Abbott, D.H., Masse, W.B., Burckle, L.D., Breger, D. and Gerard-Little, P., 2006. Burckle abyssal impact crater: Did this impact produce a global deluge? In The Atlantis Hypothesis: Searching for a Lost Land, Heliotopos Publications, St. P. Papmarinopoulous, Ed., pp. 179-190. (black and white version in book with Appendix added).
We have found an impact crater that is likely < 6000 years old. Burckle crater is in the central Indian Ocean on the edge of a fracture zone at 30.87° S 61.36°E. The crater is 29±1 km wide and is the inferred source of layers with high magnetic susceptibility in 3 deep sea cores. Each layer goes to the top of the core. Two out of 3 of the cores have basal Pleistocene ages and the basal age of the third is unknown. The high susceptibility layers contain broken plagioclase, spinel periodotite, and chrysotile asbestos. One sample contains pure Ni with drops of oxidized Ni. Because pure Ni melts at 1453°C, it is very likely that the drops formed during an impact. The high susceptibility layers from 2 cores are over 5 times thicker than they should be for a 29 km wide source crater. We also find that a 29 km wide source crater cannot vaporize enough seawater to produce meters of rain, even in a restricted region between 4750 and 7250 km from the crater. Thus, we infer that Burckle crater was produced as part of a Shoemaker-Levy type impact of a comet. The fragmented comet also produced two other large impact centers, one in the northwest Pacific and another in the central eastern Pacific. Where the rainout from these impact centers overlaps, we see deluge events that are over a week long. The impact event also produced devastating tsunamis, winds, and associated social upheaval. We date the event to around 2807 B.C.