Misplaced Pages

#631368

48-910: The Valle Mesolcina , also known as the Val Mesolcina or Misox (German), is an alpine valley of the Grisons , Switzerland , stretching from the San Bernardino Pass to Grono where it joins the Calanca Valley . It is the valley formed by the river Moesa . Like the Val Bregaglia or the Val Poschiavo , the Valle Mesolcina is a valley lying south of the main ridge of the Alps . Although politically

96-579: A large number of established small and medium-sized businesses, many of which are in the service sector. Forests are important in the La Gruyère (Greyerz) district. Power plants in the district of Sarine export electricity. The mountain areas attract tourists all year round. The lake regions are frequented by tourists in summer and autumn. The canton of Fribourg is well connected to other areas of Switzerland with motorways A1 , A12 and fast rail links. The main railway between Geneva and Lausanne in

144-543: Is above 2000 metres. PERMOS (The Swiss Permafrost Monitoring Network) is an operational monitoring service, and its main goal is to create long-term scientific documentation of the permafrost changes in the Swiss Alps. To accurately represent the current conditions of the Alps, the network records permafrost temperatures and thermal changes in boreholes, the bottom temperature of the snow cover, ground surface temperature, and

192-585: Is decreasing as the canton subsidizes mergers between municipalities. In contrast to the mainly Protestant cantons of Vaud to its west and Bern to its east, the canton of Fribourg is a predominantly Catholic enclave (as of 2000 , 70%) with a Protestant minority (15%). This explains why the canton straddles the French-German linguistic border, for in the past, denominational considerations were more important than linguistic when drawing Switzerland's cantonal borders. The main centres of population are

240-427: Is located in western Switzerland . The canton is bilingual , with French spoken by more than two thirds of the citizens and German by a little more than a quarter. Both are official languages in the canton. The canton takes its name from its capital city of Fribourg . On the shores of Lake Neuchâtel and Lake Morat significant traces of prehistoric settlements have been unearthed. The canton of Fribourg joined

288-419: Is one of many countries that need to begin to think about the future of energy production in response to climate change. Switzerland is paving the way for a new wave of innovation and creative problem solving that the rest of the world will eventually need to follow. The following table gives the surface area above 2000 m and 3000 m and the respective percentage on the total area of each canton whose high point

336-678: Is part of the Central Eastern Alps , except the Ortler Alps which belong to the Southern Limestone Alps . The Pennine , Bernese and Bernina Range are the highest ranges of the country, they contain respectively 38, 9 and 1 summit over 4000 meters. The lowest range is the Appenzell Alps culminating at 2,500 meters. Western Alps Eastern Alps The north side of the Swiss Alps is drained by

384-464: Is situated above the tree line and is clear of trees due to low average temperatures. It contains mostly grass and small plants along with mountain flowers. Below the permafrost limit (at about 2,600 meters), the alpine meadows are often used as pastures. Some villages can still be found on the lowest altitudes such as Riederalp (1,940 m) or Juf (2,130 m). The extent of the Alpine zone is limited by

432-503: Is the first World Heritage Site in the Alps. As the temperature decreases with altitude (0.56 °C per 100 meters on yearly average), three different altitudinal zones, each having distinct climate, are found in the Swiss Alps: The Subalpine zone is the region that lies below the tree line . It is the most important region as it is the largest of the three and contains almost all human settlements as well as

480-833: The Evangelical Reformed Church of the Canton of Grisons . Swiss Alps The Swiss Alps comprise almost all the highest mountains of the Alps , such as Dufourspitze (4,634 m), the Dom (4,545 m), the Liskamm (4,527 m), the Weisshorn (4,506 m) and the Matterhorn (4,478 m). The other following major summits can be found in this list of mountains of Switzerland . Since the Middle Ages , transit across

528-808: The Helvetic zone on the north and the Austroalpine nappes – Southern Alps on the south come originally from the European and African continent respectively. The rocks of the Penninic nappes belong to the former area of the Briançonnais microcontinent and the Tethys Ocean . The closure of the latter by subduction under the African plate ( Piemont Ocean first and Valais Ocean later) preceded

