Search results for " Geomorphology"

showing 10 items of 45 documents

Dynamique fluvial, changement global et pression anthropique dans le bassin, le cours et le delta de l'Ébre

2017

Le fonctionnement des rivières du bassin de l’Èbre a subi d’importants changements depuis 1950. Il s’agit d’un processus rapide et très marqué, de simplification et de stabilisation sur le fleuve principal et sur ses principaux affluents pyrénéens. Ce processus s’est manifesté par des changements dans la morphologie fluviale, le développement de la végétation sur les lits, un rétrécissement de l’espace naturel fluvial et une incision des lits fluviaux. Les facteurs de ce processus sont le changement global dans le bassin, la construction de réservoirs d’eau et d’autres nombreuses pressions humaines directes, notamment d’extractions de graviers et de canalisations. Le delta de l’Èbre, actuel…

styles fluviauximpacto ambiental010504 meteorology & atmospheric sciences0208 environmental biotechnologyGeography Planning and Development02 engineering and technologyenvironmental changecambio ambiental01 natural sciencesenvironmental impact020801 environmental engineeringUrban StudiesGeographyfluvial geomorphologyimpact environnementalgeomorfología fluvialgéomorphologie fluvialechangement environnementalestilos fluvialesHumanities0105 earth and related environmental sciencesEarth-Surface ProcessesDemographychannel patterns
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Stochastic assessment of climate impacts on hydrology and geomorphology of semiarid headwater basins using a physically-based model

2015

Hydrologic and geomorphic responses of watersheds to changes in climate are difficult to assess due to projection uncertainties and nonlinearity of the processes that are involved. Yet such assessments are increasingly needed and call for mechanistic approaches within a probabilistic framework. This study employs an integrated hydrology-geomorphology model, the Triangulated Irregular Network-based Real-time Integrated Basin Simulator (tRIBS)-Erosion, to analyze runoff and erosion sensitivity of seven semiarid headwater basins to projected climate conditions. The Advanced Weather Generator is used to produce two climate ensembles representative of the historic and future climate conditions f…

climate impacts; erosion; geomorphology; modelingmodelingclimate impactgeomorphologyerosion
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The quarry waste "Ravaneti" in Sicily: geomorphologic aspect

2009

quarry waste (ravaneti) geomorphology environment geology quarry environment managementSettore GEO/05 - Geologia Applicata
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Identification and assessment of geosites for territorial enhancement – the study and geoheritage exploitation of the Torre Salsa natural reserve (Si…

2014

The “Ecological Cross-­‐border Networks Malta-­‐Sicily” (RE.MA.SI.) is an international research project founded by the Italia-­‐Malta 2007-­‐2013 Programme. A part of the project aims to carry out a multidisciplinary study for the identification and enhancement of geosites in the Maltese Islands and Sicily. Some areas have been picked out; these areas are spectacular and interesting for the tourists and can make a significant contribution to the understanding the geological and geomorphological history. Field surveys took place for the identification and classification of the most significant geomorphosites and the verification of the collected bibliographical data; in particular, the iden…

Settore GEO/04 - Geografia Fisica E GeomorfologiaGeosites Mediterranean landscape 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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Geomorphology and surface geology of Mount St. Helens volcano

2020

Mount St. Helens is a stratovolcano of the Cascadia volcanic arc well known worldwide for its volcanic collapse and eruption in 1980, which caused considerable destruction and changed the geomorphology of the volcano and of a considerable portion of its surroundings. This paper presents a geomorphology and surface-geology map of both the wider Mount St. Helens, Washington (USA), at the 1:50,000 scale, and of its crater, at the 1:25,000 scale. The map is obtained from the interpretation of two high-resolution, air-borne acquired, digital terrain models, LiDAR dataset, combined with Google Earth imaging, geological information and field surveys. The geomorphology of the area is largely domina…

lcsh:MapsSurficial geologygeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesVolcanic arcGeomorphological mappingGeography Planning and DevelopmentGeochemistrygeomorphology010502 geochemistry & geophysics01 natural sciencesMountVolcanolcsh:G3180-9980mount st. helensEarth and Planetary Sciences (miscellaneous)Stratovolcanovolcanic geomorphologysurficial geologyGeologyAeolian archipelagogeomorphological mapping0105 earth and related environmental sciences
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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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Tidal notches, coastal landforms and relative sea-level changes during the Late Quaternary at Ustica Island (Tyrrhenian Sea, Italy)

