Ice Wedges (Freeze thaw)
-Created by freeze thaw weathering
-Ground contracts, cracks, and is filled by meltwater, which freezes/ melts and expands creating ice wedge
Patterned Ground (Freeze thaw)
-Extensive ice wedges create patterns shaped like polygons
Blockfields (Freeze thaw/Frost shatter)
-Repeated freeze thaw in rocks creates areas of angular rock fragments in situ
Pingos
-Frost heave causes flat, wide, dome shaped hills to appear
-Closed and open systems
Solifluction lobes
-Active layer saturated and slumps downhill creating lobes
Loess
Wind-blown, silt-sized sediment deposits that formed during and after glacial periods, often in areas bordering large glaciers