James A. Jackson

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James Jackson
Born (1954-12-12) 12 December 1954 (age 69)
NationalityBritish
Alma mater University of Cambridge
Scientific career
Fields Geophysics
Doctoral advisor Dan McKenzie

James Anthony Jackson CBE FRS (born 12 December 1954) is Emeritus Professor of Active Tectonics and formerly head of Bullard Laboratories, and Head of the Department of Earth Sciences, Cambridge University. He made his name in geophysics, using earthquake source seismology to examine how continents are deformed. His central research focus is to observe the active processes shaping our continents. [1]

Contents

Education and career

Jackson was born and raised in India, which probably established his interest in all aspects of Asia, which is where much of his current research has been concentrated. He was sent back to boarding school in the UK for his education. [2]

Jackson attended the University of Cambridge from 1973 graduating with a 1st Class degree in geology in 1976. Then, under the tutelage of Dan McKenzie at the Bullard Laboratories, Cambridge, he received his PhD in 1980. His research was within geophysics and used earthquakes to study the processes that produce the major surface features of the continents, such as mountain belts and basins. It included field work with seismometers in Iran and with the Seismic Discrimination Group at the Massachusetts Institute of Technology. [2] [3]

Between 1977 and 1981 he was a visiting scientist in the Seismic Discrimination Group at MIT before returning to Cambridge to take up a research fellow position in Queens' College, Cambridge, where he became Assistant Dean in 1983. In 1984, he was appointed as an assistant lecturer in the Department of Earth Sciences, Cambridge, lecturer in 1988 and reader in 1996. He was made Professor of Active Tectonics in the Department of Earth Sciences in 2003. [4]

Communicating about the implications of his research for resilience against earthquakes, and about geophysics and earthquakes, to both societies at large and organisations has been an important part of his work. In 1995 he gave the televised Royal Institution Christmas Lectures. In 2023 he was a guest on the BBC Radio 4 programme The Life Scientific. [3]

Current research

Using evidence from earthquakes, remote sensing, geodesy and geomorphology he is able to observe, quantitatively, the geometry and rates of deformation processes while they are active. [1] In addition to seismology, his current research uses space-based remote sensing (including radar interferometry, GPS measurements and optical imagery) combined with observations of the landscape in the field, to study the evolution and deformation of the continents on all scales, from the movement of individual faults in earthquakes to the evolution of mountain belts. [2]

Much of his work is carried out in collaboration with researchers from the COMET Project [5] where he is associate director.

Selected publications

Awards

Related Research Articles

<span class="mw-page-title-main">Geophysics</span> Physics of the Earth and its vicinity

Geophysics is a subject of natural science concerned with the physical processes and physical properties of the Earth and its surrounding space environment, and the use of quantitative methods for their analysis. Geophysicists, who usually study geophysics, physics, or one of the Earth sciences at the graduate level, complete investigations across a wide range of scientific disciplines. The term geophysics classically refers to solid earth applications: Earth's shape; its gravitational, magnetic fields, and electromagnetic fields ; its internal structure and composition; its dynamics and their surface expression in plate tectonics, the generation of magmas, volcanism and rock formation. However, modern geophysics organizations and pure scientists use a broader definition that includes the water cycle including snow and ice; fluid dynamics of the oceans and the atmosphere; electricity and magnetism in the ionosphere and magnetosphere and solar-terrestrial physics; and analogous problems associated with the Moon and other planets.

<span class="mw-page-title-main">Tectonics</span> Process of evolution of the Earths crust

Tectonics are the processes that result in the structure and properties of the Earth's crust and its evolution through time. The field of planetary tectonics extends the concept to other planets and moons.

<span class="mw-page-title-main">Eurasian Plate</span> Tectonic plate which includes most of the continent of Eurasia

The Eurasian Plate is a tectonic plate that includes most of the continent of Eurasia, with the notable exceptions of the Indian subcontinent, the Arabian subcontinent and the area east of the Chersky Range in eastern Siberia. It also includes oceanic crust extending westward to the Mid-Atlantic Ridge and northward to the Gakkel Ridge.

Dan Peter McKenzie is a Professor of Geophysics at the University of Cambridge, and one-time head of the Bullard Laboratories of the Cambridge Department of Earth Sciences. He wrote the first paper defining the mathematical principles of plate tectonics on a sphere, and his early work on mantle convection created the modern discussion of planetary interiors.

Earthquake forecasting is a branch of the science of seismology concerned with the probabilistic assessment of general earthquake seismic hazard, including the frequency and magnitude of damaging earthquakes in a given area over years or decades. While forecasting is usually considered to be a type of prediction, earthquake forecasting is often differentiated from earthquake prediction, Earthquake forecasting estimates the likelihood of earthquakes in a specific timeframe and region, while earthquake prediction attempts to pinpoint the exact time, location, and magnitude of an impending quake, which is currently not reliably achievable.Wood & Gutenberg (1935). Kagan says: "This definition has several defects which contribute to confusion and difficulty in prediction research." In addition to specification of time, location, and magnitude, Allen suggested three other requirements: 4) indication of the author's confidence in the prediction, 5) the chance of an earthquake occurring anyway as a random event, and 6) publication in a form that gives failures the same visibility as successes. Kagan & Knopoff define prediction "to be a formal rule where by the available space-time-seismic moment manifold of earthquake occurrence is significantly contracted ...."</ref> Both forecasting and prediction of earthquakes are distinguished from earthquake warning systems, which, upon detection of an earthquake, provide a real-time warning to regions that might be affected.

