High Resolution DEMs for the analysis of fluvial and ancient anthropogenic landforms in the alluvial plain of Padua (Italy)
Italia ; LiDAR ; Llanuraaluvial ; Modelo numérico de terreno ; Ocupación humana ; Padua ; Paleogeografía ; Sedimentario ; Teledetección ; Véneto
Alluvial plain ; Digital elevation model ; Human occupation ; Italy ; LiDAR ; Padua ; Palaeogeography ; Remote sensing ; Sedimentary ; Veneto
The alluvial plain around Padua results from the sedimentary activity of the Brenta and the Bacchiglione rivers since the last glaciation to the modern times. The inner and oldest part of the city developed on the banks of a former meander
of the Brenta River, later occupied by a minor course, the Bacchiglione. Early archaeological evidence dates back to the final Bronze Age and the first urban settlement started in the Iron Age. The underground of the city centre consists of alluvial sediments
Cono de deyección ; Geomorfología ; Holoceno ; Hungría ; Llanura de inundación ; Morfometría ; Paleoambiente ; Pleistoceno superior
The development and relationship between an alluvial plain and a neighboring alluvial fan was evaluated in the paper on the case of the Lower Tisza Region and the Maros alluvial fan. The paleo-channels on the surface differ in their size and channel
Four pedons from the alluvial plain of Drama (NE Greece) were investigated in order to provide detailed information on their morphology, chemical, physical and mineralogical properties, classification and genesis. Smectite (montmorillonite
) is the dominant clay mineral and was mainly inherited from the parent sediments and by neoformation. The pedons located in the highest points of the alluvial plain were classified as Chromic Haploxererts and those in the lowest landscape were classified as Typic
Haploxererts. The properties of these Vertisols reflect the impact of climate (alternating wet–dry periods), landscape position (alluvial plain; seasonally water saturated), and parent material (clayey, smectite-dominated fluvio-lacustrine, highly calcareous
River bifurcations are critical but poorly understood elements of many geomorphological systems. They are integral elements of alluvial fans, braided rivers, fluvial lowland plains, and deltas and control the partitioning of water and sediment
(PZ) of the western Ganga Plain. A large alluvial fan and incised river valley surfaces with numerous cut-off channels/palaeochannels are the main landforms of the area. The proximal basin margin, against the Himalaya mountain range, is defined
The lower alluvial Pineios River has reacted to major geological controls, surface deformation and uplift movements caused by the activity of the recently mapped Pineios normal fault zone and salt tectonics in Kyllini peninsula resulting
in order to determine the causes of the diversion of the lower (alluvial) Pineios River (NW Peloponnese, Greece) and shoreline displacements.
This paper presents a method of map construction that illustrates potential geomorphological effects of a catastrophic flood occurring on the alluvial plain of a mountain river. It is suggested that the map of geomorphological hazards proposed here
the intensity and spatial scale of flood damage within an alluvial plain and along a river channel. – (BJ)
Acción antrópica ; Canal aluvial ; Corriente de agua ; Datación Carbono 14 ; Diagrama polínico ; Dinámica fluvial ; Estratigrafía ; Francia ; Francia del Este ; Geocronología ; Holoceno ; Llanuraaluvial ; Ocupación humana ; Paleoambiente
Action anthropique ; Chenal alluvial ; Cours d'eau ; Datation C 14 ; Diagramme pollinique ; Dynamique fluviale ; France ; France de l'Est ; Géochronologie ; Holocène ; Occupation humaine ; Palynologie ; Paléo-environnement ; Plaine alluviale ; Saône
Alluvial channel ; Alluvial plain ; Archeological site ; C 14 dating ; Eastern France ; Fluvial dynamics ; France ; Geochronology ; Holocene ; Human impact ; Human occupation ; Lateglacial ; Palaeo-environment ; Palynology ; Pollen diagram ; Saône
methods that integrate soil science, geomorphology and palynology. To reach this goal, soil properties of a catena of the Jataí Ecological Station (Luiz Antonio — São Paulo State) were analyzed in 4 sectors : Slope, Terrace I, Terrace II and Alluvial Plain
Comunidad de Madrid ; Corriente de agua ; Cubierta vegetal ; Cuenca hidrográfica ; Dinámica fluvial ; España ; Llanuraaluvial ; Llanura de inundación ; Paisaje ; Propiedad fundaria ; Río
Alluvial plain ; Community of Madrid ; Floodplain ; Fluvial dynamics ; Landed property ; Landscape ; Plant canopy ; River ; Spain ; Stream ; Watershed