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- Lithosphere - Wikipedia
Earth's lithosphere, which constitutes the hard and rigid outer vertical layer of the Earth, includes the crust and the lithospheric mantle (or mantle lithosphere), the uppermost part of the mantle that is not convecting
- Lithosphere | Definition Facts | Britannica
Lithosphere, rigid, rocky outer layer of Earth, consisting of the crust and the solid outermost layer of the upper mantle It extends to a depth of about 60 miles (100 km) The lithosphere is broken up into about a dozen separate, rigid blocks, or plates
- Lithosphere - National Geographic Society
The lithosphere is the solid, outer part of Earth The lithosphere includes the brittle upper portion of the mantle and the crust, the outermost layers of Earth’s structure It is bounded by the atmosphere above and the asthenosphere (another part of the upper mantle) below
- A Complete Guide to Earth’s Lithosphere - Geology Base
The lithosphere is the outermost, rigid, solid layer of the Earth It is like the shell of a coconut or egg Location-wise, this layer lies above the asthenosphere and below the atmosphere, ice, or water bodies An asthenosphere is a weaker, ductile layer By ductile, we mean it stretches or deforms under stress
- The lithosphere: Facts about Earths outer shell | Space
The lithosphere is Earth's outermost layer, composed of the crust and the upper part of the mantle The layer is divided into chunks called tectonic plates
- Lithosphere and Asthenosphere – Geology In
The lithosphere and the asthenosphere are the two layers of the Earth closest to the surface These layers differ significantly in their physical properties, composition, and behavior The lithosphere is the Earth’s hard, rigid, outermost rocky shell
- Lithosphere - Encyclopedia. com
The lithosphere is the solid outer section of Earth, which includes Earth's crust (the "skin" of rock on the outer layer of planet Earth), as well as the underlying cool, dense, and rigid upper part of the upper mantle The lithosphere extends from the surface of Earth to a depth of about 44 – 62 mi (70 – 100 km) This relatively cool and
- The Role of Earth’s Lithosphere in Plate Tectonics
Where Lithosphere Dies: The Subduction Zones But just as the lithosphere is created, it must also be destroyed Earth is a closed system—if new lithosphere is constantly being added at mid-ocean ridges, it must be recycled elsewhere to keep the planet in balance This recycling occurs at subduction zones
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