WO2010087787A2 - Six-hour advance earthquake notification system - Google Patents

Six-hour advance earthquake notification system Download PDF

Info

Publication number
WO2010087787A2
WO2010087787A2 PCT/TR2010/000010 TR2010000010W WO2010087787A2 WO 2010087787 A2 WO2010087787 A2 WO 2010087787A2 TR 2010000010 W TR2010000010 W TR 2010000010W WO 2010087787 A2 WO2010087787 A2 WO 2010087787A2
Authority
WO
WIPO (PCT)
Prior art keywords
earthquake
dashboard
computer
alternans
reflecting
Prior art date
Application number
PCT/TR2010/000010
Other languages
French (fr)
Other versions
WO2010087787A9 (en
WO2010087787A3 (en
Inventor
Kurt Veysi
Original Assignee
Kurt Veysi
Priority date (The priority date is an assumption and is not a legal conclusion. Google has not performed a legal analysis and makes no representation as to the accuracy of the date listed.)
Filing date
Publication date
Application filed by Kurt Veysi filed Critical Kurt Veysi
Priority to EP10704022A priority Critical patent/EP2401637A2/en
Publication of WO2010087787A2 publication Critical patent/WO2010087787A2/en
Publication of WO2010087787A3 publication Critical patent/WO2010087787A3/en
Publication of WO2010087787A9 publication Critical patent/WO2010087787A9/en

Links

Classifications

    • G—PHYSICS
    • G01—MEASURING; TESTING
    • G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS
    • G01V1/00—Seismology; Seismic or acoustic prospecting or detecting
    • G01V1/01—Measuring or predicting earthquakes

Definitions

  • Symbol (B) represents the first fracture point to occur during discharge; symbol (P) represents the first wave created upon lithosphere by the earthquake and the discharge point; symbol (S) represents the settlement area affected by the destruction
  • the first fracture i.e. the time between (B) and (P) does not occur before six hours.
  • the cleavage time of the lithosphere is the time between a first fracture signal (B) and a surface wave (P).
  • the flux and reflux waves of magma pump gas into the holes of the lithosphere known as fault. These faults jsvacuate such gas depending on their, resistance levels.-The intensityTtime and distance of the earthquake is determined via a three-alternans analysis of the energy between the initial hit (B) and the first rupture point of pressure energy, i.e. the initial hit (B) sent by magma waves into the holes within lithosphere (faults).
  • the countdown begins following the determination of lithosphere's rupture process between an initial hit (B) and a wave (P) (the first wave of earthquake on earth) as minimum six hours upon the three-alternans analysis. Time is determined by the formation process of indication between three alternanses. The time period between three alternanses determines the speed of earthquake.
  • the 1 st item, top apparatus reflects the electrical signal among atmosphere upon dashboard in minivolts. It is operated with 2 V DC (direct current) and 220 V alternative current (AC).
  • the indefinite normal condition of the top apparatus is 205 millivolts.
  • the 2 nd item, bottom apparatus reflects the electrical signal accumulated on lithosphere within the predetermined field upon dashboard in millivolts. It is operated with 2 V DC (direct current) and 220 V Alternative Current (AC).

Landscapes

  • Physics & Mathematics (AREA)
  • Life Sciences & Earth Sciences (AREA)
  • Engineering & Computer Science (AREA)
  • Acoustics & Sound (AREA)
  • Environmental & Geological Engineering (AREA)
  • Geology (AREA)
  • Remote Sensing (AREA)
  • General Life Sciences & Earth Sciences (AREA)
  • General Physics & Mathematics (AREA)
  • Geophysics (AREA)
  • Geophysics And Detection Of Objects (AREA)

Abstract

If the indication of the earthquake emerged via the three-alternans analysis is within an area of 200 km from the location where the system subject of the invention is installed, such system subject of the invention ascertains the precise intensity, time and location of the earthquake. If the indication of the earthquake is ascertained out of the 200-km-area and within the bird's eye view of maximum 800-km, the precise intensity and time of the earthquake is specified together with the distance of location (area). Meanwhile, the notification of distance is valid for 360 degrees.

