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Serre Mourene
The Serre Mourene is a Pyrenees, pyrenean summit, located on the Franco-Spanish border between the cirques of cirque de Troumouse, Troumouse and cirque de Barrosa, Barrosa, culminating at ; it is the second highest summit of the massif de la Munia after the pic de la Munia. Topography The summit is located on the pyrenean drainage divide, watershed in the central Pyrenees between the summits of Pic de la Munia, la Munia and Troumouse. See also *List of Pyrenean three-thousanders References Landforms of Hautes-Pyrénées Mountains of the Pyrenees Mountains of Hautes-Pyrénées Pyrenean three-thousanders {{HautesPyrénées-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pic De La Munia
The Pic de la Munia culminating at is the highest point of the three cirques of Troumouse, Barroude and Barrosa. It is located on the border between France ( Hautes-Pyrénées department) and Spain (Huesca province). Toponymy ''Era Munia'' could mean "nun", from « moniale », of Spanish origin.Marcellin Bérot, ''La vie des hommes de la montagne dans les Pyrénées racontée par la toponymie'', avec le concours du Centre régional des lettres de Midi-Pyrénées, 1998, Milan et parc national des Pyrénées Otherwise, it could stem from Latin, ''moenia'' meaning « walls », which corresponds to its relief. Access There are three main access routes which lead to the summit of la Munia. The first, most direct and most frequented, runs along the impressive north face, in the vast cirque de Troumouse. The starting point is located at the Troumouse car park, at about 2,100 m. The ascent is a bit technical (PD), with two delicate passages : a first small wall (III-) that one ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pyrenees
The Pyrenees (; es, Pirineos ; french: Pyrénées ; ca, Pirineu ; eu, Pirinioak ; oc, Pirenèus ; an, Pirineus) is a mountain range straddling the border of France and Spain. It extends nearly from its union with the Cantabrian Mountains to Cap de Creus on the Mediterranean Sea, Mediterranean coast. It reaches a maximum altitude of at the peak of Aneto. For the most part, the main crest forms a divide between Spain and France, with the microstate of Andorra sandwiched in between. Historically, the Crown of Aragon and the Kingdom of Navarre extended on both sides of the mountain range. Etymology In Greek mythology, Pyrene (mythology), Pyrene is a princess who eponym, gave her name to the Pyrenees. The Greek historiography, Greek historian Herodotus says Pyrene is the name of a town in Celts, Celtic Europe. According to Silius Italicus, she was the virgin daughter of Bebryx, a king in Narbonensis, Mediterranean Gaul by whom the hero Hercules was given hospitality during his ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of The Pyrenees
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 Hautes-Pyrénées
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Pyrenean Three-thousanders
This list contains all of the Pyrenean three-thousanders, namely the 129 mountain summits of or more above sea level in the Pyrenees, a range of mountains in southwest Europe that forms a natural border between France and Spain. The Pyrenees separate the Iberian Peninsula from the rest of continental Europe, and extend for about from the Bay of Biscay (Cap Higuer) to the Mediterranean Sea ( Cap de Creus). The highest mountain in the Pyrenees is Aneto in Spain at . The summits meeting the 3,000-metre criterion were defined by a UIAA-sponsored joint Franco-Spanish team led by Juan Buyse. The UIAA list, published in 1990, also contains 83 secondary summits in addition to the 129 principal ones listed here, and divides the range into 11 zones. According to the latest surveys, three of the peaks in the original list are actually below 3000m but are still included below. The selection criteria used here are quite broad – many of the peaks included are secondary summits of major m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pic De La Munia
The Pic de la Munia culminating at is the highest point of the three cirques of Troumouse, Barroude and Barrosa. It is located on the border between France ( Hautes-Pyrénées department) and Spain (Huesca province). Toponymy ''Era Munia'' could mean "nun", from « moniale », of Spanish origin.Marcellin Bérot, ''La vie des hommes de la montagne dans les Pyrénées racontée par la toponymie'', avec le concours du Centre régional des lettres de Midi-Pyrénées, 1998, Milan et parc national des Pyrénées Otherwise, it could stem from Latin, ''moenia'' meaning « walls », which corresponds to its relief. Access There are three main access routes which lead to the summit of la Munia. The first, most direct and most frequented, runs along the impressive north face, in the vast cirque de Troumouse. The starting point is located at the Troumouse car park, at about 2,100 m. The ascent is a bit technical (PD), with two delicate passages : a first small wall (III-) that one ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drainage Divide
