Search results for "alluvial"

showing 10 items of 31 documents

Climatic and anthropogenic influences on three burgundian watercourses : geoarchaelogy of crossing sites on Loire, Saône and Doubs during the Holocene

2015

A geoarchaeological study was led on four sections of the valleys of the Loire, Saône and Doubs rivers (Burgundy, France) in order to point out the factors influencing the alluvial dynamics on a multimillennial scale, and their effects on the preservation of archaeological information. Investigations started by roman and medieval remains of bridges discovered in active channels, were then carried out on larger parts of alluvial plains, and altogether allowed the evolutions of the channels during the Holocene period to be deducted. Various types of information on alluvial characteristics were crossed through time and space: ancient maps and XXth century or aerial photographs for centennial s…

LoireSedimentological recordsClimateGéoarchéologieClimatArchives sédimentairesFloodsFranchissementsCrossingDoubsHuman activitiesDynamique alluviale[SDU.STU] Sciences of the Universe [physics]/Earth SciencesCruesSaôneAlluvial dynamicsActivités humainesGeoarchaeology
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Eolian and fluvial sedimentation in the southwestern Sinai Mountains, Egypt: a record of flash floods during the late Pleistocene

2012

Wadis emerging from the southwestern Sinai Mountains (Egypt) westwards to the Gulf of Suez are filled by >40 m thick late Pleistocene sediments, which have been subsequently incised to bedrock after the Last Glacial Maximum (LGM). Sedimentation and erosion resulted from changes in the basin's hydrological conditions caused by climate variations. Sediment characteristics indicate distinct processes ranging from high to low energy flow regimes. Airborne material is important as a sediment source. The fills are associated with alluvial fans at wadi mouths at the mountain fronts. Each alluvial fan is associated and physically correlated with the respective sediment fill in its contributi…

Marine isotope stagegeographygeography.geographical_feature_categoryPleistoceneBedrockAlluvial fanFluvialSedimentLast Glacial MaximumPaleontologyGeomorphologyGeologyWadiWater Science and TechnologyHydrology Research
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Urban growth (1956-2012) and soil sealing in the metropolitan area of Valencia (Eastern Spain)

2019

[EN] The aim of this study is to understand the urban growth dynamics from the mid-1950s to 2012 in the Metropolitan Area of Valencia, eastern Spain, and its impact on soils. The study area is a very interesting example of the many changes in land use and land cover in the landscape of Mediterranean alluvial plains. The analysis of urban growth was based on photo interpretation of aerial photographs and GIS based methodology. At a detailed scale (1:10,000), results show that there has been a highly dynamic process produced by the extent of land developed as urban area. In 1956 only 3,441 hectares (9.3% of the overall study area) were occupied by urban use. In 2012 the total sealed surface w…

Mediterranean climate010504 meteorology & atmospheric sciencesSoil ScienceLand cover010501 environmental sciencesLand capabilityUrban area01 natural sciencesSoil degradationMediterranean citiesHigh quality agricultural soilsDegradación de suelosSuelos agrícolas de alta calidad0105 earth and related environmental sciencesgeography.geographical_feature_categoryLand useUrbanizationSoil classificationForestryCiudades mediterráneasMetropolitan areaAlluvial plainGeographySoil waterCapacidad de usoUrbanizaciónSpanish Journal of Soil Science
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The MIS 5 palaeoenvironmental record in the SE Mediterranean coast of the Iberian Peninsula (Río Antas, Almería, Spain)

2015

Se realiza un estudio detallado del episodio cálido MIS 5 en la zona sureste de la Península Ibérica. Se realiza la reconstrucción paleoambiental a partir del estudio polínico y biomarcadores de un sondeo perforado en la costa de Almería. La cronología se estableció a partir del método de racemizaciónd e aminoácidos.Landwards of a MIS5 bar, a borehole core (SRA) was analyzed to establish the relationship between the lagoonal record and the raised beach deposits in the surroundings of the Antas river mouth and to reconstruct the Pleistocene palaeoenvironmental evolution 5 of the southern Mediterranean coast of the Iberian Peninsula. 63 samples were recovered for amino acid racemization datin…

Mediterranean climatePalynologygeographygeography.geographical_feature_categoryPleistoceneAlluvial fanRaised beachQuímica15. Life on landPaleontologyRiver mouthAmino acid datingGeologíaProgradationGeology
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Geochemical characterization and health risk assessment in two diversified environmental settings (Southern Italy).

