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Power CountyPower County straddles the Snake River west of Pocatello. It has fresh basalt lava of the Great Rift and Kings Bowl in its northwestern corner. The central part of the county is agricultural land irrigated by the Snake River. Here 70,000 years ago the ancestral American Falls lake existed. South of the Snake River, farming occurs in Rockland and Arbon Valleys, south of the Snake River. Massacre Rocks along the Snake River is a Miocene basalt eruptive center. The Oregon Trail runs through it. See description in Rocks, Rails and Trails. The Bannock, Deep Creek and Sublett Ranges, south of the Snake River, contain Paleozoic sedimentary rocks in the hanging wall of the Putnam thrust fault. See geology description in Rocks, Rails and Trails. P.K. Link, 10/02 Additional ReadingRocks Rails and Trails: pages Introduction to the Geology of South & East Idaho Introduction to Geologic Diagrams Geologic cross sections Relations between Geology, Topography and Drainage Systems in Idaho Drainage and mountain range map for eastern Idaho Table of Geologic Events in Southern Idaho The Snake River Plain-Yellowstone Hot Spot and its Effect on Drainage Patterns Challis Volcanic Group & Intrusive Rocks Lake Bonneville and its Flood Disposal of Wastes at the Idaho National Engineering & Environmental Laboratory References on Idaho Geology Section 3, History of Eastern Idaho Section 3, Chapter 8 -"Famous Potatoes" Agriculture & Irrigation Section 6, Chapter 21 - American Falls Area Massacre Rocks Section 7, Chapter 22 - Silent City of Rocks & Burley Area |
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Click here to see a correlation of geologic units, and the associated time scale. Click here for a printable version of this msp.
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