Pillow Ridge
Highest point
Elevation	2,400 m (7,900 ft)
Coordinates	57°45′34″N 130°39′6″W / 57.75944°N 130.65167°W / 57.75944; -130.65167
Geography
Location	British Columbia, Canada
District	Cassiar Land District
Parent range	Tahltan Highland
Topo map	NTS 104G15 Buckley Lake
Geology
Rock age	Pleistocene
Mountain type	Subglacial mound
Rock type	Pillow Formation alkali basalt
Volcanic region	Northern Cordilleran Province
Last eruption	Pleistocene

Pillow Ridge is a ridge of the Tahltan Highland in northern British Columbia, Canada, located southeast of Telegraph Creek. It extends northwest from Mount Edziza in Mount Edziza Provincial Park.^[1]

As its name suggests, Pillow Ridge was named on January 2, 1980 by the Geological Survey of Canada for the classic exposures of subaqueous pillow lava that form the ridge.^[1]

Pillow Ridge is a volcanic feature associated with the Mount Edziza volcanic complex which in turn form part of the Northern Cordilleran Volcanic Province. It is a subglacial mound that formed in the Pleistocene period when this area was buried beneath glacial ice during the last glacial period.^[2]

• List of volcanoes in Canada
• List of Northern Cordilleran volcanoes
• Volcanism of Canada
• Volcanism of Western Canada

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