Rhine Rift Valley
Quick Summary
The Rhine Rift Valley is an elongated trough in Germany formed by the subsidence of a segment of the Earth's crust between normal faults. This geological feature is a type of tectonic valley, distinct from those created by erosion. The valley is typically long and narrow, with a relatively flat floor, and its sides drop steeply.1
The Rhine River itself is a major waterway in western Europe, flowing from Switzerland through Germany to the North Sea. It has historically been a significant route for trade and industrial transport. The Rhine River valley is also associated with the Middle Rhine Highlands, a varied plateau region in Germany with areas of rugged relief. The Rhine River has been a boundary line and a route for political and cultural unification throughout history.234
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