The Matterhorn (German), Monte Cervino (Italian) or Mont Cervin (French), is a mountain in the Pennine Alps on the border between Switzerland and Italy. Its summit is 4,478 metres (14,690 ft) high, making it one of the highest peaks in the Alps. The four steep faces, rising above the surrounding glaciers, face the four compass points. The mountain overlooks the town of Zermatt in the canton of Valais to the north-east and Breuil-Cervinia in the Aosta Valley to the south. The Theodul Pass, located at the eastern base of the peak, is the lowest passage between its north and south side.
The Matterhorn was one of the last great Alpine peaks to be climbed and its first ascent marked the end of the golden age of alpinism. It was made in 1865 by a party led by Edward Whymper and ended disastrously when four of its members fell to their deaths on the descent. The north face was not climbed until 1931, and is amongst the six great north faces of the Alps. The Matterhorn is one of the deadliest peaks in the Alps: from 1865 – when it was first climbed – to 1995, 500 alpinists died on it.
The Matterhorn has become an iconic emblem of the Swiss Alps and the Alps in general. Since the end of the 19th century, when railways were built, it attracted more and more visitors and climbers. Each summer a large number of mountaineers try to climb the Matterhorn via the northeast Hörnli ridge, the most popular route to the summit.
Naming
The mountain derives its name from the German words Matte, meaning "meadow", and Horn, which means "peak". The migration of the name "meadow" from the lower part of the countryside to the peak is common in the Alps. The Italian and French names (Cervino and Cervin) come from Mons Silvius (or Mons Sylvius) from the Latin word silva, meaning forest (with again the migration of the name from the lower part to the peak). The changing of the first letter "s" to "c" is attributed to Horace Bénédict de Saussure, who thought that the word was related to a deer (French: cerf and Italian: cervo).
In Sebastian Münster's Cosmography, published in 1543, the name of Matter is given to the Theodul Pass, and this seems to be the origin of the present German name of the mountain. On Münster's topographical chart this group is marked under the names of Augstalberg ("Aosta mountain") and Mons Silvius. An hypothesis of Josias Simler (De Alpibus Commentarius, 1574) on the etymology of the name of Mons Silvius was readopted by T. G. Farinetti: "Silvius was probably a Roman leader who sojourned with his legions in the land of the Salassi and the Seduni, and perhaps crossed the Theodul Pass between these two places. This Silvius may have been that same Servius Galba whom Caesar charged with the opening up of the Alpine passes, which from that time onward traders have been wont to cross with great danger and grave difficulty. Servius Galba, in order to carry out Caesar's orders, came with his legions from Allobrogi (Savoy) to Octodurum (Martigny) in the Valais, and pitched his camp there. The passes which he had orders to open from there could be no other than the St. Bernard, the Simplon, the Theodul, and the Moro; it therefore seems likely that the name of Servius, whence Silvius and later Servin, or Cervin, was given in his honour to the famous pyramid." It is not exactly known at what period the new name of Servin, or Cervin, replaced the old, from which it seems to be derived.
The Matterhorn is also named Gran Becca by the Valdôtains and Horu by the local Walliser German speaking people.
Height
The Matterhorn is an isolated mountain. Because of its position on the main Alpine watershed and its great height, the Matterhorn is exposed to rapid weather changes. In addition the steep faces of the mountain and its isolated location make it prone to banner clouds formation with the air flowing around and creating vortices, conducting condensation of the air on the lee side.
The Matterhorn has two distinct summits, both situated on a 100-metre-long rocky ridge: the Swiss summit (4,477.5 m) on the east and the Italian summit (4,476.4 m) on the west. Their names originated from the first ascents, not for geographic reasons, as they are both located on the border. In August 1792, the Genevan geologist and explorer Horace Bénédict de Saussure made the first measurement of the Matterhorn's height, using a 50-foot-long chain spread out on the Theodul glacier and a sextant. He calculated a height of 4,501.7 metres. In 1868 the Italian engineer Felice Giordano measured a height of 4,505 metres by means of a mercurial barometer, which he had taken up to the summit. The Dufour map, which was afterwards followed by the Italian surveyors, gave 4,482 metres, or 14,704 feet, as the height of the Swiss summit. A recent survey (1999) using Global Positioning System technology has been made, allowing the height of the Matterhorn to be measured to within one centimetre accuracy, and its changes to be tracked. The result was 4,477.54 metres (14,690 ft).
Geography
The Matterhorn has a pyramidal shape with four faces facing the four compass points: the north and east faces overlook, respectively, the Zmutt valley and Gornergrat ridge in Switzerland, the south face (the only one south of the Swiss-Italian border) fronts the resort town of Breuil-Cervinia, and the west face looks towards the mountain of Dent d'Hérens which straddles the border. The north and south faces meet at the summit to form a short east-west ridge.
The Matterhorn's faces are steep, and only small patches of snow and ice cling to them; regular avalanches send the snow down to accumulate on the glaciers at the base of each face, the largest of which is the Zmutt Glacier to the west. The Hörnli ridge of the northeast (the central ridge in the view from Zermatt) is the usual climbing route.
Well-known faces are the east and north, visible from Zermatt.
The east face is 1,000 metres high and, because it is "a long, monotonous slope of rotten rocks", presents a high risk of rockfall, making its ascent dangerous. The north face is 1,200 metres high and is one of the most dangerous north faces in the Alps, in particular for its risk of rockfall and storms. The south face is 1,350 metres high and offers many different routes. The west face, the highest at 1,400 metres, has the fewest ascent routes.
