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Col De Tende
Col de Tende ( it, Colle di Tenda; elevation 1870 m) is a high mountain pass in the Alps, close to the border between France and Italy, although the highest section of the pass is wholly within France. It separates the Maritime Alps from the Ligurian Alps. It connects Nice and Tende in Alpes-Maritimes with Cuneo in Piedmont. A railway tunnel inaugurated in 1898 and a Road Tunnel inaugurated in 1882 run under the pass. The latter tunnel is 3.2 kilometre long and is among the oldest long road tunnels. French historian François Guizot states that the road was first developed by Phoenicians and later maintained by Greeks and Romans.''A Popular History of France From The Earliest Times'', Volume I. See also * List of highest paved roads in Europe * List of mountain passes * France–Italy border * Main chain of the Alps The main chain of the Alps, also called the Alpine divide is the central line of mountains that forms the drainage divide of the range. Main chains of mount ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alpes-Maritimes
Alpes-Maritimes (; oc, Aups Maritims; it, Alpi Marittime, "Maritime Alps") is a department of France located in the country's southeast corner, on the Italian border and Mediterranean coast. Part of the Provence-Alpes-Côte d'Azur region, it encompasses the French Riviera alongside neighbouring Var. Alpes-Maritimes had a population of 1,094,283 in 2019.Populations légales 2019: 06 Alpes-Maritimes INSEE Its (and largest city) is Nice, with Grasse as the sole [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
François Guizot
François Pierre Guillaume Guizot (; 4 October 1787 – 12 September 1874) was a French historian, orator, and statesman. Guizot was a dominant figure in French politics prior to the Revolution of 1848. A conservative liberal who opposed the attempt by King Charles X to usurp legislative power, he worked to sustain a constitutional monarchy following the July Revolution of 1830. He then served the "citizen king" Louis Philippe, as Minister of Education, 1832–37, ambassador to London, Foreign Minister 1840–1847, and finally Prime Minister of France from 19 September 1847 to 23 February 1848. Guizot's influence was critical in expanding public education, which under his ministry saw the creation of primary schools in every French commune. As a leader of the "Doctrinaires", committed to supporting the policies of Louis Phillipe and limitations on further expansion of the political franchise, he earned the hatred of more left-leaning liberals and republicans through his uns ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Passes Of Piedmont
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Passes Of Provence-Alpes-Côte D'Azur
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Alpes-Maritimes
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Passes Of The Alps
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Passes Of The Ligurian Alps
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Main Chain Of The Alps
The main chain of the Alps, also called the Alpine divide is the central line of mountains that forms the drainage divide of the range. Main chains of mountain ranges are traditionally designated in this way, and generally include the highest peaks of a range. The Alps are something of an unusual case in that several significant groups of mountains are separated from the main chain by sizable distances. Among these groups are the Dauphine Alps, the Eastern and Western Graians, the entire Bernese Alps, the Tödi, Albula and Silvretta groups, the Ortler and Adamello ranges, and the Dolomites of South Tyrol, as well as the lower Alps of Vorarlberg, Bavaria, and Salzburg. Main features The Alpine Divide is defined for much of its distance by the watershed between the drainage basin of the Po in Italy on one side, with the other side of the divide being formed by the Rhone, the Rhine and the Danube. Further east, the watershed is between the Adige and the Danube, before headin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
France–Italy Border
The France–Italy border is 515 km (320 mi) long. It runs from the Alps in the north, a region in which it passes over Mont Blanc, down to the Mediterranean coast in the south. Three national parks are located along the border: Vanoise National Park and Mercantour National Park on the French side and Gran Paradiso National Park on the Italian side. Features The France–Italy border is mainly mountainous. It is long, in southeast France and northwest Italy. It begins at the west tripoint of France–Italy–Switzerland () near the top of Mont Dolent ( m), in the French commune of Chamonix (department of Haute-Savoie), the Italian city of Courmayeur (Aosta Valley) and the Swiss commune of Orsières (canton of Valais). The boundary then follows a general direction towards south, to the Mediterranean, it reaches the sea at Menton in France and Ventimiglia in Italy. The border separates three regions (Aosta Valley, Piedmont and Liguria) and four provinces of Italy (Aosta, Turin, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Mountain Passes
This is a list of mountain passes. Africa Egypt * Halfaya Pass (near Libya) Lesotho * Moteng Pass * Mahlasela pass * Sani Pass Morocco * Tizi n'Tichka South Africa * Eastern Cape Passes * Western Cape Passes * Northern Cape Passes * KwaZulu Natal Passes * Free State Passes * Limpopo Province Passes * Mpumalanga Passes * Gauteng Passes * Northwest Province Passes * Swartberg Pass (Western Cape) * Lootsberg Pass Asia Afghanistan * Broghol Pass to Pakistan * Dorah Pass to Pakistan * Hajigak Pass * Khost-Gardez Pass * Khyber Pass to Pakistan * Kotal-e Khushk * Kushan Pass linking northern Afghanistan to the region. * Lataband Pass * Tang-e Gharu is a gorge which links Afghanistan with Pakistan * Salang Pass crosses the Hindu Kush linking Kabul with northern Afghanistan - nowadays through a tunnel. * Wakhjir Pass to China China * Pingxingguan Pass, Shanxi * Jiayu Pass, Beijing * Jianmen Pass, Sichuan * Niangzi Pass, Border between Shanxi and Hebei * ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Highest Paved Roads In Europe
This is a list of the highest paved roads in Europe. It includes roads that are over long and whose culminating point is at least above sea level. This height approximately corresponds to that of the highest settlements in Europe and to the tree line in several mountain ranges such as the Alps and the Pyrenees, where most of the highest roads are located. Some of the listed roads are closed to motorized vehicles, although they are normally all accessible to pedestrians and cyclists. These mountain roads are visited by drivers, motorcyclists, bicyclists and hikers for their scenery and often feature in the routes of European bicycle races such as the Giro d'Italia, the Tour de Suisse, the Tour of Austria, the Tour de France and the Vuelta a España. Due to snow conditions, most of the high roads are closed between (late) autumn and late spring/early summer. Note on the elevations: Near the highest point of the road there is often a shield that indicates the name (in local l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Col De Tende Road Tunnel
Col de Tende Road Tunnel is a 3182 metre long road tunnel running under Col de Tende between France and Italy. It was inaugurated in 1882 and it was until 1964 the longest road tunnel in the Alps The Alps () ; german: Alpen ; it, Alpi ; rm, Alps ; sl, Alpe . are the highest and most extensive mountain range system that lies entirely in Europe, stretching approximately across seven Alpine countries (from west to east): France, Sw .... At its opening time it was the world's longest road tunnel. Altitude on the French side: 1,280 m; Italian side: 1,321 m. The tunnel and its access roads were damaged by Storm Alex in October 2020, closing the tunnel. , repair work is expected to be completed by the end of 2025."La France et l'Italie ont validé la création d'un viaduc côté français pour relier la route au tunnel", ''France Info''May 6, 2021/ref> (From France, , to Italy, ) References External links * Road tunnels in France Road tunnels in Italy Tunnels com ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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