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No: the core of the Earth is not perfectly symmetrical, and that will affect the nature of our magnetic field in the long term.
We don’t know a lot about the Earth’s core is because it cannot be sampled. Located 5,000 meters below the surface, the information we have is the result of centuries of seismological and geophysical observation. Even today, all we have are models of their behavior. However, a recent study from Cambridge and Bristol, in the United Kingdom, assures that it is growing at uneven rates. This is the reason.
Unlike what we were taught in school, the Earth is not exactly spherical. Rather, it has ridges, peaks, and valleys that make our planet seem perfect blue ball from space. Seen another way, the representations we have of its layers are not exact but are for illustrative purposes only. However, this is not exactly the case. The same trend seems to be replicating within him.
Jessica Irving, a Bristol seismologist, writes in her article for The Conversation, “The core of the Earth was formed very early in the 4.5 billion years of our planet’s history.” It took only 200 million years before the center of our planet finished taking shape. Gravity dragged iron into the heart of the young planet, leaving lighter minerals – such as silicate – to form the crust and mantle.
The formation of the Earth captured a lot of heat inside it. However, it has been lost in the course of its natural history. This is not necessarily negative: on the contrary, it favored the formation of our magnetic field, which protects us from solar storms and allows life as we know it. Most likely, according to British scientists, it will not be like this forever.
We don’t know a lot about the Earth’s core is because it cannot be sampled. Located 5,000 meters below the surface, the information we have is the result of centuries of seismological and geophysical observation. Even today, all we have are models of their behavior. However, a recent study from Cambridge and Bristol, in the United Kingdom, assures that it is growing at uneven rates. This is the reason.
Unlike what we were taught in school, the Earth is not exactly spherical. Rather, it has ridges, peaks, and valleys that make our planet seem perfect blue ball from space. Seen another way, the representations we have of its layers are not exact but are for illustrative purposes only. However, this is not exactly the case. The same trend seems to be replicating within him.
Jessica Irving, a Bristol seismologist, writes in her article for The Conversation, “The core of the Earth was formed very early in the 4.5 billion years of our planet’s history.” It took only 200 million years before the center of our planet finished taking shape. Gravity dragged iron into the heart of the young planet, leaving lighter minerals – such as silicate – to form the crust and mantle.
The formation of the Earth captured a lot of heat inside it. However, it has been lost in the course of its natural history. This is not necessarily negative: on the contrary, it favored the formation of our magnetic field, which protects us from solar storms and allows life as we know it. Most likely, according to British scientists, it will not be like this forever.
Scientists discover that the inner core of the Earth is growing unevenly - OnePexel
No: the core of the Earth is not perfectly symmetrical, and that will affect the nature of our magnetic field in the long term.
onepexel.com