SECTION 10

#1732765716632

576-857: The Matterhorn Peak in California (see the Matterhorn article for a list of Matterhorns in the world ). The confluence of the Baltoro Glacier and the Godwin-Austen Glacier south of K2 in the Karakoram range was named after the Konkordiaplatz by European explorers. 46°33′33″N 8°33′41″E  /  46.55917°N 8.56139°E  / 46.55917; 8.56139 Canton of Fribourg The canton of Fribourg , also canton of Freiburg ,

624-736: The Rhône , Rhine and Inn (which is part of the Danube basin) while the south side is mainly drained by the Ticino (Po basin). The rivers on the north empty into the Mediterranean , North and Black Sea , on the south the Po empty in the Adriatic Sea . The major triple watersheds in the Alps are located within the country, they are: Piz Lunghin , Witenwasserenstock and Monte Forcola . Between

672-598: The Swiss Alpine Club in 1863) and the opening of mountain train lines ( Rigi in 1873, Pilatus in 1889, Gornergrat in 1898). The Jungfraubahn opened in 1912; it leads to the highest railway station in Europe, the Jungfraujoch . Switzerland enjoys a 62,000-km network of well-maintained trails, of which 23,000 are located in mountainous areas. Many mountains attract a large number of alpinists from around

720-473: The Swiss Confederation in 1481. The area is made up of lands acquired by the capital Fribourg. The present extent was reached in 1803 when Murten (Morat) was acquired. The canton of Fribourg joined the separatist league of Catholic cantons in 1846 ( Sonderbund ). The following year, its troops surrendered to the federal army. The canton is bounded to the west by Lake Neuchâtel, to the west and

768-668: The Swiss Plateau , before retreating and leaving remnants only in high mountain areas. In modern times the Aletsch Glacier in the western Bernese Alps is the largest and longest in the Alps, reaching a maximum depth of 900 meters at Konkordiaplatz . Along with the Fiescher and Aar Glaciers , the region became a UNESCO World Heritage Site in 2001. An effect of the retreat of the Rhine Glacier some 10,000 years ago

816-567: The cheese of the same name. The chocolate industry is also well established in Broc , home to an international chocolate research centre. Other agricultural produces include tobacco, fruit and cereals. Agriculture is predominant in the north of the canton where the most fertile lands lie. There is light industry concentrated around the capital Fribourg. Other centres of light industry are Bulle , Villars-sur-Glâne , Düdingen (Guin), Murten (Morat) and Estavayer-le-Lac . These five centers have also

864-602: The Alps are (from west to east): France , Italy , Austria and Liechtenstein . The Alps are usually divided into two main parts, the Western Alps and Eastern Alps , whose division is along the Rhine from Lake Constance to the Splügen Pass . The western ranges occupy the greatest part of Switzerland while the more numerous eastern ranges are much smaller and are all situated in the canton of Graubünden . The latter

912-726: The Alps is a key issue at national and international levels, as the European continent is at places divided by the range. Since the beginning of industrialisation Switzerland has improved its transalpine network; it began in 1882, by building the Gotthard Rail Tunnel , followed in 1906 by the Simplon Tunnel and 1913 by the Lötschberg Tunnel , and more recently, in 2007, by the Lötschberg Base Tunnel . The 57.1-km long Gotthard Base Tunnel ,

960-563: The Alps played an important role in history. The region north of St Gotthard Pass became the nucleus of the Swiss Confederacy in the early 14th century. The Alps cover 60% of Switzerland's total 41,285 square kilometres (15,940 sq mi) surface area, making it one of the most alpine countries. Despite the fact that Switzerland covers only 14% of the Alps total 192,753 square kilometres (74,422 sq mi) area, 48 out of 82 alpine four-thousanders are located in

