The sandstone rocks here are part of the broader Holy Cross Mountains geological region.
The site is legally protected as a document of the area's paleogeographic past.
The specific sediment structures visible are indicative of river-channel deposits from the Triassic period.
Plac Pod Skałkami is a protected geological site in Starachowice known for its significant exposures of Triassic sandstones. The site features distinct rock formations that serve as a testament to the region's ancient geological history. These red and multicolored sandstones belong to the Buntsandstein formation, dating back approximately 250 million years. The area is integrated into the urban landscape, providing a rare look at natural monuments preserved within a city environment. It functions as an open-air educational site for geology enthusiasts and local residents. Visitors can observe clear stratification within the exposed rock faces.
From the elevated path looking directly at the main exposed sandstone face to capture the full scale of the stratification.
Bring a sturdy pair of shoes with good grip as the terrain near the base of the rocks can be uneven.
Visit after a light rain to make the distinct colors and layers of the sandstone stand out more vividly.
Carry a magnifying glass to inspect the texture and mineral composition of the exposed rock faces.
Do not attempt to collect rock samples, as the site is under legal protection.
Do not climb on the protected rock formations, as they are fragile geological monuments.
