The Rum layered intrusion is located in Scotland, on the island of Rùm (Inner Hebrides).
It is a mass of intrusive rock, of mafic-ultramafic composition,[1] the remains of the eroded, solidified magma chamber of an extinct volcano[2] that was active during the Palaeogene Period.
[3] It is associated with the nearby Skye intrusion and Skye, Mull and Eigg lavas.
[4] It was emplaced 60 million years ago above the Iceland hotspot.
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