Interactive

Frank Evison – geophysicist

Frank Evison – geophysicist

  • Changing scientific ideas
  • Advances in science and technology
  • Biography
1900
1900
Measuring earthquakes

The first seismograph in New Zealand is installed in Wellington. Seismographs measure and record information during earthquakes.

1906
1906
Elastic rebound theory

After the San Francisco earthquake, HF Reid develops a theory that earthquakes result from the sudden elastic rebound along a fault, driven by previously stored energy. This theory underpins many long-term forecasts in the years to come.

1922
1922
Frank is born

Harry Evison

Frank Foster Evison is born in Christchurch where he lives with his family until they move to Wellington in 1937.

Image: Roger, Frank and Harry Evison, Christmas 1927
Courtesy of Harry Evison

1937
1937
Life in Wellington

Harry Evison

Attends Wellington College. A love of tramping, skiing and mountaineering develops.

Image: Rusty Rawlings and Frank Evison (on right) on Mount Duff 1951. Courtesy Harry Evison

1939
1939
World War II

From 1939-1945 Frank serves in the Royal New Zealand Air Force as the commanding officer of the radar station in Wellington for part of World War II.

1944
1944
Frank graduates

Graduates from Victoria University of Wellington with a BSc in physics in 1944 and a MA with Honours in mathematics in 1946.

1946
1946
Travels to Britain

Marries Joan Alpers. They go on to have three children – David, Margaret and Rosemary. Family holidays often involve trips to out-of-the-way seismographs!

1950
1950
Joins DSIR

Joins Geophysics Division of the Department of Scientific and Industrial Research (DSIR) and works in exploration geophysics. Discovers coal-seam guided S waves in 1955 – renamed ‘Evison waves’ in 1985.

1957
1957
Research gains recognition

NIWA

Gains a Nuffield Fellowship in 1957 and a Fulbright Award in 1963.

1960
1960
Plate tectonics

Before the 1960s, it was thought that continents were set in the same position forever. The realisation that the Earth’s plates are dynamic revolutionised the study of earthquakes.

1964
1964
Japanese prediction plan

A 5-year plan with the goal of accurate earthquake forecasting is launched in Japan. Methods to be explored include observation of tides, crustal deformation and seismic activity as well as rock testing.

1964
Evison’s wall

Creeping faults don’t tend to have large earthquakes. Frank organises the building of a wall across Alpine Fault to see if it’s creeping.

1965
1965
Data explosion

During the mid-1960s significant improvements in technology (particularly in communication and travel) make earthquake data much more uniform and readily available. This makes it much easier to look for patterns and leads to an increase in forecasting efforts.

1965
Expansion of seismograph network

Diag. 2. New Zealand network of seismograph stations', from An Encyclopaedia of New Zealand, edited by A. H. McLintock, originally published in 1966. Te Ara

As director of the Geophysics Division of DSIR, Frank organises major upgrade and expansion of New Zealand seismograph network.

1967
1967
Inaugural Professor of Geophysics

Appointed inaugural Professor of Geophysics at Victoria University of Wellington.

1970
1970
Begins research into earthquake forecasting

Possesses a strong belief that scientists have a duty to society and that reliable earthquake prediction would help minimise loss of life and suffering. Works passionately towards this goal until his death.

1971
1971
Establishes Institute of Geophysics

Has a vision for an interdepartmental institute with members from geology, physics, chemistry, mathematics and geography departments in addition to members outside the university.

1973
1973
Interest in precursors

Lloyd Homer, GNS Science

Frank uses first portable seismographs in NZ to compare mechanisms of main shock and the aftershocks of the Inangahua earthquake.

1975
1975
Earthquakes can be predicted

The predominant scientific view in the 1970s is that earthquake prediction is possible.

1975
Rikitake precursors

Tsuneji Rikitake publishes key paper suggesting use of a variety of geophysical precursors as a strategy to predict earthquakes.

1975
Haicheng prediction in China

Using a sequence of foreshocks, scientists predict the Haicheng earthquake and evacuate the city, saving thousands of lives. Some scientists do not view this as a true prediction – rather, a very lucky coincidence.

1976
1976
Collaboration with David Rhoades

GNS Science

Begins work with David Rhoades, now a statistician at GNS. This successful partnership continues until Frank’s death.

1977
1977
Predicting earthquakes in the USA

The National Earthquake Hazards Reduction Program (NEHRP) is launched in the USA with a focus on earthquake prediction techniques.

1977
Precursory swarm hypothesis

Frank’s first attempt at a forecasting model based on idea that swarms of earthquakes act as precursors to main-shock events. Frank sees predictive potential of these swarms and begins to work with statistician David Rhoades.

