Expansion of ice crystals under stones in the soil pushes the stones up to the surface
What landform does Frost Heave form?
Stone Polygons
What are Stone Polygons?
As stones burst through the surface during Frost Heave, heavier stones roll outwards and small stones stay in the centre, forming shapes in the landscape
What is Ice Contraction?
Refreezing of the active layer causes soil to contract, and the cracks fill up with meltwater
What landforms are formed by ice contraction?
Ice wedges and Pingos
What are Ice Wedges?
Meltwater in cracks of the soil freeze and widen, they can grow up as much as 1m thick and 3m deep
What are Pingos?
A very large dome-shaped isolated hill on flat plains, with summits that rupture to expose their ice cores
How large can Pingos be?
They can have diameters up to 500m and heights of 50m
How are pingos formed?
Surface water infiltrates the ground and freezes, the ice expands and the process repeats until the sediment is pushed up to form hills
What is Frost Shattering also known as?
Freeze Thaw Weathering
What are some landforms associated with Frost Shattering?
Block fields, Scree and Tors
What is a Block Field?
Flat mountains covered with large angular boulders that have broken away due to frost shattering
What is Scree?
Mixture of angular and unsorted rock deposits at the foot of steep slopes. They are also called talus cones
What is a Tor?
Well jointed rocks that usually stand above block fields, made of resistant rock that hasn’t been eroded by frost shattering
What is Nivation?
Névé in north facing hollows collects and enlarges the hollow via abrasion
What does Wind and Meltwater Rivers do to erode?
Absence of vegetation allows wind action and water to erode landscapes
What is a Solifluction Lobe?
The active layer in summer begins to slide down the hill (solifluction), and collects at the bottom (the lobe)
What is Loesś?
Equivalent of a large sand dune, where strong winds collect fine sediment into large dunes
What is a catena?
A connected series of related features changing down a slope due to periglacial processes