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Idaho Geology. The Plateau Regions. Parts of the greater volcanic Columbia Plateau of Washington. The Clearwater Plateau is the second region of Idaho formed like the Columbia Plateau. Clearwater Plateau. Area drained by the Clearwater River, including the Palouse Hills. - PowerPoint PPT Presentation
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Idaho Geology
The Plateau Regions
Parts of the greater volcanic Columbia Plateau of Washington
The Clearwater Plateau is the second region of Idaho formed like the Columbia Plateau
Clearwater Plateau
Area drained by the Clearwater River, including the Palouse Hills
Tall rolling hills and gently sloping prairies
A lot of it is ideal for farming for many reasons
Clarkston-Lewiston
Moscow
Post Falls
Snake River
Clearwater River
WA ID
Potlatch River
Dworshak
Clearwater and tributaries like the Potlatch
Snake River on border
Clearwater joining from the east
The Clearwater joins the Snake at the western edge of Idaho
Lowest point in Idaho – 738 feet
at Lewiston
Originally formed by basalt flows
Granite peaks – Cottonwood Butte and Craig Mt.
Exposed as hills uplifted and basaltic lava eroded away
Much of the region formed by wind and water erosion. Covered by a thick layer of rich topsoil of eroded volcanic
material mixed with clay-like glacial sediment blown in from Puget Sound (loess). This makes up the Palouse Hills.
Wheat farms of the Palouse with rich water-holding soil called loess
Clearwater Climate
• Fairly mild
• Summer temp. averages 89 degrees with cool evenings
• Winter temp. averages 26-31 degrees
• Precipitation 20+ inches (25-55 in higher elevations)
• 4-6 month growing season! (the Banana Belt)
Irrigation not needed because of clayey glacial loess
• The grasslands originally covering much of the region have now been generally replaced by domesticated grasses (wheat, oats, barley) and legumes (alfalfa, peas, lentils)
• Crop rotation and fallow fields help offset the loss of nutrients and water
Palouse
Camas Prairie
• At higher elevations through the plateau and as the plateau in the east rises to meet the Rockies, evergreen forests are found. These are mainly………
Pine forests
Owyhee-Bruneau Plateau
3rd Volcanic region in Idaho
Rolling hills and
mountains; dry and sparsely
populated
Mountains
Jump Creek Hills
Poison Creek Hills
French John Hills
Owyhee Mts.
Rivers
Owyhee River
Bruneau River
Jarbridge River
Salmon Falls Creek
Bruneau Gorge
ColumbiaPlateau
lava flows included Owyhee-Bruneau
Lava layers from the many preceding
fissure flows
Owyhee-Bruneau becoming a plateau through uplifting forces. This is the main difference
between it and the Snake River Plain
2000-5000 feet above the SRP;
some peaks rising to 8000 feet
WA, OR, CA
ID
Why is it so dry?
Rainshadow Effect
Climate
• Extreme and semi-arid
• Precipitation 13-20 inches
• Summer average temp. = 88 degrees
• Winter average = 12 degrees
Southern Idaho Vegetation
O-B Summary• Hostile environment and
climate
• Ranching is main industry
• Low population density (more cows and sheep than people)
• Few towns
• Murphy is the county seat of Owyhee County (pop. 600)