Rock type: Quartzite slate.
Age: Late Pre-Cambrian (approx. 800 million years).
Alta Slate represents what was originally a homogenous sandstone formation, which was deformed through horizontal movement in the earth’s crust during the formation of mountains in the Caledonian period and metamorphosed into slate.
Rock type: Feldspar metasandstone.
Age: Silurian-Devonian (approx. 650 million years).
The depositing of sediments formed the Offerdal highland region during a period of continental settling. During the formation of the Caledonian mountain range the sediment was moved, deformed and metamorphosed into the Offerdal region as you see it today.
Rock type: Quartzite slate.
Age: Late Pre-Cambrian (approx. 750 million years).
Oppdal slate represents what was originally a homogenous sandstone formation, which was deformed through horizontal movement in the earth’s crust during the formation of mountains in the Caledonian period and metamorphosed into slate.
Rock type: Phyllite slate.
Age: Ordovician (approx. 460 million years).
Otta slate represents what was originally a clay/siltstone formation which during the Caledonian period was deformed and metamorphosed with the foundation of regular cleavage strata.