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Ulupaʻu Crater (also known as Ulupaʻu Head) is a tuff cone in the U.S. state of Hawaii, located near Marine Corps Base Hawaii on the Mokapu Peninsula. It formed as a result of the Honolulu Volcanic Series, which was a set of eruptions from the Koʻolau Range during its rejuvenation stage. The HVS also created other volcanoes such as Diamond Head. The eastern part of Ulupaʻu's rim was destroyed due to erosion. A cinder cone known as Puʻu Hawaiʻiloa is located nearby on the same peninsula.

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  • Ulupaʻu Crater (en)
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  • Ulupaʻu Crater (also known as Ulupaʻu Head) is a tuff cone in the U.S. state of Hawaii, located near Marine Corps Base Hawaii on the Mokapu Peninsula. It formed as a result of the Honolulu Volcanic Series, which was a set of eruptions from the Koʻolau Range during its rejuvenation stage. The HVS also created other volcanoes such as Diamond Head. The eastern part of Ulupaʻu's rim was destroyed due to erosion. A cinder cone known as Puʻu Hawaiʻiloa is located nearby on the same peninsula. (en)
foaf:name
  • Ulupaʻu Crater (en)
name
  • Ulupaʻu Crater (en)
geo:lat
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  • http://commons.wikimedia.org/wiki/Special:FilePath/Mokapu_Peninsula_and_Kaneohe_Bay.jpg
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  • Ulupaʻu Crater within Hawaii (en)
photo
  • Mokapu Peninsula and Kaneohe Bay.jpg (en)
photo caption
  • Aerial view of Ulupaʻu Crater and the rest of the Mokapu Peninsula (en)
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  • 21.454444444444444 -157.73166666666665
has abstract
  • Ulupaʻu Crater (also known as Ulupaʻu Head) is a tuff cone in the U.S. state of Hawaii, located near Marine Corps Base Hawaii on the Mokapu Peninsula. It formed as a result of the Honolulu Volcanic Series, which was a set of eruptions from the Koʻolau Range during its rejuvenation stage. The HVS also created other volcanoes such as Diamond Head. The eastern part of Ulupaʻu's rim was destroyed due to erosion. A cinder cone known as Puʻu Hawaiʻiloa is located nearby on the same peninsula. (en)
last eruption
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  • POINT(-157.73167419434 21.454444885254)
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