A super-eruption in the Yellowstone volcanic field is even less likely than scientists have thought, say researchers.
A thorough examination of tiny crystals of zircon, a mineral found in rhyolites, an igneous rock, from the Snake River Plain has solidified evidence for this new way of looking at the life cycle of super-volcanic eruptions in the long track of the Yellowstone hotspot, say scientists.
The last eruption 640,000 years ago created the Yellowstone Caldera and the Lava Creek Tuff in what is now Yellowstone National Park.
The Yellowstone hotspot creates a conveyor-belt style of volcanism because of the southwest migration of the North American plate at 2-4 centimeters (about .8 to 1.6 inches) annually over the last 16 million years of volcanism. Due to the movement of the North American plate, the plume interaction with the crust leaves footprints in the form of caldera clusters, in what is now the Snake River Plain, says geologist Ilya N. Bindeman of University of Oregon.
The Picabo volcanic field of southern Idaho was active between 10.4 and 6.6 million years ago and experienced at least three, and maybe as many as six, violent caldera-forming eruptions.
The field has been difficult to assess, says lead author and graduate student Dana Drew, because the calderas have been buried by as much as two kilometers of basalt since its eruption cycle died.
The team reports their work early online in Earth and Planetary Science Letters.
They theorize that basalt from the mantle plume, rocks from Earth’s crust, and previously erupted volcanoes are melted together to form the rhyolites erupted in the Snake River Plain.
Before each eruption, rhyolite magma is stored in dispersed pockets throughout the upper crust, which are later mixed together, according to geochemical evidence. “We think that this batch-assembly process is an important part of caldera-forming eruptions, and generating rhyolites in general,” Drew says.
In reaching their conclusions, Drew and colleagues analyzed radiogenic and stable isotopic data—specifically oxygen and hafnium—in zircons detected in rhyolites found at the margins of the Picabo field and from a deep borehole. That data, in combination with whole rock geochemistry and zircon uranium-lead geochronology, helped provide a framework to understand the region’s ancient volcanic past.
Next door, too
Previous research on the related Heise volcanic field east of Picabo yielded similar results. “There is a growing database of the geochemistry of rhyolites in the Yellowstone hotspot track,” Drew says. “Adding Picabo provides a missing link in the database.”
Drew and colleagues, through their oxygen isotope analyses, identified a wide diversity of oxygen ratios occurring in erupted zircons near the end of the Picabo volcanic cycle. Such oxygen ratios are referred to as delta-O-18 signatures based on oxygen 18 levels relative to seawater. (Oxygen 18 contains eight protons and 10 neutrons; Oxygen 16, with eight protons and eight neutrons, is the most commonly found form of oxygen in nature.)
The approach provides a glimpse into the connection of surface and subsurface processes at a caldera cluster. The interaction of erupted rhyolite with groundwater and surface water causes hydrothermal alteration and the change in oxygen isotopes, thereby providing a fingerprinting tool for the level of hydrothermal alteration, Drew says.
“Through the eruptive sequence, we begin to generate lower delta-O-18 signatures of the magmas and, with that, we also see a more diverse signature,” Drew says. “By the time of the final eruption there is up to five per mil diversity in the signature recorded in the zircons.”
‘Pockets of melt’
The team attributes these signatures to the mixing of diverse magma batches dispersed in the upper crust, which were formed by melting variably hydrothermally altered rocks—thus diverse delta-O-18—after repeated formation of calderas and regional extension or stretching of the crust.
When the pockets of melt are rapidly assembled, the process could be the trigger for caldera-forming eruptions, Bindeman says. “That leads to a homogenized magma, but in a way that preserves these zircons of different signatures from the individual pockets of melt,” he says.
The four co-authors of the paper are: Kathryn E. Watts, who earned a doctorate in geology from University of Oregon in 2011 and now is the Mendenhall Postdoctoral Research Fellow at the US Geological Survey, Menlo Park, California; Axel K. Schmitt of the University of California, Los Angeles; Bin Fu of the Australian National University, Canberra; and Michael McCurry of Idaho State University.
The NSF provided funding for the study.
Source: University of Oregon