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File:Icelandic tephra.JPG

Tephra is fragmental material produced by a volcanic eruption regardless of composition, fragment size or emplacement mechanism.[1]

Volcanologists also refer to airborne fragments as pyroclasts. Once clasts have fallen to the ground they remain as tephra unless hot enough to fuse together into pyroclastic rock or tuff.
File:04Sep2007 Etna from SE Crater.jpg

OverviewEdit

File:BishopTuff.jpg

The distribution of tephra following an eruption usually involves the largest boulders falling to the ground quickest and therefore closest to the vent, while smaller fragments travel further — ash can often travel for thousands of miles, even circumglobal, as it can stay in the stratosphere for days to weeks following an eruption. When large amounts of tephra accumulate in the atmosphere from massive volcanic eruptions (or from a multitude of smaller eruptions occurring simultaneously), they can reflect light and heat from the sun back through the atmosphere, in some cases causing the temperature to drop, resulting in a temporary, "volcanic winter", climate change. Tephra mixed in with precipitation can also be acidic and cause acid rain and snowfall.

ClassificationEdit

Tephra fragments are classified by size:
File:Volcanic breccia in Jackson Hole.JPG
  • Ash – particles smaller than 2 mm (0.08 inches) in diameter,
  • Lapilli or volcanic cinders – between 2 and 64 mm (0.08 and 2.5 inches) in diameter,
  • Volcanic bombs or volcanic blocks – larger than 64 mm (2.5 inches) in diameter.

The words "tephra" and "pyroclast" both derive from Greek. Tephra means "ash". Pyro means "fire" and klastos means "broken"; thus pyroclasts carry the connotation of "broken by fire".

The use of tephra layers, which bear their own unique chemistry and character, as temporal marker horizons in archaeological and geological sites is known as tephrochronology.

NotesEdit

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External links Edit

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pl:Materiał piroklastyczny sv:Pyroklastiskt material


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