# Eve Cone

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Cinder cone in British Columbia, Canada

Eve Cone Eve's Cone Eve Cone from the northeast Highest point Elevation 1,740 m (5,710 ft)[1] Coordinates 57°48′47″N 130°40′32″W / 57.81306°N 130.67556°W / 57.81306; -130.67556[2] Naming Etymology Eve Brown Edzerza[2] Defining authority BC Geographical Names office in Victoria, British Columbia[2][3] Geography Eve Cone Location in British Columbia Location in Mount Edziza Provincial Park Country Canada[4] Province British Columbia[4] District Cassiar Land District[2] Protected area Mount Edziza Provincial Park[2] Parent range Tahltan Highland[4] Topo map NTS 104G15 Buckley Lake[2] Geology Formed by Volcanism[5] Mountain type Cinder cone[6] Rock type Hawaiite[7] Volcanic field Desolation Lava Field[7] Last eruption Holocene age[6] Climbing Normal route Trail on the southeastern flank[8]

**Eve Cone**, also known as **Eve's 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 1,740 metres (5,710 feet) and is one of several [volcanic cones](/source/Volcanic_cone) in the [Desolation Lava Field](/source/Desolation_Lava_Field) at the northern end of the [Big Raven Plateau](/source/Big_Raven_Plateau). Situated southeast of the community of [Telegraph Creek](/source/Telegraph_Creek), it lies in [Mount Edziza Provincial Park](/source/Mount_Edziza_Provincial_Park), one of the largest [provincial parks in British Columbia](/source/Provincial_parks_in_British_Columbia). A roughly 12-kilometre-long (7.5-mile) [lava field](/source/Lava_field) issued from Eve Cone during the [Holocene](/source/Holocene) and travelled down the northern side of the Big Raven Plateau. It branches out into much narrower [channels](/source/Lava_channel), the largest extending to [Buckley Lake](/source/Buckley_Lake_(British_Columbia)).

Eve Cone is 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 circular summit [crater](/source/Volcanic_crater) 45 m (148 ft) deep but most of the lava from the volcano appears to have issued from vents around the base of the 350 m (1,150 ft) wide cone. Eve Cone is surrounded by a number of other volcanic features, including [Tsekone Ridge](/source/Tsekone_Ridge), [Pillow Ridge](/source/Pillow_Ridge), [Sidas Cone](/source/Sidas_Cone) and the [Triplex Cones](/source/Triplex_Cones). Access is via [horse trails](/source/Horse_trail) from Telegraph Creek and [Iskut](/source/Iskut), although landing on Buckley Lake with float-equipped aircraft is also promoted to reach Eve Cone.

## Name and etymology

[Jack Souther](/source/Jack_Souther), a [geologist](/source/Geologist) of the Geological Survey of Canada who studied the area in detail from 1965 to 1992, named the cone after Eve Brown Edzerza.[2][9][10] Edzerza was a local indigenous woman who traversed [Mount Edziza](/source/Mount_Edziza) by dog sled with her husband, [Johnny Edzerza](/source/Johnny_Edzerza), and a man named [Hank Williams](/source/Hank_Williams_(Tahltan_man)) in or before 1974.[2][11][12] Johnny and Hank were killed in an [avalanche](/source/Avalanche) on the mountain during a vicious snowstorm that had blown in from the north, but Eve survived, directing a rescue team to the site of the accident.[2][12]

Hank Williams and the Edzerzas were [Tahltans](/source/Tahltan), the local [First Nations](/source/First_Nations_in_British_Columbia) people whose traditional territory covers an area of more than 93,500 km2 (36,100 mi2).[12][13] Eve Edzerza's survival and saga of courage following the avalanche is a legend among the Tahltans.[12] Johnny Edzerza was buried on Mount Edziza; both *Edzerza* and *Edziza* may be [etymologically](/source/Etymologically) linked.[11] [Williams Cone](/source/Williams_Cone) on the northeastern side of the mountain was named in honour of Hank.[14]

