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A shield volcano is a type of volcano named for its low profile, resembling a shield lying on the ground. It is formed by the eruption of highly fluid (low viscosity) lava, which travels farther and forms thinner flows than the more viscous lava erupted from a stratovolcano.
This list of shield volcanoes includes active, dormant and extinct shield volcanoes.Shield volcanoes are one of the three types [specify] of volcanoes. They have a short cone shape, and have basaltic lava which means the lava has low viscosity (viscosity is a measure of the ability for a liquid to flow)
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Mount Giluwe is the second highest mountain in Papua New Guinea at 4,367 metres (14,327 ft) (Mount Wilhelm being the highest), and the fifth highest peak on the island of New Guinea. It is located in the Southern Highlands province and is an old shield volcano with vast alpine grasslands. Ancient volcanic plugs form its two summits, with the ...
Mountain type. Pyroclastic shield, stratovolcano [1] Last eruption. 1050 BCE (?) Loloru is a pyroclastic shield volcano located in the southern region of Bougainville Island, within the Autonomous Region of Bougainville of northeastern Papua New Guinea. The volcano's summit consists of two nested calderas, with an andesitic lava dome.
Category:Shield volcanoes. Wikimedia Commons has media related to Shield volcanoes. The main article for this category is Shield volcano. Map all coordinates using OpenStreetMap. Download coordinates as: KML. GPX (all coordinates) GPX (primary coordinates) GPX (secondary coordinates)
S. Shield volcanoes of Papua New Guinea (4 P) Stratovolcanoes of Papua New Guinea (32 P)
Mount Warning is the central volcanic remnant of an ancient shield volcano, the Tweed Volcano, which would have been about 1,900 m (6,200 ft) above sea level or just under twice the height of the current mountain. [5][6] This volcano last erupted around 23 million years ago. [7] As the mountain's central vent cooled it shrank, forming a ...