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This castle was built on a basaltic layer covering a conical top of the mountain.
It is made of basaltic layers of Tertiary age.
These basaltic layers, formed from lava emitted from rift fissures in the center of what is now Lake Superior, subsided in the middle (forming the present lake basin); the edges angle upward from the lake in a serrated series of ridges known as the Sawtooth Mountains along the lakeshore.
Wörterbuch für Geologie