The name of the cone became official on January 2, 1980, and was adopted on the [National Topographic System](/source/National_Topographic_System) map 104G/15 after being submitted to the [BC Geographical Names](/source/BC_Geographical_Names) office by the [Geological Survey of Canada](/source/Geological_Survey_of_Canada).[2][15] In his 1992 report *The Late Cenozoic Mount Edziza Volcanic Complex, British Columbia*, Jack Souther gave Eve Cone the [numeronym](/source/Numeronym) *DLF-9*; *DLF* is an acronym for the [Desolation Lava Field](/source/Desolation_Lava_Field) whereas *9* refers to Eve Cone being the ninth youngest eruptive centre in the Desolation Lava Field.[16] [BC Parks](/source/BC_Parks) refers to the cone as both *Eve Cone* and *Eve's Cone*.[17]

## Geography

Eve Cone is located in [Cassiar Land District](/source/Cassiar_Land_District) of northwestern [British Columbia](/source/British_Columbia), Canada, about 11 km (6.8 mi) southeast of [Buckley Lake](/source/Buckley_Lake_(British_Columbia)) at the northern end of the [Big Raven Plateau](/source/Big_Raven_Plateau).[2][4][18] It has an [elevation](/source/Elevation) of 1,740 m (5,710 ft) and is one of several [volcanic cones](/source/Volcanic_cone) in the Desolation Lava Field, which is one of the largest areas of [Holocene](/source/Holocene) lava flows of the [Mount Edziza volcanic complex](/source/Mount_Edziza_volcanic_complex).[1][7][19] 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.[20] Eve Cone is one of the most symmetrical and best-preserved cinder cones in Canada, rising 172 m (564 ft) above the surrounding [terrain](/source/Terrain) to a circular summit [crater](/source/Volcanic_crater) 45 m (148 ft) deep.[10][21][22] [Lichen](/source/Lichen) and [pioneer vegetation](/source/Pioneer_species) sparsely grows on the base of the 350 m (1,150 ft) wide cone.[21][22]

The [Smithsonian Institution](/source/Smithsonian_Institution)'s [Global Volcanism Program](/source/Global_Volcanism_Program) lists Eve Cone as one of many [satellitic cones](/source/Satellitic_cone) of Mount Edziza due to its location on the northern flank of this stratovolcano.[1][23][24] Apart from the main edifice of Mount Edziza, which reaches an elevation of 2,786 m (9,140 ft), Eve Cone is surrounded by a number of other volcanic features.[7][24] About 5 km (3.1 mi) southwest of Eve Cone is [Tsekone Ridge](/source/Tsekone_Ridge) on the northwestern flank of Mount Edziza.[4] [Pillow Ridge](/source/Pillow_Ridge), about 5 km (3.1 mi) south of Eve Cone, extends northwest from the northern flank of Mount Edziza.[4][25] About 2 km (1.2 mi) southeast of Eve Cone are the [Triplex Cones](/source/Triplex_Cones), a southeast-trending line of three deeply eroded volcanic cones.[7][26] [Sidas Cone](/source/Sidas_Cone) about 5 km (3.1 mi) northwest of Eve Cone is a composite of two overlapping cones.[4][26] The Pillow and Tsekone ridges are older volcanic features of [Pleistocene](/source/Pleistocene) age whereas Sidas Cone and the Triplex Cones are part of the younger Desolation Lava Field.[7]

Eve Cone 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.[17][27] 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).[4][17] 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).[4][28]

## Geology

### Background

As a part of the Mount Edziza volcanic complex, Eve Cone 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).[7][29] 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)[a] [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.[31]

