Research
Phase: Initial Site Studies:
Geologic Analysis of UMN Campus and Selected Buildings Top Left Image: Civil Engineering Complex: Holocene structure of varied composition with 1-7 floor penetration into Quaternary and Paleozoic sediments: Building: Brick - local altered Paleozoic sediment. Site: differentiated glacial till - Quaternary; Decorah Shale - Ordovician; Platteville Formation - Ordovician; St. Peter Sandstone - Ordovician; Parie du Chien Group - Ordovician. Top Center Image:
College of Architecture and Landscape Architecture; Top Right Image: Pillsbury Hall: Geology Department Holocene structure of primarily Proterozoic sediments resting on Quaternary sediments with shallow penetration. Building: Fond du Lac and Hinckley sandstone: Keweenawan Supergroup, late Proterozoic Era, Northern MN. Site: same as adjacent Civil Engineering Complex. Bottom Image:
Mississippi River section (looking east): Holocene structures (UMN
campus) above late Cenozoic glacial sediments and Paleozoic marine
sediments (see Civil Eng. Complex, above). Research 1; Research 3; Conceptual 1; Conceptual 2; Conceptual 3, Design 1; Design 2; Quarry 1; Quarry 2
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