A pyramidal peak, or sometimes in its most extreme form called a glacial horn, is a mountaintop that has been modified by the action of ice during glaciation and frost weathering. If the use is unambiguous within a mountain context, then the simple terms peak or horn may be used.

Formation

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Ice fields develop U- or bowl-shaped basins in the sides of a mountain called cirques. These encroach on each other to produce ridges known as arêtes. The meeting of three or more glaciers forms a peak. A peak has a sharp summit and steep slopes on at least three sides. They are a common shape for mountain tops in well glaciated areas.

A glacial horn takes the process to its limits, producing near vertical faces on all sides. In the Alps, "Horn" is also the name of very exposed peaks with slope inclinations of 45-60°(e.g. Kitzbüheler Horn).

Examples

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Good examples would be:-

• The Matterhorn in Zermatt, on the border between Switzerland and Italy,
• the Kitzsteinhorn near Kaprun in Salzburg, Austria,
• Mt Blanc above Chamonix in eastern France,
• Mount Wilbur in Glacier National Park, Montana, USA,
• Reynolds Mountain, Glacier National Park, USA, and
• the Grand Teton, Wyoming, USA.

References

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• Illustrated Glossary of Alpine Glacial Landforms

Mountains | Landforms | Glaciology

Връх | Spitze | Topografski vrh