Mount Noel is a Miocene volcanic complex in the Chilcotin Group in British Columbia, Canada, located 7 km (4 mi) southwest of Bralorne and north of a tributary of Noel Creek.

It is 150 km (93 mi) east of the Garibaldi Volcanic Belt and is made up of flat-lying, columnar-jointed basalt flows along with debris flows and minor pyroclastic rocks.

Mount Noel is thought to have formed as a result of back-arc extension behind the Cascadia subduction zone.

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