
The Rüdersdorf Museum Park combines an open-air museum, nature reserve, and active quarry on around 17 hectares. Here you can experience over 750 years of limestone mining history, which was crucial for the construction of many buildings in Berlin. Limestone mining in Rüdersdorf began as early as the 13th century by Cistercian monks. A confirmed date is 1254, when limestone from Rüdersdorf was used to build a Dominican monastery. Over the centuries, the site developed into one of the most important sources of building materials in the region. Lime from Rüdersdorf was used for well-known Berlin buildings, including large historic structures in the city.
In the 18th century, Prussia modernized mining significantly. Two mining reformers, Friedrich Anton von Heinitz and Friedrich Wilhelm Graf von Reden, were particularly important. They improved transport routes and production techniques and made Rüdersdorf an important industrial center in Prussia. In order to transport the stone more quickly, canals were even built directly into the quarry so that ships could collect the material.

In the 19th century, the town developed into a large industrial complex: quicklime was produced, and later cement production was added. Large kilns and factories were built, and the site was connected to the railway and other industrial facilities. From 1870 onwards, mining was even carried out below the water table, which was technically extremely challenging. After 1990, preservationists and citizens campaigned to preserve the historic industrial facilities. The museum park was opened in 1994 and developed into a large open-air museum.
The most famous facility is the shaft kiln, also known as the “cathedral of lime” – a huge 19th-century kiln hall where lime was burned. Today it serves as an exhibition and event venue. Right next to the park is a limestone quarry that is still in operation. Visitors can take guided tours of the quarry and learn how mining works today. This is a rare opportunity to observe industrial history and modern production at the same time. A geological feature: the limestone deposit was formed around 246–239 million years ago in the so-called Muschelkalk Sea of the Triassic period. In the otherwise sandy Berlin area, this limestone is a geological exception.