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In this Class 11 Geography topic from “Distribution of Oceans and Continents,” students learn how the ocean floor is mapped and interpreted. They explore major features such as continental shelves, slopes, deep-sea plains, mid-ocean ridges, trenches and seamounts, and understand how soundings, sonar and bathymetric maps reveal underwater relief. The topic also helps connect ocean-floor patterns with plate boundaries, seafloor spreading and the changing distribution of continents and oceans.
Practice questions
01 Why is half of the total travel time of a sound wave used in echo sounding?
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Answer and explanation
Correct answer: A. Because the wave goes down and then returns
Explanation: The total time is for a two-way journey so half is used for depth. Exam tip: remember the two-way travel in echo sounding.
05 How is satellite altimetry different from direct sonar measurement in ocean floor mapping?
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Answer and explanation
Correct answer: D. It estimates relief from sea-surface height signals
Explanation: The satellite method does not touch the sea floor directly but estimates it from surface changes. Exam tip: remember it as an indirect method.
13 How can the relation between a seamount and island formation be understood?
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Answer and explanation
Correct answer: A. A seamount may form an island if it rises above the surface
Explanation: Seamounts are often volcanic elevations and can become islands if they rise above the surface. Exam tip: connect seamounts with volcanic origin.
14 By which feature is a guyot identified on an ocean floor map?
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Answer and explanation
Correct answer: B. A flat-topped seamount
Explanation: A guyot is a submerged seamount with a flat top. Its summit was flattened by wave erosion when it was near sea level, and it later subsided below the ocean surface. An ocean trench is a deep, narrow depression, so it is not a guyot. Exam tip: remember a guyot as a “flat-topped seamount.”
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