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Pre-Earthquake Signals at the Ground Level

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Universe of Scales: From Nanotechnology to Cosmology

Part of the book series: Springer Proceedings in Physics ((SPPHY,volume 150))

Abstract

Can we really predict earthquakes? Will we be able to do it sometime? The answer to the first question is no, we still cannot predict earthquakes but we seem to be moving in the right direction. At the ground level, several electromagnetic manifestations previous to rupture, are slowly fitting into place.

The main theme in this chapter is luminescence and the prevailing hypothesis in the case described here is the electric origin of the phenomenon commonly known as EarthQuake Lights, or EQLs. The difficulty of dealing with luminescence nowadays is separating any EQLs from noise arising from artificial lights, electric short circuits, sparks, even fire from electric power lines, from substations, circuit breakers and the like. The San Lorenzo Island off the coast of Lima, Peru has provided three very outstanding cases of pre-seismic and co-seismic EQLs—with geological consistency—spanning 266 years of observation, including two high magnitude earthquakes. In addition there are three cases linked to low magnitude events with close-by hypocenters, about 2 km, which produces pre-earthquake EQLs on the island. In these cases, the high stress resulting from the build-up of a large magnitude earthquake produced a 21-day anticipation of the EQLs, whereas the low magnitude earthquake gave rise to a short 38 hours lead time. New picture evidence collected at San Lorenzo island show rock formations at an old colonial times prison reported to have been the focus of luminescence evidence before the mega earthquake in 1746. In 2007, a strong M8.0 earthquake 160 km away from the island, produced co-seismic lights, probably via the local activation of positive hole carriers by passing seismic waves, specifically S waves, igneous rocks forming vertical dykes in the bay of Lima.

Videos taken by security cameras on the PUCP campus show a very good time correlation with ground acceleration records from a seismometer located on the campus. Videos from an off-campus location show lights that were generated at a hill at the southern end of the city and were confirmed by qualified eyewitnesses. Observations from the San Lorenzo Island point to the possibility that small rocky islets in the Bay could have been the points of origin of columns of light seemingly arising out of the ocean.

The deployment of magnetometers, in collaboration with Quakefinder, is currently building up a station network along the seismically very active Southern Peruvian coast. All in all, at least on this side of this subcontinent, luminescence seems to be coupled with the generation and transport of electric charges.

The answer to the question whether it will be able to predict earthquakes sometimes in the future is strongly linked to our ability to (i) understand the physics of rocks under stress and (ii) develop a worldwide network of ground stations to collect and process multivariate data that will allow for meaningful deductions of the data leading to predictions. This is the final quest. Wiring different types of sensors to monitor electromagnetic activity prior to earthquakes is the geophysical equivalent to an electrocardiogram except that is aimed at anticipating impending catastrophic seismic activity. Rather than just sensing the passing of mechanical waves, as cardiologists do by “feeling” the cardiac pulse at the wrist, a worldwide web of monitoring stations, combined with the Internet, might bring us early warning signs pointing at future heart attacks of mother Earth.

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References

  1. F. Freund, Toward a unified solid state theory for pre-earthquake signals. Acta Geophys. 58(5), 719–766 (2010). Institute of Geophysics, Polish Academy of Sciences

    Article  ADS  MathSciNet  Google Scholar 

  2. C.F. Richter, Elementary Seismology (W.H. Freeman and Company, San Francisco, 1958), pp. 132–133

    Google Scholar 

  3. T. Terada, On luminous phenomena accompanying earthquakes. Proc. Imp. Acad. Jpn. 6, 401–403 (1930)

    Google Scholar 

  4. T. Terada, On Luminous Phenomena Accompanying Earthquakes, vol. 9 (Bulletin Earthquake Research Institute, Tokyo University, Tokyo, 1931), pp. 225–254

    Google Scholar 

  5. J.S. Derr, Earthquake lights: a review of observations and present theories. Bull. Seismol. Soc. Am. 63(6), 2177–2187 (1973)

    Google Scholar 

  6. G.A. Papadopoulos, Luminous and Fiery phenomena associated with earthquakes in the East Mediterranean, in Ionospheric Electromagnetic Phenomena Associated with Earthquakes, ed. by M. Hayakawa (Atmospheric & TERRAPUB, Tokyo, 1999), pp. 559–575

    Google Scholar 

  7. F. St. Laurent, The Seguenay, Quebec earthquake lights of Nov. 1988–Jan. 1989. Seismol. Res. Lett. 71(2), 160–174 (2000)

    Article  Google Scholar 

  8. J.A. Heraud, J.A. Lira, Co-seismic Luminescence in Lima, 150 km from the epicenter of the Pisco, Peru earthquake of 15 August 2007. Nat. Hazards Earth Syst. Sci. 11, 1025–1036 (2011)

    Article  ADS  Google Scholar 

  9. D. de Esquivel y Navia, Noticias Cronológicas de la Gran Ciudad del Cuzco, Tomo II, Fundación Augusto N. Wiese (Banco Wiese, Ltdo., Lima, 1980). Biblioteca Peruana de Cultura Printed in Lima, Peru, Talleres Graficos, P.L., Villanueva, S.A., Chap. XXXVIII, p. 360. The Lima Earthquake, 1746 (translation from Spanish)

    Google Scholar 

  10. P.E. Perez-Mallaina, Retrato de una Ciudad en Crisis. La Sociedad Limeña ante el Movimiento Sismico de 1746 (Pontificia Universidad Catolica del Peru, Instituto Riva Agüero, Lima, 2001), 393 pp.