1979
1979
Seismic gap theory – McCann et al.

A seismic gap is a period of inactivity along a fault that has been seismically active in the past. Many scientists (including McCann et al.) theorise that the likelihood of an earthquake increases with the length of seismic gap.

1979
Frank retires

ITS Image Services, Victoria University of Wellington

Retires as chair of the Geophysics Institute and continues as Emeritus Professor.

1982
1982
Generalised precursory swarm hypothesis

Based on a study of Japanese earthquakes, Frank develops a more complex version of his first prediction model. He hypothesises that clusters of precursory swarms of earthquakes are followed by clusters of main-shock events.

1984
1984
Code of conduct for scientists

Frank is involved in the drafting of an international code of conduct for scientists involved in earthquake prediction and becomes even more committed to rigorous testing of prediction models.

1985
1985
Parkfield prediction experiment

Scientists Bakun and Lindh predict that a moderate-size earthquake will occur at Parkfield, California, between 1985 and 1993. (A large earthquake did occur but not until 2004.)

1990
1990
Franks wife, Joan dies

Joan had been Frank’s wife for 41 years.

1992
1992
Services to seismology (OBE)

Appointed as an Officer of the Most Excellent Order of the British Empire for services to seismology.

1995
1995
Earthquakes cannot be predicted

A less optimistic view prevails, and the international research focus starts to shift from earthquake prediction to damage mitigation.

1997
1997
Earthquakes cannot be predicted

Geller et al. publish a paper in Science claiming that earthquakes cannot be accurately predicted. They urge investment in earthquake-resistant structures and tsunami warning systems rather than earthquake prediction.

2000
2000
Increasing public demand for information

The rise of the internet and mobile phone technology increases public demand for information, especially following a large earthquake. This increases pressure on scientists to provide accurate short-term forecasts.

2003
2003
‘Tail wags the dog’ method

Vladimir Keilis-Borok and his team at UCLA claim to have successfully predicted two earthquakes in the USA and Japan. A subsequent publicly announced prediction of a large earthquake in California proves to be a false alarm.

2004
2004
Precursory scale increase phenomenon

Frank and David Rhoades publish their work on the precursory scale increase phenomenon. They provide 47 examples of an increase in seismicity before large earthquakes in California, Greece, Turkey, Japan and New Zealand.

2004
EEPAS forecasting model

David and Frank develop the EEPAS (every earthquake a precursor according to scale) forecasting model based on the precursory scale increase phenomenon. The model is tested and later used in operational forecasting in New Zealand.

2005
2005
Frank dies

The Wellesley Club

Passes away in his home in Wellington at the age of 82.

2006
2006
New technology renews optimism

The prevailing view is that earthquake forecasting methods will gradually improve due to new and better data streams (enabled by modern technology) combined with improved understanding of the physics of earthquake generation.

2006
Scholarship established

Frank Evison Research Scholarship in Geophysics established through donations from Frank’s family, the Earthquake Commission, GNS Science, the New Zealand Geophysical Society and a range of private donors.

2008
2008
Evison Symposium in Wellington

Evison Symposium on Seismogenesis and Earthquake Forecasting attended by national and international scientists. Two special journals are published to honour Frank’s interest in earthquake generation and forecasting.

2010
2010
Work continues on the EEPAS model

David Rhoades continues to apply the EEPAS model to catalogues of earthquakes around the world with the goal of increasing the strength of this model.

2011
2011
Scientists on trial in Italy

Six Italian scientists and one government official put on trial in Italy for manslaughter after failing to predict the 6.3 magnitude earthquake in April 2009 that caused the deaths of 309 people in the Italian city of L’Aquila. Find out more here.

Transcript

Changing scientific ideas

Each specialised field of science has key ideas and ways of doing things. Over time, these ideas and techniques can be revised or replaced in the light of new research. Most changes to key science ideas are only accepted gradually, tested through research by many people.

Advances in science and technology

All scientists build their research and theories on the knowledge of earlier scientists, and their work will inform other scientists in the future. A scientist may publish hundreds of scientific reports, but only a few are mentioned here.

Biography

This part of the timeline outlines just a few events in the personal life of the featured person, some of which influenced their work as a scientist.

CHANGING SCIENTIFIC IDEAS

1906 – Elastic rebound theory

After the San Francisco earthquake, HF Reid develops a theory that earthquakes result from the sudden elastic rebound along a fault, driven by previously stored energy. This theory underpins many long-term forecasts in the years to come.

