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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]
Schiedea adamantis, commonly known as Diamond Head schiedea, is a species of flowering plant in the family Caryophyllaceae, that is endemic to the island of Oʻahu in Hawaii. It inhabits low shrublands on steep slopes along the northwest rim of Diamond Head Crater .
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 ...
Print/export Download as PDF; Printable version; ... Pages in category "Diamond Head Classic" The following 16 pages are in this category, out of 16 total.
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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.
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