Accumulation of scree due to active slope processes

Loess deposits blanketing the landscape and forming steep scarps where eroded

Frost polygons

Boulder fields

Slope instability

Ice wedge polygons

Valley bulge

Cambering of strata

Gyttja (organic gel) in lakes

Pingos

Taliks - zones of unfrozen ground, deeper talik beneath lake

Permafrost

Solifluction lobes

Stone stripes

Taliks beneath rivers and small ponds

Active layer -
seasonally frozen

Permafrost - permanently frozen ground

Cryoturbation of originally horizontal sediments