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Pico De Aneto
Aneto (''pic d'Aneto'' in French, formerly ''pic de Néthou'') is the highest mountain in the Pyrenees and in Aragon, and Spain's third-highest mountain, reaching a height of . It stands in the Spanish province of Huesca, the northernmost of the three Aragonese provinces, south of the France–Spain border. It forms the southernmost part of the Maladeta massif. Aneto is located in the Posets-Maladeta Natural Park, in the municipality of Benasque, Huesca province, autonomous community of Aragon, Spain. It is part of the Maladeta massif and is located in the Benasque valley. It consists of Paleozoic terrain of a granitic nature and Mesozoic materials. Its northern side holds the largest glacier in the Pyrenees, covering in 2005; it is shrinking rapidly due to warming summer temperatures and decreasing winter precipitations over the 20th century – it covered 106.7 ha in 1981, and over 200 ha in the 19th century. It is estimated that it has lost more than half of its ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Peaks By Prominence
This is a list of mountain peaks ordered by their topographic prominence. Terminology The prominence of a peak is the minimum height of climb to the summit on any route from a higher peak, or from sea level if there is no higher peak. The lowest point on that route is the col. For full definitions and explanations of ''topographic prominence'', ''key col'', and ''parent'', see topographic prominence. In particular, the different definitions of the parent of a peak are addressed at length in that article. ''Height'' on the other hand simply means elevation of the summit above sea level. Regarding parents, the ''prominence parent'' of peak A can be found by dividing the island or region in question into territories, by tracing the runoff from the key col ( mountain pass) of every peak that is more prominent than peak A. The parent is the peak whose territory peak A resides in. The ''encirclement parent'' is found by tracing the contour below peak A's key col and picking the high ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
France–Spain Border
The France–Spain border (; ) was formally defined in 1659. It separates the two countries from Hendaye and Irun in the west, running through the Pyrenees to Cerbère and Portbou on the Mediterranean Sea. Features Main border The Franco-Spanish border runs for between southwestern France and northeastern Spain. It begins in the west on the Bay of Biscay at the French city of Hendaye and the Spanish city of Irun (). The border continues eastward along the Pyrenees to Andorra (). At this point, the small country interrupts the border between Spain and France for on the Spanish side and on the French side. Then the border continues eastward () to the Mediterranean Sea at Cerbère in France and Portbou in Spain (). From west to east, crossing the border: * Spain ** Gipuzkoa ( Basque Country) ** Navarre ** Province of Huesca ( Aragon) ** Province of Lleida (Catalonia) ** Province of Girona (Catalonia) * France ** Pyrénées-Atlantiques (Nouvelle-Aquitaine) ** Hautes- ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Punta De Astorg
Point of Astorg (, , ) is a peak in the Spanish Pyrenees which rises to 3,354 m above sea level, in the Maladeta massif. It is the second highest peak in the massif, after Aneto (3,404 m) and the fourth highest peak in the Pyrenees, behind Aneto, Pico Posets and Monte Perdido. Toponymy The summit was called Lerilica Peak until it was climbed on July 9, 1901 by Count René d'Astorg (1860-1940), a French Pyrenean. The summit was renamed in his name. Punta de Astorg is the highest point of a large ridge called ''Cresta Maldito'' in Spanish, literally "cursed ridge" in English. The first ascents in the Maladeta massif to overcome the Aneto were indeed the cause of several disasters in the glaciers. The death in 1824 in the bergschrund of the Maladeta glacier of Pierre Barrau of the ''Compagnie des guides de Luchon'', caused real emotion among the local guides: the latter, already very frightened by the risks of the glacier, were then panicked by this massif which they now cons ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Friedrich Parrot
Johann Jacob Friedrich Wilhelm Parrot (14 October 1791) was a Baltic German naturalist, explorer, and mountaineer, who lived and worked in Dorpat (today Tartu, Estonia) in what was then the Governorate of Livonia of the Russian Empire. A pioneer of Russian and Estonian scientific mountaineering, Parrot is best known for leading the first expedition to the summit of Mount Ararat in recorded history. Early career Born in Karlsruhe, in the Margraviate of Baden, Parrot was the son of Georg Friedrich Parrot, the first rector of the University of Dorpat (today the University of Tartu) and a close friend of Tsar Alexander I. He studied medicine and natural science at Dorpat and, in 1811, undertook an expedition to the Crimea and the Caucasus with Moritz von Engelhardt. There he used a barometer to measure the difference in sea level between the Caspian Sea and Black Sea. On his return he was appointed assistant doctor and, in 1815, surgeon in the Imperial Russian Army. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glaciology
Glaciology (; ) is the scientific study of glaciers, or more generally ice and natural phenomena that involve ice. Glaciology is an interdisciplinary Earth science that integrates geophysics, geology, physical geography, geomorphology, climatology, meteorology, hydrology, biology, and ecology. The impact of glaciers on people includes the fields of human geography and anthropology. The discoveries of water ice on the Moon, Mars, Europa and Pluto add an extraterrestrial component to the field, which is referred to as "astroglaciology". Overview A glacier is an extended mass of ice formed from snow falling and accumulating over a long period of time; glaciers move very slowly, either descending from high mountains, as in valley glaciers, or moving outward from centers of accumulation, as in continental glaciers. Areas of study within glaciology include glacial history and the reconstruction of past glaciation. A glaciologist is a person who studies glaciers. A glacia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hydrology
