Bridge Length
~15 meters
Spanning a fissure in the Mid-Atlantic Ridge lava field
Bridge Between Continents: Footbridge Across the Plate Rift
A symbolic footbridge on the Reykjanes peninsula spanning the rift between the North American and Eurasian tectonic plates on the Mid-Atlantic Ridge.
Checked September 10, 2026: Visit Reykjanes warns of new or reopened cracks near the bridge. Stay on marked paths and away from visible cracks and edges. This site-specific warning matters even when the bridge appears accessible.
Location
Reykjanes Peninsula
Sandvík • Near Keflavik Airport
Quick Answer
The Bridge Between Continents is a 15-meter footbridge from 2002 spanning a fissure between the North American and Eurasian plates on Iceland's Reykjanes peninsula.
The Bridge Between Continents (Brú milli heimsálfa) is a small footbridge on the Reykjanes peninsula in southwest Iceland that symbolically connects the North American and Eurasian tectonic plates. Built in 2002, the 15-meter bridge spans a fissure in the Leif the Lucky Bridge area at Sandvík, where the Mid-Atlantic Ridge rises above sea level. Iceland is one of the few places on Earth where the Mid-Atlantic Ridge is visible on land, and the Reykjanes peninsula has some of the most accessible examples of this plate boundary. The surrounding lava field, part of the Reykjanes UNESCO Global Geopark, is criss-crossed with fissures and rifts left by the tectonic forces shaping Iceland.
Sources and page update
Updated: 2026-09-10
This guide is a travel-planning summary, not emergency guidance. Conditions in Iceland can change quickly; check official alerts, roads, and weather before driving, hiking, or booking around volatile conditions.
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Official sources to check
Plate Drift
~2 cm/year
The North American and Eurasian plates are drifting apart
Access
Free, year-round
Short drive from Keflavik Airport on the Reykjanes peninsula
What to Expect
The Footbridge
A small metal bridge spanning a visible rift fissure; crossing it takes you, symbolically, from one continent to the other
Lava Field Landscape
Surrounding moss-covered lava fields criss-crossed with rifts and fissures from tectonic activity
Information Panels
Educational signs explaining plate tectonics, the Mid-Atlantic Ridge, and Iceland's geological formation
Crossing Certificate
Available at nearby visitor centers as a souvenir of your walk between continents
Reykjanes Geopark
Part of the UNESCO Global Geopark with numerous other geological attractions within a short drive
Coastal Views
The nearby coastline looks out on the Atlantic Ocean and the volcanic Reykjanes shoreline
Getting There
The Bridge Between Continents is located near Sandvík on the Reykjanes peninsula, about 20 minutes' drive south of Keflavik International Airport and roughly 50 minutes from Reykjavik. Take Route 41 from Keflavik toward Grindavík, then follow Route 425 south toward the coast. The bridge is signposted and has a small parking area. It is an easy stop on the way to or from the airport, or as part of a Reykjanes peninsula day trip.
Best Time to Visit
The Bridge Between Continents is accessible year-round and the visit takes only 15-30 minutes. The Reykjanes peninsula is exposed and windy, so dress warmly regardless of season. Summer has the longest daylight and the mildest weather for exploring the surrounding geopark. Gunnuhver hot springs, Reykjanesviti lighthouse, and the nearby coastline can round out a Reykjanes day trip. The site is rarely crowded as it is less visited than Golden Circle attractions.
Planning help
Bridge Between Continents FAQs
Quick answers with safety notes where it matters.
What is the Bridge Between Continents?
The Bridge Between Continents is a small footbridge on the Reykjanes peninsula that spans a fissure in the Mid-Atlantic Ridge, symbolically connecting the North American and Eurasian tectonic plates. Built in 2002, the 15-meter bridge sits in a lava field where the plates are visibly drifting apart.
Can I get a certificate for crossing the bridge?
Visit Reykjanes lists crossing certificates at the folk museum information centre in Garður and the Reykjanes Geopark visitor centre at Duus Cultural House. Check their current opening hours; do not expect a staffed certificate desk at the bridge itself.
Can you actually see the tectonic plates?
You can see the surface expression of the plate boundary: a fissure or rift in the lava field where the ground has cracked and separated as the plates drift apart. The actual plate boundary extends deep into the earth, but the surface fissures here are a visible result of the divergence, which occurs at about 2 cm per year.
What else is there to see on the Reykjanes peninsula?
The Reykjanes peninsula is rich in geological attractions. Nearby sites include the Gunnuhver hot springs (Iceland's largest mud pool), the Reykjanesviti lighthouse (Iceland's oldest), the Blue Lagoon, the Kleifarvatn lake, and the Krýsuvík geothermal area. The UNESCO Global Geopark area can fill a full day.
Country reference: Iceland statistics.