Bridge between Europe and North America on Reykjanes Peninsula.
The lava-scarred Reykjanes peninsula lies on one of the world's major plate boundaries, the Mid Atlantic Ridge. According to the continental drift theory the Eurasian and North American tectonic plates are continuously drifting apart with great forces under the gaping rifts. As the plates diverge, linear fractures, known as fissures form due to stresses created by the tension that builds up as the plates move away from each other.
The Bridge between two continents at Sandvík is a small footbridge over a major fissure which provides clear evidence of the presence of a diverging plate margin. The bridge was built as a symbol for the connection between Europe and North America.
One can cross the continental divide on Leif the Lucky's Bridge.
The gap widening occurs at a rate of 2 cm per year, part of Iceland is closer to North America, while the second part is closer to Europe