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Jefferson CountyJefferson County is entirely on the Snake River Plain, mainly north and west of the Snake River where it takes its horseshoe bend from flowing northwest to flowing south. The bend, likely controlled by the topographic high of the Menan Buttes in adjacent Madison County, allows Jefferson County to have large areas of rich irrigated agriculture in the south and east near Rigby and Market Lake. The northern and western parts of Jefferson County are Quaternary basalt lava, with the sedimentary basin of Mud Lake in the northwest corner. Around Mud Lake is another area of irrigated farming, with soils formed from lake beds of Lake Terreton, which occupied this area in much of Quaternary time. The northeast corner of the INEEL occupies the western edge of Jefferson County. See discussion of geology of the Yellowstone-Snake River Plain volcanic system in Rocks, Rails and Trails, Topographic Development of Idaho maps, and Hughes et al. and Embree et al. papers in Geology of Eastern Idaho. 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 References on Idaho Geology Section 3, History of Eastern Idaho Section 3, Chapter 8 -"Famous Potatoes" Agriculture & Irrigation The Teton Dam Disaster, June 5, 1976 |
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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 map.
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