The Delaware River doesn't have a single "turning point," but rather a shifting zone known as the "Salt Front" (or Salt Line), where the salt concentration reaches 250 mg/L of chloride. Under normal conditions, this front typically sits near the Delaware Memorial Bridge (near Wilmington, DE), approximately 70 miles upstream from the mouth of the Delaware Bay. However, because the river is tidal, the salt front is constantly moving based on the tides and the volume of freshwater flowing down from the Catskill Mountains. During periods of severe drought, the salt water can creep much further north; for instance, in the 1960s "drought of record," the salt line reached as far north as Philadelphia (near the Ben Franklin Bridge), threatening the city's drinking water intakes. In 2026, the Delaware River Basin Commission (DRBC) carefully manages the river's flow by releasing water from upstream reservoirs to "push" the salt front back down towards the sea, ensuring that the water remains fresh enough for industrial use and human consumption in the heavily populated Philadelphia-Camden corridor.