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The most notable feature in the Shenandoah Valley is Massanutten Mountain. Massanutten is a doubly-plunging synclinorium whose subsurface geology continues through the Great Valley. |
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The north and south forks of the Shenandoah River snake around Massanutten mountain to meet at Front Royal. The meanders may be structurally controlled by parallel joint sets. (Photograph from NASA.) |
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