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  2. Debris flow - Wikipedia

    en.wikipedia.org/wiki/Debris_flow

    Debris flow channel with deposits left after 2010 storms in Ladakh, NW Indian Himalaya. Coarse bouldery levees form the channel sides. Poorly sorted rocks lie on the channel floor. Debris flow in Saint-Julien-Mont-Denis, France, July 2013 Scars formed by debris flow in Ventura, greater Los Angeles during the winter of 1983. The photograph was ...

  3. Mass wasting - Wikipedia

    en.wikipedia.org/wiki/Mass_wasting

    Debris flow deposits take the form of long, narrow tracks of very poorly sorted material. These may have natural levees at the sides of the tracks, and sometimes consist of lenses of rock fragments alternating with lenses of fine-grained earthy material. [20] Debris flows often form much of the upper slopes of alluvial fans. [22]

  4. Graded bedding - Wikipedia

    en.wikipedia.org/wiki/Graded_bedding

    They can also form in terrestrial stream deposits. In reverse grading or inverse grading the bed coarsens upwards. This type of grading is relatively uncommon but is characteristic of sediments deposited by grain flow and debris flow. [2] A favored explanation for reverse grading in these processes is kinetic sieving. [3]

  5. Flow table test - Wikipedia

    en.wikipedia.org/wiki/Flow_table_test

    The flow table test or slump-flow test is a method to determine consistency of fresh concrete. Flow table test is also used to identify transportable moisture limit of solid bulk cargoes. [ 1 ] It is used primarily for assessing concrete that is too fluid (workable) to be measured using the slump test , because the concrete will not retain its ...

  6. Sediment gravity flow - Wikipedia

    en.wikipedia.org/wiki/Sediment_gravity_flow

    Debris flow deposits are characterized by a bimodal distribution of grain sizes, in which larger grains and/or clasts float within a matrix of fine-grained clay. Because the muddy matrix has cohesive strength, unusually large clasts may be able to float on top of the muddy material making up the flow matrix, and thereby end up preserved on the ...

  7. Lahar - Wikipedia

    en.wikipedia.org/wiki/Lahar

    A hyperconcentrated-flow lahar can leave even frail huts standing, while at the same time burying them in mud, [8] which can harden to near-concrete hardness. A lahar's viscosity decreases the longer it flows and can be further thinned by rain, producing a quicksand -like mixture that can remain fluidized for weeks and complicate search and rescue.

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  9. Landslide classification - Wikipedia

    en.wikipedia.org/wiki/Landslide_classification

    Debris flow channel scoured out by the passage of a debris flow. A flow is a spatially continuous movement in which surfaces of shear are short-lived, closely spaced, and usually not preserved. The distribution of velocities in the displacing mass resembles that in a viscous liquid.