Search results for "River terraces"

showing 4 items of 4 documents

STOP 9: Upper Daugava spillway valley and associated gully network at Vasargelišķi

2014

HydrologySpillwayriver terracesGeographyglaciokarstKvartāra ģeoloģijaRiver terraces:NATURAL SCIENCES::Earth sciences::Exogenous earth sciences::Quaternary geology [Research Subject Categories]erosional landformsGeomorphologyLate Quaternary Terrestrial Processes, Sediments and History: From Glacial to Postglacial Environments
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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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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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STOP 4: Internal structure and genesis of the sediments underlying Terrace III of the River Gauja at Dukuļi farmhouse and Valmiera town

2014

the River Gaujageographygeography.geographical_feature_categoryriver terracesTerrace (geology)River terracesKvartāra ģeoloģija:NATURAL SCIENCES::Earth sciences::Exogenous earth sciences::Sedimentology [Research Subject Categories]Physical geography:NATURAL SCIENCES::Earth sciences::Exogenous earth sciences::Quaternary geology [Research Subject Categories]Archaeologyflow regime
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