Thingvellir National Park is a UNESCO World Heritage Site celebrated for its geological features and historical significance. It is the site of the Althing, the world's oldest surviving parliament, established in 930 AD. The park lies in a rift valley between the North American and Eurasian tectonic plates, offering a unique view of the Earth's tectonic movements. Thingvellir's landscapes are steeped in Norse mythology and history, with the Silfra fissure being a top diving destination.
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The Althing was established in 930 AD as an open-air assembly for making laws and settling disputes
Trial and Banishment of Erik the Red
The trial and banishment of Erik the Red at the Althing led to the European discovery of Greenland
Thingvellir holds a sacred place in Norse mythology and is woven into the fabric of Viking history
Thingvellir is situated in a rift valley created by the diverging North American and Eurasian tectonic plates
Plate Divergence
The Mid-Atlantic Ridge at Thingvellir showcases the separation of the North American and Eurasian tectonic plates, drifting apart at a rate of 2.5 centimeters per year
The Silfra fissure, formed by the rifting plates, is renowned for its crystal-clear glacial waters and is considered one of the premier diving sites globally
The geological amphitheater of Thingvellir symbolizes the harmony between human society and the environment
Thingvellir's significance in Icelandic sagas emphasizes its role in the nation's cultural continuity
As a living historical site, Thingvellir invites contemplation on the development of democratic ideals and their enduring influence on governance worldwide
Thingvellir's geothermal resources demonstrate the practical use of its geological traits, marrying natural history with sustainable practices
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Establishment year of Althing
Althing, world's oldest parliament, established in 930 AD.
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Geological feature of Thingvellir
Located in rift valley between North American and Eurasian tectonic plates.
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Annual plate movement at Thingvellir
Tectonic plates drift apart at 2.5 cm/year, contributing to Iceland's volcanic landscape.
