geology of idaho
DESCRIPTION
Geology of Idaho. The Snake River Plain. Idaho can be divided into 6 natural geologic regions, each with its own unique characteristics. Clearwater Plateau. Northern Rockies. Snake River Plain. Middle Rockies. Owyhee- Bruneau Plateau. Basin & Range Province. - PowerPoint PPT PresentationTRANSCRIPT
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Geology of Idaho
The Snake River Plain
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Idaho can be divided into 6 natural geologic regions, each
with its own unique characteristics
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Northern Rockies
Clearwater
Plateau
Snake River Plain
Owyhee-BruneauPlateau
Basin & Range Province
Middle
Rockies
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The Columbia Plateau spills over into other states from Washington, even into 3 regions of Idaho
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Columbia Basalts show many layers from many sequential flows
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Clearwater Plateau
Owyhee-Bruneau Plateau
Snake River Plain
These are the 3 regions of Idaho
that share a volcanic origin by extension of the
Columbia Plateau
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Gently rolling hills and valleys; a thinly-spread grassland with some desert-like vegetation
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Some cinder cones, erroneously called “buttes”, are located in this dry grassland
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Rivers and their tributaries have left their impact on the plain
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The Snake River is the main one, arising from Jackson Lake in Jackson Hole, WY, on the eastern
slope of the Grand Teton range
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It flows westward across the southern edge of the SRP. Over thousands of years it has eroded huge canyons in some places, like the Snake River Canyon near Twin Falls (below)
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On the eastern edge of the SRP is found the Grand
Canyon of the Snake River.
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The deepest, most rugged part is called Hell’s Canyon, the deepest gorge in North America, 8000
feet below the surrounding mountain peaks
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Hell’s Canyon lies at the foot of the Seven Devils Mountains (count them)!
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Lewiston (L) and Clarkston (R) lie at the confluence of the Snake (back) and the Clearwater (bottom) Rivers
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Lost River Range
• Lost River Sinks
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The Lost Rivers flow out of the valleys of the Lost River Range and disappear into the ground of the Plain
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The waters become part of the Eastern Snake River Plain Aquifer flowing to the Snake River on the west
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The Snake and tributaries used to flood regularly through thousands of years
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And create opportunities for agriculture
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SRP Formation
• Volcanic activity
• Water erosion
• Sedimentation
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Fissure flows
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Leading to layered basalt formations
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Numerous cinder cones
(buttes)
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And every volcanic formation you can think of located at
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Located in the east-central part of the plain in a triangular area
formed by Arco, Idaho Falls and
Pocatello
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There are many self-
guided tours of the site as
well as an interpretive
center
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The Yellowstone Hot Spot is responsible for the heat that created all this volcanism
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Water is down in the summerdue to irrigation demands
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Flooding is no longer a problem due to……
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A series of dams to control flooding, create recreation, and provide
irrigation water
On June 6, 1976 the Teton Dam near
Rexburg, Idaho failed during its initial filling. At 350 feet high, it was the largest dam break in US history and the damages reached $1
billion.
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After the breach
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This water has increased the value of the mixed volcanic-sediment soil to…….
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Idaho Agriculture
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Climate
• Mild and pleasant• Summers sunny and warm with few cloudy
days; winters cool and dry• Precipitation averages 10 inches (25cm);
semi-arid (quick thundershowers)• Summer temp.= 81degrees (105 max)
with cool evenings• Winter temp.=13-35 degrees with snow in
the mountains surrounding
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From space
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End of the road!