Kirkjugólf: The Church Floor Basalt Pavement
Kirkjugólf shows the ends of basalt columns at ground level: a patchwork of stone polygons that resembles paving. Its name means “Church Floor,” but the pattern is natural.
How the floor formed
The regional tourism authority describes erosion when the sea covered this area. The exposed formation is about 80 square meters, and no building stood on it. Visit South Iceland’s Kirkjugólf record identifies it as a protected natural monument and provides a location map.
Which basalt stop fits your route?
Choose Kirkjugólf if you want to study the column pattern from above. For a different perspective, compare Dverghamrar’s upright columns and blocky upper rock. These are different forms to look for, rather than interchangeable photo stops.
Kirkjugólf lies a few hundred meters east of Kirkjubæjarklaustur. Combine the area with Systrafoss if you are already exploring the village. Follow the marked visitor access; a destination pin identifies the formation, not a guaranteed parking space or step-free route.
Planning help
Questions before you go
Quick answers with safety notes where it matters.
Was there a church at Kirkjugólf?
No. Visit South Iceland states that no church or other building stood on this natural basalt pavement. The name describes its resemblance to a floor.
How large is Kirkjugólf?
The exposed pavement covers about 80 square meters. It is a compact formation to examine from above, rather than a tall wall of columns.
Where is Kirkjugólf?
Visit South Iceland places the protected natural monument a few hundred meters east of Kirkjubæjarklaustur. Use the destination map linked above to locate the formation.
Compare Iceland’s basalt formations
Country reference: Iceland statistics.