Research opens fresh view on volcanic plumbing systems

Oregon-led research opens fresh view on volcanic plumbing systems
The iconic El Capitan at Yosemite National Park in California contains a long-running record of magma injections that never breached the surface, instead freezing into the Earth's crust. Credit: Greg M. Stock, National Park Service

Volcanic eruptions such as Mount St. Helens' in 1980 show the explosiveness of magma moving through the Earth's crust. Now geologists are excited about what uplifted granite bodies such as Yosemite's El Capitan say about magma that freezes before it can erupt on the surface.

These granite structures, called magmatic intrusions, form incrementally over time by small pulses of magma that cool and crystalize 5 to 20 kilometers—3 to 12 miles—underground. Many are uplifted and exposed by erosion. They also contain the history of magma injections that occurred tens to hundreds of millions of years ago, says Leif Karlstrom of the University of Oregon.

In a paper placed online July 10 by the journal Nature Geoscience, a three-member research team led by Karlstrom unveiled a new framework for understanding what the pattern of volcanoes seen at the surface implies about the structure of subsurface magma plumbing systems. Some 50 to 90 percent of magma, Karlstrom said, doesn't get through the crust.

"Granitic landscapes in the Yosemite Valley in California and in the North Cascades are iconic, huge cliffs with exposed rock," he said. "If you look closer, the structure of that landscape shows all kinds of intrusive bodies that record different pulses of magma coming into the crust. Our findings hopefully allow you to stare up at El Capitan and make sense of it in some new way."

In the National Science Foundation-funded research, Karlstrom, Scott R. Paterson of the University of Southern California and A. Mark Jellinek of the University of British Columbia examined more than a decade of measurements of size distributions of igneous rock intrusions in the North American Cordillera.

Magma rising in active volcanic regions in places such as the Cascades, Hawaii and Iceland, Karlstrom said, often occurs as narrow, sheet-like intrusions commonly called dikes and sills. This occurs as a cracking process in brittle crustal rocks. Over long timescales, however, the process changes.

These changes are part of a transition into a "reverse energy cascade," in which rising magma injections become trapped and lose energy, the researchers say.

Magma mixes and merges with surrounding rocks as it cools and crystalizes. Heat lost from repeated injections of magma continues to heat crustal rocks, building and the expanding granitic intrusive complexes formed by frozen magma in a viscous, rather than brittle, manner. The resulting structures are seen today where the formations are exposed.

"That act of dumping heat into the crust over time changes the nature of the mechanical response to injections of magma," Karlstrom said. "The earth's crust is a filter for rising melts. You have magma that is generated deep in the earth, and somehow it gets to the surface carrying heat and volatiles, such as carbon dioxide. How that happens is through the crustal magma transport system."

Studying the processes behind injections over long timescales, he said, helps build better understanding of volcanoes, their impacts on global climate and where large volcanoes are likely to occur.

"This paper hits on one of the primary current research problems in volcanology," Karlstrom said. "We are able to make a strong statement about the connection of deep intrusive magmatism to the surface expression of volcanism. We think that what we found provides a framework for understanding other kinds of problems related to magmatism on Earth and other planets."


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More information: Leif Karlstrom et al, A reverse energy cascade for crustal magma transport, Nature Geoscience (2017). DOI: 10.1038/ngeo2982
Journal information: Nature Geoscience

Citation: Research opens fresh view on volcanic plumbing systems (2017, July 10) retrieved 22 May 2019 from https://phys.org/news/2017-07-fresh-view-volcanic-plumbing.html
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Jul 10, 2017
Interesting --at least to me-- that these researchers(in terms of this article) completely ignore the role of active plate tectonics and the resulting faulting, folding, and deformation of the crust as having any effect upon upon the timing, location, or scale of magmatic intrusion.

Jul 10, 2017
I suppose the question is why such magma pulses halted where they did, rather than intrude as dykes & sills, or break surface. Yes, there's much intricate geochemistry at play within and between existing rock masses and incoming, but what makes a particular pulse 'stick or twist' ??

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