1008-660: The Helvetic Zone and those on the south side are part of the Penninic nappes. The Austroalpine zone concerns almost only the Eastern Alps, with the notable exception of the Matterhorn . The last glaciations greatly transformed Switzerland's landscape. Many valleys of the Swiss Alps are U-shaped due to glacial erosion. During the maximum extension of the Würm glaciation (18,000 years ago) the glaciers completely covered

SECTION 20

#1732765716632

1056-478: The Swiss Alps and practically all of the remaining 34 are within 20 kilometres (12 mi) of the country's border. The glaciers of the Swiss Alps cover an area of 1,220 square kilometres (470 sq mi) — 3% of the Swiss territory, representing 44% of the total glaciated area in the Alps i.e. 2,800 square kilometres (1,100 sq mi). The Swiss Alps are situated south of the Swiss Plateau and north of

1104-409: The Swiss Alps began with the first ascents of the main peaks of the Alps ( Jungfrau in 1811, Piz Bernina in 1850, Monte Rosa in 1855, Matterhorn in 1856, Dom in 1858, Weisshorn in 1861) mostly by British mountain climbers accompanied by the local guides. The construction of facilities for tourists started in the mid-nineteenth century with the building of hotels and mountain huts (creation of

1152-622: The Valle Mesolcina belongs to the Grisons, its population is predominantly Italian-speaking and culturally oriented towards the Ticino . The valley includes the Mesocco and Roveredo of the Moesa district , including: The majority of the population adheres to Roman Catholicism , but there is a significant Protestant presence which is part of a Reformed community. located in Grono and adhering to

1200-1002: The Witenwasserenstock and Piz Lunghin runs the European Watershed separating the basin of the Atlantic (the North Sea) and the Mediterranean Sea (Adriatic and the Black Sea). The European watershed lies only partially on the main chain . Switzerland possesses 6% of Europe's freshwater, and is sometimes referred to as the "water tower of Europe". Since the highest dams are located in Alpine regions, many large mountain lakes are artificial and are used as hydroelectric reservoirs. Some large artificial lakes can be found above 2,300 m, but natural lakes larger than 1 km are generally below 1,000 m (with

1248-419: The attractiveness of the Alpine landscape, increasing winter temperatures will result in a shorter skiing season, and these climate changes are limiting the amount of snow coverage produced. All of these climate and geographical factors are leading to a smaller number of visitors and reduced revenues which can have an intense economic impact on winter tourism. In response to these changes, Switzerland has turned to

1296-433: The canton (as of 31 December 2020) is 325,496. As of 2007 , the population included 43,838 foreign-born residents, or about 16.65% of the total population. The historical population is given in the following table: Agriculture is important in the canton of Fribourg. The main agricultural activities are cattle breeding and dairy farming . The region is a major cheese producer, especially the district of Gruyère , home of

1344-407: The canton, then joins the river Aare . The river Broye drains the west of the canton and flows northeast into Lake Morat (Murtensee). The southwest part of the canton is drained by the river Veveyse , which flows south into Lake Geneva ( French : Le Léman ). The Canton is divided into seven districts: There are 126 municipalities in the canton of Fribourg as of January 2023 . The number

1392-535: The capital Fribourg (34,300 inhabitants) and Bulle (18,200 inhabitants). Two thirds of the population speak French; the remainder speak Alemannic dialects of German. The French-speaking areas are in the west of the canton, the Alemannic-speaking areas in the east. The number of bilingual towns, and consequently the large number of people who can speak both French and German fluently, has attracted businesses such as telesales companies. The population of

1440-570: The collision between the two plates and the so-called alpine orogeny. The major thrust fault of the Tectonic Arena Sardona in the eastern Glarus Alps gives a visible illustration of mountain-building processes and was therefore declared a UNESCO World Heritage. Another fine example gives the Alpstein area with several visible upfolds of Helvetic zone material. With some exceptions, the Alps north of Rhône and Rhine are part of

