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East Molokai was one of the seven principal volcanoes, along with West Molokai, Lānaʻi, West Maui, East Maui, Penguin Bank and Kahoʻolawe, that formerly constituted the island of Maui Nui. The highest point is the peak called Kamakou on the southern rim, at 21°6′23″N 156°52′5″W / 21.10639°N 156.86806°W / 21.10639 ...
It is part of the extinct East Molokai shield volcano, which comprises the east side of the island. [2] Kamakou is located within the 2,774-acre (11.23 km 2; 4.334 sq mi) Molokai Forest Reserve, [3] estimated to contain more than 250 rare native Hawaiian plants, many of which exist only in this part of the world. [4]
Today, East Molokai volcano, like the Koʻolau Range on Oʻahu, is what remains of the southern half of the original mountain. The northern half suffered a catastrophic collapse about 1.5 million years ago and now lies as a debris field scattered northward across the bottom of the Pacific Ocean. [8] What remains of the volcano on the island ...
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]
The northern half of the East Molokai Volcano on Molokai in Hawaii suffered a catastrophic collapse about 1.5 million years ago, generating a megatsunami, and now lies as a debris field scattered northward across the ocean bottom, [35] while what remains on the island are the highest sea cliffs in the world. [36]
Olokui is the second highest peak on the island of Molokai, surpassed by only Kamakou. At 4,602 feet (1,403 m), it marks the divide between the Pelekunu and Wailau valleys. It is part of the extinct East Molokai shield volcano, which comprises the east side of the island. [2]
The six islands of Oahu, Kauai, Maui, Molokai, Lanai, and the Big Island welcome over 10 million people a year. Until you can visit the Aloha State, you can daydream with these jaw-dropping ...
A collapse occurred around (uncertain) years ago on the eastern/north eastern flank of the volcano and lava flows from East Molokai had filled in the open space, connecting the two volcanoes above surface (also known as the Molokai Saddle). The cliffs of the eastern side of West Molokai is the only remaining evidence for this land slip. Keep ...
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