# Cocoa Crater

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Cinder cone in British Columbia, Canada

Cocoa Crater Cocoa Cone Cocoa Crater from the south Highest point Elevation 2,117 m (6,946 ft)[1] Coordinates 57°39′20″N 130°42′25″W / 57.65556°N 130.70694°W / 57.65556; -130.70694[2] Geography Cocoa Crater Location in British Columbia Location in Mount Edziza Provincial Park Country Canada[3] Province British Columbia[3] District Cassiar Land District[2] Protected area Mount Edziza Provincial Park[2] Parent range Tahltan Highland[3] Topo map NTS 104G10 Mount Edziza[2] Geology Formed by Volcanism[4] Mountain type Cinder cone[5] Rock type Hawaiite[6] Volcanic field Snowshoe Lava Field[5] Last eruption Holocene age[5]

**Cocoa Crater**, sometimes called **Cocoa Cone**, is a [cinder cone](/source/Cinder_cone) in [Cassiar Land District](/source/Cassiar_Land_District) of northwestern [British Columbia](/source/British_Columbia), Canada. It has an [elevation](/source/Elevation) of 2,117 metres (6,946 feet) and is one of several [volcanic cones](/source/Volcanic_cone) in the [Snowshoe Lava Field](/source/Snowshoe_Lava_Field) at the southern end of the [Big Raven Plateau](/source/Big_Raven_Plateau). The cone is southeast of the community of [Telegraph Creek](/source/Telegraph_Creek) in [Mount Edziza Provincial Park](/source/Mount_Edziza_Provincial_Park), which is one of the largest [provincial parks in British Columbia](/source/Provincial_parks_in_British_Columbia). Coffee Crater was the source of a 2-kilometre-wide (1.2-mile) lava flow that travelled to the northwest.

Cocoa Crater is a part of the [Mount Edziza volcanic complex](/source/Mount_Edziza_volcanic_complex), which consists of diverse landforms such as [shield volcanoes](/source/Shield_volcano), [stratovolcanoes](/source/Stratovolcano), [lava domes](/source/Lava_dome) and cinder cones. The cone contains a [volcanic crater](/source/Volcanic_crater) and was the source of a 2 km (1.2 mi) wide lava flow that travelled northwest on the Big Raven Plateau into the upper portion of [Sezill Creek](/source/Sezill_Creek) canyon. Cocoa Crater is surrounded by a number of other volcanic features, including Punch Cone, [Koosick Bluff](/source/Koosick_Bluff), [Coffee Crater](/source/Coffee_Crater), [Keda Cone](/source/Keda_Cone) and Hoia Bluff.

## Name and etymology

The name of the cone became official on May 6, 1954, and was adopted on the [National Topographic System](/source/National_Topographic_System) map 104G.[2][7] In his 1992 report *The Late Cenozoic Mount Edziza Volcanic Complex, British Columbia*, Canadian volcanologist [Jack Souther](/source/Jack_Souther) gave Cocoa Crater the [numeronym](/source/Numeronym) SLF-10, SLF being an acronym for the [Snowshoe Lava Field](/source/Snowshoe_Lava_Field).[8] Cocoa Crater is called *Cocoa Cone* in the Catalogue of Canadian volcanoes, an online database provided by [Natural Resources Canada](/source/Natural_Resources_Canada).[5] *Cocoa* is a reference to the [cone](/source/Volcanic_cone)'s deep colours.[9]

