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The channel-fill deposits at Mount Benkert appear to represent fluviatile sedimentary rocks derived from hyaloclastites; the huge channel forms that compose the main outcrop, the associated mesoscopic internal bedding fo
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Document Date: 2011-05-06 22:21:22
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The channel-fill deposits at Mount Benkert appear to represent fluviatile sedimentary rocks derived from hyaloclastites; the huge channel forms that compose the main outcrop, the associated mesoscopic internal bedding fo