### Structure

False colour image of lava flows from Eve and [Sidas](/source/Sidas_Cone) cones

Eve Cone is a [monogenetic](/source/Monogenetic_volcanic_field) cinder cone, which are simple volcanic edifices that erupted over a single eruptive phase.[6][32][33][34] Such features are typically considered to erupt only once and to be short-lived; they can remain active from days to years but are fed by a relatively small amount of [magma](/source/Magma).[33][35] Eve Cone consists of hawaiite of the [Big Raven Formation](/source/Big_Raven_Formation) and is one of the two youngest eruptive centres in the Desolation Lava Field, the other being Williams Cone about 6 km (3.7 mi) to the southeast.[4][7][21] Both cones are of Holocene age but Eve Cone was most likely formed by a towering, vertical [lava fountain](/source/Lava_fountain) due to its symmetrical structure.[5][7] Loosely [aggregated](/source/Aggregate_(geology)) volcanic [ejecta](/source/Ejecta) such as [bombs](/source/Volcanic_bomb), [cinders](/source/Scoria) and [ash](/source/Volcanic_ash) cover the outer surface of Eve Cone.[21]

Relatively fine, dark grey bombs and cinders cover the northern half of Eve Cone whereas coarser, clinkery [spatter](/source/Volcanic_spatter) is exposed in the more deeply eroded southern half of the cone. Erosion on the southern flank is more extreme due to accelerated [frost wedging](/source/Frost_wedging) and [solifluction](/source/Solifluction)[b] which may be caused by greater and more frequent temperature changes.[21] In contrast to Williams Cone, whose surroundings are at least still partially covered with fine ash from its eruption, ash from the Eve Cone eruption has completely eroded away from the surrounding landscape; this suggests Eve Cone is older than Williams Cone.[37]

### Lava field

Nearly all of the lava erupted from Eve Cone appears to have originated from vents around the base of the volcanic edifice. This is particularly evident on the southeastern side of the cone, where there is a nearly 30 m (98 ft) high buttress of overlapping tiers of lava lobes.[21] Streams of lava from these vents merged to form a roughly 12 km (7.5 mi) long [lava field](/source/Lava_field) which extends down the northern side of the Big Raven Plateau. It has a maximum width of about 6 km (3.7 mi), overlies older lava flows from the Triplex Cones and abuts with older lava flows in the northeast from Sidas Cone. The lava flows comprising this field branch out into much narrower [lava channels](/source/Lava_channel) to the north and northwest, the largest of which is approximately 6 km (3.7 mi) long; it reaches the northeastern end of Buckley Lake. A shorter channel just south of Buckley Lake forms a lava bed with the Triplex Cones lava flows.[7]

## Accessibility

Eve Cone from the southeast

Eve Cone is in a remote location with no established road access.[38] The closest roads are the [Stewart–Cassiar Highway](/source/Stewart%E2%80%93Cassiar_Highway) to the east and the Telegraph Creek Road to the northwest; both come within 40 km (25 mi) of the cone.[4][39][40] Extending from these roads are [horse trails](/source/Horse_trail) that provide access to the Mount Edziza volcanic complex.[39] From Telegraph Creek, the Buckley Lake Trail extends about 15 km (9.3 mi) southeast along [Mess Creek](/source/Mess_Creek) and Three Mile Lake. It then traverses about 15 km (9.3 mi) northeast along Dagaichess Creek and Stinking Lake to the northeastern end of Buckley Lake. Here, it meets with the Klastline River Trail and the Buckley Lake to Mowdade Lake Route, the latter of which ascends onto the gently sloping northern side of the plateau.[41]

To the east, the roughly 50 km (31 mi) long Klastline River Trail begins at the community of [Iskut](/source/Iskut) on the Stewart–Cassiar Highway; it extends northwest and west along the Klastline River for much of its length.[40] The trail enters Mount Edziza Provincial Park at about 25 km (16 mi) where Kakiddi Creek drains into the Klastline River.[42] After entering Mount Edziza Provincial Park, it traverses northwest along the Klastline River for about 10 km (6.2 mi) and then crosses the river north of the Big Raven Plateau.[40] From there, it traverses west for about 5 km (3.1 mi) to the northeastern end of Buckley Lake where it meets with the Buckley Lake Trail and the Buckley Lake to Mowdade Lake Route.[41]

