# Patent

## Title
Earthquakes and sun disturbances

## Abstract

A method of tracking seismic activity through monitoring sunspots and sun disturbances and correlating them with a developed model in order to map out specific locations where an earthquake will consequently appear is provided (FP). The method of comprises mapping coordinates of electromagnetic disturbances on the sun, calculating the coordinates while taking into consideration Earth/sun geometry and relative positions (FP). These coordinates are consequently mapped to a location and time on earth wherein the location and time predicts the location and approximate time of the earthquake, which will consequently occur on earth.

## Background
CROSS-REFERENCE TO RELATED APPLICATIONS
The present application is the U.S. National Phase of International Patent Application No. PCT/IL2006/001061, filed Sep. 9, 2006, which in turn is based upon and claims priority from U.S. Provisional Patent Application Ser. No. 60/716,345, filed Sep. 12, 2005, each of which is incorporated by reference in its entirety.


FIELD OF THE INVENTION
The present invention relates to tracing seismic activities. More particularly, the present invention relates to tracing seismic activities that are directly connected to sunspots and sun disturbances.
BACKGROUND OF THE INVENTION
Earthquakes are natural disasters generated by seismic waves and tectonic pressure. They are currently understood to be unpredictable and can be very destructive. Statistics show that during one year, more than 20-30 cases of strong and destructive earthquakes occur over the whole planet.
The time and location of earthquakes are understood to be non-predictable and are one of the major concerns in the world. The consequences may be harsh due to the destructive nature of the earthquake itself, as well as from its secondary effects such as fires, pollution, floods, etc.
At this time science is unable to predict the exact time and location of an earthquake through current scientific methods.
From all of the planets in our solar system, Earth is unique and is the only planet to exhibit tectonic activity (other similar planets, such as Mars and Venus, show signs of volcanic activity in the past but there appears to be no evidence of tectonic activity neither in the past nor today). The earth's crust is divided up into tectonic plates that move around the lithosphere. These plates buckle and grind up against each other at the edges. These plates are constantly active (due to convection processes that cause different phase changes by the core's heat, gravity and radioactive emissions from within the Earth). These different forces act together to cause earthquakes.
Before an earthquake takes place, the pressure and friction between the rocks builds up until it reaches a ‘critical point’ (the Earth's crust is made up from different minerals; mostly containing oxygen, that are locked into crystals). Electro-magnetic pulses are generated through these minerals (see, for example, in Freidman, January December 2005 and Brent D. Johnson, Spectrophotometer Observes Radiation from Rocks, (accessed 23.12.05) and are released into the Earth's atmosphere. The electromagnetic pulses that are emitted from Earth's crust into the atmosphere are characterized by coherent light and continue their spectral signature when they hit the sun's photosphere. Reed et al. in THz Science and Technology Network, terahertz (THz) radiation, Physical Review Letters, 13 Jan. 2006 found that measurable coherent light can be observed emerging from the crystal in experiments, whereby coherent light was produced by shock waves through a crystal.
The sun's photosphere is a thin layer that is highly sensitive to electro-magnetic changes (like the Earth's ionosphere). The model correlates sunspot disturbances and maps them to relative locations on Earth. In addition, the pattern of these disturbances, outlined in the EMI archive, exhibits unique characteristics that emanate from different source locations from Earth (drawing on crystallography, spectroscopia, and optical non-linearity).
In this way, the Earth may be compared to a pulsing projector (like a pulsar) where the sun acts as a responsive surface reflecting the pulses that leave their traces on its photosphere.
Scientific research has been driven by the relative size and energy levels of the Earth in relation to the sun, which has influenced past and current scientific research to explore the effect of the sun on the Earth. Notably, fewer sunspot activities have been recorded during The Little Ice Age (See FIG. 8a) but the exact relationship between sun disturbances and earthquakes has not been previously understood. The inventor of the present invention has developed a model that reverses the pre-supposition that the sun is acting on the earth, and suggests that the sun is exhibiting traces that are initiated on Earth. These traces can be identified as sun disturbances that evolve as local reactions that act in response to the trigger, which is the pre-earthquake activity.
In accordance with that, it must be presumed that the increase in seismic activity correlates directly with the number and specific location of sun disturbances taking into consideration the influences of the seasonal changes of the magnetic poles of the sun and their relationship to Earth. The correlation may be discerned once the properties of the declination, Earth's inclination, and the sun's BO angle between the Earth and the sun are determined. The disturbances may then be mapped to the past or potential location of an Earthquake epicentre. Using this 10-step model that is illustrated in FIG. 1, the inventor of the present invention tracked sun disturbances and cross-checked them over a period of four years to illustrate an occurring frequency, relative location, and global pattern as will be shown herein after. The model enables a correlation of the pertinent data and demonstrates not only a documentation of past earthquake activity, but can also be successfully implemented to predict future earthquake activity.
SUMMARY OF THE INVENTION
It is an object of the present invention to provide a method of tracking seismic activity through monitoring sunspots and sun disturbances and correlating them with the developed model in order to map out specific locations where an earthquake will consequently appear.
Therefore and in accordance with a preferred embodiment of the present invention, it provides a method of correlating earthquakes on earth to electromagnetic disturbances on the sun comprising:

    
    
        mapping coordinates of electromagnetic disturbances on the sun;
        calculating said coordinates;
        mapping the calculated coordinates onto a location and time on earth;
        whereby the location and time on earth predicts the location and approximate time of the earthquake which will consequently occur on earth.
    
