Yahoo Web Search

Search results

  1. A slump is a type of mass wasting that results in the sliding of coherent rock materials along a curved surface. In a slump, a portion of the mountain moves down a short...

  2. www.encyclopedia.com › geography-general › slumpSlump | Encyclopedia.com

    May 14, 2018 · Like the term mudslide, slump is frequently used but is not defined in the classification system used by most landslide specialists. Depending on the type of earth material involved, a slump can be properly described as a rock slide, debris slide, or earth slide with predominantly rotational movement.

  3. A 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. Movement is characterized by sliding along a concave-upward or planar surface.

  4. Apr 24, 2024 · Home. Bookshelves. Geology. Physical Geology (Earle) 15: Mass Wasting. 15.2: Classification of Mass Wasting. Page ID. Steven Earle. Vancover Island University via BCCampus. It’s important to classify slope failures so that we can understand what causes them and learn how to mitigate their effects.

  5. Rotational Slide (Slump): A rotational slide is a type of landslide movement that occurs in a turning moment, about a pivot point that is above the center of gravity. This is typically due to an increased normal force on a slope, as well as a reduced cohesion factor of the soil mass materials.

  6. Jan 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.

  7. www.oxfordreference.com › display › 10Slump - Oxford Reference

    Quick Reference. A form of mass movement (also called a single rotational slide) where rock and soil rotate backwards with movement down a concave face: ‘a more or less rotational movement, about an axis that is parallel to the slope contours, involving shear displacement along a concavely up-ward facing failure surface’ (D. Varnes1978).

  1. People also search for