A drainage divide, water divide, ridgeline, watershed, water parting or height of land is elevated terrain that separates neighboring drainage basins. On rugged land, the divide lies along topographical ridges, and may be in the form of a single range of hills or mountains, known as a dividing range. On flat terrain, especially where the ground is marshy, the divide may be difficult to discern. A triple divide is a point, often a summit, where three drainage basins meet. A ''valley floor divide'' is a low drainage divide that runs across a valley, sometimes created by deposition or stream capture. Major divides separating rivers that drain to different seas or oceans are continental divides. The term ''height of land'' is used in Canada and the United States to refer to a drainage divide. It is frequently used in border descriptions, which are set according to the "doctrine of natural boundaries". In glaciated areas it often refers to a low point on a divide where it is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Massif De La Munia
In geology, a massif ( or ) is a section of a planet's crust that is demarcated by faults or flexures. In the movement of the crust, a massif tends to retain its internal structure while being displaced as a whole. The term also refers to a group of mountains formed by such a structure. In mountaineering and climbing literature, a massif is frequently used to denote the main mass of an individual mountain. The massif is a smaller structural unit of the crust than a tectonic plate, and is considered the fourth-largest driving force in geomorphology. The word is taken from French (in which the word also means "massive"), where it is used to refer a large mountain mass or compact group of connected mountains forming an independent portion of a range. One of the most notable European examples of a massif is the Massif Central of the Auvergne region of France. The Face on Mars is an example of an extraterrestrial massif. Massifs may also form underwater, as with the Atlantis Ma ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cirque De Barrosa
A (; from the Latin word ') is an amphitheatre-like valley formed by glacial erosion. Alternative names for this landform are corrie (from Scottish Gaelic , meaning a pot or cauldron) and (; ). A cirque may also be a similarly shaped landform arising from fluvial erosion. The concave shape of a glacial cirque is open on the downhill side, while the cupped section is generally steep. Cliff-like slopes, down which ice and glaciated debris combine and converge, form the three or more higher sides. The floor of the cirque ends up bowl-shaped, as it is the complex convergence zone of combining ice flows from multiple directions and their accompanying rock burdens. Hence, it experiences somewhat greater erosion forces and is most often overdeepened below the level of the cirque's low-side outlet (stage) and its down-slope (backstage) valley. If the cirque is subject to seasonal melting, the floor of the cirque most often forms a tarn (small lake) behind a dam, which marks the down ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cirque De Troumouse
A (; from the Latin word ') is an Amphitheatre#Natural amphitheatres, amphitheatre-like valley formed by glacier, glacial erosion. Alternative names for this landform are corrie (from Scottish Gaelic language, Scottish Gaelic , meaning a pot or cauldron) and (; ). A cirque may also be a similarly shaped landform arising from fluvial erosion. The concave shape of a glacial cirque is open on the downhill side, while the cupped section is generally steep. Cliff-like slopes, down which ice and glaciated debris combine and converge, form the three or more higher sides. The floor of the cirque ends up bowl-shaped, as it is the complex convergence zone of combining ice flows from multiple directions and their accompanying rock burdens. Hence, it experiences somewhat greater erosion forces and is most often overdeepening, overdeepened below the level of the cirque's low-side outlet (stage) and its down-slope (backstage) valley. If the cirque is subject to seasonal melting, the floor o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cirque
A (; from the Latin word ') is an amphitheatre-like valley formed by glacial erosion. Alternative names for this landform are corrie (from Scottish Gaelic , meaning a pot or cauldron) and (; ). A cirque may also be a similarly shaped landform arising from fluvial erosion. The concave shape of a glacial cirque is open on the downhill side, while the cupped section is generally steep. Cliff-like slopes, down which ice and glaciated debris combine and converge, form the three or more higher sides. The floor of the cirque ends up bowl-shaped, as it is the complex convergence zone of combining ice flows from multiple directions and their accompanying rock burdens. Hence, it experiences somewhat greater erosion forces and is most often overdeepened below the level of the cirque's low-side outlet (stage) and its down-slope (backstage) valley. If the cirque is subject to seasonal melting, the floor of the cirque most often forms a tarn (small lake) behind a dam, which marks the down ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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