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  2. 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 ...

  3. Hawaii Center for Volcanology - Wikipedia

    en.wikipedia.org/wiki/Hawaii_Center_for_Volcanology

    The Hawaii Center for Volcanology was a cooperative effort between the School of Ocean and Earth Science and Technology at the University of Hawaiʻi at Mānoa, the Hawaiian Volcano Observatory of the United States Geological Survey, and the Center for the Study of Active Volcanoes at the University of Hawaii at

  4. 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.

  5. 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 ...

  6. Honolulu Volcanics - Wikipedia

    en.wikipedia.org/wiki/Honolulu_Volcanics

    Like other Hawaiian volcanoes Koʻolau is a shield volcano that grew through lava flows erupted from a rift system with a central caldera, although a large section of the volcano has sunk below sea level. This volcano constitutes the tholeiitic stage of Hawaiian volcanism, [70] and developed possibly during Miocene to Pleistocene time. [41]

  7. 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.

  8. 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.

  9. Wikipedia:WikiProject Volcanoes/Bibliography - Wikipedia

    en.wikipedia.org/wiki/Wikipedia:WikiProject...

    This page is a bibliography of useful books and other references for the purposes of article-writing. General reference. WorldCat. (the world's largest library catalog, with over 1 billion items in more than 10,000 libraries worldwide; see WorldCat).