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Template: Shield volcano diagram. 1 language. Português; ... Download as PDF; Printable version; ... Diagram of the common structural features of a shield volcano
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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)
Selected geological features near the Skjaldbreiður shield volcano.(red outline). Light violet shading shows the current surface area of the Skjaldbreiður lava flows. Shading also shows: calderas, central volcanoes and fissure swarms, subglacial terrain above 1,100 m (3,600 ft), and seismically active areas. Clicking on the image enlarges to ...
Mount Elgon is an extinct shield volcano on the border of Uganda and Kenya, [5] north of Kisumu and west of Kitale. The mountain's highest point, named "Wagagai", is located entirely within Uganda. The mountain's highest point, named "Wagagai", is located entirely within Uganda.
Theia Mons is a large highland shield volcano on the planet Venus.Located near the center of Beta Regio, a large region of recent volcanic uplift due to a currently active mantle plume, [3] Theia Mons is situated at the junction of three branches of Devana Chasma, an extensive rift system. [4]
Mount Wrangell, (Ahtna: K’ełt’aeni, or K’ełedi when erupting) [3] is a massive shield volcano located in Wrangell-St. Elias National Park and Preserve in southeastern Alaska, United States. The shield rises over 12,000 feet (3,700 m) above the Copper River to its southwest.