1488-456: The country. Switzerland depends on the use of hydroelectricity to power nearby communities, but as glaciers melt and stop refreezing, the melting that creates the energy ceases to exist. Researchers have been evaluating how the topography will change as the glaciers begin to decrease and they are looking more deeply into potential construction costs, energy production, and future problems they might encounter with these new developments. Switzerland

Valle Mesolcina - Misplaced Pages Continue

1536-414: The development of snow cover. The network additionally takes air photos periodically from selected areas. These monitoring strategies continue to develop as new research and data are recorded over time. The glaciers in the Swiss Alps have lost around half their volume during the last 90–120 years. The composition of the great tectonic units reflects the history of the formation of the Alps. The rocks from

1584-540: The exceptions of lakes in the Engadin such as Lake Sils , and Oeschinen in the Bernese Oberland). The melting of low-altitude glaciers can generate new lakes, such as the 0.25 km large Triftsee which formed between 2002 and 2003. Switzerland has been using this concerning transition in climate as a positive opportunity to develop new innovations and to change the ways that energy is being produced in

1632-537: The first permanent snow, its altitude greatly varies depending on the location (and orientation), it comprises between 2,800 and 3,200 meters. The glacial zone is the area of permanent snow and ice. When the steepness of the slope is not too high it results in an accumulation and compaction of snow, which transforms into ice. The glacier-formed then flows down the valley and can reach as far down as 1,500 meters (the Upper Grindelwald Glacier ). Where

1680-523: The longest railway tunnel of the world, opened in 2016 and provides a direct flat rail link through the Alps. The different names of the mountains and other landforms are named in the four national languages . The table below gives the most recurrent names. Also, a large number of peaks outside the Alps were named or nicknamed after Swiss mountains, such as the Wetterhorn Peak in Colorado or

1728-1143: The majority of ski resorts in Switzerland tend to open in December and run through to April. The most visited places are: Other important destinations on the regional level are Engelberg - Titlis (Central Switzerland / OW ) and Gotthard Oberalp Arena with Andermatt (Central Switzerland / UR ) and Sedrun (GR), Leysin -Les Mosses, Villars-sur-Ollon , Les Diablerets -Glacier 3000 (all VD), Leukerbad (VS), Savognin , Scuol , Obersaxen , Breil/Brigels (all GR), Meiringen – Hasliberg (BE), Sörenberg ( LU ), Klewenalp with Beckenried and Emmetten (both NW ), Melchsee-Frutt ( OW ), Flumserberg and Pizol (both Sarganserland in SG ), Toggenburg with Wildhaus – Unterwasser – Alt St. Johann (SG), Hoch-Ybrig and Stoos (all SZ ), Braunwald and Elm ( GL ), Airolo and Bosco/Gurin ( TI ) and many more. The first person to ski in Grindelwald , Switzerland

1776-539: The mountain regions are within 1 to 3 hours travel of Switzerland's main cities and their respective airport . The Engadine in Graubünden is between 3 and 6 hours away from the large cities; the train journey itself, with the panoramic Glacier Express or Bernina Express , is popular with tourists. The Engadin Airport near St. Moritz at an altitude of 1,704 meters is the highest in Europe. The crossing of

1824-1081: The national border. The limit between the Alps and the plateau runs from Vevey on the shores of Lake Geneva to Rorschach on the shores of Lake Constance , passing close to the cities of Thun and Lucerne . The not well defined regions in Switzerland that lie on the margin of the Alps, especially those on the north side, are called the Swiss Prealps ( Préalpes in French, Voralpen in German, Prealpi in Italian). The Swiss Prealps are mainly made of limestone and they generally do not exceed 2,500 metres (8,200 ft). The Alpine cantons (from highest to lowest) are Valais , Bern , Graubünden , Uri , Glarus , Ticino , St. Gallen , Vaud , Obwalden , Nidwalden , Schwyz , Appenzell Innerrhoden , Appenzell Ausserrhoden , Fribourg , Lucerne and Zug . The countries with which Switzerland shares mountain ranges of

