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The Llanos (Spanish Los Llanos, "The Plains"; Spanish pronunciation: [los ˈʝanos]) is a vast tropical grassland plain situated to the east of the Andes in Colombia and Venezuela, in northwestern South America. It is an ecoregion of the tropical and subtropical grasslands, savannas, and shrublands biome.
The Llanos Basin (Spanish: Cuenca Llanos) or Eastern Llanos Basin (Spanish: Cuenca de los Llanos Orientales) is a major sedimentary basin of 96,000 square kilometres (37,000 sq mi) in northeastern Colombia.
The Orinoquía region is one of the six natural regions of Colombia that belongs to the Orinoco River watershed. It's also known colloquially as the Eastern Plains from the Spanish Llanos Orientales. The region covers most of the area of the departments of Arauca, Casanare, Meta, and Vichada. [1]
The joropo, a Llanero dance, has become the national dance of Venezuela, and of the Llanos of Colombia. While Llanero music is relatively unknown outside of Colombia and Venezuela, the musical groups Los Llaneros and Cimarrón have toured throughout the world.
Vichada department. Centro Las Gaviotas is an ecovillage located in the Llanos region of Colombia, in the department of Vichada.It was founded in 1971 by Paolo Lugari, who assembled a group of engineers and scientists in an attempt to create alternative and sustainable modes of living that were specifically adapted to the tropics in developing nations.
It is the most important commercial center in the Llanos Orientales (eastern plains) of Colombia. Villavicencio has a hot and very wet climate, with average daily temperatures ranging from 21 to 30 °C (70 to 86 °F) and an annual rainfall of around 4,500 millimetres or 180 inches. It is affectionately called "Villavo" la bella.
El Silbón (The Whistler) is a legendary figure in Colombia [citation needed] and Venezuela, associated especially with Los Llanos region, usually described as a lost soul. The legend arose in the middle of the 19th century.
This caused a segmentation of the current Magdalena Basins and the Llanos Basin to the east, previously part of a larger foreland basin to the east of the Central Ranges. [11] The León Formation in the Llanos Basin provides the first indication of the tectonic uplift of the Eastern Ranges, isolating the Llanos Basin from the Magdalena Valley. [12]
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