{{short description|Cinder cone in British Columbia, Canada}} {{Featured article}} {{Use Canadian English|date=January 2025}} {{Use mdy dates|date=January 2025}} {{Infobox mountain | name = Eve Cone | other_name = Eve's Cone | image = File:Edziza042909-- 027-6.jpg | image_alt = A partially snow-covered, cone-shaped volcano with a bowl-shaped crater on its top. | image_caption = Eve Cone from the northeast | mapframe = yes | mapframe-caption = Location in [[Mount Edziza Provincial Park]] | mapframe-zoom = 7 | elevation_m = 1740 | elevation_ref = {{sfn|Global Volcanism Program: Edziza|loc=Synonyms & Subfeatures}} | coordinates = {{Coord|57|48|47|N|130|40|32|W|type:mountain_region:CA-BC|display=inline,title}} | coordinates_ref = {{sfn|BC Geographical Names: Eve Cone}} | etymology = [[Eve Cone#Name and etymology|Eve Brown Edzerza]]{{sfn|BC Geographical Names: Eve Cone}} | authority = [[BC Geographical Names]] office in [[Victoria, British Columbia]]{{sfn|BC Geographical Names: Eve Cone}}{{sfn|Government of Canada: Geographical Names Board of Canada}} | map= Canada British Columbia | map_alt =Relief map of British Columbia pinpointing the location of Eve Cone | map_caption = Location in British Columbia | country = [[Canada]]{{sfn|Department of Energy, Mines and Resources|1989}} | region_type = [[Provinces and territories of Canada|Province]] | region = [[British Columbia]]{{sfn|Department of Energy, Mines and Resources|1989}} | district = [[Cassiar Land District]]{{sfn|BC Geographical Names: Eve Cone}} | part_type = [[Protected area]] | part = [[Mount Edziza Provincial Park]]{{sfn|BC Geographical Names: Eve Cone}} | range = [[Tahltan Highland]]{{sfn|Department of Energy, Mines and Resources|1989}} | topo_maker = [[National Topographic System|NTS]] | topo_map = {{Canada NTS Map Sheet|104|G|15}}{{sfn|BC Geographical Names: Eve Cone}} | formed_by = [[Volcanism of the Mount Edziza volcanic complex|Volcanism]]{{sfn|Souther|1992|p=27}} | type = [[Cinder cone]]{{sfn|Natural Resources Canada: Eve Cone}} | geology = [[Hawaiite]]{{sfn|Souther|1988}} | volcanic_field = [[Desolation Lava Field]]{{sfn|Souther|1988}} | last_eruption = [[Holocene]] age{{sfn|Natural Resources Canada: Eve Cone}} | normal_route = Trail on the southeastern flank{{sfn|BC Parks: Hiking and Wilderness Camping in Mount Edziza Provincial Park}} }} '''Eve Cone''', also known as '''Eve's Cone''', is a [[cinder cone]] in [[Cassiar Land District]] of northwestern [[British Columbia]], Canada. It has an [[elevation]] of {{convert|1740|m|ft|abbr=off}} and is one of several [[volcanic cone]]s in the [[Desolation Lava Field]] at the northern end of the [[Big Raven Plateau]]. Situated southeast of the community of [[Telegraph Creek]], it lies in [[Mount Edziza Provincial Park]], one of the largest [[provincial parks in British Columbia]]. A roughly {{convert|12|km|mi|adj=mid|-long|abbr=off}} [[lava field]] issued from Eve Cone during the [[Holocene]] and travelled down the northern side of the Big Raven Plateau. It branches out into much narrower [[lava channel|channels]], the largest extending to [[Buckley Lake (British Columbia)|Buckley Lake]].
