QuakeFinder

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QuakeFinder is a company focused on developing a system for earthquake prediction. QuakeFinder operates as a project of aerospace engineering firm Stellar Solutions, [1] and by subscriptions and sponsorships from the public. [2]

Contents

In the 1970s, scientists were optimistic that a practical method for predicting earthquakes would soon be found, but by the 1990s continuing failure led many to question whether it was even possible. [3] Extensive searches have reported many possible earthquake precursors, but, so far, such precursors have not been reliably identified across significant spatial and temporal scales. [4] Based on the results of this research, most scientists are pessimistic and some maintain that earthquake prediction is inherently impossible. [5]

QuakeFinder has deployed a network of sensor stations that detect the electromagnetic pulses the team believes precede major earthquakes. [6] Each sensor is believed to have a range of approximately 10 miles (16 km) from the instrument to the source of the pulses. [7] As of 2016, the company says they have 125 stations in California, [8] and their affiliate Jorge Heraud says he has 10 sites in Peru. [9] Using these sensors, Heraud says that he has been able to triangulate pulses seen from multiple sites, in order to determine the origin of the pulses. He said that the pulses are seen beginning from 11 to 18 days before an impending earthquake, and have been used to determine the location and timing of future seismic events. [10] [11]

However, insofar as a verifiable prediction would require a publicly stated announcement of the location, time, and size of an impending event before its occurrence, neither Quakefinder nor Heraud have yet verifiably predicted an earthquake, much less issued multiple predictions of the type that might be objectively testable for statistical significance.

Background

In 2010, QuakeFinder researchers said that they had observed ultra low frequency magnetic pulses emitted by the Earth near the 2007 magnitude 5.4 Alum Rock earthquake near San Jose, California, starting two weeks prior to the event. [12] Researchers from the United States Geological Survey (USGS) studied similar phenomena during the Parkfield earthquake experiment. These researchers did not find evidence of electromagnetic earthquake precursors. [13]

QuakeFinder advisor Friedemann Freund suggests that slip along a fault activates charge carriers and underground electrical currents, producing electromagnetic pulses that can be detected with magnetometers. [14] The underground currents may also cause air-conductivity changes and ground heating. QuakeFinder says that an infrared signature of the Alum Rock earthquake was detected by NASA's GOES weather satellite. [15]

The QuakeFinder team believes that the effects they are trying to study are localized in time and space, and aim to eventually be able determine "the time (within 1-2 weeks), location (within 20-40km) and magnitude (within ± 1 increment of Richter magnitude) of earthquake greater than M5.4". [16] There is no independent verification of their results so far. [6] [17]

See also

Related Research Articles

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An earthquake – also called a quake, tremor, or temblor – is the shaking of the Earth's surface resulting from a sudden release of energy in the lithosphere that creates seismic waves. Earthquakes can range in intensity, from those so weak they cannot be felt, to those violent enough to propel objects and people into the air, damage critical infrastructure, and wreak destruction across entire cities. The seismic activity of an area is the frequency, type, and size of earthquakes experienced over a particular time. The seismicity at a particular location in the Earth is the average rate of seismic energy release per unit volume.

<span class="mw-page-title-main">Seismology</span> Scientific study of earthquakes and propagation of elastic waves through a planet

Seismology is the scientific study of earthquakes and the generation and propagation of elastic waves through the Earth or other planetary bodies. It also includes studies of earthquake environmental effects such as tsunamis as well as diverse seismic sources such as volcanic, tectonic, glacial, fluvial, oceanic microseism, atmospheric, and artificial processes such as explosions and human activities. A related field that uses geology to infer information regarding past earthquakes is paleoseismology. A recording of Earth motion as a function of time, created by a seismograph is called a seismogram. A seismologist is a scientist works in basic or applied seismology.

