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Reykjanes Geopark - an island still being born

An island still being born
Reykjanes Geopark

The Mid-Atlantic ridge comes ashore on the Reykjanes peninsula.

The peninsula, with its diversity of volcanic and geothermal activity, is well suited to become a Geopark and is the only place in the world where the Mid-Atlantic Ridge is visible above sea level.  

The word geo is linked to the goddess Gaia, who was the personification of Earth in ancient Greek mythology. She was one of the primordial deities, the great mother of all, mother earth.

Reykjanes Geopark logo

The Reykjanes Peninsula lies on major plate boundaries along the Mid-Atlantic Ridge, part of the 65,000km mid-ocean ridge that encircles the earth like a seam of a baseball. Although 90% of this mountain range lies deep below the surface of the ocean, it rises above sea-level right here on the Reykjanes Peninsula, making this one of the only places on earth where it is visible.

It is home to many important geological formations, some of which are utterly unique, including numerous types of volcanoes in at least four separate volcanic zones, with hundreds of open fissures and faults.

The Reykjanes Peninsula is a continuation of the Mid-Atlantic Ridge, which rises from the sea at the very tip of the peninsula and diagonally crosses Iceland from the south-west to the north-east. You can read the area’s geological history several hundred thousand years back in time, although most of the strata are less than 100–200 thousand years old. The last series of eruptions on the Reykjanes Peninsula began around AD 1000 and ended 250 years later.

The landscape that makes up the peninsula is characterised by tuff mountains and hyaloclastite ridges that formed in subglacial eruptions, as well as several series of craters and other large shield volcanoes from more recent times. In many places, there are lava stacks that formed in fissure eruptions, when large volumes of lava flowed from craters in the faults. Eruptions in Reykjanes are rarely accompanied by ash except where the volcanic fissures opened underwater or in the sea.

Earthquakes are frequent due to the spreading of the plates and occur most commonly as earthquake swarms that can last for several years. Although most of these are minor, every so often they can be felt across the entire peninsula.

Reykjanes Peninsula is an aspiring Geopark applying for membership in the European Geopark network.

Educational experience

Reykjanes peninsula is the perfect place for educational experience.

The peninsula is used as an outdoor classroom when it comes to geological education and the visitor centers provide good facilities for further researches.

Attractions

The Reykjanes Peninsula is the home of an aspiring geopark.

The peninsula exists where the North Atlantic ridge rises from the ocean. Here you can find 100 different craters, caves and lava fields, a variety of bird life, astonishing cliffs, high geothermal activity, and black sand beaches. Below are a few selections of interesting geothermal hotspots and attractions located in this area. 
 
The peninsula is very accessable all year round and distances between places are not long as for example many places of interests are only a 5-20 minutes drive from the international airport. 

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    The Reykjanes Peninsula

    Towns & Villages

    Visitors to Iceland who arrive via Keflavik International Airport on the Reykjanes Peninsula may be somewhat surprised by the landscape that greets their eyes as they touch down in Iceland for the very first time. A seemingly endless, green-grey moss-topped lava field blankets the peninsula for as far as the eye can see, and it is this strange and rather other-worldly sight that is your first glimpse of the land of fire and ice. 

    Map Garđur Sandgerđi Reykjanesbćr Vogar Grindavík
    West Iceland Westfjords North Iceland East Iceland South Iceland Visit Reykjanes Capital Area

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