The Bell-Irving volcanic district is a volcanic field in the upper Bell-Irving River watershed of northern British Columbia, Canada. It is considered part of the Northern Cordilleran Volcanic Province, consisting of 14 volcanic centres. They comprise pillow lava and/or volcaniclastic rocks, which were possibly emplaced by alpine glaciovolcanic eruptions during the Pleistocene. The volcanic deposits were discovered between 1992 and 2004 but remained undescribed until 2006.[1]
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Transcription
Occurrences
The Bell-Irving volcanic district includes the following:[1]
- Adzich volcanic centre
- Owl Creek South volcanic deposits
- Owl Creek North volcanic deposits
- Rochester Creek Southwest volcanic centre
- Rochester Creek Southeast volcanic centre
- Upper Rochester Creek volcanic deposits
- Rochester Creek Northeast-South volcanic deposits
- Rochester Creek Northeast-North volcanic deposits
- Bell-Irving River East South volcanic deposit
- Bell-Irving River East North volcanic deposit
- Bell-Irving River volcanic centre
- Bell-Irving Northeast volcanic deposits
- Icefield Ridge volcanic deposit
- Craven Lake volcanic centre
References
- ^ a b Edwards, B. R.; Evenchick, C. A.; McNicoll, V. J.; Wetherell, K.; Nogier, M. (2006). Overview of the volcanology of the Bell-Irving volcanic district, northwestern British Columbia: new examples of mafic alpine glaciovolcanism from the northern Cordilleran volcanic province. Natural Resources Canada. pp. 1–9. ISBN 978-0-662-42826-8.
This page was last edited on 25 September 2023, at 05:00