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      "body": "(NC & T) James Wookey is the lead author of the study\n\nThe solid inner core of the Earth began to form more than a billion years ago, when the liquid iron core that surrounds it began to solidify. Since then it has grown to reach a radius of approximately 1,200 kilometers. But the difficulty to study it lies in the thousands of kilometers of rock that separate us from it. As a result, we know more about the surface of other planets than the depths of ours.\n\nHowever, scientists have a powerful tool to study the architecture of the Earth's interior. When large earthquakes or powerful explosions are triggered, vibrations (like sonic waves) travel across the Earth and seismometers can detect them at great distances, even on the other side of the planet. By studying the characteristics of these waves, such as how long they take to get to the instrument, and how strong they are, scientists can infer many things about the interior of the planet.\n\n\n<center>![whataretheea.jpg](https://steemitimages.com/DQmfPb2hg3Syu4sx81bb7uqceSTA5cCPnKRfVG1tsNchLhK/whataretheea.jpg)</center>\n\n<center>[Source](https://phys.org/news/2015-12-earth-layers.html)</center>\n\nThe most recent advances in seismology have resulted from the simultaneous observations of these waves using a very large number of instruments in dense networks. In the present, the largest of these networks is the Japanese Hi-net.\n\n\nAn extra benefit of this network is that the data can also be used to study the interior of the Earth at great depth, looking for the weak vibrations that pass through the core of the planet. One of these very subtle signals is the seismic wave called PKJKP. The properties of this wave contain a treasure trove of data about the inner core of the Earth.\n\nIn addition to obtaining direct evidence of its strength, the team observed evidence of \"texture\" in the inner core iron. This can reveal the patterns left by the solidification process of the liquid iron of the outer core.\n\nMore observations like this will allow seismologists to begin to understand these patterns and what they imply about how the deepest part of our planet has changed throughout its history.\n\n<center>![interior-of-earth.jpg](https://steemitimages.com/DQmP1Ns6L9VH3ZfvLZhGMp8ofNbCA4NeUGcMaw3Kx6GhYgF/interior-of-earth.jpg)</center>\n\n<center>[Source](http://geo-team-tc.blogspot.com/2010/04/continental-drift.html)</center>\n\nThe inner core (the innermost part of the Earth's core) fuses and solidifies simultaneously due to the circulation of heat in the rocky mantle that covers it, according to the results of a new investigation.\n\nWhat was discovered in this study could provide crucial clues to find out how the inner core was formed, and how exactly the outer core (the outermost part of the nucleus) acts as a kind of dynamo, generating the planet's magnetic field.\n\nIn many ways, the origin of Earth's magnetic field remains a mystery to scientists, as Jon Mound reminds us of the University of Leeds, in the United Kingdom, and a member of the research team.\n\nFaced with the impossibility of going to collect samples at the center of the Earth, scientists have to use measurements made much higher, as well as digital models, to try to get an idea of ​​what is happening in the nucleus.\n\nThe new model provides a fairly simple explanation to some of the measurements that have intrigued scientists for years. It suggests that all the dynamics of the center of the Earth is in some way linked to plate tectonics, which is not too evident judging only by the observations made from the surface.",
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      "body": "A tsunami is basically an earthquake that occurs under the seabed. Depending on its intensity and location, it may or may not cause a tsunami. This means that not all tsunamis generate tsunamis, but all tsunamis are generated by tsunamis.\n\nAt the media level, since 2004 when the Indian Ocean Tsunami occurred, tsunamis began to have a great impact. In general terms, a tsunami is the same as a tsunami, and although we tend to think that they are differentiated phenomena, the truth is that in general terms they refer to the same phenomenon\n\n<center>![Como-se-produce-un-maremoto.jpg](https://steemitimages.com/DQmQuwpakqMwTQ74eLwFhmJx3H6XMbxyF92YVx6AiiYNuVk/Como-se-produce-un-maremoto.jpg)</center>\n\n\n<center>[Source](https://www.vix.com/es/btg/curiosidades/2010/08/27/como-se-produce-un-maremoto)</center>\n\n# How is a tsunami formed?\n\n\nLike an earthquake, a tsunami occurs because of movement at the junction of two tectonic plates. The tsunami of the tsunami -or the epicenter of the marine earthquake- is the exact point where the movement or displacement of the tectonic plates begins to take place.\n\nThe intensity of the tsunami is determined by a complex series of variables, but the fundamental thing is the type of geological fault that characterizes the union of the plates. As we saw in another article, there are different types of geological faults, which give rise to different types of earthquakes and tidal waves.\n\n\n<center>![giphy.gif](https://steemitimages.com/DQmYyNw5wsnYLsg1bDtB6a9AnT9Hk7dNmCZ3eW518VpxAu7/giphy.gif)</center>\n\n<center>[Source](https://giphy.com/gifs/woahdude-tsunami-formation-PkjpRBeUcvSKY)</center>\n\nWhen a vertical movement occurs between the plates, the water level rises and the wave begins to form. When it is a sufficiently strong earthquake whose hypocenter is relatively close to the mainland, the elevation of the water level is seen as a withdrawal from the coastline.\n\nThat is to say that if you are on the beach at the time of a tsunami, you will see how the coastline begins to recede, and this means that a tsunami is forming. The height of the wave and the speed at which it moves depends directly on the intensity of the tremor that gives rise to it.\n\n\n\n<center>![X62NV8.gif](https://steemitimages.com/DQmTShhnVMpK3PBmeA6raAeCPS9tHWPf7H6kEo7isaUrE2v/X62NV8.gif)</center>\n\n\n<center[Source](https://stepfeed.com/a-tsumani-strikes-the-burj-khalifa-in-this-new-hollywood-film-9660)</center>\n\n\n\n\nFor example, the tsunami of December 26, 2004 in the Indian Ocean was classified as one of 9.0 Mw (seismological scale of magnitude at the moment, greater intensity than the Richter). It occurred 120 kilometers off the coast of Sumatra, and approximately 30 kilometers below sea level.\n\nThe tremor, between 8 and 10 minutes long, caused a series of tsunamis that spread throughout the Indian Ocean for a couple of hours, but the first wave, about 15 meters high, hit the coast of Sumatra so only in a matter of minutes.\n\nAs we said, a tsunami is the equivalent of an earthquake that happens on the ocean floor. If it is a low intensity one, it is likely that it does not even appear on the surface and does not generate waves so large as to be considered a tsunami. On the contrary, if it is of greater intensity and also occurs close to the coast, a tsunami is one of the most devastating natural catastrophes that can happen.",
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