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  • Measurement of solifluction rates using multi-temporal aerial photography
  • Aerial photography ; Geographical information system ; Least squares method ; Model ; Periglacial features ; Photogrammetry ; Sediment transport ; Solifluction ; Sweden ; Watershed
  • A new method is presented to assess decadal solifluction lobe movement and volumetric changes at the catchment scale. The method is based on photogrammetrical analysis of orthorectified repeat aerial photography in a geographic information system
  • (GIS). High resolution aerial photographs from two valleys in northern Sweden, Kärkevagge and Låktatjåkka valleys, are used to quantify changes of the lobe fronts, as an indication of solifluction rates over a period of 41 years. Two methods
  • , photogrammetrical analysis is recommended as an important tool for detecting decadal solifluction movement at the catchment scale.
  • Local variations of solifluction activity and environment in the Abisko Mountains, Northern Sweden
  • Erosion ; Mountain ; Northern Sweden ; Sediment transport ; Slope ; Slope dynamics ; Slope gradient ; Soil moisture ; Solifluction ; Sweden ; Vegetation
  • Seven sites were selected for measurement of solifluction movement rates and correlation with the local environmental factors. Positions of movement markers and the terrain were recorded and the grid areas were digitally reconstructed. This allowed
  • displacement than where solifluction landforms exist. Solifluction is an important denudational agent in the region and has its greatest impact on landscape development in the western part of the region.
  • A 35-year record of solifluction in a maritime periglacial environment
  • Experimentation ; Maritime environment ; Mountain ; Periglacial features ; Scotland ; Slope dynamics ; Solifluction ; United Kingdom ; Vegetation
  • Eight segmented PVC columns (Rudberg pillars) inserted vertically in the treads of 3 vegetation-covered (turf-banked) solifluction lobes at altitudes of 912–1031 m in the Fannich Mountains of NW Scotland were exhumed 35 years after insertion
  • at unvegetated sites where needle ice creep is the dominant component of solifluction.
  • Which environmental factors determine recent cryoturbation and solifluction activity in a subarctic landscape? A comparison between active and inactive features
  • Cryoturbation ; Finland ; Lapland ; Model ; Periglacial features ; Soil properties ; Solifluction ; Spatial distribution ; Statistical analysis ; Subarctic zone ; Vegetation
  • modelling approach and comprehensive data on active and inactive cryoturbation and solifluction features from a subarctic area of Finnish Lapland are investigated at a landscape scale. In the cryoturbation modelling, vegetation abundance is the most
  • and ground material in the distribution modelling. For solifluction, the key variables determining the activity-inactivity variation are mean annual air temperature and mean maximum snow depth, whereas vegetation abundance and slope angle control
  • Solifluction in the mountains of Central Asia : distribution, morphology, processes
  • Active layer ; Asia ; Central Asia ; Freeze-thaw cycle ; Holocene ; Mass movement ; Mountain ; Periglacial features ; Permafrost ; Pleistocene ; Quaternary ; Slope dynamics ; Solifluction
  • Aeolian deflation ; Cold area ; Finland ; Geomorphological mapping ; Lapland ; Model ; Palsa ; Periglacial features ; Solifluction ; Statistics ; Subarctic zone
  • The AA. downscaled 4 different periglacial features (wind deflation, palsa mire, earth hummock and sorted solifluction sheet) from a 100 ha grid to a 1 ha grid resolution utilizing 2 different techniques : point sampling (PSA) and direct (DA
  • of the palsa mire and solifluction sheet models was excellent, whereas the AUC values of deflation and earth hummock models were lower.
