Twin Cone, Mount Edziza Provincial Park
#46 among attractions in Mount Edziza Provincial Park

Facts and practical information
Twin Cone is a cinder cone in northern British Columbia, Canada. It is thought to have last erupted in the Holocene period. ()
Mount Edziza Provincial Park Canada
Twin Cone – popular in the area (distance from the attraction)
Nearby attractions include: Sidas Cone, Eve Cone, Pillow Ridge, Williams Cone.
5.5 miNW
VolcanoSidas Cone, Mount Edziza Provincial Park
140 min walk • Sidas Cone is a cinder cone on the Big Raven Plateau at the northern end of Mount Edziza Provincial Park in British Columbia, Canada.
5.4 miW
VolcanoEve Cone, Mount Edziza Provincial Park
139 min walk • Eve Cone is a well-preserved black cinder cone on the Big Raven Plateau, British Columbia, Canada. It is one of the 30 cinder cones on the flanks of the massive shield volcano of Mount Edziza that formed in the year 700, making it one of the most recent eruptions on the Big Raven Plateau and in Canada.
5.3 miSW
VolcanoPillow Ridge, Mount Edziza Provincial Park
135 min walk • 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.
2.9 miSW
VolcanoWilliams Cone, Mount Edziza Provincial Park
74 min walk • Williams Cone is a satellite cone of Mount Edziza, located 36 km east of Telegraph Creek. It lies just off the northern edge of the Tencho Icefield and is one of the many postglacial cinder cones that lie on the Mount Edziza volcanic complex.
2.8 miSW
VolcanoGlacier Dome, Mount Edziza Provincial Park
71 min walk • Glacier Dome is a lava dome in northwestern British Columbia, Canada, located near Mount Edziza in Mount Edziza Provincial Park. It last erupted during the Pleistocene epoch.
4.2 miSW
VolcanoStorm Cone, Mount Edziza Provincial Park
108 min walk • Storm Cone is a cinder cone in northern British Columbia, Canada. It is thought to have last erupted in the Holocene period and lies on the Desolation lava field which is part of the Mount Edziza volcanic complex.
1.6 miSW
VolcanoSleet Cone, Mount Edziza Provincial Park
40 min walk • Sleet Cone is a cinder cone in northern British Columbia, Canada. It lies in the Desolation Lava Field and is thought to have last erupted in the Holocene period and is part of the Mount Edziza volcanic complex.
1.8 miSE
VolcanoKlastline Cone, Mount Edziza Provincial Park
46 min walk • Klastline Cone is a cinder cone in northwestern British Columbia, Canada, located near Mount Edziza in Mount Edziza Provincial Park. It last erupted during the Pleistocene epoch.
3.8 miSW
VolcanoCinder Cliff, Mount Edziza Provincial Park
96 min walk • Cinder Cliff is a cinder cone in northern British Columbia, Canada. It is thought to have last erupted during the Holocene period and is part of the Mount Edziza volcanic complex.
3.9 miSW
VolcanoMoraine Cone, Mount Edziza Provincial Park
100 min walk • Moraine Cone is a cinder cone in northern British Columbia, Canada. It is thought to have last erupted in the Holocene period and is part of the Mount Edziza volcanic complex.
3.3 miW
VolcanoTriplex Cone, Mount Edziza Provincial Park
85 min walk • Triplex Cone is a cinder cone in northern British Columbia, Canada. It is thought to have last erupted in the Holocene period.