Colin Sproat and Brian Pratt are researchers at the University of Saskatchewan.
Brian Pratt and Colin Sproat visited three locations north of The Pas, Manitoba, where they observed that strata had been broken into pieces and mixed with the clay.
According to them, clay can only come from dry land and a tsunami.
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In an interview on the radio show Saskatoon Morning,University of Saskatchewan geological sciences professor Brian Pratt explains that faults in the region's crust were still active at the time. The movement of a fault would have triggered strong waves in the inland sea.
The coastal line and shallow waters were swept by wave trains. [The tsunami] would then have swept the coastal area, he says, adding that the tsunami would then have retreated, taking the clay with it.
The tsunami hypothesis is a radical interpretation of the facts, as Brian Pratt recognizes.
He explains that he and his colleague had an advantage over the geologists who worked before them, as over the past decade several new quarries have been dug in northern Manitoba, revealing new secrets about the Williston Basin.
Deposits similar to those observed by the researchers could in principle have been formed by major storms.
Brian Pratt and Colin Sproat, however, ruled out this hypothesis, as there were no other signs indicating regular thunderstorm activity.
Additionally, they believe the area was too close to ancient Ecuador to have experienced hurricanes.
Colin Sproat believes that these discoveries are a unique chance to study the geological processes in an environment that does not exist anywhere else on the planet today.
Researchers are also planning ;go visit other places in Canada to see if tsunamis played a more important role in Earth's history.
With information from Candice Lipski