final phase of activity produced a long glassy dacite lava flow that varies from thick. This is the largest known explosive eruption in Canada in the past 10,000 years. Two clusters of hot springs are found at the Mount Meager massif, suggesting magmatic heat is still present and volcanic activity continues. The massive Mount Edziza volcanic complex in the Northern Cordilleran Volcanic Province of northern British Columbia has had more than 20 eruptions throughout the past 10,000 years (Holocene), including Mess Lake Cone, Kana Cone, Cinder Cliff, Icefall Cone, Ridge Cone, Williams Cone, Walkout Creek Cone, Moraine Cone, Sidas Cone, Sleet Cone, Storm Cone, Triplex Cone, Twin Cone, Cache Hill, Camp Hill, Cocoa Crater, Coffee Crater, Nahta Cone, Tennena Cone, The Saucer, and the well-preserved Eve Cone. Active or recently active hot springs are found in several areas along the western flank of Edziza's lava plateau, including Elwyn springs (36 °C), Taweh springs (46 °C), and inactive springs near Mess Lake. All three hydrothermal areas are near the youngest lava fields on the lava plateau and are probably associated with the most recent volcanic activity at the Mount Edziza volcanic complex. An undated pumice deposit exists throughout the complex estimated to be younger than 500 years. Kostal Cone in the Wells Gray-Clearwater volcanic field of east-central British Columbia is a cinder cone responsible for basaltic lava flows comprising a lava bed, damming the southern end of McDougall Lake. There has been activity at this site as recently as 7,600 years ago at Dragon Cone, though more likely less than 1,000 years ago. Kostal Cone is too young for the potassium-argon dating technique (usable on specimens over 100,000 years old), and no charred organic material for radiocarbon dating has been found. However, the uneroded structure of the cone with the existence of trees on its flanks and summit have made it an area for dendrochronology studies, which reveals the growth of tree-ring patterns. Tree-ring dating has revealed an age of about 400 years for Kostal Cone, indicating it formed around 1500. This makes Kostal Cone the youngest volcano in the Wells Gray-Clearwater volcanic field and thus one of the youngest in Canada. Tseax Cone, a young cinder cone at the southernmost end of the Northern Cordilleran Volcanic Province, was the source for a major basalt lava flow eruption around the years 1750 and 1775 that travelled into the Tseax River, damming