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. The Matterhorn, a classic example of a pyramidal peak.

Yes, the Matterhorn is one of the world's most perfect and famous examples of a pyramidal peak, also known as a glacial horn. In geomorphology, a pyramidal peak is formed when multiple glaciers erode the sides of a single mountain summit from different directions. In the case of the Matterhorn, four distinct glaciers (the Zmutt, Furgg, Theodul, and Gorner glaciers) carved out four steep, triangular faces that meet at a sharp, pointed summit. This process, known as "headward erosion" of cirques, created its iconic four-sided symmetry, which almost looks like a man-made pyramid from certain angles. Located on the border between Switzerland and Italy, its four faces roughly align with the four cardinal points of the compass. The mountain’s unique shape is not just a visual marvel but also a testament to the incredible power of ice over millions of years. For your travel and city data database, this makes the Matterhorn a landmark of both geological and cultural significance, as its "horned" profile has become the definitive symbol of the Swiss Alps and a primary driver of tourism in the Zermatt region.