The Volcanic History of Mauna Kea

The tour guides give the basic story behind the creation of Mauna Kea. The story given is simple… A hot spot in the mantle is the source for a plume of magma that punches through the oceanic crust and forms the Hawaiian volcanoes. As the pacific plate moves the islands are formed one by one, the latest being the Big Island of Hawaiʻi.

Puʻu Kole Panorama
A panarama from atop Puʻu Kole showing Mauna Kea and a distant snow covered Mauna Loa
This is basically correct, but is also a vast simplification of the process. If you want to learn more about the formation of these impressive volcanoes you need to look further.

Fortunately there is a good source for answers… The Geology and Petrology of Mauna Kea Volcano, Hawaii —A Study of Postsheild Volcanism, Edward Wolfe, William Wise, and G. Brent Dalrymple. This seems to be the definitive paper on the geology of Mauna Kea. Any time I see a list of references for the geology of the mountain, this paper appears. Published in 1997 it incorporates much of the earlier studies on Mauna Kea into one compendium.

This paper is not light reading. It is 130 pages of details, tables, minerological analysis, chemical abundances, radiometric dates, figures and complex geologic terminology. Reading this strains my understanding of the subject, even after some college geology course work and a lifetime of reading on the subject. Still, the exercise is worth it, there are many answers in this paper, so many interesting details about the mountain.

Puʻu Kole
Puʻu Kole as seen from upslope across the aʻa lava field
One surprise was the site of the most recent eruption. I was curious and was looking for that specific answer in the paper. It turns out that the most recent identified eruption site is Puʻu Kole, the same puʻu I hiked to a last year. A flow on the north flank of Puʻu Kole is dated to only 4,500 years ago while the south flank is younger, at 4,400 years old. It was this north side flow I crossed to access the cone, it did look pretty fresh.

These last eruptions were part of the Laupahoehoe lavas that cover the eastern flank of the mountain. Apparently these eruptions were quite active, creating large amounts of volcanic ash that form substantial deposits on the flanks of the mountain (p.125).

Mauna Kea from ISS
Mauna Kea as seen from the International Space Station
The story behind the formation of the mountain (p. 114) is a bit more complex than the simple story in the guidebooks. One would think that the mantle material simply erupts on the surface. Not at all… What erupts is a complex stew of mantle and crustal rocks melted by the upwelling heat. This mixture is revealed in the petrochemistry of the rocks found in the various lava flows at the surface.

There is also a distinct series of phases in the formation of the volcano with differing magma production rates and different chemistry of the resulting lavas. the last and current phase is the post-shield phase, easily studied as these flows lie at the surface. Studying the older phases of Mauna Kea is more challenging as these lavas are often deeply buried and only exposed by erosion or by drilling.

There were more interesting stories here.. Magma production rates have much to do with the formation of the shorelines. The profile of the shore is a complex interaction between eruptions, erosion and sea level as the immense weight of the volcano presses down on the oceanic crust and the entire island subsides. As a diver I had noted the relic shorelines and sea cliffs that are now submerged all along Mauna Kea’s western side. These date from the last periods of the shield building phase of the mountain and the final large lava flows to pour down this slope to the sea.

Sunrise in the Saddle
The light of dawn across the flanks of Mauna Kea
A couple sections of the paper are devoted to the ice age glacial activity that shaped the summit (p. 40). The glacial deposits are extensive in the summit region. These are found as large deposits of angular boulders and cobbles shaped and smoothed by the ice. A number of very clear moraine structures are also mapped in the report.

Several distinct glacial deposits are mapped in the report, often separated by lava flows indicating alternating periods of glacial and volcanic activity. Again the story is complex as the eruptive activity and the ice alternately dominated the summit of Mauna Kea.

While the paper may require a little learning by a layman such as myself to fully understand, it is a wonderful resource in understanding Mauna Kea. I keep a copy of it on my iPad, it makes good reading for the long trips up and down our mountain.

Author: Andrew

An electrical engineer, amateur astronomer, and diver, living and working on the island of Hawaiʻi.

2 thoughts on “The Volcanic History of Mauna Kea”

Leave a Reply

Your email address will not be published.