Geologists from France and the United States have discovered that the Hawaiian island of O’ahu consists of three major volcanoes, not two, as previously thought. O’ahu is known to have remnants of Wai’anae and Ko’olau volcanoes. But extending almost 100 km from the western tip of this island is a large region of shallow bathymetry called the submarine Ka’ena Ridge. This region represents a precursor volcano to the island of O’ahu, and on whose flanks the Wai’anae and Ko’olau volcanoes later formed. Prior to this recognition of Ka’ena Volcano, Wai’anae Volcano was assumed to have been exceptionally large and to have formed an unusually large distance from its next oldest neighbor – Kaua’i. Prof John Sinton of the University of Hawai’is School of Ocean and Earth Science and Technology, who is the lead author of a paper published in the Geological Society of America Bulletin, explained: “both of these assumptions can now be revised: Wai’anae is not as large as previously thought and Ka’ena Volcano formed in the region between Kauai and Wai’anae.” In 2010 scientists documented enigmatic chemistry of some unusual lavas of Wai’anae. “We previously knew that they formed by partial melting of the crust beneath Wai’anae, but we didn’t understand why they have the isotopic composition that they do. Now, we realize that the deep crust that melted under Waianae is actually part of the earlier Ka’ena Volcano,” Prof Sinton said. High-quality bathymetric data shows that Ka’ena Ridge has an unusual morphology. This prompted Prof Sinton’s team to begin collecting samples from Ka’ena and Wai’alu submarine Ridges. The geochemical and age data, along with geological observations and geophysical data, confirmed that Ka’ena was not part of Waianae, but rather was an earlier volcanic edifice. Wai’anae must have been built on the flanks of Ka’ena. “What is particularly interesting is that Ka’ena appears to have had an unusually prolonged history as a submarine volcano, only breaching the ocean surface very late in its history,” Prof Sinton said. --> --> Read the paper!! John M. Sinton et al. Ka’ena Volcano – A precursor volcano of the island of O’ahu, Hawai’i. Geological Society of America Bulletin, published online May 02, 2014; doi: 10.1130/B30936.1 Image: Map shows the distribution of the three volcanoes – the Ka’ena, Wai’anae and Ko’olau – now thought to have made up the region of O’ahu, Hawai’i. Bold dashed lines delineate possible rift zones of the three volcanoes; also shown are the major landslide deposits around O’ahu. Image: Simplified cross-section shows how Ka’ena, Wai’anae and Ko’olau overlap. Image credits: J. Sinton et al / University of Hawai’is School of Ocean and Earth Science and Technology.
Posted on: Thu, 11 Dec 2014 16:00:00 +0000
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