The Buckley Lake to Mowdade Lake Route traverses south from Buckley Lake along Buckley Creek and gradually climbs onto the northern end of the Big Raven Plateau where Eve Cone and Sidas Cone are visible along the route.[4][8][41] BC Parks recommends visitors ascend Eve Cone using the main trail on its southeastern flank to prevent foot scarring on its delicate surface. This route leads to a small bench on the northeastern side of the cone and provides access to the crater rim.[8] Buckley Lake northwest of Eve Cone is large enough to be used by float-equipped aircraft.[4][17] However, landing on this lake with a private aircraft requires a letter of authorization from the BC Parks Stikine Senior Park Ranger. As of 2023, Alpine Lakes Air and BC Yukon Air are the only air charter companies permitted to provide access to this area via aircraft.[17]

## 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)

## Notes

1. **[^](#cite_ref-31)** *Peralkaline rocks* are magmatic rocks that have a higher ratio of sodium and potassium to aluminum.[30]

1. **[^](#cite_ref-38)** *Solifluction* is [soil creep](/source/Soil_creep) caused by waterlogged soil slowly moving downhill on top of an impermeable layer.[36]

## 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:_Eve_Cone_2-0) [***b***](#cite_ref-FOOTNOTEBC_Geographical_Names:_Eve_Cone_2-1) [***c***](#cite_ref-FOOTNOTEBC_Geographical_Names:_Eve_Cone_2-2) [***d***](#cite_ref-FOOTNOTEBC_Geographical_Names:_Eve_Cone_2-3) [***e***](#cite_ref-FOOTNOTEBC_Geographical_Names:_Eve_Cone_2-4) [***f***](#cite_ref-FOOTNOTEBC_Geographical_Names:_Eve_Cone_2-5) [***g***](#cite_ref-FOOTNOTEBC_Geographical_Names:_Eve_Cone_2-6) [***h***](#cite_ref-FOOTNOTEBC_Geographical_Names:_Eve_Cone_2-7) [***i***](#cite_ref-FOOTNOTEBC_Geographical_Names:_Eve_Cone_2-8) [***j***](#cite_ref-FOOTNOTEBC_Geographical_Names:_Eve_Cone_2-9) [***k***](#cite_ref-FOOTNOTEBC_Geographical_Names:_Eve_Cone_2-10) [***l***](#cite_ref-FOOTNOTEBC_Geographical_Names:_Eve_Cone_2-11) [BC Geographical Names: Eve Cone](#CITEREFBC_Geographical_Names:_Eve_Cone).

1. **[^](#cite_ref-FOOTNOTEGovernment_of_Canada:_Geographical_Names_Board_of_Canada_3-0)** [Government of Canada: Geographical Names Board of Canada](#CITEREFGovernment_of_Canada:_Geographical_Names_Board_of_Canada).

1. ^ [***a***](#cite_ref-FOOTNOTEDepartment_of_Energy,_Mines_and_Resources1989_4-0) [***b***](#cite_ref-FOOTNOTEDepartment_of_Energy,_Mines_and_Resources1989_4-1) [***c***](#cite_ref-FOOTNOTEDepartment_of_Energy,_Mines_and_Resources1989_4-2) [***d***](#cite_ref-FOOTNOTEDepartment_of_Energy,_Mines_and_Resources1989_4-3) [***e***](#cite_ref-FOOTNOTEDepartment_of_Energy,_Mines_and_Resources1989_4-4) [***f***](#cite_ref-FOOTNOTEDepartment_of_Energy,_Mines_and_Resources1989_4-5) [***g***](#cite_ref-FOOTNOTEDepartment_of_Energy,_Mines_and_Resources1989_4-6) [***h***](#cite_ref-FOOTNOTEDepartment_of_Energy,_Mines_and_Resources1989_4-7) [***i***](#cite_ref-FOOTNOTEDepartment_of_Energy,_Mines_and_Resources1989_4-8) [***j***](#cite_ref-FOOTNOTEDepartment_of_Energy,_Mines_and_Resources1989_4-9) [***k***](#cite_ref-FOOTNOTEDepartment_of_Energy,_Mines_and_Resources1989_4-10) [***l***](#cite_ref-FOOTNOTEDepartment_of_Energy,_Mines_and_Resources1989_4-11) [***m***](#cite_ref-FOOTNOTEDepartment_of_Energy,_Mines_and_Resources1989_4-12) [Department of Energy, Mines and Resources 1989](#CITEREFDepartment_of_Energy,_Mines_and_Resources1989).

