The North American Cordillera consists of many terranes which bear magnetic and fossil evidence suggesting they originated far to the south of the modern-day positions.

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The North American Cordillera consists of many terranes which have been transported and accreted to their current location over millions of years. Magnetic and fossil evidence suggest that these terranes originated in different locations, including ones far to the south of their current positions.

The North American Cordillera Consists of Many Terranes Which Bear