World Library  
Flag as Inappropriate
Email this Article

East Molokai Volcano

East Molokai Volcano
Aerial photo of the southwestern flank of East Molokai Volcano
Elevation 1,210 m (3,970 ft)
Location Molokai, Hawaii,
United States
Range Hawaiian Islands
Type Shield volcano
Volcanic arc/belt Hawaiian-Emperor seamount chain

The East Molokai Volcano, sometimes also known as Wailau for the Wailau valley on its north side,[1] is an extinct shield volcano comprising the eastern two-thirds of the island of Molokaʻi in the U.S. state of Hawaii.


The East Molokai has a width of 70 km (43 mi) and a length of 150 km (93 mi). It is overlapped by the West Molokai, Lanai and Haleakalā shield volcanoes. Its shield formation began two million years ago and ended 1.5 million years ago whereas its postshield eruptions occurred 1.5 to 1.3 million years ago. The pahoehoe shield volcano of the Kalaupapa Peninsula postdates the main shield volcano of East Molokai and is considered to represent the last volcanic phase of East Molokai.[1]

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 .[2][3] The Pēpēʻōpae bog is just below the rim.[4]

The northern flank of the volcano has been truncated by enormous cliffs rising 900 metres (3,000 ft) from the sea. The sea cliffs were formed when the northern third of the East Molokai Volcano suddenly collapsed and slid off into the sea, about 1.4 million years ago. The landslide was so fast and powerful that it extended 190 kilometres (120 mi) into the sea, and generated a 600 metres (2,000 ft) high megatsunami that inundated the rest of Molokai.[5]


  1. ^ a b Wood, Charles A.; Kienle, Jürgen (2001). Volcanoes of North America: United States and Canada.  
  2. ^ U.S. Geological Survey Geographic Names Information System: Kamakou
  3. ^  
  4. ^ U.S. Geological Survey Geographic Names Information System: Pēpē‘ōpae
  5. ^ "Kalaupapa Settlement Boundary Study. Along North Shore to Halawa Valley, Molokai". National Park Service. 2001. Retrieved 2014-01-29. 

External links

  • Melvin H. Beeson (1976). "Petrology, Mineralogy,and Geochemistry of the East Molokai Volcanic Series, Hawaii".  
This article was sourced from Creative Commons Attribution-ShareAlike License; additional terms may apply. World Heritage Encyclopedia content is assembled from numerous content providers, Open Access Publishing, and in compliance with The Fair Access to Science and Technology Research Act (FASTR), Wikimedia Foundation, Inc., Public Library of Science, The Encyclopedia of Life, Open Book Publishers (OBP), PubMed, U.S. National Library of Medicine, National Center for Biotechnology Information, U.S. National Library of Medicine, National Institutes of Health (NIH), U.S. Department of Health & Human Services, and, which sources content from all federal, state, local, tribal, and territorial government publication portals (.gov, .mil, .edu). Funding for and content contributors is made possible from the U.S. Congress, E-Government Act of 2002.
Crowd sourced content that is contributed to World Heritage Encyclopedia is peer reviewed and edited by our editorial staff to ensure quality scholarly research articles.
By using this site, you agree to the Terms of Use and Privacy Policy. World Heritage Encyclopedia™ is a registered trademark of the World Public Library Association, a non-profit organization.

Copyright © World Library Foundation. All rights reserved. eBooks from Project Gutenberg are sponsored by the World Library Foundation,
a 501c(4) Member's Support Non-Profit Organization, and is NOT affiliated with any governmental agency or department.