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Download as PDF; Printable version; In other projects ... Diagram of the common structural features of a shield volcano
Template talk: Shield volcano diagram. ... Print/export Download as PDF; Printable version; In other projects ...
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)
There were three main shield volcanoes built on the seamount base (from north to south): the Northern Edifice, the Central Edifice and the Jandia Edifice. [75] [27] The central shield volcano is the oldest, built mostly from 22 to 18 Ma but with a later phase from 17.5 to 13 Ma. The southern shield volcano formed from 21 to 14 Ma.
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.
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.
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]