Eleven heavily used surficial-deposit aquifers in New York were mapped in 1981 to provide a basis for their protection from contamination, particularly through underground disposal of wastes. The resulting maps and sections, originally prepared and released by the U.S. Geological Survey at a scale of 1:24,000, are presented herein at a reduced scale and in simplified form. Each illustration is accompanied by a short text describing the major features and hydrologic characteristics of the given aquifer. The areas mapped are Schenectady,
Water-level hydrograph of changes at Chugiak- .-21. Sketch map of Cordova showing well locations-_ _. 22. Hydrographs of water-level changes on the Kcnai Lowland. _.
A major fracture system in indurated sedimentary rocks forms a moderately extensive aquifer yielding 100-300 gallons per minute to wells 160 to 420 feet deep. Pumping-test data show that the fracture system is interconnected to distances more than 1,000 feet from the wells. Recharge occurs through overlying clayey till, and continuous pumping may induce recharge from surface-water sources. Partial chemical analyses indicate no water-quality problems. Systematic collection of data on pumpage, water level, and chemical quality could help to determine the long-term adequacy of the aquifer system.
scite is a Brooklyn-based organization that helps researchers better discover and understand research articles through Smart Citations–citations that display the context of the citation and describe whether the article provides supporting or contrasting evidence. scite is used by students and researchers from around the world and is funded in part by the National Science Foundation and the National Institute on Drug Abuse of the National Institutes of Health.