## Geography

Cocoa Crater is located in [Cassiar Land District](/source/Cassiar_Land_District) of northwestern [British Columbia](/source/British_Columbia), Canada, immediately southwest of [Mount Edziza](/source/Mount_Edziza) at the southern end of the [Big Raven Plateau](/source/Big_Raven_Plateau).[2][3][10] It has an [elevation](/source/Elevation) of 2,117 m (6,946 ft) and is the largest [subaerial](/source/Subaerial) cone in the [Snowshoe Lava Field](/source/Snowshoe_Lava_Field), one of the largest areas of [Holocene](/source/Holocene) lava flows in the [Mount Edziza volcanic complex](/source/Mount_Edziza_volcanic_complex).[1][6][11] The volcanic complex consists of a group of overlapping [shield volcanoes](/source/Shield_volcano), [stratovolcanoes](/source/Stratovolcano), [lava domes](/source/Lava_dome) and [cinder cones](/source/Cinder_cone) that have formed over the last 7.5 million years.[12] As its name suggests, Cocoa Crater contains a [volcanic crater](/source/Volcanic_crater); such features are common among cinder cones.[1][13] The cone is near the southwestern end of [Tencho Glacier](/source/Tencho_Glacier), the largest glacier of the Mount Edziza volcanic complex.[6][14]

Cocoa Crater is surrounded by a number of other landforms within the Mount Edziza volcanic complex. Just northeast of Cocoa Crater is Punch Cone, an older volcanic feature on the western side of Tencho Glacier. [Koosick Bluff](/source/Koosick_Bluff) immediately north of Cocoa Crater is another volcanic feature older than Punch Cone. About 3 km (1.9 mi) southwest and 5 km (3.1 mi) south-southeast of Cocoa Crater are [Coffee Crater](/source/Coffee_Crater) and [Keda Cone](/source/Keda_Cone), respectively, both of which are also in the Snowshoe Lava Field.[6] Hoia Bluff, about 7 km (4.3 mi) west of Cocoa Crater, is at the southwestern edge of the Big Raven Plateau.[3][6]

Cocoa Crater lies in [Mount Edziza Provincial Park](/source/Mount_Edziza_Provincial_Park) southeast of the community of [Telegraph Creek](/source/Telegraph_Creek).[2] With an area of 266,180 hectares (657,700 acres), Mount Edziza Provincial Park is one of the largest [provincial parks in British Columbia](/source/Provincial_parks_in_British_Columbia) and was established in 1972 to preserve the volcanic landscape.[9][15] It includes not only the Mount Edziza area but also the [Spectrum Range](/source/Spectrum_Range) to the south, both of which are separated by [Raspberry Pass](/source/Raspberry_Pass).[3][9] Mount Edziza Provincial Park is in the [Tahltan Highland](/source/Tahltan_Highland), a southeast-trending [upland](/source/Upland_and_lowland) area extending along the western side of the [Stikine Plateau](/source/Stikine_Plateau).[3][16]

## Geology

As a part of the Mount Edziza volcanic complex, Cocoa Crater lies within a broad area of volcanoes called the [Northern Cordilleran Volcanic Province](/source/Northern_Cordilleran_Volcanic_Province), which extends from northwestern British Columbia northwards through [Yukon](/source/Yukon) into easternmost [Alaska](/source/Alaska).[6][17] The dominant rocks comprising these volcanoes are [alkali basalts](/source/Alkali_basalt) and [hawaiites](/source/Hawaiite), but [nephelinite](/source/Nephelinite), [basanite](/source/Basanite) and [peralkaline](/source/Peralkaline_rock) [phonolite](/source/Phonolite), [trachyte](/source/Trachyte) and [comendite](/source/Comendite) are locally abundant. These rocks were deposited by volcanic eruptions from 20 million years ago to as recently as a few hundred years ago. Volcanism in the Northern Cordilleran Volcanic Province is thought to be due to [rifting](/source/Rift) of the [North American Cordillera](/source/North_American_Cordillera), driven by changes in relative [plate motion](/source/Plate_tectonics) between the [North American](/source/North_American_Plate) and [Pacific](/source/Pacific_Plate) plates.[18]

Cocoa Crater is a hawaiitic cinder cone of the [Big Raven Formation](/source/Big_Raven_Formation), the youngest [stratigraphic unit](/source/Stratigraphic_unit) of the Mount Edziza volcanic complex.[5][6] The construction of Cocoa Crater took place during the [Holocene](/source/Holocene) and was accompanied by the eruption of [lava](/source/Lava) and [pyroclastic rocks](/source/Pyroclastic_rock).[4][6] A 2 km (1.2 mi) wide lava flow from the cone travelled to the northwest, spread across the Big Raven Plateau and entered the upper portion of [Sezill Creek](/source/Sezill_Creek) canyon.[19] It was forced to flow around the western end of Koosick Bluff due to the presence of a stagnant [valley glacier](/source/Valley_glacier) along the southern margin of the lava flow at the time of eruption.[20] In the steep-sided upper canyon of Sezill Creek, the lava front ends 180 m (590 ft) above the valley floor where [subterranean streams](/source/Subterranean_stream) emerge from under the lava flow.[21]

