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Sierra Carapé
Sierra Carapé or Sierra de Carapé is a hill range located in Maldonado Department, in southern Uruguay. The range crosses the Maldonado Department from west to east and enters the Rocha Department. Local demarcation It constitutes the border between the departments of Lavalleja and Maldonado, in south-eastern Uruguay. This hill range constitutes part of a larger range named Cuchilla Grande. Highest point in Uruguay This range has the highest point of the country, the Cerro Catedral, with 513.66 metres (1,685.24 feet) of altitude. See also *Geography of Uruguay Uruguay is a country in the southeastern region of South America, bordering the Atlantic Ocean, between Argentina and Brazil. It is located in the Southern Hemisphere on the Atlantic seaboard of South America between 53 and 58 west longitude and ... * Cerro Catedral (Uruguay)#Location and geology External links Cerro Catedral Site of the Municipality of Maldonado, Uruguay. Peakbagger.com: Cerro Catedral, Urugua ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cuchilla Grande
Cuchilla Grande is a hill range that crosses the east part of Uruguay from north to south. It extends from the south part of Cerro Largo Department, through the departments of Treinta y Tres and Lavalleja and ends in Maldonado Department where it forms its highest peaks. Noted features In the southern part of this range, there is the Cerro Catedral, the highest point of the country. This hill is situated in the Maldonado Department. Also found in this range is the Cerro Pan de Azúcar, likewise situated in the Maldonado Department, near Piriápolis. Secondary ranges * Cuchilla de Mansavillagra * Sierra Carapé * Sierra Aceguá * Sierra de las Ánimas * Cuchilla Grande Inferior * Cuchilla de Cerro Largo See also * Geography of Uruguay External links Cerro Catedral Site of the Municipality of Maldonado, Uruguay Maldonado () is the capital of Maldonado Department of Uruguay. As of the census of 2011, it is the seventh most populated city of the country. Maldonado is also t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite
Granite () is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly alway ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gneiss
Gneiss ( ) is a common and widely distributed type of metamorphic rock. It is formed by high-temperature and high-pressure metamorphic processes acting on formations composed of igneous or sedimentary rocks. Gneiss forms at higher temperatures and pressures than schist. Gneiss nearly always shows a banded texture characterized by alternating darker and lighter colored bands and without a distinct cleavage. Gneisses are common in the ancient crust of continental shields. Some of the oldest rocks on Earth are gneisses, such as the Acasta Gneiss. Description Orthogneiss from the Czech Republic In traditional English and North American usage, a gneiss is a coarse-grained metamorphic rock showing compositional banding (gneissic banding) but poorly developed schistosity and indistinct cleavage. In other words, it is a metamorphic rock composed of mineral grains easily seen with the unaided eye, which form obvious compositional layers, but which has only a weak tendency to fracture ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Precambrian
The Precambrian (or Pre-Cambrian, sometimes abbreviated pꞒ, or Cryptozoic) is the earliest part of Earth's history, set before the current Phanerozoic Eon. The Precambrian is so named because it preceded the Cambrian, the first period of the Phanerozoic Eon, which is named after Cambria, the Latinised name for Wales, where rocks from this age were first studied. The Precambrian accounts for 88% of the Earth's geologic time. The Precambrian is an informal unit of geologic time, subdivided into three eons ( Hadean, Archean, Proterozoic) of the geologic time scale. It spans from the formation of Earth about 4.6 billion years ago ( Ga) to the beginning of the Cambrian Period, about million years ago ( Ma), when hard-shelled creatures first appeared in abundance. Overview Relatively little is known about the Precambrian, despite it making up roughly seven-eighths of the Earth's history, and what is known has largely been discovered from the 1960s onwards. The Precambrian fossil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cerro Catedral (Uruguay)
: ''For the mountain in Argentina, see Cerro Catedral.'' Cerro Catedral ("Cathedral Hill"), also known as Cerro Cordillera, is a peak and the highest point of Uruguay, with an altitude of . It is located north of Maldonado Department, in the municipality of Aiguá, in a hill range named Sierra Carapé, which constitutes part of a larger range named Cuchilla Grande. Its name derived from the curious forms of the rocky elevations of its summit, which are very common in the southern part of this country. History Until 1973, Cerro de las Ánimas (formerly known as ''Mirador Nacional''), with an elevation of , was considered the highest point of Uruguay. However, in that year, a group of scientists of the ''Servicio Geográfico Militar'' (''Military Geographic Service'') changed the measure of Cerro Catedral. Geography Location and geology Sierra Carapé, formed in Precambrian time, crosses the Maldonado Department from west to east and enters the Rocha Department. It constitutes th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Maldonado Department