The four main ridges separating the four faces are the main climbing routes. The least difficult technical climb, the Hörnli ridge (Hörnligrat), lies between the east and north faces, facing the town of Zermatt. To its west lies the Zmutt ridge (Zmuttgrat), between the north and west faces; this is, according to Collomb, "the classic route up the mountain, its longest ridge, also the most disjointed." The Lion ridge (Cresta del Leone), lying between the south and west faces is the Italian normal route and goes across Pic Tyndall; Collomb comments, "A superb rock ridge, the shortest on the mountain, now draped with many fixed ropes, but a far superior climb compared with the Hörnli." Finally the south side is separated from the east side by the Furggen ridge (Furggengrat), according to Collomb "the hardest of the ridges [...] the ridge still has an awesome reputation but is not too difficult in good conditions by the indirect finish".
The border between Italy and Switzerland is the main Alpine watershed, separating the drainage basin on the Rhone on the north (Mediterranean Sea) and the Po River on the south (Adriatic Sea). The Theodul Pass, located between the Matterhorn and Klein Matterhorn, at 3,300 metres, is the lowest passage between the Valtournenche and the Mattertal.
The pass was used as a crossover and trade route for the Romans and the Romanised Celts between 100 BC and 400 AC.
While the Matterhorn is the culminating point of the Valtournenche on the south, it is only one of the many 4000 metres summits of the Mattertal valley on the north, among which the Weisshorn (4505 m), Dom (4545 m), Lyskamm (4527 m) and the second highest in the Alps: Monte Rosa (4634 m). The whole range of mountains forming a crown of summits around Zermatt. The deeply glaciated region between the Matterhorn and Monte Rosa is listed in the Federal Inventory of Landscapes and Natural Monuments.
Geology
Apart from the base of the mountain, the Matterhorn is composed of gneiss belonging to the Dent Blanche klippe, an isolated part of the Austroalpine nappes, lying over the Penninic nappes. The Austroalpine nappes are part of the Apulian plate, a small continent which broke up from Africa before the Alpine orogeny. For this reason the Matterhorn has been popularized as an African mountain. The Austroalpine nappes are mostly common in the Eastern Alps.
The Swiss explorer and geologist Horace-Bénédict de Saussure, inspired by the view of the Matterhorn, anticipated the modern theories of geology:
What power must have been required to shatter and to sweep away the missing parts of this pyramid; for we do not see it surrounded by heaps of fragments; one only sees other peaks - themselves rooted to the ground - whose sides, equally rent, indicate an immense mass of débris, of which we do not see any trace in the neighbourhood. Doubtless this is that débris which, in the form of pebbles, boulders, and sand, fills our valleys and our plains.
The Matterhorn is an isolated mountain. Because of its position on the main Alpine watershed and its great height, the Matterhorn is exposed to rapid weather changes. In addition the steep faces of the mountain and its isolated location make it prone to banner clouds formation with the air flowing around and creating vortices, conducting condensation of the air on the lee side.
The Matterhorn has two distinct summits, both situated on a 100-metre-long rocky ridge: the Swiss summit (4,477.5 m) on the east and the Italian summit (4,476.4 m) on the west. Their names originated from the first ascents, not for geographic reasons, as they are both located on the border. In August 1792, the Genevan geologist and explorer Horace Bénédict de Saussure made the first measurement of the Matterhorn's height, using a 50-foot-long chain spread out on the Theodul glacier and a sextant. He calculated a height of 4,501.7 metres. In 1868 the Italian engineer Felice Giordano measured a height of 4,505 metres by means of a mercurial barometer, which he had taken up to the summit. The Dufour map, which was afterwards followed by the Italian surveyors, gave 4,482 metres, or 14,704 feet, as the height of the Swiss summit. A recent survey (1999) using Global Positioning System technology has been made, allowing the height of the Matterhorn to be measured to within one centimetre accuracy, and its changes to be tracked. The result was 4,477.54 metres (14,690 ft).
Geography
The Matterhorn has a pyramidal shape with four faces facing the four compass points: the north and east faces overlook, respectively, the Zmutt valley and Gornergrat ridge in Switzerland, the south face (the only one south of the Swiss-Italian border) fronts the resort town of Breuil-Cervinia, and the west face looks towards the mountain of Dent d'Hérens which straddles the border. The north and south faces meet at the summit to form a short east-west ridge.
The Matterhorn's faces are steep, and only small patches of snow and ice cling to them; regular avalanches send the snow down to accumulate on the glaciers at the base of each face, the largest of which is the Zmutt Glacier to the west. The Hörnli ridge of the northeast (the central ridge in the view from Zermatt) is the usual climbing route.
Well-known faces are the east and north, visible from Zermatt.
The east face is 1,000 metres high and, because it is "a long, monotonous slope of rotten rocks", presents a high risk of rockfall, making its ascent dangerous. The north face is 1,200 metres high and is one of the most dangerous north faces in the Alps, in particular for its risk of rockfall and storms. The south face is 1,350 metres high and offers many different routes. The west face, the highest at 1,400 metres, has the fewest ascent routes.
