From Wikipedia, the free encyclopedia
This seabed mountain is named after Empress Jingū of Japan.
The last eruption from Jingū seamount was 55 million years ago.
Related pages[change | change source]
References[change | change source]
- 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"; retrieved 2012-6-14.
- Guyots are flat-topped because they were once above sea level, and were worn down by the sea.
- Geographic.org, "Jingū Guyot"; retrieved 2012-6-10.
- VolcanoLive, Jingū Seamount