Atmospheric gravity waves are ubiquitous throughout all levels of Earth’s atmosphere. At thermospheric altitudes, these may result from upward propagation of waves originating in the lower atmosphere or be generated by strong forcing in the auroral region. These are sometimes referred to as traveling atmospheric disturbances (TADs). It is believed that they are often closely related to ionospheric perturbations known as traveling ionospheric disturbances (TIDs). While observations of TIDs are relatively commonplace, observations of the neutral gravity waves at these altitudes are comparatively rare, especially in the middle thermosphere from ~120 – 200 km altitude. Far UV observations offer one way of observing the middle thermosphere, where abundant photoelectrons produce Far UV dayglow. During several campaigns, GOLD has been able to identify gravity waves in this region. Owing to its extended field of view, GOLD is also able to track the motion of these waves over large distances. This allows properties of these waves such as their periods to be deduced. With the inclusion of ICON wind observations, their intrinsic properties can also be found. This presentation shows the results from a multi-year survey of all the gravity waves observed by GOLD during these campaigns, along with a comparison to ground-based GNSS observations of concurrent TIDs.