COSTS AND BENEFITS OF EARTHQUAKE PREDICTION STUDIES IN GREECE

For the following reasons, a (hypothetical) successful earthquake pred iction in Greece would be of, at best, limited benefit to society. (1) On average, less than 5 per cent of sizeable earthquakes (that is mag nitude greater than 4.5) cause significant damage or loss of life. (2) Organized evacuation of urban centres is unlikely to be successfully accomplished, because the public lacks confidence in the authorities a nd cannot be expected to respond promptly; panic and other undesirable side-effects can also be anticipated. (3) The lead time between a sho rt-term prediction and earthquake occurrence is too short for most act ions aimed at reducing or eliminating primary or secondary earthquake effects, in any case, most such actions would be superfluous if approp riate longer-term preparedness plans were implemented. (4) Prediction of 'an earthquake' is not an appropriate objective in an area such as Greece, which experiences complicated and long seismic sequences consi sting of several destructive events, and large earthquakes with anomal ous meizoseismal areas. (5) The seismic death toll in Greece is relati vely small (less than 10 people per year over the last 40 years), and due to recent changes in building styles and construction practices, c urrent morbidity is mainly associated with the failure of multistorey buildings. This death toll could be more effectively eliminated by ide ntifying weaknesses and structural intervention than by earthquake pre diction. Hence, earthquake prediction in Greece, even if it were scien tifically feasible, would not be cost-effective; alternative use of fu nding could be expected to save more lives with much greater certainty . Over the past 15 years, the VAN group's research on earthquake predi ction has absorbed a substantial fraction of the resources devoted to earthquake research and protection in Greece. However. the VAN method has not advanced the nation's policy on earthquake protection planning , its results continue to be widely questioned by both the Greek and i nternational scientific communities, and the underlying model is not c ommensurate with currently accepted thinking on earthquake generation and tectonophysics. Thus, VAN's methods can be regarded as basic resea rch rather than as an operational method for the reduction of seismic risk.