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  • Pleistocene and Holocene fluvial environments is presented. The record of Holocene alluvial activity is compared with geomorphological research undertaken in the adjacent uplands of the Bowland and Howgill Fells and the more extensive database of change
  • , driven by anthropogenic land-pressure appear to have rendered the floodplain prone to channel migration and the landscape more susceptible to erosion.
  • -related sedimentation. Irragric anthrosols date back more than 3500 years and provide direct evidence for the beginning of irrigation agriculture in this region.
  • various parts of the catchment. The applied methodology strongly differs with the available temporal resolution and the size of the corresponding catchment. All 3 methods show a strong increase in sedimentation rate for more recent periods that can
  • The Holocene landscape history and historical soil erosion were reconstructed at Albersdorf (Schleswig-Holstein) from soils and colluvial layers. In contrast to many landscapes in central Europe, agricultural land use and soil erosion were more