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Sierra De Guara
The Sierra de Guara is a mountain massif in the province of Huesca, the most northerly province in the autonomous community of Aragon, Spain. Its highest point is Tozal de Guara (2,077 m). It lies around 25 km northeast of the city of Huesca itself. Much of the massif is now included within the Sierra y Cañones de Guara Natural Park which extends 43 km from west to east and 25 km north to south. The Park includes, in addition to the Sierra de Guara itself, much of the Sierra de Gabardiella in the west and the Sierra de Arangol, Sierra de Balced, Sierra de Sebil and Sierra de Rufás in the east. Landscape features A number of rivers flow north-south through the area, the principal ones having their sources to the north of the massif and cut through the range by way of spectacular gorges such as those of the Rio Alcanadre, Rio Guatizalema, Rio Vero and Rio Isuala. Each of these rivers ultimately drain into the Ebro. Geology The massif is formed mainly from Palaeoge ...
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Alto Gállego
Alto Gállego ( Aragonese: ''Alto Galligo'') is a comarca located in the north of the autonomous community of Aragón, Spain. It occupies practically the entirety of the upper basin of the Río Gállego. Historically the comarca was a part of the area known as Jacetania, the original nucleus of the old county of Aragón. The historical territories integrated into that area were the Tena Valley, the lands surrounding Biescas, and the Serrablo. Today, Alto Gállego borders with the comarca of Jacetania to the West, the Sobrarbe to the East, the Hoya de Huesca, France France (), officially the French Republic ( ), is a country primarily located in Western Europe. It also comprises of Overseas France, overseas regions and territories in the Americas and the Atlantic Ocean, Atlantic, Pacific Ocean, Pac ... to the North. Territory and Population See also * Linea P References External links Official Website
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Miocene
The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recent" because it has 18% fewer modern marine invertebrates than the Pliocene has. The Miocene is preceded by the Oligocene and is followed by the Pliocene. As Earth went from the Oligocene through the Miocene and into the Pliocene, the climate slowly cooled towards a series of ice ages. The Miocene boundaries are not marked by a single distinct global event but consist rather of regionally defined boundaries between the warmer Oligocene and the cooler Pliocene Epoch. During the Early Miocene, the Arabian Peninsula collided with Eurasia, severing the connection between the Mediterranean and Indian Ocean, and allowing a faunal interchange to occur between Eurasia and Africa, including the dispersal of proboscideans into Eurasia. During the ...
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Europe
Europe is a large peninsula conventionally considered a continent in its own right because of its great physical size and the weight of its history and traditions. Europe is also considered a Continent#Subcontinents, subcontinent of Eurasia and it is located entirely in the Northern Hemisphere and mostly in the Eastern Hemisphere. Comprising the westernmost peninsulas of Eurasia, it shares the continental landmass of Afro-Eurasia with both Africa and Asia. It is bordered by the Arctic Ocean to the north, the Atlantic Ocean to the west, the Mediterranean Sea to the south and Asia to the east. Europe is commonly considered to be Boundaries between the continents of Earth#Asia and Europe, separated from Asia by the drainage divide, watershed of the Ural Mountains, the Ural (river), Ural River, the Caspian Sea, the Greater Caucasus, the Black Sea and the waterways of the Turkish Straits. "Europe" (pp. 68–69); "Asia" (pp. 90–91): "A commonly accepted division between Asia and E ...
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Caving
Caving – also known as spelunking in the United States and Canada and potholing in the United Kingdom and Ireland – is the recreational pastime of exploring wild cave systems (as distinguished from show caves). In contrast, speleology is the scientific study of caves and the cave environment.Caving in New Zealand
(from Te Ara: The Encyclopedia of New Zealand, Accessed 2012-11.)
The challenges involved in caving vary according to the cave being visited; in addition to the total absence of light beyond the entrance, negotiating pitches, squeezes,
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Rock Climbing
Rock climbing is a sport in which participants climb up, across, or down natural rock formations. The goal is to reach the summit of a formation or the endpoint of a usually pre-defined route without falling. Rock climbing is a physically and mentally demanding sport, one that often tests a climber's strength, endurance, agility and balance along with mental control. Knowledge of proper climbing techniques and the use of specialized climbing equipment is crucial for the safe completion of routes. Because of the wide range and variety of rock formations around the world, rock climbing has been separated into several different styles and sub-disciplines, such as scrambling, bouldering, sport climbing, and trad (traditional) climbing another activity involving the scaling of hills and similar formations, differentiated by the rock climber's sustained use of hands to support their body weight as well as to provide balance. Rock climbing competitions have the objectives of either ...
