Abstract
Several lines of evidence were presented in Gasperini et.al. [Terra Nova (2007), vol. 19, pp. 245-251] suggesting that Lake Cheko, a small lake close to the alleged epicentre of the 1908 Tunguska Event, might be a secondary impact crater. Collins et.al. [Terra Nova (2008), this volume] argue against this hypothesis. We reply here arguing in favour of an impact origin for Lake Cheko. © Journal compilation © 2008 Blackwell Publishing.
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CITATION STYLE
APA
Gasperini, L., Bonatti, E., & Longo, G. (2008, April). Lake Cheko and the Tunguska Event: Impact or non-impact? Terra Nova. https://doi.org/10.1111/j.1365-3121.2008.00792.x
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