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La Gran Sabana (Spanish pronunciation: [la ɣɾan saˈβana], English: The Great Savanna) is a region in southeastern Venezuela, part of the Guianan savanna ecoregion. The savanna spreads into the regions of the Guiana Highlands and south-east into Bolívar State , extending further to the borders with Brazil and Guyana . [ 1 ]
De Porta, J (1965), La posición estratigráfica de la fauna de Mamíferos del Pleistocene de la Sabana de Bogotá, Universidad Nacional de Colombia, pp. 37–54; De Porta, J (1960), Los equidos fósiles de la Sabana de Bogotá, Universidad Nacional de Colombia, pp. 51–78
A tree savanna at Tarangire National Park in Tanzania in East Africa A grass savanna at Kruger National Park in South Africa. A savanna or savannah is a mixed woodland-grassland (i.e. grassy woodland) biome and ecosystem characterised by the trees being sufficiently widely spaced so that the canopy does not close.
The 1938 Levantamiento de información geográfica de la comisión de la Gran Sabana (varios mapas) shows Tramen Tepui for first time and the American Geographical Society of USA (1940) map shows Tramen Tepui marked north of Ilu Tepui. Since then the name Tramen Tepui appears on many CVG-EDELCA, Otto Huber, IGVSB and Emilio Pérez maps.
Córdoba (Spanish: Humedal de Córdoba) is a wetland, part of the Wetlands of Bogotá in Bogotá, Colombia.It is situated on the Bogotá savanna in the locality Suba between the Avenida Boyacá and Avenida Córdoba and the streets Calle 127 and Calle 116, close to the TransMilenio stations Av. Suba Calle 116 and namesake station Humedal Córdoba. [1]
The Altiplano Cundiboyacense was formed late in the Andean orogenic phase. The Sabana Formation (Spanish: Formación Sabana, Q1 sa, QTs) is a geological formation of the Bogotá savanna, Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes.
Boletín de Antropología, Universidad de Antioquia. 28 (43): 124–156. ISSN 0120-2510; Pérez Preciado, Alfonso (2000). La estructura ecológica principal de la Sabana de Bogotá. Sociedad Geográfica de Colombia.
Other pollen and flora, as Ulmoideipites krempii, Carpolithus, Anemocardium margaritae, and Hickeycarpum peltatum have been found in the Bogotá Formation. [8] The abundant paleosols of the Bogotá Formation show an increase in chemical weathering across the Paleocene-Eocene (P-E) transition; the Paleocene–Eocene Thermal Maximum .