Brad PetersGuest
Paul GabrielsonHost
Sediment from continents flows into ocean basins where it is pushed down or subducted back into the Earth's mantle at plate boundaries.

This rock cycle can restart if the sediment re-melts and eventually erupts again as lava from a volcano.

In a recent PNAS study, Brad Peters at ETH Zurich and colleagues studied the isotopic signatures of relatively recent volcanic rocks in the Marquesas Archipelago.

The results imply an active rock cycle much earlier than plate tectonics was thought to have begun.

Sediment from continents flows into ocean basins where it is pushed down or subducted back into the Earth's mantle at plate boundaries.

This rock cycle can restart if the sediment re-melts and eventually erupts again as lava from a volcano.

In a recent PNAS study, Brad Peters at ETH Zurich and colleagues studied the isotopic signatures of relatively recent volcanic rocks in the Marquesas Archipelago.

The results imply an active rock cycle much earlier than plate tectonics was thought to have begun.
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