shield volcano wikipedia - EAS
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A shield volcano is a type of volcano named for its low profile, resembling a warrior's 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. Repeated eruptions result in
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See moreThe term 'shield volcano' is taken from the German term Schildvulkan, coined by the Austrian geologist Eduard Suess in 1888 and which had been calqued into English by 1910.
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See moreShield volcanoes are found worldwide. They can form over hotspots (points where magma from below the surface wells up), such as the Hawaiian–Emperor seamount chain and the Galápagos Islands, or over more conventional rift zones, such as the
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Shield volcanoes are distinguished from the three other major volcanic types—stratovolcanoes...
See moreWikipedia text under CC-BY-SA license - https://en.wikipedia.org › wiki › List_of_shield_volcanoes
• Heart Peaks
• Itcha Range (British Columbia, Canada)
• Lava plateau of Level Mountain (British Columbia, Canada)
• Haleakalā (Maui)Wikipedia · Text under CC-BY-SA license- Estimated Reading Time: 2 mins
- https://simple.wikipedia.org › wiki › Shield_volcano
A shield volcano is a large volcano with shallowly-sloping sides. The name derives from a translation of "Skjaldbreiður", an Icelandic shield volcano whose name means "broad shield," from its resemblance to a warrior's shield. Shield volcanoes are …
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- https://en.wikipedia.org › wiki › Category:Shield_volcanoes
List of shield volcanoes A Arsia Mons B Mount Boennighausen D Deception Island F Mount Frakes H Hallett Peninsula I Indian Heaven K Mount Kirishima Kollóttadyngja L Lunar dome M Misema Caldera P Pavonis Mons Pico do Príncipe Pyroclastic shield R Renpet Mons Rotuma Mons Rümker S Sif Mons Syrtis Major Planum T Tamu Massif Theia Mons U Ua Huka
- https://en.wikipedia.org › wiki › Category:Miocene_shield_volcanoes
Shield volcanoes that were active in the Miocene epoch (approximately 23,030,000 years to 5,330,000 million years ago) during the Neogene Period of the Cenozoic Era. Subcategories. This category has only the following subcategory. T. Tweed Volcano (6 P) Pages in category "Miocene shield volcanoes" ...
- https://en.wikipedia.org › wiki › Category:Holocene_shield_volcanoes
Shield volcanoes active during the Holocene Epoch (approximately 11,700 years ago to the present day), in the Quaternary Period of the Cenozoic Era. Subcategories. This category has only the following subcategory. K. Kīlauea (29 P) This page was last edited on 21 ...
- https://en.wikipedia.org › wiki › Kīlauea
Located along the southeastern shore of the Big Island of Hawaiʻi, the volcano is between 210,000 and 280,000 years old and emerged above sea level about 100,000 years ago. Historically, it is the most active of the five volcanoes that together form Hawaii island.
- https://en.wikipedia.org › wiki › Pyroclastic_shield
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.
- https://en.wikipedia.org › wiki › Volcano
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface.. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater.For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has …
What Type Of Volcano Was Mt St Helens - BikeHike
va.youramys.com › what-type-of-volcano-was-mt-st-helensStratovolcano – Wikipedia , a steep-sided volcano located in the Pacific Northwest region of the United States in the state of Washington. Sitting about 97 miles south of Seattle and 52 miles northeast of Portland, Oregon, Mt. Is Mt St Helens a shield volcano? Mount St.
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