#ThinSectionThursday Skeletal olivine phenocrysts ๐ ๐ฆ in quenched, fine-grained, black magnesium-rich picrite, forming thin dykes and veins in peridotites of the Central Intrusion in Rum. This magma had around 20%MgO, and was around 1500 degrees C when intruded - MUCH hotter than normal basalt magmas. Hunterian museum specimen: http://collections.gla.ac.uk/#/details/ecatalogue/32999