1872-454: The production of artificial snow to match the demand for these tourist destinations and to uphold the structure and well-being of the economy. The Swiss Alps and Switzerland enjoy an extensive transport network . Virtually every mountain village can be reached by public transport, either by rail , bus, funicular, cable car, or usually a combination of them. The main companies of the coherently integrated public transport system are: Most of

1920-612: The productive areas. The forests are mainly composed of conifers above 1,200–1,400 meters, the deciduous tree forest is confined to lower elevations. The upper limit of the Subalpine zone is located at about 1,800 meters on the north side of the Alps and about 2,000 meters on the south side. It can, however, differ in some regions such as the Appenzell Alps (1,600 meters) or the Engadin valley (2,300 meters). The Alpine zone

1968-498: The slopes are too steep, the snow accumulates to form overhanging seracs , which periodically fall off due to the downward movement of the glacier and cause ice avalanches. The Bernese Alps, Pennine Alps, and Mont Blanc Massif contain most of the glaciated areas in the Alps. Except for research stations such as the Sphinx Observatory , no settlements are to be found in those regions. Due to the change in weather patterns,

Valle Mesolcina - Misplaced Pages Continue

2016-525: The south by the canton of Vaud , and to the east by the canton of Bern . The canton includes two enclaves within Vaud and one within the canton of Bern, as well as a large exclave on the lake; it also enclaves the Bernese municipality of Münchenwiler . The area of the canton is 1,669 square kilometers (644.4 sq mi), including the small enclaves. The canton lies on the elevated Swiss Plateau . In

2064-436: The summers are expected to continue getting warmer and drier, while the winters are expected to become moister. This change in the weather increases the chances of flooding with heavier rainfall, the melting of permafrost zones, a change in the geography and wildlife, and the occurrence of more deadly rock slides. Furthermore, natural hazards are occurring more frequently, such as floods, avalanches, and landslides. Additionally,

2112-544: The water supply that the glaciers originally provided is on the decline, which is problematic for producing energy, agricultural practices, and other human use. Finally, the glacial melting puts the economy at risk because there will be less incoming financial revenue from the tourism and recreation services that these glaciers and ecosystems typically provide. All of these impacts will disrupt the nearby communities and require that updated infrastructure and safety measures be put into place to prevent mass destruction. Tourism in

2160-411: The west the lands are flat, but towards the south east of the canton, the lands rise to a hilly region. This region is commonly called pre- Alps but is part of the Bernese Alps . The highest elevation in the canton is the Vanil Noir with 2,389 m (7,838 ft). The river Saane/Sarine flows from the south to the north of the canton. Together with its tributaries it drains most of the lands in

2208-789: The world, especially the 4000-meter summits and the great north faces ( Eiger , Matterhorn and Piz Badile ). The large winter resorts are also popular destinations in summer, as most of aerial tramways operate through the year, enabling hikers and mountaineers to reach high altitudes without much effort. The Klein Matterhorn is the highest summit of the European continent to be served by cable car. The major destinations for skiing and other winter sports are located in Valais , Bernese Oberland and Graubünden . Some villages are car-free and can be accessed only with public transports such as Riederalp and Bettmeralp . Zermatt and Saas-Fee have both summer ski areas. The ski season starts from as early as November and runs to as late as May; however,

2256-460: Was Englishmen Gerald Fox (a resident of Tone Dale House in England) who put his skis on in his hotel bedroom in 1881 and walked out through the hotel Bar to the slopes wearing them. Some major sporting activities include: Climate change is impacting European Alpine tourism due to the increasing number and intensity of natural hazards, and it is endangering the accessibility and infrastructure of tourism destinations. Melting glaciers are affecting

2304-480: Was the Flims Rockslide , the biggest still visible landslide worldwide. To protect endangered species some sites have been brought under protection. The Swiss National Park in Graubünden was established in 1914 as the first alpine national park. The Entlebuch area was designated a biosphere reserve in 2001. The largest protected area in the country is the Parc Ela , opened in 2006, which covers an area of 600 square kilometres. The Jungfrau-Aletsch Protected Area

#631368