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west-iceland · Iceland

Flosagjá Fissure

Flosagjá is a narrow fissure in Þingvellir National Park formed by the separation of the North American and Eurasian tectonic plates. The fissure is filled with cold, crystal-clear glacial water.

About Flosagjá Fissure

Flosagjá is a narrow fissure in Þingvellir National Park formed by the separation of the North American and Eurasian tectonic plates. The fissure is filled with cold, crystal-clear glacial water.

Did You Know?

  • Tectonic fissure at Þingvellir
  • Formed by continental drift
  • Filled with glacial water
  • Accessible via walking paths
  • Quieter alternative to Silfra

Tours Near Flosagjá Fissure

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About Flosagjá Fissure

Flosagjá is located in Þingvellir National Park, accessible via marked walking paths from the main parking area. The fissure is narrow and deep, with steep rocky walls. Visitors can walk along the edge and peer into the clear water. The site offers excellent photo opportunities and a tangible connection to Iceland's unique geology. Flosagjá is less visited than nearby Silfra (the famous diving fissure), making it a quieter spot to appreciate Þingvellir's tectonic wonders.

Story & Folklore

Flosagjá is one of several dramatic fissures at Þingvellir created by the ongoing movement of tectonic plates. The plates drift apart by about 2 cm per year, slowly tearing Iceland apart. The water in Flosagjá is glacier-fed and incredibly clear.

Why Visit

Stand between two continents at a dramatic tectonic fissure filled with crystal-clear water.

Did You Know?

Iceland is slowly being torn apart as the North American and Eurasian plates drift in opposite directions.

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