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Cordillera Oriental (Peru)
The Cordillera Oriental (Spanish for eastern mountain range) is the eastern part of the Andes in Peru. This range contains Paleozoic metamorphic rocks. It includes many subsidiary ranges such as the Vilcanota, Vilcabamba, Urubamba and Carabaya mountain ranges and peaks above 6,000 m such as Salcantay. The highest peak is Nevado Ausangate at 6372 m. See also * Cordillera Central (Peru) The Cordillera Central (Spanish for central mountain range) is part of the Andes in Peru. It extends in a northerly direction approximately between 11º 39’ and 12º 37’S and 75º 30’ and 76º 20’W (or between 11°37' and 12°26'S and 75 ... References Mountain ranges of the Andes Mountain ranges of Peru Mountain ranges of Cusco Region Mountain ranges of Puno Region {{Puno-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Andes Del Perú
The Andes, Andes Mountains or Andean Mountains (; ) are the longest continental mountain range in the world, forming a continuous highland along the western edge of South America. The range is long, wide (widest between 18°S – 20°S latitude), and has an average height of about . The Andes extend from north to south through seven South American countries: Venezuela, Colombia, Ecuador, Peru, Bolivia, Chile, and Argentina. Along their length, the Andes are split into several ranges, separated by intermediate depressions. The Andes are the location of several high plateaus—some of which host major cities such as Quito, Bogotá, Cali, Arequipa, Medellín, Bucaramanga, Sucre, Mérida, El Alto and La Paz. The Altiplano plateau is the world's second-highest after the Tibetan plateau. These ranges are in turn grouped into three major divisions based on climate: the Tropical Andes, the Dry Andes, and the Wet Andes. The Andes Mountains are the highest mountain range outsid ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Andes
The Andes, Andes Mountains or Andean Mountains (; ) are the longest continental mountain range in the world, forming a continuous highland along the western edge of South America. The range is long, wide (widest between 18°S – 20°S latitude), and has an average height of about . The Andes extend from north to south through seven South American countries: Venezuela, Colombia, Ecuador, Peru, Bolivia, Chile, and Argentina. Along their length, the Andes are split into several ranges, separated by intermediate depressions. The Andes are the location of several high plateaus—some of which host major cities such as Quito, Bogotá, Cali, Arequipa, Medellín, Bucaramanga, Sucre, Mérida, El Alto and La Paz. The Altiplano plateau is the world's second-highest after the Tibetan plateau. These ranges are in turn grouped into three major divisions based on climate: the Tropical Andes, the Dry Andes, and the Wet Andes. The Andes Mountains are the highest m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Peru
, image_flag = Flag of Peru.svg , image_coat = Escudo nacional del Perú.svg , other_symbol = Great Seal of the State , other_symbol_type = Seal (emblem), National seal , national_motto = "Firm and Happy for the Union" , national_anthem = "National Anthem of Peru" , march = "March of Flags" , image_map = PER orthographic.svg , map_caption = , image_map2 = , capital = Lima , coordinates = , largest_city = capital , official_languages = Peruvian Spanish, Spanish , languages_type = Co-official languages , languages = , ethnic_groups = , ethnic_groups_year = 2017 , demonym = Peruvians, Peruvian , government_type = Unitary state, Unitary Semi-presidential system, semi-presidential republic , leader_title1 = President of Peru, President ... [...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 ocean ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Metamorphic Rock
Metamorphic rocks arise from the transformation of existing rock to new types of rock in a process called metamorphism. The original rock (protolith) is subjected to temperatures greater than and, often, elevated pressure of or more, causing profound physical or chemical changes. During this process, the rock remains mostly in the solid state, but gradually recrystallizes to a new texture or mineral composition. The protolith may be an igneous, sedimentary, or existing metamorphic rock. Metamorphic rocks make up a large part of the Earth's crust and form 12% of the Earth's land surface. They are classified by their protolith, their chemical and mineral makeup, and their texture. They may be formed simply by being deeply buried beneath the Earth's surface, where they are subject to high temperatures and the great pressure of the rock layers above. They can also form from tectonic processes such as continental collisions, which cause horizontal pressure, friction, and distorti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cordillera Vilcanota
The Cordillera Vilcanota (Spanish ''cordillera'': "mountain range", Aymara Willkan Uta or Willkanuta: "house of the sun") is a mountain range located in Peru southeast of Cusco, on the boundary between the regions of Cusco and Puno. It extends between 13°39' and 14°29'S and 70°31' and 71°20'W for about 80 km. It includes 469 glaciers. To the east the rivers San Gabán and Azángaro are the natural boundary which separates it from the Carabaya range. The La Raya range near the La Raya pass is sometimes included or listed separately. Toponyms Most of the names in the range originate from Quechua and Aymara. They used to be spelled according to a mainly Spanish-based orthography which is incompatible with the normalized spellings of these languages and Law 29735 which regulates the 'use, preservation, development, recovery, promotion and diffusion of the originary languages of Peru'. According to Article 20 of ''Decreto Supremo No 004-2016-MC'' (Supreme Decree) which a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vilcabamba Mountain Range
