@article{10272/8389,
year = {2007},
url = {http://hdl.handle.net/10272/8389},
abstract = {The geomorphology, sedimentology and pedology of the most recent alluvial unit (360±101 to 216±89
14C cal BP) were studied in the Bardenas Reales Natural Park (Navarra province). This unit is either
infilling former narrow channel sections, currently showing a terrace morphology (e.g. El Vedado), or
insert on older morphopedosedimentary units with wide channel morphology (e.g. Salinero). It is
composed of a sequence of slacked flood depositional units, centimetric in scale, with weak degree of
soil development. The palaeoclimatic context is interpreted within a period of arid trend, characterised
by a high hydroclimatic variability, and increase in the frequency of floods during Little Ice Age. Alluvial
dynamics shows a high degree of geomorphic effectiveness as well as a very quick response to centennial
scale climatic variability},
title = {Actividad aluvial durante la Pequeña Edad del Hielo en Bardenas Reales de Navarra},
title = {Alluvial activity during Little Ice Age in Bardenas Reales of Navarra},
author = {Sancho, Carlos and Benito, Gerardo and Muñoz, Alicia and Peña, José Luis and Longares, Luis Alberto and McDonald, Eric and Rhodes, Edward and Saz, M. A.},
}