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An isolated hill capped by Ogallala Formation conglomerates rises above a quarry in the Smoky Hill Chalk.
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A small quarry and roadcut exposure of the Smoky Hill Chalk member.
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A quarry in Smoky Hill chalk.
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A cliff of Fort Hays Limestone caps the cutbank of this tributary of the Solomon River.
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Tertiary Ogallala Formation conglomerates form a resistant cap that holds up the soft, thin bedded Cretaceous Niobrara Formation, Smoky Hill member chalk deposits below.
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