Eve Cone is part of the [[Mount Edziza volcanic complex]], which consists of diverse landforms such as [[shield volcano]]es, [[stratovolcano]]es, [[lava dome]]s and cinder cones. The cone contains a circular summit [[volcanic crater|crater]] {{convert|45|m|ft|abbr=on}} deep but most of the lava from the volcano appears to have issued from vents around the base of the {{convert|350|m|ft|abbr=on}} wide cone. Eve Cone is surrounded by a number of other volcanic features, including [[Tsekone Ridge]], [[Pillow Ridge]], [[Sidas Cone]] and the [[Triplex Cones]]. Access is via [[horse trail]]s from Telegraph Creek and [[Iskut]], although landing on Buckley Lake with float-equipped aircraft is also promoted to reach Eve Cone.
==Name and etymology== [[Jack Souther]], a [[geologist]] of the Geological Survey of Canada who studied the area in detail from 1965 to 1992, named the cone after Eve Brown Edzerza.{{sfn|BC Geographical Names: Eve Cone}}{{sfn|Souther|1966|p=89}}{{sfn|Natural Resources Canada: Mount Edziza}} Edzerza was a local indigenous woman who traversed [[Mount Edziza]] by dog sled with her husband, [[Johnny Edzerza]], and a man named [[Hank Williams (Tahltan man)|Hank Williams]] in or before 1974.{{sfn|BC Geographical Names: Eve Cone}}{{sfn|BC Geographical Names: Mount Edziza}}{{sfn|Souther|2009}} Johnny and Hank were killed in an [[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.{{sfn|BC Geographical Names: Eve Cone}}{{sfn|Souther|2009}}
Hank Williams and the Edzerzas were [[Tahltan]]s, the local [[First Nations in British Columbia|First Nations]] people whose traditional territory covers an area of more than {{Convert|93500|km2|mi2|abbr=on}}.{{sfn|Souther|2009}}{{sfn|Markey|Halseth|Manson|2012|p=242}} Eve Edzerza's survival and saga of courage following the avalanche is a legend among the Tahltans.{{sfn|Souther|2009}} Johnny Edzerza was buried on Mount Edziza; both ''Edzerza'' and ''Edziza'' may be [[etymologically]] linked.{{sfn|BC Geographical Names: Mount Edziza}} [[Williams Cone]] on the northeastern side of the mountain was named in honour of Hank.{{sfn|BC Geographical Names: Williams Cone}}
The name of the cone became official on January 2, 1980, and was adopted on the [[National Topographic System]] map 104G/15 after being submitted to the [[BC Geographical Names]] office by the [[Geological Survey of Canada]].{{sfn|BC Geographical Names: Eve Cone}}{{sfn|Geographical Names Data Base: Eve Cone}} In his 1992 report ''The Late Cenozoic Mount Edziza Volcanic Complex, British Columbia'', Jack Souther gave Eve Cone the [[numeronym]] ''DLF-9''; ''DLF'' is an acronym for the [[Desolation Lava Field]] whereas ''9'' refers to Eve Cone being the ninth youngest eruptive centre in the Desolation Lava Field.{{sfn|Souther|1992|pp=214, 222}} [[BC Parks]] refers to the cone as both ''Eve Cone'' and ''Eve's Cone''.{{sfn|BC Parks: Mount Edziza Provincial Park}}
==Geography== Eve Cone is located in [[Cassiar Land District]] of northwestern [[British Columbia]], Canada, about {{convert|11|km|mi|abbr=on}} southeast of [[Buckley Lake (British Columbia)|Buckley Lake]] at the northern end of the [[Big Raven Plateau]].{{sfn|BC Geographical Names: Eve Cone}}{{sfn|Department of Energy, Mines and Resources|1989}}{{sfn|BC Geographical Names: Cassiar Land District}} It has an [[elevation]] of {{convert|1740|m|ft|abbr=on}} and is one of several [[volcanic cone]]s in the Desolation Lava Field, which is one of the largest areas of [[Holocene]] lava flows of the [[Mount Edziza volcanic complex]].