volcanic bombs - определение. Что такое volcanic bombs
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Что (кто) такое volcanic bombs - определение

VOLCANIC PROJECTILE, RECOGNISABLE LATER BY SHAPE
Volcanic bombs; Lava bombs; Lava bomb; Breadcrust bomb; Volcano bombs; Fusiform bomb; Spherical bomb
  • "Fusiform" type volcanic bomb. [[Capelinhos]] Volcano, [[Faial Island]], [[Azores]]
  • Lava bomb, ejected from the [[Kīlauea]] Volcano, [[Hawaii]] in 1983
  • "Almond" type volcanic bomb found in the Cinder Cones region of the [[Mojave National Preserve]]
  • Various volcanic bombs in the [[National Museum of Nature and Science]], [[Tokyo]], Japan
  • "Bread-crust" type volcanic bomb at [[Vulcania]], [[Puy-de-Dôme]], France
  • date=September 2019}}.

Volcanic bomb         
A volcanic bomb or lava bomb is a mass of partially molten rock (tephra) larger than 64 mm (2.5 inches) in diameter, formed when a volcano ejects viscous fragments of lava during an eruption.
Volcanic rock         
  • {{okina}}A{{okina}}ā next to pāhoehoe lava]] at the [[Craters of the Moon National Monument and Preserve]], Idaho, United States.
  • Le Maitre, R.W.}} (''ed.''); 1989: ''A classification of igneous rocks and glossary of terms'', Blackwell Science, Oxford.
  • A German example of [[latite]], a type of volcanic rock
  • Photomicrograph of a [[volcanic lithic fragment]] ([[sand grain]]); upper picture is plane-polarized light, bottom picture is cross-polarized light, scale box at left-center is 0.25 millimeter.
  • Vesicular olivine basalt from [[La Palma]] (green [[phenocrysts]] are [[olivine]]).
  • sp=us}} piece of [[pumice]] supported by a rolled U.S. $20 bill demonstrates its very low density.
  • A sample of rhyolite
  • Amsterdam Island]] in the Indian Ocean
  • Volcanic rocks, [[Porto Moniz]], [[Madeira]]
ROCK FORMED FROM LAVA ERUPTED FROM A VOLCANO
Volcanic Rock; Lava rock; Effusive rock; Volcanite; Igneous volcanic rock; Axiolitic; Volcanic rocks; Lava stone; Volcanics; Black volcanic rock; Subalkaline igneous rocks; Subalkaline volcanic rock; Alkaline volcanic rock; Peralkaline volcanic rock
Volcanic rock (often shortened to volcanics in scientific contexts) is a rock formed from lava erupted from a volcano. In other words, it differs from other igneous rock by being of volcanic origin.
Volcanic plug         
  • Volcanic plug near [[Rhumsiki]], [[Cameroon]].
  • [[Saint Michel d'Aiguilhe]] chapel, on top of a volcanic plug in [[Le Puy-en-Velay]], France.
  • [[Roque Bentayga]] from the town of [[Artenara]]
VOLCANIC OBJECT CREATED WHEN MAGMA HARDENS WITHIN A VENT ON AN ACTIVE VOLCANO
Volcanic Neck; Volcanic neck; Lava plug; Lava neck; Bysmalith; Volcanic plugs; Volcanic Plug; Volcanic necks; Basalt plug
A volcanic plug, also called a volcanic neck or lava neck, is a volcanic object created when magma hardens within a vent on an active volcano. When present, a plug can cause an extreme build-up of high gas pressure if rising volatile-charged magma is trapped beneath it, and this can sometimes lead to an explosive eruption.

Википедия

Volcanic bomb

A volcanic bomb or lava bomb is a mass of partially molten rock (tephra) larger than 64 mm (2.5 inches) in diameter, formed when a volcano ejects viscous fragments of lava during an eruption. Because volcanic bombs cool after they leave the volcano, they are extrusive igneous rocks. Volcanic bombs can be thrown many kilometres from an erupting vent, and often acquire aerodynamic shapes during their flight. Bombs can be extremely large; the 1935 eruption of Mount Asama in Japan expelled bombs measuring 5–6 m (16-20 ft) in diameter up to 600 m (2,000 ft) from the vent. Volcanic bombs are a significant volcanic hazard, and can cause severe injuries and death to people in an eruption zone. One such incident occurred at Galeras volcano in Colombia in 1993; six people near the summit were killed and several seriously injured by lava bombs when the volcano erupted unexpectedly. On July 16, 2018, 23 people were injured on a tour boat near the Kilauea volcano as a result of a basketball-sized lava bomb from the 2018 lower Puna eruption.

Volcanic bombs are known to occasionally explode from internal gas pressure as they cool, but in most cases, most of the damage they cause is from impact, or subsequent fire damage. Bomb explosions are most often observed in "bread-crust" type bombs.