Twin Cone, Mount Edziza Provincial Park
#46 among attractions in Mount Edziza Provincial Park
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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 miNWVolcanoSidas 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 miWVolcanoEve 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 miSWVolcanoPillow 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 miSWVolcanoWilliams 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 miSWVolcanoGlacier 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 miSWVolcanoStorm 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 miSWVolcanoSleet 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 miSEVolcanoKlastline 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 miSWVolcanoCinder 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 miSWVolcanoMoraine 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 miWVolcanoTriplex 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.