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The Soatá Formation (Spanish: Formación Soatá) is a geological formation of the northern Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The formation consists mainly of shales with conglomerates and dates to the Quaternary period; Late Pleistocene epoch. The heavily eroded formation has a maximum measured thickness of 30.8 metres (101 ft). It contains the lacustrine and fluvio-glacial sediments of elongated paleolake , that existed on the Altiplano in the valley of the Chicamocha River.

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dbo:abstract
  • The Soatá Formation (Spanish: Formación Soatá) is a geological formation of the northern Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The formation consists mainly of shales with conglomerates and dates to the Quaternary period; Late Pleistocene epoch. The heavily eroded formation has a maximum measured thickness of 30.8 metres (101 ft). It contains the lacustrine and fluvio-glacial sediments of elongated paleolake , that existed on the Altiplano in the valley of the Chicamocha River. Fossils of the gomphothere Haplomastodon waringi, the capibara Neochoerus sp. and the deer species have been found in the Soatá Formation. Knowledge about the formation has been provided by Colombian geologists Carlos Villarroel, Jorge Brieva and others. (en)
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  • Type locality of the Soatá Formation to the northeast of the Altiplano Cundiboyacense. The Chicamocha River valley is clearly visible. (en)
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  • Portugalete, Soatá (en)
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  • Paleogeography of the Pleistocene (en)
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  • Soatá Formation (en)
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  • Villarroel et al. (en)
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  • Pleistocene (en)
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  • Holocene sediments of the Chicamocha River (en)
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  • The Soatá Formation (Spanish: Formación Soatá) is a geological formation of the northern Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The formation consists mainly of shales with conglomerates and dates to the Quaternary period; Late Pleistocene epoch. The heavily eroded formation has a maximum measured thickness of 30.8 metres (101 ft). It contains the lacustrine and fluvio-glacial sediments of elongated paleolake , that existed on the Altiplano in the valley of the Chicamocha River. (en)
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  • Soatá Formation (en)
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