Hydrology () is the scientific study of the movement, distribution, and management of water on Earth and other planets, including the water cycle, water resources, and environmental watershed sustainability. A practitioner of hydrology is called a hydrologist. Hydrologists are scientists studying earth or environmental science, civil or environmental engineering, and physical geography. Using various analytical methods and scientific techniques, they collect and analyze data to help solve water related problems such as environmental preservation, natural disasters, and water management. Hydrology subdivides into surface water hydrology, groundwater hydrology (hydrogeology), and marine hydrology. Domains of hydrology include hydrometeorology, surface hydrology, hydrogeology, drainage-basin management, and water quality, where water plays the central role. Oceanography and meteorology are not included because water is only one of many important aspects within those field ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Franz Schrader
Jean Daniel François Schrader (January 11, 1844 – October 18, 1924), better known as Franz Schrader, was a French mountaineer, geographer, cartographer and landscape painter, born in Bordeaux. He made an important contribution to the mapping of the Pyrenees and was highly considered among the pyreneists. Biography He was the son of Prussian Ferdinand Schrader from Magdeburg, who emigrated to Bordeaux, and of Marie-Louise Ducos, from a family of Nérac, and cousin of geographers Élisée and Onésime Reclus. He showed a talent for drawing from an early age. But his strict father, denying him the opportunity of higher education, placed him as a pen pusher at a tax gatherer. Franz then found another job in a trading house run by one of his father's friends, a situation where he could devote more time to broadening his literary and scientific knowledge. Hélène Saule-Sorbé, Michel Rodes, Guy AuriolFranz Schrader (1844–1924) : un pyrénéiste d'exceptionon ''web.univ-pau.fr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Louis Ramond De Carbonnières
Louis François Élisabeth Ramond, baron de Carbonnières (4 January 1755 Strasbourg – 14 May 1827), was a French politician, geologist and botanist. He is regarded as one of the first explorers of the high mountains of the Pyrenees who can be described as a '' pyreneist''. Life Louis Ramond was born in Strasbourg, to Pierre-Bernard Ramond (1715–1796), treasurer of war, and Rosalie-Reine Eisentrand (1732–1762). He studied law at the University of Strasbourg in 1775 and became a lawyer in February 1777. In Strasbourg he became friends with another student, Jakob Michael Reinhold Lenz (1751–1792), a writer belonging to the then-fashionable '' Sturm und Drang'' movement. During this period Ramond discovered German Romantic literature, in particular Goethe's '' The Sorrows of Young Werther''; this book inspired him to become a writer and in 1777 he published the ''Werther''-influenced ''Les Dernières aventures du jeune d’Olban'' (''The Last Adventures of Young Olban''). ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving 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 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 continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between latitudes 35°N and 35°S, glaciers occur o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mesozoic
The Mesozoic Era ( ), also called the Age of Reptiles, the Age of Conifers, and colloquially as the Age of the Dinosaurs is the second-to-last era of Earth's geological history, lasting from about , comprising the Triassic, Jurassic and Cretaceous Periods. It is characterized by the dominance of archosaurian reptiles, like the dinosaurs; an abundance of conifers and ferns; a hot greenhouse climate; and the tectonic break-up of Pangaea. The Mesozoic is the middle of the three eras since complex life evolved: the Paleozoic, the Mesozoic, and the Cenozoic. The era began in the wake of the Permian–Triassic extinction event, the largest well-documented mass extinction in Earth's history, and ended with the Cretaceous–Paleogene extinction event, another mass extinction whose victims included the non-avian dinosaurs, pterosaurs, mosasaurs, and plesiosaurs. The Mesozoic was a time of significant tectonic, climatic, and evolutionary activity. The era witnessed the gradual ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paleozoic
The Paleozoic (or Palaeozoic) Era is the earliest of three geologic eras of the Phanerozoic Eon. The name ''Paleozoic'' ( ;) was coined by the British geologist Adam Sedgwick in 1838 by combining the Greek words ''palaiós'' (, "old") and ''zōḗ'' (), "life", meaning "ancient life" ). It is the longest of the Phanerozoic eras, lasting from , and is subdivided into six geologic periods (from oldest to youngest): # Cambrian # Ordovician # Silurian # Devonian # Carboniferous # Permian The Paleozoic comes after the Neoproterozoic Era of the Proterozoic Eon and is followed by the Mesozoic Era. The Paleozoic was a time of dramatic geological, climatic, and evolutionary change. The Cambrian witnessed the most rapid and widespread diversification of life in Earth's history, known as the Cambrian explosion, in which most modern phyla first appeared. Arthropods, molluscs, fish, amphibians, reptiles, and synapsids all evolved during the Paleozoic. Life began in the oc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Province Of Huesca
Huesca ( an, Uesca, ca, Osca), officially Huesca/Uesca, is a province of northeastern Spain, in northern Aragon. The capital is Huesca. Positioned just south of the central Pyrenees, Huesca borders France and the French Departments of Haute-Garonne, Pyrénées-Atlantiques and Hautes-Pyrénées. Within Spain, Huesca's neighboring provinces are Navarre, Zaragoza and Lleida. Geography Covering a primarily mountainous area of km², the province of Huesca has a total population of in 2018, with almost a quarter of its people living in the capital city of Huesca. The low population density, 14.62/km², has meant that Huesca's lush valleys, rivers, and lofty mountain ranges have remained relatively pristine and unspoiled by progress. Home to majestic scenery, the tallest mountain in the Pyrenees, the Aneto; eternal glaciers, such as at Monte Perdido; and the National Park of Ordesa and Monte Perdido, rich in flora and protected fauna. Popular with mountaineers, spelunkers, pa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