The four main ridges separating the four faces are the main climbing routes. The least difficult technical climb, the Hörnli ridge (Hörnligrat), lies between the east and north faces, facing the town of Zermatt. To its west lies the Zmutt ridge (Zmuttgrat), between the north and west faces; this is, according to Collomb, "the classic route up the mountain, its longest ridge, also the most disjointed." The Lion ridge (Cresta del Leone), lying between the south and west faces is the Italian normal route and goes across Pic Tyndall; Collomb comments, "A superb rock ridge, the shortest on the mountain, now draped with many fixed ropes, but a far superior climb compared with the Hörnli." Finally the south side is separated from the east side by the Furggen ridge (Furggengrat), according to Collomb "the hardest of the ridges [...] the ridge still has an awesome reputation but is not too difficult in good conditions by the indirect finish".
The border between Italy and Switzerland is the main Alpine watershed, separating the drainage basin on the Rhone on the north (Mediterranean Sea) and the Po River on the south (Adriatic Sea). The Theodul Pass, located between the Matterhorn and Klein Matterhorn, at 3,300 metres, is the lowest passage between the Valtournenche and the Mattertal.
The pass was used as a crossover and trade route for the Romans and the Romanised Celts between 100 BC and 400 AC.
While the Matterhorn is the culminating point of the Valtournenche on the south, it is only one of the many 4000 metres summits of the Mattertal valley on the north, among which the Weisshorn (4505 m), Dom (4545 m), Lyskamm (4527 m) and the second highest in the Alps: Monte Rosa (4634 m). The whole range of mountains forming a crown of summits around Zermatt. The deeply glaciated region between the Matterhorn and Monte Rosa is listed in the Federal Inventory of Landscapes and Natural Monuments.
Geology
Apart from the base of the mountain, the Matterhorn is composed of gneiss belonging to the Dent Blanche klippe, an isolated part of the Austroalpine nappes, lying over the Penninic nappes. The Austroalpine nappes are part of the Apulian plate, a small continent which broke up from Africa before the Alpine orogeny. For this reason the Matterhorn has been popularized as an African mountain. The Austroalpine nappes are mostly common in the Eastern Alps.
The Swiss explorer and geologist Horace-Bénédict de Saussure, inspired by the view of the Matterhorn, anticipated the modern theories of geology:
What power must have been required to shatter and to sweep away the missing parts of this pyramid; for we do not see it surrounded by heaps of fragments; one only sees other peaks - themselves rooted to the ground - whose sides, equally rent, indicate an immense mass of débris, of which we do not see any trace in the neighbourhood. Doubtless this is that débris which, in the form of pebbles, boulders, and sand, fills our valleys and our plains.
Formation
Different layers of rock can be seen: the lower part is sedimentary rocks (yellow); the middle part is greenschists from the oceanic crust. The peak itself (above the seracs) is gneisses from the African continent.
The formation of the Matterhorn (and the whole Alpine range) started with the break-up of the Pangaea continent 200 million years ago into Laurasia (containing Europe) and Gondwana (containing Africa). While the rocks constituting the nearby Monte Rosa remained in Laurasia, the rocks constituting the Matterhorn found themselves in Gondwana, separated by the newly formed Tethys Ocean.
100 million years ago the extension of the Tethys Ocean stopped and the Apulian plate broke from Gondwana and moved toward the European continent. This resulted in the closure of the western Tethys by subduction under the Apulian plate (with the Piemont-Liguria Ocean first and Valais Ocean later). The subduction of the oceanic crust left traces still visible today at the base of the Matterhorn (accretionary prism).
The orogeny itself began after the end of the oceanic subduction when the European continental crust collided with the Apulian continent, resulting in the formation of nappes. The Matterhorn acquired its characteristic pyramidal shape in much more recent times as it was caused by natural erosion over the past million years. At the beginning of alpine orogeny, the Matterhorn was only a rounded mountain like a hill. Because its height is above the snowline, its flanks are covered by ice, resulting from the accumulation and compaction of snow. During the warmer period of summer, part of the ice melts and seeps into the bedrock. When it freezes again, it fractures pieces of rock because of its dilatation (freeze-thaw), forming a cirque. Four cirques led to the shape of the mountain. Because of its recognizable shape, many other similar mountains around the world were named or nicknamed the 'Matterhorn' of their respective countries or mountain ranges.
Rocks
Most of the base of the mountain lies in the Tsaté nappe, a remnant of the Piedmont-Liguria oceanic crust (ophiolites) and its sedimentary rocks. Up to 3,400 metres the mountain is composed of successive layers of ophiolites and sedimentary rocks. From 3,400 metres to the top, the rocks are gneisses from the Dent Blanche nappe (Austroalpine nappes).
They are divided into the Arolla series (below 4,200 m) and the Valpelline zone (the summit). Other mountains in the region (Weisshorn, Zinalrothorn, Dent Blanche, Mont Collon) also belong to the Dent Blanche nappe.
Tourism
and trekking Since the eighteenth century the Alps have attracted more and more people and fascinated generations of explorers and climbers. The Matterhorn remained relatively little known until 1865, but the successful ascent followed by the tragic accident of the expedition led by Edward Whymper caused a rush on the mountains surrounding Zermatt.
The construction of the railway linking the village of Zermatt from the town of Visp started in 1888. The first train reached Zermatt on July 18, 1891 and the entire line was electrified in 1930. Since 1930 the village is directly connected to St. Moritz by the Glacier Express panoramic train. However there is no connection with the village of Breuil-Cervinia on the Italian side. Travellers have to hire mountain guides to cross the 3,300 metres high glaciated Theodul Pass, separating the two resorts.
The town of Zermatt remains completely free of internal combustion vehicles and can be reached by train only. (Electric vehicles are used locally).
