Despite the slow nature of these changes, researchers consider them tolerance. The movement of the jelly plates in the Tibetan area, confirmed by the observations of the tool, shows the divergence of the blocks of the Earth's crust: a plate with a larger height continues to increase, and the other, lower, lowered.
An analysis of Helium content in Tibet's sources, made by experts from Stanford University, confirmed the presence of this creation process.
Another argument that is beneficial for the gradual separation of the array is the analysis of seismic waves, proving the ability to form an abnormal crack.
However, some geologists call for calm, note that the transformation of the continents is a process that is continuously conducted extremely slowly, which can be prepared. In addition, India's division seems to be less likely than similar processes on other continents.
For example, the division of African continent is more likely. According to scientists, in East Africa, divergence sheets at a speed of about 6.35 mm per year. This process, starting about 3.5 million years ago, continued to this day.
Previously, scientists have established when Antarctic ice begins. Also in the desert in Peru, a fossil of a whale 39 million years has