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Aneto
Aneto is the highest mountain in the Pyrenees and in Aragon, Spain's third-highest mountain, reaching a height of . It is in the Spanish province of Huesca, the northernmost of 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, an 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 surface in the last 100 years, and may disappear around 2050. ...
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Aneto 02
Aneto is the highest mountain in the Pyrenees and in Aragon, Spain's third-highest mountain, reaching a height of . It is in the Spanish province of Huesca (province), Huesca, the northernmost of 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, Posets-Maladeta Natural Park, in the municipality of Benasque, Province of Huesca, Huesca province, an 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 ...
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Punta De Astorg
Point of Astorg (, , ) is a peak in the Spanish Pyrenees which rises to 3,354 m above sea level, in the Macizo de la Maladeta, 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 René d'Astorg, 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 ...
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Maladeta
Maladeta (3,312 m) is a mountain in the Pyrenees, close to the highest peak in the range, Aneto. It is located in the Natural Park of Posets-Maladeta in the town of Benasque in Province of Huesca, Aragon, Spain. Its northern slope contains the Maladeta Glacier, which is divided into the Western Maladeta and the Eastern Maladeta. Maladeta was previously considered to be highest peak in the area, and attempts to reach its summit took priority over the other peaks in the range. The first successful ascent of the peak was made by Johann Jacob Friedrich Wilhelm Parrot with guide Pierre Barrau in 1817. Etymology The name "Maladeta" comes from the Spanish ''montes malditos'', which means "Damned Mountains". According to some authorities the local name for the massif was ''Mala hita'' ("bad rocks" or "bad upper regions"). When French travellers came to the region they translated the name into the French as "Maladette", on the basis that it was cognate with the Italian term ''Mal ...
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List Of Mountains In Aragon
This is a list of mountains in Aragon, Spain. They include the Aneto, the highest peak in the Pyrenees, as well as the Moncayo, the highest peak in the Sistema Ibérico. See also * List of Pyrenean three-thousanders *Pyrenees * Pre-Pyrenees * Iberian System * List of mountains in Catalonia * List of mountains in the Valencian Community Further reading * References External links Federación Aragonesa de MontañismoPlataforma en Defensa de las Montañas de Aragón
*Jesus Pardina, ''Montañas de Aragón, 180 caminatas y ascensiones'', * tp://ftp.chebro.es/Hidrogeologia/Ficha ...
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Ribagorza (comarca)
Ribagorza (, ) or Ribagorça (; ) is a ''Comarcas of Aragon, comarca'' (administrative subdivision) in Aragon, Spain, situated in the north-east of the province of Huesca. It borders the Departments of France, French ''département'' of the Haute-Garonne to the north and Catalonia (the ''comarques'' of Val d'Aran, Alta Ribagorça, Pallars Jussà, and Noguera (comarca), Noguera) to the east. Within Aragon its neighboring ''comarcas'' are Sobrarbe, Somontano de Barbastro, and La Litera. It roughly corresponds to the Aragonese part of the medieval County of Ribagorza. The administrative capital of Ribagorza is Graus, although the historical capital of the county was at Benabarre. The Ribagorçan dialect is a transitional Aragonese language, Aragonese–Catalan language, Catalan dialect spoken in the western part of the ''comarca''. Municipalities in the eastern part, bordering Catalonia, are part of La Franja, a geolinguistic area, where the local language is a variety of Catalan. H ...
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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 (moon), Europa and Pluto add an extraterrestrial component to the field, which is referred to as "astroglaciology". Overview A glacier is a persistent body of dense ice, a form of rock) 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 ...
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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 drainage basin sustainability. A practitioner of hydrology is called a hydrologist. Hydrologists are scientists studying earth science, earth or environmental science, civil engineering, 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 Environmentalism, environmental preservation, natural disasters, and Water resource management, water management. Hydrology subdivides into surface water hydrology, groundwater hydrology (hydrogeology), and marine hydrology. Domains of hydrology include hydrometeorology, surface-water hydrology, surface hydrology, hydrogeology, drainage basin, drainage-basin management, and water quality. Oceanography and meteorology are not included beca ...
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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 The son of Prussian Ferdinand Schrader from Magdeburg, who emigrated to Bordeaux, and of Marie-Louise Ducos, Schrader was from a family of Nérac and the 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.uni ...
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Friedrich Parrot
Johann Jacob Friedrich Wilhelm Parrot (14 October 1791) was a Baltic German naturalist, explorer, and mountaineer, who lived and worked in 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 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. In 1816 and 1817, he visited the Alps and Pyrenees. ...
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Glacier
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 ever ...
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Mesozoic
The Mesozoic Era is the Era (geology), era of Earth's Geologic time scale, geological history, lasting from about , comprising the Triassic, Jurassic and Cretaceous Period (geology), Periods. It is characterized by the dominance of archosaurian reptiles such as the dinosaurs, and of Gymnosperm, gymnosperms such as cycads, ginkgoaceae and Araucariaceae, araucarian conifers; a hot Greenhouse and icehouse earth, greenhouse climate; and the tectonic break-up of Pangaea. The Mesozoic is the middle of the three eras since Cambrian explosion, complex life evolved: the Paleozoic, the Mesozoic, and the Cenozoic. The era began in the wake of the Permian–Triassic extinction event, the largest mass extinction in Earth's history, and ended with the Cretaceous–Paleogene extinction event, another mass extinction whose victims included the non-avian dinosaurs, Pterosaur, pterosaurs, Mosasaur, mosasaurs, and Plesiosaur, plesiosaurs. The Mesozoic was a time of significant tectonic, climatic, an ...
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Paleozoic
The Paleozoic ( , , ; or Palaeozoic) Era is the first of three Era (geology), geological eras of the Phanerozoic Eon. Beginning 538.8 million years ago (Ma), it succeeds the Neoproterozoic (the last era of the Proterozoic Eon) and ends 251.9 Ma at the start of the Mesozoic Era. The Paleozoic is subdivided into six period (geology), geologic periods (from oldest to youngest), Cambrian, Ordovician, Silurian, Devonian, Carboniferous and Permian. Some geological timescales divide the Paleozoic informally into early and late sub-eras: the Early Paleozoic consisting of the Cambrian, Ordovician and Silurian; the Late Paleozoic consisting of the Devonian, Carboniferous and Permian. The name ''Paleozoic'' was first used by Adam Sedgwick (1785–1873) in 1838 to describe the Cambrian and Ordovician periods. It was redefined by John Phillips (geologist), John Phillips (1800–1874) in 1840 to cover the Cambrian to Permian periods. It is derived from the Ancient Greek, Greek ''palaiós'' (π� ...
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