The Vilcabamba mountain range is located in the region of Cusco, Peru, in the provinces of Anta, La Convención and Urubamba. It extends between 13°10' and 13°27'S. and 72°30' and 73°15'W for about 85 km.usgs.gov USGS, Peruvian Cordilleras Its highest peak is Salcantay, which is 6,271 m (20,574 ft) above sea level. Toponyms Most of the names in the range originate from . They used to be spelled according to a mainly Spanish-based orthography which is incompatible with the normalized spellings of these languages and Law 29735 which regulates the 'use, preservation, development, recovery, promotion and diffusion of the originary languages of Peru'. According to Arti ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Urubamba Mountain Range
The Urubamba mountain range (possibly from Quechua ''uru'' spider, ''pampa'' a plain) lies in the Cusco Region in Peru.The American Alpine Journal, Vol. 15, No. 2, Issue 47, 1973, p. 389. ''Cordillera Urubamba'' It extends in a northwesterly direction between 13°08' and 13°17'S and 71°58' and 72°16'W for about 30 km. Toponyms Most of the names in the range originate from Quechua and Aymara. They used to be spelled according to a mainly Spanish-based orthography which is incompatible with the normalized spellings of these languages and Law 29735 which regulates the 'use, preservation, development, recovery, promotion and diffusion of the original languages of Peru'. According to Article 20 of ''Decreto Supremo No 004-2016-MC'' (Supreme Decree) which approves the Regulations to Law 29735, published in the official newspaper El Peruano on July 22, 2016, adequate spellings of the toponyms in the normalized alphabets of the indigenous languages must progressively be proposed ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carabaya Mountain Range
The Cordillera Carabaya (Spanish for "Carabaya mountain range") lies in the Andes of Peru. It extends between 14°00' and 14°22'S and 69°38' and 70°19'W for about 75 km. It is located in the Puno Region, Carabaya Province, between the Vilcanota mountain range in the north-west and the Apolobamba mountain range in the south-east, north and north-east of Macusani. Mountains The highest peak in the range is Allincapac at . Other mountains are listed below:Taken from Mountaineering in the Andes by Jill Neate RGS-IBG Expedition Advisory Centre, 2nd edition, May 1994Michael Cocker, Frost, Dust and Tear Gas, Exploratory Mountaineering in the Peruvian Cordillera Carabaya, in: Alpine Journal 2008, p. 53-69allthemountains.com Maps of the Eastern Andes of Peru including two maps of the Carabaya mountain range (inactive website) See also * Chaupicocha * Kallawaya The Kallawaya are an indigenous group living in the Andes of Bolivia. They live in the Bautista Saavedra Pro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Salcantay
Salcantay, Salkantay or Sallqantay (in Quechua) is the highest peak in the Vilcabamba mountain range, part of the Peruvian Andes. It is located in the Cusco Region, about west-northwest of the city of Cusco. It is the 38th-highest peak in the Andes and the twelfth-highest in Peru. However, as a range highpoint in deeply incised terrain, it is the second most topographically prominent peak in the country, after Huascarán. Salcantay's proximity to Machu Picchu makes trekking around it an alternative to the oversubscribed Inca Trail; this is known as the Salkantay trek. History The name ''Salkantay'' is from ''sallqa'', a Quechua word meaning wild, uncivilized, savage, or invincible, and was recorded as early as 1583. The name is thus often translated as "Savage Mountain". Directly to the north of Salkantay lies Machu Picchu, which is at the end of a ridge that extends down from this mountain. Viewed from Machu Picchu's main sundial, the Southern Cross is above Salkantay's ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cordillera Central (Peru)
The Cordillera Central (Spanish for central mountain range) is part of the Andes in Peru. It extends in a northerly direction approximately between 11º 39’ and 12º 37’S and 75º 30’ and 76º 20’W (or between 11°37' and 12°26'S and 75°30' and 76°18'W) for about 60 km to 100 km. It contains the Paryaqaqa (P), Yauyos (Y) and Pichqa Waqra (PW) mountain ranges. It is located in the Junín Region and in the Lima Region. The name ''Cordillera Central'' is also applied for one of the three ranges that cross Peru in a northwesterly direction between the Cordillera Occidental ("the western range") where the Cordillera Central of the Junín and Lima Regions is located and the Cordillera Oriental ("the eastern range"). The mountaineer Evelio Echevarría uses the term for the La Viuda range and the Khaskaqucha range. Mountains The highest mountain in the range is Qutuni Ticlla or Qutuni (Aymara ''qutu'' heap, pile, ''-ni'' a suffix to indicate ownership, "the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Ranges Of The Andes
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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