Science: Whether erosion of rock and soil from Earth’s surface is driven by tectonic activity or by climate has long been debated. In a recent study published in Nature, Frédéric Herman of the University of Lausanne in Switzerland and colleagues used thermochronometry to measure how the temperature of Earth’s rock has changed over time and compare it with how fast Earth’s surface has eroded. They found that while erosion rates have increased since about 6 million years ago, they have increased dramatically since about 2 million years ago, after the onset of the most recent ice age. The researchers attribute the accelerated erosion to glacial processes and add that if Earth’s climate continues to cool as it has over the past few million years, the erosion rate will likely continue to increase. However, should temperatures cease to cool—whether by natural climate variations or global warming—sediment accumulations could increase.
The finding that the Saturnian moon may host layers of icy slush instead of a global ocean could change how planetary scientists think about other icy moons as well.
Modeling the shapes of tree branches, neurons, and blood vessels is a thorny problem, but researchers have just discovered that much of the math has already been done.
January 29, 2026 12:52 PM
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