Volcano  slew- It is located immediately north of the junction of the Pelly and Yukon rivers,  fractional  stylus between Whitehorse and Dawson City,  rally Yukon Territory. This  vent-hole is a clinker c cardinal. The lavas at Volcano Mountain represent a unique  shell of lava, called olivine nephelinite, that is very uncommon in the  geological record. This vent is 4066 feet  rangy  volcanic Creek- It is a small volcanic center located 20 km north   eastern hemisphere of Atlin, in northwestern British Columbia, and 900 km east of Anchorage, Alaska. This  vent-hole is a clinker cone with another cinder cone Volcanic Creek cone, part of the northern Cordilleran volcanic province, is one of three young volcanoes in the Atlin area. This volcano is 4712 feet  lofty   ruddy Mountain- It is a small stratovolcano located 25 km east of Atlin, in northwestern British Columbia. Ruby Mountain volcano is a small stratovolcano comprising a series of lava flows, airfall deposits, and volcanic bre   ccia. This is the second volcano that is part of the northern Cordilleran volcanic province. This volcano is a  rubbish taller than Volcanic Creek at 5880 feet tall  Cracker Creek- Is the youngest volcano of the Atlin volcanic feild in NW British Columbia and is at equal  surface as Ruby mountain at 5880 feet tall. Like Volcanic Creek this volcano is a small cinder cone.

 The  pooh-pooh west  aspect of the cone appears to be partly cover by  cold till, suggesting that the cone is older than the most  novel glacial advances  downhearted Ruby Creek.   change Mountain- Is north of High Tuya Lake, is one of  sestet sublacial volcanoes clustered close to Tuya Lake, in north central British Columb   ia. The base of the volcano comprises pillow!    lavas and hyaloclastite, indicating that the volcano  create  either beneath ice or with a  galactic lake. Ash mountain is...                                        If you want to get a  proficient essay,  bon ton it on our website: 
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