Pyroclastic shield

Emi Koussi seen from International Space Station

In volcanology, a pyroclastic shield or ignimbrite shield is an uncommon type of shield volcano. Unlike most shield volcanoes, pyroclastic shields are formed mostly of pyroclastic and highly explosive eruptions rather than relatively fluid basaltic lava issuing from vents or fissures on the surface of the volcano.^[1] They typically display low-angle flank slopes and often have a central caldera caused by large eruptions. Lava is commonly extruded after explosive activity has ended. The paucity of associated Plinian fall deposits indicates that pyroclastic shields are characterized by low Plinian columns.

Pyroclastic shields are commonly known to form in the Central Andes of South America, as well as in Melanesia (the island of Bougainville alone has two). There are also pyroclastic shields in Africa, such as Emi Koussi in Chad.

Examples

• Ambrym, Vanuatu
• Apoyeque, Nicaragua
• Masaya, Nicaragua
• Billy Mitchell, Bougainville, Papua New Guinea
• Emi Koussi, Chad
• Loloru, Bougainville, Papua New Guinea
• Purico Complex, Chile
• Rabaul Volcano, New Britain, Papua New Guinea
• Sacabaya, Bolivia
• Tata Sabaya, Bolivia

See also

• Pyroclastic cones

References

External links

• Pyroclastic Shield Volcano - John Seach

Volcanoes
Volcano types	Caldera Cinder cone Complex volcano Cryovolcano Fissure vent Lava cone Lava dome Maar Mud volcano Parasitic cone Pyroclastic cone Pyroclastic shield Rootless cone Shield volcano Somma volcano Stratovolcano Subglacial volcano Submarine volcano Supervolcano Volcanic cone Volcanic field (polygenetic · monogenetic)
Volcanic rocks	Volcanic rock Agglomerate Andesite Basalt Basaltic andesite Benmoreite Blairmorite Dacite Felsite Komatiite Latite Leucitite Nephelinite Obsidian Phonolite Phonotephrite Rhyodacite Rhyolite Tephriphonolite Trachyte Trachyandesite Trachybasalt Tuff
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