The way in which a mechanical lock‐on type of direction finder of small aperture can be used for recording the variations of incoming wave‐normal direction in both the vertical and horizontal planes is discussed. The limitations arising from the inertia of the system are considered. It is shown that, in the case of near‐antipodal short‐wave ionospheric propagation (Great Britain to New Zealand), the received cone of rays usually contains two or more main groups displaced in angle in a plane that is nearly vertical.