1960 – Plate tectonics

Before the 1960s, it was thought that continents were set in the same position forever. The realisation that the Earth’s plates are dynamic revolutionised the study of earthquakes.

Find out more about Plate tectonics.

1965 – Data explosion

during the mid 1960s significant improvements in technology (particularly in communication and travel) make earthquake data much more uniform and readily available. This makes it much easier to look for patterns and leads to an increase in forecasting efforts.

1975 – Earthquakes can be predicted

The predominant scientific view in the 1970s is that earthquake prediction is possible.

1995 – Earthquakes cannot be predicted

A less optimistic view prevails during the 1990s, and the international research focus starts to shift from earthquake prediction to damage mitigation.

2000 – Increasing public demand for information

The rise of the internet and mobile phone technology increases public demand for information, especially following a large earthquake. This increases pressure on scientists to provide accurate short-term forecasts.

2006 – New technology renews optimism

The prevailing view is that earthquake forecasting methods will gradually improve due to new and better data streams (enabled by modern technology) combined with improved understanding of the physics of earthquake generation.

ADVANCES IN SCIENCE AND TECHNOLOGY

1900 – Measuring earthquakes

The first seismograph in New Zealand is installed in Wellington. Seismographs measure and record information during earthquakes.

Image: 'Modern seismograph', from An Encyclopaedia of New Zealand, edited by A. H. McLintock, originally published in 1966. www.teara.govt.nz/en/1966/earthquakes/5/2

1964 – Evison’s wall

Creeping faults don’t tend to have large earthquakes. Frank organises the building of a wall across the Alpine Fault to see if it’s creeping.

Image: Peter Knoop, Creative Commons Attribution ShareAlike 3.0

1964 – Japanese prediction plan

A 5-year plan with the goal of accurate earthquake forecasting is launched in Japan. Methods to be explored include observation of tides, crustal deformation and seismic activity as well as rock testing.

1965 – Expansion of seismograph network

As director of the Geophysics Division of DSIR, Frank organises major upgrade and expansion of New Zealand seismograph network.

Image: Diag. 2. New Zealand network of seismograph stations', from An Encyclopaedia of New Zealand, edited by A. H. McLintock, originally published in 1966. www.TeAra.govt.nz/en/1966/25316/diag-2-new-zealand-network-of-seismograph-stations

1973 – Interest in precursors

Frank uses first portable seismographs in NZ to compare mechanisms of main shock and the aftershocks of the Inangahua earthquake.

Image: GNS Science Limited, Lloyd Homer

1975 – Rikitake precursors

Tsuneji Rikitake publishes key paper suggesting use of a variety of geophysical precursors as a strategy to predict earthquakes.

1975 – Haicheng prediction in China

Using a sequence of foreshocks, scientists predict the Haicheng earthquake and evacuate the city, saving thousands of lives. Some scientists do not view this as a true prediction – rather, a very lucky coincidence.

1977 – Precursory swarm hypothesis

Frank’s first attempt at a forecasting model based on idea that swarms of earthquakes act as precursors to main-shock events. Frank sees predictive potential of these swarms and begins to work with statistician David Rhoades.

1977 – Predicting earthquakes in the USA

The National Earthquake Hazards Reduction Program (NEHRP) is launched in the USA with a focus on earthquake prediction techniques.

1979 – Seismic gap theory – McCann et al.

A seismic gap is a period of inactivity along a fault that has been seismically active in the past. Many scientists (including McCann et al.) theorise that the likelihood of an earthquake increases with the length of seismic gap.

1982 – Generalised precursory swarm hypothesis

Based on a study of Japanese earthquakes, Frank develops a more complex version of his first prediction model. He hypothesises that clusters of precursory swarms of earthquakes are followed by clusters of main-shock events.

1984 – Code of conduct for scientists

Frank is involved in the drafting of an international code of conduct for scientists involved in earthquake prediction and becomes even more committed to rigorous testing of prediction models.

1985 – Parkfield prediction experiment

Scientists Bakun and Lindh predict that a moderate-size earthquake will occur at Parkfield, California, between 1985 and 1993. (A large earthquake did occur but not until 2004.)

1997 – Earthquakes cannot be predicted

Geller et al. publish a paper in Science claiming that earthquakes cannot be accurately predicted. They urge investment in earthquake-resistant structures and tsunami warning systems rather than earthquake prediction.

2003 – ‘Tail wags the dog’ method

Vladimir Keilis-Borok and his team at UCLA claim to have successfully predicted two earthquakes in the USA and Japan. A subsequent publicly announced prediction of a large earthquake in California proves to be a false alarm.

