Method for accurately predicting earthquake through adoption of earthquake cloud
An accurate and seismic technology, applied to alarms, instruments, etc., can solve problems such as inability to predict accurately in advance
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Embodiment 1
[0045] Earthquakes are a process of gradual energy accumulation and energy release. When the energy accumulation reaches the extreme value of breaking the crust, it will develop into a surface earthquake. During this period, an earthquake cloud will be generated for people to see.
[0046] Earthquakes don't burst out of the earth's crust all of a sudden. It has an energy gathering process, and the length of energy gathering depends on the size of the bulging space of the inner crust on the surface, the hardness and thickness of the crust, and the healing of the fault zone in the past. Diffusion, and finally the formation of surface earthquakes. During this process, high-pressure gas will be released into the air through the fault zone and the weak zone on the surface, and gradually integrate into the seismic cloud that can be seen clearly by people. Clouds of small earthquakes of magnitude 2 to 4 are usually seen 5 to 10 minutes before a surface earthquake[ figure 1 ]; 1 da...
Embodiment 2
[0048] For an earthquake of magnitude 2 to 4, people can feel and see the rapid rise of dark brown fog (earthquake cloud) covering the low-altitude surface of the epicenter 5 minutes before the earthquake, and people feel uncomfortable breathing. The shock cloud disappears about 5 minutes after the earthquake [such as Figure 14 ]; earthquakes of magnitude 4 to 6, earthquake clouds often appear around or near the hollow sun at 10 to 15 o'clock and 8,000 meters, and the duration does not exceed 30 minutes. Generally, this can be seen 1 to 5 days before the earthquake hits the surface Seismic clouds of magnitude [eg Figure 15 ]; earthquakes of magnitude 6 to 7, earthquake clouds often appear at 12 to 14 o'clock on sunny days when the sun is stronger at noon, the cloud system is small but relatively white and high (about 20,000 meters by visual inspection), and lasts for about 20 to 40 minutes The deformation disappears, and this kind of tremor cloud is usually seen 5 to 7 days ...
Embodiment 3
[0051] The deeper the epicenter, the greater the amplitude, the greater the magnitude, and the smaller the intensity; the more rounded and larger the earthquake cloud, the deeper the epicenter, the greater the amplitude, and the flatter the surface of the area to be earthquaked (plain, city) [such as Figure 18 ]; the clouds are broken and uneven in thickness, and the area to be shaken is hilly or mountainous [such as Figure 19 ]; earthquake clouds are like a mountain range, a row of several lines spaced in the same direction, side by side and not connected to each other, showing that they will shake the bottom of the sea to the island at high altitudes [such as Figure 20 ], multiple rows of such shocking clouds will shake the islands [such as Figure 21 ]; If the shaking cloud is a very complete piece or there are blurred ripples in one or more places on the edge, it will shake a large lake or wetland [such as Figure 22 ].
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