Yūryaku Seamount - Simple English Wikipedia, the free encyclopedia

Yūryaku Seamount (雄略海山) is an underwater volcano (seamount) of the Hawaiian–Emperor seamount chain in the Pacific Ocean.^[1] Yūryaku is an extinct volcano.^[2]

The seamount is also known as the "Yūryaku Guyot" because it has a flat top.^[3] This undersea geologic feature is also called a "guyot" or "tablemount".^[4]

This seabed mountain is named after Emperor Yūryaku of Japan.

The last eruption from Yūryaku seamount was 43 million years ago.^[5]

Related pages

References

↑ Tarduno, John A. et al. "The Emperor Seamounts: southward motion of the Hawaiian hotspot plume in Earth's mantle," Science, 22 August 2003, pp. 1064-1069 DOI:10.1126/science.1086442; retrieved 2012-6-14.
↑ Monterey Bay Aquarium Research Institute, "Life-cycle of Hawaiian hot spot volcanoes" Archived 2013-04-14 at the Wayback Machine; retrieved 2012-6-14.
↑ Guyots are flat-topped because they were once above sea level, and were worn down by the sea.
↑ Geographic.org, "Yuryaku Guyot"; retrieved 2012-6-9.
↑ VolcanoLive, Yuryaku Seamount

Other websites

Seamount Biogeosciences Network, database

32°40.20′N 172°16.2′E / 32.67000°N 172.2700°E / 32.67000; 172.2700

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[1] Tarduno, John A. et al. "The Emperor Seamounts: southward motion of the Hawaiian hotspot plume in Earth's mantle," Science, 22 August 2003, pp. 1064-1069 DOI:10.1126/science.1086442; retrieved 2012-6-14.

[2] Monterey Bay Aquarium Research Institute, "Life-cycle of Hawaiian hot spot volcanoes" Archived 2013-04-14 at the Wayback Machine; retrieved 2012-6-14.

[3] Guyots are flat-topped because they were once above sea level, and were worn down by the sea.

[4] Geographic.org, "Yuryaku Guyot"; retrieved 2012-6-9.

[5] VolcanoLive, Yuryaku Seamount

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