Mittelquartäre Klimaverhältnisse und Reliefentwicklung im semiariden Becken von Vera (Südostspanien)

Gerd Wenzens
In the northern part of the Vera basin the oldest quaternary forms are alluvial fans and glacis plains near the base of the mountains. Travertine layers at their bottom are dated by ESR as approximately 1.6 mio years old. A revival of tectonic activities in the transition zone between basin and mountains during the early quaternary caused a period of intense erosion so that today there appear only small relics of the glacis which once...