As is well known, LiDAR provides an enormous, almost overwhelming amount of information pertaining to glacial geology. Some of this is obvious, such as LiDAR imagery for hummocky stagnant ice deposits which commonly have a very distinctive signature on LiDAR imagery. However, LiDAR imagery commonly also shows quite subtle features. Study of such imagery, it seems, reveals an unending array of evidence. The more one examines LiDAR, the more one sees. Some of these subtleties almost certainly relate to the receding ice margin, even if their exact nature and origin is uncertain. Some features were not initially recognized but once identified became apparent and recurrently found upon further examination of LiDAR. The following discussion reviews the findings from this LiDAR examination according to different types of features identified.