In a fluid at rest, pressure increases with depth due to the weight of the overlying fluid. The pressure difference between two points in a fluid, P2 and P1, separated by a vertical distance h, can be expressed as P2 - P1 = ρgh, where ρ is the fluid's density and g is the acceleration due to gravity. When the top point (P1) is at the surface of a liquid open to atmospheric pressure, the absolute pressure at any depth h is given by P = Pa + ρgh. This section emphasizes that the shape or area of the container does not affect the pressure at a given depth, highlighting that pressure in a liquid is the same at any horizontal level in an incompressible fluid, leading to applications such as gauge pressure calculations.