Rail and cable-car facilities have been built to make some of the summits in the area more accessible. The Gornergrat railway, reaching a record altitude of 3,100 metres, was inaugurated in 1898. Areas served by cable car are the Unterrothorn and the Klein Matterhorn (Little Matterhorn) (3,883 m, highest transportation system in Europe). The Hörnli Hut (3,260 m), which is the start of the normal route via the Hörnli ridge, is easily accessible from Schwarzsee (2,600 m) and is also frequented by hikers. Both resorts of Zermatt and Cervinia function as ski resort all year round and are connected by skilifts over the Theodul Pass. A cable car running from Testa Grigia to Klein Matterhorn is currently planned for 2014. It will finally provide a link between the Swiss and Italian side of the Matterhorn.
The Matterhorn Museum (Zermatt) relates the general history of the region from alpinism to tourism. In the museum, which is in the form of a reconstituted mountain village, the visitors can relive the first and tragic ascent of the Matterhorn and see the objects having belonged to the protagonists.
The Tour of the Matterhorn can be effected by trekkers in about 10 days. Considered by some as one of the most beautiful treks in the Alps, it follows many ancient trails that have linked the Swiss and Italian valleys for centuries. The circuit includes alpine meadows, balcony trails, larch forests and glacial crossings. It connects six valleys embracing three different cultures: the German speaking high Valais, the French speaking central Valais and the Italian speaking Val d'Aosta. Good conditions are necessary to circumnavigate the peak. After reaching Zinal by the Augstbord and Meiden passes, the trekker crosses the Torrent before arriving at Arolla. Then the Col Collon must be crossed on the road to Prarayer and another one to Breuil-Cervinia and back to Zermatt via the Theodul. In total, seven passes between 2,800 and 3,300 metres must be crossed on a relatively difficult terrain.
Climbing history
The Matterhorn was one of the last of the main Alpine mountains to be ascended, not because of its technical difficulty, but because of the fear it inspired in early mountaineers. The first serious attempts began around 1857, mostly from the Italian side; but despite appearances, the southern routes are harder, and parties repeatedly found themselves having to turn back. However, on July 14, 1865, in what is considered the last ascent of the golden age of alpinism, the English party of Edward Whymper, Charles Hudson, Lord Francis Douglas, Douglas Robert Hadow, Michel Croz and the two Peter Taugwalders (father and son) were able to reach the summit by
an ascent of the Hörnli ridge in Switzerland. Upon descent, Hadow, Croz, Hudson and Douglas fell to their deaths on the Matterhorn Glacier, and all but Douglas (whose body was never found) are buried in the Zermatt churchyard.
Only three days after Whymper's ascent, the mountain was ascended from the Italian side via an indirect route by Jean-Antoine Carrel and Jean-Baptiste Bich on July 17, 1865.
Different layers of rock can be seen: the lower part is sedimentary rocks (yellow); the middle part is greenschists from the oceanic crust. The peak itself (above the seracs) is gneisses from the African continent.
The formation of the Matterhorn (and the whole Alpine range) started with the break-up of the Pangaea continent 200 million years ago into Laurasia (containing Europe) and Gondwana (containing Africa). While the rocks constituting the nearby Monte Rosa remained in Laurasia, the rocks constituting the Matterhorn found themselves in Gondwana, separated by the newly formed Tethys Ocean.
100 million years ago the extension of the Tethys Ocean stopped and the Apulian plate broke from Gondwana and moved toward the European continent. This resulted in the closure of the western Tethys by subduction under the Apulian plate (with the Piemont-Liguria Ocean first and Valais Ocean later). The subduction of the oceanic crust left traces still visible today at the base of the Matterhorn (accretionary prism).
The orogeny itself began after the end of the oceanic subduction when the European continental crust collided with the Apulian continent, resulting in the formation of nappes. The Matterhorn acquired its characteristic pyramidal shape in much more recent times as it was caused by natural erosion over the past million years. At the beginning of alpine orogeny, the Matterhorn was only a rounded mountain like a hill. Because its height is above the snowline, its flanks are covered by ice, resulting from the accumulation and compaction of snow. During the warmer period of summer, part of the ice melts and seeps into the bedrock. When it freezes again, it fractures pieces of rock because of its dilatation (freeze-thaw), forming a cirque. Four cirques led to the shape of the mountain. Because of its recognizable shape, many other similar mountains around the world were named or nicknamed the 'Matterhorn' of their respective countries or mountain ranges.
Rocks
Most of the base of the mountain lies in the Tsaté nappe, a remnant of the Piedmont-Liguria oceanic crust (ophiolites) and its sedimentary rocks. Up to 3,400 metres the mountain is composed of successive layers of ophiolites and sedimentary rocks. From 3,400 metres to the top, the rocks are gneisses from the Dent Blanche nappe (Austroalpine nappes).
They are divided into the Arolla series (below 4,200 m) and the Valpelline zone (the summit). Other mountains in the region (Weisshorn, Zinalrothorn, Dent Blanche, Mont Collon) also belong to the Dent Blanche nappe.
Tourism
and trekking Since the eighteenth century the Alps have attracted more and more people and fascinated generations of explorers and climbers. The Matterhorn remained relatively little known until 1865, but the successful ascent followed by the tragic accident of the expedition led by Edward Whymper caused a rush on the mountains surrounding Zermatt.
