USGS/Cascades Volcano Observatory, Vancouver, Washington
DESCRIPTION:
Lake Bonneville and the Bonneville Flood
- Lake Bonneville and the Bonneville Flood
- Great Salt Lake
- Snake River Canyon
Lake Bonneville and the Bonneville Flood
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From:
U.S. National Park Service Website, Ice Age Floods, 2002
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The "Bonneville flood" occurred bout 15,000 years
ago when the great Lake Bonneville, which covered
much of Utah (Great Salt Lake is the minuscule remnant) overtopped Red Rock Pass causing the lake surface to drop 300 feet to the Provo shoreline. The Bonneville flood released 1,000 cubic miles of water. The volume of this flood was twice as large as the biggest
Missoula flood. However, unlike the Ice Age Floods,
the Bonneville Flood occurred over a period of a couple of weeks.
From:
U.S. National Park Service Website, Ice Age Floods, 2002
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Ice Age Lake Bonneville,
which existed around 14,500 years ago, covered more than 20,000
square miles in Utah and parts of Idaho and Nevada.
For hundreds of years, the water level of
Lake Bonneville maintained a fairly constant level.
The water level dropped almost 400 feet
when part of Red Rock Pass, which was holding
back the water, eroded. The floodwaters
flowed down the Snake River and joined the Columbia River
near the Tri-Cities. For a short
period of time, the resulting floodwaters from
Lake Bonneville increased the size of the Snake River
and the Columbia River by more
than 20 times their normal flow. After the flood
occurred, the water levels of the Great Salt Lake
eventually subsided close to what they
are now. Lake Bonneville drained only once, with
catastrophic results.
From:
U.S. Bureau of Land Management, Snake River Birds of Prey National Conservation Area Website, 2002
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As glaciers receded during the last ice age, the inland basin of
central Utah slowly
filled with meltwater, creating Lake Bonneville. This lake covered approximately 20,000
square miles. The water level rose and finally crested at the lowest point in the basin --
Red Rock Pass, Idaho. The soft soils were easily eroded as the water spilled over,
creating a large outlet for the lake. Water spilled out of Lake Bonneville and flowed north
into the valleys of Marsh Creek and the Portneuf River. The deluge entered the
Snake River Plain
just north of Pocatello, and flowed west across southern Idaho before turning
back north into the Hell's Canyon region. This flood took place about 14,000 years ago.
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The
Snake River and its canyons
were the major geographic features across the
volcanic plain and became the main conduit for the Bonneville flood. The varying
topographic features of the Snake River produced distinct types of hydraulics. In places
where the canyon is deep and constricted, the velocity of the water increased
tremendously. This increased energy allowed the water to pick up talus boulders the size
of houses, turn, roll, and smooth out their rough edges, and deposit them many miles
downstream. When the water entered wide, open stretches, the velocity decreased and
the energy of the water could not keep the boulders suspended. The rocks settled in the
bottom of the river and are now exposed on the larger bars along the river. These large,
rounded boulders were nicknamed "melon gravel" due to the resemblance to big
watermelons. ...
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Some people think the Bonneville Flood created the Snake River Canyon. This is not
completely accurate. The canyon existed prior to the flood in much the same condition as
it is today. Floodwaters completely filled the canyon in some locations and flowed above
the canyon rim in other areas. The force of the flood waters scoured the canyon in
constricted locations. The river carved out many "box" canyons along the cliffs in places
where large eddies formed.
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What would it have been like to stand on the rim and watch the river flow by at that
time? From geologic evidence it has been calculated that the peak discharge flow at
Swan Falls was 33 million cubic feet/second. If railroad tank cars were filled with 33
million cubic feet of water, it would form a train 165 miles long. This volume of water
passed by Swan Falls every second! For those who think a raft trip through the Grand
Canyon would be exciting, a raft on the river during the peak discharge would have been
traveling at 70 miles/hour (without rowing) on a wall of water 312 feet deep. Now that's
big water rafting.
From:
NASA, Goddard Space Flight Center Website, 2002
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The Great Salt Lake is the remnant of ancient Lake Bonneville, which gave the Bonneville Salt Flats their name. Geologists
estimate that Lake Bonneville existed between 23,000 and 12,000 years ago, during the last glacial period. Lake Bonneville's
existence ended abruptly when the waters of the lake began to drain rapidly through Red Rock Pass in southern Idaho into the
Snake River system. As the Earth's climate warmed and became drier, the remaining
water in Lake Bonneville evaporated, leaving the highly saline waters of the Great Salt Lake. The reason for the high concentration
of dissolved minerals in the Great Salt Lake is due to the fact that it is a "terminal basin" lake; water than enters the lake from
streams and rivers can only leave by evaporation. As the process occurs over time, the dissolved substances in the river water
become increasingly concentrated.
From:
U.S. Bureau of Land Management's Website, 2002
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As you drop into the Snake River Canyon, you can trace some of the geologic history of the area. The canyon cliffs show layer upon layer of lava flows interspersed with sedimentary layers. As you reach the bottom, the canyon floor is scattered with hundreds of house-size boulders left behind from the Bonneville flood. This flood raced through the canyon 15,000 years ago with more than 100 meters (350 feet) of water rushing at 110 kilometers (70 miles) per hour.
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01/22/03, Lyn Topinka