List of volcanoes in Canada
Encyclopedia

Alberta
Alberta
Alberta is a province of Canada. It had an estimated population of 3.7 million in 2010 making it the most populous of Canada's three prairie provinces...

Name Elevation Location Last eruption
metres feet Coordinates
BH225 pipe  - - - Late Cretaceous
Late Cretaceous
The Late Cretaceous is the younger of two epochs into which the Cretaceous period is divided in the geologic timescale. Rock strata from this epoch form the Upper Cretaceous series...

BH229 pipe  - - - Late Cretaceous
Late Cretaceous
The Late Cretaceous is the younger of two epochs into which the Cretaceous period is divided in the geologic timescale. Rock strata from this epoch form the Upper Cretaceous series...

BH230 pipe  - - - Paleocene
Paleocene
The Paleocene or Palaeocene, the "early recent", is a geologic epoch that lasted from about . It is the first epoch of the Palaeogene Period in the modern Cenozoic Era...

BH155 pipe  - - - -
BM2 pipe  - - - Paleocene
Paleocene
The Paleocene or Palaeocene, the "early recent", is a geologic epoch that lasted from about . It is the first epoch of the Palaeogene Period in the modern Cenozoic Era...

BM3 pipe  - - - -
BM16 pipe  - - - -
Dragon pipe
Dragon pipe
The Dragon pipe is a diatreme associated with the Birch Mountains kimberlite field in northern Alberta, Canada. It is thought to have formed about 75 million years ago when this part of Alberta was volcanically active during the Late Cretaceous period....

 
- - - Late Cretaceous
Late Cretaceous
The Late Cretaceous is the younger of two epochs into which the Cretaceous period is divided in the geologic timescale. Rock strata from this epoch form the Upper Cretaceous series...

Kendu pipe
Kendu pipe
The Kendu pipe is a diatreme associated with the Birch Mountains kimberlite field in northern Alberta, Canada. It is thought to have formed about 75 million years ago when this part of Alberta was volcanically active during the Late Cretaceous period....

 
- - - Late Cretaceous
Late Cretaceous
The Late Cretaceous is the younger of two epochs into which the Cretaceous period is divided in the geologic timescale. Rock strata from this epoch form the Upper Cretaceous series...

K1A pipe  - - - Paleocene
Paleocene
The Paleocene or Palaeocene, the "early recent", is a geologic epoch that lasted from about . It is the first epoch of the Palaeogene Period in the modern Cenozoic Era...

K1B pipe  - - - Paleocene
Paleocene
The Paleocene or Palaeocene, the "early recent", is a geologic epoch that lasted from about . It is the first epoch of the Palaeogene Period in the modern Cenozoic Era...

K14A pipe  - - - Late Cretaceous
Late Cretaceous
The Late Cretaceous is the younger of two epochs into which the Cretaceous period is divided in the geologic timescale. Rock strata from this epoch form the Upper Cretaceous series...

K14B pipe  - - - Late Cretaceous
Late Cretaceous
The Late Cretaceous is the younger of two epochs into which the Cretaceous period is divided in the geologic timescale. Rock strata from this epoch form the Upper Cretaceous series...

K14C pipe  - - - Late Cretaceous
Late Cretaceous
The Late Cretaceous is the younger of two epochs into which the Cretaceous period is divided in the geologic timescale. Rock strata from this epoch form the Upper Cretaceous series...

K160 pipe  - - - -
K2 pipe  - - - Paleocene
Paleocene
The Paleocene or Palaeocene, the "early recent", is a geologic epoch that lasted from about . It is the first epoch of the Palaeogene Period in the modern Cenozoic Era...

K251 pipe  - - - Late Cretaceous
Late Cretaceous
The Late Cretaceous is the younger of two epochs into which the Cretaceous period is divided in the geologic timescale. Rock strata from this epoch form the Upper Cretaceous series...

K252 pipe
K252 pipe
K252 pipe is a diamondiferous diatreme in the Buffalo Head Hills kimberlite field of Northern Alberta, Canada. It is thought to have formed about 85 million years ago when this part of Alberta was volcanically active during the Late Cretaceous period...

 
- - - Late Cretaceous
Late Cretaceous
The Late Cretaceous is the younger of two epochs into which the Cretaceous period is divided in the geologic timescale. Rock strata from this epoch form the Upper Cretaceous series...

K296 pipe  - - - -
K3 pipe  - - - Paleocene
Paleocene
The Paleocene or Palaeocene, the "early recent", is a geologic epoch that lasted from about . It is the first epoch of the Palaeogene Period in the modern Cenozoic Era...

K32 pipe  - - - -
K300 pipe  - - - -
K4A pipe  - - - Late Cretaceous
Late Cretaceous
The Late Cretaceous is the younger of two epochs into which the Cretaceous period is divided in the geologic timescale. Rock strata from this epoch form the Upper Cretaceous series...

K4B pipe  - - - Late Cretaceous
Late Cretaceous
The Late Cretaceous is the younger of two epochs into which the Cretaceous period is divided in the geologic timescale. Rock strata from this epoch form the Upper Cretaceous series...

K4C pipe  - - - Late Cretaceous
Late Cretaceous
The Late Cretaceous is the younger of two epochs into which the Cretaceous period is divided in the geologic timescale. Rock strata from this epoch form the Upper Cretaceous series...

K5B pipe  - - - Late Cretaceous
Late Cretaceous
The Late Cretaceous is the younger of two epochs into which the Cretaceous period is divided in the geologic timescale. Rock strata from this epoch form the Upper Cretaceous series...

K5A pipe  - - - Late Cretaceous
Late Cretaceous
The Late Cretaceous is the younger of two epochs into which the Cretaceous period is divided in the geologic timescale. Rock strata from this epoch form the Upper Cretaceous series...

K6 pipe
K6 pipe
K6 pipe is a diamondiferous diatreme in the Buffalo Head Hills kimberlite field of Northern Alberta, Canada. It is thought to have formed about 85 million years ago when is part of Alberta was volcanically active during the Late Cretaceous period...

 
- - - Late Cretaceous
Late Cretaceous
The Late Cretaceous is the younger of two epochs into which the Cretaceous period is divided in the geologic timescale. Rock strata from this epoch form the Upper Cretaceous series...

K7A pipe  - - - Late Cretaceous
Late Cretaceous
The Late Cretaceous is the younger of two epochs into which the Cretaceous period is divided in the geologic timescale. Rock strata from this epoch form the Upper Cretaceous series...

K7B pipe  - - - Late Cretaceous
Late Cretaceous
The Late Cretaceous is the younger of two epochs into which the Cretaceous period is divided in the geologic timescale. Rock strata from this epoch form the Upper Cretaceous series...

K7C pipe  - - - Late Cretaceous
Late Cretaceous
The Late Cretaceous is the younger of two epochs into which the Cretaceous period is divided in the geologic timescale. Rock strata from this epoch form the Upper Cretaceous series...

K8 pipe  - - - -
K10 pipe  - - - -
K11 pipe  - - - Late Cretaceous
Late Cretaceous
The Late Cretaceous is the younger of two epochs into which the Cretaceous period is divided in the geologic timescale. Rock strata from this epoch form the Upper Cretaceous series...

K15 pipe  - - - -
K19 pipe
K19 pipe
K19 pipe is a diatreme in the southwestern part of the Buffalo Head Hills kimberlite field in Northern Alberta, Canada. It is thought to have formed about 60 million years ago, making it one of the youngest volcanic formations in the Buffalo Head Hills kimberlite field and in Alberta...

 
- - - Paleocene
Paleocene
The Paleocene or Palaeocene, the "early recent", is a geologic epoch that lasted from about . It is the first epoch of the Palaeogene Period in the modern Cenozoic Era...

K91 pipe  - - - Late Cretaceous
Late Cretaceous
The Late Cretaceous is the younger of two epochs into which the Cretaceous period is divided in the geologic timescale. Rock strata from this epoch form the Upper Cretaceous series...

K92 pipe  - - - -
K93 pipe  - - - -
K95 pipe  - - - -
Legend pipe
Legend pipe
The Legend pipe is a diatreme associated with the Birch Mountains kimberlite field in northern Alberta, Canada. It is thought to have formed about 75 million years ago during the Late Cretaceous period.-See also:*Volcanism of Canada...

 
- - - Late Cretaceous
Late Cretaceous
The Late Cretaceous is the younger of two epochs into which the Cretaceous period is divided in the geologic timescale. Rock strata from this epoch form the Upper Cretaceous series...

LL8 pipe  - - - Late Cretaceous
Late Cretaceous
The Late Cretaceous is the younger of two epochs into which the Cretaceous period is divided in the geologic timescale. Rock strata from this epoch form the Upper Cretaceous series...

Phoenix pipe
Phoenix pipe
The Phoenix pipe is a diatreme associated with the Birch Mountains kimberlite field in northern Alberta, Canada. It is thought to have formed about 75 million years ago when this part of Alberta was volcanically active during the Late Cretaceous period....

 
- - - Late Cretaceous
Late Cretaceous
The Late Cretaceous is the younger of two epochs into which the Cretaceous period is divided in the geologic timescale. Rock strata from this epoch form the Upper Cretaceous series...

Valkyrie pipe
Valkyrie pipe
The Valkyrie pipe is a diatreme in northern Alberta, Canada. It is associated with a group of diatremes called the Birch Mountains kimberlite field which is thought to have formed about 75 million years ago when this part of Alberta was volcanically active during the Late Cretaceous period.-See...

 
- - - Late Cretaceous
Late Cretaceous
The Late Cretaceous is the younger of two epochs into which the Cretaceous period is divided in the geologic timescale. Rock strata from this epoch form the Upper Cretaceous series...

WP pipe  - - - Late Cretaceous
Late Cretaceous
The Late Cretaceous is the younger of two epochs into which the Cretaceous period is divided in the geologic timescale. Rock strata from this epoch form the Upper Cretaceous series...

Xena pipe
Xena pipe
The Xena pipe is a diatreme associated with the Birch Mountains kimberlite field in northern Alberta, Canada. It is thought to have formed about 75 million years ago when this part of Alberta was volcanically active during the Late Cretaceous period.-See also:...

 
- - - Late Cretaceous
Late Cretaceous
The Late Cretaceous is the younger of two epochs into which the Cretaceous period is divided in the geologic timescale. Rock strata from this epoch form the Upper Cretaceous series...


British Columbia
British Columbia
British Columbia is the westernmost of Canada's provinces and is known for its natural beauty, as reflected in its Latin motto, Splendor sine occasu . Its name was chosen by Queen Victoria in 1858...

Name Elevation Location Last eruption
metres feet Coordinates
Anahim Peak
Anahim Peak
Anahim Peak, sometimes mistakenly called Anaheim, is a volcanic cone in the Anahim Volcanic Belt in British Columbia, Canada, located northwest of Anahim Lake and east of Tsitsutl Peak. It was formed when the North American Plate moved over a hotspot, similar to the one feeding the Hawaiian...

 
1897 6224 52.44°N 125.41°W Miocene
Armadillo Peak
Armadillo Peak
Armadillo Peak is a 7.5 million year old caldera, located about 3 km north of Bourgeaux Creek and northeast of Raspberry Pass, British Columbia, Canada. It is south of Mount Edziza and is overlapped by the Ice Peak central volcano, which was formed during the early Pleistocene. Its caldera is...

 
2210 7251 57.53°N 130.55°W Miocene
Ash Mountain
Ash Mountain (British Columbia)
Ash Mountain is the highest summit in the Tuya Range of the Stikine Ranges in northcentral British Columbia, Canada, located immediately north of High Tuya Lake at the north end of Tuya Mountains Provincial Park. It is one of the six tuyas clustered close to Tuya Lake...

