Periglacial processes

    Cards (19)

    • What is Frost Heave?
      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