Nintoku Seamount

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

The seamount is also known as the "Nintoku 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 Nintoku of Japan.

The last eruption from Nintoku seamount was 65 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," Archived 2011-10-08 at the Wayback Machine 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, "Nintoku Guyot"; retrieved 2012-6-9.
↑ VolcanoLive, Nintoku Seamount

Other websites

Seamount Biogeosciences Network, database

41°4.80′N 170°34.20′E / 41.08000°N 170.57000°E / 41.08000; 170.57000

This short article about a place or feature can be made longer. You can help Wikipedia by adding to it.

[1] Tarduno, John A. et al. "The Emperor Seamounts: southward motion of the Hawaiian hotspot plume in Earth's mantle," Archived 2011-10-08 at the Wayback Machine 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, "Nintoku Guyot"; retrieved 2012-6-9.

[5] VolcanoLive, Nintoku Seamount

[1]

[2]

[3]

[4]

[5]