  • Observations on regional variation in solifluction landform morphology and environment in the Abisko region, northern Sweden
  • Cold area ; Geomorphometry ; Periglacial features ; Slope deposit ; Snow cover ; Soil properties ; Solifluction ; Spatial variation ; Sweden ; Vegetation
  • Morphometric analysis of solifluction lobes and rock glaciers in the Swiss Alps
  • Alps (The) ; Classification ; Creep ; Freeze-thaw cycle ; Geomorphometry ; Mountain ; Periglacial features ; Permafrost ; Rock glacier ; Solifluction ; Switzerland
  • Active layer ; Arctic Region ; Climatic warming ; Cold area ; Ice wedge ; Periglacial features ; Permafrost ; Pingo ; Soil temperature ; Solifluction ; Spitsbergen ; Svalbard
  • This report overviews observations on periglacial geomorphology in central Spitsbergen, which have been undertaken by the Japanese geomorphological groups. Focus is given to permafrost-related processes, including solifluction, thermal contraction
  • cracking and pingo growth. Annual freeze-thaw action dominates the ground, resulting in extensive occurence of solifluction and shallow landslides on soil slopes. Special attention will be paid to how permafrost and the overlying active layer constrain
  • Arctic Region ; Cold area ; Gley ; Grain size distribution ; Microrelief ; Patterned ground ; Plant canopy ; Soil ; Soil properties ; Solifluction ; Spitsbergen ; Svalbard
  • The following patterning of the ground surface was observed in the Bellsund region: sorted circles, mud boils, cell forms, solifluction (striped) forms and large polygons (tundra polygons). The soils associated with these forms often have different
  • France ; Landslide ; Mass movement ; Microstructure ; Slope ; Slope dynamics ; Soil ; Soil properties ; Solifluction
  • cases, mass movements can be related to simple shear. The development of these features varies according mainly to the type of mass movement (solifluction, debris flow or earth slide). A careful study of the microscopic features leads to a better
  • Late Holocene solifluction lobe activity in the Mount Rae area, southern canadian Rocky Mountains
  • Soil development on sandstone solifluction deposits with varying contents of loess materials
  • Radiocarbon dating evidence for the initiation of solifluction ca. 5500 years B.P. at Okstindan, North Norway
  • Relationship between ground ice and solifluction : field measurements in the Daisetsu Mountains, Northern Japan
  • Creep ; Ground ice ; Hokkaido ; Japan ; Mountain ; Periglacial features ; Slope dynamics ; Solifluction ; Thawing
  • Soil temperature, surface heave and downslope movements were monitored continuously for one year (1998-99) within a solifluction lobe developed on seasonally frozen ground in the Daisetsu Mountains, northern Japan. Observations were also made
  • Solifluction processes on permafrost and non-permafrost slopes : results of a large-scale laboratory simulation
  • Basse-Normandie ; Caen ; Experimentation ; France ; Freeze-thaw cycle ; Model ; Periglacial features ; Permafrost ; Seasonal variation ; Slope dynamics ; Solifluction
  • The AA. compare solifluction processes observed in 2 large-scale laboratory physical models that had identical slope geometries and soil characteristics, but contrasting thermal regimes. Model 1 was subject to cycles of freezing and thawing from
  • The role of interannual climate variability in controlling solifluction processes, Endalen, Svalbard
  • Active layer ; Air temperature ; Arctic Region ; Climatic variability ; Cold area ; Freeze-thaw cycle ; Periglacial features ; Soil temperature ; Solifluction ; Svalbard ; Temperature
  • of the likely impacts of longer term and larger scale changes in climate. The first 3 years of measurements reported here represent the initial phase of a planned long-term solifluction monitoring programme. Comparisons between the 3 annual cycles of ground
  • Optical Dates from British Isles Solifluction Sheets Suggests Rapid Landscape Response to Late Pleistocene Climate Change
  • Climatic change ; Dating ; Lateglacial ; North-East England ; Palaeogeography ; Paraglacial ; Periglacial features ; Quaternary ; Solifluction ; United Kingdom ; Upper Pleistocene
  • The most widespread depositional landforms in many of the upland valleys of the British Isles which have undergone glaciation during the Last Glacial Maximum (LGM) are so-called solifluction sheets. This paper presents the first dates from
  • Rates and controls of soil movement on a solifluction slope in the Mount Rae area, Canadian Rocky Mountains in Periglacial processes and landforms.
  • Aeolian deflation ; Debris flow ; Landslide ; Mountain ; Nivation ; Periglacial features ; Slope dynamics ; Slovak Republic ; Solifluction ; Tatra Mountains
  • This paper presents the results of direct measures of some geomorphic processes acting, or said to be active, in the alpine area of the Tatra Mountains. Measurements of debris flows and debris slides, as well as of eolian-nivational, solifluction