Güzelcehisar Lava Columns: An 80-Million-Year Story on the Bartın Coast
Designated as a natural monument, the Güzelcehisar Lava Columns in Bartın are a rare 80-million-year-old geological wonder formed by cooling volcanic lava along the Black Sea coast.
October 19, 2026
At first, you might think they were built by human hands. Standing side by side, the stone columns resemble the wall of an immense, forgotten structure. Then you notice the irregular lines and sections leaning in different directions.
The shapes before you at Güzelcehisar were formed by cooling volcanic rock.
With the sea moving beside them, their estimated age of 80 million years is difficult to grasp. You can see a wave and hear it break. Millions of years take a different kind of imagination.
Where Are the Güzelcehisar Lava Columns?
The Güzelcehisar Lava Columns stand at the western end of the beach in Güzelcehisar village, within Bartın’s central district. They are approximately 17 kilometres from Bartın city centre.
They are not in Amasra. If you want to visit both places during your trip, plan the journeys separately.
When you reach the shore, take in the surroundings before concentrating on the columns. Sand, sea, vegetation and dark rock all contribute to the scene.
Are They Really 80 Million Years Old?
The formations are described as approximately 80 million years old. Using “approximately” preserves the estimated nature of their geological age.
The landscape at the time should not be imagined as the beach you see today. These rocks originated through ancient volcanic processes; the present coastline emerged after a long history of geological change.
Distinguishing the age of the rock from the age of today’s coastal scenery is a useful first step in understanding the site.
How Does Lava Form Columns?
As lava cools and solidifies, it contracts. The resulting stresses can cause cracks to develop through the rock. Under suitable conditions, these fractures divide the rock into column-like sections.
This process, known as columnar jointing, creates the striking geometry at Güzelcehisar.
The columns did not rise separately and freeze into stone pillars. They formed as a larger mass of volcanic rock cooled and fractured.
Look again with that in mind. The boundaries between the columns become visible traces of the cooling process.
What Should You Look For?
Begin from a little distance. Follow the formations along the shore, noticing changes in height and direction.
Then choose a smaller section to study from a safe, accessible position. Look at how repeated lines sit alongside irregular breaks in the same rock face.
The contrasting textures are part of the appeal: the constantly changing water, the soft appearance of the sand and the sharp divisions in the rock. Try including several of these in a photograph rather than isolating the columns alone.
Give Yourself Time for Photographs
As the sunlight changes direction, shadows between the columns change too. A surface that looks flat from one angle may appear deeper and more divided in different light.
Before taking one photograph and leaving, move a little within the safe visitor area. Begin with a wide view of the coastline, then concentrate on the lines in the rock.
Climbing is unnecessary. Showing the formations within their surroundings can convey their scale more effectively than getting closer.
What Should You Know Before Visiting?
Check the weather and sea conditions. Keep away from the water’s edge in rough conditions, avoid wet rocks and follow the designated walking and viewing arrangements.
Do not remove pieces of stone or mark the surfaces. Let photographs and observations be what you take home.
Before leaving Güzelcehisar, look at the sea and columns together once more. A wave reaches the shore, breaks and is followed by another. Beside it, the lines left by an ancient cooling process remain in the rock.
💬 Comments (0)
Traveler comments are shown in their original language.
No comments yet. Be the first to share your experience.
💬 Want to join the discussion?
Log in or create an account to leave a comment.