Search results for "River"

showing 10 items of 564 documents

Les sites du lit mineur de la Saône en Chalonnais (Saône-et Loire) à la fin du Bronze final

2017

The underwater archaeological campaigns carried out over twenty years, from 1970 to 1990, in the Saône valley, more particularly in the area of Chalon-sur-Saône, first by Louis Bonnamour and then by Annie Dumont, generated a considerable quantity of data concerning settlements, located on fjords or river banks. This documentation, stored at the Musée Denon in Chalon-sur-Saône, was the subject of new studies, initiated by Jean-Michel Treffort for the Ouroux-sur-Saône “Marnay” site and continued by Franck Ducreux, notably for the Chalon-sur-Saône “le gué des Piles” site. On this occasion most of the sites of the region having yielded protohistoric assemblages were reconsidered. This article p…

fords[SHS.ARCHEO] Humanities and Social Sciences/Archaeology and Prehistoryriveschronologiehauts-fondsgués[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistorySaône valleyriverbanksvallée de la Saônechronologyshallow banks
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Shifts in plankton assemblages promoted by free water surface constructed wetlands and their implications in eutrophication remediation

2015

Abstract Two units of free water surface constructed wetlands (FWSCWs) were created in 2009 in a Mediterranean protected site, the Albufera de Valencia Natural Park, to treat eutrophic inflows to the Albufera de Valencia lagoon, the largest coastal lagoon in the Iberian Peninsula, affected by cultural eutrophication. Data of phytoplankton and zooplankton biomass and richness of the inflows and outflows corresponding to the first 3.5 years of operation of the system have been analyzed to evaluate the role of plankton in the eutrophication reversion. The FWSCWs significantly reduced the exported microalgal biomass, stimulated the potential mixotrophic groups of phytoplankton such as Euglenoph…

geographyBiomass (ecology)Environmental EngineeringRiver ecosystemgeography.geographical_feature_categoryEcologyLake ecosystemWetlandManagement Monitoring Policy and LawPlanktonZooplanktonOceanographyPhytoplanktonEnvironmental scienceEutrophicationNature and Landscape ConservationEcological Engineering
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Geophysical investigations in the Flumendosa River Delta, Sardinia (Italy) — Seismic reflection imaging

2006

A geophysical investigation that included seismic-reflection surveying and time-domain electromagnetics (EM) was carried out in the Flumendosa River Delta plain in southeastern Sardinia, Italy. The objective was to improve knowledge of geologic and hydrogeologic controls on a highly productive aquifer hosted in thick Quaternary deposits and known to be affected by an extensive saltwater intrusion. The seismic reflection survey, whose results are reported here, aimed to image the Paleozoic bedrock topography and to obtain detailed structural and stratigraphic information on the sequence of largely fluvial sediments extending from the surface down to bedrock. The survey consisted of two inli…

geographyHydrogeologygeography.geographical_feature_categoryElectromagneticsRiver deltaBedrockFluvialAquiferGeophysicsGeophysicsStratigraphyGeochemistry and PetrologySaltwater intrusionGeomagnetism Hydrology Rivers Rocks Sediments Seismolog yStratigraphy Terrestrial electricity Topography (Earth)Geology
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Partitioning between “wedge-top” river- and wave-dominated successions: an example from the late Tortonian — early Messinian Terravecchia Formation (…

2011

AbstractDetailed field sedimentological and facies analyses have been performed in the Terravecchia Formation cropping out in NW Sicily, in order to differentiate and describe, for the first time, wave- and river-dominated shallow-marine (deltaic) siliciclastic successions. The latter were deposited filling syntectonic basins, developed between the late Tortonian and early Messinian time, within the wedge-top depozone of the Sicilian Foreland Basin System. It has been observed that river-dominated successions, recording the deposition of small fan-deltas are characterized by fining- to coarsening upward, transgressive-regressive sequences which were mostly deposited filling relatively narro…

geographyQE1-996.5geography.geographical_feature_categoryOutcropterravecchia formationwedge-top depozoneGeologyEnvironmental Science (miscellaneous)Sedimentary basinLate Miocenelate miocenelanguage.human_languageforeland basin systemPaleontologyFacieslanguageGeneral Earth and Planetary SciencessicilySiliciclasticriver-dominated deltasTransgressivewave-dominated deltasSicilianForeland basinGeologyOpen Geosciences
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Human Impact Effects on Târnava River Basin Aquatic Biodiversity (Transylvania, Romania)

2020

Today the following categories of human impact are present in the Tarnava Watershed: hydrotechnical works, insufficiently treated/cleaned sewage, river substratum mineral exploitation/over-exploitation, manure leakage, artificial standing water, industry, river embankment, deforestation, pouching, etc., the first three of these inducing the highest impact on the lotic systems habitats and biodiversity.

geographyWatershedgeography.geographical_feature_categoryRiver ecosystembusiness.industryBiodiversityDrainage basinSewageManureDeforestationEnvironmental scienceLeveeWater resource managementbusiness
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The Status of Romanogobio uranoscopus (Agassiz, 1828) Species, in Maramureş Mountains Nature Park (Romania)