## See also

- [Volcanoes portal](https://en.wikipedia.org/wiki/Portal:Volcanoes)
- [Mountains portal](https://en.wikipedia.org/wiki/Portal:Mountains)

- [List of Northern Cordilleran volcanoes](/source/List_of_Northern_Cordilleran_volcanoes)

- [List of volcanoes in Canada](/source/List_of_volcanoes_in_Canada)

- [Volcanism of the Mount Edziza volcanic complex](/source/Volcanism_of_the_Mount_Edziza_volcanic_complex)

## References

1. ^ [***a***](#cite_ref-FOOTNOTEGlobal_Volcanism_Program:_EdzizaSynonyms_&_Subfeatures_1-0) [***b***](#cite_ref-FOOTNOTEGlobal_Volcanism_Program:_EdzizaSynonyms_&_Subfeatures_1-1) [***c***](#cite_ref-FOOTNOTEGlobal_Volcanism_Program:_EdzizaSynonyms_&_Subfeatures_1-2) [Global Volcanism Program: Edziza](#CITEREFGlobal_Volcanism_Program:_Edziza), Synonyms & Subfeatures.

1. ^ [***a***](#cite_ref-FOOTNOTEBC_Geographical_Names:_Cocoa_Crater_2-0) [***b***](#cite_ref-FOOTNOTEBC_Geographical_Names:_Cocoa_Crater_2-1) [***c***](#cite_ref-FOOTNOTEBC_Geographical_Names:_Cocoa_Crater_2-2) [***d***](#cite_ref-FOOTNOTEBC_Geographical_Names:_Cocoa_Crater_2-3) [***e***](#cite_ref-FOOTNOTEBC_Geographical_Names:_Cocoa_Crater_2-4) [***f***](#cite_ref-FOOTNOTEBC_Geographical_Names:_Cocoa_Crater_2-5) [***g***](#cite_ref-FOOTNOTEBC_Geographical_Names:_Cocoa_Crater_2-6) [BC Geographical Names: Cocoa Crater](#CITEREFBC_Geographical_Names:_Cocoa_Crater).

1. ^ [***a***](#cite_ref-FOOTNOTEDepartment_of_Energy,_Mines_and_Resources1989_3-0) [***b***](#cite_ref-FOOTNOTEDepartment_of_Energy,_Mines_and_Resources1989_3-1) [***c***](#cite_ref-FOOTNOTEDepartment_of_Energy,_Mines_and_Resources1989_3-2) [***d***](#cite_ref-FOOTNOTEDepartment_of_Energy,_Mines_and_Resources1989_3-3) [***e***](#cite_ref-FOOTNOTEDepartment_of_Energy,_Mines_and_Resources1989_3-4) [***f***](#cite_ref-FOOTNOTEDepartment_of_Energy,_Mines_and_Resources1989_3-5) [***g***](#cite_ref-FOOTNOTEDepartment_of_Energy,_Mines_and_Resources1989_3-6) [Department of Energy, Mines and Resources 1989](#CITEREFDepartment_of_Energy,_Mines_and_Resources1989).

1. ^ [***a***](#cite_ref-FOOTNOTESouther199227_4-0) [***b***](#cite_ref-FOOTNOTESouther199227_4-1) [Souther 1992](#CITEREFSouther1992), p. 27.

