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  2. Kohala (mountain) - Wikipedia

    en.wikipedia.org/wiki/Kohala_(mountain)

    Kohala is 606 km 2 (234 sq mi) in area and 14,000 km 3 (3,400 cu mi) in volume, and thus constitutes just under 6% of the island of Hawaii. [1] Kohala is a shield volcano cut by multiple deep gorges, which are the product of thousands of years of erosion. Unlike the typical symmetry of other Hawaiian volcanoes, Kohala is shaped like a foot.

  3. List of volcanoes in the Hawaiian–Emperor seamount chain

    en.wikipedia.org/wiki/List_of_volcanoes_in_the...

    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]

  4. Lava-flow hazard zones - Wikipedia

    en.wikipedia.org/wiki/Lava-flow_hazard_zones

    Zone 7 - Younger part of Mauna Kea volcano. 20% of this area was covered by lava in the past 10,000 years. Zone 8 - Remaining part of Mauna Kea. Only a few percents of this area has been covered by lava in the past 10,000 years. Zone 9 - Kohala Volcano, which last erupted over 60,000 years ago. Lava Flow Hazard map of Haleakala.

  5. Evolution of Hawaiian volcanoes - Wikipedia

    en.wikipedia.org/.../Evolution_of_Hawaiian_volcanoes

    The evolution of Hawaiian volcanoes occurs in several stages of growth and decline. The fifteen volcanoes that make up the eight principal islands of Hawaii are the youngest in a chain of more than 129 volcanoes that stretch 5,800 kilometers (3,600 mi) across the North Pacific Ocean, called the Hawaiian–Emperor seamount chain. [1]

  6. Koʻolau Range - Wikipedia

    en.wikipedia.org/wiki/Koʻolau_Range

    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 ...

  7. Kīlauea - Wikipedia

    en.wikipedia.org/wiki/Kīlauea

    The oldest volcano on the island, Kohala, is more than a million years old, [17] while Kīlauea, the youngest, is between 300,000 and 600,000 years of age. [16] Kamaʻehuakanaloa (the ruddy, reddish child of Kanaloa, [18] formerly Lōʻihi), on the island's flank, is younger and has yet to breach the surface. [19]

  8. Kohala, Hawaii - Wikipedia

    en.wikipedia.org/wiki/Kohala,_Hawaii

    The Kohala Mountain Road (250) provides a link between Waimea and the Kohala CDP's of Halaʻula, Hāwī, and Kapaʻau. Spencer Beach Park on the South Kohala Coast. Kohala has two small airports. Upolu Airport is on Upolu Point at the northern tip of the island. [9] Waimea-Kohala Airport is south of the town of Waimea, Hawaii County, Hawaii. [10]

  9. ʻUpolu Point - Wikipedia

    en.wikipedia.org/wiki/ʻUpolu_Point

    ʻUpolu Point is the most northern point on the island of Hawaiʻi in the Hawaiian Islands. [1] It is an extruding landform created by cooled lava from an old eruption from Kohala volcano.

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