 
2125 6550 59.27°N 130.05°W Pleistocene
The Ash Pit
The Ash Pit
The Ash Pit is a volcanic crater, located in the Spectrum Range in British Columbia, Canada. It is Holocene in age and is considered the youngest feature in the Spectrum Range volcanic complex...

 
1580 5184 57.45°N 130.78°W Holocene
Atwell Peak
Atwell Peak
Atwell Peak is a dramatic pyramid shaped volcanic peak located at the southern edge of Mount Garibaldi, British Columbia, Canada. Atwell Peak was formed during an initial period of volcanism 0.51-0.22 million years ago and was the source of many pyroclastic flows during Garibaldi's development....

 
2655 8711 49.50°N 123.33°W Pleistocene
Bennett Lake Volcanic Complex
Bennett Lake Volcanic Complex
The Bennett Lake Volcanic Complex is a huge 50 million year old extinct caldera complex that spans across the BC-Yukon border in Canada. The caldera complex is surrounded by granitic rocks containing pendants....

 
1500 4900 60.3°N 134.52°W Eocene
Black Dome Mountain
Black Dome Mountain
Black Dome Mountain is the most northerly summit of the Camelsfoot Range, which lies along the west side of the Fraser River, north of Lillooet, British Columbia, Canada...

 
2252 7388 51.19°N 122.29°W Pliocene
Black Tusk
Black Tusk
Black Tusk is a remarkably abrupt pinnacle of volcanic rock located in Garibaldi Provincial Park of British Columbia, Canada. At above sea level, the upper spire is visible from a great distance in all directions. It is particularly noticeable from the Sea-to-Sky Highway just south of Whistler,...

 
2319 7608 49.97°N 123.04°W Pleistocene
Blackfoot diatreme
Blackfoot diatreme
The Blackfoot diatreme is a diatreme in southeastern British Columbia, Canada, located northeast of Cranbrook. It is in length with a maximum width of . The diatreme is elongate in shape, and outcrops east of Blackfoot Creek.-See also:*Volcanism in Canada...

 
- - 49.58°N 115.17°W -
Big Timothy Mountain
Big Timothy Mountain
Big Timothy Mountain, formerly called Boss Mountain and Takomkane Mountain, is a cinder cone in central British Columbia, Canada, located west of Hendrix Lake and southwest of Mount Perseus.-See also:*List of volcanoes in Canada...

 
2455 8054 52.12°N 120.91°W Pleistocene
Mount Boucherie
Mount Boucherie
Mount Boucherie is a mountain located in West Kelowna on the west shore of Okanagan Lake, British Columbia, Canada, opposite the city of Kelowna. It is the remnants of a former stratovolcano created nearly 60 million years ago. Between four and six different glacial periods over the past 50...

 
758 2487 49.51°N 119.34°W Paleocene
Bowie Seamount
Bowie Seamount
Bowie Seamount is a large submarine volcano in the northeastern Pacific Ocean, located west of Haida Gwaii, British Columbia, Canada.The seamount is named after William Bowie of the Coast & Geodetic Survey....

 
-24 -79 53.3°N 135.63°W 18000 years ago
Mount Brew
Mount Brew (Cheakamus River)
Mount Brew is a rounded mountain in southwestern British Columbia, Canada, located southwest of Whistler in the Pacific Ranges of the Coast Mountains. A public cabin run by the Varsity Outdoor Club, Brew Hut, is located near the summit...

 
1757 5764 50.4°N 123.19°W Pleistocene
Bridge River Cones
Bridge River Cones
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 west of the town of Gold Bridge...

 
2500 8202 50.80°N 123.40°W Holocene
Buck Hill
Buck Hill (British Columbia)
Buck Hill is a hill in east-central British Columbia, Canada, located north of Clearwater. It rises from the west slope of Trophy Mountain. Buck Hill is just outside the boundary of Wells Gray Provincial Park.-Geology:...

 
1585 5200 51.48°N 119.59°W Pleistocene
Cache Hill
Cache Hill
Cache Hill is a cinder cone in northern British Columbia, Canada. It is thought to have last erupted in the Holocene period. Once used as an airdrop for food and supplies by the Geophysical Survey of Canada, hence its name, it is located north of Raspberry Pass in Mount Edziza Provincial Park.-See...

 
2110 6923 57.53°N 130.67°W Holocene
Mount Callaghan
Mount Callaghan
Mount Callaghan is a volcanic peak located east of the headwaters of the Squamish River, just northeast of the Powder Mountain Icefield and just south of the Pemberton Icefield in the Sea to Sky Country of southwestern British Columbia, Canada, about 20 km directly west of the Resort...

 
2409 7909 50.13°N 123.15°W -
Camp Hill
Camp Hill (British Columbia)
Camp Hill is a cinder cone in northern British Columbia, Canada. It is thought to have last erupted in the Holocene period.-See also:*List of volcanoes in Canada*List of Northern Cordilleran volcanoes*Volcanism of Canada*Volcanism of Western Canada...

 
1880 6168 57.58°N 130.78°W Holocene
Capricorn Mountain
Capricorn Mountain
Capricorn Mountain is one of the several volcanic peaks of the Mount Meager massif in southwestern British Columbia, Canada. The slopes of Capricorn Mountain appear to be more gentle than other volcanic peaks of the massif...

 
2551 8369 50.62°N 123.52°W Pleistocene
Caribou Tuya
Caribou Tuya
Caribou Tuya is a basaltic subglacial mound in far northwestern British Columbia that began eruptive activity under glacial ice during the Fraser glaciation . Like Ash Mountain and South Tuya, sections of the subglacial mound reveal a consistent stratigraphic progression from pillow lavas to...

 
1770 5807 59.24°N 130.56°W Pleistocene
Cartoona Peak
Cartoona Peak
Cartoona Peak, also unofficially called Cartoona Ridge, is a volcanic peak in northern British Columbia, Canada, located just southeast of Coffee Crater in Mount Edziza Provincial Park.-See also:*List of volcanoes in Canada...

 
2305 7562 57.36°N 130.36°W Miocene
The Castle
The Castle (volcano)
The Castle is a lava spine located west of Squamish in southwestern British Columbia, Canada. Volcanism at The Castle is controlled by north-south structures and there are no hot springs known in the area...

 
798 2618 49.69°N 123.2°W Pleistocene
Castle Rock
Castle Rock (volcano)
Castle Rock is a volcanic neck located west of Iskut and 8 km northwest of Tuktsayda Mountain in British Columbia, Canada. It is part of the Pacific Ring of Fire that includes over 160 active volcanoes and is in the Klastline Group, Northern Cordilleran Volcanic Province and last erupted in...

 
1862 6109 57.84°N 131.15°W Pleistocene
Cauldron Dome
Cauldron Dome
Cauldron Dome is a tuya in the Mount Cayley volcanic field, British Columbia, Canada. Cauldron Dome is made of coarsely plagioclase-orthophyroxene-phyric andesite lava flows and last erupted during the Holocene...

 
2233 7326 50.16°N 123.32°W Pleistocene
Mount Cayley
Mount Cayley
Mount Cayley is a potentially active stratovolcano in Squamish-Lillooet Regional District of southwestern British Columbia, Canada. Located north of Squamish and west of Whistler in the Pacific Ranges of the Coast Mountains, it rises above the Squamish River to the west and above the Cheakamus...

 
2377 7799 50.12°N 123.28°W Pleistocene
Chakatah Creek Peak
Chakatah Creek Peak
Chakatah Creek Peak is a subglacial mound in northwestern British Columbia, Canada. It is one of the volcanoes of the Northern Cordilleran Volcanic Province and last erupted in the Pleistocene period.-See also:*List of volcanoes in Canada...

 
1815 5955 59.25°N 131.03°W Pleistocene
Chelan Seamount
Chelan Seamount
The Chelan Seamount is a seamount located in the Pacific Ocean off the coast of northern Vancouver Island, British Columbia, Canada....

 
-1459 -4787 49.45°N 131.32°W -
Chikoida Mountain
Chikoida Mountain
Chikoida Mountain is a mountain on the Taku Plateau in northwestern British Columbia, Canada, located southeast of Atlin on the east side of the Silver Salmon River....

 
1927 6322 59.2°N 133.4°W Cenozoic
Cinder Cliff
Cinder Cliff
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.-See also:*List of volcanoes in Canada*List of Northern Cordilleran volcanoes...

 
1800 5906 57.75°N 130.57°W Holocene
Cinder Cone
Cinder Cone (British Columbia)
Cinder Cone is a cinder cone with a small crater on the west side of the Helm Glacier in Garibaldi Provincial Park. Cinder Cone is surrounded by cinder flats and its crater is filled with melt water during the summer. Cinder Cone gets eroded easily by melt water during the spring, washing the...

 
1910 6266 49.97°N 123.00°W Holocene
Cinder Mountain
Cinder Mountain
Cinder Mountain is a partly eroded cinder cone at the head of Snippaker Creek, British Columbia, Canada. It is one of the Iskut-Unuk River Cones and is the source of a basaltic lava flow that extends north into Copper King Creek. An isolated pile of subaerial basalt flows and associated pillow...

 
300 984 56.57°N 130.61°W Pleistocene
Clinker Peak
Clinker Peak
Clinker Peak is a stratovolcano, in the Garibaldi Volcanic Belt, British Columbia, Canada. It is located on the west shoulder of Mount Price on the west side of Garibaldi Lake...

 
1992 6535 49.93°N 123.4°W 9000 years ago
Cindercone Peak  2033 6670 52.46°N 125.18°W
Clisbako Caldera Complex
Clisbako Caldera Complex
The Clisbako Caldera Complex is a large dissected caldera complex in the Chilcotin Group and Anahim Volcanic Belt in central British Columbia, Canada. It has a diameter of and is composed mainly of Eocene felsic and mafic volcanic rocks...

 
- - 52.43°N 124.4°W Eocene
Cocoa Crater  2123 6965 57.39°N 130.42°W Holocene
Coffee Crater
Coffee Crater
Coffee Crater is a well-preserved cinder cone south of Mount Edziza, British Columbia, Canada. It was formed during the Holocene period. It is within the Snowshoe lava field which in turn form part of the Mount Edziza volcanic complex.-See also:...

 
2000 6562 57.63°N 130.67°W Holocene
Cottonwood Peak
Cottonwood Peak
Cottonwood Peak is a mountain in northwestern British Columbia, Canada, located in the Iverson Creek area. It is a volcanic feature of the Northern Cordilleran Volcanic Province that formed in the past 1.6 million years during the Pleistocene Epoch.-See also:...

 
1638 5374 59.40°N 130.25°W Pleistocene
Cracker Creek Cone
Cracker Creek Cone
Cracker Creek Cone is a small cinder cone in northwestern British Columbia. A large lava flow that partly filled Ruby Creek may have originated from this cone. The lower west side of the cone appears to be partly covered by glacial till suggesting that the cone is older than the most recent glacial...

 
1895 5880 59.7°N 133.4°W Holocene
Cross diatreme
Cross diatreme
The Cross diatreme is a diatreme in southeastern British Columbia, Canada, located east of the Rocky Mountain Trench and northeast of Elkford....

 
2200 7218 - -
Crow Lagoon
Crow Lagoon
Crow Lagoon is a little-known volcanic center located north of Prince Rupert, British Columbia, Canada. There are beds of thick, basaltic tephra that are of Holocene age....

 
335 1099 54.7°N 130.23°W Holocene
Dark Mountain
Dark Mountain
Dark Mountain, formerly also known as Black Mountain, is a mountain in the Tanzilla Plateau of the Northern Interior of British Columbia, Canada, located northeast of the settlement of Dease Lake, near Cry Lake.-See also:...

