Relict slopes and palaeovalleys at Taracena-Guadalajara (central Spain): Geomorphological and palaeogeographical interpretation

Abstract

Relict talus are of great interest for the reconstruction of Quaternary paleoenvironments. In this study, a special type of talus developed in the central zone of the Iberian Peninsula is analyzed, which we will refer to as talus-palaeovalley alignments. They constitute talus sequences that conserve the intermediate paleovalleys, arranged in parallel alignments, and separated by the tributary streams of the Henares River. This special arrangement could explain the accelerated transformation of the Pleistocene talus, with very much higher scarp retreat rates than those recorded in the bibliography. The chronologies obtained through OSL in some of the six differentiated stages (S1-S6) are placed in relation with various climatic reconstructions of the Pleistocene and, especially with the glacial phases of the Pyrenees, with which they show good temporal correlations. A further two stages of talus flatirons (S7 and S8) were recorded, which developed during the Holocene, both at the foot of older talus. Independent accumulations also formed at the foot of the main scarps (Muela de Alarilla and Valdenoches). The chronology provided by archaeological remains and radiocarbon dating placed their formation in the Iron Age Cold Epoch and the Little Ice Age (LIA), respectively.