Murray Monolith is a detached part of Torlyn Mountain in Mac.Robertson Land, Antarctica. It is a steep massif of metasedimentary gneiss and granitic origin, with the adjacent coastline consisting of 40 m high ice cliffs. The monolith is dome-shaped with steep sides, rising to a seaward summit of 339 m and an inland summit of 363 m at Torlyn Mountain.[1]