How did the Belogradchik Rocks form?

How did the Belogradchik Rocks form?

The Belogradchik Rocks are towering natural sculptures in Bulgaria, with peaks reaching up to 200 meters high.

Located in northwestern Bulgaria, these striking red sandstone formations were sculpted by wind and rain over millions of years. Their distinctive crimson color comes from iron oxide in the rock. The erosion has carved out recognizable shapes that resemble animals and people, including famous formations like 'The Schoolgirl' and 'The Bear'. These rocks began forming more than 230 million years ago and remain one of Bulgaria's most remarkable natural landmarks.
Nerd Mode
The Belogradchik Rocks are located in the Balkan Mountains of northwestern Bulgaria and cover an area of approximately 50 square kilometers. The geological process began during the Permian period, roughly 230 million years ago, when tectonic movements folded the Earth's crust. This activity created a vast basin that was eventually filled with sand, gravel, and clay, which compressed into thick layers of sandstone and conglomerate over millions of years.During the Triassic period, these layers were submerged under a shallow sea. The red tint seen today results from iron oxide minerals that oxidized when exposed to the atmosphere. As the sea receded and the region uplifted, the rocks underwent intense vertical fracturing. This created deep cracks that allowed water and wind to penetrate the stone and begin the long process of mechanical weathering.The unique shapes, such as 'The Madonna' and 'The Adam and Eve,' are the result of differential erosion. Softer layers of rock wore away faster than the harder, more resistant sections, leaving behind the tall, jagged pillars seen today. In 2009, the site gained international recognition when it was nominated as one of the New 7 Wonders of Nature. Today, it remains a primary geological site protected by the Bulgarian government for its scientific and historical value.
Verified Fact FP-0002777 · Feb 17, 2026

- Earth Science -

geology erosion nature Belogradchik
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