Isostatic rebound Many published papers demonstrate that
isostatic depression of the Earth's crust happened in the early Holocene. This process has led to submerging substantial portions of coastal areas adjacent to continental
ice sheets and resulted in the accumulations of
marine sediments and
fossils within them. A well-documented example of flooding caused by isostatic depression is the case of
Charlotte, The Vermont Whale, a fossil whale found in the deposits of the former
Champlain Sea. As with many similar marine deposits, the sediments which accumulated within the Champlain Sea lack the physical characteristics—sedimentary structures, interlayers, and textures—that characterise sediments deposited by a mega-
tsunami. These deposits and the associated fossils have been dated to significantly earlier periods than the times the bolide hypothesis proposed. In the case of the Champlain Sea, its sediments started to accumulate around 13,000 BP, almost 3,400 years before the oldest of the hypothesized Holocene bolide impacts.
Dating lakes (17,500 years BP), and modern remnants A significant amount of the physical evidence used by Kristan-Tollmann and Tollmann, has dated the Australasian tektites to the
Middle Pleistocene; about 790,000 years
BP. In addition, the formation of salt lakes and salt flats is neither synchronous nor consistent with the hypothesized impacts having occurred about either 9,640 BP or 5,150 BP. For example, in the case of
Lake Bonneville,
Lake Lahontan,
Mono Lake, and other
Pleistocene pluvial lakes in the western United States, the transition to salt lakes and salt flats occurred at different times between 12,000 and 16,000 BP. Thus, the change from freshwater to salty water and eventually salt flats started over 2,400 to 6,400 years before the oldest of the impacts hypothesized by the Tollmann bolide hypothesis occurred. As a result, it is impossible that the formation of these salt lakes could have been associated with the impact hypothesized by Kristan-Tollmann and Tollmann. == Megatsunami ==