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The Honolulu Volcanics are a series of volcanoes in the southeastern sector of Oʻahu [2] and includes dikes, lava flows, spatter cones, [3] tephra deposits, [4] tuff cones, [3] and mesas where the surrounding terrain has been eroded away. [5]
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]
The seamount is a submarine volcano, southwest of Molokaʻi. The submarine volcano used to be part of Maui Nui, a prehistoric island made from seven shield volcanoes. Koʻolau Range: Oʻahu <32,000 BP (possibly dormant) [n 3: 2.7 million [28]
Volcanoes of O‘ahu.This category includes various named volcanic vents and other features found on the Island of O‘ahu. The Island was formed by only two volcanoes: Wai‘anae and Ko‘olau.
Like all Hawaiian volcanoes, Kīlauea was formed as the Pacific tectonic plate moved over the Hawaiian hotspot in the Earth's underlying mantle. [12] Hawaii island volcanoes are the most recent evidence of this process that, over 70 million years, has produced the 6,000 km (3,700 mi)-long Hawaiian–Emperor seamount chain. [13]
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.
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