- Pyroclastic rock
Pyroclastic rocks or "pyroclastics" (derived from the Greek "πῦρ", meaning fire, and "κλαστός", meaning broken) are
clasticrocks composed solely or primarily of volcanicmaterials. Where the volcanic material has been transported and reworked through mechanical action, such as by wind or water, these rocks are termed "volcaniclastic". Commonly associated with explosive volcanic activity - such as Plinianor krakatoan eruption styles, or phreatomagmaticeruptions - pyroclastic deposits are commonly formed from airborne ash, lapilliand bombs or blocks ejected from the volcano itself, mixed in with shattered country rock.
Pyroclastic rocks may be composed of a large range of
clastsizes; from the largest agglomerates, to very fine ashes and tuffs. Pyroclasts of different sizes are classified as volcanic bombs, lapilliand volcanic ash. Ash is considered to be pyroclastic because it is a fine dust made up of volcanic rock. One of the most spectacular forms of pyroclastic deposit are the ignimbrites, deposits formed by the high-temperature gas and ash mix of a pyroclastic flowevent.
Three modes of transport can be distinguished:
pyroclastic flow, pyroclastic surge, and pyroclastic fall. During Plinian eruptions, pumiceand ash are formed when silicic magmais fragmented in the volcanic conduit, because of decompression and the growth of bubbles. Pyroclasts are then entrained in a buoyant eruption plume which can rise several kilometers into the air and cause aviation hazards. Particles falling from the eruption clouds form layers on the ground (this is pyroclastic fall or tephra). Pyroclastic density currents, which are referred to as 'flows' or 'surges' depending on particle concentration and the level turbulence, are sometimes called "glowing avalanches". The deposits of pumice-rich pyroclastic flows can be called ignimbrites.
A pyroclastic eruption entails spitting or "fountaining" lava, where the lava will be thrown into the air along with ash, pyroclastic materials, and other volcanic byproducts. Hawaiian eruptions such as those at
Kilaueacan eject clots of magma suspended into gas; this is called a 'fire fountain'. The magma clots, if hot enough may coalesce upon landing to form a lava flow.
Pyroclastic deposits consist of pyroclasts which are not cemented together. Pyroclastic rocks (
tuff) are pyroclastic deposits which have been lithified.
*Blatt, Harvey and Robert J. Tracy (1996) "Petrology: Igneous, Sedimentary, and Metamorphic", W.H. Freeman & Company; 2nd ed., pp. 26-29; ISBN 0-7167-2438-3
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