The photograph illustrates patterned ground in a periglacial environment.
Identify the geometric shape of the repeated ground patterns.
State one visible characteristic of the vegetation cover.
Explain two ways seasonal thaw can alter periglacial landscapes.
Explain two factors that influence the development of patterned ground in periglacial environments.
The photograph illustrates the sorting of surface material in a periglacial landscape.
State where the larger stones and the finer material are concentrated within the ground patterns.
Outline one reason why freeze-thaw weathering can be effective in periglacial environments.
Explain two conditions that promote solifluction in periglacial environments.
The diagram illustrates the relationship between moving glacier ice and associated landscape features.
Identify the glacier zone above the equilibrium line.
State the position of the lateral moraine relative to the glacier ice.
Outline one way in which debris is supplied to a lateral moraine.
Explain two factors that influence the rate of glacial abrasion.
The diagram illustrates zones of glacier activity and the accumulation of glacial debris.
Identify the zone occupying the lower glacier tongue below the equilibrium line.
Identify the named moraine feature shown beside the tributary glacier.
Outline one way in which glacier melting results in sediment deposition.
Explain the formation of a medial moraine.
Explain one way in which glacial action can lead to the formation of a lake.
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Examine the importance of glacial transport in explaining the distribution of moraines and erratics.
Examine the influence of wind conditions and sand supply on the shape and movement of dunes.
To what extent is thawing more important than freezing in shaping periglacial landscapes?
To what extent is running water more important than wind in the erosion, transportation and deposition of material in hot, arid environments?
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Examine why rock structure has a greater influence on the development of some hot, arid landforms than others.
To what extent can glacial erosion alone explain the formation of cirques and pyramidal peaks?