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Ice Age Floods, Lake Missoula, Bonneville Flood and the Columbia River Basalts

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    [Intro Music]
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    The Pacific Northwest is famous for many
    things.
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    Including huge floods.
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    Floods of lava that buried almost 40%
    of Washington,
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    and floods of Ice Age water that
    created more than 2,000 square miles
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    of scab lands.
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    What are the odds that such rare events
    both happened here in this corner of
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    North America?
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    We're just south of Lewiston Idaho at the
    mouth of Hills Canyon,
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    the lowest point in the state.
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    The basalt bedrock here,
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    the floods of lava, came out of deep
    cracks that formed in response to a heat
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    source that's now, in the state of
    Wyoming.
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    A flood of water from a giant lake in Utah
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    came all the way through Southern Idaho,
    through Hills Canyon,
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    dropped rocks here, and the water made it
    to the Pacific Ocean.
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    A giant lake in Montana
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    flowed to the cascades, got backed up
    to here.
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    Each of these layers representing a
    separate flood.
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    The Columbia River basalts,
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    the Bonneville flood,
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    and the Missoula floods.
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    Let's dig into together and learn,
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    about huge floods in the Pacific
    Northwest.
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    [ Music Plays ]
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    The Ice Age floods have helped exposed
    and incredible pile of lavas
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    from erupting volcanoes that are not
    related to our famous cascade volcanoes.
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    The Columbia River basalt group,
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    a pile of lava rock more then 2 miles
    thick,
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    is an exception to the global rule.
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    Basalt lavas usually erupt in ocean
    basins,
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    but these low silica lavas flooded North
    America from below.
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    Much like a boat with a leak.
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    They're similar flood in central India,
    southern Brazil, southern Africa,
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    and central Siberia.
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    In each case, very large volumes of fluid
    basaltic magma
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    erupted rapidly from cracks and continents
    to form sheets of lava rock covering
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    tens of thousands of square miles.
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    The deep crack called fissures cracked
    the North American crust in south eastern
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    Washington and eastern Oregon,
    starting 17.5 million years ago.
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    Today many geologist agree that the
    fissures are directly related to the birth
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    of a tectonic hot spot,
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    beneath the out south-eastern Oregon
    17.5 million years ago,
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    and now located underneath Yellowstone
    National Park in Wyoming due to the
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    North American plates slowly moving over
    the stationary hot spot.
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    These spectacular basalt lava eruptions,
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    more than 300 distinct events punctuated
    by thousands of years of quiet between
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    each lava flood.
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    Flooded and buried, the rugged inland
    landscape of the Pacific Northwest.
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    Many of the biggest lava flows made it
    from their fissures in Idaho all the way
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    to the tower cliffs of the Oregon coast.
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    At Pasco Washington the stack of Columbia
    River basalt lava flows is 1,600 ft. thick
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    more then 3 miles of lava.
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    Sitting on top of a 17 million year old
    landscape.
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    There isn't one visage to see all the
    lava flows, how could you?
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    To truly grasp the scale of the lava stack
    one has to visit scattered canyons that
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    expose a dozen flows at a time, like
    in the Yakama River Canyon,
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    and the Columbia River Gorge,
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    or in the Grand Coulee,
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    which was carved just thousands of years
    ago, not millions.
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    By the Ice Age floods.
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    [ Music Plays ]
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    During the Ice Age, a thick ice sheet
    covered much of North America,
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    advancing and retreating in response to
    global climate.
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    In Washington, Canadian ice crossed the
    border in different places.
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    West of the cascade range, the Puget Lobe
    filled the Puget Lowland with 3,000 ft.
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    of ice, above present day Seattle.
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    With
Title:
Ice Age Floods, Lake Missoula, Bonneville Flood and the Columbia River Basalts
Description:

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Video Language:
English
Duration:
16:18

English subtitles

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