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Asset Overview
Glacial erratic boulder. The lithology is metamorphic (schist), so this boulder must have been transported by the glacier all the way from the Alpine crystalline basement, which is about 200 km south of the boulder's present location. The boulder currently sits in the front yard of the Geology building of LMU, and it was originally found during construction work in the city of Munich, Germany.
Same boulder as [this one](https://skfb.ly/6V9zt), but model redone using a smartphone video rather than photos.
