The arid zones
237
Figure 10.6. Aeolian deposits fossilised by Lower Pleistocene detrital material. Escorihuela (province of
Teruel), northwards of the Semifosa of Teruel. East-central Iberian chain, Spain.
Africa (Fig. 10.7). These large flats are erosion surfaces of diverse ages (Fig. 10.8) or wide
alluvial plans of endorheic basins, such as those of the Lake Chad south of the Sahara; also
they are associated with landscapes modeled by the wind, which include regs, fields of
Figure 10.7. Fault escarpment in the central sector of the Dead Sea rift-valley, Israel.
237
Figure 10.6. Aeolian deposits fossilised by Lower Pleistocene detrital material. Escorihuela (province of
Teruel), northwards of the Semifosa of Teruel. East-central Iberian chain, Spain.
Africa (Fig. 10.7). These large flats are erosion surfaces of diverse ages (Fig. 10.8) or wide
alluvial plans of endorheic basins, such as those of the Lake Chad south of the Sahara; also
they are associated with landscapes modeled by the wind, which include regs, fields of
Figure 10.7. Fault escarpment in the central sector of the Dead Sea rift-valley, Israel.