What the statewide pattern says
A sole-source aquifer under suburbia
New York's documented nitrate center is Long Island's sole-source aquifer — septic and cesspool nitrogen in the suburbs, fertilizer in the east-end farm belt — with a thinner dairy-country signal upstate.
Long Island drinks only groundwater, and USGS has tracked its nitrate since the 1970s: the upper glacial aquifer, the water-table layer, takes nitrogen directly from cesspools, septic tanks, lawn fertilizer and storm runoff (USGS Water-Resources Investigations Report 78-41). Isotope work in Suffolk County confirms the source mix — fertilizer, septic effluent and animal waste — and in the east-end farm belt, test-farm wells have run 10 to 30 mg/L from fertilizer alone (USGS SIR 2025-5010).
The deeper Magothy aquifer, which supplies most public water, starts cleaner — but pumping drags shallow nitrate down into it, which is why Long Island utilities blend and treat, and why Nassau and Suffolk still anchor this page's map. In the village of Patchogue, one shallow well reached 40 mg/L beside the Patchogue River (USGS SIR 2010-5132).
Upstate reads differently: Cattaraugus County's showing sits in western New York dairy-and-fractured-rock country, and Dutchess and Columbia counties mix fractured bedrock with septic — settings the Long Island literature does not cover, so this page marks the signal without claiming a certified source for them.
The supported source reading is on-site wastewater first, fertilizer second, on Long Island; mixed and less-studied upstate — not a certified source at any individual system (Nolan and Hitt, 2006).