey, provided new stratigraphic, geomorphological and biological data, contributing to the knowledge of the geological evolution of this sector for the last 125 ky.This coastal area is framed between two main structural features active during the Pleistocene in north…

geographygeography.geographical_feature_categoryPleistoceneHoloceneLast Glacial MaximumSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia StrutturaleSettore GEO/04 - Geografia Fisica E GeomorfologiaMarine geologyLast Glacial MaximumFault (geology)Last Interglaciallaw.inventionTectonicsTectonic upliftlawRelative Sea level changeUplift rateLate Quaternary depositional sequenceRadiocarbon datingGeomorphologyGeologyHoloceneEarth-Surface Processes
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Holocene sea level change in Malta

2013

A multidisciplinary approach has been applied to study sea level changes along the coast of Malta using data collected from underwater archaeological remains. The elevation of archaeological markers have been compared with predicted sea level curves providing new bodies of evidence that outline the vertical tectonic behaviour of this region, allowing estimation of the relative sea level changes that occurred in this area of the Mediterranean since the Bronze Age. During the Roman Age, sea level was at −1.36 ± 0.1 m, while in the Midde Age it was at −0.56 ± 0.2 m, in agreement with previous estimations for the Mediterranean region. Data indicate that Malta was tectonically stable during the …

vertical movementMediterranean climateClimatic changes -- MaltaSea level -- MaltaSettore GEO/02 - Geologia Stratigrafica E SedimentologicaPleistoceneMaltaSettore GEO/03 - Geologia StrutturaleSettore GEO/04 - Geografia Fisica E GeomorfologiaElevationLast Glacial Maximumrelative sea level changePaleoecology -- Maltarelative sea level change; Late Holocene; MaltaLate HoloceneTectonicsPaleontologyPalynology -- MaltaBronze Agesealevel changeHoloceneGeologySea levelEarth-Surface Processes
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The land bridge between Europe and Sicily over the past 40 kyrs: Timing of emersion and implications for the migration of Homo sapiens

2012

The submerged Sill in the Messina Strait, which is located at a depth of -81 m m.s.l., represents the only possibile connection between Calabria and Sicily during the last lowstand, when the sea level was at about -126 m m.s.l. This multidisciplinary research aim at documenting times and modes the bridge between Calabria and Sicily was emerged, during the last 40 ka BP. The analysis carried out on morphobathymetric, lithological and relative sea level change (both isostatic and tectonic) data allow to hypothesize the continental bridge emerged at least between 21.5 ka and 20 ka cal BP. Moreover, considering erosion processes due to very strong marine currents, it could be emerged for a long…

continental bridgeRelative sea level changestrait of messina strait; continental bridge; relative sea level changeSettore GEO/02 - Geologia Stratigrafica E Sedimentologicastrait of messina straitContinental bridgeSettore GEO/04 - Geografia Fisica E GeomorfologiaStrait of Messina straitGeologyrelative sea level changeContinental bridge; Relative sea level change; Strait of Messina strait; GeologyStrait of Messina strait continental bridge relative sea level change.
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Millstone coastal quarries of the Mediterranean: A new class of sea level indicator

2014

The coasts of Italy still preserve several remnants of coastal quarries built in antiquity, that now provide insights into the intervening sea-level changes occurred during the last millennia. In this paper, we show and discuss a new class of sea level indicator consisting of millstones carved along the rocky coast of southern Italy since 2500 BP, that are currently submerged. They were extracted from beachrocks, sandstones or similar sedimentary rocks, easier for carving by ancient carving tools. Our study focuses on 10 coastal sites located at Capo d'Orlando, Avola, and Letojanni, in Sicily; Soverato, Tropea, and Capo dell'Armi, in Calabria; Castellabate, Palinuro, and Scario, in Campania…

Coastal quarry; Oil millstone; Relative sea level changes; Archaeological sea level markerMediterranean climatecave costiereCarvingCoastal quarryCoastal quarry; Oil millstone; Relative sea level changesSettore GEO/04 - Geografia Fisica E GeomorfologiamacineRelative sea level changesArchaeological sea level markerPresent dayArchaeologymetodologia della ricercaMillstoneTectonicsRelative sea level changeRelative sea level changes;Archaeological sea level marker;Oil millstone;Coastal quarryCoastal quarry Oil millstone Relative sea level changes Archaeological sea level markerSedimentary rockArcheologia dei paesaggi costierivariazioni del livello del mareOil millstoneSea levelGeologyEarth-Surface Processes
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