Tertiary Igneous Rocks of Northeastern Cache Valley, Idaho
The tuffs and limestones of the Tertiary Salt Lake Formation in northeastern Cache Valley, Franklin County, Idaho, are intruded by basic and intermediate igneous dikes and sills. The Tertiary intrusives are exposed in an area 10 miles long and 2 miles wide between Bear River and Maple Creek in the f...
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| Format: | Others |
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DigitalCommons@USU
1972
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| Online Access: | https://digitalcommons.usu.edu/etd/2108 https://digitalcommons.usu.edu/cgi/viewcontent.cgi?article=3113&context=etd |