
Along the eastern front of the Appalachian Mountains, buried just below the surface, lies a fragment of a lost continent.
Running from Maine to Georgia, the 200-kilometer-thick slab of crust was probably created by volcanic eruptions during the breakup of the Pangaea supercontinent some 200 million years ago and later buried by silt from eroding mountains.
Known as the Piedmont Resistor, this piece of Pangaea is one of the signature discoveries of the Magnetotelluric (MT) Array, 1800 temporary stations scattered across the contiguous United States that measured the conductivity of deep rocks.
Now, 20 years after it started, the MT Array has released its final map and model. It shows how the assembly of the continent left hidden structures such as the Piedmont Resistor—and mineral riches.
Learn more: scim.ag/3PgPC9M

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