South Dakota State University
This publication explains how ground-water levels react when water is withdrawn by pumping and how ground water is being managed. Consideration is given only to the glacial ground-water aquifers which are 30 to 300 feet beneath the land surface. Deep artesian aquifers are not included.
South Dakota State University, Cooperative Extension,, "How Wells Affect Shallow Glacial Ground-Water Supplies in South Dakota" (1968). SDSU Extension Circulars. 728.
This item was digitized with the support from Project CERES, a collaboration between USAIN, AgNIC, and the Center for Research Libraries.