1. ^ [***a***](#cite_ref-FOOTNOTESouther199227_5-0) [***b***](#cite_ref-FOOTNOTESouther199227_5-1) [Souther 1992](#CITEREFSouther1992), p. 27.

1. ^ [***a***](#cite_ref-FOOTNOTENatural_Resources_Canada:_Eve_Cone_6-0) [***b***](#cite_ref-FOOTNOTENatural_Resources_Canada:_Eve_Cone_6-1) [***c***](#cite_ref-FOOTNOTENatural_Resources_Canada:_Eve_Cone_6-2) [Natural Resources Canada: Eve Cone](#CITEREFNatural_Resources_Canada:_Eve_Cone).

1. ^ [***a***](#cite_ref-FOOTNOTESouther1988_7-0) [***b***](#cite_ref-FOOTNOTESouther1988_7-1) [***c***](#cite_ref-FOOTNOTESouther1988_7-2) [***d***](#cite_ref-FOOTNOTESouther1988_7-3) [***e***](#cite_ref-FOOTNOTESouther1988_7-4) [***f***](#cite_ref-FOOTNOTESouther1988_7-5) [***g***](#cite_ref-FOOTNOTESouther1988_7-6) [***h***](#cite_ref-FOOTNOTESouther1988_7-7) [***i***](#cite_ref-FOOTNOTESouther1988_7-8) [***j***](#cite_ref-FOOTNOTESouther1988_7-9) [Souther 1988](#CITEREFSouther1988).

1. ^ [***a***](#cite_ref-FOOTNOTEBC_Parks:_Hiking_and_Wilderness_Camping_in_Mount_Edziza_Provincial_Park_8-0) [***b***](#cite_ref-FOOTNOTEBC_Parks:_Hiking_and_Wilderness_Camping_in_Mount_Edziza_Provincial_Park_8-1) [***c***](#cite_ref-FOOTNOTEBC_Parks:_Hiking_and_Wilderness_Camping_in_Mount_Edziza_Provincial_Park_8-2) [BC Parks: Hiking and Wilderness Camping in Mount Edziza Provincial Park](#CITEREFBC_Parks:_Hiking_and_Wilderness_Camping_in_Mount_Edziza_Provincial_Park).

1. **[^](#cite_ref-FOOTNOTESouther196689_9-0)** [Souther 1966](#CITEREFSouther1966), p. 89.

1. ^ [***a***](#cite_ref-FOOTNOTENatural_Resources_Canada:_Mount_Edziza_10-0) [***b***](#cite_ref-FOOTNOTENatural_Resources_Canada:_Mount_Edziza_10-1) [Natural Resources Canada: Mount Edziza](#CITEREFNatural_Resources_Canada:_Mount_Edziza).

1. ^ [***a***](#cite_ref-FOOTNOTEBC_Geographical_Names:_Mount_Edziza_11-0) [***b***](#cite_ref-FOOTNOTEBC_Geographical_Names:_Mount_Edziza_11-1) [BC Geographical Names: Mount Edziza](#CITEREFBC_Geographical_Names:_Mount_Edziza).

1. ^ [***a***](#cite_ref-FOOTNOTESouther2009_12-0) [***b***](#cite_ref-FOOTNOTESouther2009_12-1) [***c***](#cite_ref-FOOTNOTESouther2009_12-2) [***d***](#cite_ref-FOOTNOTESouther2009_12-3) [Souther 2009](#CITEREFSouther2009).

