The Lieth open pit in Schleswig-Holstein offers the opportunity to examine the interior of a salt dome. The dome consists of salt-bearing sedimentary rocks of the two Permian subunits, the Rotliegend and the Zechstein. The rocks ascended from a depth of at least six kilometres to the Earth’s surface. However, salty-tasting rocks are not encountered in the open pit, as the salt was dissolved by groundwater and transported away in solution. This process left behind an unconsolidated residue, the so-called “Liether limestone ash”, which, because of its use as fertiliser, was mined and thus generated the open pit. More information, the 3D model and impressions on www.digitalgeology.de .