 
1974 6476 58.64°N 129.35°W Pleistocene
Dellwood Seamounts
Dellwood Seamounts
The Dellwood Seamounts, also called the Dellwood Seamount Range or the Dellwood Seamount Chain, is a range of seamounts located in the Pacific Ocean northwest of Vancouver Island, British Columbia, Canada.-References:*-See also:...

 
-1474 -4836 50.37°N 130.42°W -
Devastator Peak
Devastator Peak
Devastator Peak, also known as The Devastator, is the lowest and southernmost of the six subsidiary peaks that form the Mount Meager massif in southwestern British Columbia, Canada. It is located west of Bralorne.-Geology:...

 
2327 7635 50.59°N 123.53°W Pleistocene
Dome Mountain
Dome Mountain
Round Mountain is a mountain in northwestern British Columbia, Canada, located east of Dease Lake.Round Mountain is a volcanic feature of the Northern Cordilleran Volcanic Province that formed in the past 1.6 million years of the Pleistocene epoch....

 
1754 5755 58.45°N 129.59°W Pleistocene
Mount Downton
Mount Downton
Mount Downton is the highest summit of the diameter Itcha Range, located northeast of Anahim Lake and east of Far Mountain in the Chilcotin District of the Central Interior of British Columbia, Canada. It lies within Itcha Ilgachuz Provincial Park....

 
2375 7792 52.42°N 124.51°W Pleistocene
Dragon Cone
Dragon Cone
Dragon Cone is a monogenetic cinder cone located in Wells Gray Provincial Park in east-central British Columbia. It is the source of a long lava flow, called Dragon's Tongue. This lava covered the floor of narrow Falls Creek Valley and terminated at the Clearwater River, damming it to a height of ...

 
1830 6000 51.8°N 119.98°W Holocene
Dufferin Island
Dufferin Island
Dufferin Island is an island on the coast of the Canadian province of British Columbia. It is located on the south side of Seaforth Channel just northwest of Bella Bella...

 
50 164 52.22°N 128.32°W Holocene
Mount Edziza
Mount Edziza
Mount Edziza is a stratovolcano in the Stikine Country of northwestern British Columbia, Canada. The volcano and the surrounding area are protected within Mount Edziza Provincial Park. It consists of a complex of multiple peaks and ridges, with several glaciers flowing in all directions. The summit...

 
2787 9144 57.72°N 130.63°W Pleistocene
Mount Edziza volcanic complex
Mount Edziza volcanic complex
The Mount Edziza volcanic complex is a large and potentially active north-south trending complex volcano in Stikine Country, northwestern British Columbia, Canada, located southeast of the small community of Telegraph Creek...

 
2787 9144 57.72°N 130.63°W Holocene
Ember Ridge
Ember Ridge
Ember Ridge is a volcanic mountain ridge associated with the Mount Cayley volcanic field in British Columbia, Canada. Ember Ridge is made of a series of steep-sided domes of glassy, complexly jointed, hornblende-phyric basalt with the most recent eruptions during the Holocene...

 
2348 7703 50.8°N 123.23°W Pliocene
Enid Creek Cone
Enid Creek Cone
Enid Creek Cone is a subglacial mound in northwestern British Columbia, Canada, located in the Dark Mountain area. It last erupted during the Pleistocene epoch.-See also:*List of volcanoes in Canada*List of Northern Cordilleran volcanoes...

 
1914 6280 58.38°N 129.52°W Pleistocene
Eve Cone
Eve Cone
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...

 
1702 5584 57.82°N 130.67°W 700 AD
Exile Hill
Exile Hill
Exile Hill is an isolated hill in the Spectrum Range of northern British Columbia, Canada, located southeast of Mess Lake. It lies at the southern end of Mount Edziza Provincial Park.-History:...

 
1874 6148 57.38°N 130.82°W Pliocene
Explorer Seamount
Explorer Seamount
The Explorer Seamount is a seamount located in the Pacific Ocean off the coast of British Columbia, Canada. It is on the Explorer Ridge, a tectonic spreading centre that separates the Pacific and Explorer plates and so the volcanism is rift-related...

 
-830 -2723 49.5°N 130.48°W -
Mount Fee
Mount Fee
Mount Fee is a volcanic peak in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. It is located south of Callaghan Lake and west of the resort town of Whistler. With a summit elevation of and a topographic prominence of , it rises above the surrounding rugged...

 
2162 7093 50.90°N 123.24°W Pleistocene
Fiftytwo Ridge
Fiftytwo Ridge
Fiftytwo Ridge is a mountain ridge in east-central British Columbia, Canada, located just southwest of Battle Mountain at the southeastern end of Wells Gray Provincial Park.-Geology:...

 
1866 6188 51.93°N 119.89°W Pleistocene
Mount Fitzgerald  2641 8665 51.31°N 126.3°W -
Flatiron
Flatiron (volcano)
The Flatiron is the name for an eroded volcanic outcrop in east-central British Columbia, Canada, located in Wells Gray Provincial Park.The Flatiron is high, long and generally about wide...

 
730 2395 51.88°N 120.5°W Pleistocene
Flourmill Cone
Flourmill Cone
The Flourmill Volcanoes, also known as The Flourmills, are a small volcano range near the west boundary of Wells Gray Provincial Park in east-central British Columbia, Canada...

 
1495 4905 52.5°N 120.32°W Holocene
Franklin Glacier Volcano
Franklin Glacier Volcano
Franklin Glacier Volcano is a deeply eroded and huge long and wide caldera complex in southwestern British Columbia, Canada, located east-southeast of the Silverthrone Caldera in the Hoodoo Creek and Franklin Glacier area on the northwest flank of the Waddington Massif of the Pacific Ranges...

 
2252 7388 51.20°N 125.24°W Pliocene
Gabrielse Cone
Gabrielse Cone
Gabrielse Cone is a remarkably fresh, clearly postglacial monogenetic cinder cone, located in the Tuya Volcanic Field in British Columbia, Canada. It is about in diameter and has a central crater about deep. It is Holocene in age and to its northeast appears to be breached with the remnants of a...

 
1600 5249 59.44°N 130.46°W Holocene
Gage Hill
Gage Hill
Gage Hill is a tuya in east-central British Columbia, Canada, located in Wells Gray Provincial Park.-See also:*List of volcanoes in Canada*Volcanism of Canada*Volcanism of Western Canada...

 
1090 3576 52.5°N 120.1°W Pleistocene
Mount Garibaldi
Mount Garibaldi
Mount Garibaldi is a potentially active stratovolcano in the Sea to Sky Country of British Columbia, north of Vancouver, Canada. Located in the southernmost Coast Mountains, it is one of the most recognized peaks in the South Coast region, as well as British Columbia's best known volcano...

 
2678 8786 49.84°N 123.1°W Holocene
Glacier Dome
Glacier Dome
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.-See also:*List of volcanoes in Canada*List of Northern Cordilleran volcanoes...

 
2225 7300 57.77°N 130.58°W Pleistocene
Glacier Pikes
Glacier Pikes
Glacier Pikes is a Lava dome, located in the Garibaldi Lake volcanic field, British Columbia, Canada. The dome has two rocky points at the southern end of the Sentinel Glacier Neve.-See also:*List of volcanoes in Canada*Volcanism of Canada...

 
2145 7037 49.89°N 122.85°W Pleistocene
Graham Seamount
Graham Seamount
The Graham Seamount is a seamount located in the Pacific Ocean off the coast of the Queen Charlotte Islands, British Columbia, Canada.-References:*-See also:*Volcanism of Canada*Volcanism of Western Canada*List of volcanoes in Canada...

 
-1474 -4836 53.14°N 134.31°W -
Grizzly Butte
Grizzly Butte
Grizzly Butte small shield volcano located in northwestern British Columbia, Canada. It is Holocene in age and stands in relief above the surrounding area north of the Nazcha Creek and comprises the West Tuya lava field with West Vent and Volcano Vent...

 
1412 4633 50.3°N 119.6°W Holocene
HP diatreme
HP diatreme
The HP diatreme, also called the HP pipe, is a diatreme in the Rocky Mountains of southeastern British Columbia, Canada, located northeast of Golden....

 
2400 7874 51.41°N 116.57°W -
Haddington Island
Haddington Island (British Columbia)
Haddington Island is a small volcanic island in the Canadian province of British Columbia, located south of Malcolm Island and Broughton Strait...

 
- - 50.36°N 127.2°W Pliocene
Heart Peaks
Heart Peaks
Heart Peaks, originally known as the Heart Mountains, is a mountain massif in the Northern Interior of British Columbia, Canada. It is located northwest of the small community of Telegraph Creek and just southwest of Callison Ranch. With a maximum elevation of , it rises above the surrounding...

 
2012 6601 58.60°N 131.97°W Pleistocene
Heck Seamount
Heck Seamount
The Heck Seamount is a seamount located in the Pacific Ocean off the coast of central Vancouver Island, British Columbia, Canada.-References:*-See also:*Volcanism of Canada*Volcanism of Western Canada*List of volcanoes in Canada...

 
1320 4331 48.3°N 130.1°W -
Helmet Peak  318 1043 52.35°N 128.35°W Holocene
Hodgkins Seamount
Hodgkins Seamount
Hodgkins Seamount is a seamount in the Kodiak-Bowie Seamount chain, located south of Pierce Seamount and north of Bowie Seamount. Hodgkins Seamount has apparently experienced two generically different episodes of volcanism, separated by about 12 million years ago...

 
-790 -2592 53.3°N 136.5°W Pliocene
Hoodoo Mountain
Hoodoo Mountain
Hoodoo Mountain is a potentially active flat-topped stratovolcano in the Stikine Country of northwestern British Columbia, Canada, located northeast of Wrangell, Alaska on the north side of the lower Iskut River and east of its junction with the Stikine River...

 
1850 6070 56.78°N 131.28°W 7050 years ago
Hyalo Ridge
Hyalo Ridge
Hyalo Ridge is a tuya in Wells Gray Provincial Park. Hyalo Ridge last erupted during Pleistocene.-See also:* List of volcanoes in Canada* Volcanism of Canada* Volcanism of Western Canada...

 
2012 6601 52.11°N 120.36°W Pleistocene
IGC Centre
IGC Centre
IGC Centre is a lava dome in Mount Edziza Provincial Park of northern British Columbia, Canada. It is thought to have formed and last erupted during the Miocene period.-See also:*List of volcanoes in Canada*List of Northern Cordilleran volcanoes...

 
2074 6804 57.56°N 130.62°W Miocene
Ice Peak
Ice Peak
Ice Peak is a stratovolcano, located west of Tatogga and south of Mount Edziza, British Columbia, Canada. It overlaps the 7.5 million year old Armadillo Peak. It lies on a large volcanic plateau, which is made of basaltic lava flows from the massive Mount Edziza volcanic complex...

 
2526 8287 57.70°N 130.63°W Holocene
Icefall Cone
Icefall Cone
Icefall Cone is a cinder cone in northern British Columbia, Canada. It is thought to have last erupted during the Holocene period and forms part of the Mount Edziza volcanic complex.-See also:*List of volcanoes in Canada...

 
2285 7497 57.70°N 130.6°W Holocene
Ida Ridge
Ida Ridge
Ida Ridge is an eroded cinder cone in east-central British Columbia, Canada, located in the southeastern corner of Wells Gray Provincial Park.-See also:* List of volcanoes in Canada* Volcanism of Canada* Volcanism of Western Canada...

 
1981 6499 51.8°N 119.94°W Pleistocene
Ilgachuz Range
Ilgachuz Range
The Ilgachuz Range is a name given to an extinct shield volcano in British Columbia, Canada. It is not a mountain range in the normal sense, because it was formed as a single volcano that has been eroded for the past 5 million years. It lies on the Chilcotin Plateau, located some north-northwest...

