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Wrangellian volcanic and sedimentary rocks in southwest Yukon underwent multiple deformation phases from Late Triassic to Miocene time. Bedrock mapping completed within the White River area documents these events, including Late Jurassic-Early Cretaceous compression and Cretaceous-Miocene strike-slip faulting. The dataset is provided by the Government of Yukon and was last updated on April 17, 2026.
Data is provided under the OGL-CA-2.0 license.