About the exhibition
Since the Earth’s formation, the face of its surface has been constantly changing. One reason for this is plate tectonics, the structure of the Earth’s crust, which has repeatedly changed the position of the continents throughout the Earth’s history. Spectacular volcanic eruptions and devastating earthquakes are the consequences of these plate shifts. Volcanoes are not only signs of a dynamic Earth, but also provide insights into the depths of the Earth that would otherwise be inaccessible to research. Geological processes thus shape the entire surface of the Earth.
Rocks are the solid part of the Earth’s crust. Age determinations have shown that the oldest rocks were formed about 4.2 billion years ago. They are full of clues about the Earth’s geological past and are largely responsible for shaping our landscape. They consist of minerals that can form magnificent crystals under certain conditions. These crystals are formed from different elements depending on pressure and temperature.