Slump (geology) - Wikipedia
WEBA slump is a form of mass wasting that occurs when a coherent mass of loosely consolidated materials or a rock layer moves a short distance down a slope. [1] Movement is characterized by sliding along a concave-upward or planar surface.
Slump | Earthquake, Landslide & Subsidence | Britannica
WEBslump, in geology, downward intermittent movement of rock debris, usually the consequence of removal of buttressing earth at the foot of a slope of unconsolidated material. It commonly involves a shear plane on which a back-tilting of the top of the slumped mass occurs.
15.2: Classification of Mass Wasting - Geosciences LibreTexts
WEBApr 24, 2024 · Slump is a type of slide (movement as a mass) that takes place within thick unconsolidated deposits (typically thicker than 10 meters). Slumps involve movement along one or more curved failure surfaces, with downward motion near the top and outward motion toward the bottom (Figure \(\PageIndex{8}\)).
Types of Wasting: Slump, Rockslide & Debris Flow – Geology In
WEBMass wasting is a type of erosion that results in the mass movement of rock, soil and debris down a slope. Learn about the different types of mass wasting, including slumps, rockslides, debris flows and earthflows.
10.5: Reading- Slump and Creep - Geosciences LibreTexts
WEBSlump moves materials as a large block along a curved surface (figure 1). Slumps often happen when a slope is undercut, with no support for the overlying materials, or when too much weight is added to an unstable slope.
15.2 Classification of Mass Wasting – Physical Geology
WEBSlump is a type of slide (movement as a mass) that takes place within thick unconsolidated deposits (typically thicker than 10 m). Slumps involve movement along one or more curved failure surfaces, with downward motion near the top and outward motion toward the bottom (Figure 15.14).
5.2: Classification of Mass Wasting - Geosciences LibreTexts
WEBNov 24, 2023 · Slump is a type of slide (movement as a mass), that takes place within thick unconsolidated deposits (typically greater than 10 m). Slumps involve movement along a curved surface, with downward motion near to the top and outward motion towards the bottom (Figure 5.2.7).
Slide and Slump - SpringerLink
WEBJan 1, 2016 · Slides and rotational slides (slumps) include downward and horizontal displacement of rigid or semi-rigid masses of soil (earth and debris), or rock under the influence of gravity. This includes movements of land and the sea bottom. It differs from a collapse where displacement is entirely vertical.
Slide and slump structures - SpringerLink
WEBJan 1, 2013 · Slumps and slides are downslope movements of sediments above a basal shear surface where there is, respectively, significant and insignificant internal distortion of the bedding (Stow, 1986). In slumps, the bedding should be recognizable, otherwise they classify as debris flows.
Reading: Slump and Creep | Geology - Lumen Learning
WEBSlump moves materials as a large block along a curved surface (figure 1). Slumps often happen when a slope is undercut, with no support for the overlying materials, or when too much weight is added to an unstable slope.
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