What the statewide pattern says
Sprawl on fractured rock and sandy plain
South Carolina's modest nitrate signal sits in its fastest-growing counties, on Piedmont fractured rock and sandy Coastal Plain — settings whose mechanics are documented just across the state line.
South Carolina's deep public supplies are well protected: USGS sampling of the Southeastern Coastal Plain aquifer system, which underlies the state's lower half, found nutrients absent at high or moderate concentrations at public-supply depth (Barlow, 2016 — USGS Fact Sheet 2016-3076).
The counties that do light up — York, Lexington, Sumter — are growth counties on the two shallow settings the region knows well. York and Lexington sit on Piedmont fractured crystalline rock under Charlotte and Columbia sprawl, the same province where North Carolina's geochemistry work documents nitrate moving through shallow fractures with denitrification only at depth (USGS SIR 2009-5149). Sumter and Marlboro lie on the sandy Coastal Plain, the province where Delmarva-to-Georgia studies repeatedly find shallow unconfined nitrate.
That is the honest South Carolina reading: the mechanism is documented at province scale, but South Carolina itself has no county-level nitrate study this page can cite, so the map marks the signal and the regional literature supplies the plausible pathway — nothing more.
The supported source reading is mixed suburban and agricultural nitrogen on shallow fractured rock and sandy plain — not a certified source at any individual system (Nolan and Hitt, 2006).