I think you're relying on a single source for the name Wailau, a 2001 book on the volcanoes of all of the US and Canada. It is sponsored by the, Information about large Quaternary eruptions (VEI >= 4) is cataloged in the, EarthChem develops and maintains databases, software, and services that support the preservation, discovery, access and analysis of geochemical data, and facilitate their integration with the broad array of other available earth science parameters. The maps database originated over 30 years ago, but was only recently updated and connected to our main database. East Molokai is a shield volcano which makes up the eastern two-thirds of Mauna Loa volcano. It lies east of Oahu across the 25-mile wide Kaiwi Channel and north of Lnai, separated from it by the Kalohi Channel. 1989). This compilation of synonyms and subsidiary features may not be comprehensive. Kamakou is the highest peak on the island of Molokai, at 4,961 feet (1,512 m). In fact, the chain continues beyond Kure as a series of now- submerged former islands known as seamounts. A shield volcano Geology. There is no Emissions History data available for East Molokai. Further reading Xu, Guangping, et al. [2][3] The Pppae bog is just below the rim. The East Molokai has a width of 70 km (43 mi) and a length of 150 km (93 mi). Sequences of older tholeiitic to younger alkalic basalt that erupted as this volcano evolved from the shield to postshield stage of volcanism Kalaupapa Pali. Select from premium East Molokai Volcano of the highest quality. The shield of East Molokai volcano, at greater than 1.5 Ma, is the oldest volcano on the Kea trend. Vancouver, BC Canada V6T 1Z4. The Global Volcanism Program has no photographs available for East Molokai. In some cases additional feature type, elevation, or location details are provided. [4], The northern flank of the volcano has been truncated by enormous cliffs rising 900m (3,000ft) from the sea. It is overlapped by the West Molokai, Lanai and Haleakal shield volcanoes. Its shield formation began two million years ago and ended 1.5million years ago whereas its postshield eruptions occurred 1.5to1.3million years ago. The East Molokai Volcano, sometimes also known as Wailau for the Wailau valley on its north side, is an extinct shield volcano comprising the eastern two-thirds of the island of Molokai in the U.S. state of Hawaii. Bolkan ang East Molokai Volcano sa Tinipong Bansa. Maui view from the front yard. What are some facts about East Molokai volcano? The highest point is the peak called Kamakou on the southern rim, at 21623N 156525W / 21.10639N 156.86806W / 21.10639; -156.86806 (Kamakou). East Molokai volcano was constructed along an E-W trending rift zone. The The northern half of the volcano is truncated by a cliff more than 1 km high resulting from the massive Wailau debris avalanche that extended more than 100 km N (Moore et al. Argiope Appensa -- Garden Spider. It is overlapped by the West Molokai, Lanai and Haleakal shield volcanoes. Click Link Below For Video http://docs.google.google.com/a/hoovermiddleschool.org/file/d/0B3UAyP-YzTxPYU9NQ2x5YmE1N0E/edit East Molokai Volcano Paper Mache And First coat of paint East East Molokai Volcano, Hawaii: Petrogenesis of Shield-, Postshield-and Rejuvenated Stage Lavas: Publication Type: Conference Paper: Authors: Xu G, Frey FA, Clague DA, Wise S: Department of Earth, Ocean and Atmospheric Sciences. Each of the Hawaiian Islands is generally older than the next when one moves up the island chain from southeast (the Big Island) to northwest (Kure).