Abstract: The present invention describes methods, systems, and devices for utilizing high-intensity regions within atmospheres of planetary bodies to receive and harvest electricity. Such high-intensity regions are formed as a result of the combined gravitational forces affecting a given planetary body and particularly the particles within the atmosphere of that planetary body. The combined gravitational forces result in a gravitational resonant frequency which affects the atmosphere most intensely within said high-intensity regions. By determining moments of gravitational resonant frequencies based on a given location, the methods, systems, and devices described herein utilize the energy provided within the high-intensity regions during the determined moments. Harvesting and further transmitting the collected energy is also disclosed.

Abstract: Disclosed are methods and systems for detecting and predicting events of increased seismic activity (i.e. earthquake activity). The methods include providing data catalogs, constructing magnitude versus time coordinate graphs, identifying energy levels of the graphs, and identifying further the obliquity angles of maximum and minimum energy levels and average increments between minimum and maximum energy levels. The methods also comprise constructing time arrows using the identified information, identifying energy centers via the time arrows, and analyzing variability throughout the seismic structure to predict a future event. Also disclosed are methods for predicting events based on attenuation wedge and energy parallelogram analysis.

Abstract: The present invention may be used for forecasting various weather phenomena including but not limited to flyby anomalies, cyclones, tornadoes, killer (rogue) waves, earthquakes, lightning, sprites, and temperature fluctuations. The invention is based on knowledge of physical and mathematical models regarding the occurrence of Kukharev regions (i.e., K regions) resulting from gravitational resonances occurring within the Earth-Moon-Sun system (and similar systems located elsewhere). These gravitational resonances and combinations thereof, among other things, cause jumps in atmospheric pressure. Such jumps can be recorded and extrapolated to predict the locations and times of the occurrence of Kukharev regions and, in turn, the associated weather-related effects.

Abstract: The present invention may be used for forecasting various weather phenomena including but not limited to flyby anomalies, cyclones, tornadoes, killer (rogue) waves, earthquakes, lightning, sprites, and temperature fluctuations. The invention is based on knowledge of physical and mathematical models regarding the occurrence of Kukharev regions (i.e., K regions) resulting from gravitational resonances occurring within the Earth-Moon-Sun system (and similar systems located elsewhere). These gravitational resonances and combinations thereof, among other things, cause jumps in atmospheric pressure. Such jumps can be recorded and extrapolated to predict the locations and times of the occurrence of Kukharev regions and, in turn, the associated weather-related effects.

Abstract: Based on determined locations of Kukharev (K) regions, and the estimated times of their formation on Earth, in the atmosphere, and in space, antimatter may be produced and collected, as described by the present invention. Due to jumps in the gravitational field, various standing waves are formed from the resonances of the gravitational tides. A wave of charged particles is formed within the K region and can be setup to collide with targets comprising heavy metal atoms (or other equivalents), the colliding thereby creating antimatter particles. These antimatter particles can then be stored in various traps and used for various purposes, e.g., energy formation.

Abstract: Based on determined locations of Kukharev (K) regions, and the estimated times of their formation on Earth, in the atmosphere, and in space, antimatter may be produced and collected, as described by the present invention. Due to jumps in the gravitational field, various standing waves are formed from the resonances of the gravitational tides. A wave of charged particles is formed within the K region and can be setup to collide with targets comprising heavy metal atoms (or other equivalents), the colliding thereby creating antimatter particles. These antimatter particles can then be stored in various traps and used for various purposes, e.g., energy formation.

Abstract: All fluids, when placed within a Kukharev region at a moment of gravitational resonance, form vibrations of different frequencies within themselves. If, at the same moments of gravitational resonance, forced oscillations of the same frequency are provided as a treatment on a living organism, a double resonance is formed within the fluid, and a sharp increase in the amplitude of oscillations within the fluid formed as a result of the double resonance in turn causes the destruction of the fluid. The method is determined utilizing Kukharev region data on the particular fluid desired to be destroyed or otherwise removed from the living organism. By further fine-tuning the forced oscillation (i.e., the directed radiation), the natural oscillations of the base fluid can be further adjusted to modify the fluid's properties.

