| Bridge River Cones | |
|---|---|
   | |
| Highest point | |
| Elevation | 2,500 m (8,200 ft) |
| Coordinates | 50°51′30″N 123°24′00″W / 50.85833°N 123.40000°W |
| Geography | |
| Location | Upper Bridge River, British Columbia, Canada |
| Parent range | Pacific Ranges |
| Geology | |
| Age of rock | Holocene |
| Mountain type | Volcanic field |
| Volcanic arc/belt | Canadian Cascade Arc Garibaldi Volcanic Belt |
| Last eruption | Unknown, possibly younger than 500[1] |
The Bridge River Cones, sometimes referred to as the Lillooet Cones and Salal Creek Cones, is the name given to a volcanic field located on the north flank of the upper Bridge River, about 40 km (25 mi) west of the town of Gold Bridge. The cones are in the lee of the Lillooet Icecap and sit astride a group of passes between the Bridge River, which flows W-E to their south, and the Lord River, which flows north to the Taseko Lakes in the Chilcotin District.