Lake Güija
Description
The lake is of volcanic origin and was formed by a large basaltic lava flow from Volcán de San Diego in the San Diego volcanic field which blocked the Güija depression's original drainage. Lake Güija is fed by the Ostúa, Angue and Cusmapa rivers and is drained on its southeastern side by the río Desagüe, a tributary of the río Lempa. The lake is surrounded by the volcanic cones of the Mita, San Diego and Cerro Quemado. The Salvadoran side of the lake has several small isles: Teotipa, Cerro de Tule and Iguatepec, where a substantial number of pre-Columbian céramics have been discovered since excavations started in 1924. Bosque San Diego La Barra lies on the eastern side of the lake.
World Heritage Status
This site was added to the UNESCO World Heritage Tentative List on September 21, 1992, in the Mixed (Cultural + Natural) category.
Important Bird Area
The lake and its surrounds has been designated an Important Bird Area (IBA) by BirdLife International because it supports significant populations of range-restricted birds, including white-bellied chachalacas, orange-fronted parakeets, Nutting's flycatchers and white-throated magpie-jays.
References
- ^ "Complejo Güija". Ramsar Sites Information Service. Retrieved 25 April 2018.
- ^ "Lago de Güija". CTPT (in Spanish). SICA. Archived from the original on 8 March 2009. Retrieved 15 July 2008.
- ^ Herrera, Néstor (2005). "Evaluación Ambiental del complejo Lago de Güija - Informe final" (PDF). MARN. Retrieved 15 July 2008.
- ^ "San Diego Volcano". GVP. Smithsonian Institution. Retrieved 18 July 2008.
- ^ Lake Guija - UNESCO World Heritage Centre
- ^ "Lake Güija". BirdLife Data Zone. BirdLife International. 2024. Retrieved 2024-09-18.
External links