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oai:uvadoc.uva.es:10324/410192021-06-23T10:28:39Zcom_10324_1161com_10324_931com_10324_894col_10324_1318

González Gutiérrez, Rosa Blanca 4c0beae9-7f5e-4614-9822-bf84b0ecace0 500 Santos González, Javier 5dc8ab42-dd3a-4b02-96e1-48c23a844a1e 500 Gómez Villar, Amelia b5206e3d-b1e1-4194-b113-3b551cf7ee1b 500 Alonso Herrero, Eduardo 3dc5a370-0908-47b4-8517-2c7c5f996e77 500 García de Celis, Alipio José b8d0423feca5323e 500 0000-0003-3314-3166 Cano, Martín 9b5bf61e-4549-4b99-a23a-b65ed54c5741 500 Redondo Vega, José María d1091ba2-a0ab-4987-878f-ed1a38af4429 500 2020-06-09T18:52:35Z 2020-06-09T18:52:35Z 2017 Acta Carsologica, 2017, vol. 46, n. 2-3. p. 165–178 1580-2612 http://uvadoc.uva.es/handle/10324/41019 10.3986/ac.v46i2-3.5001 Producción Científica Landforms resulting from the interaction between paleo-glaciers and karst are studied by using the Sierra de los Grajos (Cantabrian Mountains) as a model. This area contains glacial landforms that have not interested geomorphologists due to their low altitude (Peña Castillo is about 1857 m a.s.l.), the absence of glacial cirques and the scarcity of large moraines. However, the prevalence of groundwater flow and chemical dissolution has favoured the preservation of glacial landforms. Lateral and frontal moraines show three main glacial stages and other minor glacier stabilization phases, with the paleo-ELA oscillating between 1650 and 1760 m. Moraines are combined with depressions and sinks resulting from subglacial karstic drainage. This convergence of forms and processes is an exception in the Cantabrian Mountains, where postglacial erosion has usually eroded the frontal moraines and the proglacial sediments. In the case of the Sierra de los Grajos, despite the underground drainage and preservation of many glacial deposits on karstic landforms, an outwash-plain was formed. These proglacial sediments and others from non-karstified areas filled the depressions of the preglacial terrain located at their edges. The main glaciokarstic landforms have been mapped and a sedimentological analysis of the outwash plain was made in order to reconstruct the glacial dynamics of this area. Ministerio de Economía, Industria y Competitividad - Fondo Europeo de Desarrollo Regional (projects CGL2016-76215-R and CGL2015-65569-R) application/pdf eng Slovenian Academy of Sciences and Arts info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by-nc-nd/4.0/ © 2017 Slovenian Academy of Sciences and Arts Attribution-NonCommercial-NoDerivatives 4.0 Internacional Glacial geomorphology Geomorfología glaciar Karst geomorphology Geomorfología kárstica Cantabrian Mountains Cordillera Cantábrica 2506.07 Geomorfología 54 Geografía Glaciokarst landforms in the Sierra de los Grajos, Babia and Luna natural park (Cantabrian Mountains, NW Spain) info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion https://ojs.zrc-sazu.si/carsologica/article/view/5001 SI THUMBNAIL Glaciokarst-landforms.pdf.jpg Glaciokarst-landforms.pdf.jpg IM Thumbnail image/jpeg 3431 https://uvadoc.uva.es/bitstream/10324/41019/4/Glaciokarst-landforms.pdf.jpg 28fe01234839572f1396a6e9b891c6e9 MD5 4 LICENSE license.txt license.txt text/plain 3926 https://uvadoc.uva.es/bitstream/10324/41019/3/license.txt 017313583e37a1e4d1253e1ef6c66c6c MD5 3 CC-LICENSE license_rdf license_rdf application/rdf+xml; charset=utf-8 817 https://uvadoc.uva.es/bitstream/10324/41019/2/license_rdf 975848b171c53b753f7e445c8b5bc0e1 MD5 2 ORIGINAL Glaciokarst-landforms.pdf Glaciokarst-landforms.pdf application/pdf 2789063 https://uvadoc.uva.es/bitstream/10324/41019/1/Glaciokarst-landforms.pdf d8f376ec2ff27d55b6190b7fc7e993c1 MD5 1 10324/41019 oai:uvadoc.uva.es:10324/41019 2021-06-23 12:28:39.438 UVaDOC repositorio@uva.es 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