    


Furthermore, in accordance with another preferred embodiment of the present invention, the electromagnetic disturbances are based on those observed on EIT images.
Furthermore, in accordance with another preferred embodiment of the present invention, the electromagnetic disturbances are based on those observed on a magnetogram image.
Furthermore, in accordance with another preferred embodiment of the present invention, said mapping coordinates is performed by marking the disturbances on a transparency of sun's diameter on a grid and transferring the marked coordinated onto a broadsheet.
Furthermore, in accordance with another preferred embodiment of the present invention, said mapping the calculated coordinates is performed by marking said coordinates on a scaled BO transparency divided into lines of latitude.
Furthermore, in accordance with another preferred embodiment of the present invention, said location is determined from the line of latitude using a model in which an angle of declination of a corresponding day is adjusted to the indications of sunspot disturbances from the broadsheet transparency and wherein the centre of the BO transparency is lined up to the center of the broadsheet and rotated to the daily declination, and wherein the center of the BO transparency is also moved up or down along the center of the broadsheet in accordance with the daily declination.
Furthermore, in accordance with another preferred embodiment of the present invention, the method further comprises determining the location of a potential earthquake on the line of longitude.
Furthermore, in accordance with another preferred embodiment of the present invention, determining the location of the potential earthquake on the line of longitude is performed by identifying the disturbances on an EIT and a magnetogram image.
Furthermore, in accordance with another preferred embodiment of the present invention, determining the location of the potential earthquake on the line of longitude is further comprises a: referencing to the pattern archive (EMI Archive); b. statistical analyzing the location of tectonic plates that indicated current seismic activity and c. geological mapping of characteristics of the earth's crust.
Furthermore, in accordance with another preferred embodiment of the present invention, the method further comprises enhancing results from the coordinates harvested from EIT and magnetogram images.
Furthermore, in accordance with another preferred embodiment of the present invention, wherein enhancing the results comprising: a. using a global seismic map; b. examining historic seismic activity of the earth such as occurrence, magnitude and depth and c. taking into consideration the movements of the tectonic plates.
Furthermore, in accordance with another preferred embodiment of the present invention, the prediction of the earthquake is performed by an online simulator.
Additionally and in accordance with yet another preferred embodiment of the present invention, the earthquake has a magnitude that is calculated by the shape of the pattern, the speed in which the sun disturbance develops and the size and location of the disturbance.



BRIEF DESCRIPTION OF THE FIGURES
In order to better understand the present invention and appreciate its practical applications, the following Figures are attached and referenced herein. Like components are denoted by like reference numerals.
It should be noted that the figures are given as examples and preferred embodiments only and in no way limit the scope of the present invention as defined in the appending Description and Claims.
FIG. 1 schematically illustrates a model developed by the inventor in which show EM pulses and the earth/sun/earth relationship.
FIG. 2 illustrates a map showing the Pacific Plate and the Magnetic Equator.
FIG. 3 illustrates a block diagram of the 10-step process of tracking earthquakes in accordance with a preferred embodiment of the present invention.
FIG. 4 illustrates a grid of transparency that is used in the process according to preferred embodiment of the present invention.
FIG. 5 illustrates a broadsheet used in the process according to a preferred embodiment of the present invention.
FIGS. 6a-b illustrate BO latitudes (BO 0 and BO 7) used in the process according to a preferred embodiment of the present invention.
FIG. 7 illustrates a section of the pattern archive (EMI archive) in accordance with a preferred embodiment of the present invention.
FIG. 8a illustrates daily sunspot area averaged over individual solar rotations and the limited tectonic activity during the Little Ice age.
FIG. 8b illustrates earthquake diagram of August 2003 that were checked in an experiment, the balance (pairing) of earthquakes in the northern and southern hemispheres against lines of latitude monitored day by day (over 4.9 magnitude).
FIG. 9 illustrates a magnetogram image showing sunspots 0743 and 0742 taken on Mar. 19, 2005.
FIG. 10 illustrates 2 magnetogram images taken by SOHO and sun disturbances.
FIG. 11 illustrates 3 magnetogram images taken by SOHO and sun disturbances.



