The area, dubbed the Athabasca granulite terrane, is exciting geologists who say they would have to somehow transport themselves 25 miles below the planet's surface to see features they can observe underfoot while strolling around hundreds of acres of rocky outcrop, Postmedia News reported this week.
The formation was created when a vast amount of molten rock was thrust up from the Earth's lower crust before solidifying at the surface 2 billion years ago.
While similar features exist around the world, none are as expansive or varied in the clues they offer into the planet's hidden depths, scientists say.
"We do not have the technology to drill anywhere near to the lower crust," Michael Williams, a geoscientist at the University of Massachusetts, says.
"But in northern Saskatchewan, we can walk around on lower crust, mapping and sampling. Even if we could drill that deep, we would only get a small round core of rock to look at. In Saskatchewan, we have acres of exposure."
Williams says the region still has many secrets to reveal about the creation of the Earth's crust, the formation of mountain chains such as the Himalayas and the dynamics of the San Andreas Fault and other geological rifts.
"The region is a natural laboratory for studying the boundary area between the Earth's crust and mantle -- at least the processes that were active in the deep crust long ago," said Williams. "We hypothesize that similar processes are occurring today deep in the crust. This is what makes it so special."