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  2. Debris flow - Wikipedia

    en.wikipedia.org/wiki/Debris_flow

    Debris flows with volumes ranging up to about 100,000 cubic meters occur frequently in mountainous regions worldwide. The largest prehistoric flows have had volumes exceeding 1 billion cubic meters (i.e., 1 cubic kilometer). As a result of their high sediment concentrations and mobility, debris flows can be very destructive.

  3. Sediment gravity flow - Wikipedia

    en.wikipedia.org/wiki/Sediment_gravity_flow

    Most flows are liquefied, and many references to fluidized sediment gravity flows are in fact incorrect and actually refer to liquefied flows. [5] Debris flow or mudflow – Grains are supported by the strength and buoyancy of the matrix. Mudflows and debris flows have cohesive strength, which makes their behavior difficult to predict using the ...

  4. Mudflow - Wikipedia

    en.wikipedia.org/wiki/Mudflow

    Today the bottom of Spirit Lake is 100 ft (30 m) above the original surface, and it has two and a half times more surface area than it did before the eruption. The largest known of all prehistoric landslides was an enormous submarine landslide that disintegrated 60,000 years ago and produced the longest flow of sand and mud yet documented on ...

  5. 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]

  6. Sedimentary structures - Wikipedia

    en.wikipedia.org/wiki/Sedimentary_structures

    Flow regimes in single-direction (typically fluvial) flow, which at varying speeds and velocities produce different structures, are called bedforms. In the lower flow regime, the natural progression is from a flat bed, to some sediment movement (saltation etc.), to ripples, to slightly larger dunes. Dunes have a vortex in the lee side of the dune.

  7. Volcanism of the Mount Edziza volcanic complex - Wikipedia

    en.wikipedia.org/wiki/Volcanism_of_the_Mount...

    [160] [170] Lava flows from the two oldest cones travelled to the west and most likely cascaded down the escarpment into Mess Creek valley, but no evidence of this phenomenon has been found on or below the escarpment. [170] The youngest cinder cone, The Ash Pit, formed at the south end of the Mess Lake Lava Field on the northern side of Nagha ...

  8. 2 victims of ancient Pompeii eruption found, along with gold ...

    www.aol.com/news/2-victims-ancient-pompeii...

    An archaeologist works on the recently discovered remains of a victim in the archaeological site of the ancient city of Pompeii, which was destroyed in AD 79 by the eruption of Mount Vesuvius, in ...

  9. Debitage - Wikipedia

    en.wikipedia.org/wiki/Debitage

    He then compared the counts and weights of experimental samples with debris from two prehistoric workshop sites in western North Dakota. The result shows the experimental data sets can explain the technological composition of archaeological samples. Samples from several other sites also are applied this method and derive clear discriminant results.

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