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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 ...
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Cerro Catedral
Cerro Catedral is a mountain located from San Carlos de Bariloche, and inside the Nahuel Huapí National Park, in Patagonia, Argentina. The mountain is the biggest ski center in South America and in the Southern Hemisphere, with a skiable area of , of ski runs, and a lift capacity of 35,000 skiers per hour. It is also popular due to the views of the Nahuel Huapi lake. There are also a number of hotels and hostels at the foot of the mountain, and a summer hikers' hut called ''Refugio Lynch'' on one of the tops of the mountain. During the summer, the ''Refugio Frey'' and a camping accommodate trekkers and rock climbers next to ''Tonček'' lagoon, near the ''Torre Principal''; Catedral's highest point. On August 27, 2005, the 2005 South American Ski Mountaineering Championship, 1st South American Ski Mountaineering Championship in combination with the last race of the 2005 South American Ski Mountaineering Cup and the 2nd International Open of ski mountaineering was carried out ...
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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 ...
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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 the name of the municipality to which the city belongs. It includes the following zones: Maldonado, Punta Ballena, Portezuelo, Barrio Hipódromo, Canteras de Marelli, Los Ceibos, Abra de Perdomo, Laguna del Diario, El Placer, Cantegril, Maldonado Nuevo, Cerro Pelado, San Francisco, San Fernando, Estación, Leonel, Perlita, El Molino, and Biarritz. History The origin of Maldonado's name dates back to January 1530, when Sebastian Cabot, an Italian explorer, departed for Castilla and left his Lieutenant, Francisco Maldonado, in what is now the bay of Maldonado. After the Treaty of Madrid, when they started to divide Spanish and Portuguese properties in that region of America, the military governor of Montevideo, José Joaquín de Viana, suggested to the King that they should establish two populations, one in Maldonado and ...
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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 ...
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Cerro Pan De Azúcar
Cerro Pan de Azúcar (''Sugar Loaf Hill'') is among the top 10 highest points of Uruguay, with an altitude of 423 metres (1,387.8 ft). Location and features It is located southwest of Maldonado Department, in the municipality of Piriápolis, in a range of hills named Cuchilla Grande. At the eastern feet of the hill and partly on its side, is the Reserva de Flora y Fauna del Pan de Azúcar, a nature reserve and zoo. On its summit, there is a cross made of cement, with a height of 35 metres (114.8 feet), visible from a considerable distance. The cross is visitable inside with a spiral staircase leading to the horizontal part of the cross, which offers view of the area through small openings. History In 1890 Don Francisco Piria, founder of the resort of Piriápolis, had bought a big stretch of land including the Cerro Pan de Azúcar and stretching all the way to the beach. The hill was rich in granite and by his decision one of its slopes became a quarry which provi ...
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Snow
Snow comprises individual ice crystals that grow while suspended in the atmosphere—usually within clouds—and then fall, accumulating on the ground where they undergo further changes. It consists of frozen crystalline water throughout its life cycle, starting when, under suitable conditions, the ice crystals form in the atmosphere, increase to millimeter size, precipitate and accumulate on surfaces, then metamorphose in place, and ultimately melt, slide or sublimate away. Snowstorms organize and develop by feeding on sources of atmospheric moisture and cold air. Snowflakes nucleate around particles in the atmosphere by attracting supercooled water droplets, which freeze in hexagonal-shaped crystals. Snowflakes take on a variety of shapes, basic among these are platelets, needles, columns and rime. As snow accumulates into a snowpack, it may blow into drifts. Over time, accumulated snow metamorphoses, by sintering, sublimation and freeze-thaw. Where the climate is co ...
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Precipitation (meteorology)
In meteorology, precipitation is any product of the condensation of atmospheric water vapor that falls under gravitational pull from clouds. The main forms of precipitation include drizzle, rain, sleet, snow, ice pellets, graupel and hail. Precipitation occurs when a portion of the atmosphere becomes saturated with water vapor (reaching 100% relative humidity), so that the water condenses and "precipitates" or falls. Thus, fog and mist are not precipitation but colloids, because the water vapor does not condense sufficiently to precipitate. Two processes, possibly acting together, can lead to air becoming saturated: cooling the air or adding water vapor to the air. Precipitation forms as smaller droplets coalesce via collision with other rain drops or ice crystals within a cloud. Short, intense periods of rain in scattered locations are called showers. Moisture that is lifted or otherwise forced to rise over a layer of sub-freezing air at the surface may be condense ...
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Frost
Frost is a thin layer of ice on a solid surface, which forms from water vapor in an above-freezing atmosphere coming in contact with a solid surface whose temperature is below freezing, and resulting in a phase change from water vapor (a gas) to ice (a solid) as the water vapor reaches the freezing point. In temperate climates, it most commonly appears on surfaces near the ground as fragile white crystals; in cold climates, it occurs in a greater variety of forms. The propagation of crystal formation occurs by the process of nucleation. The ice crystals of frost form as the result of fractal process development. The depth of frost crystals varies depending on the amount of time they have been accumulating, and the concentration of the water vapor (humidity). Frost crystals may be invisible (black), clear (translucent), or white; if a mass of frost crystals scatters light in all directions, the coating of frost appears white. Types of frost include crystalline frost (hoar fro ...
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Winter
Winter is the coldest season of the year in polar and temperate climates. It occurs after autumn and before spring. The tilt of Earth's axis causes seasons; winter occurs when a hemisphere is oriented away from the Sun. Different cultures define different dates as the start of winter, and some use a definition based on weather. When it is winter in the Northern Hemisphere, it is summer in the Southern Hemisphere, and vice versa. In many regions, winter brings snow and freezing temperatures. The moment of winter solstice is when the Sun's elevation with respect to the North or South Pole is at its most negative value; that is, the Sun is at its farthest below the horizon as measured from the pole. The day on which this occurs has the shortest day and the longest night, with day length increasing and night length decreasing as the season progresses after the solstice. The earliest sunset and latest sunrise dates outside the polar regions differ from the date of the winte ...
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Summer
Summer is the hottest of the four temperate seasons, occurring after spring and before autumn. At or centred on the summer solstice, the earliest sunrise and latest sunset occurs, daylight hours are longest and dark hours are shortest, with day length decreasing as the season progresses after the solstice. The date of the beginning of summer varies according to climate, tradition, and culture. When it is summer in the Northern Hemisphere, it is winter in the Southern Hemisphere, and vice versa. Timing From an astronomical view, the equinoxes and solstices would be the middle of the respective seasons, but sometimes astronomical summer is defined as starting at the solstice, the time of maximal insolation, often identified with the 21st day of June or December. By solar reckoning, summer instead starts on May Day and the summer solstice is Midsummer. A variable seasonal lag means that the meteorological centre of the season, which is based on average temperature pattern ...
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Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indi ...
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Oceanic Climate
An oceanic climate, also known as a marine climate, is the humid temperate climate sub-type in Köppen classification ''Cfb'', typical of west coasts in higher middle latitudes of continents, generally featuring cool summers and mild winters (for their latitude), with a relatively narrow annual temperature range and few extremes of temperature. Oceanic climates can be found in both hemispheres generally between 45 and 63 latitude, most notably in northwestern Europe, northwestern America, as well as New Zealand. Precipitation Locations with oceanic climates tend to feature frequent cloudy conditions with precipitation, low hanging clouds, and frequent fronts and storms. Thunderstorms are normally few, since strong daytime heating and hot and cold air masses meet infrequently in the region. In most areas with an oceanic climate, precipitation comes in the form of rain for the majority of the year. However, some areas with this climate see some snowfall annually during winter. M ...
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