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Par Collection Par Auteur Par Date Par Sujet Par Titre
  • Production systems and innovation in satellite regions : lessons from a comparison between Mechanic Valley (France) and Beauce (Québec)
  • 2011
  • Three-dimensionality, longitudinal profile setting, and paleo-discharge capacity of incised valleys in recent stratigraphy of the Sunda Shelf, Indonesia
  • 2011
  • An analytic multicriteria hierarchical approach to assess landslide vulnerability. Case study: Cornu village, Subcarpathian Prahova Valley/Romania
  • 2011
  • Exposure ages and relative-age data are presented from 8 sites in the Łomnica and Łomniczka valleys to provide information for reconstructing local glaciation chronology. A combination of 10Be exposure ages and Schmidt hammer data obtained
  • for moraines indicate relatively short period of glacier accumulation. A comparison of the obtained chronological data with timing of mountain glaciation in the nearby Úpa Valley is used to propose the first correlative model of Late Quaternary glaciation
  • 2011
  • Hydrologic response of a small forested swamp complex, Seymour Valley, British Columbia
  • 2011
  • Optically stimulated luminescence (OSL) dating of the sedimentation history of the Yzeron Basin (Chaudanne sub-catchment), Rhône Valley, France
  • 2011
  • Spatial structure of valley economic development in the mountainous areas in Beijing
  • 2011
  • Soil organic carbon (SOC) in a humid subtropical forest in Puerto Rico is higher at ridge locations compared to valleys, and therefore opposite to what is commonly observed in other forested hillslope catenas. To better understand the spatial
  • dynamics and soil chemistry. To investigate the influence of litter dynamics, the Century soil organic model was parameterized to simulate the effect of substituting valley species for ridge species. Soil chemical controls on C concentrations were
  • 2011
  • Physical properties and formation of flutes at a polythermal valley glacier : Midre Lovénbreen, Svalbard
  • 2011
  • A spatially explicit degree-day model of Rift Valley fever transmission risk in the continental United States
  • 2011
  • between Pakistan and Afghanistan, extending from the top of the Chapursan Valley of the Hunza region to the Yarkhun Valley from the Karambar Pass to Gazin and to the upper part of the Rich Gol, which belong to Chitral. - (NF)
  • 2011
  • Accessibility ; Alsace ; Communication network ; Europe ; Germany ; Infrastructure ; Region ; Rhine ; Spatial organization ; Switzerland ; Trans-border area ; Transport ; Upper valley
  • 2011
  • on the regional geography of the Garonne valley, and then occupied teaching positions at the Catholic University in Lille, and at universities in Brazil and Quebec. He was also the long-serving director of the French Institute in Barcelona. He was a prolific
  • 2011
  • linked to the direct action of tectonics at the macro-scale level, as in the case of the orientation of the principal valleys. Tectonics have also promoted the spread of gravitational phenomena. The glacial footprint is evident in the numerous inactive
  • 2011
  • Alluvial nappe ; Centre ; Cross section ; Dating ; ESR dating ; France ; Loir-et-Cher ; Palaeogeography ; Pleistocene ; Stratigraphy ; Valley
  • 2011
  • Basse-Normandie ; Discourse ; Enquiry ; Environment ; France ; Landscape ; Living environment ; Perception ; Valley
  • 2011
  • Barents Sea ; C 14 dating ; Catastrophe ; Debris flow ; Earthquake ; European part of Russia ; Geomorphology ; Kola Peninsula ; Landform evolution ; Lithology ; Natural hazards ; Russia ; Sedimentary rock ; Slope ; Valley
  • 2011
  • Aeolian deflation ; Africa ; Erosion ; Escarpment ; Exfoliation ; Mountain ; Namibia ; Pediment ; Planation ; Relief ; Rift ; South Africa ; Valley ; Water parting
  • 2011
  • regions, while minimum temperatures were exceptionally high along the coast. The broad-scale pattern of heat can be tied to adiabatic warming associated with subsidence downstream of a persistent upper-level ridge centered over the Mississippi River Valley
  • 2011
  • in youthful karst where valley floors are narrow. Here, footcaves not only may have been initiated, but also occasionally maintained, enhanced, and modified by migrating streams, as well as by scarp-foot weathering and sapping. Microorganisms that colonize
  • 2011