Description

SIX-HOUR ADVANCE EARTHQUAKE NOTIFICATION SYSTEM
The present invention is a system which precisely determines the time, intensity and location of an earthquake within minimum six hours and maximum one hundred twenty hours in advance by analyzing the electrical energy resulting from Motion=Energy and potential difference between two points via three alternance analyses. Ban/sphere and pyrosphere = endosphere, and magma are located respectively beneath the lithosphere. Flux and reflux waves of magma determine the earthquake intensity. The electrical accumulation and heat of atmosphere, lithosphere, barysphere and pyrosphere = endosphere are always determined by magma. Magma, flux=first alternans = provides the electrical expansion accumulated within the atmosphere and lithosphere. Reflux=second alternans = provides the depth or distance. Re-flux=flux=third alternans: determines the time of earthquake and establishes its certainty. With respect to the known and adopted condition of the art, there is currently no proven method to determine earthquakes precisely in advance although worldwide studies have been executed in regard to the predetermination of earthquakes. The present system that is subject of the invention ascertains earthquakes in advance via the three- alternans analysis and is, therefore, unique within the local country and abroad.
Within the scope of technical problems to be solved by the invention, the lack of predetermination in time, intensity and location of earthquakes causes loss of life and property. The loss of life and property will be prevented with the use of the system that is subject of the invention.
Explanation of the symbols used in the three-alternans analysis is as follows:
Symbol (B) represents the first fracture point to occur during discharge; symbol (P) represents the first wave created upon lithosphere by the earthquake and the discharge point; symbol (S) represents the settlement area affected by the destruction
(the most effective wave field diffused by the P wave of the earthquake). The first fracture, i.e. the time between (B) and (P) does not occur before six hours. The cleavage time of the lithosphere is the time between a first fracture signal (B) and a surface wave (P). The flux and reflux waves of magma pump gas into the holes of the lithosphere known as fault. These faults jsvacuate such gas depending on their, resistance levels.-The intensityTtime and distance of the earthquake is determined via a three-alternans analysis of the energy between the initial hit (B) and the first rupture point of pressure energy, i.e. the initial hit (B) sent by magma waves into the holes within lithosphere (faults).
The countdown begins following the determination of lithosphere's rupture process between an initial hit (B) and a wave (P) (the first wave of earthquake on earth) as minimum six hours upon the three-alternans analysis. Time is determined by the formation process of indication between three alternanses. The time period between three alternanses determines the speed of earthquake.
Method of determining an earthquake by using three alternanses is as follows: a) The first alternans, magnitude of the sign, indicates the earthquake intensity. b) Second alternans, depth, determines the distance between the location of the system that is subject of the invention and the location of the prospective earthquake. c) Third alternans confirms that the earthquake will certainly occur. The speed between three alternanses specifies the time of the prospective earthquake. Items within the System Subject of the Invention:
(1) Top apparatus,
(2) Bottom apparatus,
(3) Dashboard,
(4) First computer (5) A camera with lens,
(6) Second computer
(7) A 1 " don's camera
(8) Receiving antenna
The 1st item, top apparatus, reflects the electrical signal among atmosphere upon dashboard in minivolts. It is operated with 2 V DC (direct current) and 220 V alternative current (AC). The indefinite normal condition of the top apparatus is 205 millivolts.
The 2nd item, bottom apparatus, reflects the electrical signal accumulated on lithosphere within the predetermined field upon dashboard in millivolts. It is operated with 2 V DC (direct current) and 220 V Alternative Current (AC).

Claims

CLAIMS:
1. A six-hour advance earthquake notification system characterized in that such system is composed of a top apparatus (1) reflecting the electrical signal among atmosphere upon dashboard in millivolts, a bottom apparatus (2) reflecting the electrical signal accumulated on lithosphere within the predetermined field upon dashboard in millivolts, a dashboard (3) being a panel on which electrical signals transmitted via the accumulation from the top and bottom apparatus (1 and 2) are formed with the three-alternans method, a receiving antenna (8) reflecting electrical signals transmitted from the top apparatus and bottom apparatus (1 and 2) upon dashboard (3), a first computer (4), a camera with lens (5) recording the whole data appearing on the dashboard to the first computer (4), a Second computer (6) and a 1" don's camera (7) controlling the installation field of system subject of the invention via recording it to the Second computer (6) so as to avoid from misleading indications.
PCT/TR2010/000010 2009-01-28 2010-01-20 Six-hour advance earthquake notification system WO2010087787A2 (en)

Priority Applications (1)

Application Number Priority Date Filing Date Title
EP10704022A EP2401637A2 (en) 2009-01-28 2010-01-20 Six-hour advance earthquake notification system

Applications Claiming Priority (2)

Application Number Priority Date Filing Date Title
TR2009/00618A TR200900618A2 (en) 2009-01-28 2009-01-28 Six hours in advance earthquake notification system.
TR2009/00618 2009-01-28

Publications (3)

Publication Number Publication Date
WO2010087787A2 true WO2010087787A2 (en) 2010-08-05
WO2010087787A3 WO2010087787A3 (en) 2011-06-23
WO2010087787A9 WO2010087787A9 (en) 2011-08-11

Family

ID=42396243

Family Applications (1)

Application Number Title Priority Date Filing Date
PCT/TR2010/000010 WO2010087787A2 (en) 2009-01-28 2010-01-20 Six-hour advance earthquake notification system

Country Status (3)

Country Link
EP (1) EP2401637A2 (en)
TR (1) TR200900618A2 (en)
WO (1) WO2010087787A2 (en)

Cited By (1)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
WO2015002619A1 (en) * 2013-07-01 2015-01-08 Kurt Veysi Earthquake prediction and early warning system

Family Cites Families (4)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
EP0067924B1 (en) * 1981-06-19 1985-10-02 Panagiotis Varotsos Method for predicting earthquakes
AU1336695A (en) * 1994-12-06 1996-06-26 David F. Farnsworth Method for forecasting an earthquake from precusor signals
US5694129A (en) * 1995-08-29 1997-12-02 Science And Technology Agency National Research Institute For Earth Science And Disaster Prevention Method of imminent earthquake prediction by observation of electromagnetic field and system for carrying out the same
US5742166A (en) * 1996-11-04 1998-04-21 Park; Larry Seismic activity predictor including a dielectric for receiving precursor seismic electromagnetic waveforms

Non-Patent Citations (1)

* Cited by examiner, † Cited by third party
Title
None

Cited By (1)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
WO2015002619A1 (en) * 2013-07-01 2015-01-08 Kurt Veysi Earthquake prediction and early warning system

Also Published As

Publication number Publication date
WO2010087787A9 (en) 2011-08-11
TR200900618A2 (en) 2009-08-21
EP2401637A2 (en) 2012-01-04
WO2010087787A3 (en) 2011-06-23

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