2004 – Precursory scale increase phenomenon

Frank and David Rhoades publish their work on the precursory scale increase phenomenon. They provide 47 examples of an increase in seismicity before large earthquakes in California, Greece, Turkey, Japan and New Zealand.

2004 – EEPAS forecasting model

David and Frank develop the EEPAS (every earthquake a precursor according to scale) forecasting model based on the precursory scale increase phenomenon. The model is tested and later used in operational forecasting in New Zealand.

2006 – Formation of CSEP

CSEP (Collaboratory for the Study of Earthquake Predictability) is established and promotes renewed international collaboration and rigorous computer testing of earthquake prediction models.

2010 – Work continues on the EEPAS model

David Rhoades continues to apply the EEPAS model to catalogues of earthquakes around the world with the goal of increasing the strength of this model.

2011 – Scientists on trial in Italy

Six Italian scientists and one government official put on trial in Italy for manslaughter after failing to predict the 6.3 magnitude earthquake of April 2009 that caused the deaths of 309 people in the Italian city of L’Aquila. In 2012 they were each sentenced to 6 years imprisonment but their convictions were overturned in 2014. Find out more here.

Image: TheWiz83 via Wikimedia Commons. Creative Commons ShareAlike 3.0 GNU Free Documentation License 1.2

BIOGRAPHY

1922 – Frank is born

Frank Foster Evison is born in Christchurch where he lives with his family until they move to Wellington in 1937. Image caption: Roger, Frank and Harry Evison, Christmas 1927

Image: Harry Evison

1937 – Life in Wellington

Attends Wellington College. A love of tramping, skiing and mountaineering develops. Image caption: Rusty Rawlings and Frank Evison (on right) on Mount Duff 1951

Image: Harry Evison

1944 – Frank graduates

Graduates from Victoria University of Wellington with a BSc in physics in 1944 and a MA with Honours in mathematics in 1946.

1939 – World War II

From 1939-1945 serves in the Royal New Zealand Air Force as the commanding officer of the radar station in Wellington for part of World War II.

1946 – Travels to Britain

Initially works at Cambridge and then gains a Diploma from the Imperial College of Science and Technology and a PhD in geophysics from the University of London.

1949 – Frank marries

Marries Joan Alpers. They go on to have three children – David, Margaret and Rosemary. Family holidays often involve trips to out-of-the-way seismographs!

1950 – Joins DSIR

Joins Geophysics Division of the Department of Scientific and Industrial Research (DSIR) and works in exploration geophysics. Discovers coal-seam guided S waves in 1955 – renamed ‘Evison waves’ in 1985.

1957 – Research gains recognition

Gains a Nuffield Fellowship in 1957 and a Fulbright Award in 1963.

Image: NIWA, www.teara.govt.nz/en/photograph/8208/leaders-in-geophysics-and-oceanography

1967 – Inaugural Professor of Geophysics

Appointed inaugural Professor of Geophysics at Victoria University of Wellington.

1971 – Establishes Institute of Geophysics

Has a vision for an interdepartmental institute with members from geology, physics, chemistry, mathematics and geography departments in addition to members outside the university.

1970 – Begins research into earthquake forecasting

Possesses a strong belief that scientists have a duty to society and that reliable earthquake prediction would help minimise loss of life and suffering. Works passionately towards this goal until his death.

1976 – Collaboration with David Rhoades

Begins work with David Rhoades, now a statistician at GNS Science. This successful partnership continues until Frank’s death.

Image: GNS Science

1979 – International work

Heads up a UNESCO conference on earthquake prediction in Paris. Helps to formulate a code of practice for earthquake prediction and chairs the Commission of Earthquake Prediction.

1988 – Frank retires

Retires as chair of the Geophysics Institute and continues as Emeritus Professor.

Image: Robert Cross, VUW Image Services

1990 – Franks wife, Joan dies

Joan had been Frank’s wife for 41 years.

1992 – Services to seismology (OBE)

Appointed as an Officer of the Most Excellent Order of the British Empire for services to seismology.

2005 – Frank dies

Passes away in his home in Wellington at the age of 82.

Image: The Wellesley Club

2006 – Scholarship established

Frank Evison Research Scholarship in Geophysics established through donations from Frank’s family, the Earthquake Commission, GNS Science, the New Zealand Geophysical Society and a range of private donors.

2008 – Evison Symposium in Wellington

Evison Symposium on Seismogenesis and Earthquake Forecasting attended by national and international scientists. Two special journals are published to honour Frank’s interest in earthquake generation and forecasting.

Rights: University of Waikato
Published: 23 February 2012