This pretty well seals the deal. Recall that I began looking for a major impact
event merely knowing that there had to be one to provide the energy necessary
to shift the crust thirty degrees south.
This led to the discovery of scant evidence that effectively meant that
any such impact was a planned event that struck a bull’s eye at the North Pole. This led to a complete reconsideration of the
last 70,000 years of human history.
Now we have a stack of evidence
including this decisive lake bottom that confirms the necessary trajectory
although the shoe has not dropped yet with other researchers in the understanding
that this struck the North Polar Region then located thirty degrees north from
its present location in Hudson Bay .
As surmised, it was also a comet
and importantly, it was unique since the impact that took out the dinosaurs. This means that a putative earlier shift was
a natural result of Ice imbalance and merely proved the crustal mobility,
setting the stage for a direct intervention that would end the Ice Age.
The bulk of the impact mass would
have struck the ice over a broad area and induced a kinetic impulse into the
crust in the correct direction to send the pole South to its natural limit
caused by the elimination of the free space for the movement in the critical
viscosity free carbon zone.
Other fragments outside the
impact halo entered the atmosphere and explode over Mexico in particular where ample
evidence is now been recognized. This
lake bottom confirms dates and that it is an impact event as large as we
expected.
Study supports theory of extraterrestrial impact
by Staff Writers
This is James Kennett. Credit: University
of California - Santa Barbara .
A 16-member international team of researchers that includes James
Kennett, professor of earth science
at UC Santa Barbara , has identified a nearly
13,000-year-old layer of thin, dark sediment buried in the floor of Lake Cuitzeo
in central Mexico .
The sediment layer contains an exotic assemblage of materials,
including nanodiamonds, impact spherules, and more, which, according to the
researchers, are the result of a cosmic body impacting Earth.
These new data are the latest to strongly support of a controversial
hypothesis proposing that a major cosmic impact with Earth occurred 12,900
years ago at the onset of an unusual cold climatic period called the YoungerDryas.
The researchers' findings appear in the Proceedings of the National Academy
of Sciences.
Conducting a wide range of exhaustive tests, the researchers
conclusively identified a family of nanodiamonds, including the impact form of
nanodiamonds called lonsdaleite, which is unique to cosmic impact.
The researchers also found spherules that had collided at high
velocities with other spherules during the chaos of impact. Such features,
Kennett noted, could not have formed through anthropogenic, volcanic, or other
natural terrestrial processes. "These materials form only through cosmic
impact," he said.
The data suggest that a comet or asteroid - likely a large, previously
fragmented body, greater than several hundred meters in diameter - entered the
atmosphere at a relatively shallow angle.
The heat at impact burned biomass, melted surface rocks,
and caused major environmental disruption. "These results are consistent
with earlier reported discoveries throughout North America
of abrupt ecosystem change, megafaunal extinction, and human cultural change
and population reduction," Kennett explained.
The sediment layer identified by the researchers is of the same age as that
previously reported at numerous locations throughout North America, Greenland, and
Western Europe . The current discovery extends
the known range of the nanodiamond-rich layer into Mexico and the tropics. In
addition, it is the first reported for true lake deposits.
In the entire geologic record, there are only two known continent-wide
layers with abundance peaks in nanodiamonds, impact spherules, and aciniform
soot. These are in the 65-million-year-old Cretaceous-Paleogene boundary layer
that coincided with major extinctions, including the dinosaurs and ammonites;
and the Younger Dryas boundary event at 12,900 years ago, closely associated
with the extinctions of many large North American animals, including mammoths,
mastodons, saber-tooth cats, and dire wolves.
"The timing of the impact event coincided
with the most extraordinary biotic and environmental changes over Mexico and Central America
during the last approximately 20,000 years, as recorded by others in several
regional lake deposits," said Kennett. "These changes were large,
abrupt, and unprecedented, and had been recorded and identified by earlier
investigators as a 'time of crisis.' "
Other scientists contributing to the research include
Isabel Israde-Alcantara and Gabriela Dominguez-Vasquez of the Universidad
Michoacana de San Nicolas de Hidalgo; James L. Bischoff of the U.S. Geological
Survey; Hong-Chun Li of National Taiwan University; Paul S. DeCarli of SRI
International; Ted E. Bunch and James H. Wittke of Northern Arizona University;
James C. Weaver of Harvard University; Richard B. Firestone of Lawrence
Berkeley National Laboratory; Allen West of GeoScience Consulting;
Chris Mercer of the National Institute for Materials Science; Sujing Zie and
Eric K. Richman of the University of Oregon, Eugene; and Charles R. Kinzie and
Wendy S. Wolbach of DePaul University.
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