<span class="mw-page-title-main">San Andreas Fault</span> Geologic feature in California

The San Andreas Fault is a continental right-lateral strike-slip transform fault that extends roughly 1,200 kilometers (750 mi) through the U.S. state of California. It forms part of the tectonic boundary between the Pacific plate and the North American plate. Traditionally, for scientific purposes, the fault has been classified into three main segments, each with different characteristics and a different degree of earthquake risk. The average slip rate along the entire fault ranges from 20 to 35 mm per year.

Earthquake prediction is a branch of the science of seismology concerned with the specification of the time, location, and magnitude of future earthquakes within stated limits, and particularly "the determination of parameters for the next strong earthquake to occur in a region". Earthquake prediction is sometimes distinguished from earthquake forecasting, which can be defined as the probabilistic assessment of general earthquake hazard, including the frequency and magnitude of damaging earthquakes in a given area over years or decades.

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Induced seismicity is typically earthquakes and tremors that are caused by human activity that alters the stresses and strains on Earth's crust. Most induced seismicity is of a low magnitude. A few sites regularly have larger quakes, such as The Geysers geothermal plant in California which averaged two M4 events and 15 M3 events every year from 2004 to 2009. The Human-Induced Earthquake Database (HiQuake) documents all reported cases of induced seismicity proposed on scientific grounds and is the most complete compilation of its kind.

<span class="mw-page-title-main">Parkfield earthquake</span> Series of earthquakes in California, US

Parkfield earthquake is a name given to various large earthquakes that occurred in the vicinity of the town of Parkfield, California, United States. The San Andreas fault runs through this town, and six successive magnitude 6 earthquakes occurred on the fault at unusually regular intervals, between 12 and 32 years apart, between 1857 and 1966. The latest major earthquake in the region struck on September 28, 2004.

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A slow earthquake is a discontinuous, earthquake-like event that releases energy over a period of hours to months, rather than the seconds to minutes characteristic of a typical earthquake. First detected using long term strain measurements, most slow earthquakes now appear to be accompanied by fluid flow and related tremor, which can be detected and approximately located using seismometer data filtered appropriately. That is, they are quiet compared to a regular earthquake, but not "silent" as described in the past.

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.

Episodic tremor and slip (ETS) is a seismological phenomenon observed in some subduction zones that is characterized by non-earthquake seismic rumbling, or tremor, and slow slip along the plate interface. Slow slip events are distinguished from earthquakes by their propagation speed and focus. In slow slip events, there is an apparent reversal of crustal motion, although the fault motion remains consistent with the direction of subduction. ETS events themselves are imperceptible to human beings and do not cause damage.

<span class="mw-page-title-main">Didier Sornette</span> French researcher

Didier Sornette is a French researcher studying subjects including complex systems and risk management. He is Professor on the Chair of Entrepreneurial Risks at the Swiss Federal Institute of Technology Zurich and is also a professor of the Swiss Finance Institute, He was previously a Professor of Geophysics at UCLA, Los Angeles California (1996–2006) and a Research Professor at the French National Centre for Scientific Research (1981–2006).

Seismo-electromagnetics are various electro-magnetic phenomena believed to be generated by tectonic forces acting on the Earth's crust, and possibly associated with seismic activity such as earthquakes and volcanoes. Study of these has been prompted by the prospect they might be generated by the increased stress leading up to an earthquake, and might thereby provide a basis for short-term earthquake prediction. However, despite many studies, no form of seismo-electromagnetics has been shown to be effective for earthquake prediction. A key problem is that earthquakes themselves produce relatively weak electromagnetic phenomena, and the effects from any precursory phenomena are likely to be too weak to measure. Close monitoring of the Parkfield earthquake revealed no significant pre-seismic electromagnetic effects. However, some researchers remain optimistic, and searches for seismo-electromagnetic earthquake precursors continue.

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<span class="mw-page-title-main">Earthquake cycle</span> Natural phenomenon

The earthquake cycle refers to the phenomenon that earthquakes repeatedly occur on the same fault as the result of continual stress accumulation and periodic stress release. Earthquake cycles can occur on a variety of faults including subduction zones and continental faults. Depending on the size of the earthquake, an earthquake cycle can last decades, centuries, or longer. The Parkfield portion of the San Andreas fault is a well-known example where similarly located M6.0 earthquakes have been instrumentally recorded every 30–40 years.

