1977
DOI: 10.3133/ofr77397
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Ground-water resources in the Libby area, northwestern Montana

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“…Lake-bottom sediments in a bluff east of Libby are 90 m thick, almost massive, without distinct laminae, and they contain no pebbles, boulders, or fossils (Alden 1953). The sediments underlying Libby Valley are about 30 m thick, as estimated from Boettcher and Wilke (1978). These combined observations suggest about 120 m total thickness of lakebottom sediments in the Libby area.…”
Section: Bull Lake Spillwaymentioning
confidence: 80%
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“…Lake-bottom sediments in a bluff east of Libby are 90 m thick, almost massive, without distinct laminae, and they contain no pebbles, boulders, or fossils (Alden 1953). The sediments underlying Libby Valley are about 30 m thick, as estimated from Boettcher and Wilke (1978). These combined observations suggest about 120 m total thickness of lakebottom sediments in the Libby area.…”
Section: Bull Lake Spillwaymentioning
confidence: 80%
“…Harrison and Cressman (1993) mapped the distribution of glacial deposits in northwest Montana at a scale of 1:125,000 as part of their study of the Libby Thrust Belt, but they did not discuss the glacial deposits in detail. Boettcher and Wilke (1978) mapped the lake-bottom deposits in the Libby area at a scale of 1:48,000 as part of a ground-water investigation. Two geologic maps in the Bonners Ferry, Idaho area provide insight to the history of Glacial Lake Kootenai: (1) a 1:24,000-scale map of the Elmira Quadrangle (Lewis et al 2007), and (2) a 1:100,000-scale map of the Bonners Ferry quadrangle (Miller and Burmester 2003).…”
Section: Study Methodsmentioning
confidence: 99%
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