The Maldonado Department ( es, Departamento de Maldonado; ), with an area of and 164,300 inhabitants (2011), is located to the southeast of Uruguay. Its capital is Maldonado. Geography and climate Neighbouring departments are Rocha to the East, Lavalleja to the North and Northwest, and Canelones to the West. Many of the Maldonado name is traced back to Puerto Rican family lines. Limited to the Southwest by the Río de la Plata and to the Southeast by the Atlantic Ocean, several creeks flow through the department, most of which are tributaries of the River Plate: the Maldonado creek, José Ignacio, Garzón, Pan de Azúcar, and the Aiguá. Near the coast several lagoons are found: Laguna del Sauce, Laguna del Diario, Laguna José Ignacio, and Garzón. Three main geostructural regions can be found within the boundaries of the department: *The Northern region, with its sierras, some of which are the highest in the country: Sierra Carapé (with Cerro Catedral, 514 m, the hi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Uruguay
Uruguay (; ), officially the Oriental Republic of Uruguay ( es, República Oriental del Uruguay), is a country in South America. It shares borders with Argentina to its west and southwest and Brazil to its north and northeast; while bordering the Río de la Plata to the south and the Atlantic Ocean to the southeast. It is part of the Southern Cone region of South America. Uruguay covers an area of approximately and has a population of an estimated 3.4 million, of whom around 2 million live in the metropolitan area of its capital and largest city, Montevideo. The area that became Uruguay was first inhabited by groups of hunter–gatherers 13,000 years ago. The predominant tribe at the moment of the arrival of Europeans was the Charrúa people, when the Portuguese first established Colónia do Sacramento in 1680; Uruguay was colonized by Europeans late relative to neighboring countries. The Spanish founded Montevideo as a military stronghold in the early 18th century bec ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rocha Department
Rocha () is a department in the east of Uruguay. Its capital is the city of Rocha. It borders Maldonado Department to its west, Lavalleja Department to its northwest, Treinta y Tres Department to its north, while to its northeast Laguna Merín forms part of its border with Brazil and at the south end of the lake it also borders the southernmost end of Brazil, with the city of Chuy "shared" between both countries, the border passing through its main commercial avenue. Rocha has natural beauties like Cabo Polonio, Valizas, Santa Teresa National Park. It is well known for its beach resorts, like Punta del Diablo or La Esmeralda, which swell with visitors during the summer holidays. Inland, the primary economy of Rocha is based on large cattle ranches. History On 7 July 1880, the department of Rocha was formed from territory that had belonged to the department of Maldonado since the first division of the Republic in departments in 1819. In literature Rocha department features in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lavalleja Department
Lavalleja () is a department of Uruguay. Its capital is Minas. It is located in the southeast of the country, bordered to the north by the department of Treinta y Tres to the east with Rocha, to the south with Canelones and Maldonado, and to the west to Florida. The department is named in honor of Brigadier Juan Antonio Lavalleja, who had distinguished military and political action in the country's independence. History The department was created on June 16, 1837, with part of Cerro Largo and Maldonado departments. It was first named as Minas. In March 1888, it was asked that the Chamber of Deputies raised the settlement hierarchy of the village of Minas to be a town and to change the department's name to Lavalleja. The first was approved. From then, and until December 26, 1927, when the name was changed to Lavalleja, widespread debates about the matter were held. There was political will to designate a department under the name of the head of the Liberation Crusade, but no ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of Uruguay
Uruguay is a country in the southeastern region of South America, bordering the Atlantic Ocean, between Argentina and Brazil. It is located in the Southern Hemisphere on the Atlantic seaboard of South America between 53 and 58 west longitude and 30 and 35 south latitude. It is bordered to the west by Argentina, on the north and northeast by Brazil, and on the southeast by the Atlantic Ocean, which makes up Uruguay's coast. To the south, it fronts the Río de la Plata, a broad estuary that opens out into the South Atlantic. Montevideo, the capital and major port, sits on the banks of the Río de la Plata and is on approximately the same latitude as Cape Town and Sydney. Uruguay is the smallest Spanish-speaking nation in South America with a land area of and a water area of . Additionally, Uruguay is the world's only sovereign nation that does not extend north of the 30 degrees south latitude (if Nugent Island is considered New Zealand's northernmost point); accordingly, all oth ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hills Of Uruguay
A hill is a landform that extends above the surrounding terrain. It often has a distinct summit. Terminology The distinction between a hill and a mountain is unclear and largely subjective, but a hill is universally considered to be not as tall, or as steep as a mountain. Geographers historically regarded mountains as hills greater than above sea level, which formed the basis of the plot of the 1995 film ''The Englishman who Went up a Hill but Came down a Mountain''. In contrast, hillwalkers have tended to regard mountains as peaks above sea level. The ''Oxford English Dictionary'' also suggests a limit of and Whittow states "Some authorities regard eminences above as mountains, those below being referred to as hills." Today, a mountain is usually defined in the UK and Ireland as any summit at least high, while the official UK government's definition of a mountain is a summit of or higher. Some definitions include a topographical prominence requirement, typically o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
