if you walk across the mid atlantic ridge in iceland you are traveling between

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

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!

The Mid-Atlantic Ridge has a major impact on Iceland, not only because the ridge divides the country in two, but also because the ridge is 

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.

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 and take home a personalised certificate at the Reykjanes information center and Reykjanes Geopark visitor center at Duus Cultural house . N63° 52' 5.558" W22° 40' 31.588". Get directions.

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 

The tectonic plates whose turbulent interactions formed Iceland are the Eurasian tectonic plate and the North American tectonic plate. Spanning the Mid-Atlantic Ridge Iceland emerged as a result of the divergent spreading boundary between these two plates and the activity of Iceland´s own hotspot or mantle plume. Is Iceland convergent or

The bridge is a bit of a gimmick because the rift it spans is at the northern edge of the Mid-Atlantic Ridge (which runs north-south under the Atlantic Ocean, but curves almost 90 degrees

The Mid-Atlantic Ridge Iceland is situated atop the divergent boundary called the Mid-Atlantic Ridge. The Ridge runs through the center of Iceland, and much tectonic activity occurs because two plates, the North American Plate and the Eurasian Plate, are pulling away from each other.

Jul 01,  · This video is about The Mid-Atlantic Ridge in Iceland(R)

The Mid-Atlantic Ridge is in effect an immensely long mountain chain extending for about 10,000 miles (16,000 km) in a curving path from the Arctic Ocean to near the southern tip of Africa. The ridge is equidistant between the continents on either side of it. The mountains forming the ridge reach a width of 1,000 miles.

The Mid Atlantic Ridge is an underwater mountain range that runs down the center of the Atlantic Ocean from a northern point near Iceland to a southern point near the Antarctic Peninsula. This

TIL that due to Iceland's location on the Mid-Atlantic Ridge between the North American and Eurasian Tectonic plates, the country it is technically part of both North America and Europe, and is the only place where you can walk between them.

The western side of the Eurasian and eastern side of the North American tectonic plates form the northernmost part of the Mid-Atlantic Ridge which Iceland is located on. In a sense, it can be said that Iceland is a kind of bridge between continents due to this unique location on the Mid-Atlantic Ridge.

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 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.

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.

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

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

The Mid-Atlantic Ridge (MAR) is known as a mid-ocean ridge, an underwater mountain system formed by plate tectonics. It is the result of a convergent plate boundary that runs from 87° N - about 333 km (207 mi) south of the North Pole - to 54 °S, just north of the coast of Antarctica.

Sep 02,  · The Silfra lava fissure at Thingvellir National Park is a spectacular underwater world where you can snorkel over the gorge which separates the Eurasian and

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.

The Mid-Atlantic Ridge is a submarine mountain range that extends north from Iceland to near the Antarctic Circle through the middle of the Atlantic. It separates the Atlantic Ocean into two large troughs each of which with a depth ranging from 12,100-18,000 ft (3,700-5,500 metres).

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 

Sep 30,  · Iceland –where you can walk a mid-Atlantic rift –and some other geology photos. While Iceland hosts an amazing variety of awesome landscapes, what stands out to me most

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

Iceland is home to the largest portion of exposed Mid-Atlantic Ridge in the world, and one of the only places where you can stand upon it on dry land.

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.

Iceland is one of the most unique places in the world because you can snorkel between two continental tectonic plates.

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, 

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