Nearly 25% of all lakes on earth are located at high latitudes. These formed by a combination thermokarst, glacial, and geological processes. Evidence suggests that the origin periglacial lake formation may be an important factor controlling likelihood to drain. However, geospatial data regarding spatial distribution these dominant Arctic subarctic limited or do not exist. Here, we use lake-spe...

Two cores from a Weichselian periglacial alluvial fan were dated using 14C and OSL, to verify the reliability of both methods check upper dating limit method. Both yielded similar chronology for core Eerbeek-I, with infinite dates lower part where OSL indicated ages over 45 ka. Finite obtained throughout Eerbeek-II, despite stratigraphic evidence suggesting beyond limits. Apparently, additional...

Climate change is amplified in the Arctic, and establishing baseline data for its current character important. Here we present a map of geomorphology Femmilsjøen area, Spitsbergen, northern Svalbard. The regional physiography characterised by low-relief, high elevation mountain plateau, high-relief steep slopes, low-relief coastal lowlands. results indicate that glaciers were most likely warm-b...

A systematic mapping approach characterizes Dartmoor periglacial landform signatures using the geomorphology of nine summit areas displaying well developed tor and blockfield landforms. This combines manual vectorisation with automatic classification surface boulder identification, spectral to reveal patterns distribution. Tors were classified a three-fold scheme: T0 - summits no tors; T1 caste...