The thermally activated movement of a dislocation intersecting a small density of strong point obstacles imbedded in a large density of weak obstacles is calculated analytically by modelling the geometrical correlations. The superposition of the flow stresses for the isolated processes is only valid for zero temperature. At high temperatures only the strong obstacles impede the movement wheras at low temperatures the weak obstacles contribute to or controll the flow stress. It is suggested that the plateau‐stress in solid solutions has its origin in the dislocation forest which acts like strong obstacles.