Cabana (ancient lake)
Lake Cabana is an ancient lake in the Altiplano.
The lake reached a water level of 3,900 metres (12,800 ft) over the central and northern Altiplano,[1] 90 metres (300 ft) above the current lake levels of Lake Titicaca.[2] The Capalla-Ulloma sill, which separates the Altiplano into a northern and southern basin,[3] did not exist at that time and it did not split up the Cabana lake body. It left deposits reaching thicknesses of 50 metres (160 ft) of thickness;[4] they have been found on the western and eastern sides of the basin.[2] Erosion platforms and terraces covered with gravels[5] and other wave cut structures are remnants of Lake Cabana.[6]
In 1984, this lake was named by a group of researchers
The lake existed about 1 million years ago. It was preceded by Lake Mataro and succeeded by
References
- ^ S2CID 56399697.
- ^ a b Wirrmann et al. 1992, p. 40.
- ^ Wirrmann et al. 1992, p. 10.
- ^ a b Wirrmann et al. 1992, p. 8.
- ^ Newell 1949, p. 91.
- ^ Newell 1949, p. 92.
- .
- ^ Lavenu, A.; Fornari, M.; Sebrier, M. (1984). "Existence de deux nouveaux izpisodes lacustres Quaternaires dans l'altiplano péruvo-bolivien" (PDF). Cah ORSTOM Sér Géol (in French). 15 (1): 107.
- ISBN 978-0-521-03168-4.
- )
- ^ Newell 1949, p. 82.
- ^ Newell 1949, p. 85.
- ^ Wirrmann et al. 1992, p. 12.
- PMID 22957159.
Sources
- Newell, Norman D. (1949). "Geology of the Lake Titicaca Region, Peru and Bolivia". GSA Memoirs. Geological Society of America Memoirs. Vol. 36. Geological Society of America. pp. 1–124. .
- Wirrmann, Denis; Ybert, Jean-Pierre; Mourguiart, Philippe; Ybert, J.-P. (1992-01-01). "Paleohydrology". In Dejoux, C.; Iltis, A. (eds.). Lake Titicaca. Monographiae Biologicae. Vol. 68. Springer Netherlands. pp. 40–62. ISBN 9789401050616.