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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]
After hundreds of thousands of years of dormancy, Koʻolau volcano began to erupt again. Some thirty eruptions over the past 500,000 years or so have created many of the landmarks around eastern Oʻahu, such as Diamond Head, Koko Head (Hanauma Bay), Koko Crater, Punchbowl Crater, Tantalus, and Āliapaʻakai, and are collectively known as the Honolulu Volcanic Series, or simply Honolulu ...
HONOLULU — The ongoing eruption at Hawaii’s Kilaeua volcano became more active Saturday evening. ... the HVO says all current and recent activity is still within Hawaii Volcanoes National Park ...
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. Consequently, there is no clear limitation on what could or should be included here as almost any geological feature found on the island originated from one of these two ...