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Capas de la geosfera
Ismael Pérez Pulido
Created on February 3, 2024
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Transcript
Crust
It It is the outer layer and the thinnest and therefore the one with the most depth. It is made up of minerals and solid rocks. It has a thickness of 80 km. It is differentiated into two layers: oceanic crust and continental crust. Continental crust: It is the one that is formed by the continents. Oceanic crust: It is that which is found in the depths of the oceans.
differences between them
The oceanic crust is younger than the continental crust ·The continental crust measures more than its thickness (almost double)
- The oceanic crust is denser but it is thinner (in the case of the continental crust it is the opposite)
LTOSPHERE:Litosphere is the layer that separates the crust from Earth and has a depth of 830 km The Litosphere is the most solid part of our planet
Core:It is the innermost layer. It is a solid layer formed by ice and nickel with a high density. It has a radius of 3500 km. It has a high temperature. It is divided into two parts: the outer core, which is more fluid, and the inner core, which belongs to the solid part of the earth. The layer that separates the inner core from the outer core is called Lehman, it is 5100km deep.
GUTERBERG DISCONTINUITY
The separation between the mantle and the core is called the Guterberg discontinuity and is 290 km deep.
Núcleo
Lorem ipsum dolor sit amet, consectetur adipiscing elit, sed do eiusmod tempor incididunt ut labore et dolore magna aliqua. Lorem ipsum dolor sit amet, consectetur adipiscing elit, sed do eiusmod.
Lorem ipsum dolor sit
- Lorem ipsum dolor sit amet.
- Consectetur adipiscing elit.
- Sed do eiusmod tempor incididunt ut.
- Labore et dolore magna aliqua.
MANTLE
The mantle is the intermediate layer, it is a solid layer formed by rocks denser than the crust, it has a thickness of 1900 kilometers Thanks to its temperature and thickness, its depth increases, representing 83 percent of the total volume of the geosphere, being the outermost layer. This layer is divide into 2 parts: The upper mantle and the lower mantle are separated by REPETTI dyscontinia.It is 670km deep. Upper mantle has a volume of 670 km and is 200 degrees Lower mantle has 2900 km of volume and occupies 56% of the Earth