2021

An integrated approach using chemical and microbial indicators has been tested in two different sites of the Campania Plain (Southern Italy) with different land use covering and different hydrogeological features in order: (1) to define the water-rock interaction processes, (2) to differentiate sources of pollution in a detailed way (3) to evaluate the degree of water quality in the studied alluvial aquifer and (4) to identify the most worrying elements for human's health. Groundwater have showed a HCO3-Ca signature for both investigated sites, and a progressive enrichment in alkali ions has been highlighted moving from the boundary of the plain toward the coastal areas, due to groundwater …

PollutionEnvironmental Engineering010504 meteorology & atmospheric sciencesmedia_common.quotation_subjectFecal pollution010501 environmental sciences01 natural sciencesRisk AssessmentGQIGeochemistry and PetrologyWater QualityEnvironmental ChemistryHumansGroundwaterAlluvial aquifer Factor analysis Fecal pollution GQI HRA Trace elements0105 earth and related environmental sciencesGeneral Environmental ScienceWater Science and Technologymedia_commonHydrogeologyNitratesLand useHealth risk assessmentbusiness.industryGeneral MedicineHRAFactor analysiTrace ElementsFecal coliformAgricultureAlluvial aquiferEnvironmental scienceWater qualityWater resource managementbusinessGroundwaterWater Pollutants ChemicalEnvironmental MonitoringEnvironmental geochemistry and health
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Scour on alluvial bed downstream of grade-control structures

2004

This paper describes an approach for predicting local scour downstream of grade control structures. The developed analysis applies the incomplete self-similarity (ISS) theory for deducing some physically based dimensionless groups controlling the geometrical pattern of the scour profile. The scour measurements available in the literature in conjunction with numerous unpublished data allow a multiregressive calibration of the ISS relationships. The experimental sample includes different bed grain-size distributions and scales of the erosive phenomenon. The results prove that the ratio between the upstream water head and the weir height is able to explain the measurements of scour depth carri…

River and stream beds Scour Drop structures Alluvial channels Particle size distribution Grain (material) Grade control structures Structural controlSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali
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Human settlement dynamics and alluvial dynamics of the Rhine River during the Holocene: Geoarchaeology of the site of Oedenburg (Haut-Rhin, France).

2007

The relationship between alluvial dynamics and control parameters such as climate are well known and understood at plurimillennial and pluriannual time-scales. But it is not really the case at multicentennial and multidecennal time-scales compatible with human society settlement time-scales. In a present and near future context, when human settlement may be affected by strong climatic variation, alluvial dynamics understanding is however a major centre of attention to the development of efficient models. To approach this scale-related question, a segment of the Upper Rhine River presenting both anastomosed and braided was investigated. This area also gives us the opportunity to study settle…

Tomographie électrique[SDU.STU.GM] Sciences of the Universe [physics]/Earth Sciences/Geomorphology[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistoryStratigraphy[SDE.MCG]Environmental Sciences/Global ChangesCartes anciennesMonnaies romainesInondationsMagnetic prospectingStratigraphieGéoradarProspections géomagnétiquesGround Penetrating RadarRhin supérieurArchéologieSystème d'information géographique[ SDU.ENVI ] Sciences of the Universe [physics]/Continental interfaces environmentAlluvial forestsForêts alluviales[SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentPedestrian prospecting[ SDU.STU.GM ] Sciences of the Universe [physics]/Earth Sciences/Geomorphology[SHS.ARCHEO] Humanities and Social Sciences/Archaeology and PrehistoryGeographic Information SystemSédimentologieUpper RhineGeomorphologySedimentology[SDE.ES]Environmental Sciences/Environmental and Society[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces environmentFloodsElectrical Tomography[ SDE.MCG ] Environmental Sciences/Global Changes[SDE.MCG] Environmental Sciences/Global ChangesArchaeology[ SHS.ARCHEO ] Humanities and Social Sciences/Archaeology and PrehistoryProspections pédestres[SDE.ES] Environmental Sciences/Environmental and SocietyGéomorphologie[ SDE.ES ] Environmental Sciences/Environmental and SocietyAncient maps
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Miocene to recent history of the western Altiplano in northern Chile revealed by lacustrine sediments of the Lauca basin (18�15??18�40? S/69�30??69�0…