2017

In this paper we present and discuss data concerning the morphostructural evolution at Ustica Island (Tyrrhenian Sea, Italy) during Late Quaternary. New insights on the relative sea-level changes of Ustica are coming from data collected during a geomorphological field survey around the island, together with the bathymetric analysis of the surrounding seabed and 14C datings on samples of speleothems, flowstones and marine shells found inside three selected sea caves. The survey was mainly accomplished on June 2015 through the first complete snorkel investigation off the about 18 km-long volcanic coast of the island, which allowed to precisely define location, relationship and morphometric fe…

Mediterranean Sea; Sea caves; Tectonic uplift; Ustica; Volcanic geomorphology; Earth-Surface ProcessesTectonic upliftPillow lava010504 meteorology & atmospheric sciencesSettore GEO/04 - Geografia Fisica E GeomorfologiaUstica;Volcanic geomorphology;Tectonic uplift;Mediterranean Sea;Sea caves010502 geochemistry & geophysics01 natural scienceslaw.inventionPaleontologyTectonic upliftMediterranean seaCavelawVolcanic geomorphology; Tectonic uplift; Sea caves; Ustica; Mediterranean SeaMediterranean SeaSea caveRadiocarbon datingSea levelSea caves0105 earth and related environmental sciencesEarth-Surface Processesgeographygeography.geographical_feature_categoryVolcanic geomorphology Tectonic uplift Sea caves Ustica Mediterranean SeaVolcanic geomorphology Tectonic upliftVolcanic rockOceanographyUsticaVolcanic geomorphologyQuaternaryGeology
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Bridging Malta and Sicily through geoheritage exploitation: Identification and assessment of geosites for territorial enhancement

2013

Malta and Sicily show common geological and geomorphological features, having been also physically linked not later than the Last Glacial Maximum. At present both islands have a high tourist vocation, but their environmental potential is not fully exploited for attracting tourists and visitors. In the framework of an international research project, “Ecological Cross-border Networks Malta-Sicily” (RE.MA.SI.), a multidisciplinary study for the identification, selection and enhancement of geosites in the Maltese and Sicilian islands was carried out. A number of sites both in Malta and Sicily have been identified and qualitatively and quantitatively assessed applying a methodology already teste…

Settore GEO/04 - Geografia Fisica E GeomorfologiaGeosites Mediterranean landscape Geomorphology
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Flank Margin Caves In Telogenetic Limestones In Italy

2017

Almost 20% of Italy is characterized by the outcropping of carbonate massifs ranging in age from Cambrian to Quaternary. Coastal karst is present in many Italian regions: from North-East to South and West: the Gulf of Trieste, the Conero (South of Ancona, Marche), the Adriatic coast of Apulia including Gargano, Murge and Salento, Maratea in Basilicata, Cilento in Campania, Circeo and Gaeta in Latium, Argentario and Giannutri Island in Tuscany, the southernmost part of the Ligurian Alps, Palermo Mts., San Vito Lo Capo, Syracuse coast and Marettimo Island in Sicily, and, especially, in Sardinia, which has carbonate rocks touching the sea along the coast of Balai near Porto Torres, Capo Caccia…

Settore GEO/04 - Geografia Fisica E GeomorfologiaKarstsalt-fresh water mixing coastal karst cave geomorphology coastal uplift speleogenesis
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