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Gendarme (mountaineering)
A gendarme is a pinnacle of rock on a mountain ridge. They are typical of alpine areas. Gendarmes often form on the intersection of two ridges due to the lower erosion of glaciers here. The name originates from the French Alps, where they were seen as resembling the gendarmerie A gendarmerie () is a paramilitary or military force with law enforcement duties among the civilian population. The term ''gendarme'' () is derived from the medieval French expression ', which translates to " men-at-arms" (). In France and so ... police. References Mountains Geographical terminology in mountaineering {{geomorph-stub ...
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Krapf Rognon And Glacier After Snowstorm
Johann Ludwig Krapf (11 January 1810 – 26 November 1881) was a German missionary in East Africa, as well as an explorer, linguist, and traveler. Krapf played an important role in exploring East Africa with Johannes Rebmann. They were the first Europeans to see Mount Kenya with the help of Akamba who dwelled at its slopes and Kilimanjaro. Ludwig Krapf visited Ukambani, the homeland of the Kamba people, in 1849 and again in 1850. He successfully translated the New Testament to the Kamba language. Krapf also played a key role in exploring the East African coastline, especially in Mombasa. Early life Krapf was born into a Lutheran family of farmers in southwest Germany. From his school days onward he developed his gift for languages. He initially studied Latin, Greek, French and Italian. More languages were to follow throughout his life. After finishing school he joined the Basel Mission Seminary at age 17 but discontinued his studies as he had doubts about his missionary vocation ...
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Erosion
Erosion is the action of surface processes (such as Surface runoff, water flow or wind) that removes soil, Rock (geology), rock, or dissolved material from one location on the Earth's crust#Crust, Earth's crust and then sediment transport, transports it to another location where it is deposit (geology), deposited. Erosion is distinct from weathering which involves no movement. Removal of rock or soil as clastic sediment is referred to as ''physical'' or ''mechanical'' erosion; this contrasts with ''chemical'' erosion, where soil or rock material is removed from an area by Solvation, dissolution. Eroded sediment or solutes may be transported just a few millimetres, or for thousands of kilometres. Agents of erosion include rainfall; bedrock wear in rivers; coastal erosion by the sea and Wind wave, waves; glacier, glacial Plucking (glaciation), plucking, Abrasion (geology), abrasion, and scour; areal flooding; Aeolian processes, wind abrasion; groundwater processes; and Mass wastin ...
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Glaciers
A glacier (; or ) is a persistent body of dense ice, a form of rock, that is constantly moving downhill under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as crevasses and seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land“Glacier, N., Pronunciation.” Oxford English Dictionary, Oxford UP, June 2024, https://doi.org/10.1093/OED/7553486115. Accessed 25 Jan. 2025. and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every c ...
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French Alps
The French Alps are the portions of the Alps mountain range that stand within France, located in the Auvergne-Rhône-Alpes and Provence-Alpes-Côte d'Azur regions. While some of the ranges of the French Alps are entirely in France, others, such as the Mont Blanc massif, are shared with Switzerland and Italy. At , Mont Blanc, on the France–Italy border, is the highest mountain in the Alps, and the highest Western European mountain. Notable towns in the French Alps include Grenoble, Chamonix, Annecy, Chambéry, Évian-les-Bains and Albertville. Ranges and summits Ski areas The largest connected ski areas are: # Les Trois Vallées ( Courchevel, Méribel, La Tania, Brides-les-Bains, Saint-Martin-de-Belleville, Les Menuires, Val Thorens and Orelle): 338 slopes, 600 km of pistes. # Portes du Soleil ( Avoriaz, Châtel, Morzine, Les Gets, Saint-Jean d'Aulps, La Chapelle d'Abondance, Abondance, Montriond, Swiss resorts): 288 slopes, 650 km of sl ...
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Gendarmerie
A gendarmerie () is a paramilitary or military force with law enforcement duties among the civilian population. The term ''gendarme'' () is derived from the medieval French expression ', which translates to " men-at-arms" (). In France and some Francophone nations, the gendarmerie is a branch of the armed forces that is responsible for internal security in parts of the territory (primarily in rural areas and small towns in the case of France), with additional duties as military police for the armed forces. It was introduced to several other Western European countries during the Napoleonic conquests. In the mid-twentieth century, a number of former French mandates and colonial possessions (such as Lebanon, Syria, the Ivory Coast and the Republic of the Congo) adopted a gendarmerie after independence. Similar forces exist in most European countries. The European Gendarmerie Force is a structure, aligned with the European Union, that facilitates joint operations. A similar ...
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Mountains
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 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 climate, mountains ...
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