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Mass of warm rock rising beneath New England

Date:
November 30, 2017
Source:
Rutgers University-New Brunswick
Summary:
Slowly but steadily, an enormous mass of warm rock is rising beneath part of New England, although a major volcanic eruption isn't likely for millions of years, a new study suggests. The research is unprecedented in its scope and challenges textbook concepts of geology.
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Slowly but steadily, an enormous mass of warm rock is rising beneath part of New England, although a major volcanic eruption isn't likely for millions of years, a Rutgers University-led study suggests. The research is unprecedented in its scope and challenges textbook concepts of geology.

"The upwelling we detected is like a hot air balloon, and we infer that something is rising up through the deeper part of our planet under New England," said lead author Vadim Levin, a geophysicist and professor in the Department of Earth and Planetary Sciences at Rutgers University-New Brunswick. "It is not Yellowstone (National Park)-like, but it's a distant relative in the sense that something relatively small -- no more than a couple hundred miles across -- is happening."

The study, which tapped seismic data through the National Science Foundation's EarthScope program, was published online today in Geology. Study co-authors include Yiran Li and Peter Skryzalin, who did their research through Rutgers' Aresty Research Assistant program, and researchers at Yale University.

"Our study challenges the established notion of how the continents on which we live behave," Levin said. "It challenges the textbook concepts taught in introductory geology classes."

Through EarthScope, thousands of seismic measurement devices, which were 46.6 miles apart, covered the continental United States for two years. Nothing on Earth has been done on this scale, Levin said. The EarthScope program seeks to reveal the structure and evolution of the North American continent and the processes that cause earthquakes and volcanic eruptions, the NSF says.

Levin studies seismic waves, or the vibrations that pass through our planet following earthquakes. Seismic waves provide a window into the Earth's interior by revealing the shapes of objects, changes in the state of materials and clues about their texture. The Rutgers-led study focused on New England, where scientists had previously documented an area of great warmth (hundreds of degrees Celsius warmer than neighboring areas) in the Earth's upper mantle. The lithosphere, Earth's solid outer shell, consists of the upper mantle and the crust that includes the surface.

"We're interested in what happens at the interface between tectonic plates -- thick, solid parts that cover our planet -- and material in the upper mantle beneath the plates," Levin said. "We want to see how North America is gliding over the deeper parts of our planet. It is a very large and relatively stable region, but we found an irregular pattern with rather abrupt changes in it."

Levin thinks the upwelling pattern detected is largely beneath central Vermont and western New Hampshire, but it's also under western Massachusetts. It may be present elsewhere, but the study's findings were based on available seismic observations.

"The Atlantic margin of North America did not experience intense geologic activity for nearly 200 million years," Levin said. "It is now a so-called 'passive margin' -- a region where slow loss of heat within the Earth and erosion by wind and water on the surface are the primary change agents. So we did not expect to find abrupt changes in physical properties beneath this region, and the likely explanation points to a much more dynamic regime underneath this old, geologically quiet area."

"It will likely take millions of years for the upwelling to get where it's going," he added. "The next step is to try to understand how exactly it's happening."


Story Source:

Materials provided by Rutgers University-New Brunswick. Note: Content may be edited for style and length.


Journal Reference:

  1. Vadim Levin, Maureen D. Long, Peter Skryzalin, Yiran Li, Ivette López. Seismic evidence for a recently formed mantle upwelling beneath New England. Geology, 2017; DOI: 10.1130/G39641.1

Cite This Page:

Rutgers University-New Brunswick. "Mass of warm rock rising beneath New England." ScienceDaily. ScienceDaily, 30 November 2017. <www.sciencedaily.com/releases/2017/11/171130094142.htm>.
Rutgers University-New Brunswick. (2017, November 30). Mass of warm rock rising beneath New England. ScienceDaily. Retrieved March 1, 2024 from www.sciencedaily.com/releases/2017/11/171130094142.htm
Rutgers University-New Brunswick. "Mass of warm rock rising beneath New England." ScienceDaily. www.sciencedaily.com/releases/2017/11/171130094142.htm (accessed March 1, 2024).

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