W. T. Harry; Basement Carboniferous in Upper Teesdale, N. Yorks. Geological Magazine ; 87 (4): 297–299. doi:
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Describes the conglomerate, consisting of andesite, rhyolite, vein quartz, and shale pebbles, that occurs at the base of the Carboniferous unconformably overlying Silurian shales, as exposed at Upper Teesdale, northern Yorkshire, England.
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