The Raspberry Formation is a stratigraphic unit of Miocene age in northwestern British Columbia, Canada.

Rocks of the Stikinia terrane underlie the Raspberry Formation.

[1] The Raspberry Formation consists of flat-lying alkali basalt and hawaiite flows.

These flows are rusty brown and are interbedded with reddish-brown to yellow or orange scoria.

[1] The Raspberry Formation represents three overlapping Miocene shield volcanoes.