Earth's Internal Structure: Lithosphere, Asthenosphere, and Core
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Lithosphere and the Asthenosphere Paradigm
The crust and mantle form a rigid layer known as the lithosphere. This layer is fractured into lithospheric plates, which include:
- Oceanic Plates: Composed of basaltic oceanic crust.
- Continental Plates: Composed of granitic continental crust.
The Asthenosphere
The lithosphere is a rigid, fragmented layer consisting of large blocks moving at speeds of several centimeters per year. During the 1970s and 1980s, it was established that the asthenosphere acts as a continuous layer beneath the lithosphere, serving as a lubricant. Without this layer, the movement of the lithosphere would be impossible due to friction with the underlying mantle.
The Terrestrial Core
Heat generated by early planetary collisions and... Continue reading "Earth's Internal Structure: Lithosphere, Asthenosphere, and Core" »