1. **[^](#cite_ref-FOOTNOTEMarkeyHalsethManson2012242_13-0)** [Markey, Halseth & Manson 2012](#CITEREFMarkeyHalsethManson2012), p. 242.

1. **[^](#cite_ref-FOOTNOTEBC_Geographical_Names:_Williams_Cone_14-0)** [BC Geographical Names: Williams Cone](#CITEREFBC_Geographical_Names:_Williams_Cone).

1. **[^](#cite_ref-FOOTNOTEGeographical_Names_Data_Base:_Eve_Cone_15-0)** [Geographical Names Data Base: Eve Cone](#CITEREFGeographical_Names_Data_Base:_Eve_Cone).

1. **[^](#cite_ref-FOOTNOTESouther1992214,_222_16-0)** [Souther 1992](#CITEREFSouther1992), pp. 214, 222.

1. ^ [***a***](#cite_ref-FOOTNOTEBC_Parks:_Mount_Edziza_Provincial_Park_17-0) [***b***](#cite_ref-FOOTNOTEBC_Parks:_Mount_Edziza_Provincial_Park_17-1) [***c***](#cite_ref-FOOTNOTEBC_Parks:_Mount_Edziza_Provincial_Park_17-2) [***d***](#cite_ref-FOOTNOTEBC_Parks:_Mount_Edziza_Provincial_Park_17-3) [***e***](#cite_ref-FOOTNOTEBC_Parks:_Mount_Edziza_Provincial_Park_17-4) [BC Parks: Mount Edziza Provincial Park](#CITEREFBC_Parks:_Mount_Edziza_Provincial_Park).

1. **[^](#cite_ref-FOOTNOTEBC_Geographical_Names:_Cassiar_Land_District_18-0)** [BC Geographical Names: Cassiar Land District](#CITEREFBC_Geographical_Names:_Cassiar_Land_District).

1. **[^](#cite_ref-FOOTNOTESouther1992214_19-0)** [Souther 1992](#CITEREFSouther1992), p. 214.

1. **[^](#cite_ref-FOOTNOTESouther1990124,_125_20-0)** [Souther 1990](#CITEREFSouther1990), pp. 124, 125.

1. ^ [***a***](#cite_ref-FOOTNOTESouther1992223_21-0) [***b***](#cite_ref-FOOTNOTESouther1992223_21-1) [***c***](#cite_ref-FOOTNOTESouther1992223_21-2) [***d***](#cite_ref-FOOTNOTESouther1992223_21-3) [***e***](#cite_ref-FOOTNOTESouther1992223_21-4) [***f***](#cite_ref-FOOTNOTESouther1992223_21-5) [Souther 1992](#CITEREFSouther1992), p. 223.

1. ^ [***a***](#cite_ref-FOOTNOTEDinwiddieLambReynolds2011116_22-0) [***b***](#cite_ref-FOOTNOTEDinwiddieLambReynolds2011116_22-1) [Dinwiddie, Lamb & Reynolds 2011](#CITEREFDinwiddieLambReynolds2011), p. 116.

1. **[^](#cite_ref-FOOTNOTESouther1990125_23-0)** [Souther 1990](#CITEREFSouther1990), p. 125.

1. ^ [***a***](#cite_ref-FOOTNOTEGlobal_Volcanism_Program:_EdzizaGeneral_Information_24-0) [***b***](#cite_ref-FOOTNOTEGlobal_Volcanism_Program:_EdzizaGeneral_Information_24-1) [Global Volcanism Program: Edziza](#CITEREFGlobal_Volcanism_Program:_Edziza), General Information.

1. **[^](#cite_ref-FOOTNOTEBC_Geographical_Names:_Pillow_Ridge_25-0)** [BC Geographical Names: Pillow Ridge](#CITEREFBC_Geographical_Names:_Pillow_Ridge).

1. ^ [***a***](#cite_ref-FOOTNOTESouther1992219_26-0) [***b***](#cite_ref-FOOTNOTESouther1992219_26-1) [Souther 1992](#CITEREFSouther1992), p. 219.

