Tropical Storm David produced numerous tornadoes during its transit up the East Coast in September 1979. One of these occurred in Fairfax County, Virginia, during early evening daylight and in a residential community. A study of this tornado was conducted through ground inspection, personal interviews, examination of low-level aerial photography, and meteorological records. Several eyewitness accounts of this storm are of special interest, considering the general paucity of data on hurricane and/or tropical storm tornadoes. Among such observations were: an isolated break in the overcast immediately south of the tornado, with an echo-free “hole” seen by radar 10 min prior to its formation; an outflow gust front wrapping around the tornadic circulation; and widely varying sound reports. The isolated visual and radar break in the clouds may be a significant forecast indicator of these small, short-lived, but destructive storms.