DETAILED DESCRIPTION OF THE INVENTION
The present invention provides a new and unique model that correlates seismic activity on Earth directly with the number and specific location of sun disturbances. This model is utilized in order to predict earthquakes through sunspot disturbances. This tracking of sun activities is essential to forecast future earthquakes in order to warn authorities to avoid the consequences of potential damage to human and material resources.
The Sun's Electro-Magnetic Disturbances
Sunspots are strong magnetic fields (3000 gauss) apparently formed by convection processes. The electromagnetic disturbance of sunspots can be compared to tectonic activity, such as a volcanic eruption on the Earth, behaving similarly to convection processes on the tectonic plates.
The disturbances in the sun's magnetic field occur between the area that releases heat (convective zone) and the radiating area (radioactive zone) creating traces on the sensitive photosphere.
The sunspot cycle is not constant (approximately 8-11 years) and repeats when the solar poles are reversed. Sunspots usually appear in pairs or groups (clusters) and with a life span of a few days or weeks.
In all probability, the direction of the sun's magnetic lines of force change the magnetic disturbances that develop as sunspots appear on a magnetogram—at solar minimum—as small disturbances.
The behavior of the sun disturbances, their location, and especially their cycle in the photosphere indicates that disturbances evolve from an external magnetic source. The Earth's core (differentiation) is made out of an internal solid with a diameter of 2400 km, surrounded by an external layer of 7000 km diameter of hot, liquid metal. The core revolves slower than its external layer and the outer crust. As a result, there are differences between the speed of the core electrons and those in the outer layer [X. Song and P. G. Richards, Detecting Possible Rotation of Earth's Inner Core, Nature 382, 221 (1996)]. These movements result in a natural dynamo.
In the outer core of the Earth, the very hot liquid metal (mostly iron) seems to behave like the sun's core, in that it moves and ripples and causes electro-magnetic and electric storms in the depth of the Earth (explained also by Robert Roy Britt in “When North Becomes South: New Clues to Earth's Magnetic Flip-Flops”. About one percent of the electromagnetic field escapes and combines with other elements to create the Earth's magnetic field. According to the behavior of the Earth's core, the geo and electronic-magnetic field also fluctuate. The magnetic axis of the Earth is slightly tilted in relationship to the geographical axis with an inclination of approximately 11 degrees. The strength of the magnetic field is stronger at the poles and weaker around the equator region. Had the axis of the magnetic field been parallel to the geographic axis of the Earth, then the geographic latitudes would follow the same lines of the magnetic latitudes. However, the magnetic lines are similar, but not identical to the geographical lines of latitude. Superimposing the magnetic equatorial line onto the tectonic plate map produces shapes (like a butterfly). The tectonic plates are associated with convection processes.
In addition, the tectonic plates on the Earth's crust are affected by the geo-magnetic field. The main “butterfly” shape appears almost perfectly balanced when superimposed on the Pacific plates (around the Ring of Fire). A further butterfly-like shape emerges from the African and Indian plates. The rest of the plates also complete this magnetic balance with the magnetic equator marking the middle of the ‘butterfly’.
Reference is now made to FIG. 2 illustrating a map showing the Pacific Plate that makes up 80% of the tectonic activity.
The following examples demonstrate the pairing and magnetic balance of earthquakes.














Date
Lat.
Long.
Mag.
Location







2006-09-04
 9.24 S
107.57 E
5.3
SOUTH OF JAWA,






INDONESIA


2006-09-05
 7.71 N
126.51 E
5.6
MINDANAO, 






PHILIPPINE ISLANDS


2006-08-23
 5.54 N
 94.58 E
5.0
NORTHERN






SUMATERA, INDONESIA


2006-08-23
 4.58 S
153.56 E
5.0
NEW IRELAND


2006-08-31
28.81 N
130.01 E
5.5
RYUKYU ISLANDS,






JAPAN


2006-09-01
24.63 S
168.58 E
5.0
NEW CALEDONIA






REGION


2006-08-24
57.61 S
148.30 E
5.5
WEST OF MACQUARIE






ISLAND


2006-08-24
51.14 N
157.59 E
6.5
NEAR E. CST






KAMCHATKA PEN









Accordingly, a 10-step model was developed by the inventor of the present invention in order to determine the location and time of potential earthquakes. The factors taken into consideration in the process include: sun/earth geometry and orbit.
Reference is now made to FIG. 3 illustrating a block diagram of a 10-step process of tracking earthquakes in accordance with a preferred embodiment of the present invention. The steps of the process are as follows:
1. Monitoring Sun Disturbance Activity:
In this step, the user identifies the initial appearance of sunspot disturbance at UTC time. The evidence of the emergence of new sunspot activity and disturbances are identified from satellite imagery; EIT and magnetograms.
2. Marking the Disturbances on a Transparency of the Sun's Diameter on a Grid:
The exact coordinates of the sun disturbances (usually the dark areas of the disturbances or alternatively the cloud-like patterns of sunspot activities) are marked on the transparency that is placed over the EIT and magnetogram images directly on the monitor or over a printout of the EIT and magnetogram image. Reference is now made to FIG. 4 sun's diameter grid transparency) illustrating a grid of transparency that is used in the process according to preferred embodiment of the present invention.
3. Transferring Sunspot Activities From the Transparency to a Broadsheet:
The exact coordinates of the sunspot disturbances are then transferred from the transparency onto a broadsheet that has been divided up into a grid on a larger scale (to enable more precise working picture of current sunspot activities). Reference is now made to FIG. 5 illustrating a broadsheet used in the process according to a preferred embodiment of the present invention.
4. Correlating the Sunspot Disturbance to a Location on Earth (Lines of Latitude):
The BO transparency, divided into lines of latitude on the same scale of that of the broadsheet is marked with a full range of BO options (see 2 examples; BO-0 and BO-7. The coordinates on the transparency (sun's diameter grid transparency) can then be transferred to the broadsheet, indicating the same angle of declination+BO.
Reference is now made to FIGS. 6a-b illustrating BO latitudes used in the process according to a preferred embodiment of the present invention.
5. Determining the Location of the Potential Earthquake on the Line of Latitude:
The line of latitude is determined using the model (will be shown in the examples). The angle of declination of the corresponding day is adjusted to the indications of sunspot disturbances from the broadsheet transparency The centre of the BO transparency is lined up to the center of the broadsheet and rotated to the daily declination. In addition, the center of the BO transparency is also moved up or down along the center of the broadsheet in accordance with the daily declination.
6. Determining the Location of the Potential Earthquake on the Line of Longitude I:
The disturbances identified on the EIT and the magnetogram image (where the black markings represent the south pole and the white marking the north pole) exhibit noticeably different patterns that indicate their specific geographical source. Reference is now made to FIG. 7 illustrating an example of a pattern archive (EMI Archive) in accordance with a preferred embodiment of the present invention.
7. Determining the Location of the Potential Earthquake on the Line of Longitude II:
The location of a potential earthquake on a line of longitude is also determined in the following manner:


    
    
        a. Reference to the pattern archive (EMI Archive) a section is shown in FIG. 7 (the EMI archive documents observations of historic sun disturbance patterns identified from magnetograms over 4 years).
        b. Statistical analysis of the location of tectonic plates that indicated current seismic activity.
        c. Geological mapping of the characteristics of the earth's crust.
    
