Class 11 Geography Important Chapter 3 Interior of the Earth

Class 11 Geography Important Chapter 3 Interior of the Earth Solutions English Medium As Per AHSEC New Syllabus to each chapter is provided in the list so that you can easily browse through different chapters ASSEB Class 11 Geography Important Solutions and select need one. AHSEC Class 11 Elective Geography Additional Notes English Medium Download PDF. HS 1st Year Finance Important Solutions in English.

Class 11 Geography Important Chapter 3 Interior of the Earth

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Also, you can read the NCERT book online in these sections Solutions by Expert Teachers as per Central Board of Secondary Education (CBSE) Book guidelines. ASSEB Class 11 Elective Geography Additional Question Answer are part of All Subject Solutions. Here we have given HS 1st Year Elective Geography Important Notes in English for All Chapters, You can practice these here.

Chapter: 3

SECOND UNIT : OUR EARTH
IMPORTANT QUESTION AND ANSWER

Answer The Following Questions:

1. What is the Core?

Ans: The core is the innermost layer of the Earth, extending from the lower region of the mantle to the centre of the Earth.

2. What is the Crust?

Ans: The crust is the thin, outermost, and solid rocky layer of the Earth, composed of two sub-layers — Sial and Sima.

3. Why is the Core called NiFe?

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Ans: The core is called NiFe because it mainly consists of nickel (Ni) and iron (Fe).

4. What are the main elements found in the Earth’s crust?

Ans: The Earth’s crust mainly contains silicon (Si), aluminium (Al), magnesium (Mg), and oxygen (O).

5. What is the Kola Project?

Ans: The Kola Project refers to the deepest drilling experiment in the world, where a borehole was drilled up to a depth of 12 kilometres.

6. What are L-Waves?

Ans: L-waves are surface seismic waves that travel only along the Earth’s surface and are the most destructive type of earthquake waves.

7. Where is the Kola Basin located?

Ans: The Kola Basin is located in the Arctic Ocean.

8. What is Moho?

Ans: The surface separating the crust and the mantle is called the Mohorovičić Discontinuity or simply the Moho.

9. What do earthquakes originating inside the Earth produce?

Ans: Earthquakes originating inside the Earth produce waves or vibrations.

10. At what depth is the earthquake’s focus generally located?

Ans: The focus of an earthquake is generally located between 50 and 100 kilometres below the Earth’s surface.

Long Question & Answer:

1. On what sources does our knowledge about the interior of the Earth mainly depend? How do these sources help reveal the Earth’s internal structure?

Ans: Our knowledge about the Earth’s interior mainly depends on indirect sources because human exploration is limited to about 12 kilometres below the surface. 

Scientists use several indirect methods to study the Earth’s structure, such as:

(i) Seismic waves.

(ii) Volcanic lava.

(iii) Deep mines and ocean drilling.

(iv) Geothermal heat.

(v) Meteorites.

Seismic waves (P and S waves) travel at different speeds through different materials, helping scientists identify solid and molten zones. Lava from volcanoes provides direct evidence of molten material from the Earth’s interior. Deep mining and drilling help study the composition, density, and temperature of rocks. The study of meteorites reveals information about the Earth’s primitive composition and temperature-pressure conditions. All these indirect sources together help scientists classify the Earth into three main layers — crust, mantle, and core.

2. Express your opinion on how the study of earthquakes, meteorites, and heat flow helps understand the structure of the Earth’s interior.

Ans: The study of the Earth’s interior is an important scientific pursuit. Since direct exploration is not possible, scientists depend on indirect evidence such as earthquakes, meteorites, and heat flow.

(i) The movement of seismic waves (P and S waves) helps determine the density, composition, and state of materials inside the Earth. The inability of S-waves to travel through liquid matter proves that the Earth’s outer core is molten.

(ii) Meteorites, which are ancient cosmic bodies, have compositions similar to the Earth’s early materials. Their study helps identify the basic structure and mineral composition of the interior.

(iii) The geothermal gradient shows that temperature increases with depth, helping scientists estimate the heat and molten state inside the Earth.

These studies have given scientists a clear, evidence-based understanding of the crust, mantle, and core — knowledge crucial for mineral exploration, earthquake prediction, and human safety.

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