In honor of Dutchsinse you tube channel shut down by the F
How to forecast an earthquake -- TEXT VERSION -- Fundamental Principles
This has been made for anyone to test the method.
How to forecast an earthquake THE TEXT VERSION: By Dutchsinse (Michael Yuri Janitch)
Simply put, almost anyone can do earthquake forecasting down to a region of a few hundred miles, down to an approximate 7-10 day time period, and usually within 1 magnitude of what actually ends up striking.
HOW TO:
Standing wave principles apply. See here for a video example: https://rumble.com/vbdn5d-concentic-s...
Video above shows the whole process from deep earthquakes to the spread up, the halfway sorting and the spread out......... (video shows concentric waves , into a singularity spike upwards, then a standing wave in a tank building power reflecting back into itself.. then the middle points are sorted via vibration on a shake plate, then the wave travels as a soliton solitary wave of translation, then sorts to middle points again as it distributes out along the linear plate boundaries and across craton edges)
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Explanation:
Between any two earthquakes , a middle point exists.
Think of two earthquakes like two waves in a standing wave tank. Then a new earthquake (a new single wave of same size or combined larger) pops up in the "middle point" between the two previous waves.
Like book ends, the two previous earthquakes define the area to watch for the NEW earthquake to strike in the nearterm future. The middle point usually is struck with the combined total of both previous earthquakes.
Example:
Two 5.0's hit across Japan.. (one M5.0 on the south at Kyushu, one M5.0 on the north at Hokkaido)..... then a few days later or less a new M5.1 to M5.2 strikes the middle point at Tokyo.
The standing wave usually spreads onwards along the plate boundaries and craton edges after striking in a particular area more than a few times.
As the standing wave spreads, new sets of quakes occur at the halfway points previously mentioned.
Just as a standing wave spreads in a tank, and then reflects into itself, earthquakes spread and strike the same way, but instead of being in a "tank", the seismo-electrical wave which is spreading follows the plate boundaries and craton edges "out and away" from where the wave comes up.
The seismo-electrical wave comes up from below the plates (coming up from the core itself as a Ultra low frequency or Extremely low frequency wave).
When the seismo-electrical ULF/ELF wave comes up from the plasma core of the earth (like lightning spreads up from the plate into the atmosphere).. this seismo-electrical wave spreads up and out through the plate.
The ULF / ELF seismo-electrical wave is usually accompanied by a "deep earthquake" recorded at the bottom of the plate receiving the wave, or even deeper below the plate receiving the wave in the semi-melted asthenosphere.
The deep earthquakes sizes (magnitudes) and locations are importan
