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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 ]
[48] [49] This 15 kilometres (9.3 mi) long rift includes at least 12 separate volcanic vents [25] and its vents appear to have formed in a single eruption. [50] Diamond Head is a 1,700-metre (5,600 ft) (rim-to-rim) wide [40] typical tuff cone with a wide and not overly deep crater that forms a prominent promontory east of Honolulu. [38]
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 ...
The crater was formed some 75,000 to 100,000 years ago during the secondary activity of the Honolulu ... Diamond Head, Punchbowl Crater and Honolulu from Na Pueo park.
Koko Crater is a part of the Honolulu Volcanics, which were craters that formed as vents of the Koʻolau Volcano during its rejuvenation stage. [1] Other notable landmarks within the Honolulu Volcanics include nearby Hanauma Bay and the well-known Diamond Head crater.
Oahu rose above the sea during the Pliocene period 4 million years ago when volcanoes erupted and formed the peaks of two shield volcanoes. Then a period of extensive erosion followed, leaving the Wai‘anae and the young Ko‘olau Range as dormant volcanic ranges from remnants of volcanism.
In November, the "Exposure of a Dream" home video was released. [78] In 1993, Mustaine guested on a new album by one of the bands who had influenced his own sound: Diamond Head, and also began a U.S. tour with Stone Temple Pilots as their opening act.
Aerial view of Hanauma Bay. Hanauma (/ ˌ h ɑː n ə ˈ uː m ə /; Hawaiian: [həˈnɔumə]) [1] is a marine embayment formed within a tuff ring and located along the southeast coast of the Island of Oʻahu in the Hawaii Kai neighborhood of East Honolulu, in the Hawaiian Islands.