Kalksteinbruch Salzgitter-Salder

The Kalksteinbruch Salzgitter-Salder is a limestone quarry in the Salder area with steep rock walls and various geological deposits. The walls display multiple layers that specialists and schools visit to study natural rock formations.

The quarry opened in 1885 and served for decades as a source of limestone for cement and iron production. Operations ended in 1992 when extraction at this site concluded.

The site shows geological layers that reveal how the earth was formed over millions of years. Visitors can observe these natural records in the exposed rock walls during guided visits.

The site is not open to the general public and visits require advance arrangements with the operators. Visitors should wear sturdy shoes and exercise caution as the terrain is steep and rocky.

Scientists recognize this location as an important point for comparing rock layers from different periods of earth history. This makes the site internationally significant for studying how the earth changed over time.

Location: Salder

GPS coordinates: 52.12449,10.32997

Latest update: December 14, 2025 13:06