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The oceanic lithosphere is usually between 31 and 87 miles thick. The continental lithosphere is usually between 25 and 174 miles thick.

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What is the thickness of the 2 parts in the lithosphere?

both of them together is 333 kilometers. you can search the Internet for how thick the crust is and subtract that from 333 to get the thickness of the mantle part.


What is the average thickness of the lithosphere?

The average thickness of the lithosphere is around 100 kilometers, but it can vary depending on the location and whether it is oceanic or continental lithosphere. Oceanic lithosphere is typically thinner (around 5-10 kilometers) compared to continental lithosphere, which can be up to 200 kilometers thick.


Where is lithosphere located?

The lithosphere is located on the outermost layer of the Earth, consisting of the crust and part of the upper mantle. It is broken into tectonic plates that float on the semi-fluid asthenosphere beneath them. The lithosphere varies in thickness beneath the oceans and continents.


How is earth lithosphere related to the crust?

how is the earths crust related to the lithosphere


How far is it to the lithosphere from the crust?

The lithosphere is part of the Earth's crust and uppermost mantle; it includes the crust itself. So, the distance to the lithosphere is essentially the same as the thickness of the crust, which varies from about 5 to 75 kilometers (3 to 46 miles) beneath the oceans and continents.


What what is the lithosphere?

The lithosphere is the solid, rocky layer covering the entire surface of the planet, composed of the crust and the hard uppermost mantle, and reacts to stresses as a brittle solid. The lithosphere ranges in thickness from 50 - 200 km and is fragmented into tectonic plates with boundaries where plates collide, diverge, or grind past each other.Lithosphere is the solid part of the Earth.Like land,and crops.The land part of the earth on the crust


What are facts about the earth lithosphere?

Facts about the Earths's lithosphere:The lithosphere includes the Earths's crust and upper mantle.it is broken into tectonic plates.The uppermost part of the lithosphere is known as the 'pedosphere'. This is the part that reacts to the atmosphere and biosphere through the soil forming process.there are two types of lithosphere - oceanic and continental.Oceanic lithosphere ranges between 50-100 km in thickness.Continental lithosphere ranges between 40 and 200 km in thickness.


What are facts about Earth's lithosphere?

Facts about the Earths's lithosphere:The lithosphere includes the Earths's crust and upper mantle.it is broken into tectonic plates.The uppermost part of the lithosphere is known as the 'pedosphere'. This is the part that reacts to the atmosphere and biosphere through the soil forming process.there are two types of lithosphere - oceanic and continental.Oceanic lithosphere ranges between 50-100 km in thickness.Continental lithosphere ranges between 40 and 200 km in thickness.


What is the thickeness of each part?

the thickness of each part is the mantle, the inner core, and inner core


What includes the uppermost part of the mantle and the crust?

The lithosphere encompasses the uppermost part of the mantle and the crust. This layer is broken into tectonic plates that move and interact with each other at plate boundaries. The lithosphere is relatively rigid compared to the underlying asthenosphere.


Which is thicker the earth's crust or the lithosphere?

The lithosphere is thicker than the Earth's crust. The lithosphere includes the crust and the upper part of the mantle, typically ranging in thickness from about 100 to 200 kilometers beneath the oceanic crust and up to 250 kilometers beneath continental crust.


Earths crust and the very top of the mantle combined?

This combined layer is called the lithosphere, which includes the crust and the uppermost solid portion of the mantle. It varies in thickness beneath the oceans and continents, with the oceanic lithosphere being thinner and denser than the continental lithosphere. The lithosphere is divided into large plates that move and interact with each other, causing geological phenomena like earthquakes and volcanic eruptions.