1. ^ [***a***](#cite_ref-FOOTNOTENatural_Resources_Canada:_Cocoa_Cone_5-0) [***b***](#cite_ref-FOOTNOTENatural_Resources_Canada:_Cocoa_Cone_5-1) [***c***](#cite_ref-FOOTNOTENatural_Resources_Canada:_Cocoa_Cone_5-2) [***d***](#cite_ref-FOOTNOTENatural_Resources_Canada:_Cocoa_Cone_5-3) [***e***](#cite_ref-FOOTNOTENatural_Resources_Canada:_Cocoa_Cone_5-4) [Natural Resources Canada: Cocoa Cone](#CITEREFNatural_Resources_Canada:_Cocoa_Cone).

1. ^ [***a***](#cite_ref-FOOTNOTESouther1988_6-0) [***b***](#cite_ref-FOOTNOTESouther1988_6-1) [***c***](#cite_ref-FOOTNOTESouther1988_6-2) [***d***](#cite_ref-FOOTNOTESouther1988_6-3) [***e***](#cite_ref-FOOTNOTESouther1988_6-4) [***f***](#cite_ref-FOOTNOTESouther1988_6-5) [***g***](#cite_ref-FOOTNOTESouther1988_6-6) [***h***](#cite_ref-FOOTNOTESouther1988_6-7) [Souther 1988](#CITEREFSouther1988).

1. **[^](#cite_ref-FOOTNOTEGeographical_Names_Data_Base:_Cocoa_Crater_7-0)** [Geographical Names Data Base: Cocoa Crater](#CITEREFGeographical_Names_Data_Base:_Cocoa_Crater).

1. **[^](#cite_ref-FOOTNOTESouther1992214_8-0)** [Souther 1992](#CITEREFSouther1992), p. 214.

1. ^ [***a***](#cite_ref-FOOTNOTEBC_Parks:_Mount_Edziza_Provincial_Park_9-0) [***b***](#cite_ref-FOOTNOTEBC_Parks:_Mount_Edziza_Provincial_Park_9-1) [***c***](#cite_ref-FOOTNOTEBC_Parks:_Mount_Edziza_Provincial_Park_9-2) [BC Parks: Mount Edziza Provincial Park](#CITEREFBC_Parks:_Mount_Edziza_Provincial_Park).

1. **[^](#cite_ref-FOOTNOTEBC_Geographical_Names:_Cassiar_Land_District_10-0)** [BC Geographical Names: Cassiar Land District](#CITEREFBC_Geographical_Names:_Cassiar_Land_District).

1. **[^](#cite_ref-FOOTNOTESouther1992214,_229_11-0)** [Souther 1992](#CITEREFSouther1992), pp. 214, 229.

1. **[^](#cite_ref-FOOTNOTESouther1990124,_125_12-0)** [Souther 1990](#CITEREFSouther1990), pp. 124, 125.

1. **[^](#cite_ref-FOOTNOTEUnited_States_Geological_Survey2011_13-0)** [United States Geological Survey 2011](#CITEREFUnited_States_Geological_Survey2011).

1. **[^](#cite_ref-FOOTNOTEBC_Geographical_Names:_Tencho_Glacier_14-0)** [BC Geographical Names: Tencho Glacier](#CITEREFBC_Geographical_Names:_Tencho_Glacier).

1. **[^](#cite_ref-FOOTNOTEGlobal_Volcanism_Program:_EdzizaPhoto_Gallery_15-0)** [Global Volcanism Program: Edziza](#CITEREFGlobal_Volcanism_Program:_Edziza), Photo Gallery.

1. **[^](#cite_ref-FOOTNOTEHolland197649_16-0)** [Holland 1976](#CITEREFHolland1976), p. 49.

1. **[^](#cite_ref-FOOTNOTEEdwardsRussell20001280,_1281,_1283,_1284_17-0)** [Edwards & Russell 2000](#CITEREFEdwardsRussell2000), pp. 1280, 1281, 1283, 1284.

1. **[^](#cite_ref-FOOTNOTEEdwardsRussell20001280_18-0)** [Edwards & Russell 2000](#CITEREFEdwardsRussell2000), p. 1280.

1. **[^](#cite_ref-FOOTNOTESouther1992230_19-0)** [Souther 1992](#CITEREFSouther1992), p. 230.

