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  2. Volcanic ash - Wikipedia

    en.wikipedia.org/wiki/Volcanic_ash

    The density of volcanic ash varies between 700 and 1200 kg/m 3 for pumice, 2350–2450 kg/m 3 for glass shards, 2700–3300 kg/m 3 for crystals, and 2600–3200 kg/m 3 for lithic particles. [26] Since coarser and denser particles are deposited close to source, fine glass and pumice shards are relatively enriched in ash fall deposits at distal ...

  3. Ancient footprints of Acahualinca - Wikipedia

    en.wikipedia.org/wiki/Ancient_footprints_of...

    The tracks are fossil Late Holocene human footprints left behind in volcanic ash and mud, which solidified about 2,120±120 years ago, shortly after the group of up to 15 people passed by. [2] It is sometimes reported that the people were running to escape from a volcanic explosion, but the distance between the footprints indicates a walking ...

  4. Tephra - Wikipedia

    en.wikipedia.org/wiki/Tephra

    Tephrochronology is a geochronological technique that uses discrete layers of tephra—volcanic ash from a single eruption—to create a chronological framework in which paleoenvironmental or archaeological records can be placed. Often, when a volcano explodes, biological organisms are killed and their remains are buried within the tephra layer.

  5. The Biggest Volcanic Eruptions in Human History

    www.aol.com/biggest-volcanic-eruption-human...

    A.D. 79: Mount Vesuvius, Italy. Mount Vesuvius has erupted eight times in the last 17,000 years, most recently in 1944, but the big one was in A.D. 17. One of the most violent eruptions in history ...

  6. Volcanic hazard - Wikipedia

    en.wikipedia.org/wiki/Volcanic_hazard

    Tephra is a generalized word for the various bits of debris launched out of a volcano during an eruption, regardless of their size. [4] Pyroclastic materials are generally categorized according to size: dust measures at <1/8 mm, ash is 1/8–2 mm, cinders are 2–64 mm, and bombs and blocks are both >64 mm. [5] Different hazards are associated with the different kinds of pyroclastic materials.

  7. What you need to know about volcanic ash

    www.aol.com/know-volcanic-ash-195524299.html

    A volcanic eruption is one of the most powerful forces in nature, a seemingly unstoppable phenomenon that can have far-reaching impacts far beyond the area surrounding the volcano itself. When a ...

  8. Siberian Traps - Wikipedia

    en.wikipedia.org/wiki/Siberian_Traps

    It has been suggested that, as the Earth's lithospheric plates moved over the mantle plume (the Iceland plume), the plume produced the Siberian Traps in the Permian and Triassic periods, after earlier producing the Viluy Traps to the east, and later going on to produce volcanic activity on the floor of the Arctic Ocean in the Jurassic and ...

  9. Ashfall Fossil Beds - Wikipedia

    en.wikipedia.org/wiki/Ashfall_Fossil_Beds

    The ash preserved the animals in three dimensions; not even the delicate bones of birds or the carapaces of turtles were crushed. Above the layer of ash, a stratum of more erosion-resistant sandstone has acted as "caprock" to preserve the strata beneath. Fossil of a Teleoceras in volcanic ash. Paleontologists working on the site