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palygorskite, also known by the informal name 'mountain leather', forms in a variety of environments, such as hydrothermal deposits, soils and as slicken sides on fault planes. Although it can form quite large crystals it more commonly occurs as leathery-looking masses.
Vivian (1887) reported the presence of 'mountain leather' associated with the hematite deposits of South Wales, but stated no specific locality details. North (1916) stated that mountain leather had been found at Mwyndy Mines, near Llantrisant, South Wales and Criddle & Symes (1977) subsequently recorded palygorskite from Ty-coch.
Mineralogical Magazine, 41, 85-90.