Abstract
Located 90 km straight east of the Deep Bay crater in the Saskatchewan region, the Gow crater is roughly circular lake with the prominent Calder Island, 1.5 km high and 35 m wide, defined as its central uplift.
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References
Hodge, P. W. (1994). Meteorite craters and impact structures of the Earth. Cambridge University Press.
Osinski, G. R., Singleton, A. C., Ozaruk, A., & Hansen, J. R. (2012). New investigations of the Gow Lake impact structure, Saskatchewan, Canada. In 43rd Lunar and Planetary Science Conference.
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Flamini, E., Coletta, A., Battagliere, M.L., Virelli, M. (2019). Gow, Canada. In: Flamini, E., Di Martino, M., Coletta, A. (eds) Encyclopedic Atlas of Terrestrial Impact Craters. Springer, Cham. https://doi.org/10.1007/978-3-030-05451-9_144
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DOI: https://doi.org/10.1007/978-3-030-05451-9_144
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