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  2. Hawaiʻi Volcanoes National Park - Wikipedia

    en.wikipedia.org/wiki/Hawaiʻi_Volcanoes_National...

    Hawaiʻi Volcanoes National Park is a national park of the United States located in Hawaii on the island of Hawaii. The park encompasses two active volcanoes: Kīlauea , one of the world's most active volcanoes, and Mauna Loa , the world's largest shield volcano.

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

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

    The island of Hawaiʻi comprises five volcanoes, of which two (Kilauea and Mauna Loa) are still active. Kamaʻehuakanaloa Seamount (formerly Lōʻihi) continues to grow offshore, and is the only known volcano in the chain in the submarine pre-shield stage .

  4. What travelers to Hawaii can expect following Mauna Loa's ...

    www.aol.com/travelers-hawaii-expect-following...

    The largest active volcano in the world, Mauna Loa, is erupting after 38 years. This is how the eruption might affect travel plans to Hawaii.

  5. 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]

  6. Kamaʻehuakanaloa Seamount - Wikipedia

    en.wikipedia.org/wiki/Kamaʻehuakanaloa_Seamount

    In the preshield stage, Hawaiian volcanoes have steeper sides and a lower level of activity, producing an alkali basalt lava. [17] [18] Continued volcanism is expected to eventually give birth to an island at Kamaʻehuakanaloa. It experiences frequent landslides; the growth of the volcano has destabilized its slopes, and extensive areas of ...

  7. Diamond Head, Hawaii - Wikipedia

    en.wikipedia.org/wiki/Diamond_Head,_Hawaii

    View from the top of Diamond Head, 2015. Diamond Head is a volcanic tuff cone on the Hawaiian island of Oʻahu.It is known to Hawaiians as Lēʻahi (pronounced [leːˈʔɐhi]), which is most likely derived from lae (browridge, promontory) plus ʻahi (tuna) because the shape of the ridgeline resembles the shape of a tuna's dorsal fin. [3]

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