Abstract: All fluids, when placed within a Kukharev region at a moment of gravitational resonance, form vibrations of different frequencies within themselves. If, at the same moments of gravitational resonance, forced oscillations of the same frequency are provided as a treatment on a living organism, a double resonance is formed within the fluid, and a sharp increase in the amplitude of oscillations within the fluid formed as a result of the double resonance in turn causes the destruction of the fluid. The method is determined utilizing Kukharev region data on the particular fluid desired to be destroyed or otherwise removed from the living organism. By further fine-tuning the forced oscillation (i.e., the directed radiation), the natural oscillations of the base fluid can be further adjusted to modify the fluid's properties.

Abstract: The present invention describes methods, systems, and devices for utilizing high-intensity regions within atmospheres of planetary bodies to receive and harvest electricity. Such high-intensity regions are formed as a result of the combined gravitational forces affecting a given planetary body and particularly the particles within the atmosphere of that planetary body. The combined gravitational forces result in a gravitational resonant frequency which affects the atmosphere most intensely within said high-intensity regions. By determining moments of gravitational resonant frequencies based on a given location, the methods, systems, and devices described herein utilize the energy provided within the high-intensity regions during the determined moments. Harvesting and further transmitting the collected energy is also disclosed.

Abstract: Disclosed are methods and systems for detecting and predicting events of increased seismic activity (i.e. earthquake activity). The methods include providing data catalogs, constructing magnitude versus time coordinate graphs, identifying energy levels of the graphs, and identifying further the obliquity angles of maximum and minimum energy levels and average increments between minimum and maximum energy levels. The methods also comprise constructing time arrows using the identified information, identifying energy centers via the time arrows, and analyzing variability throughout the seismic structure to predict a future event. Also disclosed are methods for predicting events based on attenuation wedge and energy parallelogram analysis.

Abstract: Disclosed are methods for locating deposits of mineral resources below the Earth's crust. A period of resonance of 14-day gravitational tides is predicted based on known information about a location. During the period of resonance, element vapor emissions and/or other data are recorded using gas analyzers and/or other devices, which are spread in an array over the location. The vapors and/or other data are recorded for a period of about 3-4 days. The recorded data is analyzed to determine when and where any anomalies exist. By comparing anomalies to control data, the changes can be further extrapolated to obtain more accurate data. After anomalies are detected and analyzed, the locations of deposits comprising mineral resources can be determined and maps of the locations correlating to the surface are generated.

Abstract: Disclosed are methods for locating deposits of mineral resources below the Earth's crust. A period of resonance of 14-day gravitational tides is predicted based on known information about a location. During the period of resonance, element vapor emissions and/or other data are recorded using gas analyzers and/or other devices, which are spread in an array over the location. The vapors and/or other data are recorded for a period of about 3-4 days. The recorded data is analyzed to determine when and where any anomalies exist. By comparing anomalies to control data, the changes can be further extrapolated to obtain more accurate data. After anomalies are detected and analyzed, the locations of deposits comprising mineral resources can be determined and maps of the locations correlating to the surface are generated.

Abstract: Methods, systems, and devices for the location of oil and gas deposits are disclosed. The technology is based on the recording of natural (i.e. not man-made) oscillations of oil and gas environments under the influence of the energy of resonances of the gravitational tides. The recording is performed by low-frequency geophones (0.1-10 Hz). The resonances are recorded, graphed, and analyzed. The time of the onset of the resonances of 14-day gravitational tides is pre-calculated by adding the tidal waves from the Moon, the Sun, and the stress wave arising in the Earth's lithosphere in connection with the periodic oscillation of the position of the barycenter of the Earth-Moon system. The calculation of the time of the onset allows for the prediction of optimal times for surveying according to the method of the present invention.