Finding the Pattern of Counterbalancing Quakes Will Help in Earthquake Prediction

By Norma Hickox
Platinum Quality Author
There have been several mysterious jolts recently in not only our country, but around the world. This is a different kind of earth movement, one that cannot be detected by instruments now in use. The earth herself hit a "pocket" of vacuum left from the original explosion. As she is shifting into uncharted seas of eternity, this will happen more often. Instruments above the earth are the only ones that can measure these "bumps." These jolts are not as dangerous as earthquakes themselves. It is just a momentary absence of normal gravity pull that causes a slight bump, but they will serve as warnings of movement within the earth itself. The next time a "mystery jolt" is felt, it should be noted that within twenty-four hours the earth will also move from the inside. They are related.
Picture it as a bowl of water that is traveling along a conveyor belt. Suddenly the belt floats free, for a moment, of the drag that is on it. This causes a sloshing of the water inside the bowl. This is what happens inside the earth. The molten lava in the center of the earth sloshes up against the sides and causes all sorts of problems. The volcanoes and earthquakes are all part of the realignment of the earth in virgin space. Once she is settled into her new area all will return to normal. This will take a period of approximately twenty to thirty years of our time. She will be mostly into the new space in about ten years but the settling into the new orbit will take longer.
Those that are doing earthquake prediction still are not looking over the fracturing pattern of the whole surface of the earth. They need to keep in mind that what occurs in one area will always be counterbalanced in another area. A map of all quake activity world wide needs to be kept and monitored at all times and studied with locations and dates compared to find the pattern of counterbalancing. It is not as simple as it may sound to find what quake counterbalanced which other quake. There are many factors involved that need taken into account.
One of these is the temperature of the shell at the point of the quake, followed by a line to the center and then to a counterbalancing temperature. How this could be arrived at would require temperature monitors at strategic points around the world with a map being done of similar temperature of the outer shell at a level of three miles below the surface. I realize this would take a lot of work and time and money, but would enable us to accurately predict earthquakes in the future.
It is not just a matter of one earthquake having, then, a counterbalancing one. It is more like a jigsaw puzzle because the counterbalancing one will then have a counterbalancing one, and so on. Time is also a factor that will be able to be predicted, not just location, by the temperature monitoring. Hotter temperatures will cause a slower reaction as far as a counterbalancing action.
The variation of temperature between quakes needs studied very thoroughly and degrees of differences marked on all the locations of past quakes. This, then, would show the pattern of timing based on temperature differences. This is a ways into the future, but is the only way for exact predictions to be made. Many lives could be saved this way and much devastation could be avoided because care could be taken to not allow certain areas to be populated.
This same map would then allow volcanic action to be monitored. There is a close link, hence the taking of the temperature of the shell as given. This releasing of volcanic action will lessen the pressure that causes the quakes. At times it is difficult to tell which pressure release will take place until just shortly before it happens.
It is a matter of timing, you see. If the temperature of the shell is cooler in a certain area than the previous quake or volcano, then the next release will be faster to come than if the last one was at a hot spot in the shell. When it is at a hot spot in the shell, the fluidity of the shell allows for expansion and movement, but when in a colder area, the hardening of the shell matter does not allow for this expansion and contraction process, and the release must come rather quickly. There are other monitoring indications as far as the oceans go, but they are more complex and not as easily reachable as what has been given.