{{sfn|Global Volcanism Program: Edziza|loc=Synonyms & Subfeatures}}{{sfn|Souther|1988}}{{sfn|Souther|1992|p=214}} The volcanic complex consists of a group of overlapping [[shield volcano]]es, [[stratovolcano]]es, [[lava dome]]s and [[cinder cone]]s that have formed over the last 7.5 million years.{{sfn|Souther|1990|pp=124, 125}} Eve Cone is one of the most symmetrical and best-preserved cinder cones in Canada, rising {{convert|172|m|ft|abbr=on}} above the surrounding [[terrain]] to a circular summit [[volcanic crater|crater]] {{convert|45|m|ft|abbr=on}} deep.{{sfn|Natural Resources Canada: Mount Edziza}}{{sfn|Souther|1992|p=223}}{{sfn|Dinwiddie|Lamb|Reynolds|2011|p=116}} [[Lichen]] and [[Pioneer species|pioneer vegetation]] sparsely grows on the base of the {{convert|350|m|ft|abbr=on}} wide cone.{{sfn|Souther|1992|p=223}}{{sfn|Dinwiddie|Lamb|Reynolds|2011|p=116}}
The [[Smithsonian Institution]]'s [[Global Volcanism Program]] lists Eve Cone as one of many [[satellitic cone]]s of Mount Edziza due to its location on the northern flank of this stratovolcano.{{sfn|Global Volcanism Program: Edziza|loc=Synonyms & Subfeatures}}{{sfn|Souther|1990|p=125}}{{sfn|Global Volcanism Program: Edziza|loc=General Information}} Apart from the main edifice of Mount Edziza, which reaches an elevation of {{convert|2786|m|ft|abbr=on}}, Eve Cone is surrounded by a number of other volcanic features.{{sfn|Souther|1988}}{{sfn|Global Volcanism Program: Edziza|loc=General Information}} About {{convert|5|km|mi|abbr=on}} southwest of Eve Cone is [[Tsekone Ridge]] on the northwestern flank of Mount Edziza.{{sfn|Department of Energy, Mines and Resources|1989}} [[Pillow Ridge]], about {{convert|5|km|mi|abbr=on}} south of Eve Cone, extends northwest from the northern flank of Mount Edziza.{{sfn|Department of Energy, Mines and Resources|1989}}{{sfn|BC Geographical Names: Pillow Ridge}} About {{convert|2|km|mi|abbr=on}} southeast of Eve Cone are the [[Triplex Cones]], a southeast-trending line of three deeply eroded volcanic cones.{{sfn|Souther|1988}}{{sfn|Souther|1992|p=219}} [[Sidas Cone]] about {{convert|5|km|mi|abbr=on}} northwest of Eve Cone is a composite of two overlapping cones.{{sfn|Department of Energy, Mines and Resources|1989}}{{sfn|Souther|1992|p=219}} The Pillow and Tsekone ridges are older volcanic features of [[Pleistocene]] age whereas Sidas Cone and the Triplex Cones are part of the younger Desolation Lava Field.{{sfn|Souther|1988}}
Eve Cone lies in [[Mount Edziza Provincial Park]] southeast of the community of [[Telegraph Creek]].{{sfn|BC Geographical Names: Eve Cone}} With an area of {{Convert|266180|ha|acre|abbr=off}}, Mount Edziza Provincial Park is one of the largest [[provincial parks in British Columbia]] and was established in 1972 to preserve the volcanic landscape.{{sfn|BC Parks: Mount Edziza Provincial Park}}{{sfn|Global Volcanism Program: Edziza|loc=Photo Gallery}} It includes not only the Mount Edziza area but also the [[Spectrum Range]] to the south, both of which are separated by [[Raspberry Pass]].{{sfn|Department of Energy, Mines and Resources|1989}}{{sfn|BC Parks: Mount Edziza Provincial Park}} Mount Edziza Provincial Park is in the [[Tahltan Highland]], a southeast-trending [[Upland and lowland|upland]] area extending along the western side of the [[Stikine Plateau]].{{sfn|Department of Energy, Mines and Resources|1989}}{{sfn|Holland|1976|p=49}}
