Dynamic geomorphology of the coast of La Araucania

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dc.contributor.authorPena Cortes, Fernando
dc.contributor.authorLimpert, Carlos
dc.contributor.authorAndrade, Elias
dc.contributor.authorHauenstein Barra, Enrique
dc.contributor.authorTapia, Jaime
dc.contributor.authorBertran, Carlos
dc.contributor.authorVargas Chacoff, Luis
dc.date2014
dc.date.accessioned2021-04-30T16:47:49Z
dc.date.available2021-04-30T16:47:49Z
dc.description.abstractThis paper describes the geomorphology of the coast of La Araucania, using methods proposed by Tricart (1985) End licher (1985) and the classification methods of Francke et al. (2004). Based on morphological, morphometric, morphogenetic and land use patterns, the most representative geomorphic units were the mountain range of metamorphic rock, cord metamorphic rock mountain with granite intrusions, both Paleozoic, the metamorphic rock platform and the fluvial-marine plain represented by wetlands of high ecological value. Water erosion was low to moderate in much of the study area and is mainly associated with human factors, such as the historic reduction and change in vegetation cover, poor agricultural practices and almost no application of soil conservation practices.
dc.identifier.citationREVISTA DE GEOGRAFIA NORTE GRANDE,Vol.,241-260,2014
dc.identifier.urihttp://repositoriodigital.uct.cl/handle/10925/3556
dc.language.isoes
dc.publisherPONTIFICA UNIV CATOLICA CHILE. INST GEOGRAFIA
dc.sourceREVISTA DE GEOGRAFIA NORTE GRANDE
dc.subject.englishCoastal geomorphology
dc.subject.englishhydric erosion
dc.subject.englishgeomorphological units
dc.subject.englishmorphometric
dc.subject.englishmorphogenesis and cultural landscape
dc.titleDynamic geomorphology of the coast of La Araucania
dc.typeArticle
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uct.indizacionSCI
uct.indizacionSSCI
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