Abstract
ON the sea-coast at Portraine, Co. Dublin, there is an apparent thickness of over 700 feet of conglomeratic rocks, which have hitherto been regarded and described as of volcanic origin, contemporaneous with the Lower Silurian strata and associated felspathic igneous rocks.
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MCHENRY, A. Crush-Conglomerates in Ireland. Nature 53, 414 (1896). https://doi.org/10.1038/053414a0
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DOI: https://doi.org/10.1038/053414a0
