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Geological

Bridge Between Continents

Brúin milli heimsálfa

Region: Reykjanes PeninsulaCoordinates: 63.8683° N, 22.6754° W

A roughly 15-metre footbridge near Sandvík on the Reykjanes Peninsula, built in 2002 to span a fissure marking the boundary between the North American and Eurasian tectonic plates. The Reykjanes Peninsula sits directly on the Mid-Atlantic Ridge, and the plates here are drifting apart at an average rate of about 2 cm per year, in episodic bursts rather than continuously.

Plan the stop

Who it suits
All ages
Short, mostly flat walk suitable for all ages, though young children should be supervised near the tectonic fissure and any cracked ground.

Accessibility

Wheelchair · Partial
A paved/boardwalk path runs from the car park to the bridge and is passable for wheelchairs, though it has a slight incline and the remote site has no staff on hand; surface conditions can vary with weather and recent seismic ground cracking nearby.
Limited mobility · Partial
The walk is short, but wind, uneven ground near the fissure, and remote conditions can make it harder than an urban stop.
Sensory · Partial
A simple outdoor stop, but the site is exposed to strong wind and weather, and recent seismic cracking nearby can add visual and supervision stress.
Cognitive · Full
A single short route from parking to bridge with a clear landmark and simple return.

Why it matters

The bridge itself is a modern, purpose-built symbol of continental drift rather than a historic structure, but it sits within a landscape shaped by the same rifting that has produced Reykjanes's lava fields and fissures for millennia. Visitors who cross it can obtain a certificate confirming they "walked from Europe to America."

More photos

Sign at the Bridge Between Continents marking the mid-point between the two plates.

Sign at the Bridge Between Continents marking the mid-point between the two plates.

Photo by Reykholt, CC BY-SA 3.0

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