<span class="mw-page-title-main">Dimitar Ouzounov</span> Bulgarian-American geophysicist

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References

  1. "Quakefinder Mission" . Retrieved 13 November 2016.
  2. Note however that, according to IRS Publication 78 ("Cumulative List of Organizations described in Section 170(c) of the Internal Revenue Code of 1986" ) Quakefinder is not a tax-exempt organization.
  3. Geller et al. 1997 , p. 1617; Geller 1997, §2.3, p. 427; Console 2001, p. 261.
  4. Geller 1997 , Summary.
  5. Kagan 1997b; Geller 1997. See also Nature Debates; Uyeda, Nagao & Kamogawa 2009. "...at the present stage, the general view on short-term prediction is overly pessimistic. There are reasons for this pessimism because mere conventional seismological approach is not efficient for this aim. Overturning this situation is possible only through multi-disciplinary science. Despite fairly abundant circumstantial evidence, pre-seismic EM signals have not yet been adequately accepted as real physical quantities."
  6. 1 2 John Upton (13 August 2011). "Pursuing the Grail of an Earthquake Predictor, but Facing Skeptics". The New York Times. Retrieved 28 August 2011.
  7. Lisa Sibley (25 March 2011). "QuakeFinder's mission: Detect quakes before they shake". Silicon Valley / San Jose Business Journal. American Cities Business Journals. Retrieved 30 September 2011.
  8. "Quakefinder Blog". QuakeFinder. 2016. Retrieved 19 November 2016.
  9. Heraud, Jorge (2016). "presenter bio". Singularity University Summit. Retrieved 19 November 2016.
  10. Heraud, J. A.; Centa, V. A.; Bleier, T. (1 December 2015). "Electromagnetic Precursors Leading to Triangulation of Future Earthquakes and Imaging of the Subduction Zone". AGU Fall Meeting Abstracts. 32: NH32B–03. Bibcode:2015AGUFMNH32B..03H.
  11. Enriquez, Alberto (2015). "Earthquake-prediction technology deserves to be taken seriously (OPINION)". OregonLive.com. Retrieved 19 November 2016.
  12. Bleier, T.; Dunson, C. (2010). "Correlation of pre-earthquake electromagnetic signals with laboratory and field rock experiments" (PDF). Nat. Hazards Earth Syst. Sci. 10 (9): 1965–1975. Bibcode:2010NHESS..10.1965B. doi: 10.5194/nhess-10-1965-2010 . Retrieved 30 September 2011.
  13. "The Parkfield, California Earthquake Experiment". United States Geological Survey. Retrieved 29 August 2011.PD-icon.svg This article incorporates text from this source, which is in the public domain .
  14. Freund, F. T.; Takeuchi, A.; Lau, B. W. (2006). "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. Bibcode:2006PCE....31..389F. doi:10.1016/j.pce.2006.02.027.
  15. Quakefinder (20 June 2009). "QuakeFinder Detects Quake: Pre-Quake Signatures Detected by QuakeFinder and NASA". SpaceRef.com. Retrieved 30 September 2011.
  16. Bleier, T. E.; Dunson, C.; Roth, S.; Heraud, J.; Freund, F. T.; Dahlgren, R.; Bryant, N.; Bambery, R.; Lira, A. (December 2010). "Current progress in using multiple electromagnetic indicators to determine location, time, and magnitude of earthquakes in California and Peru". AGU Fall Meeting Abstracts. 2010. American Geophysical Union: NH24A–02. Bibcode:2010AGUFMNH24A..02B. abstract #NH24A-02.
  17. John Upton (15 August 2011). "The Science of Predicting Earthquakes: U.S. Geological Survey refuses to fund controversial research into electromagnetic signals". The Bay Citizen. The New York Times. Archived from the original on 25 September 2011. Retrieved 28 August 2011.

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Further reading