The University of Queensland Seismology Station was established in 1938 at the University of Queensland, Brisbane, Australia.
The University of Queensland Seismology Station is a long term research project of the University, second only to the Pitch Drop experiment. The station was established following the Gayndah earthquake of April 12, 1935.W.H. Bryan, who was a lecturer in Geology at the University of Queensland, undertook an investigation into the earthquake, distributing a questionnaire to those affected by it, and undertook field investigations. This was done to establish the epicentre of the earthquake, and its cause and effects. Newspaper coverage of the event was extensive in 1935, and following on from an interview with W.H. Bryan, a donor presented a Milne-Shaw Seismograph to the University to aid their continuing research. A second seismograph was loaned to the University by the Commonwealth Council for Scientific and Industrial Research (CSIR) and the University purchased several more. An official station was set up in the basement of a building at the University of Queensland, then in George Street, Brisbane. It was designed to monitor tremors.
The Geology department of the University of Queensland, was led by Professor H.C. Richards from 1911-1947. Both Richards and Bryan made use of the public's interest in the 1935 earthquake to push for further research into earthquakes in Queensland and overseas. They also had a role to play in cyclone prediction. After the University moved to it new location in St Lucia, Brisbane in 1951, the existing seismographs, and in time new models, were re-housed in the basement levels of the new Richards Building, but the near constant construction of new buildings at St Lucia, played havoc with the readings. Eventually the seismographs were removed to new observatories at Mt Nebo in 1956 and Charters Towers in 1960.