Solitary Mountain consists of Late Cretaceous volcanics of the Carmacks Group, a 63,000 km2 (24,000 sq mi) volcanic group that may have its origin from volcanism of the Yellowstone hotspot some 70 million years ago.[1] Unlike much of the Carmacks Group, the volcanics comprising Solitary Mountain are separated by the large strike-slip Teslin Fault.[2]
^Enkin, Randolph J.; Johnston, Stephen T.; Larson, Kyle P.; Baker, Judith (2006). "Paleomagnatism of the 70 Ma Carmacks Group at Solitary Mountain, Yukon, confirms and extends controversial results: Further evidence for the Baja British Columbia model" (Document). Geological Survey of Canada. p. 221.
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