• As tectonic plates pull apart, what driv

    From ScienceDaily@1:317/3 to All on Mon Feb 7 21:30:44 2022
    As tectonic plates pull apart, what drives the formation of rifts?
    Research on a young rift in Iceland sheds new light on the process

    Date:
    February 7, 2022
    Source:
    University at Buffalo
    Summary:
    At the boundaries between tectonic plates, narrow rifts can form
    as Earth's crust slowly pulls apart. But how, exactly, does this
    rifting happen? Does pressure from magma rising from belowground
    force the land apart? Or is a rift just a rip, created mainly by
    the pulling motion of tectonic plates that are drifting away from
    each other? A study explores these questions and sheds new light
    on how this process works.



    FULL STORY ==========================================================================
    At the boundaries between tectonic plates, narrow rifts can form as
    Earth's crust slowly pulls apart.


    ==========================================================================
    But how, exactly, does this rifting happen? Does pressure from magma
    rising from belowground force the land apart? Or is a rift just a rip,
    created mainly by the pulling motion of tectonic plates that are drifting
    away from each other? A study in the journalGeology explores these
    questions and sheds new light on how this process works.

    Past research has pointed to magma as a key driver in rifting events. But
    the new findings highlight that, "We have to be a bit more nuanced
    and acknowledge that rift processes do not have to operate identically
    across the entire globe," says lead scientist Stephan Kolzenburg, PhD, assistant professor of geology in the University at Buffalo College of
    Arts and Sciences.

    Study tells the story of a newly formed rift in Iceland The new study
    was published in November 2021. It describes how a trench-like structure
    called a rift-graben opened in 2014 in Iceland near what is now known
    as the Holuhraun lava field, in a region that straddles the tectonic
    boundary between the North American and Eurasian plates. A graben forms
    when a chunk of land sags downward as the land on both sides of it moves
    away, creating a chasm called a rift.



    ==========================================================================
    The team concluded that in this particular case, the slow drift of
    tectonic plates, and not pressure from a magma chamber along the rift,
    was the driver.

    The graben formed within a period of a few days, and then, "it just stayed
    like that, and it didn't care about anything else that happened in the
    magmatic plumbing system," Kolzenburg says. "The graben was remarkably
    stable even though lots of dynamic processes were happening underneath,
    such as pressure changes in the magmatic feeder system of the eruption."
    Magma leaked through the rift once it was open, but that magma didn't
    appear to be the main force behind the initial creation of the rift,
    Kolzenburg says.

    The study benefited from the work of an international group of scientists
    who had been closely monitoring Holuhraun and the surrounding region, documenting seismic activity and the volume of magma emerging during a
    period of unrest from 2014-15. Kolzenburg's team compared this information
    to digital elevation models that detailed how the area's topography
    changed over time, capturing the graben's sudden appearance and tracking
    the landscape for nearly five years after the graben's formation.

    Not all rifts are created the same way The findings apply specifically
    to the graben the team studied. In other rift zones, different dynamics
    may be at play, including in the Afar Region of Ethiopia, where magma
    is believed to play a more important role in driving rift formation,
    Kolzenburg says.



    ==========================================================================
    As he and co-authors write in their 2021 paper in Geology, "In concert,
    the data suggest that while some rifts may be magmatically controlled,
    not all rift zones require the presence of a deep-seated pressurized
    magma chamber to control their dynamics." The study was a collaboration between Kolzenburg, Julia Kubanek at the European Space Agency, Mariel Dirscherl and Ernst Hauber at the German Aerospace Center, Christopher
    W. Hamilton at the University of Arizona, Stephen. P. Scheidt at Howard University and Ulrich Mu"nzer at Ludwig-Maximilians-Universita"t.

    The research team was funded by the Marie Sk?odowska-Curie Actions
    Horizon 2020 project; NASA; the Fulbright Program; U.S. National Science Foundation; and the Bavarian Ministry of Economic Affairs, Regional
    Development and Energy in Germany.

    ========================================================================== Story Source: Materials provided by University_at_Buffalo. Original
    written by Charlotte Hsu.

    Note: Content may be edited for style and length.


    ========================================================================== Related Multimedia:
    * A_view_of_the_graben,_which_emerged_in_Iceland.

    ========================================================================== Journal Reference:
    1. S. Kolzenburg, J. Kubanek, M. Dirscherl, C.W. Hamilton, E. Hauber,
    S.P.

    Scheidt, U. Mu"nzer. Solid as a rock: Tectonic control of graben
    extension and dike propagation. Geology, 2021; DOI: 10.1130/G49406.1 ==========================================================================

    Link to news story: https://www.sciencedaily.com/releases/2022/02/220207155645.htm

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