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Montes De Toledo
The Montes de Toledo are one of the main systems of mountain ranges in the Iberian Peninsula. They divide the drainage basin of the Tagus from the basin of the Guadiana. The highest peak is high La Villuerca. Description The Montes de Toledo are located in the central regions of the Iberian Peninsula, cutting transversally from east to west across the lower portion of the Meseta Central. The length of the Montes de Toledo is and their maximum width up to near Sonseca and Puertollano. The eastern Montes de Toledo ranges form one of the natural limits of the historical La Mancha region in Castile-La Mancha and the western end, including the ranges forming the broader Montes de Toledo, reaches into Portalegre District, Portugal. Geology Geologically the series of ranges making up the system were formed by Alpine orogeny, but unlike the Central System further north the Montes de Toledo comprise an older terrain of elongated belts of folded and thrust faulted sedimentary rocks t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cabañeros National Park
Cabañeros National Park (in Spanish: ''Parque Nacional de Cabañeros'') is a national park in the Montes de Toledo, Spain. It falls within two provinces, the northwest of Ciudad Real and the southwest of Toledo. The Park was designated in 1995 and has an area of . It lies between the Estena and Bullaque rivers, extending into the Chorito and Miraflores mountain ranges. It is the best and largest surviving area of Iberian Mediterranean forest, with an enormous variety of plant species. It also includes sites of geological interest (Paleozoic sites known as ''Cámbrico y Ordovícico del Parque Nacional de Cabañeros'').Gutiérrez-Marco, J.C.; García-Bellido, D.C.; Rábano, I.; Baeza Chico, E.; Sá, A.A. & Sarmiento, G.N. 2011. Geotouristic trails in the Cabañeros National Park (central Spain), pp. 125--128. In: Geotourism in Action. Proceedings of the International Congress of Geotourism–Arouca 2011, Arouca (Portugal). The antipodes of the park are located in Tongariro Nationa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Portugal
Portugal, officially the Portuguese Republic ( pt, República Portuguesa, links=yes ), is a country whose mainland is located on the Iberian Peninsula of Southwestern Europe, and whose territory also includes the Atlantic archipelagos of the Azores and Madeira. It features the westernmost point in continental Europe, and its Iberian portion is bordered to the west and south by the Atlantic Ocean and to the north and east by Spain, the sole country to have a land border with Portugal. Its two archipelagos form two autonomous regions with their own regional governments. Lisbon is the capital and largest city by population. Portugal is the oldest continuously existing nation state on the Iberian Peninsula and one of the oldest in Europe, its territory having been continuously settled, invaded and fought over since prehistoric times. It was inhabited by pre-Celtic and Celtic peoples who had contact with Phoenicians and Ancient Greek traders, it was ruled by the Ro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Corral De Cantos
A pen is an enclosure for holding livestock. It may also perhaps be used as a term for an enclosure for other animals such as pets that are unwanted inside the house. The term describes types of enclosures that may confine one or many animals. Construction and terminology vary depending on the region of the world, purpose, animal species to be confined, local materials used and tradition. ''Pen'' or ''penning'' as a verb refers to the act of confining animals in an enclosure. Similar terms are kraal, boma, and corrals. Encyclopædia Britannica notes usage of the term "kraal" for elephant corrals in India, Sri Lanka, and Thailand. Australia and New Zealand In Australia and New Zealand a ''pen'' is a small enclosure for livestock (especially sheep or cattle), which is part of a larger construction, e.g. ''calf pen'', ''forcing pen'' (or yard) in sheep or cattle yards, or a ''sweating pen'' or ''catching pen'' in a shearing shed. In Australian and New Zealand English, a paddo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Montes De Toledo Comarca
Montes de Toledo Comarca ( es, Comarca de los Montes de Toledo) is a ''comarca'' located at the southern end of the province of Toledo, Spain. The natural comarca includes some municipal terms in Ciudad Real Province. It is named after the Montes de Toledo mountain system. and, like other mountainous rural areas in central Spain, this comarca has been traditionally a place of cattle rearers, with some honey production as well. Nowadays the comarca has suffered heavy depopulation as the economy has diversified. Municipal terms and villages Municipal terms in Ciudad Real Province * Alcoba * Arroba de los Montes * El Robledo * Fontanarejo * Fuente el Fresno * Las Labores * Los Cortijos * Navalpino Navalpino is a municipality in Ciudad Real, Castile-La Mancha, in the Montes de Toledo area of Spain. In the 2014 census A census is the procedure of systematically acquiring, recording and calculating information about the members of a given po ... * Navas de Estena * Por ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Toledo Province
Toledo is a province of central Spain, in the western part of the autonomous community of Castile–La Mancha. It is bordered by the provinces of Madrid, Cuenca, Ciudad Real, Badajoz, Cáceres, and Ávila. Its capital is the city of Toledo. Demography Of the province's 711,228 people (2012), only about 1/9 live in the capital, Toledo, which is also the capital of the autonomous community. The most populated municipalities in the province are Toledo and Talavera de la Reina with 83,741 and 83,303 inhabitants each (INE, 2017). The province contains 204 municipalities. The smallest municipality in Spain, Illán de Vacas, with a population of 8, is in Toledo province. See List of municipalities in Toledo. Population development The historical population is given in the following chart: Colors= id:lightgrey value:gray(0.9) id:darkgrey value:gray(0.7) id:sfondo value:rgb(1,1,1) ImageSize = width:600 height:auto barincrement:30 PlotArea = left:40 bottom:40 top:20 right: ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ciudad Real Province