    


8. Enhancements of the Results From the Data Harvested from the EIT and Magnetogram Images:
The results from these observations may be further enhanced in the following manner:


    
    
        a. Using a global seismic map
        b. Examining of historic seismic activity of the area (occurrence, magnitude and depth)
        c. Taking into consideration the movements of the tectonic plates (and transfer of the pressure, seismic balance).

The factors in steps 5, 6, 7 and 8 determine together the location of a potential earthquake.

    
    


9. Determining a Potential Earthquake by Online Simulator:
A preferred method to determine longitude in accordance with a preferred embodiment of the present invention is by calculating and determining the relative location of the earth to the sun at all times by using an online simulator using a time zone such as the one shown in Table 1. The time zone and the simulator illustrate the relationship of the Earth to the sun as in the broadsheets (‘Y’ axis). This enables the inventor to distinguish the amount of time that takes the sun disturbance to develop (usually between 10-12 hours).
10. Determining the Magnitude of a Potential Earthquake:
The earthquake magnitude is calculated by the shape of the pattern, the speed in which the sun disturbance develops and the size and location of the disturbance.
As mentioned herein before, the model was implemented and checked for the past four years, (2001, 2002, 2003, and 2004) to show repeatability. The correlation between earthquakes and sun disturbances consistently occur together in clusters both quantitatively as well as in the order they occur. An example of this correlated activity is demonstrated in the table that illustrates sun and earthquake activity from August 2003 (an example from the 4 year data set). It has been shown that earthquakes produce unequal distribution of mass over the Earth, and the Earth's equilibrium is therefore destabilized. In a short time, other earthquakes appear that compensate for, and adjust to this imbalance, usually at the opposing side of the plate. Therefore with most earthquakes, there is a responding earthquake (balance).
Reference is now made to FIG. 8b illustrating earthquake diagram of August 2003 that were evaluated over a specific period of time. The diagram illustrates earthquake occurrences from August 2003 as mapped, by date to their geographic latitude. As shown, numerous earthquakes occur, one after another and illustrate a self-similarity that may be compared to the behavior of sun disturbances. Earthquakes occur in series or clusters that are reminiscent of the ways that sunspots occur.
Reference is now made to FIG. 8a illustrating daily sunspot area average over individual solar rotations. The pairing of earthquakes as shown in the butterfly pattern and the plate map has a similar pattern to the sunspot butterfly pattern.
Each earthquake at each specific location ‘acts on’ the edges of the connected platelets and initiates the next earthquake, as explained by Ross S. Stein, Aykut A. Barka and James H. Dieterich, Progressive failure on the North Anatolian fault since 1939 by earthquake stress triggering, Geophysical Journal International, 1997, VOL 128, (pp 594-604). The fact that earthquakes come in clusters has a physical explanation—‘a large earthquake can trigger another large earthquake on a nearby fault where the static stress increases. This explanation can be found in Davide Castelvecchi, Magnet Theory Meets Earthquakes, ISSN 1539-0748, 2005 by The American Physical Society, 2005.
Earthquake activity was monitored and mapped to sun disturbance activity for August 2003. The results are provided in Table 2 that compares the earthquakes that occurred during that time on the Earth showing the latitude of the earthquake and disturbances on magnetogram as measured by the inventor of the present invention. According to the exact position of the disturbance, the inventor of the present invention calculated according to the 10-steps method explained herein before the latitude in which an earthquake is expected. It can be noticed that the correlation between the results of the calculation is in close proximity to the actual earthquakes that occurred. The earthquake data were taken from the US Geological Survey while sunspots data are from magnetogram images provided by the SOHO LASCO, EIT and MDI teams (X and Y values determined by EMI mapping).
In a series of controlled experiments, additional earthquakes location forecasts were documented and distributed on the 14th and 18th of Oct. 2005 and on 24 Feb. and 6 Mar. 2006.
In each set, the number of forecasts harvested from the data available was idiosyncratic and reflected the potential events that were distinguishable on the specific days that the experiment took place.
The coordinates (in Italic and bold) represent the forecasted locations and the locations (with underline) represent actual earthquakes that occurred during this period:












14 Oct. 2005









1.
 
 



Mag
5.8



Date-Time
Sat Oct 22 12:16:36 2005 UTC (8 days)



Location
5.96S 130.01E



Region
IN BANDA SEA


2.
 
 



Mag
4.1 (this event was published online only after list was compiled) (−2




days)



Date-Time
Wednesday, Oct. 12, 2005 at 23:37:35 (UTC)



Location
16.249N, 96.842W



Region
OAXACA, MEXICO



Mag
4.9



Date-Time
Monday, Oct. 24, 2005 at 01:23:59 (UTC) (10 days)



Location
17.71N, 105.77W



Region
OFF COAST OF JALISCO, MEXICO



Mag
4.7



Date-Time
Monday, Oct. 24, 2005 at 01:20:57 (UTC) (10 days)



Location
16.249N, 96.842W



Region
OFF COAST OF JALISCO, MEXICO


3.
 
