Honolulu Civil Beat reporter, Denby Fawcett, recently published a story highlighting the 2014 pioneering publication led by John Sinton, emeritus professor of Earth Sciences at SOEST, that revealed Ka‘ena Volcano as the precursor volcano of the island of O‘ahu, Hawai‘i. Excerpts from the story are below.
“My purpose here is to describe and honor the long-lost third volcano that scientists named Kaena — at one time a massive shield volcano, the first to form Oahu.
Why focus on a precursor volcano that’s now submerged thousands of feet under the sea? One reason is that Kaena is still largely unknown to the general public. And if you ask, who cares, I contend it is just as interesting to know about the earth we are standing on as to be aware of what towers above us.
According to the findings of the scientific team led by University of Hawaii geologist John Sinton, the volcano Kaena erupted off today’s Kaena Point about 5 million years ago, making it the oldest volcano responsible for the creation of Oahu.
Sinton says at one point in Oahu’s geologic history all three volcanoes stood together high above sea level. Kaena, the shortest of the trio, rose about 3,000 feet.
All that remains of Kaena volcano today is a long ridge under the sea, extending westward from Kaena Point with half of the underwater ridge covered by younger lavas from the Waianae volcano. The original extent of Kaena is not known, but it must have extended to the south at least as far as present day Waianae Valley. The sheer size of Kaena’s remnants suggest Oahu once was about two times larger than it is today.
[SOEST] Geologist Scott Rowland says the fact that we can no longer see Kaena volcano, whose summit is now almost 2,600 feet below the sea, would help explain why this Oahu first-born volcano is still off the radar of most of us today.
[The] team from the UH collaborated on the project with Laboratoire des Sciences du Climat et de L’Environment (France), and the Monterey Bay Aquarium Research Institute. UH researchers on the Kaena expeditions included Deborah Eason, Mary Tardona, Douglas Pyle and Iris van der Zander.
Sinton says he looks forward to more research on Kaena Ridge using the latest high-resolution techniques, especially to better understand samples gathered from neighboring Waialu Ridge but not yet dated.
In the 2014 paper, Sinton and his co-authors describe Waialu Ridge as a part of Kaena volcano, not a separate magma producing structure — but maybe it isn’t, says Sinton.
Maybe Waialu is another volcano, a fourth volcano that was situated between Kaena and Waianae volcanoes.
Just when we think we know everything, we don’t. That is the beauty of science.”
Read the full story on Civil Beat.