Lidar-Based Detection and Interpretation of Glaciotectonic Features of the Morainic Topography of Finland

Figure 2

Locations of the sites, for example (red numbers refer to the Figures) of glaciotectonic landforms and possible glaciological boundaries for frozen bed conditions in Finland, during Last Glacial Maximum (cross-line) and during final local deglaciation (dark blue area) with diminishing frozen bed areas (grey) around areas marked with dark blue, when deglaciation progressed after Younger Dryas. Younger Dryas ice margin marked with blue line (modified from Stroeven et al. 2016 [23]: Figure ).