List of volcanoes in the Hawaiian–Emperor seamount chain
The Hawaiian–Emperor seamount chain is a series of volcanoes and seamounts extending about 6,200 kilometres (3,900 mi) across the Pacific Ocean. The chain has been produced by the movement of the ocean crust over the Hawaiʻi hotspot, an upwelling of hot rock from the Earth's mantle. As the oceanic crust moves the volcanoes farther away from their source of magma, their eruptions become less frequent and less powerful until they eventually cease to erupt altogether. At that point, erosion of the volcano and subsidence of the seafloor cause the volcano to gradually diminish. As the volcano sinks and erodes, it first becomes an atoll island and then an atoll. Further subsidence causes the volcano to sink below the sea surface, becoming a seamount and/or a guyot. This list documents the most s
Daikakuji Guyot
Gardner Pinnacles
Hawaiian–Emperor seamount chain
Jingū Seamount
Kaena Ridge
Kammu Seamount
Kaʻula
Kimmei Seamount
Kohala (mountain)
Koko Guyot
Kīlauea
Kīlauea Caldera
Lisianski Island
Maro Reef
Necker Island (Hawaii)
Nihoa
Nintoku Seamount
Ojin Seamount
Yomei Seamount
Yuryaku Seamount
Abbott SeamountColahan SeamountEvolution of Hawaiian volcanoesHancock SeamountIndex of Hawaii-related articlesKalākaua's 1881 world tourList of volcanoes in the Hawaiian-Emperor Seamount chainList of volcanoes in the Hawaiian-Emperor seamount chainList of volcanoes in the Hawaiian - Emperor seamount chainList of volcanoes in the Hawaiian – Emperor seamount chainList of volcanoes in the Pacific OceanLists of volcanoesLōʻihi SeamountMauna_LoaOutline of oceanographyRing of FireTypes of volcanic eruptions
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List of volcanoes in the Hawaiian–Emperor seamount chain
The Hawaiian–Emperor seamount chain is a series of volcanoes and seamounts extending about 6,200 kilometres (3,900 mi) across the Pacific Ocean. The chain has been produced by the movement of the ocean crust over the Hawaiʻi hotspot, an upwelling of hot rock from the Earth's mantle. As the oceanic crust moves the volcanoes farther away from their source of magma, their eruptions become less frequent and less powerful until they eventually cease to erupt altogether. At that point, erosion of the volcano and subsidence of the seafloor cause the volcano to gradually diminish. As the volcano sinks and erodes, it first becomes an atoll island and then an atoll. Further subsidence causes the volcano to sink below the sea surface, becoming a seamount and/or a guyot. This list documents the most s
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The Hawaiian–Emperor seamount ...... zone at the border of Russia.
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The Hawaiian–Emperor seamount ...... This list documents the most s
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List of volcanoes in the Hawaiian–Emperor seamount chain
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