Aykut A. Barka (1952-2002)
EOS, Trans. Amer. Geophys. Union, vol. 83 (44), pp. 499-500 (2002).

Aykut Barka, a scientist respected throughout the world for the quality and depth of his research, died on 1 February 2002 from injuries suffered in a car accident five weeks earlier. Barka embodied the highest calling of science in service to the public. He was known for his unstinting integrity; his humor, openness, and selflessness; his plain talk to the Turkish public; and his tireless efforts to convince the Turkish government to confront the potential for an earthquake disaster in one of the most vulnerable countries in the world.

An identical twin, Barka was born in Istanbul on 7 January 1952. He received a Ph.D. in 1981 from Bristol University in England, studying under the late Paul Hancock. Barka was a senior geologist for the Turkish Geological Survey (MTA) until 1985, a research scientist at the Massachusetts Institute of Technology from 1986 to 1990, professor at the Kandilli Observatory of Bosphorus University from 1990 to 1991, and later, professor at Istanbul Technical University. From 1983 to 1984 he was a visiting scientist at the Geological Survey of Japan. In 1985, he was a visiting professor at the University of Bristol, and in 1998 he was a visiting professor at the Institut de Physique du Globe de Paris. He also was a frequent visitor to the U.S. Geological Survey in Menlo Park.

Barka made deep and lasting contributions to the study of active faulting, drawing upon the tools of geomorphology, paleoseismology, and space geodesy. In a series of papers with R. Armijo, E. Altunel, S. Wesnousky, K. Kadinsky-Cade, and N. Toksoz, Barka studied the neotectonics and paleoseismology of the north and east Anatolian fault systems, focusing on the complexities of this great transform fault at its eastern and western extremities. He showed how basins could be used to understand the interaction of branching fault strands. This work not only extended the precious record of large earthquakes back several thousand years, but also offered a comprehensive model of the fault-driven evolution of the Marmara Sea that, since his death, is being tested with side-scan sonar and high-resolution bathymetric surveys and ocean bottom seismometer networks. In a long and fruitful collaboration with R. Reilinger, C. Straub, H. Kahle, R. McCluskey, and O. Lenk, Barka carried out the first comprehensive global positioning system (GPS) surveys of the North Anatolian fault system, determining its contemporary slip rate and the partitioning of slip on the strands that lace the Marmara Sea. This knowledge is critical to an assessment of the likelihood and size of earthquakes that threaten this heavily industrialized part of Turkey.

With C. Finkel and T. Rockwell, Barka re-appraised the record of earthquakes that occurred over the past 500 years by tracing Roman canals offset by the fault and trenching into its prehistoric ruptures. With H. Eyidogan, he investigated the large 1992 Erzincan and 1995 Dinar earthquakes to learn how the ruptures were controlled by fault geometry. When Barka realized that many of the villagers who had experienced the great 1939-1944 earthquakes along the North Anatolian fault would soon be gone, he went from village to village along 700 km of the fault, sipping tea with the elders and letting them lead him to sites where evidence of the earthquakes was uniquely preserved. His 1996 study of the slip distribution for the 12 great earthquakes increased the number of observations by an order of magnitude, opening the door to a new way to evaluate earthquake interaction.

A 1997 study that Barka co-authored identified Izmit as the second-most likely site for the next large North Anatolian fault event, and a M=7.4 event struck there on 17 August 1999, catapulting him into the public eye. In a prescient 17 September 1999 article in Science, Barka argued that two faults were made more vulnerable by the August 1999 Izmit shock: the Yalova to the west, and the Duzce to the east. Two months later, the 12 November, M=7.1 Duzce earthquake struck. This accurate and timely warning is simply without peer in the literature. As a result of this warning, Duzce buildings partially damaged in August were not reoccupied, and many of these collapsed in November. In papers that appeared in Nature and Science in 2000, Barka and colleagues T. Parsons, S. Nalbant, A. Hubert-Ferrari, G. King, and R. Stein studied how the 1999 Izmit and Duzce shocks increased the seismic risk to Istanbul.

Barka felt that the public deserved to know the truth--both what is known and what isn’t. He worried that reporters were unwilling or unable to distinguish authoritative scientific counsel from the pronouncements of those who seek only to soothe or scare the public. He urged the press corps to demand to see publications in refereed journals on the topics in which scientists claimed to have expertise.

Barka was relentless in his efforts to encourage the Turkish government to take action to reduce the losses in future earthquakes, and he was rarely satisfied with the response. He felt that as a citizen of Turkey and an inhabitant of his beloved Istanbul, he could not face himself if he had not adequately warned the public of the risks they confront. He neither sought nor enjoyed the limelight of media attention, and the time away from his family and work came at a huge cost. I know of few other scientists who sacrificed so much research time to make such a public gift. Since his death, the city of Istanbul has acknowledged this debt by naming a high school, a park, and a Bosphorus ferry in his honor.

A daily stream of scientists from all over the world traipsed through Barka's cramped office at Istanbul Technical University and modest field camps to share in research with him. Scientific collaboration can often be prickly, with struggles for lead authorship sapping the pleasure of working together. With Barka, these issues never arose. His generosity and humility made collaboration a joy and an adventure. His scientific prestige sometimes made him a target for public attacks in the press and at international meetings. Although this deeply upset him, he argued cogently for his views and never lost his temper or took it personally. At the time of his death, Barka had five papers in press and was supervising 10 graduate students. His students adored him, took care of him, and flourished because of him. They are a precious resource for their nation and will carry his torch far into this century. Emre Evren, one of Barka's PhD students, is the recipient of the privately-funded 'Aykut A. Barka Memorial Scholarship.' Evren will study under Philip England and Barry Parsons at Oxford University during 2003, and will continue his GPS and stress-triggering studies of the North Anatolian and Marmara faults.

Barka ran about 2 hours late for every appointment. He slept for just several hours a night. His phones rang every 30 seconds. He rarely answered his hundreds of daily e-mail messages, so one never knew where and when he would show up next; every encounter came as a surprise. His travel schedule was impossible and constantly in flux. He lovingly maintained his 1972 Peugeot, doing valve jobs at the university parking lot before racing to the airport to fly down the fault, or walking for hours in the middle of the night, carrying his radiator, in search of an insomniac welder. He loved fresh seafood simply prepared, Turkish carpets, and sailing down the Bosphorus on the yacht he restored with his brothers. Most of all, he loved to laugh with family and friends. He is survived by his wife, Sheree, and his children, Dagcan and Isabel.

Barka's death is a great loss to both his nation and Earth science. But the message of his life's work is clear: Strive to understand the mystery and hazards of the Earth on which we live and communicate that insight--both the joy of discovery and the risk of disaster--to those most affected.

Author:
R.S. Stein, U.S. Geological Survey, Menlo Park, CA.

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