 



Mag
5.2



Date-Time
Thursday, Oct. 20, 2005 at 23:32:24 (6 days)



Location
31.71N, 50.51E



Region
NORTHERN IRAN


4.
 
 



Mag
6.6



Date-Time
Saturday, Oct. 15, 2005 at 15:51:08 (UTC) (1 days)



Location
25.304N, 123.263E



Region
NORTHEAST OF TAIWAN


5.
 
 



Mag
5.4



Date-Time
Friday, Oct. 14, 2005 at 03:36:45 (UTC) (same day)



Location
23.710S, 176.003W



Region
SOUTH OF THE FIJI ISLANDS







18 Oct. 2005









6.
 
 



Mag
5.0



Date-Time
Tuesday, Oct. 18, 2005 at 08:42:13 (UTC) (same day)



Location
14.176° S, 72.608° W



Region
CENTRAL PERU



Mag
4.8



Date-Time
Thursday, Oct. 20, 2005 at 19:30:22 (UTC) (2 days)



Location
13.49° S, 70.20° W



Region
CENTRAL PERU


7.
 
 



Mag
5.2



Date-Time
Saturday, Oct. 29, 2005 at 01:17:32 (UTC) (11 days)



Location
2.553N, 127.009E



Region
MOLUCCA SEA


8.
 
 



Mag
4.9



Date-Time
Monday, Oct. 17, 2005 at 18:48:26 (UTC) (−1 days)



Location
37.892° N, 142.061° E



Region
OFF THE EAST COAST OF HONSHU, JAPAN



Mag
6.4



Date-Time
Wednesday, Oct. 19, 2005 at 11:44:43 (UTC) (1 day)



Location
36.374° N, 140.849° E



Region
NEAR THE EAST COAST OF HONSHU, JAPAN



Mag
5.5



Date-Time
Saturday, Oct. 22, 2005 at 13:12:47 (UTC) (4 days)



Location
37.118° N, 140.913° E



Region
EASTERN HONSHU, JAPAN



Mag
5.9



Date-Time
Sunday, Oct. 23, 2005 at 10:08:13 (UTC) (5 days)



Location
37.372° N, 134.490° E



Region
SEA OF JAPAN11. 17-18s 69-70w



Mag
4.8



Date-Time
Thursday, Oct. 20, 2005 at 10:02:23 (UTC) (2 days)



Location
20.761° S, 70.363° W



Region
OFFSHORE TARAPACA, CHILE



Mag
5.6



Date-Time
Sunday, Oct. 23, 2005 at 04:49:17 (UTC) (5 days)



Location
21.541° S, 68.185° W



Region
ANTOFAGASTA, CHILE


9.
 
 



Mag
5.7



Date-Time
Thursday, Oct. 20, 2005 at 15:26:32 (UTC) (2 days)



Location
52.334° N, 169.109° W



Region
FOX ISLANDS, ALEUTIAN ISLANDS, ALASKA


10. 
 
 



Mag
5.0



Date-Time
Thursday, Oct. 27, 2005 at 08:41:46 (UTC) (9 days)



Location
30.851N, 138.494E



Region
IZU ISLANDS, JAPAN REGION


11. 
 
 



Mag
5.3



Date-Time
Monday, Oct. 24, 2005 at 00:44:43 (UTC) (6 days)



Location
15.16° S, 172.95° W



Region
Samoa Islands Region







24 Feb. 2006









1)
   
 



Source 20/2
x = 126 y = 44



06/03
45.69N 26.45E




ROMANIA




Mag 4.6



Or 46N 151E
Kuril Island



09/03
45.12N 151.6E




KURIL ISLANDS




Mag 5.2



14/03
47.96N 147.2E




NORTHWEST OF KURIL ISLANDS




Mag 5.3


3)
   
 



Source 4/3
x = 115 y = 30



09/03
37.868N 26.654E




Dodecanese Islands, Greece




Mag 4.3


4)
   



Source 3/3
x = 110 y = 113




The main trigger



14/03
3.60S 127.19E




SERAM, INDONESIA




Mag 6.8



17/03
5.22S 123.13E




BANDA SEA




Mag 5.6



17/03
7.50S 125.16E




BANDA SEA




Mag 5.6



18/03
4.68S 126.2E




TALAUD ISLANDS, INDONEDIA




Mag 5


5)
   



Source
5/3 x = 80 y = 48



16/03
7.38S 106.72E




JAWA, INDONESIA




Mag 5.1


6)
   



Source 2/3
x = 109 y = 135




The main trigger



7/03
14.83S 167.34E




VANUATU ISLANDS




Mag 6.2



17/03
14.98S 167.39E




VANUATU ISLANDS




Mag 5.2



17/03
15.27S 175.82E




TONGA ISLANDS




Mag 5.2



19/03
13.57S 172.41E




VAUNUATU REGION




Mag 5.8


7)
 




The main trigger



12/03
5.05S 153.65E




NEW IRELAND REGION, P.N.G.




Mag 5.9



14/03
3.91S 151.59E




NEW IRELAND REGION, P.N.G.




Mag 5.4



17/03
4.92S 149.92E




BISMARCK SEA




Mag 5.









