Mapa topográfico Bischberg

Winds can shape landforms, via a variety of aeolian processes such as the formation of fertile soils, for example loess, and by erosion. Dust from large deserts can be moved great distances from its source region by the prevailing winds; winds that are accelerated by rough topography and associated with dust…

Altitude média: 284 m

Altitude média: 328 m

Altitude média: 305 m

Altitude média: 331 m

Altitude média: 300 m

Altitude média: 260 m

Altitude média: 484 m

Altitude média: 274 m