 
2410 7907 52.47°N 125.19°W Pliocene
Iskut-Unuk River Cones
Iskut-Unuk River Cones
The Iskut-Unuk River Cones are a group of eight small basaltic centres at the southern end of the Northern Cordilleran Volcanic Province in the Boundary Ranges of the Coast Mountains. The lava flows date back 70,000 years, but the subaerial vents produced cinder cones and lava flows that were...

 
1880 6168 56.52°N 130.33°W 1800?
Isspah Butte
Isspah Butte
Isspah Butte is a tuya in the Atsutla Range of the Kawdy Plateau in northern British Columbia, Canada. It lies on the north side of the Nazcha Creek.-See also:* List of volcanoes in Canada* List of Northern Cordilleran volcanoes* Volcanism of Canada...

 
1673 5489 59.4°N 131.18°W Pleistocene
Itcha Mountain
Itcha Mountain
Itcha Mountain is one of the two main volcanic peaks of the Itcha Range, which is located in the Chilcotin District of the Central Interior of British Columbia, Canada. It is in the Anahim Volcanic Belt, which formed when the North American Plate moved over a hotspot, similar to the one feeding the...

 
2290 7513 52.43°N 124.49°W Pleistocene
Itcha Range
Itcha Range
The Itcha Range is a mountain range on the Chilcotin Plateau of the West-Central Interior of British Columbia, Canada. The range is located 25 miles northeast of Anahim Lake...

 
2375 7792 52.42°N 124.5°W Pleistocene
Jack's Jump
Jack's Jump
Jack's Jump is a subglacial volcano in east-central British Columbia, Canada, located at the northeastern end of Wells Gray Provincial Park.-See also:* List of volcanoes in Canada* Volcanism of Canada* Volcanism of Western Canada...

 
1895 6217 52.12°N 120.5°W Pleistocene
Mount Job
Mount Job
Mount Job is one of the six named volcanic peaks of Mount Meager in British Columbia, Canada. It is a pile of rubble held together by volcanic ash and sand...

 
2493 8180 50.62°N 123.55°W Pleistocene
Mount Josephine
Mount Josephine (British Columbia)
Mount Josephine is a subglacial mound in the Tuya Range in British Columbia, Canada. It is located near the northwestern shore of Tuya Lake.-See also:* Northern Cordilleran Volcanic Province* Tuya Range* List of Northern Cordilleran volcanoes...

 
1767 5797 59.6°N 130.7°W Pleistocene
Kana Cone
Kana Cone
Kana Cone is a red nested cinder cone in northern British Columbia, Canada, located northeast of Eve Cone in Mount Edziza Provincial Park.-See also:*List of volcanoes in Canada*List of Northern Cordilleran volcanoes*Volcanism of Canada...

 
1100 3609 57.90°N 130.62°W Holocene
Kawdy Mountain
Kawdy Mountain
Kawdy Mountain is a subglacial mound on the Kawdy Plateau, the northernmost sub-plateau of the Stikine Plateau in northwestern British Columbia, Canada. It consists of nearly horizontal beds of basaltic lava, capping outward dipping beds of fragmental volcanic rocks and last erupted in Pleistocene...

 
1936 6352 58.88°N 131.23°W Pleistocene
Kena Cone
Kena Cone
Kena Cone is a cinder cone in northwestern British Columbia, Canada, located in the Snowshoe Lava Field of Mount Edziza Provincial Park. It last erupted during the Holocene epoch.-See also:*List of volcanoes in Canada*List of Northern Cordilleran volcanoes...

 
1980 6496 57.6°N 130.68°W Holocene
Mount Kinch
Mount Kinch
Mount Kinch is a volcanic knob in southwestern British Columbia, Canada, located east of Rivers Inlet. It is almost completely ice-covered.-See also:* List of volcanoes in Canada* Volcanism of Canada* Volcanism of Western Canada...

 
2470 8104 51.25°N 126.10°W -
Kitasu Hill
Kitasu Hill
Kitasu Hill is a young basaltic cinder cone on southwestern Swindle Island on the coast of the Canadian province of British Columbia. It is located southwest of Klemtu and south of Kitasu Bay. Kitasu Hill produced lava flows that extend to the north...

 
235 771 52.50°N 128.73°W Holocene
Klastline Cone
Klastline Cone
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.-See also:*List of volcanoes in Canada*List of Northern Cordilleran volcanoes...

 
1400 4593 57.78°N 130.5°W Pleistocene
Klinkit Creek Peak
Klinkit Creek Peak
Klinkit Creek Peak is a tuya in northwestern British Columbia, Canada, located near Klinkit Lake. It lies in the Northern Cordilleran Volcanic Province and last erupted during the Pleistocene epoch.-See also:*List of volcanoes in Canada...

 
1519 4984 59.47°N 131.28°W Pleistocene
Klinkit Lake Peak
Klinkit Lake Peak
Klinkit Lake Peak is a tuya in northwestern British Columbia, Canada, located near Klinkit Lake. It lies in the Northern Cordilleran Volcanic Province and last erupted during the Pleistocene epoch.-See also:*List of volcanoes in Canada...

 
1516 4974 59.49°N 131.1°W Pleistocene
Kostal Cone
Kostal Cone
Kostal Cone, also called Kostal Volcano, is a young cinder cone in Wells Gray Provincial Park in east-central British Columbia, Canada. It rises from the northeast shore of Kostal Lake in the Cariboo Mountains...

 
1440 4724 52.17°N 119.94°W 1550 (?)
Level Mountain Range
Level Mountain Range
The Level Mountain Range, also known as Level Mountain, is a mountain range in Cassiar Country, northwestern British Columbia, Canada, located just northeast of Callison Ranch, southwest of Dease Lake and about north of Mount Edziza. It consists of a massive shield volcano and lies on the Nahlin...

 
2190 7185 58.25°N 131.21°W Holocene?
Lightning Peak  2139 7018 49.88°N 118.53°W Pliocene
Little Bear Mountain
Little Bear Mountain
Little Bear Mountain is a basaltic Pleistocene age tuya in the Boundary Ranges of the Coast Mountains that adjoins Hoodoo Mountain to the north. Little Bear Mountain is part of the Northern Cordilleran Volcanic Province.-See also:* List of volcanoes in Canada...

 
1180 3875 56.80°N 131.3°W Pleistocene
Little Eagle Cone
Little Eagle Cone
Little Eagle Cone is a subglacial mound in northwestern British Columbia, Canada, located in the Dark Mountain area. It last erupted during the Pleistocene epoch.-See also:*List of volcanoes in Canada*List of Northern Cordilleran volcanoes...

 
1545 5069 58.52°N 129.71°W Pleistocene
Little Ring Mountain  2165 7103 50.16°N 123.18°W Unknown
Llangorse Mountain
Llangorse Mountain
Llangorse Mountain is a mountain in northern British Columbia, Canada, located southeast of Atlin on the eastern side of the head of the Gladys River...

 
1962 6437 59.32°N 132.9°W Cenozoic
Lone Butte
Lone Butte (British Columbia)
Lone Butte is a low, steep-sided mesa butte or volcanic plug in southern British Columbia, Canada, located on the southern Cariboo Plateau to the southeast of 100 Mile House. It is composed of columnar basalt that formed within a prehistoric volcano six million years ago...

 
1237 4058 51.33°N 131.11°W Miocene
Mount MacKenzie
Mount MacKenzie
Mount MacKenzie is a volcanic peak, located northeast of Hagenborg, British Columbia, Canada. It is one of the volcanic peaks of the Rainbow Range, which is one of the three major shield volcanoes that form the Anahim Volcanic Belt...

 
2143 7031 52.37°N 126.5°W Miocene
Machmel River Cone
Machmel River Cone
Machmell River Cone is a cinder cone in the Silverthrone Caldera complex in the Pacific Ranges section of the Coast Mountains in British Columbia, Canada...

 
1800 5906 51.51°N 126.21°W Holocene
Maitland Volcano
Maitland Volcano
Maitland Volcano was a Pliocene age shield volcano in the western Cassiar Mountains of northwestern British Columbia, Canada. In the course of one million years, Maitland Volcano was formed on a mature, eroded Tertiary surface by rifting of the North American continent as thin alkali olivine basalt...

 
2514 8248 57.4°N 129.7°W Pliocene
Maquinna
Maquinna (volcano)
Maquinna is an active submarine mud volcano on the Coast of British Columbia, Canada, located 16-18 kilometers west of Vancouver Island. It rises approximately above the mean level of the northeastern Pacific Ocean and lies directly along the southern expression of the left laterial, strike slip...

 
-2500 -8202 - Holocene
Mathews Tuya
Mathews Tuya
Mathews Tuya is a subglacial mound in northcentral British Columbia. It is one of the six tuyas close to Tuya Lake. It has been partly glaciated so it is probably older than 10,000 years. The other volcanoes in the area include Tuya Butte, South Tuya and Ash Mountain...

 
1676 5499 59.20°N 130.43°W Pleistocene
McLeod Hill
McLeod Hill
McLeod Hill is a tuya, located north of Clearwater in the Wells Gray-Clearwater volcanic field in Wells Gray Provincial Park, east-central British Columbia, Canada....

 
1284 4213 52.02°N 120.01°W Pleistocene
Mount Meager
Mount Meager
Mount Meager, originally known as Meager Mountain, is a complex volcano in the Sea-to-Sky Corridor of southwestern British Columbia, Canada. It is located north of Vancouver at the northern end of the Pemberton Valley. Part of the Cascade Volcanic Arc of western North America, its summit is above...

 
2680 8793 50.63°N 123.5°W 2350 years ago
Meehaz Mountain
Meehaz Mountain
Meehaz Mountain is a mountain in the Cassiar Country of the Northern Interior of British Columbia, Canada, located on the north side of the headwaters of Teslin River and to the south of the Atsutla Range...

 
1608 5276 59.1°N 131.27°W Pleistocene
Meszah Peak
Meszah Peak
Meszah Peak is a volcanic cone located north of Telegraph Creek and southwest of Zus Mountain. It is the highest mountain of the Level Mountain Range, a massive shield volcano forming the most voluminous and most persistent eruptive centre in the Northern Cordilleran Volcanic Province.-See also:*...

 
2166 7106 58.48°N 131.43°W Pleistocene
Moraine Cone
Moraine Cone
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.-See also:*List of volcanoes in Canada*List of Northern Cordilleran volcanoes...

 
2135 7005 57.77°N 130.62°W Holocene
Mosquito Mound
Mosquito Mound
Mosquito Mound is a tuya in east-central British Columbia, Canada, located in Wells Gray Provincial Park.-See also:*List of volcanoes in Canada*Volcanism of Canada*Volcanism of Western Canada...

 
1065 3494 52.02°N 120.18°W Pleistocene
Nahta Cone
Nahta Cone
Nahta Cone is a cinder cone in northern British Columbia, Canada, located southwest of Tatogga, north of Wetalth Ridge and south of Telegraph Creek...

 
1690 5545 57.32°N 130.82°W Holocene
Nanook Dome
Nanook Dome
Nanook Dome is a lava dome in northwestern British Columbia, Canada, located just northeast of Mount Edziza in Mount Edziza Provincial Park. It last erupted during the Pleistocene epoch.-See also:*List of volcanoes in Canada...

 
2710 8891 57.72°N 130.6°W Pleistocene
Nazko Cone
Nazko Cone
Nazko Cone is a small potentially active basaltic cinder cone in central British Columbia, Canada, located 75 km west of Quesnel and 150 kilometers southwest of Prince George. It is considered the easternmost volcano in the Anahim Volcanic Belt. The small tree-covered cone rises 120 m above...

