Steekaul Burermillen – a former sandstone quarry
The oldest rocks in the region can be observed: red sandstones from the Lower Triassic (Buntsandstein) period. The red colour is due to oxidyzed iron concentrations in the rock. These older sandstones are outcropping at the surface in this area because the geological strata buckles here upwards and forms an arch-like structure, the “Born saddle”. […]
The oldest rocks in the region can be observed: red sandstones from the Lower Triassic (Buntsandstein) period. The red colour is due to oxidyzed iron concentrations in the rock. These…
The oldest rocks in the region can be observed: red sandstones from the Lower Triassic (Buntsandstein) period. The red colour…