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Slippery stretching explains ocean floor formation

Researchers found regions of the earth's crust stretching apart to form new sea floor, a process previously underestimated. The study reveals detachment faults, characterized by curved surfaces and swarms of tiny earthquakes, are common along the Mid-Atlantic Ridge.

SourceUniversity of Leeds·JournalNature·DateJul 27, 2006
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New study shows earthquake shaking triggers aftershocks

Researchers found that the amplitude of shaking directly affects the chance of an aftershock, following an inverse power law relation. This discovery challenges the long-held assumption that aftershocks are triggered by static stress resulting from crust movement.

SourceUniversity of California - Santa Cruz·JournalNature·DateJun 7, 2006

Weird wave behavior near earth's core

Researchers used experiments and mathematical modeling to understand seismic wave behavior in the lower mantle, finding that mineral grain alignment causes unusual wave behavior. The study provides a window into Earth's inner workings and is an important step toward integrating seismology and geodynamics in the lower mantle.

SourceUniversity of Michigan·JournalNature·DateMar 20, 2002

Just how old is the Tibetan Plateau?

A new study reveals the Tibetan Plateau is approximately 13.5 million years old and has reached its maximum average height of 5 kilometers. The plateau's formation is attributed to the collision between two tectonic plates, resulting in a flat-topped spreading plateau.

SourceUniversity of California - Santa Barbara·JournalNature·DateAug 8, 2001