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Chapter - 3 Structure of the Earth’s Interior (English Medium NCERT Exercise Solution)

NCERT Exercise

                Que 1       Choose the correct answer from the four options given below :-

(i)         Which one of the following earthquake waves is more destructive?

(a) P-waves

(b) S-waves

(c) Surface waves

(d) None of the above

ANS. (c) Surface waves

(ii)        Which one of the following is a direct source of information about the interior of the earth?

(a) Earthquake waves

(b) Volcanoes

(c) Gravitational force

(d) Earth magnetism

ANS. (b) Volcanoes

(iii)       Which types of volcanic eruptions have caused Deccan Trap formations?

(a) Shield

(b) Flood

(c) Composite

(d) Caldera

ANS. (b) Flood

(iv)       Which one of the following describes the lithosphere:

(a) Upper and lower mantle

(b) Crust and upper mantle

(c) Crust and core

(d) Mantle and core

ANS. (b) Crust and upper mantle


         Que 2 Answer the following questions in about 30 words: -

(i) What are body waves?

ANS.  The waves produced by an earthquake are called Earthquake Waves. Geologic waves are generated during the release of energy from the center of an earthquake’s origin and move in all directions in the interior of the earth. These are also called body waves.

There are three types of geological Or Body waves:-

1. P – Primary Waves,

2. S - Secondary Waves

3. L – Long Waves.



(ii) Name the direct sources of information about the interior of the earth.

ANS. 

1. Mining

2. Deep wells

3. Excavating Pipelines

4. Volcano Eruption

5. Deep sea drilling


(iii) Why do earthquake waves develop shadow zone?

ANS.  The area inside the Earth where no seismic wave is recorded on a seismograph is called the shadow region or shadow zone. The area between 105 degrees to 145 degrees from the earthquake epicenter, where no seismic waves are recorded, forms a shadow zone for P and S waves. The shadow zone of S waves is wider than the shadow zone of P waves, which is more than 40% of the Earth's area. The formation of the shadow region proves that the Earth's interior is made up of heavy metals.

 





(iv) Briefly explain the indirect sources of information of the interior of the earth other than those of seismic activity.

ANS. 

In addition to seismic activities, the following are the direct or indirect means of giving information about the earth: -

1. Density of different layers of the earth

2. Rock pressure

3. Temperature

4. Composition of meteorites

5. Gravity

6. Magnetic field.


Que 3       Answer the following questions in about 150 words:-

(i) What are the effects of propagation of earthquake waves on the rock mass through which they travel?

ANS.  Different types of seismic waves have different modes of transmission. For example, the direction of vibration of P waves is parallel to the direction of the waves. This transmission exerts pressure on the material in the same direction of motion. As a result, there is a difference in the density of the substances. The process of contraction and expansion takes place in rocks.

S waves produce vibrations in the vertical plane at right angles to the direction of the waves. Hence, they form bulges and troughs in the medium through which they pass. Surface waves are considered the most destructive.


(ii) What do you understand by intrusive forms? Briefly describe various intrusive forms.

ANS.  When lava solidifies into rock layers below the crust before reaching the surface, various types of forms are formed, which are called intrusive forms. 


Some of the important interpolating figures are as follows: -


1. Batholith: - Whenever the hot magma generated by the volcano cools down in the form of a large body and dome in the cracks inside the earth crust before coming to the surface, then this shape or body made of granite is called batholith. Huh. Sometimes these bodies appear on the surface when the upper matter is removed by denudation (erosion) processes. For example, "Devil's Tower" located in the Devil's Tower National Monument located in the Utah region of America is a similar type of batholith rock.

 




2. Lacolith:- Whenever hot magma in penetrating rocks gets deposited in a flat or pipe-like conveyance tube, it is called lacolith. Their shape resembles the dome of a mixed volcano found on the surface. Lacoliths are found at greater depths. Many such domed hills made of granite rocks are found in the Karnataka plateau.




3.   Lapolith:- If some part of the rising lava goes in the horizontal direction and freezes in the form of a saucer, then it is called Lapolyth.


4. Phacolith:- When magma freezes in the form of anticline and syncline in a wavy or flaky shape, it is called a phacolith.

5. Sill or sheet:- The cooling of penetrating igneous rocks in the form of a sheet in a horizontal plane is called a sill or sheet. On the basis of the thickness of the deposit, it is divided into - low thickness deposits are called sheets and high thickness deposits are called sill.

6. Dyke:- When the lava flows into the cracks at approximately right angles to the surface and if it cools down to this stage, it forms a wall like structure, which is called a dike. Such figures are found in abundance in the Deccan trap of western Maharashtra.


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