Obernkirchen sandstone

Obernkirchen sandstone is a naturally occurring sandstone formation in Lower Saxony composed of nearly pure quartz material. The stone displays a range of warm tones from pale yellow to deep red depending on its layer depth.

Quarrying of this sandstone began around the 11th century and became important for building projects across northern Germany and beyond. The stone was transported to many European locations where it was used in major structures.

The sandstone formation contains dinosaur tracks and fossils from the Early Cretaceous period, making it valuable for paleontological research.

This stone resists weathering extremely well and works for both indoor and outdoor use. It requires minimal maintenance and retains its appearance over many years of exposure.

The stone layers contain thin coal bands and dinosaur tracks from the Early Cretaceous period. These features reveal clues about an ancient sandy ecosystem that existed millions of years ago.

GPS coordinates: 52.30000,9.10000

Latest update: December 10, 2025 20:10