Reference is now made to FIGS. 9-11 illustrating different magnetogram images. The following examples represent major earthquakes events that are shown with relation to sunspots in FIGS. 9-11, respectively. The magnetograms were analyzed in accordance with the method of the present invention explained herein before.

    1. an earthquake occurred in Sumatra (3.3N-96E) of Mag.9 on 26.12.04 (and consequently tsunami). According to the calculations made on the magnetograms shown in FIG. 10, the following results were calculated:


Average sun's B.O. (−1)
Earth's declination 23.3 S
No data available 21.12.04 from SOHO (possibly because of flares or controlled bakeout)
Average data taken from B.B.S.O.













Data from

Fusion point
Estimated Lat. Location











SOHO
Sunspot No.
X
Y
after calculation





21.12.04
714
89
73
3-S









    2. In Sumatra (2.1N-97E) an earthquake of mag. 8.7 occurred on 28.3.05


from the calculations:

    
    
        Average sun's B.O. (−7)
        Earth's declination N 2.8
    
    

















Sunspot
Fusion no.
Estimated lat. Location after











Data from SOHO
No.
X
Y
calculation














19.3.05
744
93.5
74
2-N




93
74
3N Total 2-3 N









    3. Banda Sea (5.4S-128.1E) experienced an earthquake of Mag. 7.7 that occurred on 27.1.06. The calculations showed:


Average sun's B.O. (−5)
Earth's declination S 20.6

















Fusion


Estimated lat.


Data

point
Magnetogram
EIT 171
Location















from SOHO
Sunspot No.
X
Y
X
Y
X
Y
after calculation





18.1.06
848
79-48
6-5
77
47 (5.5)
77
47 (5.5)
5-6 S




80-52
5-5









It should be noted that according to the model illustrated herein, a mathematical calculation can be developed. This mathematical calculation can automatically perform the correlation needed in order to predict an earthquake from sun disturbances in a mathematical manner known in the art such as trial and error.
It should be clear that the description of the embodiments and attached Figures set forth in this specification serves only for a better understanding of the invention, without limiting its scope as covered by the following Claims.
It should also be clear that a person skilled in the art, after reading the present specification can make adjustments or amendments to the attached Figures and above described embodiments that would still be covered by the following Claims.









TABLE 1









(‘Y’ axis on Broadsheet)



















Invisible
180
160
140
120
100
80
60
40
20
Invisible























00:00
90
105
120
135
150
165
180
165
150
135
120
105
90


01:00
105
120
135
150
165
180
165
150
135
120
105
90
75


02:00
120
135
150
165
180
165
150
135
120
105
90
75
60


03:00
135
150
165
180
165
150
135
120
105
90
75
60
45


04:00
150
165
180
165
150
135
120
105
90
75
60
45
30


05:00
165
180
165
150
135
120
105
90
75
60
45
30
15


06:00
180
165
150
135
120
105
90
75
60
45
30
15
0


07:00
165
150
135
120
105
90
75
60
45
30
15
0
15


08:00
150
135
120
105
90
75
60
45
30
15
0
15
30


09:00
135
120
105
90
75
60
45
30
15
0
15
30
45


10:00
120
105
90
75
60
45
30
15
0
15
30
45
60


11:00
105
90
75
60
45
30
15
0
15
30
45
60
75


12:00
90
75
60
45
30
15
0
15
30
45
60
75
90


13:00
75
60
45
30
15
0
15
30
45
60
75
90
105


14:00
60
45
30
15
0
15
30
45
60
75
90
105
120


15:00
45
30
15
0
15
30
45
60
75
90
105
120
135


16:00
30
15
0
15
30
45
60
75
90
105
120
135
150


17:00
15
0
15
30
45
60
75
90
105
120
135
150
165


18:00
0
15
30
45
60
75
90
105
120
135
150
165
180


19:00
15
30
45
60
75
90
105
120
135
150
165
180
165


20:00
30
45
60
75
90
105
120
135
150
165
180
165
150


21:00
45
60
75
90
105
120
135
150
165
180
165
150
135


22:00
60
75
90
105
120
135
150
165
180
165
150
135
120


23:00
75
90
105
120
135
150
165
180
165
159
135
120
105







Direction of Earth's rotation


 

















