High-resolution mapping of glacial landforms in the North Alpine Foreland, Austria

In this study results from traditional field mapping were merged with precise elevation information from airborne LiDAR (Light detection and ranging) surveys. Morphological and sedimentological data provide new results fromthe Austrian (eastern) part of the Salzach piedmont glacier during times of and shortly after the Last GlacialMaximum(LGM). The variations inmeltwater discharge had amajor impact on the development of glacial landforms. In areas with high meltwater supply erosional or debris reworking processes play a major role, represented by drainage channels, drumlins and kettled, low relief hummocky moraine with low slope angles. Lowdischarge areas are associatedwith distinct depositional forms such as high relief endmoraines (up to 30 m) and hummockymoraine (averaging 20 m)with high slope angles. Isolated conical kamesmay reach heights up to 45 m. Fluvial activity is supposed to rise towards the end of the glacial cycle causing high melting rates and comprehensive debris reworking. The formation of terminal lakes and associated widespread, inorganic lake clays are the last depositswithin the study area before the Salzach Glacier completely receded to its main valley. The survey of glacial landforms through the combination of field mapping and high-resolution DEMderived from airborne LiDAR missions gives precise information on transport and deposition during the last glacial cycle of the eastern Salzach Glacier piedmont lobe.