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Canyoning
Canyoning (canyoneering in the United States, kloofing in South Africa) is a type of mountaineering that involves travelling in canyons using a variety of techniques that may include other outdoor activities such as walking, scrambling, climbing, jumping, abseiling (rappelling), and swimming. Although non-technical descents such as hiking down a canyon (''canyon hiking'') are often referred to as ''canyoneering'', the terms ''canyoning'' and ''canyoneering'' are more often associated with technical descents — those that require abseils (rappels) and ropework, technical climbing or down-climbing, technical jumps, and/or technical swims. Canyoning is frequently done in remote and rugged settings and often requires navigational, route-finding, and other wilderness travel skills. Canyons that are ideal for canyoning are often cut into the bedrock stone, forming narrow gorges with numerous drops, beautifully sculpted walls, and sometimes spectacular waterfalls. Most canyo ...
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Barbastro
Barbastro (Latin: ''Barbastrum'' or ''Civitas Barbastrensis'', Aragonese: ''Balbastro'') is a city in the Somontano county, province of Huesca, Spain. The city (also known originally as Barbastra or Bergiduna) is at the junction of the rivers Cinca and Vero. History An ancient Celtiberian city called '' Bergidum'' or ''Bergiduna'', in Roman times Barbastro (now called ''Brutina'') was included in the Hispania Citerior region, and later of Hispania Tarraconensis. After the fall of the Western Roman Empire, it was part of the Visigoth kingdom. Barbastro and the Barbitaniya area were overtaken by Musa bin Nusair in 717, as part of the Umayyad push to conquer northern states of the Marca Hispanica and the name Madyar was given to the town. It was later settled by the Banu Jalaf who made it the capital of the Emirate of Barbineta and Huesca until 862, and was known as the Emirate of Brabstra until 882. In 1064, Sancho Ramírez, King of Aragón, and his Frankish Christian fo ...
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Tourism
Tourism is travel for pleasure or business; also the theory and practice of touring (other), touring, the business of attracting, accommodating, and entertaining tourists, and the business of operating tour (other), tours. The World Tourism Organization defines tourism more generally, in terms which go "beyond the common perception of tourism as being limited to holiday activity only", as people "travelling to and staying in places outside their usual environment for not more than one consecutive year for leisure and not less than 24 hours, business and other purposes". Tourism can be Domestic tourism, domestic (within the traveller's own country) or International tourism, international, and international tourism has both incoming and outgoing implications on a country's balance of payments. Tourism numbers declined as a result of a strong economic slowdown (the late-2000s recession) between the second half of 2008 and the end of 2009, and in consequence of t ...
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Rodellar
Rodellar is a locality located in the municipality of Bierge, in Huesca province, Aragon, Spain. As of 2020, it has a population of 54. Geography Rodellar is located 64km east-northeast of Huesca Huesca (; an, Uesca) is a city in north-eastern Spain, within the autonomous community of Aragon. It is also the capital of the Spanish province of the same name and of the comarca of Hoya de Huesca. In 2009 it had a population of 52,059, almo .... References Populated places in the Province of Huesca {{huesca-geo-stub ...
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Alquézar
Alquézar ( Aragonese: ''Alquezra'') is a municipality in the province of Huesca, in the autonomous community of Aragon, Spain. As of 2012, its population was 301. Overview Situated on a limestone outcrop of the Eocene age to the west of the canyon of the Rio Vero in the Sierra y Cañones de Guara Natural Park, the village grew up around a castle and the Collegiate church of Santa Maria, which was consecrated in 1099. The name of the village comes from the Arabic القصر '' al qaçr'' for "fort" or "castle" (renamed as Alcazar in Spanish). The castle became the main defense point of the nearby city of Barbastro. Since Alquézar is situated in the Sierra y Cañones de Guara Natural Park, there are various campsites in the local area to cater to outdoor enthusiasts. Popular activities include canyoning, walking, rock climbing and abseiling, as well as ornithology (since vultures nest on the steep faces of the Rio Vero canyon). The surrounding area to the south towards Barba ...
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Conglomerate (geology)
Conglomerate () is a clastic sedimentary rock that is composed of a substantial fraction of rounded to subangular gravel-size clasts. A conglomerate typically contains a matrix of finer-grained sediments, such as sand, silt, or clay, which fills the interstices between the clasts. The clasts and matrix are typically cemented by calcium carbonate, iron oxide, silica, or hardened clay. Conglomerates form by the consolidation and lithification of gravel. They can be found in sedimentary rock sequences of all ages but probably make up less than 1 percent by weight of all sedimentary rocks. In terms of origin and depositional mechanisms, they are closely related to sandstones and exhibit many of the same types of sedimentary structures, e.g., tabular and trough cross-bedding and graded bedding.Boggs, S. (2006) ''Principles of Sedimentology and Stratigraphy.'', 2nd ed. Prentice Hall, New York. 662 pp. Friedman, G.M. (2003) ''Classification of sediments and sedimentary rocks.'' In G ...
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