The top flow line of a saturated soil mass below which seepage takes place, is called the Phreatic line.
Hydrostatic pressure acts below the phreatic line whereas atmospheric pressure exists above the phreatic line. [1] This line separates a saturated soil mass from an unsaturated soil mass. It is not an equipotential line, but a flow line.
For an earthen dam, the phreatic line approximately assumes the shape of a parabola.