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.
Sleet is a regionally variant term for some meteorological phenomena: Ice pellets, pellets of ice composed of frozen raindrops or refrozen melted snowflakes (United States) Rain and snow mixed, snow that partially melts as it falls (United Kingdom,...
The Desolation Lava Field (DLF) is a volcanic field at Mount Edziza in British Columbia, Canada. It reaches an elevation of 2,165 metres (7,103 feet) on the Big Raven Plateau, but decreases to 820 m (2,690 ft) at Buckley Lake and 670 m (2,200 ft) in...
Eve Cone, also referred to as Eve's Cone, is a cinder cone in Cassiar Land District of northwestern British Columbia, Canada. It has an elevation of 1,740 metres (5,710 feet) and is one of several volcanic cones in the Desolation Lava Field....
Williams Cone is a cinder cone on the northeastern flank of Mount Edziza in Cassiar Land District of northwestern British Columbia, Canada. It has an elevation of 2,100 metres (6,900 feet) and is one of several volcanic cones in the Desolation Lava...
Tseax Cone ( SEE-aks) is a small volcano in the Nass Ranges of the Hazelton Mountains in northwestern British Columbia, Canada. It has an elevation of 609 metres (1,998 feet) and lies within an east–west valley through which a tributary of the Tseax...
The Triplex Cones are a group of three cinder cones in northern British Columbia, Canada. They are thought to have last erupted during the Holocene epoch.
A list of cinder cones is shown below. The list contains either individual cinder cones, or a group of cinder cones with no other volcanic features.
Tennena Cone, alternatively Icebridge Cone, is a small volcanic cone in Cassiar Land District of northwestern British Columbia, Canada. It has an elevation of 2,390 metres (7,840 feet) and lies on the upper western flank of Ice Peak, the prominent...
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.