Mary Lou Zoback is an American geophysicist and seismologist. A specialist in tectonic stress and natural hazards risks, she spent most of her career as a research scientist with the United States Geological Survey. Zoback chaired the World Stress Map project of the International Lithosphere Program from 1986 to 1992. Zoback served on the U.S. Nuclear Waste Technical Review Board from 2012 to 2018.

<span class="mw-page-title-main">Paul Silver</span> American seismologist (1948–2009)

Paul Gordon Silver was an American seismologist. A member of the research staff at the Department of Terrestrial Magnetism of the Carnegie Institution of Washington since 1982, Paul Silver made a series of important contributions to the investigation of seismic anisotropy and to earthquake research by observing the slow redistribution of stress and strain along fault zones.

<span class="mw-page-title-main">Outline of geophysics</span> Topics in the physics of the Earth and its vicinity

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<span class="mw-page-title-main">Kathryn Whaler</span> Geophysicist

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Derek Keir has been an associate professor of geophysics at the University of Southampton since 2015. In 2013 he received the Bullerwell Lecture award from the British Geophysical Association (BGA) for significant contributions to geophysics.

Volcano tectonics is a scientific field that uses the techniques and methods of structural geology, tectonics, and physics to analyse and interpret physical processes and the associated deformation in volcanic areas, at any scale.

Alik Ismail-Zadeh is a mathematical geophysicist known for his contribution to computational geodynamics and natural hazard studies, pioneering work on data assimilation in geodynamics as well as for outstanding service to the Earth and space science community. He is Senior Research Fellow at the Karlsruhe Institute of Technology in Germany.

Éric Calais is a French geologist-geophysicist, born in 1964, internationally recognized practitioner of high-precision space geodesy and a pioneer in its applications to measure seismic deformations at the boundaries of tectonic plates and in their interiors. He has been a member of the French Academy of Sciences since 2017.

<span class="mw-page-title-main">Oblique subduction</span> Tectonic process

Oblique subduction is a form of subduction for which the convergence direction differs from 90° to the plate boundary. Most convergent boundaries involve oblique subduction, particularly in the Ring of Fire including the Ryukyu, Aleutian, Central America and Chile subduction zones. In general, the obliquity angle is between 15° and 30°. Subduction zones with high obliquity angles include Sunda trench and Ryukyu arc.

The 1858 Prome earthquake occurred on August 24 at 15:38 local time in British Burma. The earthquake occurred with a magnitude of 7.6–8.3 on the moment magnitude scale. It had an epicenter in near the city of Pyay (Prome), Bago. The shock was felt with a maximum Modified Mercalli intensity of XI (Extreme) for about one minute. Severe damage was reported in Bago, and off the coast of Rakhine, an island sunk.

The 1957 Alborz earthquake struck northern Iran's Mazandaran province at 04:12 local time on 2 July. It had a moment magnitude (Mw ) of 7.1 and occurred at a focal depth of 15 km (9.3 mi). The thrust-faulting shock was assigned a maximum Modified Mercalli intensity of IX (Violent). It devastated 120 villages in the Alborz Mountains and caused an estimated 1,500 fatalities. The earthquake also triggered landslides including one that dammed the Haraz River. Some damage was also reported in Tehran, Qaem Shahr and Sari. The total damage was estimated at US$25 million.

Susan Marian Ellis is a geophysicist based in New Zealand, who specialises in modelling the geodynamics of the Earth's crust deformation, at different scales. Ellis is a principal scientist at GNS Science and her main interests are in subduction, seismology, tectonics, crust and petrology. Ellis's current work focuses on the influence of faulting on stresses in the crust, and how this is related to geological hazard and the tectonic settings in New Zealand.

Juliet J. Biggs is a British geologist who is Professor of Earth Sciences at the University of Bristol. Her research uses satellite geodesy and interferometric synthetic-aperture radar (InSAR) to understand the physics of the Earth's crust. She was awarded the American Geophysical Union John Wahr Award in 2017 and a European Research Council (ERC) consolidator grant in 2020.

Ernest Henry Rutter is a British geologist and geophysicist. He is known for his research on structural geology and the physics of natural rock deformation.

References

  1. 1 2 "James Jackson's profile on the COMET Project web site". Archived from the original on 9 January 2009. Retrieved 5 August 2008.
  2. 1 2 3 Darwin College Lecture Series
  3. 1 2 "Understanding earthquakes and building resilience" . Retrieved 21 March 2023.
  4. University of Cambridge Annual Report, 2003: Awards and prizes and appointments
  5. COMET Project
  6. "Bullerwell Lecturers and Lectures".
  7. "The UK's 100 leading practising scientists". 17 January 2014.
  8. "Wollaston Medal". Geological Society of London . Retrieved 30 August 2015.
  9. "The Wollaston Medal 2015 citation & reply". Geological Society of London . Retrieved 30 August 2015.
Academic offices
Preceded by Head of Department of Earth Sciences, University of Cambridge
2008 - 2016
Succeeded by