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- The Sabana Formation (Spanish: Formación Sabana, Q1sa, QTs) is a geological formation of the Bogotá savanna, Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The formation consists mainly of shales with at the edges of the Bogotá savanna lignites and sandstones. The Sabana Formation dates to the Quaternary period; Middle to Late Pleistocene epoch, and has a maximum thickness of 320 metres (1,050 ft), varying greatly across the savanna. It is the uppermost formation of the lacustrine and fluvio-glacial sediments of paleolake , that existed at the edge of the Eastern Hills until the latest Pleistocene. The uppermost sediments of the Sabana Formation were deposited during the Last Glacial Maximum, a time when the first humans populated the Bogotá savanna. These hunter-gatherers used the bones of the still extant Pleistocene megafauna as Haplomastodon waringi, Cuvieronius hyodon and Equus amerhippus lasallei, of which fossils have been found in the Sabana Formation. Knowledge about the formation has been provided by geologists Alberto Guerrero, Thomas van der Hammen and others. (en)
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- Altiplano Cundiboyacense .png (en)
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- The location of the capital of the New Kingdom of Granada Bogotá is different from its namesake, Bacatá (en)
- Main settlements of the Muisca Confederation on the Altiplano Cundiboyacense. (en)
- Type locality of the Sabana Formation on the Bogotá savanna (en)
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- Paleogeography of the Pleistocene (en)
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- Holocene unconsolidated sediments (en)
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- 4.717305555555556 -74.217
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- The Sabana Formation (Spanish: Formación Sabana, Q1sa, QTs) is a geological formation of the Bogotá savanna, Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The formation consists mainly of shales with at the edges of the Bogotá savanna lignites and sandstones. The Sabana Formation dates to the Quaternary period; Middle to Late Pleistocene epoch, and has a maximum thickness of 320 metres (1,050 ft), varying greatly across the savanna. It is the uppermost formation of the lacustrine and fluvio-glacial sediments of paleolake , that existed at the edge of the Eastern Hills until the latest Pleistocene. (en)
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