The province of Ciudad Real () is a province in the southwestern part of the autonomous community of Castile-La Mancha, Spain. It is bordered by the provinces of Cuenca, Albacete, Jaén, Córdoba, Badajoz, and Toledo. It is partly located in the old natural region of La Mancha. Its capital is Ciudad Real. It is the third largest province by area in all of Spain, after Cáceres and Badajoz. The historic comarca Campo de Calatrava is located in the center of the province. History Ciudad Real was one of the 49 provinces in which Spain was divided in the territorial reorganization of 1833, taking its name from its largest city and capital. Its limits corresponded more or less to the historical province of La Mancha, which was part of the kingdom of Toledo. The Spanish government created the autonomous community of Castilla-La Mancha on 15 November 1978, as one of several autonomous regions. The new, hyphenated name was chosen to join the historic Castilla region, which exte ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Physiographic
Physical geography (also known as physiography) is one of the three main branches of geography. Physical geography is the branch of natural science which deals with the processes and patterns in the natural environment such as the atmosphere, hydrosphere, biosphere, and geosphere. This focus is in contrast with the branch of human geography, which focuses on the built environment, and technical geography, which focuses on using, studying, and creating tools to obtain,analyze, interpret, and understand spatial information. The three branches have significant overlap, however. Sub-branches Physical geography can be divided into several branches or related fields, as follows: * Geomorphology is concerned with understanding the surface of the Earth and the processes by which it is shaped, both at the present as well as in the past. Geomorphology as a field has several sub-fields that deal with the specific landforms of various environments e.g. desert geomorphology and fluvial ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sierra Morena
The Sierra Morena is one of the main systems of mountain ranges in Spain. It stretches for 450 kilometres from east to west across the south of the Iberian Peninsula, forming the southern border of the ''Meseta Central'' plateau and providing the watershed between the valleys of the Guadiana to the north and the west, and the Guadalquivir to the south. Its highest summit is 1,332 m high Bañuela. Other notable peaks are Corral de Borros 1,312 m and Cerro de la Estrella 1,298 m. The name ''Sierra Morena'' has a strong legendary reputation in Spanish culture and tradition, with myths about bandits ''(Los bandidos de Sierra Morena)'', a giant snake ''(El Saetón de Sierra Morena)'' and a child brought up by wolves (Marcos Rodríguez Pantoja), among others. This range is also mentioned in the famous Mexican song "Cielito Lindo" and in one of the most well known traditional Spanish songs, "Soy Minero", interpreted by Antonio Molina. Description The Sierra Morena stretches f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology Of The Appalachians
The geology of the Appalachians dates back to more than 480 million years ago. A look at rocks exposed in today's Appalachian Mountains reveals elongate belts of folded and thrust faulted marine sedimentary rocks, volcanic rocks and slivers of ancient ocean floor – strong evidence that these rocks were deformed during plate collision. The birth of the Appalachian ranges marks the first of several mountain building plate collisions that culminated in the construction of the supercontinent Pangaea with the Appalachians and neighboring Anti-Atlas mountains (now in Morocco) near the center. These mountain ranges likely once reached elevations similar to those of the Alps and the Rocky Mountains before they were eroded. Geological history Paleozoic Era During the earliest part of the Paleozoic Era, the continent that would later become North America straddled the equator. The Appalachian region was a passive plate margin, not unlike today's Atlantic Coastal Plain Province. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sedimentary Rocks
Sedimentary rocks are types of rock that are formed by the accumulation or deposition of mineral or organic particles at Earth's surface, followed by cementation. Sedimentation is the collective name for processes that cause these particles to settle in place. The particles that form a sedimentary rock are called sediment, and may be composed of geological detritus (minerals) or biological detritus (organic matter). The geological detritus originated from weathering and erosion of existing rocks, or from the solidification of molten lava blobs erupted by volcanoes. The geological detritus is transported to the place of deposition by water, wind, ice or mass movement, which are called agents of denudation. Biological detritus was formed by bodies and parts (mainly shells) of dead aquatic organisms, as well as their fecal mass, suspended in water and slowly piling up on the floor of water bodies (marine snow). Sedimentation may also occur as dissolved minerals precipitate from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thrust Fault
A thrust fault is a break in the Earth's crust, across which older rocks are pushed above younger rocks. Thrust geometry and nomenclature Reverse faults A thrust fault is a type of reverse fault that has a dip of 45 degrees or less. If the angle of the fault plane is lower (often less than 15 degrees from the horizontal) and the displacement of the overlying block is large (often in the kilometer range) the fault is called an ''overthrust'' or ''overthrust fault''. Erosion can remove part of the overlying block, creating a ''fenster'' (or ''window'') – when the underlying block is exposed only in a relatively small area. When erosion removes most of the overlying block, leaving island-like remnants resting on the lower block, the remnants are called ''klippen'' (singular ''klippe''). Blind thrust faults If the fault plane terminates before it reaches the Earth's surface, it is referred to as a ''blind thrust'' fault. Because of the lack of surface evidence, blind thr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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