Earth and Environment Atlas

How The Planet Works
Sign In
Text size
100%
Theme
Geological Formation

Belogradchik Rocks

Erosional and Karst Formations

The Belogradchik Rocks are a group of strangely shaped sandstone and conglomerate formations on the western slopes of the Balkan Mountains near the town of Belogradchik in northwestern Bulgaria. The rocks range in colour from red to yellow, some rising as high as 200 metres, and many have taken on fantastic shapes that folk legend has named after the people or objects they resemble. Declared a Natural Landmark by the Bulgarian government, they are also the only known habitat of the critically endangered Bulgarian endemic plant Hieracium belogradcense. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

Facts
Classification
Protected Status
National Monument or Landmark 1
Connections

Caused By

Orogeny, Processes

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Belogradchik Rocks

In Discipline

Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Belogradchik Rocks
In the Other Atlases
Sources
1. Wikidata: Belogradchik Rocks
  • Wikidata Q3042478, class allow-list match (w-wdresolver-0926)
  • declared a Natural Landmark by the Bulgarian government
View the Source
Belogradchik Rocks (Wikipedia)
Lead section
Quote, Lead section
The Belogradchik Rocks (Bulgarian: Белоградчишки скали, Belogradchishki skali) are a group of strangely shaped sandstone and conglomerate rock formations located on the western slopes of the Balkan Mountains (Stara Planina) near the town of Belogradchik in northwest Bulgaria.
View the Source
Comments (0)
No comments yet. Be the first to share a thought.
Reader Challenges (0)
No disputes yet. Spotted an error or a better source? Open the first one.