
On the evening of 3 April 1966, a radar operator at Tullamarine recorded an unidentified plot near an inbound air route. The ensuing Department of Civil Aviation file contains the observer’s form, an air-safety report, enquiries to the Bureau of Meteorology and a specific proposed explanation. Its interest lies in that surviving investigation, including the careful wording of the final meteorological advice.
Approximate area: the map uses a rounded Tullamarine suburb reference for the observer’s general location. It does not identify the exact 1966 radar installation or place the target on the ground. The reported return was more than fifty nautical miles away to the northeast. The modern terminal photograph is later local airport context, not a picture of the equipment or observation point.
The original report
The eleven-page National Archives of Australia file MT1298/1, VTI-66/319 is titled Unidentified Aerial Object 3/4/1966 Tullamarine. Its final two scanned pages contain the report attributed to J. Reinmuth. He identified the equipment as CSF radar and initially recorded observations from 8.15 to 8.27 p.m. Additional entries extend the observation history to 8.43 p.m.
The first plot was about 54½ nautical miles from Tullamarine on a bearing of 055 degrees. It attracted attention because it lay near the inbound route. The reported movement was northeastward along a straight path at about sixty knots. A later entry places it at sixty-one nautical miles, with additional notes recording sixty-four nautical miles at 8.40 and 8.43 p.m.
These details describe an instrument return, not a close visual encounter. The form supplies no colour, visible shape, construction, propulsion or sound. Those unanswered questions should not be filled with features taken from other Australian cases. Nor does the use of an aerial-object reporting form establish that a solid manufactured craft was seen.
The air-traffic context
The report identifies nearby known traffic as TJA on its normal inbound route. It also notes a southwesterly airstream. The distinction between an unidentified plot and an identified flight was therefore part of the original record. It does not establish that the unknown return performed an evasive manoeuvre or followed the known aircraft.
The sequence is also more measured than a sudden high-speed crossing. Positions were recorded over a period of minutes, and the stated speed was compatible with ordinary aerial drift under some conditions. The file does not include a surviving continuous radar recording from which a modern analyst could independently reconstruct every plot or measure changes between sweeps.
Civil aviation asks a specific question
An April memorandum from A. R. Woodward’s office asked the Victorian Bureau of Meteorology whether a balloon had been released at a suitable place and time to match the observed return, allowing for the prevailing winds. A handwritten regional-investigator note already considered a meteorological balloon likely and said that possibility was being investigated.
This was a proposed identification tied to testable circumstances: a release location, a launch time and atmospheric movement. It differed from an unsupported assumption that any unexplained radar return must be a balloon. The enquiry also shows that the balloon suggestion preceded the final administrative closure, rather than being inferred simply because the file later stopped.
A May reply said relevant data were still being collected. That intermediate stage matters when reading the archive out of order: the file’s later assessment and earlier requests are all retained, so the mere presence of an unanswered question on one page does not mean no answer was subsequently received.
The weather bureau’s assessment
In July 1966, the Bureau advised that the object could have been a meteorological balloon carrying a radar reflector, released from RAAF Laverton. Its position and movement were considered consistent with the release time and the winds affecting the balloon. The original memorandum is preserved on PDF page 5.
The reflector is a significant detail. The hypothesis concerns an ordinary balloon with equipment intended to produce a radar return; a matching visible aircraft was not required. Nevertheless, the surviving memorandum gives the conclusion rather than a complete table of launch data, wind observations and calculated positions. This article has not independently reproduced the meteorological reconstruction.
A subsequent civil aviation memorandum relayed the explanation to the airport manager and asked that radar controllers be informed. The closure memorandum says the regional controllers had been advised, no further action was intended and the incident was closed. That establishes an administrative outcome and the explanation accepted for operational purposes.
A possible identification rather than a recovered object
The bureau’s qualification remains important. It reported consistency and used conditional wording, rather than saying a particular reflector had been recovered and its track conclusively matched. The evidence supports a credible possible balloon explanation. It does not justify changing the historical conclusion into certainty or treating the case as an unexplained high-performance vehicle.
Keith Basterfield’s 2013 original review of the file drew attention to the same distinction. His research credits Paul Dean with locating the civil aviation record and notes that the radar event occurred three days before Westall. The present assessment checks the underlying documents, rather than relying on the file’s later discovery as a new incident.
Why this is a separate case from Westall
The Westall school reports concern a different observation on 6 April 1966. Reinmuth’s return was recorded on the evening of 3 April. Temporal proximity and the discussion of balloons in both histories do not make this a radar confirmation of the school event. Each report requires its own chronology and evidence.
Assessment
The outcome is Possibly Explained. The original investigation records a specific Laverton balloon proposal supported by the weather bureau’s comparison of location, timing and movement. Its cautious conclusion warrants retaining a qualification. The archive demonstrates a reported radar return and a documented official response; it does not establish a visually identified extraordinary craft or a confirmed connection with Westall.

