Cerberean Cauldron

Short description: Supervolcanic caldera

The Cerberean Cauldron is a caldera in Australia which was formed by a supervolcano^{[citation needed]} which erupted about 374 million years ago and was a possible cause of the Late Devonian extinction.^{[citation needed]} It forms the northern part of the Marysville Igneous Complex in central Victoria and is now in the Lake Eildon National Park.^[1]^[2]

References

↑ Clemens, J. D.; Birch, W. D. (2012-12-15), "Assembly of a zoned volcanic magma chamber from multiple magma batches: The Cerberean Cauldron, Marysville Igneous Complex, Australia" (in en), Lithos 155: 272–288, doi:10.1016/j.lithos.2012.09.007, ISSN 0024-4937, https://www.sciencedirect.com/science/article/pii/S0024493712003714
↑ Birch, W. D. (1970), An investigation of the Upper Devonian Cerberean Cauldron complex in central Victoria, University of Melbourne

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[L-1] Clemens, J. D.; Birch, W. D. (2012-12-15), "Assembly of a zoned volcanic magma chamber from multiple magma batches: The Cerberean Cauldron, Marysville Igneous Complex, Australia" (in en), Lithos 155: 272–288, doi:10.1016/j.lithos.2012.09.007, ISSN 0024-4937, https://www.sciencedirect.com/science/article/pii/S0024493712003714

[B-2] Birch, W. D. (1970), An investigation of the Upper Devonian Cerberean Cauldron complex in central Victoria, University of Melbourne