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A pyramidal peak, sometimes in its most extreme form called a glacial horn, is an angular, sharply pointed mountain peak which results from the cirque erosion due to multiple glaciers diverging from a central point.hese 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 Moench. mÃ¶nch
As a result, previous traces of other materials have vanished, so the oldest surviving animal horn dates back to the Late Iron Age in Visnum, Sweden. As big horned animals are rarely found in Scandinavia, blowing horns are often made from wood, wound birch bark or bout, called a lur.he hunting horn was used to communicate on a hunt and is still used today in some places. In Biscay, territory of the Basque Country, following an old tradition, a practice is being restored to blow the horn from five mountains in the province once a year.