The construction of the railway linking the village of Zermatt from the town of Visp started in 1888. The first train reached Zermatt on July 18, 1891 and the entire line was electrified in 1930. Since 1930 the village is directly connected to St. Moritz by the Glacier Express panoramic train. However there is no connection with the village of Breuil-Cervinia on the Italian side. Travellers have to hire mountain guides to cross the 3,300 metres high glaciated Theodul Pass, separating the two resorts.
The town of Zermatt remains completely free of internal combustion vehicles and can be reached by train only. (Electric vehicles are used locally).
Rail and cable-car facilities have been built to make some of the summits in the area more accessible. The Gornergrat railway, reaching a record altitude of 3,100 metres, was inaugurated in 1898. Areas served by cable car are the Unterrothorn and the Klein Matterhorn (Little Matterhorn) (3,883 m, highest transportation system in Europe). The Hörnli Hut (3,260 m), which is the start of the normal route via the Hörnli ridge, is easily accessible from Schwarzsee (2,600 m) and is also frequented by hikers. Both resorts of Zermatt and Cervinia function as ski resort all year round and are connected by skilifts over the Theodul Pass. A cable car running from Testa Grigia to Klein Matterhorn is currently planned for 2014. It will finally provide a link between the Swiss and Italian side of the Matterhorn.
The Matterhorn Museum (Zermatt) relates the general history of the region from alpinism to tourism. In the museum, which is in the form of a reconstituted mountain village, the visitors can relive the first and tragic ascent of the Matterhorn and see the objects having belonged to the protagonists.
The Tour of the Matterhorn can be effected by trekkers in about 10 days. Considered by some as one of the most beautiful treks in the Alps, it follows many ancient trails that have linked the Swiss and Italian valleys for centuries. The circuit includes alpine meadows, balcony trails, larch forests and glacial crossings. It connects six valleys embracing three different cultures: the German speaking high Valais, the French speaking central Valais and the Italian speaking Val d'Aosta. Good conditions are necessary to circumnavigate the peak. After reaching Zinal by the Augstbord and Meiden passes, the trekker crosses the Torrent before arriving at Arolla. Then the Col Collon must be crossed on the road to Prarayer and another one to Breuil-Cervinia and back to Zermatt via the Theodul. In total, seven passes between 2,800 and 3,300 metres must be crossed on a relatively difficult terrain.
Climbing history
The Matterhorn was one of the last of the main Alpine mountains to be ascended, not because of its technical difficulty, but because of the fear it inspired in early mountaineers. The first serious attempts began around 1857, mostly from the Italian side; but despite appearances, the southern routes are harder, and parties repeatedly found themselves having to turn back. However, on July 14, 1865, in what is considered the last ascent of the golden age of alpinism, the English party of Edward Whymper, Charles Hudson, Lord Francis Douglas, Douglas Robert Hadow, Michel Croz and the two Peter Taugwalders (father and son) were able to reach the summit by
an ascent of the Hörnli ridge in Switzerland. Upon descent, Hadow, Croz, Hudson and Douglas fell to their deaths on the Matterhorn Glacier, and all but Douglas (whose body was never found) are buried in the Zermatt churchyard.
Only three days after Whymper's ascent, the mountain was ascended from the Italian side via an indirect route by Jean-Antoine Carrel and Jean-Baptiste Bich on July 17, 1865.
History
Aegidius Tschudi, one of the earliest Alpine topographers and historians, was the first to mention the region around the Matterhorn in his work, De Prisca ac Vera Alpina Raethi, published in Basel in 1538. He approached the Matterhorn as a student when in his Alpine travels he reached the summit of the Theodul Pass but he does not seem to have paid any particular attention to the mountain itself.
The Matterhorn remained unstudied for more than two centuries, until a geologist from Geneva, Horace Benedict de Saussure, travelled to the mountain, which filled him with admiration. However de Saussure was not moved to climb the mountain, and had no hope of measuring its altitude by taking a barometer to its summit. "Its precipitous sides," he wrote, "which give no hold to the very snows, are such as to afford no means of access." Yet his scientific interest was kindled by "the proud peak which rises to so vast an altitude, like a triangular obelisk, that seems to be carved by a chisel." His mind intuitively grasped the causes which gave the peak its present precipitous form: the Matterhorn was not like a perfected crystal; the centuries had laboured to destroy a great part of an ancient and much larger mountain. On his first journey de Saussure had come from Ayas to the Col des Cimes Blanches, from where the Matterhorn first comes into view; descending to Breuil, he ascended to the Theodul Pass. On his second journey, in 1792, he came to the Valtournanche, studying and describing it; he ascended to the Theodul Pass, where he spent three days, analysing the structure of the Matterhorn, whose height he was the first to measure, and collecting stones, plants and insects. He made careful observations, from the sparse lichen that clung to the rocks to the tiny but vigorous glacier fly that fluttered over the snows and whose existence at such heights was mysterious. At night he took refuge under the tent erected near the ruins of an old fort at the top of the pass. During these days he climbed the Klein Matterhorn (3,883 metres), which he named the Cime Brune du Breithorn.
The first inquirers began to come to the Matterhorn.
There is a record of a party of Englishmen who in the summer of 1800 crossed the Great St. Bernard Pass, a few months after the passage of Bonaparte; they came to Aosta and thence to Valtournanche, slept at the chalets of Breuil, and traversed the Theodul Pass, which they called Monte Rosa. The Matterhorn was to them an object of the most intense and continuous admiration.
