RT Journal Article
T1 El antiguo deslizamiento rocoso del Peñón de Ocenilla (Sierra de Cabrejas, Cordillera Ibérica, Soria)
T1 The ancient rockslide of the Peñón de Ocenilla (Sierra de Cabrejas, Iberian Range, Soria)
A1 Sanz Pérez, Eugenio
AB A 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 characteristics
YR 2010
FD 2010
LK http://hdl.handle.net/10272/7857
UL http://hdl.handle.net/10272/7857
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 31 may 2026