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Ancient plate tectonics in the Archean period differs from modern plate tectonics in the Phanerozoic period because of the higher mantle temperatures inside the early Earth, the thicker basaltic crust, and the non-depletion of melt-mobile incompatible trace elements in the mantle. Credit: Science China Press

Plate tectonics in the Archean: Observation versus interpretation

Discovery of a dinosaur tail in northern Mexico

Scientists create world’s first 3D thermal image of volcano

A quick step on hot lava

Taking Selfie at Crater Base

Formation of Hydrocarbon Trap

White Desert, Farafra, Egypt

River of Fire

Debris Flow

A cut slice of altered mantle rock. (Photo by: Solvin Zankl)

Researchers studying ocean transform faults, describe a previously unknown part of...

Meet Spinosaurus, the first-known water dinosaur

When Magma Meets Water

Debris Flow Dynamics

Molten Paradise “Kilauea Volcano”

Early Hawaiian Volcano Footage

Lava Eruption at Colima Volcano, Mexico

Door to Hell “Gate to Hell”

Silurian Scorpion from Ontario – Out of the water

A Landslide-Induced Tsunami Hit Nuugaatsiaq, Greenland

Sampling Hot Molten Lava

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