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Reykjanes Route

Valahnúkamöl
High boulder ridge composed of well rounded stones. The ridge is about 420 m long, 80 m wide and 10 m high. The rounded stones are 1-3 feet thick. Created by powerful storms, high waves and surf. Located: On the tip of Reykjanes, next to cliff Valahnúkur. Take road 425.
Stóra-Sandvík
Stóra-Sandvík is a beautiful cove with black sand beach and grassy dunes. Located close to Bridge between Continents, it is the perfect stop while exploring the area.
Valahnúkur
Valahnúkur is composed of tuff layers, pillow lava and breccia. The mountain was formed in a single eruption and shows evidence of the different phases of the eruption. The tuff forms in explosive eruption, while the pillow lava forms when the lava erupts under water.
Reykjanes Lighthouse
The lightsignal height is 69 meters above sealevel but the actual height of the lighthouse is 26 metres. Reykjanes lighthouse also has a radio beacon with a correction signal. There is carved rock and concrete in the lighthouse. Architect Frederik Kjørboe and engineer Thorvald Krabbe designed the lighthouse.
Karlinn
Karlinn („The Man“) is a 50-60 m high seacliff, an eroded volcanic plug, which stands high and mighty just off the coast of Valahnúkur. Karlinn is popular spot with visitors and especially among photographers, as it is truly picturesque when the unremitting waves hit the rock.
Hafnaberg Sea Cliffs
Hafnarberg is very popular among hikers and bird watchers as various marine birds nest at the cliffs. A parkingplace is located 4 km from Hafnir on road 44 and from there is a marked path from the road to the cliffs.
Gunnuhver
The mud pools take form where steam from boiling geothermal reservoir water emanates and condenses and mixes with surface water. Accompanying gases such as carbon dioxide and hydrogen sulphide make the water acid. This causes alteration of the fresh lava rock to clay. Steaming of the ground at Reykjanes increased markedly as a consequence of a pressure drawdown in the geothermal reservoir upon the start of production from the reservoir in 2006.
Bridge Between Continents
The Bridge between two continents at Sandvík is a small footbridge over a major fissure which provides clear evidence of the presence of a diverging plate margin. The bridge was built as a symbol for the connection between Europe and North America.
Stampar
Two volcanic fissures lie from the sea onto land on the western side of Reykjanes and form a series of craters. These crater series have been named Stampar. The crater series are from two periods. This series lies in the SW-NE direction and follow thereby the most common fissure angle in Reykjanes.