WebbComplex cliff profiles are produced where cliffs are composed of strata of differing lithology. Less resistant strata erode and weather quickly, being cut back rapidly, wave cut notches may be formed. Resistant strata erode and weather slowly, retreating less rapidly. They may form a 'bench' feature at the cliff base. WebbThe slumping material usually moves intact as a single mass, without any internal deformation of material. It's slower than blockfall, often occurring in 'slow motion', and …

What is slumping in geography? - Our Planet Today

Webb1) The type of wave hitting the coastline (destructive or constructive). Constructive waves have strong swash (the movement of the wave up the beach) and weaker backwash (the … WebbProcesses of glacial transportation. Glaciers move very slowly. As they move, they transport material from one place to another: As freeze-thaw weathering occurs along … scs gran canaria

Coastal Systems: How Mass Movement Affects the …

WebbSlumping. Slumping occurs when material moves along a curved path. The technical term is ‘rotation’ so slumping is also known as ‘rotational slip’ or ‘rotational slump’. In the photograph the path of the slump is highlighted by the red line. It occurs mainly in soft and uniform rocks such as silts and clays, and can be triggered by ... Webb16 juni 2011 · Enjoy access to millions of presentations, documents, ebooks, audiobooks, magazines, and more ad-free. Webb2B.6C: Landforms produced by Mass Movement. The angular blockfall debris accumulates at the cliff foot to form a talus scree slope, a fan shaped mound of material. Undercutting of cliffs by the creation of wave-cut notches can lead to large falls and talus scree slopes at their base. A talus scree slope has a slope angle of 34-40' (larger ... scs grantham