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。
2
The horizontal stress is high in the uplift and low in the subsidence areas.
隆起区多属高水平应力区，沉降区多属低水平应力区。
3
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