The team of researchers studied a type of rock called Idiwhaa gneiss, which is more than 4 billion years old, found in northwest Canada and the oldest large swath of rock on Earth. Although scientists have identified some grains of even older rocks, those grains are so tiny they're practically microscopic.

Specifically, the team looked at the chemical composition of those rocks and modeled what conditions rocks with that recipe could have formed under. The magic combination seemed to be temperatures of up to 1,650 degrees Fahrenheit (900 degrees Celsius) partnered with low pressures.

That's a tricky combination to find under normal circumstances, the researchers said. Usually, hotter temperatures require traveling deeper into the earth, but pressures there are higher. The team found, however, that meteorites could solve that conundrum.

That's because when meteorites were common, in the early days of Earth, the impacts could have raised temperatures enough to melt rocks in the very top of the crust — just the first 1.8 miles (3 kilometers) or so ― without the rocks experiencing high pressures.

Most of the rocks produced during that time have fallen back into the Earth's interior through plate tectonics, melting away its identifiable characteristics. But the Idiwhaa rocks remain, where they were named by the local Tlicho people long before scientists came to analyze them.

The research is described in a paper published today in the journal Nature Geoscience.