Lithosphere - Definition, Features, Diagram, FAQs

Lithosphere - Definition, Features, Diagram, FAQs

Vishal kumarUpdated on 02 Jul 2025, 04:59 PM IST

The lithosphere refers to the hard outer shell of the Earth that includes the crust and the uppermost part of the mantle. It is responsible for the planet's surface and nurtures life by its ever-changing geological processes. In this article, the discussion will give the meaning of lithosphere, its important elements, a labelled illustration and its diagram and the commonly asked questions.

Lithosphere - Definition, Features, Diagram, FAQs
Lithosphere

What is Lithosphere?

“The lithosphere is the rigid, outermost shell of planet Earth.” It is composed of the crust and the portion of the upper mantle that behaves elastically on time scales of thousands of years or greater.

Lithosphere Examples- the Rocky Mountain range of mountains in western North America is one of the examples of the lithosphere.

Also read -

Lithosphere Composition

The Lithosphere is made up of the brittle, rigid and solid upper portion of the mantle and the crust, the outermost layers of Earth’s structure. The lithosphere consists of rocks of the earth’s crust & it also contains thin layers of soil. The soil holds the nutrient elements which sustain organisms. The lithosphere is exposed to the atmosphere from the top and is bounded by the asthenosphere (another part of the upper mantle) below it.

Lithosphere Meaning

"Litho" is from the Greek word lithos, meaning stone. "Sphere" is from the Greek word sphaira, meaning globe or ball.

Features of Lithospheres

The lithosphere consists of the crust and the upper mantle.

  • The lithosphere is the outer part of the Earth.

  • The lithosphere is made up of the Earth’s crust and upper mantle(It is the outermost layer of the upper mantle).

  • The lithosphere is about 55 km thick below the oceans.

  • The lithosphere is up to about 200 km thick below the continents.

  • The seismic waves propagate with very high velocity through the lithosphere and these waves suggest that Lithosphere is completely solid.

NEET Highest Scoring Chapters & Topics
This ebook serves as a valuable study guide for NEET exams, specifically designed to assist students in light of recent changes and the removal of certain topics from the NEET exam.
Download E-book

How is the Lithosphere Formed?

Earth Time → Cooling Solidification Condensation into small size.

Development of outer surface(crust)

Explanation:

This has been explained in many lithosphere pdf and lithosphere ppt: “During the primordial stage, Earth was in a volatile state. At that time there was nothing called the Lithosphere”. We were not aware of How the lithosphere formed. Then due to the gradual increase in the density, the temperature of the Earth increased. As a result of this change, the material inside the Earth began to separate depending on their densities. This becomes the reason for the answer to the question How is the lithosphere formed?

Consequently, the heavier material (like iron) sank into the centre of the Earth i.e. the core. And the lighter material moved towards the surface of the Earth. Then with time the lighter material cooled down and solidified, further condensed into small sizes. This process leads to the development of the Lithosphere.

Earth's lithosphere includes the crust and the mantle (uppermost). The uppermost mantle is the outer layer of Earth which is solid, rigid and brittle. The lithosphere is subdivided into tectonic plates. The Lithosphere- Asthenosphere boundary is formed due to the difference in response to stress. That’s why the lithosphere deforms elastically while the asthenosphere deforms viscously.

Lithosphere Facts

  • Scientists nowadays use robots to examine the lithosphere on outer space planets. For Example, recently on Mars.

  • Lithosphere depth is different at different places.

  • At the boundaries of each plate, the composition of the crust changes.

Frequently Asked Questions (FAQs)

Q: What is the future of Earth's lithosphere?
A:
The future of Earth's lithosphere will involve continued plate tectonic activity, with the creation of new oceanic lithosphere at mid-ocean ridges and the destruction of old lithosphere at subduction zones. Over hundreds of millions of years, the configuration of continents will change, potentially forming new supercontinents. However, as the Earth slowly cools, tectonic activity may eventually slow down, potentially leading to a "stagnant lid" scenario similar to what we see on other terrestrial planets.
Q: How does the lithosphere affect Earth's magnetic field?
A:
The lithosphere records the Earth's magnetic field as it forms, particularly in oceanic lithosphere. This "fossil magnetism" has been crucial in understanding plate tectonics and the history of Earth's magnetic field reversals.
Q: How does the lithosphere affect global climate?
A:
The lithosphere affects global climate through processes like weathering of rocks (which consumes CO2), volcanic emissions (which release CO2 and other gases), and the arrangement of continents, which influences ocean currents and atmospheric circulation patterns.
Q: What is meant by lithospheric stress?
A:
Lithospheric stress refers to the forces acting on the lithosphere that can cause it to deform. These stresses can be compressional, tensional, or shear, and they drive processes like mountain building, rifting, and the formation of faults and folds.
Q: What is the role of the lithosphere in the formation of mineral deposits?
A:
The lithosphere plays a crucial role in the formation of mineral deposits. Processes like magmatism, hydrothermal circulation, and metamorphism within the lithosphere concentrate valuable minerals, forming economically important ore deposits.
Q: How does the lithosphere affect seismic wave propagation?
A:
The lithosphere affects seismic wave propagation due to its rigid nature and varying thickness. Seismic waves travel faster through the cold, rigid lithosphere than through the underlying asthenosphere, allowing seismologists to map the thickness and structure of the lithosphere.
Q: How does lithospheric structure vary between continents and oceans?
A:
Continental lithosphere is generally thicker (up to 200 km or more) and less dense than oceanic lithosphere. Oceanic lithosphere is thinner (usually less than 100 km), denser, and compositionally more uniform. These differences affect how these types of lithosphere behave in tectonic processes.
Q: What is lithospheric foundering?
A:
Lithospheric foundering, also known as delamination, is a process where a portion of the dense lower lithosphere detaches and sinks into the less dense asthenosphere. This can lead to uplift, increased heat flow, and volcanism at the surface.
Q: What is the relationship between the lithosphere and Earth's gravity field?
A:
Variations in the thickness and density of the lithosphere create small but measurable variations in Earth's gravity field. These gravity anomalies are used to study the structure of the lithosphere and underlying mantle.
Q: What is meant by lithospheric instability?
A:
Lithospheric instability refers to conditions where parts of the lithosphere become unstable and prone to deformation or removal. This can occur due to thermal or compositional factors and can lead to processes like delamination or convective removal of the lithosphere.

Questions related to

On Question asked by student community

Have a question related to ?

Correct Answer: The theory of plate tectonics proposes that the earth’s lithosphere is divided into seven major and some minor plates.


Solution : The correct answer is The theory of plate tectonics proposes that the Earth’s lithosphere is divided into seven major and some minor plates.

The theory of plate tectonics suggests that the outer shell, also called the lithosphere, is divided into several plates, of which there are seven and some minor plates. The theory interacts with three types of plate boundaries: divergent, convergent and transform. Alfred Wegener is considered the father of the theory of plate tectonics.

Correct Answer: 7


Solution : The correct option is 7.

Plate tectonics proposes that the Earth's lithosphere is divided into several rigid plates that interact with each other, leading to various geological phenomena. There are seven major tectonic plates:

  1. Pacific Plate
  2. North American Plate
  3. South American Plate
  4. Eurasian Plate
  5. African Plate
  6. Antarctic Plate
  7. Indo-Australian Plate

In addition to the seven major tectonic plates, there are numerous minor plates, also known as secondary or microplates.