 
1230 4035 52.55°N 123.44°W 7200 years ago
Nuthinaw Mountain
Nuthinaw Mountain
Nuthinaw Mountain is a mountain on the Stikine Plateau in northern British Columbia, Canada, located east of Tutsingale Mountain and northwest of Dease Lake on the north side of Tachilta Lakes...

 
1732 5682 58.47°N 131.3°W Pleistocene
Mount Noel
Mount Noel
Mount Noel is a Miocene volcanic complex in the Chilcotin Group in British Columbia, Canada, located southwest of Bralorne and north of a tributary of Noel Creek. It is east of the Garibaldi Volcanic Belt and is made up of flat-lying, columnar-jointed basalt flows along with debris flows and...

 
2541 8337 50.42°N 122.51°W Miocene
Opal Cone
Opal Cone
Opal Cone is a cinder cone located on the southeast flank of Mount Garibaldi in the Coast Mountains of British Columbia, Canada. It is the source of a 15 km long broad dacite lava flow with prominent wrinkled ridges...

 
1736 5696 49.82°N 122.97°W 9300 years ago
Oshawa Seamount
Oshawa Seamount
The Oshawa Seamount is a seamount located in the Pacific Ocean off the coast of the Queen Charlotte Islands, British Columbia, Canada.-References:*-See also:*Volcanism of Canada*Volcanism of Western Canada*List of volcanoes in Canada...

 
2127 6978 53.14°N 134.31°W -
Ospika pipe
Ospika pipe
The Ospika pipe is a small composite diatreme in northern British Columbia, Canada, located approximately north-northwest of Mackenzie, on the east side of Williston Lake between the Peace Reach and Ospika River....

 
1550 5085 56.27°N 123.45°W -
Outcast Hill
Outcast Hill
Outcast Hill is an isolated hill in northern British Columbia, Canada, located southeast of Mess Lake. It lies at the southern end of Mount Edziza Provincial Park.-History:...

 
1800 5906 57.23°N 130.46°W Pleistocene
Mount Overill
Mount Overill
Mount Overill is a volcanic peak in southwestern British Columbia, Canada, located east of Rivers Inlet and northwest of Mount Somolenko.-See also:* List of volcanoes in Canada* Volcanism of Canada* Volcanism of Western Canada...

 
2354 7723 51.28°N 126.7°W -
Pali Dome
Pali Dome
Pali Dome is the unofficial name for a volcanic peak in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada.-See also:*List of volcanoes in Canada*Mount Cayley volcanic field*Volcanism of Canada*Volcanism of Western Canada...

 
1767 5797 50.13°N 123.25°W Pleistocene
Peak 1924  1565 5135 59.4°N 130.38°W Pleistocene
Peak 2050  2036 6680 59.39°N 130.18°W Pleistocene
Peak 2166  2064 6800 59.31°N 130.59°W Pleistocene
Peirce Seamount
Peirce Seamount
Peirce Seamount, also called Pierce Seamount, is a seamount located in the Pacific Ocean west of the Queen Charlotte Islands, British Columbia, Canada...

 
-1800 -5906 53.44°N 136.32°W -
Perkin's Pillar
Perkin's Pillar
Perkin's Pillar was a vertical pillar of volcanic rock of the Mount Meager massif in southwestern British Columbia, Canada. It existed on the steep north flank of Capricorn Mountain...

 
2430 7972 50.37°N 123.31°W -
Pharaoh Dome
Pharaoh Dome
Pharaoh 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.-See also:*List of volcanoes in Canada*List of Northern Cordilleran volcanoes...

 
2200 7218 57.65°N 130.6°W Pleistocene
Pillow Creek
Pillow Creek
Pillow Creek is a creek in east-central British Columbia, Canada, located in the northeast corner of Wells Gray Provincial Park.Pillow Creek is home to a subglacial volcano that formed and last erupted during the Pleistocene period.-See also:...

 
1829 6001 52.02°N 119.84°W Pleistocene
Pillow Ridge
Pillow Ridge
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.-History:...

 
2400 7874 57.76°N 130.64°W Pleistocene
Plinth Peak
Plinth Peak
Plinth Peak, sometimes called Plinth Mountain, is the highest satellite cone of Mount Meager, and one of four overlapping volcanic cones which together form the northernmost volcanic complex in the Cascade Volcanic Arc and the Garibaldi Volcanic Belt...

 
2677 8783 50.64°N 123.51°W 2350 years ago
Pointed Stick Cone
Pointed Stick Cone
Pointed Stick Cone is a cinder cone in east-central British Columbia, Canada, located in Wells Gray Provincial Park.-See also:* List of volcanoes in Canada* Volcanism of Canada* Volcanism of Western Canada...

 
1820 5971 52.24°N 120.08°W Holocene
Powder Mountain
Powder Mountain (British Columbia)
Powder Mountain, , is a volcanic summit in the Powder Mountain Icefield in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada....

 
2347 7700 50.8°N 123.16°W -
Mount Price  2052 6732 49.92°N 123.3°W 9000 years ago
Pylon Peak
Pylon Peak
Pylon Peak is the southernmost summit of the six named volcanic peaks of Mount Meager in British Columbia, Canada. Two pinnacled ridges extend out from Pylon and are named respectively the Pylons and the Marionettes. Pylon Peak overlooks the Meager Creek Hot Springs.Erosional remnants of flows from...

 
2481 8140 50.35°N 123.31°W Pleistocene
Pyramid Dome
Pyramid Dome
The Pyramid, also called Pyramid Dome, is a young lava dome on the northeast flank of Mount Edziza in British Columbia, Canada. It is on the northeastern edge of the Tencho Glacier and represents several different styles of volcanic activity on the Mount Edziza complex...

 
2199 7215 57.77°N 130.57°W Pleistocene
Pyramid Mountain
Pyramid Mountain (volcano)
Pyramid Mountain is a subglacial mound located on the Murtle Plateau in Wells Gray Provincial Park, east-central British Columbia, Canada.-Formation:...

 
240 1103 51.99°N 120.1°W Pleistocene
Pyroclastic Peak
Pyroclastic Peak
Pyroclastic Peak is the second highest of the five named volcanic peaks immediately south of Mount Cayley in British Columbia, Canada. It is steep and rotten and is located southwest of Callaghan Lake and west of Whistler...

 
2349 7707 50.6°N 123.17°W Pleistocene
Rainbow Range
Rainbow Range (Coast Mountains)
The Rainbow Range, formerly known as the Rainbow Mountains, is a mountain range in British Columbia, Canada, located northwest of Anahim Lake...

 
2495 8186 52.43°N 125.46°W Miocene
Ray Mountain
Ray Mountain
Ray Mountain is a subglacial mound in Wells Gray Provincial Park, British Columbia, Canada. Ray Mountain last erupted during the Pleistocene. It is part of the Wells Gray-Clearwater volcanic field....

 
2050 6726 52.24°N 120.11°W Pleistocene
Ridge Cone
Ridge Cone
Ridge 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.-See also:*List of volcanoes in Canada*List of Northern Cordilleran volcanoes...

 
2285 7497 57.68°N 130.62°W Holocene
Ring Mountain  2192 7192 50.13°N 123.17°W Unknown
Round Mountain
Round Mountain (volcano)
Round Mountain is an eroded volcanic outcrop in the Garibaldi Volcanic Belt in British Columbia, Canada, located 8 km southwest of Eanastick Meadows, east of Brackendale and south of Mount Garibaldi. It is the highpoint of Paul Ridge and is located in the southwest corner of Garibaldi...

 
1646 5400 49.45°N 123.1°W Pleistocene
Ruby Mountain
Ruby Mountain
Ruby Mountain is a cinder cone in Stikine Region, British Columbia, Canada, located 23 km northeast of Atlin and south of Mount Barham. A recent collapse on the volcanoes eastern side created a large landslide which dissects this side of Ruby Mountain...

 
1895 6217 59.68°N 123.33°W 1898?
Satah Mountain
Satah Mountain
Satah Mountain is a cinder cone, located east-northeast of Nimpo Lake in central British Columbia, Canada. It areas to the south form a N-S-trending chain of cinder cones of Pleistocene and Holocene age. It lies on the Chilcotin Plateau....

 
1921 6302 52.28°N 124.41°W Unknown
The Saucer
The Saucer
The Saucer is a cinder cone in northern British Columbia, Canada. It is thought to have last erupted in the Holocene epoch.-See also:*List of volcanoes in Canada*List of Northern Cordilleran volcanoes*Volcanism of Canada*Volcanism of Western Canada...

 
1920 6299 57.63°N 130.63°W Holocene
Seminole Seamount
Seminole Seamount
The Seminole Seamount is a seamount located in the Pacific Ocean off the coast of northern Vancouver Island, British Columbia, Canada.-References:*-See also:*Volcanism of Canada*Volcanism of Western Canada*List of volcanoes in Canada...

 
-1653 -5423 49.46°N 129.5°W -
Sezill Volcano
Sezill Volcano
Sezill Volcano is a lava dome in Mount Edziza Provincial Park of northern British Columbia, Canada. It is thought to have formed and last erupted during the Miocene period...

 
2050 6726 57.59°N 130.62°W Miocene
Sham Hill
Sham Hill
Sham Hill is a volcanic plug in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada, located near the upper Bridge River. It is part of a volcanic group called the Bridge River Cones which in turn is part of the Garibaldi Volcanic Belt of the Cascade Volcanic Arc....

 
60 197 50.9°N 123.52°W Pleistocene
Sidas Cone
Sidas Cone
Sidas Cone is one of the cinder cones located north on the Mount Edziza plateau in British Columbia, Canada. Sidas Cone is visible from almost anywhere around the plateau.-See also:* Northern Cordilleran Volcanic Province* Volcanism of Canada...

 
1540 5052 57.87°N 130.63°W Holocene
Mount Silverthrone
Mount Silverthrone
Mount Silverthrone, officially named Silverthrone Mountain, is a mountain in the Regional District of Mount Waddington, British Columbia, located over northwest of the city of Vancouver and about west of Mount Waddington, British Columbia, Canada...

 
3160 10367 51.31°N 126.6°W Unknown
Silverthrone Caldera
Silverthrone Caldera
The Silverthrone Caldera is a potentially active caldera complex in southwestern British Columbia, Canada, located over northwest of the city of Vancouver and about west of Mount Waddington in the Pacific Ranges of the Coast Mountains. The caldera is one of the largest of the few calderas in...

 
3160 10367 51.26°N 126.18°W Unknown
Skoatl Point
Skoatl Point
Skoatl Point is a volcanic plug located in the formation known as the Chilcotin Group, which lie between the Pacific Ranges of the Coast Mountains and the mid-Fraser River in British Columbia, Canada.-Location and terrain:...

 
1640 5381 51.9°N 120.25°W -
Slag Hill
Slag Hill
Slag Hill is a subglacial volcano associated with the Mount Cayley volcanic field in British Columbia, Canada. It consists of glassy, augite-phyric basaltic andesite in steep-sided, glassy, finely jointed domes and one small, flat-topped bluff. The finely jointed domes are similar to those of Ember...

 
2088 6850 50.19°N 123.3°W Pleistocene
Sleet Cone
Sleet Cone
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.-See also:*List of volcanoes in Canada...

 
1783 5850 57.78°N 130.55°W Holocene
Mount Somolenko
Mount Somolenko
Mount Somolenko is a volcanic peak in southwestern British Columbia, Canada, located east of Rivers Inlet and south of Mount Silverthrone. It is the highest peak south of Mount Silverthrone in the Ha-Iltzuk Icefield....

 
2658 8720 51.28°N 126.6°W -
Source Hill
Source Hill
Source Hill is a cinder cone in northwestern British Columbia, Canada. It is polygenetic in nature, having erupted more than once throughout its eruptive history...