2017

Abstract The condition of aquatic habitats typically occupied by Romanogobio uranoscopus within the Maramureş Mountains Natural Park fluctuates, in the best cases, between reduced to average. Good or excellent conservation status is now absent for populations of this species in the researched area. The identified human impact types (poaching, minor riverbeds morphodynamic changes, solid and liquid natural flow changes, destruction of the riparian vegetation and bush vegetation, habitat fragmentation/isolation of population, organic and mining pollution and displaced fish that are washed away during the periodic flooding in the lotic sectors uniformized by humans) are contributing to the dim…

geographyeducation.field_of_studyhuman impactRomanogobio uranoscopusgeography.geographical_feature_categoryHabitat fragmentationRiver ecosystemEcologybiologyEcologyassessment020209 energyPopulationRare species02 engineering and technologybiology.organism_classificationHabitatEnvironmental protectiondanubian longbarbel gudgeonhabitats0202 electrical engineering electronic engineering information engineeringConservation statuseducationQH540-549.5Riparian zoneTransylvanian Review of Systematical and Ecological Research
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Late Holocene erosion of the Canopic promontory (Nile Delta, Egypt)

2017

International audience; The mouths of the Nile Delta are sensitive coastal areas, their geomorphology primarily being mediated by relative sea-level rise and sediment supply. To further document the Holocene evolution of the Nile's Canopic mouth, a core was taken from the southern shores of Abu Qir Bay, close to the ancient Canopic channel. Core bio-sedimentology and chronostratigraphy highlight four stages of marine incursion which are juxtaposed upon the general progradation trend of the Nile coast in this area. Compiled age-depth points from sediment cores taken in Abu Qir Bay underscore two phases of negative sediment budget at the Canopic mouth: (1) a first period, between 3.5 and 2 ka…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesGeoarchaeologySubmersion (coastal management)[SDU.STU]Sciences of the Universe [physics]/Earth SciencesGeology15. Life on land010502 geochemistry & geophysicsOceanography01 natural sciencesOceanography13. Climate actionGeochemistry and PetrologyRiver mouth14. Life underwaterProgradationChronostratigraphySedimentary budgetGeologySea levelHolocene0105 earth and related environmental sciencesMarine Geology
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Middle-Late Pleistocene marine terraces and fault activity in the Sant’Agata di Militello coastal area (north-eastern Sicily)

2012

Abstract The coastal sector of Sant’Agata di Militello (north-eastern Sicily) is characterized by a flight of raised Middle-Upper Pleistocene marine terraces occurring at different heights with respect to present sea level. In particular, the geomorphological survey and the analysis of stereo-pairs of aerial photographs allowed to recognize at least five main orders of well preserved Quaternary surfaces and relative deposits mostly located at the hanging wall and at the footwall of the Pleistocene northwest-dipping Capo d’Orlando normal fault, which controlled the geomorphological evolution of the coastal area. The marine terraces show an overall good morphological continuity and are formed…

geographygeography.geographical_feature_categoryPleistoceneOSL datingFault (geology)coastal tectonicsPaleontologyTectonicsGeophysicsTerrace (geology)marine terracesRiver terracesSedimentary rockQuaternarycoastal tectonics; marine terraces; OSL datingSea levelGeologyEarth-Surface ProcessesJournal of Geodynamics
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Flow-induced vegetation uprooting in a meandering bend : experimental investigation

2022

Abstract Vegetation uprooting is a complex process which depends on many interrelated factors. In this paper, attention is focused on the flow-induced uprooting in river bends, where the flow characteristics vary as effected by the channel's curvature and its continuous changing in the downstream direction. Results are presented by an experimental work done in a high-amplitude meandering flume with mature herbaceous vegetation on the bed. In the first part of the paper, the variation along the bend of the geometrical (length, thickness, and radical architecture) and the mechanical (resistance force) characteristics of the roots are analyzed. In the second part of the paper, the transition f…

geographygeography.geographical_feature_categoryStratigraphyriverFlow (psychology)ElevationSedimentGeologyGeometryexperimentsCurvatureSettore ICAR/01 - IdraulicaFlumevegetationmedicineResistance forcemedicine.symptomVegetation (pathology)uprootingChannel (geography)Geology
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Rhine flood deposits recorded in the Gallo-Roman site of Oedenburg (Haut-Rhin, France).

2006

13 pages; International audience; From the first to the fourth century AD, the Gallo-Roman town of Oedenburg developed in the alluvial landscape of the southern Upper Rhine Graben. Throughout this period, the landscape mosaic, composed of palaeochannels, stable palaeoislands and river terraces, continued to evolve. A district of this town, situated on a lateral Rhine channel system, was archaeologically excavated. Largescale excavation and cross-section analysis provide evidence of changing fluvial conditions during the period under study. At about AD 20 or earlier, this lateral part of the floodplain, affected by very fine sedimentation, was occupied by moribund marshy palaeochannels. When…

geographygeography.geographical_feature_category[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistoryFloodplainFluvialExcavationContext (language use)[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/StratigraphyArchaeologyGraben[ SHS.ARCHEO ] Humanities and Social Sciences/Archaeology and Prehistory[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyRiver terracesPalaeochannelAlluviumGeologyEarth-Surface Processes
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