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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]
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
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]
It is part of the extinct East Molokai shield volcano, which comprises the east side of the island. [2] On the west it is bounded by the Kapapa Pali, and on the south and east sides, there is a steep drop down to the Pulena stream and Wailau River, respectively. The north side of the mountain was destroyed in a catastrophic collapse along with ...
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]
Molokai, Hawaii: East Molokai Volcano: Landslide: One-third of the East Molokai volcano collapsed into the Pacific Ocean, generating a tsunami with an estimated local height of 2,000 feet (610 m). The wave traveled as far as California and Mexico. [17] [18] [19] ≈220,000–170,000 BCE Tenerife, Canary Islands: Mount Teide: Eruption and landslide
Kahoʻolawe is an extinct shield volcano, which formed during the Pleistocene epoch. It was once connected to the island of Maui Nui before splitting off about 300,000 years ago. Most of the island is covered by basaltic lava flows. A caldera is located in the eastern part of the island. The last confirmed volcanic activity on the island ...