 
1630 5348 57.28°N 130.82°W Pleistocene
South Tuya
South Tuya
South Tuya, also called Southern Tuya, is a tuya clustered around Tuya Lake in the Northern Cordilleran Volcanic Province in British Columbia, Canada...

 
1829 5637 59.2°N 130.5°W Pleistocene
Spanish Bonk
Spanish Bonk
Spanish Bonk is a volcanic plug located in the Quesnel Highland of the Wells Gray-Clearwater volcanic field in southeastern British Columbia, Canada. Spanish Bonk last erupted during the Pleistocene.-External links:*...

 
1770 5807 52.13°N 120.37°W Pleistocene
Spanish Lake Centre  1770 5807 52.07°N 120.31°W Holocene
Spanish Mump
Spanish Mump
Spanish Mump is a subglacial mound in east-central British Columbia, Canada, located in the northeastern corner of Wells Gray Provincial Park.-See also:* List of volcanoes in Canada* Volcanism of Canada* Volcanism of Western Canada...

 
1800 5906 52.16°N 120.33°W Pleistocene
Spectrum Range
Spectrum Range
The Spectrum Range, formerly called the Spectrum Mountains and the Rainbow Mountains, is a subrange of the Tahltan Highland in the Stikine Country of northwestern British Columbia, 20 km west of the Stewart-Cassiar Highway, south of Mount Edziza and north of the Arctic Lake Plateau. The...

 
2430 7972 57.26°N 130.41°W Unknown
The Sphinx
The Sphinx
The Sphinx is a subglacial mound in the southernmost Coast Mountains of British Columbia, Canada. It is south-east of Garibaldi Lake. The volcano is part of the Garibaldi Volcanic Belt which is a segment of the Cascade Volcanic Arc, but it is not within the geographic boundary of the Cascade Range...

 
1525 5003 49.93°N 122.85°W Pleistocene
Sphinx Dome
Sphinx Dome
Sphinx 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.-See also:*List of volcanoes in Canada*List of Northern Cordilleran volcanoes...

 
2380 7808 57.75°N 130.58°W Pleistocene
Stirni Seamount
Stirni Seamount
The Union Seamount is a seamount located in the Pacific Ocean off the coast of northern Vancouver Island, British Columbia, Canada.-References:*-See also:*Volcanism of Canada*Volcanism of Western Canada*List of volcanoes in Canada...

 
-1710 -5610 49.8°N 132.18°W -
Stockton Hill
Stockton Hill
Stockton Hill is a volcanic plug located in the formation known as the Chilcotin Group, which lie between the Pacific Ranges of the Coast Mountains and the mid-Fraser River in British Columbia, Canada.-Location and terrain:...

 
1574 5164 51.10°N 120.33°W -
Storm Cone
Storm Cone
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.-See also:*List of volcanoes in Canada...

 
2135 7005 57.77°N 130.63°W Holocene
The Table
The Table
The Table, sometimes called Table Mountain, is a high flow-dominated andesite tuya located south of Garibaldi Lake, northeast of Cheekye and north of Mount Garibaldi, British Columbia, Canada...

 
1645 5397 49.9°N 123.2°W Pleistocene
Tadeda Peak
Tadeda Peak
Tadeda Peak, also known unofficially as Tadeda Centre, is a volcanic peak in northern British Columbia, Canada, located just southeast of Coffee Crater in Mount Edziza Provincial Park.-See also:* List of volcanoes in Canada...

 
2194 7198 57.54°N 130.61°W Miocene
Tadekho Hill
Tadekho Hill
Tadekho Hill is an isolated hill in the Spectrum Range of northern British Columbia, Canada, located southwest of Tatogga and southwest of Kitsu Peak...

 
1860 6102 57.35°N 130.78°W Pleistocene
Tennena Cone
Tennena Cone
Tennena Cone is a subglacial mound in northern British Columbia, Canada, located just southwest of Mount Edziza in Mount Edziza Provincial Park.-See also:*List of volcanoes in Canada*List of Northern Cordilleran volcanoes*Volcanism of Canada...

 
2350 7710 57.68°N 130.67°W Holocene
The Thumb
The Thumb (Omineca)
The Thumb is a mountain located south of Sitchiada Mountain on the east side of Bear Lake, on the divide between the upper Omineca River and the basin of the Bear River in the Omineca Country of the Central-North Interior of British Columbia, Canada...

 
1854 6083 56.16°N 126.7°W Unknown
Toozaza Peak
Toozaza Peak
Toozaza Peak is a tuya in the Stikine Ranges of the Cassiar Mountains in northern British Columbia, Canada, located in the Iverson Creek. Toozaza Peak is the summit of a north-south aligned ridge between the head of Toozaza Creek and the head of the Jennings River, just south of the Jennings'...

 
2182 7182 59.50°N 130.3°W Pleistocene
Tow Hill
Tow Hill
Tow Hill is a large isolated volcanic plug located east of Masset on the north end of the Naikoon Peninsula of northeast Graham Island in Haida Gwaii, British Columbia, Canada, east of McIntyre Bay and near the mouth of the Hiellen River, which is the site of Hiellen a now-abandoned Haida village...

 
125 410 54.4°N 131.47°W Pliocene
Triangle Dome
Triangle Dome
Triangle Dome is a trachytic lava dome in northern British Columbia, Canada. It is thought to have formed in the Pleistocene period.-See also:*List of volcanoes in Canada*List of Northern Cordilleran volcanoes*Volcanism of Canada...

 
2680 8793 57.72°N 130.65°W Pleistocene
Triplex Cone
Triplex Cone
Triplex Cone is a cinder cone in northern British Columbia, Canada. It is thought to have last erupted in the Holocene period.-See also:*List of volcanoes in Canada*List of Northern Cordilleran volcanoes*Volcanism of Canada*Volcanism of Western Canada...

 
1785 5856 57.80°N 130.62°W Holocene
Tseax Cone
Tseax Cone
The Tseax Cone , also called the Tseax River Cone or alternately the Aiyansh Volcano, is a young cinder cone and adjacent lava flows associated with the Nass Ranges and the Northern Cordilleran Volcanic Province...

 
600 1969 55.12°N 126.9°W 1750-1775
Tsekone Ridge
Tsekone Ridge
Tsekone Ridge, also known as Tsekone Peak and Black Knight Cone, is a subglacial mound that sits out by itself in the Desolation Lava Field in northwestern British Columbia, Canada.-See also:* List of volcanoes in Canada...

 
1920 6299 57.77°N 130.69°W Pleistocene
Tuber Hill
Tuber Hill
Tuber Hill is a small 600,000 year old basaltic stratovolcano that was constructed on the Bridge River highlands when nearby valleys were packed with ice...

 
2500 8202 50.93°N 123.44°W Pleistocene
Tucker Seamount
Tucker Seamount
The Tucker Seamount is a seamount located in the Pacific Ocean off the coast of northern Vancouver Island, British Columbia, Canada.-References:*-See also:*Volcanism of Canada*Volcanism of Western Canada*List of volcanoes in Canada...

 
-1242 -4075 49.5°N 133.3°W -
Tutsingale Mountain
Tutsingale Mountain
Tutsingle Mountain is a mountain on the Stikine Plateau in northern British Columbia, Canada, located east of Nuthinaw Mountain and northwest of Dease Lake on the northeast side of the Tachilta Lakes...

 
1722 5650 58.78°N 130.87°W Pleistocene
Tuya Butte
Tuya Butte
Tuya Butte is a tuya in the Tuya Range of north-central British Columbia, Canada. It is a bit less isolated from other ranges than neighbouring Mount Josephine...

 
1685 5528 59.13°N 130.55°W Pleistocene
Tuzo Wilson Seamounts
Tuzo Wilson Seamounts
The Tuzo Wilson Seamounts, also called J. Tuzo Wilson Knolls and Tuzo Wilson Knolls, are two young active submarine volcanoes off the coast of British Columbia, Canada, located northwest of Vancouver Island and south of the Queen Charlotte Islands...

 
-1410 -4626 51.4°N 130.9°W Holocene
Twin Cone
Twin Cone
Twin Cone is a cinder cone in northern British Columbia, Canada. It is thought to have last erupted in the Holocene period.-See also:*List of volcanoes in Canada*List of Northern Cordilleran volcanoes*Volcanism of Canada*Volcanism of Western Canada...

 
1430 4692 57.70°N 130.64°W Holocene
Union Seamount
Union Seamount
The Union Seamount is a seamount located in the Pacific Ocean off the coast of northern Vancouver Island, British Columbia, Canada.-References:*-See also:*Volcanism of Canada*Volcanism of Western Canada*List of volcanoes in Canada...

 
-293 -961 49.35°N 132.45°W -
Victoria Peak
Victoria Peak (British Columbia)
Victoria Peak is a mountain located in the Sutton Range of the Vancouver Island Ranges. At 2163 m, it is the third highest peak on Vancouver Island. The mountain is located on the White River valley and has no mountains of comparable elevation nearby...

 
2163 7096 50.3°N 126.6°W -
Volcanic Creek Cone
Volcanic Creek Cone
Volcanic Creek Cone is a small cinder cone northeast of Atlin in northwestern British Columbia. There are two cinder cones and a lava flow at least 3 kilometers long which is present below parts of the tree covered area. The subdued form of Volcanic Creek cone is visible directly below the largest...

 
1600 5249 59.75°N 133.45°W Holocene
The Volcano
The Volcano (British Columbia)
The Volcano, also known as Lava Fork volcano, is a small cinder cone in the Boundary Ranges of the Coast Mountains in northwestern British Columbia, Canada. It is located approximately northwest of the small community of Stewart near the head of Lava Fork...

 
1330 4364 56.42°N 130.85°W 1880 (?)
Vulcan's Thumb
Vulcan's Thumb
Vulcan's Thumb is a deeply dissected, unstable stratovolcano located directly on the southern ridge of Pyroclastic Peak. It is one of the five main volcanic peaks of the Mount Cayley massif and remains unclimbed because of technical difficulties and its loose rock...

 
2290 7500 50.11°N 123.29°W Pleistocene
Warden Peak
Warden Peak
Warden Peak is a mountain on Vancouver Island, British Columbia, Canada, located north of Gold River and north of Victoria Peak.Warden Peak is part of the Vancouver Island Ranges which in turn form part of the Insular Mountains.-Geology:...

 
1970 6463 50.3°N 126.5°W -
Watts Point volcanic centre
Watts Point volcanic centre
The Watts Point volcanic centre is a small outcrop of Pleistocene age volcanic rock at Watts Point in British Columbia, Canada, about south of Squamish and north of Vancouver, and just north of Britannia Beach. It is the southernmost volcanic zone in the Squamish volcanic field and of the...

 
240 800 49.65°N 123.21°W Pleistocene
Wetalth Ridge
Wetalth Ridge
Wetalth Ridge is an isolated ridge in northern British Columbia, Canada, located southwest of Tatogga and south of Telegraph Creek. It lies on the southwest side of Little Arctic Lake at the southwest corner of Mount Edziza Provincial Park.-History:...

 
1830 6004 57.32°N 130.78°W Pleistocene
White Creek Cone  1712 5617 52.55°N 124.84°W Pleistocene
White Horse Bluff  200 6200 51.90°N 120.11°W Pleistocene
Williams Cone
Williams Cone
Williams Cone is a satellite cone of Mount Edziza, located 36 kilometers 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...

 
2080 6824 57.78°N 130.6°W 1350 years ago
Yeda Peak
Yeda Peak
Yeda Peak is a volcano and the highest peak of the Spectrum Range in the Boundary Ranges of northwestern British Columbia, Canada, located southwest of Tatogga and south of Kitsu Peak...

 
2263 7425 57.38°N 130.68°W Pliocene

New Brunswick
New Brunswick
New Brunswick is one of Canada's three Maritime provinces and is the only province in the federation that is constitutionally bilingual . The provincial capital is Fredericton and Saint John is the most populous city. Greater Moncton is the largest Census Metropolitan Area...

