The Town lies in the contact of the Silurian bedrock and underlying Maquoketa shale. This area is characterized by a dense and universal fracture network, shallow soil surface, and little surface runoff, allowing water to easily infiltrate to the subsurface. Recharge is exceedingly rapid and carries surface contaminants to the water table. Flow within the aquifer occurs primarily along bedding plane fractures with little to no reduction of contaminants within the aquifer. This type of a geologic setting makes the area extremely vulnerable to groundwater contamination, especially for shallower private wells. Source: Presentations of UW-Oshkosh Geology Professor Dr. Maureen Muldoon and USDA Agricultural Researcher Dr. Mark Borchardt to the Town of Ledgeview Town Board, May 29, 2018, https://www.ledgeviewwisconsin.com/govenrment/departments/community- developmentbuilding-inspection/zoning-and-planning/adopted-plans-documents-maps/; Kevin Erb, Eric Ronk, Vikram Koundinya, and John Luczaj, Groundwater Quality Changes in a Karst Aquifer of Northeastern Wisconsin, USA: Reduction of Brown Water Incidence and Bacterial Contamination Resulting from Implementation of Regional Task Force Recommendations, Resources 2015, 4, 655-672; doi:10.3390/resources4030655; K. Erb and R. Stieglitz, Final Report of the Northeast Wisconsin Karst Task Force, February 9, 2007.