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  2. Hawaii hotspot - Wikipedia

    en.wikipedia.org/wiki/Hawaii_hotspot

    The Hawaiʻi hotspot is a volcanic hotspot located near the namesake Hawaiian Islands, in the northern Pacific Ocean.One of the best known and intensively studied hotspots in the world, [1] [2] the Hawaii plume is responsible for the creation of the Hawaiian–Emperor seamount chain, a 6,200-kilometer (3,900 mi) mostly undersea volcanic mountain range.

  3. Hawaiian Volcano Observatory - Wikipedia

    en.wikipedia.org/wiki/Hawaiian_Volcano_Observatory

    The Hawaiian Volcano Observatory (HVO) is an agency of the United States Geological Survey (USGS) and one of five volcano observatories operating under the USGS Volcano Hazards Program. Based in Hilo, Hawaii , the observatory monitors six Hawaiian volcanoes: Kīlauea , Mauna Loa , Kamaʻehuakanaloa (formerly Lōʻihi), Hualālai , Mauna Kea ...

  4. Hotspot (geology) - Wikipedia

    en.wikipedia.org/wiki/Hotspot_(geology)

    Over millions of years, the Pacific plate has moved over the Hawaii hotspot, creating a trail of underwater mountains that stretches across the Pacific. Kilauea is the most active shield volcano in the world. The volcano erupted from 1983 to 2018 and is part of the Hawaiian–Emperor seamount chain. Mauna Loa is a large shield volcano.

  5. Kamaʻehuakanaloa Seamount - Wikipedia

    en.wikipedia.org/wiki/Kamaʻehuakanaloa_Seamount

    The name Kamaʻehuakanaloa is a Hawaiian language word for "glowing child of Kanaloa", the god of the ocean. [10] This name was found in two Hawaiian mele from the 19th and early twentieth centuries based on research at the Bishop Museum and was assigned by the Hawaiʻi Board on Geographic Names in 2021 and adopted by the U.S. Geological Survey.

  6. List of volcanoes in the Hawaiian–Emperor seamount chain

    en.wikipedia.org/wiki/List_of_volcanoes_in_the...

    The Emperor and Hawaiian chains are separated by a large L-shaped bend that causes the orientations of the chains to differ by about 60 degrees. This bend was long attributed to a relatively sudden change in the direction of plate motion, but research conducted in 2003 suggests that it was the movement of the hotspot itself that caused the bend ...

  7. Hawaiian–Emperor seamount chain - Wikipedia

    en.wikipedia.org/wiki/Hawaiian–Emperor_seamount...

    The Hawaiian–Emperor seamount chain is a mostly undersea mountain range in the Pacific Ocean that reaches above sea level in Hawaii.It is composed of the Hawaiian ridge, consisting of the islands of the Hawaiian chain northwest to Kure Atoll, and the Emperor Seamounts: together they form a vast underwater mountain region of islands and intervening seamounts, atolls, shallows, banks and reefs ...

  8. United States Geological Survey - Wikipedia

    en.wikipedia.org/wiki/United_States_Geological...

    U.S. Geological Survey National Center in Reston, Virginia Earthquake animations from May 16 to May 22, 2010 Earthquakes around the world from April 23 to May 23, 2010. Since 2012, the USGS science focus has been directed at topical "Mission Areas" [8] that have continued to evolve. Further organizational structure includes headquarters ...

  9. Evolution of Hawaiian volcanoes - Wikipedia

    en.wikipedia.org/wiki/Evolution_of_Hawaiian...

    The evolution of Hawaiian volcanoes occurs in several stages of growth and decline. The fifteen volcanoes that make up the eight principal islands of Hawaii are the youngest in a chain of more than 129 volcanoes that stretch 5,800 kilometers (3,600 mi) across the North Pacific Ocean , called the Hawaiian–Emperor seamount chain . [ 1 ]