Ancient Plate Remnants Cause Slow Subsidence in North America
Researchers have discovered that remnants of an ancient tectonic plate known as the Farallon Plate are causing slow subsidence in the core (craton) of the North American continent. The study, published on March 28, 2025, in Nature Geosciences, highlights a phenomenon called “cratonic drip” – the gradual descent of rock blocks that make up the … Read more