1. **[^](#cite_ref-FOOTNOTESouther1992232,_233_20-0)** [Souther 1992](#CITEREFSouther1992), pp. 232, 233.

1. **[^](#cite_ref-FOOTNOTESouther1992230,_232_21-0)** [Souther 1992](#CITEREFSouther1992), pp. 230, 232.

### Sources

- "A 502" (Topographic map). [*Telegraph Creek, Cassiar Land District, British Columbia*](https://web.archive.org/web/20210502071600/https://volcano.si.edu/maps/GVAlaskaCanada/G910509-006.jpg) (3 ed.). 1:250,000. 104 G (in English and French). [Department of Energy, Mines and Resources](/source/Department_of_Energy%2C_Mines_and_Resources). 1989. Archived from [the original](https://volcano.si.edu/maps/GVAlaskaCanada/G910509-006.jpg) on May 2, 2021.

- ["Cassiar Land District"](https://web.archive.org/web/20180627144631/http://apps.gov.bc.ca/pub/bcgnws/names/41229.html). *[BC Geographical Names](/source/BC_Geographical_Names)*. Government of British Columbia – B.C. Geographical Names Office (BCGNO). Archived from [the original](https://apps.gov.bc.ca/pub/bcgnws/names/41229.html) on June 27, 2018.

- ["Cocoa Crater"](https://web.archive.org/web/20211001001856/https://apps.gov.bc.ca/pub/bcgnws/names/10266.html). *[BC Geographical Names](/source/BC_Geographical_Names)*. Government of British Columbia – B.C. Geographical Names Office (BCGNO). Archived from [the original](https://apps.gov.bc.ca/pub/bcgnws/names/10266.html) on October 1, 2021.

- ["Cocoa Cone"](https://web.archive.org/web/20101212060930/http://gsc.nrcan.gc.ca/volcanoes/cat/volcano_e.php?id=svb_ccn_088). *Catalogue of Canadian Volcanoes*. [Natural Resources Canada](/source/Natural_Resources_Canada). March 10, 2009. Archived from [the original](http://gsc.nrcan.gc.ca/volcanoes/cat/volcano_e.php?id=svb_ccn_088) on December 12, 2010.

- ["Cocoa Crater"](https://geonames.nrcan.gc.ca/search-place-names/unique?id=JASFK). *[Geographical Names Data Base](/source/GeoBase_(geospatial_data)#Geographical_Names_Data_Base)*. [Natural Resources Canada](/source/Natural_Resources_Canada). Retrieved February 9, 2025.

- Edwards, Benjamin R.; Russell, James K. (2000). "Distribution, Nature, and Origin of Neogene–Quaternary Magmatism in the Northern Cordilleran Volcanic Province, Canada". *[Geological Society of America Bulletin](/source/Geological_Society_of_America_Bulletin)*. **112** (8). [Geological Society of America](/source/Geological_Society_of_America): 1280–1295. [Bibcode](/source/Bibcode_(identifier)):[2000GSAB..112.1280E](https://ui.adsabs.harvard.edu/abs/2000GSAB..112.1280E). [doi](/source/Doi_(identifier)):[10.1130/0016-7606(2000)112<1280:dnaoon>2.0.co;2](https://doi.org/10.1130%2F0016-7606%282000%29112%3C1280%3Adnaoon%3E2.0.co%3B2). [ISSN](/source/ISSN_(identifier)) [0016-7606](https://search.worldcat.org/issn/0016-7606).

- ["Edziza"](https://web.archive.org/web/20250114000000/https://volcano.si.edu/volcano.cfm?vn=320060). *[Global Volcanism Program](/source/Global_Volcanism_Program)*. [Smithsonian Institution](/source/Smithsonian_Institution). Archived from [the original](https://volcano.si.edu/volcano.cfm?vn=320060) on January 14, 2025.

