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pyramidal peak

{{Short description|Angular, sharply pointed mountainous peak}}

{{Other uses|Peak (disambiguation)}}

{{Use dmy dates|date=January 2025}}

File:Matterhorn from Domhütte - 2.jpg, a classic example of a pyramidal peak.]]

A pyramidal peak, sometimes called a glacial horn in extreme cases, is an angular, sharply pointed mountain peak which results from the cirque erosion due to multiple glaciers diverging from a central point. Pyramidal peaks are often examples of nunataks.

Formation

File:Cirques mountainmass en.svg

File:Kinnerly Peak.jpg in Glacier National Park in the U.S. state of Montana|alt=]]

Glaciers, typically forming in drainages on the sides of a mountain, develop bowl-shaped basins called cirques (sometimes called 'corries' – from Scottish Gaelic {{lang|gd|coire}} [kʰəɾə] (a bowl) – or {{lang|cy|cwm}}s). Cirque glaciers have rotational sliding that abrades the floor of the basin more than walls and that causes the bowl shape to form. As cirques are formed by glaciation in an alpine environment, the headwall and ridges between parallel glaciers called arêtes become more steep and defined. This occurs due to freeze/thaw and mass wasting beneath the ice surface. It is widely held{{by whom|date=November 2012}} that a common cause for headwall steepening and extension headward is the crevasses known as bergschrund that occur between the moving ice and the headwall. Plucking and shattering can be seen here by those exploring the crevasses. A cirque is exposed when the glacier that created it recedes.{{Citation needed|date=February 2021}}

When three or more of these cirques converge on a central point, they create a pyramid-shaped peak with steep walls. These horns are a common shape for mountain tops in highly glaciated areas. The number of faces of a horn depends on the number of cirques involved in the formation of the peak: three to four is most common. Horns with more than four faces include the Weissmies and the Mönch.{{cite book | first1=Clifford | title=Glacial and Periglacial Geomorphology | publisher=St. Martin's Press | last2=King | first2=Cuchlaine A. | last1=Embleton | author-link1 = Clifford Embleton| author-link2 = Cuchlaine King| lccn=68-20348 | year=1968 | location=New York | page=193}} A peak with four symmetrical faces is called a Matterhorn (after the Matterhorn, a mountain in the Alps).{{cite web | url=http://pubs.usgs.gov/of/2004/1216/text.html#h | title=Glossary of Glacier Terminology | publisher=US Geological Survey | access-date=12 October 2012}}

The peak of a glacial horn will often outlast the arêtes on its flanks. As the rock around it erodes, the horn gains in prominence. Eventually, a glacial horn will have near vertical faces on all sides.{{citation needed|date=October 2012}} In the Alps, "horn" is also the name of very exposed peaks with slope inclinations of 45-60° (e.g. Kitzbüheler Horn).{{citation needed|date=October 2012}}

Examples

File:Alpamayo 12.jpg in Huascarán National Park, Peru]]

File:Artesonraju.jpg in Huascarán National Park, Peru]]

File:Zabeshkoto ezero pirin IMG 7410.jpg Mountain, Bulgaria]]

See also

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References

{{Reflist}}

Bibliography

  • {{cite book | title=Surface Processes and Landforms | publisher=Prentice Hall | author=Easterbrook, Don J. | year=1999 | location=Upper Saddle River, NJ | pages=334–336 | isbn=978-0138609580 | edition=2nd}}

External links

  • {{cite web | url=http://www.uwsp.edu/geo/faculty/lemke/alpine_glacial_glossary/landforms/horn.html | title=Illustrated Glossary of Alpine Glacial Landforms | access-date=12 October 2012 | author=Lemke, Karen A. | year=2010 | url-status=dead | archive-url=https://web.archive.org/web/20120813190415/http://www4.uwsp.edu/geo/faculty/lemke/alpine_glacial_glossary/landforms/horn.html | archive-date=13 August 2012 }}

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