kviðarhol

Kviðarhol is a geological term referring to a specific type of landform. It describes a glacial valley that has been significantly widened and deepened by the erosive power of glaciers. These valleys are typically U-shaped in cross-section, with steep, often cliff-like sides and a relatively flat floor. This distinctive shape is a result of the immense weight and abrasive action of the ice as it moves down the valley, scraping away rock and sediment.

The formation of kviðarhol involves several stages. Initially, a river valley, often V-shaped, is carved by a river. When glaciation occurs, the ice fills this valley, and its slow, powerful movement begins to widen and deepen the existing channel. Over time, the glacier's base grinds against the valley floor and sides, plucking out rock fragments and transporting them, further contributing to erosion. This process can transform a relatively narrow valley into a broad, expansive one.

Features commonly associated with kviðarhol include hanging valleys, which are smaller valleys that enter the main glacial valley at a higher elevation due to the main glacier's greater erosive power. Waterfalls or steep cascades often mark the junction where the stream from a hanging valley descends into the main valley. Moraines, ridges of rock and sediment deposited by the glacier, may also be present at the valley floor or sides. Kviðarhol are prominent features in mountainous regions that have experienced significant glaciation, such as Scandinavia, the Alps, and parts of North America.