TABLE 2







Earthquakes
Disturbances on magnetogram















Date
Lat
Long
Mag
Date
Sun No.
X
Y
Calculated latitude


















01
54.65 S
01.25 E
5.1
29.7.03
Disturbance
57
57
52 S


01
32.77 N
141.12 E
5.2
29.7.03
Disturbance
120
101
30 N


02
9.96 S
124.64 E
4.9


02
7.48 S
128.36 E
4.9


03
30.74 S
179.19 W
5.0


03
56.11 N
153.32 W
5.2





5.3


03
58.91 S
25.56 W
4.9


03
40.49 S
176.03 E
5.3
27.7.03
Disturbance
74
46
40.5 S


03
17.69 S
174.41 W
4.9
31.7.03
Disturbance
67
101
18.5 S


03
3.69 N
118.76 E
4.9


03
22.57 S
177.01 W
5.2
29.7.03
Disturbance
105
30
22 S


04
65.99 N
5.47 E
4.9


04
29.08 N
59.75 E
5.3
31.7.03
Disturbance
109
120
27.5 N


04
60.53 S
43.41 W
6.2
29.7.03

38
72
60S





7.5


04
60.54 S
44.44 W
5.4
1.8.03
424
73
27
58 S


04
21.99 N
120.59 E
5.0
27.7.03
Disturbance
122
77
19.5 N


04
44.64 N
148.58 E
4.9


04
6.06 N
126.29 E
5.2
28.7.03
Disturbance
110
66
4 N


04
21.82 S
169.32 E
5.1


05
20.94 S
178.9 W
5.1


05
23.69 N
70.44 E
5.1
4.8.03
Disturbance
116
96
23 N


05
4.61 S
153.63 E
4.9


05
0.52 S
29.45 E
5.3
2.8.03
Disturbance
73
129
3.5 S


06
43.38 N
147.28 E
5.3
30.7.03
Disturbance
114
157
44 N


06
15.58 S
173.13 W
5.1
29.7.03
Disturbance
80
82
15 S


06
30.58 S
178.02 W
5.1
2.8.03
Disturbance
60
89
31 S


06
7.66 N
36.68 W
5.0
2.8.03
Disturbance
98
102
9 N


06
15.50 S
13.20 W
4.9

Disturbance


07
17.72 S
172.99 W
5.0
2.8.03
Disturbance
78
79
18 S





5.2


07
00.75 N
125.28 E
4.9


07
03.95 S
136.91 E
4.9
7.8.03
430
82
102
4 S


08
13.80 S
71.81 W
4.9
3.8.03
Disturbance
77
77
15 S


08
26.69 N
97.04 E
5.0
4.8.03
Disturbance
116
105
28 N


09
51.50 N
171.21 W
5.2


09
32.91 S
178.54 W
5.0


10
06.62 S
147.90 E
4.9
6.8.03
Disturbance
75
117
5 S





5.0


11
1.14 N
128.15 E
5.7
7.8.03
Disturbance
82
117
00


11
18.35 N
106.04 W
5.1


11
20.20 S
69.74 W
5.0
5.8.03
Disturbance
82
66
21 S


11
33.01 S
178.38 W
4.9


11
56.91. S
147.61 E
5.6
5.8.03
Disturbance
64
63
55 S





5.7


11
12.12 N
93.53 E
5.5
9.8.03
Disturbance
121
25
11 N


12
51.17 N
159.05 E
5.1


12
20.48 N
121.38 E
4.9
7.8.03
Disturbance
123
75
20 N


13
17.65 S
173.07 W
4.9
7.8.03
Disturbance
76
82
18 S


13
09.36 N
79.94 W
5.0


13
30.58. S
178.11 W
5.1
12.8.03
Disturbance
85
42
30 S


13
9.83 S
119.01 E
5.0
5.8.03
Disturbance
84
82
10 S


13
14.28 N
90.09 W1
5.0
10.8.03
Disturbance
131
51
15 N


14
39.16 N
20.61 E
5.6





6.2


14
60.54 S
43.89 W
5.3
12.8.03
Disturbance
52
53
60 S


14
11.65 N
126.71 E
4.9
9.8.03
Disturbance
114
73
12 N


14
38.83 N
20.57 E
5.1





5.2


14
19.90 S
177.98 W
5.2


14
21.12 N
146.56 E
5.0
4.8.03
Disturbance
130
70
23 N


14
55.58 N
162.38 E
4.9


15
40.99 N
125.43 W
5.1


15
28.15 N
113.22 W
4.9
10.8.03
Disturbance
105
130
27 N


15
33.14 S
178.55 W
5.0
13.8.03
432
93
24
33 S


15
11.99 N
143.10 E
4.9


16
43.77 N
119.64 E
5.5
11.8.03
Disturbance
119
147
45 N


16
05.47 S
151.14 E
5.2
11.8.03
Disturbance
74
116
7 S


16
4.62 S
151.82 E
5.3
11.8.03
Disturbance
79
112
4 S


16
05.62 S
151.82 E
5.3


17
20.35 N
121.83 E
5.2
13.2.03
Disturbance
62
112
21 N


18
29.57 N
95.60 E
5.6
14.8.03
Disturbance
110
111
26 N


18
37.63 N
139.97 E
4.9


18
35.63 N
139.97
4.9
15.8.03
Disturbance
138
74
35 N


19
32.93 S
179.21 W
5.2
14.8.03
433
65
59
35 S


19
29.12 N
129.34 E
4.9


19
05.82 S
147.03 E
4.9
12.8.03
Disturbance
89
85
4 S


19
21.99 S
179.55 W
5.0
18.8.03
Disturbance
87
53
21 S


20
11.40 S
166.22 E
5.0
16.8.03
436
111
22
13 S


20
30.30 N
41.92 W
4.9
14.8.03
Disturbance
110
127
30 N


21
00.02 N
126.77 E
4.9


21
1467. N
52.24 E
4.9


21
45.10 S
167.14 E
6.6
8.8.03
431
83
25
45 S





7.5


21
02.25 N
96.53 E
5.1
15.8.03
Disturbance
116
49
2.5 N


21
68.69 N
148.04 W
5.2


22
03.13 N
77.87 W
5.0
17.8.03
Disturbance
122
36
2 N


22
13.37 S
167.14 E
5.0
14.8.03
Disturbance
63
133
14.5 S


23
00.88 S
133.70 E
5.4
20.8.03
Disturbance
110
150
1 S


23
00.78 N
125.22 E
5.0


23
27.56 S
63.26 W
5.0
13.8.03
Disturbance
57
110
27.5 S


24
17.45 S
167.89 E
5.0





5.1


24
40.37 S
98.26 E
5.2


25
14.03 N
91.07 W
5.4
14.8.03
Disturbance
105
101
16 N


25
08.91 S
113.18 E
5.2
16.8.03
Disturbance
37
139
10 S


25
18.54 N
106.70 W
5.5
15.8.03
Disturbance
105
107
18 N


26
04.81 N
125.63 E
4.9
15.8.03
Disturbance
110
64
5 N


26
20.25 S
175.73 W
4.9
20.8.03
Disturbance
82
60
22 S


26
33.11 S
179.22 W
5.1
18.8.03
Disturbance
85
32
35 S


26
17.156 S
70.67 W
5.8
14.8.03
Disturbance
105
101