==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]], which extends from northwestern British Columbia northwards through [[Yukon]] into easternmost [[Alaska]].{{sfn|Souther|1988}}{{sfn|Edwards|Russell|2000|pp=1280, 1281, 1283, 1284}} The dominant rocks comprising these volcanoes are [[alkali basalt]]s and [[hawaiite]]s, but [[nephelinite]], [[basanite]] and [[peralkaline rock|peralkaline]]{{efn|''Peralkaline rocks'' are magmatic rocks that have a higher ratio of sodium and potassium to aluminum.{{sfn|McGraw Hill|2003|p=253}}}} [[phonolite]], [[trachyte]] and [[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 [[rift]]ing of the [[North American Cordillera]], driven by changes in relative [[plate tectonics|plate motion]] between the [[North American Plate|North American]] and [[Pacific Plate|Pacific]] plates.{{sfn|Edwards|Russell|2000|p=1280}}
===Structure=== [[File:Edziza cones and lava flow.jpg|thumb|upright=1.2|alt=Overhead view of lava flows from two volcanic cones|False colour image of lava flows from Eve and [[Sidas Cone|Sidas]] cones]] Eve Cone is a [[monogenetic volcanic field|monogenetic]] cinder cone, which are simple volcanic edifices that erupted over a single eruptive phase.{{sfn|Natural Resources Canada: Eve Cone}}{{sfn|Kelman|Wilson|2024|p=411}}{{sfn|Mátyás et al.|2023|p=1}}{{sfn|Foote et al.|2023|p=1}} 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]].{{sfn|Mátyás et al.|2023|p=1}}{{sfn|Nemeth|2010|p=43}} Eve Cone consists of hawaiite of the [[Big Raven Formation]] and is one of the two youngest eruptive centres in the Desolation Lava Field, the other being Williams Cone about {{convert|6|km|mi|abbr=on}} to the southeast.{{sfn|Department of Energy, Mines and Resources|1989}}{{sfn|Souther|1988}}{{sfn|Souther|1992|p=223}} Both cones are of Holocene age but Eve Cone was most likely formed by a towering, vertical [[lava fountain]] due to its symmetrical structure.{{sfn|Souther|1992|p=27}}{{sfn|Souther|1988}} Loosely [[Aggregate (geology)|aggregated]] volcanic [[ejecta]] such as [[volcanic bomb|bombs]], [[scoria|cinders]] and [[volcanic ash|ash]] cover the outer surface of Eve Cone.{{sfn|Souther|1992|p=223}}
Relatively fine, dark grey bombs and cinders cover the northern half of Eve Cone whereas coarser, clinkery [[volcanic spatter|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]] and [[solifluction]]{{efn|''Solifluction'' is [[soil creep]] caused by waterlogged soil slowly moving downhill on top of an impermeable layer.{{sfn|Giardino|Houser|2015|p=417}}}} which may be caused by greater and more frequent temperature changes.{{sfn|Souther|1992|p=223}} 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.{{sfn|Souther|1992|pp=223, 224}}
===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 {{convert|30|m|ft|abbr=on}} high buttress of overlapping tiers of lava lobes.{{sfn|Souther|1992|p=223}} Streams of lava from these vents merged to form a roughly {{convert|12|km|mi|abbr=on}} long [[lava field]] which extends down the northern side of the Big Raven Plateau. It has a maximum width of about {{convert|6|km|mi|abbr=on}}, 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 channel]]s to the north and northwest, the largest of which is approximately {{convert|6|km|mi|abbr=on}} 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.{{sfn|Souther|1988}}
