The 1952 Washington DC UFO Flap
On the nights of July 19–20 and July 26–27, 1952, a series of unidentified objects flew over restricted airspace above Washington DC, tracked simultaneously on radar at Washington National Airport (now Reagan National) and Andrews Air Force Base, observed by civilian air traffic controllers and military personnel, and intercepted — unsuccessfully — by USAF F-94 jet interceptors.
The Radar Confirmation
Air traffic controller Edward Nugent first detected seven unidentified objects on the National Airport radar at 11:40 PM on July 19. The objects were tracked moving at speeds between 100 and 130 mph before some accelerated to an estimated 7,200 mph. Simultaneously, radar at Andrews AFB confirmed contacts. Visual sightings by airline pilots in the area corroborated the radar tracks.
The critical evidentiary point: the objects appeared simultaneously on ground radar at two separate facilities (National Airport and Andrews) and were visually confirmed by commercial pilots in the vicinity. This is not a single radar return or single witness — it is multi-sensor, multi-observer confirmation.
The Air Force Response
F-94 Starfire interceptors were scrambled from Newcastle Air Force Base in Delaware. By the time they arrived over Washington, the objects had disappeared. When the fighters returned to base, the objects reappeared on radar. The pattern repeated across both nights — objects disappearing when interceptors arrived, reappearing after they left.
The Largest Pentagon Press Conference Since WWII
On July 29, 1952, the Air Force held what was described at the time as the largest Pentagon press conference since the end of World War II to address the Washington sightings. Major General John Samford, Director of Air Intelligence, acknowledged the radar contacts, confirmed that “credible observers” had seen “relatively incredible things,” and attempted to attribute the sightings to temperature inversions. Meteorologists subsequently stated that conditions at the time were not consistent with the type of temperature inversion that would produce the observed radar returns.