    Google Scholar 

  11. Mercurio Peruano (newspaper), III, 95, folios 239–240, Lima (1791)

    Google Scholar 

  12. C.F. Walker, Shaky Colonialism/The 1746 Earthquake—Tsunami in Lima, Peru and Its Long Aftermath (Duke University Press, Durham & London, 2008)

    Book  Google Scholar 

  13. H. Tavera, I. Bernal, Distribución espacial de áreas de ruptura y lagunas sísmicas en el borde oeste del Perú. Bol. Soc. Geol. Perú 6, 89–102 (2005)

    Google Scholar 

  14. H. Tavera, I. Bernal, H. Salas, El Sismo de Pisco del 15 de Agosto, 2007 (7.9 Mw), Departamento de Ica, Perú (Preliminary Report). Instituto Geofísico del Perú, Lima, Peru, August, 5–47 (2007)

    Google Scholar 

  15. L. Ocola, U. Torres, Testimonios y Fenomenología de la Luminiscencia Cosísmica del Terremoto de Pisco del 15 de Agosto 2007. Instituto Geofísico del Perú, http://www.igp.gob.pe/sismologia/libro/trabajo_19.pdf (2007)

  16. Institute for Radio Astronomy, Pontificia Universidad Catolica del Peru (INRAS-PUCP) Video of Earthquake Lights recorded at the PUCP campus, Lima, Peru, during the Pisco earthquake of August 15, 2007. http://www.pucp.edu.pe/inras/peru-magneto/mod-3cam-3.exe

  17. A. Takeuchi, Y. Futada, K. Okubo, N. Takeuchi, Positive electrification on the floor of an underground mine gallery at the arrival of seismic waves and similar electrification on the surface of partially stressed rocks in laboratory. Terra Nova 22(3), 203–207 (2004)

    Article  Google Scholar 

  18. M.M. Freund, F. Freund, F. Batllo, Highly mobile oxygen holes in magnesium oxide. Phys. Rev. Lett. 63, 2096–2099 (1989)

    Article  ADS  Google Scholar 

  19. F. Freund, Charge generation and propagation in rocks. J. Geodyn. 33(4–5), 545–572 (2002)

    Google Scholar 

  20. F.T. Freund, A. Takeuchi, B.W. Lau, Electric currents streaming out of stressed igneous rocks—a step towards understanding pre-earthquake low frequency EM emissions. Phys. Chem. Earth 31(4–9), 389–396 (2006)

    Article  Google Scholar 

  21. J.C. Dunson, T.E. Bleier, S. Roth, J.A. Heraud, C.H. Alvarez, J.A. Lira, The Pulse Azimuth effect as seen in induction coil magnetometers located in California and Peru 2007–2010, and its possible association with earthquakes. Nat. Hazards Earth Syst. Sci. 11, 2085–2105 (2011)

    Article  ADS  Google Scholar 

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Acknowledgements

I want to express my recognition to the late Mino Freund, whose dedicated work in various areas of his scientific interest, brought all of us together in this book. From the multidisciplinary symposium held in NASA Ames Research Center on August 10, 2012, it was clear that the broad view Mino had and his enthusiasm for science was the catalyst for a group of scientists in discussing together topics that mixed and matched superbly. My thanks to Friedemann Freund for the honor of being invited to participate.

Part of this work, pertaining to the co-seismic observations in Lima in 2007, was published together with Juan A. Lira. My thanks to Carlos Sotomayor of PUCP for providing me the video recording obtained on the PUCP campus, to CORPAC, the Peruvian Aeronautical Authority and qualified witnesses like air traffic controller Jorge Merino and pilot Giancarlo Crapesi, lieutenant Guillermo Zamorano of the Peruvian Navy, Juan Salas, chief security officer of LAP, the Lima Airport operators and the Larcomar shopping center. I would also like to thank seismologists Daniel Huaco of CERESIS (Regional Seismology Center for South America) and Leonidas Ocola, professor at San Marcos University in Lima. My thanks to Silvia Rosas, Professor and head of the Mining and Geology area at PUCP for her interpretations of the geological maps of the bay of Lima, as well as INRAS research assistants Neils Vilchez and Daniel Menendez for their participation in the experimental work and Victor Centa for the programming and signal processing. Useful discussions were also held with Thomas Bleier of Quakefinder and Friedemann Freund of the SETI Institute, France St-Laurent and Robert Theriault. Pictures of the San Lorenzo prison were taken during a trip to the island supported by the Peruvian Navy. We are indebted to Quakefinder for providing us with magnetometers and to Telefonica del Peru for the donation of the magnetometer now installed at San Lorenzo island, modems and indefinite airtime for getting the data from our magnetometers via cellular 3G data links.

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Correspondence to Jorge A. Heraud P. .

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Heraud P., J.A. (2014). Pre-Earthquake Signals at the Ground Level. In: Freund, F., Langhoff, S. (eds) Universe of Scales: From Nanotechnology to Cosmology. Springer Proceedings in Physics, vol 150. Springer, Cham. https://doi.org/10.1007/978-3-319-02207-9_16

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