- Holland, Stuart S. (1976). [Landforms of British Columbia: A Physiographic Outline](https://web.archive.org/web/20181114024907/http://cmscontent.nrs.gov.bc.ca/geoscience/PublicationCatalogue/Bulletin/BCGS_B048.pdf) (PDF) (Report). Vol. 48. [Government of British Columbia](/source/Government_of_British_Columbia). [ASIN](/source/ASIN_(identifier)) [B0006EB676](https://www.amazon.com/dp/B0006EB676). [OCLC](/source/OCLC_(identifier)) [601782234](https://search.worldcat.org/oclc/601782234). Archived from [the original](http://cmscontent.nrs.gov.bc.ca/geoscience/PublicationCatalogue/Bulletin/BCGS_B048.pdf) (PDF) on November 14, 2018.

- ["Mount Edziza Provincial Park"](https://web.archive.org/web/20230123120553/https://bcparks.ca/explore/parkpgs/mt_edziza/). [BC Parks](/source/BC_Parks). Archived from [the original](https://bcparks.ca/explore/parkpgs/mt_edziza/) on January 23, 2023.

- ["Principal Types of Volcanoes"](https://web.archive.org/web/20241224113216/https://pubs.usgs.gov/gip/volc/types.html). [United States Geological Survey](/source/United_States_Geological_Survey). January 3, 2011. Archived from [the original](https://pubs.usgs.gov/gip/volc/types.html) on December 24, 2024.

- [Souther, J. G.](/source/Jack_Souther) (1988). "1623A" ([Geological map](/source/Geological_map)). *Geology, Mount Edziza Volcanic Complex, British Columbia*. 1:50,000. Cartography by M. Sigouin, [Geological Survey of Canada](/source/Geological_Survey_of_Canada). [Energy, Mines and Resources Canada](/source/Energy%2C_Mines_and_Resources_Canada). [doi](/source/Doi_(identifier)):[10.4095/133498](https://doi.org/10.4095%2F133498).

- [Souther, J. G.](/source/Jack_Souther) (1990). Wood, Charles A.; Kienle, Jürgen (eds.). [*Volcanoes of North America: United States and Canada*](https://books.google.com/books?id=eyDRib-FJh4C). [Cambridge University Press](/source/Cambridge_University_Press). [ISBN](/source/ISBN_(identifier)) [0-521-43811-X](https://en.wikipedia.org/wiki/Special:BookSources/0-521-43811-X).

- [Souther, J. G.](/source/Jack_Souther) (1992). The Late Cenozoic Mount Edziza Volcanic Complex, British Columbia. *[Geological Survey of Canada](/source/Geological_Survey_of_Canada)* (Report). Memoir 420. Canada Communication Group. [doi](/source/Doi_(identifier)):[10.4095/133497](https://doi.org/10.4095%2F133497). [ISBN](/source/ISBN_(identifier)) [0-660-14407-7](https://en.wikipedia.org/wiki/Special:BookSources/0-660-14407-7).

- ["Tencho Glacier"](https://web.archive.org/web/20240607215233/https://apps.gov.bc.ca/pub/bcgnws/names/15009.html). *[BC Geographical Names](/source/BC_Geographical_Names)*. Government of British Columbia – B.C. Geographical Names Office (BCGNO). Archived from [the original](https://apps.gov.bc.ca/pub/bcgnws/names/15009.html) on June 7, 2024.

## External links

- ["Cocoa Crater, British Columbia"](http://www.peakbagger.com/peak.aspx?pid=51407). *Peakbagger.com*.

