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. 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 Laguna Colorada, Bolivia Loloru, Bougainville, Papua New Guinea Cerro Panizos, Bolivia Purico Complex, Chile Rabaul Volcano, New Britain, Papua New Guinea Sacabaya, Bolivia Mount Shiribetsu, Hokkaido, Japan Tata Sabaya, Bolivia Taal Volcano, Philippines Hofsjökull, Iceland - initially built from basaltic lava, but may have transitioned to highly viscous lava.
See also Stratovolcano – Type of conical volcano composed of layers of lava and tephra Pyroclastic fall – Deposit of material ejected from a volcanic eruption Categories:
Pyroclastic cones
References
External links Pyroclastic Shield Volcano - John Seach


