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In about 250 million years, continents may merge again into a new supercontinent scientists call Pangaea Ultima or Amasia.Earth’s surface will look dramatically
different — yet driven by the same deep processes at work today.

By studying hotspot tracks, scientists can calculate both the direction and velocity of plate motion. In addition, mid-ocean ridges, where new oceanic crust is created, can host deposits of sulfide minerals that are rich in copper, zinc, and other metals.
These deposits are formed by hydrothermal fluids that are
released from the subducting slab and the overlying mantle wedge, causing mineral precipitation in the surrounding rocks.
At convergent plate boundaries, subduction zones can generate large-scale mineral deposits,
including porphyry copper, epithermal gold, and silver, and massive sulfide deposits.


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