The Matterhorn is mentioned in a guide-book to Switzerland by Johann Gottfried Ebel, which was published in Zürich towards the end of the eighteenth century, and translated in English in 1818. The mountain appeared in it under the three names of Silvius, Matterhorn, and Mont Cervin, and was briefly described as one of the most splendid and wonderful obelisks in the Alps. On Zermatt there was a note: "A place which may, perhaps, interest the tourist is the valley of Praborgne (Zermatt); it is bounded by huge glaciers which come right down into the valley; the village of Praborgne is fairly high, and stands at a great height above the glaciers; its climate is almost as warm as that of Italy, and plants belonging to hot countries are to be found there at considerable altitudes, above the ice."
Aegidius Tschudi, one of the earliest Alpine topographers and historians, was the first to mention the region around the Matterhorn in his work, De Prisca ac Vera Alpina Raethi, published in Basel in 1538. He approached the Matterhorn as a student when in his Alpine travels he reached the summit of the Theodul Pass but he does not seem to have paid any particular attention to the mountain itself.
The Matterhorn remained unstudied for more than two centuries, until a geologist from Geneva, Horace Benedict de Saussure, travelled to the mountain, which filled him with admiration. However de Saussure was not moved to climb the mountain, and had no hope of measuring its altitude by taking a barometer to its summit. "Its precipitous sides," he wrote, "which give no hold to the very snows, are such as to afford no means of access." Yet his scientific interest was kindled by "the proud peak which rises to so vast an altitude, like a triangular obelisk, that seems to be carved by a chisel." His mind intuitively grasped the causes which gave the peak its present precipitous form: the Matterhorn was not like a perfected crystal; the centuries had laboured to destroy a great part of an ancient and much larger mountain. On his first journey de Saussure had come from Ayas to the Col des Cimes Blanches, from where the Matterhorn first comes into view; descending to Breuil, he ascended to the Theodul Pass. On his second journey, in 1792, he came to the Valtournanche, studying and describing it; he ascended to the Theodul Pass, where he spent three days, analysing the structure of the Matterhorn, whose height he was the first to measure, and collecting stones, plants and insects. He made careful observations, from the sparse lichen that clung to the rocks to the tiny but vigorous glacier fly that fluttered over the snows and whose existence at such heights was mysterious. At night he took refuge under the tent erected near the ruins of an old fort at the top of the pass. During these days he climbed the Klein Matterhorn (3,883 metres), which he named the Cime Brune du Breithorn.
The first inquirers began to come to the Matterhorn.
There is a record of a party of Englishmen who in the summer of 1800 crossed the Great St. Bernard Pass, a few months after the passage of Bonaparte; they came to Aosta and thence to Valtournanche, slept at the chalets of Breuil, and traversed the Theodul Pass, which they called Monte Rosa. The Matterhorn was to them an object of the most intense and continuous admiration.
The Matterhorn is mentioned in a guide-book to Switzerland by Johann Gottfried Ebel, which was published in Zürich towards the end of the eighteenth century, and translated in English in 1818. The mountain appeared in it under the three names of Silvius, Matterhorn, and Mont Cervin, and was briefly described as one of the most splendid and wonderful obelisks in the Alps. On Zermatt there was a note: "A place which may, perhaps, interest the tourist is the valley of Praborgne (Zermatt); it is bounded by huge glaciers which come right down into the valley; the village of Praborgne is fairly high, and stands at a great height above the glaciers; its climate is almost as warm as that of Italy, and plants belonging to hot countries are to be found there at considerable altitudes, above the ice."
William Brockedon, who came to the region in 1825, considered the crossing of the Theodul Pass from Breuil to Zermatt a difficult undertaking. He gave however, expression to his enthusiasm on the summit. When he arrived exhausted on the top of the pass, he gazed "on the beautiful pyramid of the Cervin, more wonderful than aught else in sight, rising from its bed of ice to a height of 5,000 feet, a spectacle of indescribable grandeur." In this "immense natural amphitheatre, enclosed from time immemorial by snow- clad mountains and glaciers ever white, in the presence of these grand walls the mind is overwhelmed, not indeed that it is unable to contemplate the scene, but it staggers under the immensity of those objects which it contemplates." Those who made their way up through the Valtournanche to the foot of the mountain were few in number. W. A. B. Coolidge, a diligent collector of old and new stories of the Alps, mentions that during those years, besides Brockedon, only Hirzel-Escher of Zürich, who crossed the Theodul Pass in 1822, starting from Breuil, accompanied by a local guide. The greater number came from the Valais up the Visp valley to Zermatt. In 1813, a Frenchman, Henri Maynard, climbed to the Theodul Pass and made the first ascent of the Breithorn; he was accompanied by numerous guides, among them J. M. Couttet of Chamonix, the same man who had gone with de Saussure to the top of the Klein Matterhorn in 1792. The writings of these pioneers make much mention of the Matterhorn; the bare and inert rock is gradually quickened into life by men's enthusiasm. "Stronger minds," remarked Edward Whymper, "felt the influence of the wonderful form, and men who ordinarily spoke or wrote like rational beings, when they came under its power seemed to quit their senses, and ranted and rhapsodised, losing for a time all common forms of speech."
Among the poets of the Matterhorn during these years (1834 to 1840) were Elie de Beaumont, a famous French geologist; Pierre Jean Édouard Desor, a naturalist of Neuchatel, who went up there with a party of friends, two of whom were Louis Agassiz and Bernhard Studer. Christian Moritz Engelhardt, who was so filled with admiration for Zermatt and its neighbourhood that he returned there at least ten times (from 1835 to 1855), described these places in two valuable volumes, drew panoramas and maps, and collected the most minute notes on the mineralogy and botany of the region. Zermatt was at that time a quiet little village, and travellers found hospitality at the parish priest's, or at the village doctor's.