Name Elevation Location Last eruption
metres feet Coordinates
Mount Pleasant Caldera
Mount Pleasant Caldera
The Mount Pleasant Caldera is a large eroded Late Devonian volcanic caldera complex, located in the northern Appalachian Mountains of southwestern New Brunswick, Canada. It is one of few noticeable pre-Cenozoic calderas, and its formation is associated to a period of crustal thinning that followed...

 
248 815 45°44′16"N 67°19′50"W Late Devonian
Sugarloaf Mountain
Sugarloaf Mountain (New Brunswick)
Sugarloaf Mountain is a mountain in the northern Appalachian Mountains in Campbellton, New Brunswick, Canada. The mountain is within Sugarloaf Provincial Park and lies within city limits, just south of the urban area...

 
305 1,001 47°59′21.9"N 66°41′15.4"W Late Devonian

Newfoundland and Labrador
Newfoundland and Labrador
Newfoundland and Labrador is the easternmost province of Canada. Situated in the country's Atlantic region, it incorporates the island of Newfoundland and mainland Labrador with a combined area of . As of April 2011, the province's estimated population is 508,400...

Name Elevation Location Last eruption
metres feet Coordinates
Flowers River caldera complex
Flowers River caldera complex
The Flowers River caldera complex is a caldera complex, located in eastern Labrador, Canada. The complex is made up of pyroclastic flow tuffs.-See also:*Volcanism of Canada*Volcanism of Eastern Canada*List of volcanoes in Canada...

 
- - - -
Fogo Seamounts
Fogo Seamounts
The Fogo Seamounts, also called the Fogo Seamount chain, are a group of seamounts located about offshore of Newfoundland and southwest of the Grand Banks of Newfoundland. They consist of basaltic submarine volcanoes that formed during the Early Cretaceous period.The volcanic activity that formed...

 
- - - Cretaceous
Cretaceous
The Cretaceous , derived from the Latin "creta" , usually abbreviated K for its German translation Kreide , is a geologic period and system from circa to million years ago. In the geologic timescale, the Cretaceous follows the Jurassic period and is followed by the Paleogene period of the...

Newfoundland Seamounts
Newfoundland Seamounts
The Newfoundland Seamounts are a group of seamounts offshore of Eastern Canada in the northern Atlantic Ocean. Named for the island of Newfoundland, this group of seamounts formed during the Cretaceous period and are poorly studied.-See also:...

 
- - - Cretaceous
Cretaceous
The Cretaceous , derived from the Latin "creta" , usually abbreviated K for its German translation Kreide , is a geologic period and system from circa to million years ago. In the geologic timescale, the Cretaceous follows the Jurassic period and is followed by the Paleogene period of the...

Springdale Caldera
Springdale Caldera
The Springdale Caldera is a large Early Silurian caldera in west-central Newfoundland, Canada. It is at least long and wide with an area more than...

 
- - - Early Silurian

Northwest Territories
Northwest Territories
The Northwest Territories is a federal territory of Canada.Located in northern Canada, the territory borders Canada's two other territories, Yukon to the west and Nunavut to the east, and three provinces: British Columbia to the southwest, and Alberta and Saskatchewan to the south...

Name Elevation Location Last eruption
metres feet Coordinates
Aristifats Diatreme
Aristifats Diatreme
The Aristifats Diatreme is a diatreme in the Northwest Territories, Canada, located about east of Yellowknife. It is thought to have formed about 1850 million years ago with the eruption of pyroclastic breccia.-See also:*Volcanism of Canada...

 
- - - Paleoproterozoic
Paleoproterozoic
The Paleoproterozoic is the first of the three sub-divisions of the Proterozoic occurring between . This is when the continents first stabilized...

Artemisia pipe
Artemisia pipe
Artemisia pipe is a diamond bearing diatreme in the Slave craton region of northern Northwest Territories, Canada.-See also:*List of volcanoes in Canada*Volcanism of Canada*Volcanism of Northern Canada...

 
- - - -
Back River volcanic complex
Back River volcanic complex
The Back River volcanic complex is an Archean stratovolcano in the Northwest Territories and Nunavut, Canada. It is located northwest of Yellowknife and to the northwest of the Back River from which it takes its name...

 
- - - Archean
Archean
The Archean , also spelled Archeozoic or Archæozoic) is a geologic eon before the Paleoproterozoic Era of the Proterozoic Eon, before 2.5 Ga ago. Instead of being based on stratigraphy, this date is defined chronometrically...

Gahcho Kué kimberlite pipes
Gahcho Kué kimberlite pipes
The Gahcho Kué kimberlite pipes is a cluster of Cambrian kimberlite diatremes located northeast of Yellowknife, Northwest Territories, Canada. It consists of four pipes: 5034, Hearne, Tuzo and Tesla.-See also:*Volcanism of Canada...

 
- - - Cambrian
Cambrian
The Cambrian is the first geological period of the Paleozoic Era, lasting from Mya ; it is succeeded by the Ordovician. Its subdivisions, and indeed its base, are somewhat in flux. The period was established by Adam Sedgwick, who named it after Cambria, the Latin name for Wales, where Britain's...

Jericho pipe
Jericho pipe
The Jericho pipe is a diamondiferous diatreme in the Slave craton of the Northwest Territories, Canada, located northeast of Yellowknife near the northern end of Contwoyto Lake. It is home to the Jericho Diamond Mine.-See also:*Volcanism of Canada...

 
- - - -
Kam Group
Kam Group
The Kam Group is a thick Archean volcanic group in the Yellowknife greenstone belt of the Northwest Territories, Canada. It consists of tholeiitic mafic and subordinate felsic volcanic rocks that were erupted in a submarine environment about 2706 million years ago.-See also:*List of volcanoes in...

 
- - - Archean
Archean
The Archean , also spelled Archeozoic or Archæozoic) is a geologic eon before the Paleoproterozoic Era of the Proterozoic Eon, before 2.5 Ga ago. Instead of being based on stratigraphy, this date is defined chronometrically...

Misery Kimberlite Complex
Misery Kimberlite Complex
The Misery Kimberlite Complex is a diatreme cluster in the Northwest Territories, Canada. It was formed approximately 56 million years ago by several overlapping explosive eruptions and intrusions. All seem to have been structurally controlled by zones of weakness related with faults, dikes and a...

 
- - - Paleogene
Paleogene
The Paleogene is a geologic period and system that began 65.5 ± 0.3 and ended 23.03 ± 0.05 million years ago and comprises the first part of the Cenozoic Era...

Mountain Diatreme
Mountain Diatreme
The Mountain Diatreme is a diatreme in the Northwest Territories, Canada, located southwest of Norman Wells. It has a diameter of and is one of the nearly 100 diatremes in the central Mackenzie Mountains.-See also:*Volcanism of Canada...

 
- - - -

Nunavut
Nunavut
Nunavut is the largest and newest federal territory of Canada; it was separated officially from the Northwest Territories on April 1, 1999, via the Nunavut Act and the Nunavut Land Claims Agreement Act, though the actual boundaries had been established in 1993...

Name Elevation Location Last eruption
metres feet Coordinates
Ellesmere Island Volcanics
Ellesmere Island Volcanics
The Ellesmere Island Volcanics are a Late Cretaceous volcanic group of volcanoes and lava flows in the Qikiqtaaluk Region of northern Ellesmere Island, Nunavut, Canada.Ellesmere Island Volcanics are part of the Arctic Cordillera...

 
- - - Late Cretaceous
Late Cretaceous
The Late Cretaceous is the younger of two epochs into which the Cretaceous period is divided in the geologic timescale. Rock strata from this epoch form the Upper Cretaceous series...

Elwin Bay diatreme
Elwin Bay diatreme
The Elwin Bay diatreme, also called the Elwin Bay kimberlite, is a small post-Silurian diatreme located approximately south of Elwin Bay at the eastern margin of Somerset Island, Nunavut, Canada. It has a diameter of .-See also:*Volcanism in Canada...

 
- - - -
JD-03 pipe
JD-03 pipe
The JD-03 pipe is a kimberlite diatreme in Nunavut, Canada, located from the Jericho Diamond Mine. It was discovered in 1996 and is interpreted to be pyroclastic with intense serpentinization....

 
- - - -
Strand Fiord Formation
Strand Fiord Formation
The Strand Fiord Formation is a Late Cretaceous volcanic component, located on northwestern and west-central Axel Heiberg Island, Nunavut, Canada. The formation contains flood basalts which are found on western Axel Heiberg Island at Dragon Cliffs tall....

 
- - - Late Cretaceous
Late Cretaceous
The Late Cretaceous is the younger of two epochs into which the Cretaceous period is divided in the geologic timescale. Rock strata from this epoch form the Upper Cretaceous series...


Ontario
Ontario
Ontario is a province of Canada, located in east-central Canada. It is Canada's most populous province and second largest in total area. It is home to the nation's most populous city, Toronto, and the nation's capital, Ottawa....

Name Elevation Location Last eruption
metres feet Coordinates
Sturgeon Lake Caldera
Sturgeon Lake Caldera
Sturgeon Lake Caldera is a large extinct caldera complex in Kenora District of Northwestern Ontario, Canada. It is one the world's best preserved mineralized Neoarchean caldera complexes, containing well-preserved mafic-intermediate pillow lavas, pillow breccias, hyaloclastite and peperites,...

 
- - 49°52′13"N 91°00′10"W Neoarchean
Neoarchean
The Neoarchean is a geologic era within the Archaean. It spans the period of time from —the period being defined chronometrically and not referenced to a specific level in a rock section on Earth...

Manitou Islands
Manitou Islands (Lake Nipissing)
The Manitou Islands are a series of small islands in Lake Nipissing, in Nipissing District, Ontario, Canada. The islands form a circle and lie southwest of North Bay.-History:...

 
- - 46°15′57"N 79°34′13"W -
Callander Bay
Callander Bay
Callander Bay is a bay at the extreme east of Lake Nipissing in Parry Sound District, Ontario, Canada. It is in diameter and the main community of Callander is located on its east side.-Geology:...

 
- - 46°12′47"N 79°23′03"W -
Blake River Megacaldera Complex
Blake River Megacaldera Complex
The Blake River Megacaldera Complex, also called the Blake River Group, is a giant subaqueous caldera cluster or a nested caldera system that spans across the Ontario-Quebec border in Canada....

 
- - 48°14′58"N 79°20′29"W Neoarchean
Neoarchean
The Neoarchean is a geologic era within the Archaean. It spans the period of time from —the period being defined chronometrically and not referenced to a specific level in a rock section on Earth...

Misema Caldera
Misema Caldera
The Misema Caldera is a striking 2,704-2,707 million year old caldera in Ontario and Quebec, Canada.- Geographic extent :It is the caldera that forms the Blake River Megacaldera Complex and has a diameter of 40-80 kilometers.- Composition :...

 
- - 48°14′58"N 79°24′15"W Neoarchean
Neoarchean
The Neoarchean is a geologic era within the Archaean. It spans the period of time from —the period being defined chronometrically and not referenced to a specific level in a rock section on Earth...

Attawapiskat kimberlite field
Attawapiskat kimberlite field
The Attawapiskat kimberlite field is a field of diatremes located astride the Attawapiskat River in the Hudson Bay Lowlands, in Northern Ontario, Canada...

 
- - 52°49′14"N 83°53′00"W Jurassic
Jurassic
The Jurassic is a geologic period and system that extends from about Mya to  Mya, that is, from the end of the Triassic to the beginning of the Cretaceous. The Jurassic constitutes the middle period of the Mesozoic era, also known as the age of reptiles. The start of the period is marked by...

