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Geography

Sources of information

In Class 11 Geography, this topic introduces how scientists investigate the Earth’s interior, which cannot be observed directly. Students distinguish direct evidence from mines, deep drilling and volcanic materials, and indirect evidence from seismic waves, meteorites, gravity, magnetic fields, and variations in temperature and pressure. The topic explains how these sources help infer the Earth’s internal structure and composition within the chapter Interior of the Earth.

Easy · Level 4 · 25 questions

Practice questions

01Density inside Earth can be inferred from what?

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02Why are meteorites linked with the study of Earth's interior?

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03Information obtained from mining is mostly limited to which part of Earth?

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04Volcanic lava is not always a direct sample of which deep part of Earth?

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05Why are artificial explosions used in studying Earth's interior?

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06Which property of seismic waves helps estimate thickness of Earth's layers?

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07Which source gives clues about magnetic properties of internal materials?

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08Internal temperature of Earth can be directly measured by what?

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09What is the graph obtained from a seismograph called?

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10If S waves are absent in a region what can scientists infer?

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11What generally happens when seismic waves pass through rigid material?

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12Why is direct digging to Earth's centre not possible?

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13Which of the following is a direct method of studying Earth's interior?

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14Information obtained from earthquake waves is of what type?

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15What gives a clue that the core is metallic?

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16Different layers inside Earth are mainly known through what?

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17Which example is the correct match of source and information?

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18Which question is most important for knowing the state of internal layers?

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19Rocks of the ocean floor provide information about what?

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20Which evidence is most useful in understanding the boundary between crust and mantle?

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21In which method does real material from inside Earth come out for study?

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22Why are indirect sources needed?

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23Which of the following shows a limitation of direct sources?

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24Which source helps understand Earth's internal structure without digging?

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25How are correct conclusions made in the study of Earth's interior?

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