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Quaternary Geology of Richland County, Wisconsin
The topography of the Driftless Area, which was never glaciated during the Quaternary Period, is dominated by fluvial incision into flat-lying Paleozoic bedrock, resulting in deep, dendritic valleys. Local relief reaches 115 meters. Sediment coring across the region reveals that the geology of unconsolidated surficial materials is often controlled by the...-
GIS Data for Quaternary Geology of Richland County, Wisconsin [dataset 1]
2025
GIS Data: GeMS Level 3 file geodatabase (.gdb file format)
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Core Data for Quaternary Geology of Richland County, Wisconsin [dataset 2]
2025
Data: Spreadsheet (.csv file format)
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Quaternary Geology of Vernon County, Wisconsin
The topography of the Driftless Area, which was never glaciated during the Quaternary Period, is dominated by fluvial incision into flat-lying Paleozoic bedrock, resulting in deep, dendritic valleys. Local relief reaches 115 meters. Sediment coring across the region reveals that the geology of unconsolidated surficial materials is often controlled by the...-
GIS Data for Quaternary Geology of Vernon County, Wisconsin [dataset 1]
2025
GIS Data: GeMS Level 3 file geodatabase (.gdb file format)
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Core Data for Quaternary Geology of Vernon County, Wisconsin [dataset 2]
2025
Data: Spreadsheet (.csv file format)
Publications Catalog
Wisconsin Geological and Natural History Survey