==Accessibility== [[File:Edziza042909-- 023-5.jpg|thumb|right|alt=A partially snow-covered, cone-shaped volcano with a bowl-shaped crater on its top.|Eve Cone from the southeast]] Eve Cone is in a remote location with no established road access.{{sfn|Souther|1990|pp=125, 126}} The closest roads are the [[Stewart–Cassiar Highway]] to the east and the Telegraph Creek Road to the northwest; both come within {{Convert|40|km|mi|abbr=on}} of the cone.{{sfn|Department of Energy, Mines and Resources|1989}}{{sfn|Souther|1992|p=31}}{{sfn|Mussio|2018|pp=88, 89}} Extending from these roads are [[horse trail]]s that provide access to the Mount Edziza volcanic complex.{{sfn|Souther|1992|p=31}} From Telegraph Creek, the Buckley Lake Trail extends about {{Convert|15|km|mi|abbr=on}} southeast along [[Mess Creek]] and Three Mile Lake. It then traverses about {{Convert|15|km|mi|abbr=on}} 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.{{sfn|Mussio|2018|p=88}}
To the east, the roughly {{Convert|50|km|mi|abbr=on}} long Klastline River Trail begins at the community of [[Iskut]] on the Stewart–Cassiar Highway; it extends northwest and west along the Klastline River for much of its length.{{sfn|Mussio|2018|pp=88, 89}} The trail enters Mount Edziza Provincial Park at about {{Convert|25|km|mi|abbr=on}} where Kakiddi Creek drains into the Klastline River.{{sfn|Mussio|2018|p=89}} After entering Mount Edziza Provincial Park, it traverses northwest along the Klastline River for about {{Convert|10|km|mi|abbr=on}} and then crosses the river north of the Big Raven Plateau.{{sfn|Mussio|2018|pp=88, 89}} From there, it traverses west for about {{Convert|5|km|mi|abbr=on}} to the northeastern end of Buckley Lake where it meets with the Buckley Lake Trail and the Buckley Lake to Mowdade Lake Route.{{sfn|Mussio|2018|p=88}}
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.{{sfn|Department of Energy, Mines and Resources|1989}}{{sfn|BC Parks: Hiking and Wilderness Camping in Mount Edziza Provincial Park}}{{sfn|Mussio|2018|p=88}} 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.{{sfn|BC Parks: Hiking and Wilderness Camping in Mount Edziza Provincial Park}} Buckley Lake northwest of Eve Cone is large enough to be used by float-equipped aircraft.{{sfn|Department of Energy, Mines and Resources|1989}}{{sfn|BC Parks: Mount Edziza Provincial Park}} 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.{{sfn|BC Parks: Mount Edziza Provincial Park}}
==See also== {{Portal|Volcanoes|Mountains}} *[[List of Northern Cordilleran volcanoes]] *[[List of volcanoes in Canada]] *[[Volcanism of the Mount Edziza volcanic complex]]
==Notes== {{notelist}}
==References== {{Reflist}}
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web|url=https://bcparks.ca/explore/parkpgs/mt_edziza/|archive-url=https://web.archive.org/web/20230123120553/https://bcparks.ca/explore/parkpgs/mt_edziza/|archive-date=January 23, 2023|title=Mount Edziza Provincial Park|publisher=[[BC Parks]]|ref={{harvid|BC Parks: Mount Edziza Provincial Park}}}} *{{cite web|url=https://bcparks.ca/explore/parkpgs/mt_edziza/hikecamp.html|archive-url=https://web.archive.org/web/20220626073359/https://bcparks.ca/explore/parkpgs/mt_edziza/hikecamp.html#hiking|archive-date=June 26, 2022|title=Mount Edziza Provincial Park: Hiking and Wilderness Camping|publisher=[[BC Parks]]|ref={{harvid|BC Parks: Hiking and Wilderness Camping in Mount Edziza Provincial Park}}}} *{{cite book|editor-last1=Mussio|editor-first1=Russell|title=Northern BC Backroad Mapbook|publisher=Mussio Ventures|year=2018|isbn= 978-1-926806-87-7}} *{{cite report|editor-last1=Cañón-Tapia|editor-first1=Edgardo|editor-last2=Szakács|editor-first2=Alexandru|last1=Nemeth|first1=Karoly|title=What is a Volcano?