The Earth is a vibrating planet. Its crust has been vibrating since its formation. Constant tremors affect everything on Earth, constructively or destructively. While a wave at the sea shore destroys the sandcastle of a child, many crabs and oysters attached to the nearby cliffs are enjoying the food it carries. Vibration creates and destroys numerous things, not only on the surface, but also in the deep beds of oceans. In a single word, "constant change" is the net result of persistent vibration. What is the energy source of vibration? The energy of Earth crust vibration comes from multiple natural sources. Most of these energy sources are individually well-known, but the sum of them, and especially their interactions, are not yet well understood. I have named this obscure combined energy the "vibration force" and have tried to explain it in the context of "vibration theory". What is the importance of vibration theory? Vibration theory has many useful applications in geosciences. Firstly, observation of geologic events under the light of "vibration theory" will give us a new insight which simplifies many difficult and essential problems in Earth sciences, such as plate tectonics, mountain formation, volcanic eruptions, and earthquakes. It also helps in discovering underground resources more easily. Subsequently, it gives us the power of anticipation of some future geological events. And lastly, but certainly not least, the vibration theory states that the "vibration force" is one of the most powerful sources of cheap and clean energy in nature and can be harnessed for many beneficial purposes. I recommend using it for extensive artificial upwelling in order to cool coastlines in the Middle East. Artificial upwelling has enough capacity to cool many regional coastlines and small gulfs in the region. Fortunately, there is a good sample of natural deep sea cold water upwelling in Dohfar (Arab Sea). Surely, by imitating this natural phenomenon, we can save our world in this harsh situation during the global warming era.
Read More ...