Ads
related to: history of diamond head volcano in oahu hawaii tourvisitacity.com has been visited by 100K+ users in the past month
Search results
Results from the WOW.Com Content Network
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 ]
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] Inland from Diamond Head lie the Kaimukī and Mauʻumae cones, [51] which appear to come from a shared fissure. [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 ...
Fifty years later, Congress authorized a small appropriation to establish a national cemetery in Honolulu with two provisions: that the location be acceptable to the War Department, and that the site would be donated rather than purchased. In 1943, the governor of Hawaii offered the Punchbowl for a national cemetery. The $50,000 appropriation ...
Fort Ruger is a fort on the island of Oʻahu that served as the first military reservation in the Territory of Hawaii.Named after Civil War General Thomas H. Ruger and built in and around Diamond Head Crater, the fort was established by the United States for the purpose of defending the harbor of its newly annexed territory. [2]
The sound of bustling Honolulu has faded away to simply birds melodically chirping. Even talking loudly feels wrong. This place easily lives up to its name of " to make a place of peace " in Hawaiian.
The cinder cone formed after the demise of Koʻolau Volcano, during a time of rejuvenated-stage volcanism in southeastern Oʻahu that also formed Punchbowl Crater, Diamond Head and Koko Head as part of the Honolulu Volcanics. Tantalus overlooks the modern city of Honolulu, which is built on top of Tantalus cinders.
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.
Ads
related to: history of diamond head volcano in oahu hawaii tourvisitacity.com has been visited by 100K+ users in the past month