Lake Timiskaming kimberlite field
Lake Timiskaming kimberlite field
The Lake Timiskaming kimberlite field is Canada's southermost kimberlite field, located in Northeastern Ontario and western Quebec, Canada. It is within the Lake Timiskaming Structural Zone which contains over 50 kimberlite pipes, several of which are diamondiferous...

 
- - 47°18′36"N 79°29′03"W Jurassic
Jurassic
The Jurassic is a geologic period and system that extends from about Mya to  Mya, that is, from the end of the Triassic to the beginning of the Cretaceous. The Jurassic constitutes the middle period of the Mesozoic era, also known as the age of reptiles. The start of the period is marked by...

Deadhorse Creek diatreme complex
Deadhorse Creek diatreme complex
The Deadhorse Creek diatreme complex is a diatreme complex in northwestern Ontario, Canada, located approximately west of Marathon. It is thought to have formed by the Midcontinent Rift System, a long rift in the center of the North American continent that was active in the Mesoproterozoic.-See...

 
- - 48°44′49"N 86°55′29"W -
Kirkland Lake kimberlite field
Kirkland Lake kimberlite field
The Kirkland Lake kimberlite field is a 165 to 152 million year old kimberlite field in the Kirkland Lake area of northeastern Ontario, Canada.-See also:*Volcanism of Canada*Volcanism of Eastern Canada*List of volcanoes in Canada...

 
- - 48°10′54"N 80°01′20"W Jurassic
Jurassic
The Jurassic is a geologic period and system that extends from about Mya to  Mya, that is, from the end of the Triassic to the beginning of the Cretaceous. The Jurassic constitutes the middle period of the Mesozoic era, also known as the age of reptiles. The start of the period is marked by...


Quebec
Quebec
Quebec or is a province in east-central Canada. It is the only Canadian province with a predominantly French-speaking population and the only one whose sole official language is French at the provincial level....

Name Elevation Location Last eruption
metres feet Coordinates
Lac des Vents volcanic complex
Lac des Vents volcanic complex
The Lac des Vents volcanic complex is a thick Archean volcanic complex in the Abitibi greenstone belt of Quebec, Canada. It is an important part of a major submarine volcanic structure....

 
- - 51°19′59"N 69°15′15"W -
Blake River Megacaldera Complex
Blake River Megacaldera Complex
The Blake River Megacaldera Complex, also called the Blake River Group, is a giant subaqueous caldera cluster or a nested caldera system that spans across the Ontario-Quebec border in Canada....

 
- - 48°14′58"N 79°20′29"W Neoarchean
Neoarchean
The Neoarchean is a geologic era within the Archaean. It spans the period of time from —the period being defined chronometrically and not referenced to a specific level in a rock section on Earth...

New Senator Caldera
New Senator Caldera
The New Senator Caldera is a large striking Archean caldera complex within the heart of the Blake River Megacaldera Complex, Quebec, Canada. It has a diameter of 15-30 kilometers and is made of thick massive mafic sequences. The caldera complex has inferred to be a subaqueous lava lake during the...

 
- - 48°26′53"N 79°24′15"W Neoarchean
Neoarchean
The Neoarchean is a geologic era within the Archaean. It spans the period of time from —the period being defined chronometrically and not referenced to a specific level in a rock section on Earth...

Noranda Caldera
Noranda Caldera
The Noranda Caldera is a well-known large subaqueous Archean caldera complex within the Blake River Megacaldera Complex, Quebec, Canada. The caldera contains a 7-to-9-km-thick succession of bimodal mafic-felsic tholeiitic to calc-alkaline volcanic rocks which were erupted during five major series...

 
- - 48°17′44"N 79°08′26"W Neoarchean
Neoarchean
The Neoarchean is a geologic era within the Archaean. It spans the period of time from —the period being defined chronometrically and not referenced to a specific level in a rock section on Earth...

Misema Caldera
Misema Caldera
The Misema Caldera is a striking 2,704-2,707 million year old caldera in Ontario and Quebec, Canada.- Geographic extent :It is the caldera that forms the Blake River Megacaldera Complex and has a diameter of 40-80 kilometers.- Composition :...

 
- - 48°14′58"N 79°24′15"W Neoarchean
Neoarchean
The Neoarchean is a geologic era within the Archaean. It spans the period of time from —the period being defined chronometrically and not referenced to a specific level in a rock section on Earth...

Lake Timiskaming kimberlite field
Lake Timiskaming kimberlite field
The Lake Timiskaming kimberlite field is Canada's southermost kimberlite field, located in Northeastern Ontario and western Quebec, Canada. It is within the Lake Timiskaming Structural Zone which contains over 50 kimberlite pipes, several of which are diamondiferous...

 
- - 47°18′36"N 79°29′03"W Jurassic
Jurassic
The Jurassic is a geologic period and system that extends from about Mya to  Mya, that is, from the end of the Triassic to the beginning of the Cretaceous. The Jurassic constitutes the middle period of the Mesozoic era, also known as the age of reptiles. The start of the period is marked by...

Hunter Mine caldera
Hunter Mine caldera
The Hunter Mine caldera is a caldera complex in the North Volcanic Zone of the Abitibi greenstone belt in Ontario and Quebec, Canada. It is located at the eastern end of Lake Abitibi....

 
- - 48°37′15"N 79°23′26"W Archean
Archean
The Archean , also spelled Archeozoic or Archæozoic) is a geologic eon before the Paleoproterozoic Era of the Proterozoic Eon, before 2.5 Ga ago. Instead of being based on stratigraphy, this date is defined chronometrically...


Saskatchewan
Saskatchewan
Saskatchewan is a prairie province in Canada, which has an area of . Saskatchewan is bordered on the west by Alberta, on the north by the Northwest Territories, on the east by Manitoba, and on the south by the U.S. states of Montana and North Dakota....

Name Elevation Location Last eruption
metres feet Coordinates
Fort à la Corne kimberlite field
Fort à la Corne kimberlite field
The Fort à la Corne kimberlite field is a 104-95 million year old diamond-bearing kimberlite field in east-central Saskatchewan, Canada. Its kimberlite pipes are among the most complete examples in the world, preserving maar-shaped craters.-See also:...

 
- - - Cretaceous
Cretaceous
The Cretaceous , derived from the Latin "creta" , usually abbreviated K for its German translation Kreide , is a geologic period and system from circa to million years ago. In the geologic timescale, the Cretaceous follows the Jurassic period and is followed by the Paleogene period of the...


Yukon
Yukon
Yukon is the westernmost and smallest of Canada's three federal territories. It was named after the Yukon River. The word Yukon means "Great River" in Gwich’in....

Name Elevation Location Last eruption
metres feet Coordinates
Alligator Lake Volcanic Complex  2217 7274 60.42°N 135.42°W Unknown
Bennett Lake Volcanic Complex
Bennett Lake Volcanic Complex
The Bennett Lake Volcanic Complex is a huge 50 million year old extinct caldera complex that spans across the BC-Yukon border in Canada. The caldera complex is surrounded by granitic rocks containing pendants....

 
1500 4900 60.3°N 134.52°W Eocene
Felsite Peak
Felsite Peak
Felsite Peak is an eroded volcanic outcrop in the Wrangell Volcanic Field, Yukon Territory, Canada, located 54 km south of Silver City, 8 km southwest of Snowshoe Peak and 30 km east of Pinnacle Peak....

 
2530 8301 60.67°N 138.23°W Pliocene
Mount Harper
Mount Harper
Mount Harper is a deeply eroded Late Proterozoic volcanic complex located north of Dawson City and west of Mount Gibben. Mount Harper is in the Ogilvie Mountains and is the thick remnant of a subaqueous-to-emergent basaltic shield volcano capped by small rhyodacitic and andesitic lava flows...

 
1845 6053 64.40°N 139.52°W Late Proterozoic
Ibex Mountain
Ibex Mountain
Ibex Mountain is a young cinder cone in the Yukon Territory, Canada, located 33 km southwest of Whitehorse and 12 km southeast of Mount Arkell. It is in a group of basaltic cones and lava flows called Alligator Lake and is in the Northern Cordilleran Volcanic Province. It is believed Ibex...

 
2108 6909 60.53°N 135.52°W Pleistocene
Mount McNeil
Mount McNeil
Mount McNeil is a rhyolite lava dome, located 41 km west of Carcross and 7 km south of Mount Skukum, Yukon Territory, Canada. It was formed during the Tertiary eruptions of the Skukum Group.-See also:*List of volcanoes in Canada...

 
2300 7546 60.8°N 135.26°W Tertiary
Montana Mountain
Montana Mountain
Montana Mountain is a deeply eroded Late Cretaceous stratovolcano located south of Carcross, Yukon, Canada. As well as its main peak, the mountain includes many sub-peaks and contains felsic pyroclastics and flows; typically altered and orange-weathering...

 
2205 7234 60.3°N 134.41°W Late Cretaceous
Mount Skukum Volcanic Complex
Mount Skukum Volcanic Complex
The Mount Skukum Volcanic Complex is an early Eocene caldera complex, located 43 km west of Carcross and 32 km northeast of Mount Porsild in the Yukon Territory, Canada. The complex composes the Skukum Group...

 
2382 7815 60.11°N 135.29°W Eocene
Mount Nansen
Mount Nansen
Mount Nansen is a prominent mountain, surmounting the steep eastern escarpment of the Eisenhower Range, 17 km south of Mount Baxter, in Victoria Land. Discovered by the British National Antarctic Expedition , and named for Fridtjof Nansen, Norwegian Arctic explorer from whom Capt...

 
1827 5994 62.6°N 137.18°W Late Cretaceous
Ne Ch'e Ddhawa
Ne Ch'e Ddhawa
Ne Ch'e Ddhawa is a cinder cone, located 7 km upstream from Fort Selkirk in the Fort Selkirk Volcanic Field, Yukon, Canada. The volcano erupted subglacially during the late Pleistocene, erupting hyaloclastite tuffs, breccias, and pillow breccias.-See also:*Volcanism of Canada*List of Northern...

 
712 2336 62.75°N 137.27°W Pleistocene
Rabbit Mountain
Rabbit Mountain
Rabbit Mountain is an eroded volcanic outcrop in the Wrangell Volcanic Field, Yukon Territory, Canada, located 30 km southwest of Koidern and 4 km northwest of Canyon Mountain. It is east of the Yukon-Alaska boundary and can be accessed by old mining roads that reach Rabbit Creek...

 
2090 6857 61.88°N 140.96°W Pliocene
Volcano Mountain
Volcano Mountain
Volcano Mountain is an active cinder cone in central Yukon Territory, Canada, located a short distance north of Fort Selkirk, near the confluence of the Pelly and Yukon Rivers...

 
1239 4065 62.93°N 137.37°W Holocene

See also

  • Volcanism of Canada
    • Volcanism of Northern Canada
      Volcanism of Northern Canada
      Volcanism of Northern Canada has led to the formation of hundreds of volcanic areas and extensive lava formations across Northern Canada, indicating volcanism played a major role in shaping its surface...

    • Volcanism of Western Canada
      Volcanism of Western Canada
      Volcanism of Western Canada produces lava flows, lava plateaus, lava domes, cinder cones, stratovolcanoes, shield volcanoes, submarine volcanoes, calderas, diatremes and maars, along with examples of more less common volcanic forms such as tuyas and subglacial mounds.-Volcanic belts:*Anahim...

    • Volcanism of Eastern Canada
      Volcanism of Eastern Canada
      Volcanism of Eastern Canada has led to the formation of hundreds of volcanic areas and extensive lava formations, indicating volcanism played a major role in shaping its surface. The region's different volcano and lava types originate from different tectonic settings and types of volcanic...

    • List of Northern Cordilleran volcanoes
  • List of mountains in Canada


External links

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