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The ancient rockslide of the Peñón de Ocenilla (Sierra de Cabrejas, Iberian Range, Soria)

dc.contributor.authorSanz Pérez, Eugenio
dc.date.accessioned2014-03-11T13:48:57Z
dc.date.available2014-03-11T13:48:57Z
dc.date.issued2010
dc.identifier.urihttp://hdl.handle.net/10272/7857
dc.description.abstractA large-dimension rockslide occurred at one end of the 80 m high calcareous cliff face of the so-called Peñón de Ocenilla, where the inclination of the dip is 12° greater than the slope. A large mass of limestone and marly limestone slipped along the contact with the underlying marl deposits in a single, rapid displacement. The blocks were intensely fractured in this rockfall, producing an accumulation of 5x106 m3 coarse scree. Based on the Celtiberian ceramics found in the surface of the rockslide mass, the antiquity of the rockslide may have at least more than 2100 BP, possibly from the upper or middle Holocene, due to its relatively well preserved geomorphological characteristicsen_US
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherAncient translational rockslideen_US
dc.subject.otherPlane failureen_US
dc.subject.otherHoloceneen_US
dc.subject.otherIberian Rangeen_US
dc.titleEl antiguo deslizamiento rocoso del Peñón de Ocenilla (Sierra de Cabrejas, Cordillera Ibérica, Soria)en_US
dc.titleThe ancient rockslide of the Peñón de Ocenilla (Sierra de Cabrejas, Iberian Range, Soria)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess


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