Previous knowledge about the Formation and Evolution of our beloved Planet Earth.
Fraternal greeting to the entire community, this time I come to give you a summary of how the creation of the Earth was, collecting some classes of the career that I love so much, as is Geography.
At first there were great controversies between two opposing ideas, for the moment there was a group of geologists who thought that all the rocks had been formed at the bottom of the seas, this idea was subject by the German Abraham Werner; On the other hand there were the English James Hutton and James Hall who thought that some rocks had at least been formed by cooling on the surface of the Earth, by cooling volcanic rocks or lava. These scientists were called the Plutonists and it was a controversy between two schools, where neither of them were right, but they were right.
How was the Planet Earth formed?
On the other hand were the catastrophe, they thought that the earth had been formed by successive catastrophes and that since the last catastrophe there were no changes on Earth, an example of a catastrophe was Georges Cuvier, with time the Uniformists obviously predominated.
At the same time, an English engineer by the name of Willian Smith came up with the mapping of the surface of England according to the relative age of the layers, this engineer drew the first geological map of England where the different units put the different successive layers and observed that they were characterized by different fossils and discovered which were older and which were more modern, in this way the mapping and a very fundamental breakthrough was originated.
What materials exist on Earth?
The Structure of the Earth
The crust of the Earth is formed by the continental crust and is where the continents are located, this crust is thicker between 30 and 50 km thick and is formed by very light rocks. The oceanic crust is thinner than the continental one between 5 and 10 km thick and is formed by denser rocks. Both the continental crust and the oceanic crust together with the most superficial layer of the mantle form what is called Lithosphere, of great importance since the plates that form the earth are not formed only by crust, that is to say they are lithospheric plates that cover the crust plus the upper layer of the mantle, between the lithosphere and the asthenosphere occurs a discontinuity that causes the plates to slide.
There were moments in the history of the Earth in which the poles were as they are observed today, and moments when the poles were reversed, this led to a study of Paleomagnetism of the rocks of the ocean floor, perpendicular to the oceanic ridge it was observed that the rocks closest to the dorsal had magnetism coincident with the current, then there was a strip of reverse magnetism and another of normal magnetism, but it was also observed that it was symmetrical with respect to the large oceanic ridges, that is, both sides of the dorsal the normal and reverse magnetism bands were totally symmetrical, this allowed us to think that what was happening was that the rocks that were in the center of the dorsal are the most modern, and that as we move away from the dorsal the rocks are the oldest and give an idea that the ocean floor expanded and that the magma that rises in the center of those ridges solidifies and moves. and moving away from the dorsals gradually. This theory was proposed by Harry Hess, then it would only be to join the theory of the drift of the continents and reach the theory of plate tectonics, where basically the lithosphere is fragmented into discrete plates and that these plates move relatively with respect to the others.
There are margins of the plates where the plate is produced or grown by the production of new bark, which would be at the oceanic ridges and there are places where the plates collide in different ways creating mountainous chains, such as the Himalayas, a mountain range formed by the collision of plates; the plates can also get under each other forming what we call subduction.
Hi, I am a big fan of geology content and am looking forward to read more from you.
But it would be nice if you could source your information and double check if your images are copyrighted.
Hello friend, the images are from google, each of them has its respective source ...