Pobiti Kamani — protected area
Diego Delso · CC BY-SA 4.0

Pobiti Kamani

  • 2 min read
  • 43.226° N 27.707° E

Interesting facts

  • Pobiti Kamani became the very first natural landmark officially protected by the Bulgarian state, in 1937.
  • Until 1942 the site was known by its Turkish name, Dikilitash, which also means 'planted stones'.
  • Viktor Teplyakov visited on 22 April 1829 during the Russo-Turkish war, measured the thinnest column at 1.35 m across and found it as hard as marble.
  • The pillars have no solid foundations; many are hollow and filled with sand, and some stand stacked in tiers up to about 5 metres high.
  • The calcite cementing the columns is strongly depleted in the heavy carbon isotope carbon-13, the chemical fingerprint of methane-eating microbes.
  • Fossils date the rock to the Lower Eocene, roughly 48.6 to 53 million years ago, and the sand around the pillars is strewn with shells.
  • Bulgarian surveys count up to 18 separate groups of pillars scattered over an area of about 50 square kilometres.
  • Finds made in the area are reported as the only evidence in Bulgaria of people living here in the Mesolithic.
  • In 2020 a photo of the stone forest, tinted red, went viral as a supposed NASA picture of Mars until fact-checkers exposed it.
  • The site is part of the Natura 2000 network, protecting Bulgaria's largest inland sand habitats with their specialised plants and animals.

Why it is worth it

Pobiti Kamani — "the beaten-in stones", often called the Stone Forest — is a field of natural stone columns scattered across the sandy hills west of Varna, in north-eastern Bulgaria. Hundreds of pillars stand in the sand like the trunks of a petrified wood — hence the popular name — many five to seven metres tall and anything from about thirty centimetres to three metres thick, rough and pitted, sometimes hollow inside. The formations are spread over a strip roughly 8 kilometres long and 3 wide, in several distinct groups; the main group, Dikilitash, alone holds more than 350 stones.

Their origin puzzled scientists for a long time. The Russian archaeologist Victor Teplyakov described them in 1829, and early theories ranged from petrified trees to coral growth to purely mechanical erosion. Current research reads them as the remains of an ancient seabed seep system: in the Lower Eocene, around 50 million years ago, methane-rich fluids rose through the sediments of a shallow sea, and microbes that fed on the gas cemented the sand around each rising plume into a tube. When the soft sand was later washed and blown away, the hardened tubes were left standing.

The groups have their own character. At Strashimirovo the stones stand in rows and swell in the middle, while elsewhere pillars lean together, break off or lie like fallen logs in the sand. The site has been protected as a natural landmark since the late 1930s, and in low evening light the whole place looks less like Bulgaria than like a small desert.

The geology is the astonishing story here: a fossil record of gas escaping from an ancient sea floor, now standing on dry land a short drive from the Black Sea coast.

Getting there

The main group lies about 18 km west of Varna on the old road toward Sofia; the listed nearest town, Asparuhovo, is about 16 km away. Varna Airport (VAR) is about 10 km away. The site is easiest to reach by car or taxi from Varna.

On these lists

From the encyclopaedia

Pobiti Kamani, tubular concretions formed around "rising methane-bearing fluid plumes", is a desert-like rock phenomenon located on the north west Varna Province border in Bulgaria.

Wikipedia · CC BY-SA 4.0

43.22639, 27.70667per Wikidata