In 1841 James David Forbes, professor of natural philosophy at the University of Edinburgh, came to see the Matterhorn. A philosopher and geologist, and an observant traveller, he continued the work of De Saussure in his journeys and his writings. He was full of admiration for the Matterhorn, calling it the most wonderful peak in the Alps, unsealed and unscalable. These words, pronounced by a man noted among all his contemporaries for his thorough knowledge of mountains, show what men's feelings then were towards the Matterhorn, and how at a time when the idea of Alpine exploration was gaining ground in their minds, the Matterhorn stood by itself as a mountain apart, of whose conquest it was vain even to dream. And such it remained till long after this; as such it was described by John Ball twenty years later in his celebrated guide-book. Forbes ascended the Theodul Pass in 1842, climbed the Breithorn, and came down to Breuil; as he descended from the savage scenery of the Matterhorn, the Italian landscapes of the Valtournanche seemed to him like paradise.
Meanwhile Gottlieb Samuel Studer, the geographer, together with Melchior Ulrich, was describing and mapping the topographical features of the Zermatt peaks.
Among the poets of the Matterhorn during these years (1834 to 1840) were Elie de Beaumont, a famous French geologist; Pierre Jean Édouard Desor, a naturalist of Neuchatel, who went up there with a party of friends, two of whom were Louis Agassiz and Bernhard Studer. Christian Moritz Engelhardt, who was so filled with admiration for Zermatt and its neighbourhood that he returned there at least ten times (from 1835 to 1855), described these places in two valuable volumes, drew panoramas and maps, and collected the most minute notes on the mineralogy and botany of the region. Zermatt was at that time a quiet little village, and travellers found hospitality at the parish priest's, or at the village doctor's.
In 1841 James David Forbes, professor of natural philosophy at the University of Edinburgh, came to see the Matterhorn. A philosopher and geologist, and an observant traveller, he continued the work of De Saussure in his journeys and his writings. He was full of admiration for the Matterhorn, calling it the most wonderful peak in the Alps, unsealed and unscalable. These words, pronounced by a man noted among all his contemporaries for his thorough knowledge of mountains, show what men's feelings then were towards the Matterhorn, and how at a time when the idea of Alpine exploration was gaining ground in their minds, the Matterhorn stood by itself as a mountain apart, of whose conquest it was vain even to dream. And such it remained till long after this; as such it was described by John Ball twenty years later in his celebrated guide-book. Forbes ascended the Theodul Pass in 1842, climbed the Breithorn, and came down to Breuil; as he descended from the savage scenery of the Matterhorn, the Italian landscapes of the Valtournanche seemed to him like paradise.
Meanwhile Gottlieb Samuel Studer, the geographer, together with Melchior Ulrich, was describing and mapping the topographical features of the Zermatt peaks.
Rodolphe Töpffer, who first accompanied and guided youth to the Alps for purposes of education and amusement, began his journeys in 1832, but it is only in 1840 that he mentions the Matterhorn. Two years later Töpffer and his pupils came to Zermatt. He has described this journey of his in a chapter entitled Voyage autour du Mont Blanc jusqu'à Zermatt, here he sings a hymn of praise to the Matterhorn, comparing its form with a "huge crystal of a hundred facets, flashing varied hues, that softly reflects the light, unshaded, from the uttermost depths of the heavens". Töpffer's book was illustrated by Alexandre Calame, his master and friend, with drawings of the Matterhorn, executed in the romantic style of the period. It is an artificial mountain, a picture corresponding rather with the exaggerated effect it produces on the astonished mind of the artist, than with the real form of the mountain.
About this time there came a man who studied the Matterhorn in its structure and form, and who sketched it and described it in all its parts with the curiosity of the artist and the insight of the scientist. This was John Ruskin, a new and original type of philosopher and geologist, painter and poet, whom England was enabled to create during that period of radical intellectual reforms, which led the way for the highest development of her civilisation. Ruskin was the Matterhorn's poet par excellence. He went to Zermatt in 1844, and it is to be noticed as a curious fact, that the first time he saw the Matterhorn it did not please him. The mountain on its lofty pedestal in the very heart of the Alps was, perhaps, too far removed from the ideal he had formed of the mountains; but he returned, studied and dreamt for long at its feet, and at length he pronounced it "the most noble cliff in Europe." Ruskin was no mountaineer, nor a great friend to mountaineering; he drew sketches of the mountains merely as an illustration of his teaching of the beauty of natural forms, which was the object of his whole life. In his work on Modern Painters he makes continual use of the mountains as an example of beauty and an incentive to morality. The publication of Ruskin's work certainly produced a great impression at the time on educated people in England, and a wide spread desire to see the mountains.
It is a fragment of some size; a group of broken walls, one of them overhanging; crowned with a cornice, nodding some hundred and fifty feet over its massive flank, three thousand above its glacier base, and fourteen thousand above the sea, — a wall truly of some majesty, at once the most precipitous and the strongest mass in the whole chain of the Alps, the Mont Cervin.
Other men of high attainments followed, but in the years 1850 scientists and artists were about to be successed by real climbers and the passes and peaks around Zermatt were explored little by little. In the preface to the first volume of the Alpine Journal, which appeared in 1863, the editor, Mr. H. B. George, after remarking that nearly all the highest peaks in the Alps had by then been conquered, wrote the following words, which sounded an appeal to English climbers : " While even if all other objects of interest in Switzerland should be exhausted, the Matterhorn remains (who shall say for how long?) unconquered and apparently invincible."
