Die jungpleistozänen Äolianite in der südlichen Küstenzone von Israel: Ein Beitrag zur zeitlich-räumlichen Klimaentwicklung

Karl Brunnacker, Avraham Ronen & Wolfgang Tillmanns
Aeolian deposits appear between Gaza and Beer Sheva with near shore sand (Kurkar), landwards sandy clay-loess and finally clay-loess. According to the facial arrangement and the heavy mineral association the source of origin of the aeolian material was the coastal zone of the last glacial time. It has been drifted during the regression of the sea. Macro-morphologically very stable soils (Hamra) have been built during the transgression. This "Middle paleolithic soil complex" comprises the last...