v t e Mount Edziza volcanic complex Cinder cones The Ash Pit Cache Hill Camp Hill Cinder Cliff Cocoa Crater Coffee Crater Eve Cone Exile Hill Icefall Cone Kana Cone Keda Cone Klastline Cone Mess Lake Cone Moraine Cone Nahta Cone Outcast Hill Ridge Cone Sidas Cone Sleet Cone Source Hill Storm Cone Thaw Hill Triplex Cones Twin Cone Walkout Creek centres Williams Cone Subglacial volcanoes Pillow Ridge Tennena Cone Tsekone Ridge Wetalth Ridge Central volcanoes Armadillo Peak Mount Edziza Ice Peak Spectrum Range Lava domes Glacier Dome IGC Centre Nanook Dome Pharaoh Dome The Pyramid Sphinx Dome Triangle Dome Lava fields Desolation Lava Field Mess Lake Lava Field Snowshoe Lava Field Plateaus Arctic Lake Plateau Big Raven Plateau Kitsu Plateau Ridges Artifact Ridge Cartoona Ridge Idiji Ridge Obsidian Ridge Pillow Ridge Sorcery Ridge Tsekone Ridge Wetalth Ridge Yagi Ridge Mountain passes Destell Pass Raspberry Pass Bluffs Koosick Bluff Ornostay Bluff Glaciers Idiji Glacier Tenchen Glacier Tencho Glacier Tennaya Glacier Streams Artifact Creek Ball Creek Bourgeaux Creek Chakima Creek Crayke Creek Elwyn Creek Flyin Creek Gerlib Creek Kadeya Creek Kitsu Creek Little Iskut River More Creek Nagha Creek Nido Creek Pyramid Creek Raspberry Creek Sezill Creek Shaman Creek Sorcery Creek Stewbomb Creek Tadekho Creek Taweh Creek Tenchen Creek Tennaya Creek Tsecha Creek Walkout Creek Stratigraphic units Armadillo Formation Big Raven Formation (Sheep Track Member) Edziza Formation Ice Peak Formation Kakiddi Formation Klastline Formation Little Iskut Formation Nido Formation (Tenchen Member) Pyramid Formation Raspberry Formation Other Cartoona Peak Gnu Butte Mess Creek Escarpment Volcanism of the Mount Edziza volcanic complex

v t e Volcanoes of the Northern Cordilleran Volcanic Province Cinder cones Cache Hill Camp Hill Cinder Cliff Cinder Mountain Cocoa Crater Coffee Crater Cone Glacier Volcano Cracker Creek Cone Eve Cone Exile Hill Fort Selkirk Vent Gabrielse Cone Icefall Cone Ibex Mountain Iskut Canyon Cone Kana Cone Keda Cone Klastline Cone Mess Lake Cone Moraine Cone Ne Ch'e Ddhawa Nahta Cone Outcast Hill Prindle Volcano Ridge Cone Ruby Mountain Second Canyon Cone Sidas Cone Sleet Cone Snippaker Creek Cone Source Hill Storm Cone Thaw Hill The Saucer The Volcano Triplex Cones Tseax Cone Twin Cone Volcanic Creek Cone Volcano Mountain Walkout Creek Cone Watson Lake Cone Williams Cone Subglacial volcanoes Ash Mountain Chakatah Creek Peak Caribou Tuya Dark Mountain Dome Mountain Enid Creek Cone Isspah Butte Kawdy Mountain King Creek Cone Klinkit Creek Peak Klinkit Lake Peak Little Bear Mountain Little Eagle Cone Mathews Tuya Meehaz Mountain Mount Josephine Nuthinaw Mountain Pillow Ridge South Tuya Tennena Cone Tadekho Hill Toozaza Peak Tom MacKay Creek Cone Tsekone Ridge Tutsingale Mountain Tuya Butte Wetalth Ridge Lava domes Cartoona Peak Glacier Dome IGC Centre Nanook Dome Pharaoh Dome Sezill Volcano Sphinx Dome The Pyramid Triangle Dome Shield volcanoes Grizzly Butte Heart Peaks Level Mountain Maitland Volcano Spectrum Range Volcano Vent West Vent Volcanic fields Atlin Bell-Irving Desolation Fort Selkirk Mess Lake Snowshoe Tuya Stratovolcanoes Armadillo Peak Hoodoo Mountain Ice Peak Mount Edziza Volcanic plugs Castle Rock The Neck The Thumb

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Adapted from the Wikipedia article [Cocoa Crater](https://en.wikipedia.org/wiki/Cocoa_Crater) by Wikipedia contributors ([contributor history](https://en.wikipedia.org/wiki/Cocoa_Crater?action=history)). Available under [Creative Commons Attribution-ShareAlike 4.0 International](https://creativecommons.org/licenses/by-sa/4.0/). Changes may have been made.