Open Letter to the scientific community, to the decision makers and to the public
April 2007
How far along are we in
Understanding Pre-Earthquake Signals?

Friedemann T. Freund
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Principal Investigator, Carl Sagan Center, SETI Institute
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NASA Ames Research Center, MS 242-4
MOFFETT FIELD, CA 94035-1000
Tel (at NASA) 650 604-5183
Tel (at CSC) 650 810-0218
Cell 650 279-8478
e-mail ffreund@mail.arc.nasa.gov
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Department of Physics
San Jose State University


Earthquakes cause enormous destruction. They cause (and have caused in Turkey) the death of tens of thousands of people. They cause (and have caused in Turkey) billions of dollars in economic damage.


The next major earthquake is sure to come. It may turn out to be the most disastrous in Turkish history.
Earthquakes are feared because they seem to strike so suddenly. Many seismologists say that such cataclysmic events are inherently unpredictable.
To put this into perspective, we need to remind ourselves that seismologists use earthquakes as “flash lights” to illuminate the Earth’s interior. By analyzing the seismic waves and understanding how they propagate, seismologists have developed sophisticated tools to uncover the hidden structures of our dynamic planet. They have done a marvelous job for which they deserve our unmitigated appreciation.

However, when it comes to earthquake prediction, the tools developed by seismologists are blunt. They are blunt because the seismological approach to earthquake risk is retrospective: look at past events and calculate the probability of future events during, for instance, the next 7 or next 30 years.
This backward-looking approach is deeply unsatisfactory.

Those who say that earthquakes are unpredictable do not face up to an inconvenient truth: Earthquake prediction depends not only on the history of past seismic events but also – and even more so – on the processes that unfold in real time deep in the Earth’s crust.

It has been known for decades, even centuries, that the Earth sends out signals before major seismic events – a bewildering multitude of signals, sometimes distinct, more often subtle and patchy:

(i) Perturbations in the ionosphere 100-300 km above the ground,
(ii) Changes in the atmosphere near the ground and at altitudes up to about 1000 m,
(iii) Enhanced infrared emission from the epicentral region visible in night-time satellite images,
(iv) Low-ultralow frequency electromagnetic emissions recorded all around the globe,
(v) Local magnetic field variations,
(vi) Strange animal behavior,
(vii) and others…

Until recently the scientific community had been unable to explain, not even in a broad brush, how the different types of signals may be generated. Nobody had been able to provide a physical basis for these signals and describe how they may be related or interconnected.


FFreund: Pre-Earthquake Signals 2

The last two years have brought major progress in our insight into the processes deep in the Earth that seem to be responsible for the generation of most, if not all of the pre-earthquake signals listed above.
Key is the discovery that, when igneous rocks are subjected to stress, dormant electronic charge carriers are activated. As a consequence of this activation process the stressed rock volume turns into a battery from where electric currents can flow out (Freund and Sornette, 2007; Freund et al., 2006).

These currents can be quite strong. According to laboratory data, every cubic kilometer of rock that is being stressed can deliver up to 10,000 –100,000 Amps flowing for extended periods of time. What is even more surprising, these currents can flow through thick layers of rock. Their charge carriers pass through loose or consolidated sand and soil. They are not stopped by water. They probably travel over distances on the order of kilometers or tens of kilometers. The same charge carriers cause the surface of the rocks studied in the laboratory – and presumably the surface of the Earth – to become positively charged. This charge may be strong enough to affect the
ionosphere and lead to the widely reported pre-earthquake ionospheric perturbations (Liu et al., 2006).

The same charge carriers generate microscopically small but very steep electric fields at the surface, sufficient to spontaneously ionize the air (Freund, 2003). If the water vapor pressure in the atmosphere is in the right range, the airborne ions can cause the condensation of water droplets and, hence, cloud formation. If the number of charge carriers streaming to the surface increases further, sparking and corona discharges can occur that lead to the emission of visible light and to the emission of broad-band radio noise (Freund, 2002).

When the same charge carriers recombine at the surface, they form vibrationally highly excited, “hot” atoms that de-excite by emitting a tell-tale spectrum of mid-infrared photons (Freund et al., 2007). This newly discovered emission process may be responsible for strange pre-earthquake “thermal anomalies” captured in night-time infrared satellite images.
Though mainstream science has not yet caught up with the rapid developments at the scientific front, we are well on our way to unravel the mystery of the pre-earthquake signals. We begin to understand what these signals are, how they are generated and what they can tell us about the dangers lurking deep in the Earth. One thing is for sure: Pre-earthquake signals are not the invention of some crazy fringe scientists or of old village folk who want to tell tall tales. They are real physical phenomena.

Saying – as many in the seismological community have done in the past and continue to do – that preearthquake signals are untrustworthy or don’t even exist, is morally and scientifically irresponsible.

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Freund, F.T. 2002. Charge generation and propagation in rocks. Journal of Geodynamics, 33: 545-572.
Freund, F.T., 2003. Rocks that crackle and sparkle and glow – Strange pre-earthquake phenomena.
Journal of Scientific Exploration, 17: 37-71.
Freund, F.T. and Sornette, D., 2007. Electromagnetic earthquake bursts and critical rupture of peroxy bond networks in rocks. Tectonophysics, 431: 33-47.
Freund, F.T., Takeuchi, A. and Lau, B.W., 2006. Electric currents streaming out of stressed igneous rocks - A step towards understanding pre-earthquake low frequency EM emissions. Physics and Chemistry of the Earth, 31: 389-396.
Freund, F.T. et al., 2007. Stimulated thermal IR emission from rocks: Assessing a stress indicator. eEarth, 2: 1-10.
Liu, J.Y. et al., 2006. Seismo-geomagnetic anomalies and M5.0 earthquakes observed in Taiwan during 1988-2001. Physics and Chemistry f the Earth, 31: 215-222

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