Research news on continenetal drift

Continental drift is the geophysical phenomenon describing the gradual horizontal movement of Earth’s continental lithospheric plates relative to one another over geological time. Driven primarily by mantle convection, slab pull, and ridge push forces, this process results in the reconfiguration of ocean basins and continents, influencing orogenesis, basin formation, and large-scale patterns of volcanism and seismicity. Continental drift operates on timescales of millions of years, with typical plate velocities of a few centimeters per year, and is quantitatively constrained by paleomagnetic data, marine magnetic anomalies, hotspot tracks, GPS geodesy, and stratigraphic and fossil correlation across now-separated continental margins.

Where was your backyard millions of years ago?

An international team of Earth scientists led by Utrecht professor Douwe van Hinsbergen has developed an online tool that allows you to see, for any given location on Earth, what latitude it occupied in the distant past, ...

How our planet's history was shaped when the Earth moved

The history of Earth is written on the great tablets of tectonic plates. The motions of plates shaped land masses, formed oceans, and created the varied climates and habitats that set the stage for evolution and the diversity ...

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