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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 ...
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 ...
Molokai developed from two distinct shield volcanoes known as East Molokai and the much smaller West Molokai. The highest point is Kamakou [7] on East Molokai, at 4,970 ft (1,510 m). Today, East Molokai volcano, like the Koʻolau Range on Oʻahu, is what remains of the southern half of the
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]
The location of this volcano is the light red area immediately west of Moloka'i. Penguin Bank is the name given to a now-submerged shield volcano of the Hawaiian Islands. Its coral-capped remains lie immediately west of the island of Molokaʻi, under relatively shallow water (see bathymetric map at the right).
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 ...
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