The Matterhorn is located on the border between Switzerland and Italy. It rises above the town of Zermatt in the canton of Valais to the northeast and Breuil-Cervinia in the Aosta Valley to the south. Its peak reaches a height of 4.478 meters, making it one of the highest peaks in the Alps. It is probably the most famous mountain in the Alps, and its imposing pyramid shape has been replicated many times.
In this article we are going to tell you all the characteristics, geology, formation and much more about Mount Cervino.
Key features
The Matterhorn's unique shape makes it one of the world's most iconic mountains. Its name varies depending on the region and language: Matterhorn in German and Monte Cervino in Italian and Spanish, to name a few. The name appears to mean "mountain in the meadow" in German.
Symbol of the Alps, it is one of the highest peaks in Europe, climbed for the first time in 1865 by the English mountaineer Edward Whymper.
The Matterhorn is one of the high peaks of the Alps, located on the border of Switzerland and Italy. It lies in a mountain range known as the Pennine Alps, about 10 km from Zermatt, Switzerland. It features a rare and almost perfectly pyramid-shaped peak with four steep, nearly flat sides separated by the Leone, Zmutt, Furggen, and Hörnli ridges, pointing almost directly to the four cardinal directions. North, east, and west are aligned on the Swiss side, while south is on the Italian side.
The mountain has two peaks: the Swiss peak and the Italian peak. With an estimated height of 4.478 meters, it is the sixth highest in the Alps. Unlike other alpine mountains, its surface is not completely covered by snow and ice, but large brown sections of rock can be glimpsed, however, it has not been abandoned by large glaciers at the base of the mountain. For example, the Matterhorn Glacier sits at the base of the north face of the mountain. Mornings are usually a few degrees below zero due to elevation and snowfall, but the day can be a bit warmer.
In 2014, geologists reported in the journal Nature Revelation that they had found evidence of a huge hollow chamber inside the Matterhorn, suggesting that it may have collapsed rapidly and violently at some point in history. Of course, more research is needed in this area.
Formation of the Matterhorn
Since the Matterhorn is a mountain in the Alps, its formation began when the mountain range started to rise above the Earth's surface. This process began when Pangaea started to break apart into Laurasia and Gondwana. These two landmasses are separated by the Tethys Ocean. The shape changed again when the Earth's inner crust shifted more than 100 million years ago , and then Africa slowly moved toward Europe until they were very close to each other.
When the European continent collided with the Apulian Plate, the Earth's crust folded over several million years. Then, about 50 million years ago, the crust began to rise until the Matterhorn became fully visible. However, it is not the same as it is today because its shape is the product of glacial erosion, and its summit is formed by several layers of rock.
Flora and fauna of the Matterhorn
Due to its natural beauty and historical and cultural significance, this mountain is one of the most photographed in the world. Surrounding its majestic peaks are vast green valleys filled with pastures, grasses, and short-flowering plants, as well as some trees such as conifers. The Alps are home to flowering plants that can survive at altitudes of over 4000 meters , making the flora of the Alps interesting to study , although technically the upper half of the mountain is devoid of vegetation. Lichens are often found clinging to the highest rocks and are frequented by wild goats.
As for wildlife, the mountains are known to be home to more than 30.000 species , including mammals, birds, insects, and some reptiles. The Iberian ibex (Capra ibex) is a renowned climber, capable of spending long periods high up in the narrow spaces between the rocks.
Climate
The Matterhorn has two distinct peaks, both on rocky ridges 100 meters long: the Swiss peak (4477,5 m) in the east and the Italian peak (4476,4 m) in the west. Its name comes from the first ascent, not for geographical reasons, since both are on the border. The height of the mount was first measured by Geneva geologist and explorer Horace Bénédict de Saussure in August 1792, using a 50-foot chain spanning the Theodul Glacier and a sextant. He calculated the height to be 4.501,7 meters. In 1868, the Italian engineer Felice Giordano measured the height of 4.505 meters with a mercury barometer that he took to the summit. The Dufour map, followed later by Italian explorers, gave 4.482 meters, or 14.704 feet, as the height of the Swiss summit.
A recent measurement (1999) has been made using GPS technology, which gave the height of the Matterhorn with an accuracy of one centimeter, and its changes have been checked. The result was 4.477,54 meters above sea level.
Geology
Most of the foothills are located on the Tsaté nappe, the remnants of the Piedmontese-Ligurian oceanic crust (ophiolite) and its sedimentary rocks . The mountain reaches a height of 3.400 meters and is formed by continuous layers of ophiolite and sedimentary rocks. From 3.400 meters to the summit, the rock is gneiss of the Dent Blanche nappe (an Australian alpine rock formation). These are separated by the Arolla series (below 4.200 m) and the Valpelline belt (above). Other mountains in the region (Weisshorn, Zinalrothorn, Dent Blanche, Mont Collon) also belong to the Dent Blanche nappe.
The Matterhorn developed its characteristic pyramidal shape more recently due to natural erosion over the last few million years. At the beginning of the Alpine orogeny, the Matterhorn was just a rounded, small mountain. Because of its height above the snow line, its sides are covered in ice, which causes the snow to accumulate and compact.
I hope that with this information you can learn more about Mount Cervino and its characteristics.