|
|||||||||||||||||||||||||||||||||||||||
Ada CountyAda County, Idaho's most populous county, has relatively simple geology, compared to some much more sparsely populated areas. On the northeast is the Cretaceous Idaho batholith, home to Bogus Basin ski area. The batholith forms a mountainous area uplifted on south-dipping normal faults which form the northeast margin of the western Snake River Plain. In the Boise foothills are a complex assemblage of sandstones and lake beds formed on the edges and within Lake Idaho in the last 10 million years. The Table Rock Sandstone, quarried since the mid 1800s belongs to these strata. The city of Boise lies in the alluvial valley of the Boise River, which joins the Snake River on the Oregon border, south of Nyssa. A series of northwest striking normal faults cuts Ada County, part of the western Snake River Plain graben. On the south are extensive Quaternary gravel deposits that overlie Quaternary basalt. Recent cinder cones line the Snake River near Swan Falls. P.K. Link, 9/02 Additional Reading
|
Click here to see a correlation of geologic units, and the associated time scale. Click here for a printable version of this map. Click here for a discussion of the Geology of the Boise Valley (PDF)
|