1995

The intramontane Lauca Basin at the western margin of the northern Chilean Altiplano lies to the west of and is topographically isolated from the well-known Plio-Pleistocene lake system of fluvio-lacustrine origin that covers the Bolivian Altiplano from Lake Titicaca to the north for more than 800 km to the Salar de Uyuni in the south. The Lauca Basin is filled by a sequence of some 120 m of mainly upper Miocene to Pliocene elastic and volcaniclastic sediments of lacustrine and alluvial origin. Volcanic rocks, partly pyroelastic, provide useful marker horizons. In the first period (6–4 Ma) of its evolution, the ‘Lago Lauca’ was a shallow ephemeral lake. Evaporites indicate temporarily close…

Volcanic rockgeographyPaleontologygeography.geographical_feature_categoryPleistoceneEvaporiteGeneral Earth and Planetary SciencesAlluviumStructural basinSedimentologyHoloceneGeologyAlluvial plainGeologische Rundschau
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Hydrogéomorphologie du site, paléoenvironnements et dynamique alluviale.

2015

In Landuré C., Arcelin P., Arnaud-Fassetta G. (Eds.) Le village de La Capelière en Camargue (Arles, Bouches-du-Rhône) du début du Ve s. av. n. è. à la période du Haut Moyen Âge - 2017

[ SDU.STU.GM ] Sciences of the Universe [physics]/Earth Sciences/Geomorphology[SDU.STU.GM] Sciences of the Universe [physics]/Earth Sciences/Geomorphology[SHS.GEO] Humanities and Social Sciences/GeographyCamargue[SDU.STU]Sciences of the Universe [physics]/Earth Sciences[ SDU.STU ] Sciences of the Universe [physics]/Earth Sciences[SHS.GEO]Humanities and Social Sciences/Geography[SHS]Humanities and Social Sciences[SDU] Sciences of the Universe [physics]paléoenvironnementHydrogéomorphologie[SDU]Sciences of the Universe [physics][SDU.STU] Sciences of the Universe [physics]/Earth Sciences[SDU.STU.HY] Sciences of the Universe [physics]/Earth Sciences/Hydrology[SHS] Humanities and Social SciencesFrance[SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphologydynamique alluviale[SDU.STU.HY]Sciences of the Universe [physics]/Earth Sciences/Hydrology[ SDU.STU.HY ] Sciences of the Universe [physics]/Earth Sciences/Hydrology[ SDU ] Sciences of the Universe [physics]ComputingMilieux_MISCELLANEOUS
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A complex thrust sequence in western Himalaya: the active Medlicott Wadia Thrust.

2017

15 pages; International audience; The recent activity of the Medlicott-Wadia Thrust (MWT) is investigated by geomorphic and tectonic studies in the Riasi zone, south of the Pir Panjal range (India, Jammu-Kasmir state of western Himalaya). In the Riasi area, the MWT forms a splay of five faults that dip northward. The recent activity of the splay is quantified using a set of deformed Quaternary alluvial units. The central branch of the thrust splay moved Precambrian limestones above Quaternary sediments and is sealed by 36 ± 3 ka (youngest OSL age) deposits. The other branches offset the top of a 15 ± 1 ka (youngest OSL age) alluvial fan by 180 to 120 m; the two southernmost branches form 17…

[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonicsgeographygeography.geographical_feature_categoryEarthquake010504 meteorology & atmospheric sciencesHimalayaAlluvial fan[ SDU.STU.TE ] Sciences of the Universe [physics]/Earth Sciences/TectonicsActive faultFault (geology)010502 geochemistry & geophysicsFault scarpActive fault01 natural sciencesThrust tectonicsPrecambrianTectonicsIn-sequence thrustThrust splayQuaternaryOut-of-sequence thrustGeomorphologyGeology0105 earth and related environmental sciencesEarth-Surface Processes
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