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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 ...
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 ]
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]
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 ...
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 Hawaiian–Emperor seamount chain is a mostly undersea mountain range in the Pacific Ocean that reaches above sea level in Hawaii.It is composed of the Hawaiian ridge, consisting of the islands of the Hawaiian chain northwest to Kure Atoll, and the Emperor Seamounts: together they form a vast underwater mountain region of islands and intervening seamounts, atolls, shallows, banks and reefs ...
Wailau valley was formed by stream erosion of the Wailau River, after the massive collapse of the East Molokai Volcano enabled streams from this part of the island to flow north. Numerous major landmarks dominate the area, such as Olokui , Molokai 's second highest peak, and the Kukuinui Ridge.