Hawaii's Kilauea, Mauna Loa volcanoes linked
Mauna Loa's and Kilauea have an opposing pattern: when one is active, the other is quiet because eruptions at one release pressure in the other.
Wed, Oct 24, 2012 at 03:57 PM
Lava flows from Pu'u O'o Crater on Kilauea. (Photo: U.S. Geological Survey)
The past decade of eruptions of Hawaii's Kilauea volcano may have acted as a pressure-relief valve for neighboring Mauna Loa, according to a new model suggesting two of the planet's biggest volcanoes connect deep underground.
Scientists know each of the two Hawaiian volcanoes has its own plumbing —separate, shallow magma chambers. Such chambers are the source of Kilauea's rising lava lake, which is threatening to spill over. But 50 miles (80 kilometers) down, in a part of the Earth's mantle layer called the asthenosphere, Mauna Loa and Kilauea are dynamically coupled, said Helge Gonnermann, a professor at Rice University in Houston, who is the lead author of a new study showing the link.
"It's like groundwater in an aquifer or oil in an oil reservoir," Gonnermann told OurAmazingPlanet. "We know that there is melt that extends beneath both volcanoes. Changes in pressure can be transmitted to both volcanoes."
The Hawaiian Islands are hotspot volcanoes, formed as the Pacific plate moves over a plume of hot magma in the mantle. Pressure changes in the pooled magma in the mantle could rapidly affect both volcanoes, the model indicates.
The model helps explains some intriguing observations: When one volcano inflates, the other starts to bulge about six months later. At times, such as in 2005, both volcanoes inflate at the same, GPS data show
The study suggests that Mauna Loa's and Kilauea's opposing pattern — when one is active, the other is quiet — occurs because eruptions at one volcano release pressure in the other.
The model suggests Mauna Loa, which produced its most recent blast in 1984, had accumulated enough magma for another eruption, but its pressure was relieved by Kilauea's heightened activity.
"The hypothesis coming out of this model is that if we hadn't seen this increased activity at Kilauea, then we would not have seen this pressure relief," Gonnermann said.
The summit of Kilauea has recently started inflating, giving the researchers a real-world test. "If Kilauea continues to inflate like it is right now, and if our model holds water, we should also see another period of inflation at Mauna Loa in about half a year," Gonnermann said.
The scientists also hope to test the model in other hotspot volcanoes, such as those of the Galapagos.
The findings are detailed in the November issue of the journal Nature Geosciences.
Reach Becky Oskin at email@example.com. Follow her on Twitter @beckyoskin. Follow OurAmazingPlanet on Twitter @OAPlanet. We're also on Facebook and Google+.
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