Inselbergs near medellín

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dc.creatorGarcía, C.
dc.creatorHermelin, M.
dc.date.accessioned2021-03-26T21:28:27Z
dc.date.available2021-03-26T21:28:27Z
dc.date.issued2015-01-01
dc.description.abstractThe northernmost part of the Central Cordillera is characterized by plateaus stretching from 1900 to 2700 m a.s.l. which were formed by erosion before the uplift of the cordillera, their different altitudes is an evidence of the successive pulses which were separated by quiet periods. One of the results of these tranquil epochs was the appearance of bornhardts at different altitude. Carved during Miocene and Pliocene in the Antioquian Batholith, a granodiorite intrusive which crystallized in the Upper Cretaceous. Main inselbergs are the Peñol de Guatapé (1900 m s.a.l.) the Tabor Mount (1880 m a.s.l.) in San Carlos and the Peñol de Entrerrios (2300 m a.s.l.). © Springer International Publishing Switzerland 2016. All rights reserved.
dc.identifierhttps://eafit.fundanetsuite.com/Publicaciones/ProdCientif/PublicacionFrw.aspx?id=4952
dc.identifierhttps://www.scopus.com/inward/record.uri?eid=2-s2.0-84955089397&doi=10.1007%2f978-3-319-11800-0_12&partnerID=40&md5=41ef73a8e6c48513b0e667dfa87494d0
dc.identifier.urihttp://hdl.handle.net/10784/27306
dc.languageeng
dc.publisherSpringer International Publishing
dc.relationDOI;10.1007/978-3-319-11800-0_12
dc.relationSCOPUS;2-s2.0-84955089397
dc.rightsSpringer International Publishing
dc.sourceLandscapes and landforms of Colombia
dc.sourceISBN: 9783319118000
dc.subjectErosion surfaces; Granite landscape; Inselbergs
dc.titleInselbergs near medellín
dc.typeinfo:eu-repo/semantics/bookPart
dc.typeCapítulo de un Libro
dc.typeinfo:eu-repo/semantics/publishedVersion

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