Search results for "coastal geomorphology"

showing 6 items of 6 documents

Geoarchaeology as a tool to understand ancient navigation in the northern Persian Gulf and the harbour history of Siraf

2020

International audience; Historical texts and archaeological studies attest to the maritime and trade importance of the Persian Gulf since the Sassanid Empires. Nonetheless, there is a paucity of data regarding ancient navigation and the reasons for a shift in m aritim e trade from the western (e.g. Shatt-al-Arab) to eastern (Siraf) Persian Gulf by the Abbasid dynasty. For som e scholars, Siraf was occupied between 360 and 977 CE, after which tim e an earthquake en-trained the dem ise of the city. However, it is unclear when Siraf was founded and how natural navigation conditions changed for ocean-going vessels in harbours of the NW Persian Gulf. To address this knowledge gap, we here presen…

010506 paleontologyArcheologyPersian GulfSirafCoastal geographyHiatusSiraf Geoarchaeology Persian Gulf Shamal winds Coastal geomorphology Relative sea level01 natural sciencesNatural (archaeology)0601 history and archaeology14. Life underwaterShamalGeoarchaeology0105 earth and related environmental sciencescomputer.programming_language060102 archaeologyGeoarchaeology06 humanities and the artsDemiseArchaeologyCoastal geomorphologyCoastal erosionGeography13. Climate actionRelative sea levelHarbour[SDE]Environmental SciencesShamal windscomputer
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Geomorphological environment: dunes in Agrigento coast

2008

[ITA] La fascia costiera di San Leone (Agrigento-Siclia). è costituita da una spiaggia sabbiosa delimítala verso terra da un complesso dunale di particolare pregio. L'assetto geomorfologico di questo litorale è stato inlluenzato dal forte grado di antropizzazione del luogo. La fascia costiera nel tempo ha súbito degli avanzamenti e arreiramenti. Sono stati quindi analizzati e proposti alcuni rimedi. mirali alia ricostruzione. al mantenimenlo e alia diíesa della duna.

GeomorphologyCoastal environment dunes coastal geomorphology
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Preservation of modern and mis 5.5 erosional landforms and biological structures as sea level markers: A matter of luck?

2021

The Mediterranean Basin is characterized by a significant variability in tectonic behaviour, ranging from subsidence to uplifting. However, those coastal areas considered to be tectonically stable show coastal landforms at elevations consistent with eustatic and isostatic sea level change models. In particular, geomorphological indicators—such as tidal notches or shore platforms—are often used to define the tectonic stability of the Mediterranean coasts. We present the results of swim surveys in nine rocky coastal sectors in the central Mediterranean Sea using the Geoswim approach. The entire route was covered in 22 days for a total distance of 158.5 km. All surveyed sites are considered to…

Marine isotope stageSettore BIO/07 - EcologiaErosion -- Mediterranean RegionBiological indicators; Coastal geomorphology; Geoswim; Landforms; Mediterranean Sea; MIS 5.5; Sea level change010504 meteorology & atmospheric sciencesGeography Planning and DevelopmentGeoswimAquatic ScienceCoastal geography010502 geochemistry & geophysicsBiological indicator01 natural sciencesBiochemistryNeotectonics -- Mediterranean RegionMediterranean seaMediterranean SeaSea level changeTD201-500Sea level0105 earth and related environmental sciencesWater Science and TechnologyShoregeographyPast sea levelgeography.geographical_feature_categorycoastal geomorphologyWater supply for domestic and industrial purposesCoast changes -- Mediterranean Region -- Case studiesSubsidenceHydraulic engineeringcoastal geomorphology MIS 5.5 landforms biological indicators sea level change Mediterranean Sea GeoswimSettore GEO/01 - Paleontologia E Paleoecologiabiological indicatorsCoastal geomorphologyMIS 5Sea level -- Mediterranean RegionMIS 5.5LandformInterglacialBeach erosion -- Mediterranean RegionPhysical geographyTC1-978landformssea level changeGeology
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Comparing marine geology and coastal geomorphology vertical tectonic data, a case study between Acquedolci and Patti (Messina)

2011

The study of new data on vertical movements show a complex geologic response in a restricted sector of coastal area between Acquedolci and Patti (north-eastern Sicily). Different surveys allowed to the recognition of morphological, biological and archaeological markers of paleo-sea level. The analysis of these markers and the absolute datings performed, allowed to reconstruct the history of vertical deformation of this sector but only the comparison among coastal geomorphological data and marine geological data of platform-scarp continental system associates, allowed to find the necessary keys words to explain the geologic complexity of this sector.

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaCoastal geomorphology Tectonic uplift North-eastern Sicily
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Spatial extent of recent vertical tectonic motions misured in NE Sicily coastal area. Insights from marine geology and coastal geomorphology studies.

2011

Vertical position of sea-level, pointed out by related deposits and morphologies, provide useful markers to estimate tectonic uplift rates. For the Holocene very high uplift rates are misured in the northeast Sicily coast (Antonioli et al., 2009). This study compare vertical tectonic movements and marine geology data in the coastal sector between Capo d’Orlando and Brolo (NE Sicily); tectonic lineaments show different trends both onland (Nigro & Sulli, 1995) and offshore (Nicolich et al.,1982) and also the morphological response follow closely this difference. The geomorphologic survey provided data on Holocene uplift rates. We studied an archaeological ancient quarry of grinding wheels for…

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaCoastal geomorphology Tectonic uplift North-eastern Sicily Marine geology
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The San Leone (Agrigento) dunes: coastal geomorphology

2007

dunes coastal geomorphologySettore GEO/05 - Geologia Applicata
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