The extinct volcano is one of many cinder cones in the Atherton Tableland region. Its crater is approximately 500 m across, with the main cone being to the northwest. Several of the nearby Seven Sisters cinder cones also have their craters to the southeast, which is possibly due to the ash and scoria being blown to the northwest by the prevailing SE winds. Swamp deposits within the crater were dated at 7250 years old, making that the minimum age for Mt Quincan. The scoria deposits also contain abundant mantle xenoliths of peridotite.
- Johnson, Robert Wallace (1989). Intraplate Volcanism: In Eastern Australia and New Zealand. Cambridge University Press. p. 92. ISBN 978-0521380836. Retrieved 21 November 2012.
- Lottermoser, B. G.; Whitehead, P. W.; Nelson, P. N.; Beaman, R. J. (2008). Rocks, Landscapes and Resources of the Wet Tropics. Brisbane: Geological Society of Australia, Queensland Division. p. 17. ISBN 9780975789483.
- KERSHAW, A. P. (1971). "A POLLEN DIAGRAM FROM QUINCAN CRATER, NORTH-EAST QUEENSLAND, AUSTRALIA". New Phytologist. 70 (4): 669–681. doi:10.1111/j.1469-8137.1971.tb02567.x. ISSN 0028-646X.
- Whitehead, P. W.; Stephenson, P. J.; McDougall, I.; Hopkins, M. S.; Graham, A. W.; Collerson, K. D.; Johnson, D. P. (2007). "Temporal development of the Atherton Basalt Province, north Queensland". Australian Journal of Earth Sciences. 54 (5): 691–709. doi:10.1080/08120090701305236. ISSN 0812-0099.
- Yungaburra Quarry. Retrieved on 21 November 2012.
|This Queensland location article is a stub. You can help Wikipedia by expanding it.|