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  2. Mass wasting - Wikipedia

    en.wikipedia.org/wiki/Mass_wasting

    A landslide, also called a landslip, [10] is a relatively rapid movement of a large mass of earth and rocks down a hill or a mountainside. Landslides can be further classified by the importance of water in the mass wasting process. In a narrow sense, landslides are rapid movement of large amounts of relatively dry debris down moderate to steep ...

  3. A landslide destroyed my North Carolina home during Hurricane ...

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    5 minutes could get you up to $2M in life insurance coverage — with no medical exam or blood test Hurricane Helene caused a flurry of flooding, which can trigger landslides .

  4. Downhill creep - Wikipedia

    en.wikipedia.org/wiki/Downhill_creep

    Downhill creep, also known as soil creep or commonly just creep, is a type of creep characterized by the slow, downward progression of rock and soil down a low grade slope; it can also refer to slow deformation of such materials as a result of prolonged pressure and stress.

  5. Landslide classification - Wikipedia

    en.wikipedia.org/wiki/Landslide_classification

    Finally, landslides triggered by Hurricane Mitch in 1998 killed an estimated 18,000 people in Honduras, Nicaragua, Guatemala and El Salvador. Rainfall triggers a large amount of landslides principally because the rainfall drives an increase in pore water pressure within the soil. Figure A illustrates the forces acting on an unstable block on a ...

  6. Does your home insurance cover a landslide? Here's what you ...

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  7. Rockslide - Wikipedia

    en.wikipedia.org/wiki/Rockslide

    Rockslide at Oddicombe Beach in Devon, UK Rockslides in Nigeria Landslips. A rockslide is a type of landslide caused by rock failure in which part of the bedding plane of failure passes through compacted rock and material collapses en masse and not in individual blocks.

  8. Earthflow - Wikipedia

    en.wikipedia.org/wiki/Earthflow

    It is an intermediate type of mass wasting that is between downhill creep and mudflow. The types of materials that are susceptible to earthflows are clay, fine sand and silt, and fine-grained pyroclastic material. [1] When the ground materials become saturated with enough water, they will start flowing (soil liquefaction). Its speed can range ...

  9. Debris flow - Wikipedia

    en.wikipedia.org/wiki/Debris_flow

    Before a storm that can potentially nucleate debris flows, forecasting frameworks can often quantify the likelihood that a debris flow might occur in a watershed; [18] however, it remains challenging to predict the amount of sediment mobilized and therefore, the total size of debris flows that may nucleate for a given storm, and whether or not ...