
Lake Valencia (Spanish language: ''Lago de Valencia'') is the second largest lake in Venezuela, exceeded in size only by Lake Maracaibo. It occupies one of the so-called Aragua valleys, enclosed between the parallel ranges of the Cordillera de la Costa, the Maritime Andes. Its surface is 405 m above sea level, is about 30 km long, has an area of 350 km2, and a catchment basin of 2,646 km², and lies partly in the state of Aragua. The maximum depth is 39 m, the mean depth 18 m. The lake has a number of small islands, some inhabited, and receives the waters of a score of small stream from the surrounding mountains. The lake is Endorheic lake, as the natural discharge level is at 427 m above sea level; the water level declined below this height about 250 years ago. It was formed approximately 2-3 million years ago due to faulting and subsequent damming of the Valencia River. The lake has been completely dry during several discrete periods of its geologic history. Since 1976 Lake Valencia water levels have risen due to diversion of water from neighboring watersheds—it currently acts as a reservoir for the surrounding urban centers (such as Maracay). The vivid green algal blooms present in this image result from a continual influx of untreated wastewater from the surrounding urban, agricultural, and industrial land uses. This contributes to ongoing eutrophication, contamination, and salinization of the lake. Despite its picturesque location between the Cordillera de la Costa to the north and the Serrania del Interior to the south, Lake Valencia’s poor water quality limits opportunities for tourism and recreational activities. Lakes of Venezuela
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Lake Valencia
Lake Valencia (Spanish language: ''Lago de Valencia'') is the second largest lake in Venezuela, exceeded in size only by Lake Maracaibo. It occupies one of the so-called Aragua valleys, enclosed between the parallel ranges of the Cordillera de la Costa, the Maritime Andes. Its surface is 405 m above sea level, is about 30 km long, has an area of 350 km2, and a catchment basin of 2,646 km², and lies partly in the state of Aragua. The maximum depth is 39 m, the mean depth 18 m. The lake has a number of small islands, some inhabited, and receives the waters of a score of small stream from the surrounding mountains. The lake is Endorheic lake, as the natural discharge level is at 427 m above sea level; the water level declined below this height about 250 years ago. It was formed approximately 2-3 million years ago due to faulting and subsequent damming of the Valencia River. The lake has been completely dry during several discrete periods of its geologic history. Since 1976 Lake Valencia water levels have risen due to diversion of water from neighboring watersheds—it currently acts as a reservoir for the surrounding urban centers (such as Maracay). The vivid green algal blooms present in this image result from a continual influx of untreated wastewater from the surrounding urban, agricultural, and industrial land uses. This contributes to ongoing eutrophication, contamination, and salinization of the lake. Despite its picturesque location between the Cordillera de la Costa to the north and the Serrania del Interior to the south, Lake Valencia’s poor water quality limits opportunities for tourism and recreational activities. Lakes of Venezuela
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