RT Journal Article
T1 Las arenas eólicas del Pleistoceno Superior en Gibraltar
T1 Late Pleistocene windblown sand record in the Rock of Gibraltar
A1 Rodríguez Vidal, Joaquín
A1 Cáceres Puro, Luis Miguel
A1 Ruiz Muñoz, Francisco
A1 Abad de los Santos, Manuel
A1 Finlayson, Clive
A1 Finlayson, Geraldine
A1 Martínez Aguirre, Arancha
A1 Fa, Darren A.
AB During the period represented by the sandy infills of the eastern flank caves and the Catalan Sand formation, it was likely that Gibraltar was part of the mainland, including a broad coastal plain covered with transgressive wind-blown dunes. All aeolian formations originated on marine beaches, from 6 m a.s.l. to 100 m b.s.l., before being blown inland to accumulate as topographic dunes. CUff-front aeolian accumulations comprise echo dunes, climbing dunes and sand ramps. Aeolian deposition began immediately before the last interglacial marine highstand (MIS 6-5 transition) and continued during the subsequent fall in sea level until the end ofMIS 3
YR 2010
FD 2010
LK http://hdl.handle.net/10272/7895
UL http://hdl.handle.net/10272/7895
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026