Unlocking Earth's Secrets: The Role of Seismic Waves in Understanding Earth's Interior Layers

Unlocking Earth’s Secrets: The Role of Seismic Waves in Understanding Earth’s Interior Layers | Sociology UPSC | Triumph IAS

Layers of Earth

(Relevant for Geography Section of General Studies Paper Prelims/Mains)

Unlocking Earth's Secrets: The Role of Seismic Waves in Understanding Earth's Interior Layers

Layers of earth: role of seismic waves in the study of the interior of earth.

On the basis of seismic investigations, the earth can be divided into three major layers: crust, mantle, core.

Differentiation of layers of Earth

Earth Structure:

  • Crust: The Earth’s outermost layer is referred to as the “crust.” In regions with continents, the crust can be categorized into two distinct layers. The upper layer, characterized by its lower density and granitic composition, is known as the “sial.” Conversely, the lower layer, consisting of basaltic composition, is termed “sima.” This division extends approximately 30 to 40 kilometers beneath continental areas and about 10 kilometers beneath ocean basins.
  • Mantle: Beneath the Earth’s crust lies the mantle, which has a thickness of approximately 2900 kilometers. The mantle can be segmented into two layers: (i) the upper mantle and (ii) the lower mantle. The demarcation between these layers occurs around 700 kilometers beneath the surface. An integral zone within the upper mantle is the “asthenosphere,” situated at depths ranging from 50 to 100 kilometers. This zone plays a pivotal role in supplying lava for volcanic activities.
  • Core: The Earth’s core, comprising both the inner core and the outer core, occupies merely 16 percent of the planet’s volume yet contributes to 33 percent of its mass. Similar to the mantle, the core can be delineated into two layers: the outer core and the inner core. The outer core is composed of a mixture of iron, nickel, and trace quantities of lighter elements. Due to the insufficient pressure exerted on the outer core, it remains in a liquid state, despite sharing a composition akin to that of the inner core.

The study of the passage of seismic waves through the earth has helped in knowing the structure of the earth’s interior and in defining the physical properties of various layers. For example:

  • The “outer core” was discovered when it was found that P-waves were bent inwards thereby producing a “shadow zone” at the surface.
  • Since the S-waves do not pass through the outer core, it is concluded that it may be in the liquid state.

Seismic waves travel different velocities depending on the nature of the layer in which they are travelling. Thus they not only indicate the position of each layer but also give clues as to its composition.

Sample Question for UPSC Sociology Optional Paper:

Question 1: What are the major layers of the Earth’s interior?

Short Answer: The Earth’s interior is primarily divided into three major layers: the crust, the mantle, and the core.

Question 2: How do seismic waves help in the study of Earth’s interior?

Short Answer: Seismic waves help in the study of Earth’s interior by providing data on the speed and direction of wave travel. This information enables scientists to deduce the composition and properties of various layers, such as the presence of a liquid outer core.

Question 3: Explain the concept of the “shadow zone” in seismic studies.

Short Answer: The “shadow zone” refers to the area where seismic waves, particularly P-waves, are bent inwards and do not reach, revealing information about the composition of Earth’s layers like the outer core.

Question 4: What role does the asthenosphere play in Earth’s geology?

Short Answer: The asthenosphere, located within the upper mantle, is a zone that plays a critical role in plate tectonics and supplies lava for volcanic activities.

Question 5: How does the velocity of seismic waves vary across different layers of Earth?

Short Answer: The velocity of seismic waves changes depending on the nature and composition of the layer they travel through. For example, S-waves do not travel through the outer core, suggesting it is liquid, while P-waves are refracted due to changes in density and composition.

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