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Water plus magma equals increased explosivity

And other newly released GSA Bulletin articles

Date:
February 10, 2016
Source:
Geological Society of America
Summary:
When water interacts with magma, it can dramatically increase the explosivity of the eruption. However, water in the eruption cloud can also increase the rate at which the particles aggregate into larger clumps, allowing them to settle out faster. The five-week-long 2008 Okmok eruption in the Aleutian Islands of Alaska was explosive due to the interaction of the magma with the abundant water inside the caldera.
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This is Figure 1 from Unema et al., including the location of Okmok volcano on Umnak Island in central Aleutian Islands.
Credit: J.A. Unema and GSA Bulletin

When water interacts with magma, it can dramatically increase the explosivity of the eruption. However, water in the eruption cloud can also increase the rate at which the particles aggregate into larger clumps, allowing them to settle out faster. The five-week-long 2008 Okmok eruption in the Aleutian Islands of Alaska was explosive due to the interaction of the magma with the abundant water inside the caldera, producing billowing clouds that deposited most of the tephra as fine-grained ash within 10 km of the vent area.

The first four hours of the eruption produced coarse tephra that extended well offshore of Umnak Island, but the remainder deposited ash as ash pellets and as muddy rain and mist. This plume scrubbing likely reduced any aviation hazards.

This paper by Joel A. Unema and colleagues describes the stratigraphy, distribution, and grain size, shape, and composition characteristics of the medial to distal deposits of the 2008 Okmok eruption. These are used to interpret water-magma interactions in the conduit and eruption column, eruption parameters (e.g., volume, column height, mass flux), and fragmentation style. Unema and colleagues then compare the Okmok eruption with the Eyjafjallajökull eruption of 2010.


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The above post is reprinted from materials provided by Geological Society of America. Note: Content may be edited for style and length.


Journal Reference:

  1. Joel A. Unema, Michael H. Ort, Jessica F. Larsen, Christina A. Neal, Janet R. Schaefer. Water-magma interaction and plume processes in the 2008 Okmok eruption, Alaska. Geological Society of America Bulletin, 2016; B31360.1 DOI: 10.1130/B31360.1

Cite This Page:

Geological Society of America. "Water plus magma equals increased explosivity: And other newly released GSA Bulletin articles." ScienceDaily. ScienceDaily, 10 February 2016. <www.sciencedaily.com/releases/2016/02/160210135201.htm>.
Geological Society of America. (2016, February 10). Water plus magma equals increased explosivity: And other newly released GSA Bulletin articles. ScienceDaily. Retrieved August 25, 2016 from www.sciencedaily.com/releases/2016/02/160210135201.htm
Geological Society of America. "Water plus magma equals increased explosivity: And other newly released GSA Bulletin articles." ScienceDaily. www.sciencedaily.com/releases/2016/02/160210135201.htm (accessed August 25, 2016).