About this time there came a man who studied the Matterhorn in its structure and form, and who sketched it and described it in all its parts with the curiosity of the artist and the insight of the scientist. This was John Ruskin, a new and original type of philosopher and geologist, painter and poet, whom England was enabled to create during that period of radical intellectual reforms, which led the way for the highest development of her civilisation. Ruskin was the Matterhorn's poet par excellence. He went to Zermatt in 1844, and it is to be noticed as a curious fact, that the first time he saw the Matterhorn it did not please him. The mountain on its lofty pedestal in the very heart of the Alps was, perhaps, too far removed from the ideal he had formed of the mountains; but he returned, studied and dreamt for long at its feet, and at length he pronounced it "the most noble cliff in Europe." Ruskin was no mountaineer, nor a great friend to mountaineering; he drew sketches of the mountains merely as an illustration of his teaching of the beauty of natural forms, which was the object of his whole life. In his work on Modern Painters he makes continual use of the mountains as an example of beauty and an incentive to morality. The publication of Ruskin's work certainly produced a great impression at the time on educated people in England, and a wide spread desire to see the mountains.
It is a fragment of some size; a group of broken walls, one of them overhanging; crowned with a cornice, nodding some hundred and fifty feet over its massive flank, three thousand above its glacier base, and fourteen thousand above the sea, — a wall truly of some majesty, at once the most precipitous and the strongest mass in the whole chain of the Alps, the Mont Cervin.
Other men of high attainments followed, but in the years 1850 scientists and artists were about to be successed by real climbers and the passes and peaks around Zermatt were explored little by little. In the preface to the first volume of the Alpine Journal, which appeared in 1863, the editor, Mr. H. B. George, after remarking that nearly all the highest peaks in the Alps had by then been conquered, wrote the following words, which sounded an appeal to English climbers : " While even if all other objects of interest in Switzerland should be exhausted, the Matterhorn remains (who shall say for how long?) unconquered and apparently invincible."
The traditional inaccessibility of the Matterhorn was vanquished after an expedition led by Whymper successfully reached the summit in 1865. But it ended dramatically with four men perishing on the descent. The news of the catastrophe gave rise to a universal cry of horror. Of all Alpine disasters, not one, not even of those which had a larger number of victims, ever moved men's minds as this one did. The whole of Europe talked of it; the English papers discussed it with bitter words of blame; Italian papers invented a tale of a rock detaching itself from the summit, and sweeping the helpless victims to destruction, or of a hidden crevasse opening wide its terrible jaws to swallow them. A German newspaper published an article in which Whymper was accused of cutting the rope between Douglas and Taugwalder, at the critical moment, to save his own life.
In 1890 the Federal Government was asked simultaneously by the same contractor for a concession for the Zermatt-Gornergrat railway, and for a Zermatt-Matterhorn one. The Gornergrat railway was constructed, and has been working since 1899, but there has been no more talk of the other. The project essentially consisted of a line which went up to the Hörnli, and continued thence in a rectilinear tunnel about two kilometres long, built under the ridge, and issuing near the summit on the Zmutt side. Sixty years later in 1950, Italian engineer Count Dino Lora Totino planned a cable car on the Italian side from Breuil-Cervinia to the summit. But the Alpine Museum of Zermatt sent a protest letter with 90'000 signatures to the Italian government. The latter declared the Matterhorn a natural wonder worthy of protection and refused the concession to the engineer.
During the 20th century, the Matterhorn and the story of the first ascent in particular, inspired various artists and film producers such as Luis Trenker and Walt Disney.
Designed in 1908 by Emil Cardinaux, a leading poster artist of the time, the Matterhorn affiche for the Zermatt tourist office is often considered the first modern poster. It has been described as a striking example of marriage of tourism, patriotism and popular art. It served as decoration in many Swiss military hospices during the war in addition to be found in countless middle class living rooms. Since then, the Matterhorn has become a reference that still inspires graphic artists today and has been used extensively for all sort of publicity and advertising.
In 1890 the Federal Government was asked simultaneously by the same contractor for a concession for the Zermatt-Gornergrat railway, and for a Zermatt-Matterhorn one. The Gornergrat railway was constructed, and has been working since 1899, but there has been no more talk of the other. The project essentially consisted of a line which went up to the Hörnli, and continued thence in a rectilinear tunnel about two kilometres long, built under the ridge, and issuing near the summit on the Zmutt side. Sixty years later in 1950, Italian engineer Count Dino Lora Totino planned a cable car on the Italian side from Breuil-Cervinia to the summit. But the Alpine Museum of Zermatt sent a protest letter with 90'000 signatures to the Italian government. The latter declared the Matterhorn a natural wonder worthy of protection and refused the concession to the engineer.
During the 20th century, the Matterhorn and the story of the first ascent in particular, inspired various artists and film producers such as Luis Trenker and Walt Disney.
Designed in 1908 by Emil Cardinaux, a leading poster artist of the time, the Matterhorn affiche for the Zermatt tourist office is often considered the first modern poster. It has been described as a striking example of marriage of tourism, patriotism and popular art. It served as decoration in many Swiss military hospices during the war in addition to be found in countless middle class living rooms. Since then, the Matterhorn has become a reference that still inspires graphic artists today and has been used extensively for all sort of publicity and advertising.