Continental drift

 

In the summer of 2000, two severe earthquakes occurred in South Iceland. Though their source lay 40-50 kilometres southeast of Þingvellir, stones fell from the ravine walls and water splashed up from the rifts. The water in the Flosagjá rift, normally crystal clear, became so murky that you couldn't see the coins lying on the bottom. The earthquakes were a result of movement of the Eurasian and North-American plate boundaries that run through Iceland. In the south, the plates inch past each other, but at Þingvellir, they break apart and the land between subsides. Away from the plate boundaries the activity is fairly constant, about two centimetres a year, but, in the rift zones themselves, tensional stress accumulates during a long period and is then released in a burst of activity when fracture boundaries are reached. The most recent burst of activity swept over Þingvellir in spring 1789.

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Iceland owes its existence to a mantle plume that produces twice as much volcanic matter as the Mid-Atlantic ridge. The mantle plume is located east of the ridge channel, but the eruptive belt tends to follow the plume, and it's there that volcanic activity is greatest.

The earthquake zone is formed where the eruptive belt is shunted. In the eruptive belt, a new earth crust is formed that accumulates at the fault edges and gradually drifts away. The oldest rocks in the country are thus found a long way from eruptive belt, in the east and west of the country. Þingvellir is in a seven-kilometre wide graben that lies between the Almannagjá and Heiðargjá faults. It's covered with 10,000 year-old lava that originated in a crater south of mount Hrafnabjörg.


oxararfoss.jpgDuring the time since the lava flowed, the land subsidence has been about 40 metres and the spreading or rifting about 70 metres. The rift valley is part of an active volcanic and fissure region that extends north from just outside the Reykjanes area to the Langjökull glacier. The outer boundaries of this are the Súlnaberg rock face in mount Botnssúlur and, in the east, mounts  Lyngdalsheiði and Laugarvatnsfjall.

The landscape at Þingvellir is now quiet different to that at the time when Grímur geitskór chose the site for the general assembly. In the Sturlunga Saga it is said that the river Öxará had been diverted into Almannagjá and onto Þingvellir. The river Öxará then changed the appearance of the site through sedimentation, and land subsidence caused encroachment of water up to the assembly site. We can assume that the subsidence amounts to almost four metres from when the Alþing was established in 930

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Safe travel in Iceland
Travellers should prepare well for each trip and know its trail and route conditions.
The THING Project
The THING Project is based on the Thing sites that are the assembly sites spread across North West Europe as a result of the Viking diaspora and Norse settlements.
World heritage
Thingvellir was accepted on the World Heritage list for its cultural values in 2004 at World Heritage Committee meeting in China.
Protection and management
Thingvellir National Park was designated by a special law on the protection of the area, passed by the Alþing on 7th May, 1928.