16 N


26
05.31 S
145.23 E
4.9
17.8.03
Disturbance
87
92
4 S


27
06.59 S
147.17 E
5.1
22.8.03
Disturbance
72
131
7 S


27
39.16 S
72.44 W
5.1
19.8.03
Disturbance
47
110
38


S27
65.13 S
179.26 E
4.9
19.8.03
Disturbance
48
50
65 S


27
06.78 N
33.97 W
5.0
26.8.03
Disturbance
123
32
5 N


27
43.74 N
28.92 W
5.1
27.8.03
Disturbance
128
104
42 N


27
11.29 N
57.57 E
5.3
20.8.03
Disturbance
89
136
10 N


28
49.82 S
114.81 W
5.4
26.8.03
Disturbance
64
39
50 S





6.1


28
55.85 S
146.84 E
5.1


28
07.32 S
126.05 E
5.6
23.8.03
Disturbance
109
41
7 S


28
05.04 S
103.51 E
5.0
23.8.03
Disturbance
110
34
6.5 S


28
56.10 S
143.60 W
5.0


28
21.98 S
179.58 W
5.1
22.8.03
Disturbance
63
110
22 S


28
00.21 N
126.18 E
5.1


28
13.16 N
145.33 E
5.3


29
26.27 S
177.26 W
5.3
17.8.03
437
31
103
26 S


29
14.95 S
176.8 W
4.9
24.8.03
Disturbance
99
37
16 S


29
59.29 S
24.88 W
5.2


29
02.32 S
139.58 E
5.1
21.8.03
Disturbance
83
108
2 S


29
60.56 S
43.21 W
4.9


29
30.90 S
178.87 W
4.9


29
05.43 S
102.23 E
5.1
25.8.03
Disturbance
76
113
7 S


30
14.80 S
167.24 E
5.2
28.8.03
Disturbance
86
58
17 S


30
73.27 N
06.42 E
5.0


30
30.76 S
178.24 W
5.1


30
41.86 N
142.55 E
5.2
28.8.03
Disturbance
120
138
40 N


31
10.54 N
146.35 E
5.8
27.8.03
Disturbance
106
83
11 N


31
13.86 N
119.75 E
5.3


31
43.39 N
132.27 E
5.5
28.8.03
Disturbance
120
138
40 N

## Claims

1. A method of correlating earthquakes on earth to electromagnetic disturbances on the sun comprising:
mapping coordinates of electromagnetic disturbances on the sun;
calculating said coordinates;
mapping the calculated coordinates onto a location and time on earth;

whereby the location and time on earth predicts the location and approximate time of the earthquake which will consequently occur on earth.

2. The method as claimed in claim 1, wherein the electromagnetic disturbances are based on those observed on EIT images.

3. The method as claimed in claim 1, wherein the electromagnetic disturbances are based on those observed on a magnetogram image.

4. The method as claimed in claim 1, wherein said mapping coordinates is performed by marking the disturbances on a transparency of sun's diameter on a grid and transferring the marked coordinated onto a broadsheet.

5. The method as claimed in claim 1, wherein said mapping the calculated coordinates is performed by marking said coordinates on a scaled BO transparency divided into lines of latitude.

6. The method as claimed in claim 1, wherein said location is determined from the line of latitude using a model in which an angle of declination of a corresponding day is adjusted to the indications of sunspot disturbances from the broadsheet transparency and wherein the centre of the BO transparency is lined up to the center of the broadsheet and rotated to the daily declination, and wherein the center of the BO transparency is also moved up or down along the center of the broadsheet in accordance with the daily declination.

7. The method as claimed in claim 1, further comprising determining the location of a potential earthquake on the line of longitude.

8. The method as claimed in claim 7, wherein determining the location of the potential earthquake on the line of longitude is performed by identifying the disturbances on an EIT and a magnetogram image.

9. The method as claimed in claim 7, wherein determining the location of the potential earthquake on the line of longitude is further comprises a: referencing to the pattern archive (EMI Archive); b. statistical analyzing the location of tectonic plates that indicated current seismic activity and c. geological mapping of characteristics of the earth's crust.

10. The method as claimed in claim 1, further comprising enhancing results from the coordinates harvested from EIT and magnetogram images.

11. The method as claimed in claim 10, wherein enhancing the results comprising: a. using a global seismic map; b. examining historic seismic activity of the earth such as occurrence, magnitude and depth and c. taking into consideration the movements of the tectonic plates.

12. The method as claimed in claim 1, wherein the prediction of the earthquake is performed by an online simulator.

13. The method as claimed in claim 1, wherein the earthquake has a magnitude that is calculated by the shape of the pattern, the speed in which the sun disturbance develops and the size and location of the disturbance.