That's what I'm trying to find out. Can somebody please answer it.! D:
The thickest part of the lithosphere is typically found beneath continental regions, where the crust can be up to 70 km thick. This thick continental lithosphere is composed of both the crust and the uppermost part of the mantle.
The lithosphere can have two main types of crust: continental crust and oceanic crust. Continental crust is thicker, older, and less dense than oceanic crust. Oceanic crust is thinner, younger, and denser, primarily composed of basaltic rocks.
The parts of the Lithosphere are the crust, mantel and core.
When two continental plates collide, the crust is thickened, buckled and deformed--gaining elevation. Mountain chains are the result; their creation occurring over periods of millions of years.
The upper section of the lithosphere is known as the crust. It is made up of solid rock that includes both continental crust, found beneath landmasses, and oceanic crust, found beneath oceans. The crust is the outermost layer of the Earth's surface.
Collisions Of Continental Plates
The thickest part of the lithosphere is typically found beneath continental regions, where the crust can be up to 70 km thick. This thick continental lithosphere is composed of both the crust and the uppermost part of the mantle.
the crust + lithosphere earth's crust: crust crust continental crust lithosphere crust continental and oceanic crust mantle asthenosphere mantle lower mantle mantle outer core outer core inner core inner core
The lithosphere can have two main types of crust: continental crust and oceanic crust. Continental crust is thicker, older, and less dense than oceanic crust. Oceanic crust is thinner, younger, and denser, primarily composed of basaltic rocks.
The parts of the Lithosphere are the crust, mantel and core.
When two continental plates collide, the crust is thickened, buckled and deformed--gaining elevation. Mountain chains are the result; their creation occurring over periods of millions of years.
Most are found on converging
The upper section of the lithosphere is known as the crust. It is made up of solid rock that includes both continental crust, found beneath landmasses, and oceanic crust, found beneath oceans. The crust is the outermost layer of the Earth's surface.
The lithosphere displaces the asthenoshpere. Thick tectonic plates, such as those made of continental crust, displace more asthenosphere than do thin plates, such as those made of oceanic lithosphere. The lithosphere displaces the asthenoshpere. Thick tectonic plates, such as those made of continental crust, displace more asthenosphere than do thin plates, such as those made of oceanic lithosphere.
Iron, Fe, is the 4th largest element found on the lithosphere.
Normal faulting predominantly occurs at divergent plate boundaries. At these boundaries, tectonic plates move apart, causing the hanging wall to drop relative to the footwall. This results in the extension of the Earth's crust, which is characteristic of normal faults. Such faults are commonly found at mid-ocean ridges and continental rift zones.
The lithosphere typically starts at a depth of about 0 kilometers at the Earth's surface, extending down to approximately 100 kilometers (62 miles) beneath the surface. It encompasses the crust and the uppermost portion of the mantle. The exact depth can vary depending on tectonic settings, with thicker lithosphere found in continental regions compared to oceanic areas.