|chapter=Monogenetic Volcanic Fields: Origin, Sedimentary Record, and Relationship with Polygenetic Volcanism|publisher=[[Geological Society of America]]|pages=43–66|year=2010|volume=470|isbn=978-0-8137-2470-6|doi=10.1130/2010.2470(04)}} *{{cite bcgnis|id=16786|name=Pillow Ridge|archive-url=https://web.archive.org/web/20211001004911/https://apps.gov.bc.ca/pub/bcgnws/names/16786.html|archive-date=October 1, 2021|ref={{harvid|BC Geographical Names: Pillow Ridge}}}} *{{cite report|last1=Souther|first1=J. G.|author-link1=Jack Souther|title=Report of Activities, Part A: May to October, 1966|chapter=Cordilleran Volcanic Study, 1966|url=https://publications.gc.ca/collections/collection_2017/rncan-nrcan/M41-1-4-67-1A-eng.pdf|archive-url=https://web.archive.org/web/20230107151915/https://publications.gc.ca/collections/collection_2017/rncan-nrcan/M41-1-4-67-1A-eng.pdf|archive-date=January 7, 2023|publisher=[[Geological Survey of Canada]]|year=1966}} *{{cite map|last1=Souther|first1=J. G.|author-link1=Jack Souther|title=Geology, Mount Edziza Volcanic Complex, British Columbia|map=1623A|scale=1:50,000|type=[[Geological map]]|cartography=M. Sigouin, [[Geological Survey of Canada]]|publisher=[[Energy, Mines and Resources Canada]]|year=1988|language=en|doi=10.4095/133498|doi-access=free}} *{{cite book|editor-last1=Wood|editor-first1=Charles A.|editor-last2=Kienle|editor-first2=Jürgen|last1=Souther|first1=J. G.|author-link1=Jack Souther|url=https://books.google.com/books?id=eyDRib-FJh4C|title=Volcanoes of North America: United States and Canada|year=1990|publisher=[[Cambridge University Press]]|isbn=0-521-43811-X}} *{{cite report|last1=Souther|first1=J. G.|author-link1=Jack Souther|title=The Late Cenozoic Mount Edziza Volcanic Complex, British Columbia|work=[[Geological Survey of Canada]]|publisher=Canada Communication Group|series=Memoir 420|year=1992|isbn=0-660-14407-7|doi=10.4095/133497|doi-access=free}} *{{cite web|last1=Souther|first1=J.|author-link1=Jack Souther|title=History Surrounds Mount Edziza|url=https://www.piquenewsmagazine.com/travel/history-surrounds-mount-edziza-2481730|archive-url=https://web.archive.org/web/20200805221333/https://www.piquenewsmagazine.com/travel/history-surrounds-mount-edziza-2481730|website=Pique Newsmagazine|publisher=[[Glacier Media]]|date=February 27, 2009|archive-date=August 5, 2020}} *{{cite web|title=Stikine Volcanic Belt: Mount Edziza|work=Catalogue of Canadian volcanoes|publisher=[[Natural Resources Canada]]|date=2009-04-01|url=http://gsc.nrcan.gc.ca/volcanoes/cat/feature_edziza_e.php|url-status=dead|archive-url=https://web.archive.org/web/20090608034953/http://gsc.nrcan.gc.ca/volcanoes/cat/feature_edziza_e.php|archive-date=June 8, 2009|ref={{harvid|Natural Resources Canada: Mount Edziza}}}} *{{cite bcgnis|id=22171|name=Williams Cone|archive-url=https://web.archive.org/web/20240609204708/https://apps.gov.bc.ca/pub/bcgnws/names/22171.html|archive-date=June 9, 2024|ref={{harvid|BC Geographical Names: Williams Cone}}}} {{refend}}
==External links== *{{cite peakbagger|pid=51400|name=Eve Cone, British Columbia}} *{{Commons category-inline|Eve Cone}}
{{Mount Edziza volcanic complex}} {{Northern Cordilleran volcanoes}}
[[Category:Cinder cones of British Columbia]] [[Category:Holocene cinder cones]] [[Category:Monogenetic cinder cones]] [[Category:Parasitic cones of Mount Edziza]] [[Category:Desolation Lava Field]] [[Category:One-thousanders of British Columbia]]