1. **[^](#cite_ref-FOOTNOTEGlobal_Volcanism_Program:_EdzizaPhoto_Gallery_27-0)** [Global Volcanism Program: Edziza](#CITEREFGlobal_Volcanism_Program:_Edziza), Photo Gallery.

1. **[^](#cite_ref-FOOTNOTEHolland197649_28-0)** [Holland 1976](#CITEREFHolland1976), p. 49.

1. **[^](#cite_ref-FOOTNOTEEdwardsRussell20001280,_1281,_1283,_1284_29-0)** [Edwards & Russell 2000](#CITEREFEdwardsRussell2000), pp. 1280, 1281, 1283, 1284.

1. **[^](#cite_ref-FOOTNOTEMcGraw_Hill2003253_30-0)** [McGraw Hill 2003](#CITEREFMcGraw_Hill2003), p. 253.

1. **[^](#cite_ref-FOOTNOTEEdwardsRussell20001280_32-0)** [Edwards & Russell 2000](#CITEREFEdwardsRussell2000), p. 1280.

1. **[^](#cite_ref-FOOTNOTEKelmanWilson2024411_33-0)** [Kelman & Wilson 2024](#CITEREFKelmanWilson2024), p. 411.

1. ^ [***a***](#cite_ref-FOOTNOTEMátyás_et_al.20231_34-0) [***b***](#cite_ref-FOOTNOTEMátyás_et_al.20231_34-1) [Mátyás et al. 2023](#CITEREFMátyás_et_al.2023), p. 1.

1. **[^](#cite_ref-FOOTNOTEFoote_et_al.20231_35-0)** [Foote et al. 2023](#CITEREFFoote_et_al.2023), p. 1.

1. **[^](#cite_ref-FOOTNOTENemeth201043_36-0)** [Nemeth 2010](#CITEREFNemeth2010), p. 43.

1. **[^](#cite_ref-FOOTNOTEGiardinoHouser2015417_37-0)** [Giardino & Houser 2015](#CITEREFGiardinoHouser2015), p. 417.

1. **[^](#cite_ref-FOOTNOTESouther1992223,_224_39-0)** [Souther 1992](#CITEREFSouther1992), pp. 223, 224.

1. **[^](#cite_ref-FOOTNOTESouther1990125,_126_40-0)** [Souther 1990](#CITEREFSouther1990), pp. 125, 126.

1. ^ [***a***](#cite_ref-FOOTNOTESouther199231_41-0) [***b***](#cite_ref-FOOTNOTESouther199231_41-1) [Souther 1992](#CITEREFSouther1992), p. 31.

1. ^ [***a***](#cite_ref-FOOTNOTEMussio201888,_89_42-0) [***b***](#cite_ref-FOOTNOTEMussio201888,_89_42-1) [***c***](#cite_ref-FOOTNOTEMussio201888,_89_42-2) [Mussio 2018](#CITEREFMussio2018), pp. 88, 89.

1. ^ [***a***](#cite_ref-FOOTNOTEMussio201888_43-0) [***b***](#cite_ref-FOOTNOTEMussio201888_43-1) [***c***](#cite_ref-FOOTNOTEMussio201888_43-2) [Mussio 2018](#CITEREFMussio2018), p. 88.

1. **[^](#cite_ref-FOOTNOTEMussio201889_44-0)** [Mussio 2018](#CITEREFMussio2018), p. 89.

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## External links

- ["Eve Cone, British Columbia"](http://www.peakbagger.com/peak.aspx?pid=51400). *Peakbagger.com*.

- Media related to [Eve Cone](https://commons.wikimedia.org/wiki/Category:Eve_Cone) at Wikimedia Commons

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 [Eve Cone](https://en.wikipedia.org/wiki/Eve_Cone) by Wikipedia contributors ([contributor history](https://en.wikipedia.org/wiki/Eve_Cone?action=history)). Available under [Creative Commons Attribution-ShareAlike 4.0 International](https://creativecommons.org/licenses/by-sa/4.0/). Changes may have been made.