The resulting stress remained stored for millions of years until uplift associated with the Mississippi erosion event led to the unclamping of old faults lying beneath.

由此产生的应力被压存了数百万年，直到隆起伴随着密西西比的侵蚀导致下面的旧断层松脱释放。

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The resulting stress remained stored for millions of years until uplift associated with the Mississippi erosion event led to the unclamping of old faults lying beneath.

由此产生的应力被压存了数百万年，直到隆起伴随着密西西比的侵蚀导致下面的旧断层松脱释放。

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