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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. [2]
Maunalua Bay is a bay in the southeast of Honolulu, the capital of Hawaiʻi. The bay extends about 6.3 miles (10.1 kilometers) from the southern tip of Diamond Head , the Black Point , also called Kūpikipikiʻō , in the west to Portlock Point, also known as Kawaihoa Point , to the east.
Hanauma Bay, Koko Crater and Hawaii Kai. Koko Head is the headland that defines the eastern side of Maunalua Bay along the southeastern side of the Island of Oahu in Hawaii.On its western slope is the community of Portlock, a part of Hawaiʻi Kai.
Hanauma Bay close to Kalanianaʻole Highway is located 13 kilometres (8.1 mi) east of Honolulu [41] and is a 0.4 by 0.8 kilometres (0.25 mi × 0.50 mi) large, 18 metres (59 ft) deep [42] compound crater [43] /tuff cone [44] with several associated dykes and lava flows-[45] It was breached by the sea [44] and coral reefs grow within it. [46]
HAW-1 (Hawaii No. 1) was the first submarine telephone cable laid between Hawaii and the mainland United States. HAW-1 was laid in 1957, and consisted of two cables, each transmitting in one direction over 36 channels, with an individual length of 2,625 Nmi (4,862 km). The cable spans between Hanauma Bay, Oahu, Hawaii and Point Arena, California.
Aerial view of Maunalua (Hawaii Kai) and Koko Head Location of Maunalua (Hawaiʻi Kai), Hawaiʻi Hawaiʻi Kai Hawaiʻi Kai at Sunrise. Hawaiʻi Kai, also known as Maunalua or Koko Marina, is a largely residential area located in the City & County of Honolulu, in the East Honolulu CDP, on the island of Oʻahu. Hawaiʻi Kai is the largest of ...
Koko Crater, Hanauma Bay and other nearby tuff cones form the Koko Rift Zone, which marks the latest episode of volcanic activity on the island of Oahu. [1] Radiocarbon dating suggests that the latest eruption within the Koko Rift Zone occurred 7,000 years ago, [ 1 ] although the validity of these results are disputed. [ 2 ]
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 ...
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