We continue our way to the Bridge Between Continents, a symbolic bridge over a fissure between the North American and Eurasian tectonic plates. With the Mid- 

To the north and south, the ridge lies beneath some 2500m of water, forming a rift that separates the North American plate from the Eurasian plate. The rift spreads apart at a rate of some 2.5 cm/year, forming new oceanic lithosphere in the process. But in Iceland, you can actually walk around in it!

Sep 26,  · Summary Author: Sue Strickland. Slicing through the center of Iceland is the Mid-Atlantic Ridge. This is the boundary between the North American and Eurasian tectonic plates. Tectonic plates are the enormous slabs that make up the earth's crust. The North American and Eurasian plates are slowly separating, at a rate of about three millimeters

It's an important location on the planet: when you swim into the mid-Atlantic ridge, you're actually swimming into the rift that separates 

After the volcano hike, we stop by the bridge between continents, where you can walk between the continental plates that divide the peninsula.

Filled with pure glacier water, Silfra is the only place on Earth where divers can touch two continental plates at once.

Reykjanes peninsula is located directly on the Mid-Atlantic Ridge where the Eurasian and North American tectonic plates are moving apart. Iceland is the only place where the ridge is visible on land and it is possible to walk between the two tectonic plates.

Iceland is the only place where the ridge is visible on land and it is possible to walk between the two tectonic plates. Miðlína or The Bridge Between Continents is located at Sandvík and there you can walk from Europe to North America in only few seconds but the bridge was actually built as a symbol for the connection between Europe and

The Mid-Atlantic Ridge that crosses Iceland is an impressive rift between active continental plates. The ridge is the meeting-point of the North American and Eurasian plates and the Leif the Lucky Bridge, or the Bridge Between Continents, acts to symbolically connect the two land masses while treating visitors to a stunning view of the rift

Iceland is the only place in the world that you can walk between two tectonic plates (there are a few other places in the country that you can do this as well). This is a pretty cool spot, and the bridge connecting both of the plates is a pretty neat concept. Worth going if

The rate of spreading along the Mid-Atlantic Ridge averages about 2.5 centimeters (1 inch) per year, or 25 kilometers (15.5 miles) in a million years. As you can see on the maps above the earthquakes occur directly along the boundary between the plates. The map to the right shows earthquakes that have been recorded in the last 48 hours.

Thingvellir is a favorite stop among travelers along the Golden Circle route. It has been a National Park in Iceland since 1930 and became a UNESCO World Heritage site in 2004. When Viking settlers arrived in the 10th century, it was their chosen site for Althingi, the world’s oldest Parliament. Thingvellir’s unique geology created a

The reason for this seismic activity is Iceland's location right on the divergent boundary between the Eurasian plate and the North American 

The Bridge between Continents (or Midlina) is a 15 meter (50 ft) footbridge in the Reykjanes Peninsula spanning a gaping rift between the Eurasian and North American tectonic plates. The lava-scarred Reykjanes Peninsula lies directly on the Mid Atlantic Ridge.

Walking on the Mid-Atlantic Ridge in Iceland Sarah Masters. Iceland lies on the ridge. Iceland lies on the northern part of the Mid-Atlantic Ridge. It has formed over both the ridge and a hot spot. Iceland on the western side is part of the North American Plane and on the eastern side lies the Eurasian Plate. The Thingvellir Rift Valley on

Why is Iceland a portion of the mid-ocean ridge? Iceland represents the largest portion of the MAR exposed above sea level. Formed from volcanic eruptions on the Mid-Atlantic Ridge, about 24 million years ago, it is one of the few places where you can stand on the ridge on dry land.This makes Iceland very special and a popular place for geologists and scientists.

Most tectonic plate boundaries are found under the ocean, there are only two spots on earth where they can be seen from land: Iceland and East 

The other two plates are the African Plate and the South American Plate. How was Iceland created and is it still growing? celand was created by the lava oozing out of the mid atlantic ridge and it is still growing about 40 cm every two weeks. Earthquakes happen at transform boundaries. Iceland has earthquakes.

Mid-Atlantic Ridge. Mid-Atlantic Ridge Underwater topographic feature along the margin between the diverging American crustal plate on one side and the European and African plates on the other. It runs for 14,000km (8700mi) along the middle of the Atlantic Ocean. Iceland is located on the ridge itself, and was formed by the outpourings of

Iceland is located mostly south of the Arctic Circle in the North Atlantic Ocean, less than 200 miles across the Denmark Strait from the coast of Greenland. Iceland has a unique geological location on top of the mid-Atlantic Ridge, a divergent plate boundary between the North American Plate and the Eurasian Plate.

While most of this happens deep on the ocean floor, in Iceland, the ridge—a major tectonic plate boundary that sits between the North American 

Iceland is a place where a mid-ocean ridge can be seen on land What's more, Iceland is probably the only place in the world where the effects of two major 

The valley in between, in which Þingvellir is contained, is the rift valley. You are welcome to walk alongside both of these plates. One of the park's most pleasant walks takes you between the edge of the North-American plate and an old part of the wall that collapsed away; this is called the Almannagjá gorge.

Where is the Mid-Atlantic Ridge above sea level? The average depth to the crest (top) of the ridge is 2500 m, but it rises above sea-level in Iceland and is more than 4000 m deep in the Cayman Trough. Mid-ocean ridges are geologically important because they occur along the kind of plate boundary where new ocean floor is created as the plates spread apart.

The ridge is where two tectonic plates meet and seem to be in agreement to drift apart. And here you can walk between the two tectonic plates on a bridge 

Whether you are aware that Iceland is located directly on top of the Mid-Atlantic ridge or not, the Reykjanes Peninsula is one place you won't want to skip 

If the weather is nice when arriving Keflavik you should invest in a 15 minutes drive to the Bridge Between Continents near , south-west of the 

The ocean ridge rises up to between 4 km above the ocean floor. a rift valley at its crest marks the location at which the two plates are moving apart - hotter, less dense and more buoyant crust

Why is Iceland a portion of the mid-ocean ridge? Iceland represents the largest portion of the MAR exposed above sea level. Formed from volcanic eruptions on the Mid-Atlantic Ridge, about 24 million years ago, it is one of the few places where you can stand on the ridge on dry land.This makes Iceland very special and a popular place for geologists and scientists.

This place, lava-scarred Reykjanes peninsula is located over the world's major plate boundaries, the Mid Atlantic Ridge. Going by the Eurasian and North 

In the UNESCO World Heritage Site of Thingvellir in Iceland, there's a crack between two tectonic plates, filled with crystal clear glacial