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Norway sits on a very old part of the Earth's crust

Norway sits on a very old part of the Earth's crust known as a craton. The cratons have survived geodynamic processes and plate tectonics, and have long been a mystery in geology. Interview with Trond H. Torsvik and Jyotirmoy Paul, Dept of Geosciences/PHAB in an article on sciencenorway.no.

Amidst this mountain formation viewed from Ofotfjorden, the characteristic mountain Stetinden can be seen. The pointed Stetinden is part of the craton that rises above. Photo: Helge Høifødt, ​​​​​​​Wikipedia, (CC BY-SA 3.0)

Amidst this mountain formation viewed from Ofotfjorden, the characteristic mountain Stetinden can be seen. The pointed Stetinden is part of the craton that rises above. Photo: Helge Høifødt, Wikipedia, (CC BY-SA 3.0)

Norway, Sweden, and Finland all sit on an ancient part of the Earth's crust, known as a craton. This craton is referred to as the Baltic Craton or the Baltic Shield. As a result, there are bedrock formations in East Finnmark, Lofoten, and Vesterålen in Norway that are up to 3 billion years old. The bedrock in parts of Eastern and Western Norway can be 1 to 1.5 billion years old.

Cratons are stable and have not been destroyed by processes in the Earth's crust. They are also often rich in mineral resources, such as gold, diamonds, and iron. Finland, which also lies on the Baltic Shield, is Europe's largest gold producer, and gold has been mined in Finnmark. Likewise, Sweden has large iron deposits, and in Kirkenes, Norway, there is Europe's third-largest iron ore mine.

Read more in the article on sciencenorway.no:

Norway sits atop a strange and ancient part of the Earth's crust, sciencenorway.no, 4.8.2025

Published Aug. 7, 2025 11:24 AM - Last modified Aug. 7, 2025 11:24 AM