The long-term failure characteristics of overconsolidated clay shales in the Mount Diablo region

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Relatively shallow slides at inclinations comparable to the residual friction angle of the existing clay shales are occurring within Lime Ridge. A stability analyses was preformed on three potential slides to determine some of the failure mechanisms commonly associated with overconsolidated clay shales.

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Thesis Number: 2580.
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University of Nevada, Reno

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