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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 If a seafloor map shows rock age increasing on both sides away from a mid oceanic ridge what is the most accurate interpretation?
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Answer and explanation
Correct answer: A. New crust forms at the ridge and spreads on both sides
Explanation: Symmetrical age pattern is strong evidence of seafloor spreading. Exam tip: read distance from ridge with crustal age.
04 On a bathymetric map if isobaths are widely spaced on a ridge top but closely spaced on its flank what does it mean?
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Answer and explanation
Correct answer: A. Ridge crest is relatively gentle and flank is steep
Explanation: The direct answer is A: the ridge top has a relatively gentle slope, while its flank has a steep slope. An isobath is a line joining places of equal water depth on a bathymetric map. The key rule is about spacing: widely spaced isobaths show that depth changes slowly over a long horizontal distance, so the slope is gentle. Closely spaced isobaths show that depth changes quickly over a short distance, so the slope is steep. Therefore, wide spacing on the crest and close spacing on the flank gives the conclusion in A. B is wrong because equal depth would not produce this changing spacing pattern. C is wrong because spacing alone does not prove that the ridge is a continental shelf. D is wrong because isobaths do indicate underwater slope. Memory cue: close contours mean a sharp slope; wide contours mean a gentle slope.
05 If fracture zones are seen cutting a ridge into segments on a detailed seafloor map what is their main significance?
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Answer and explanation
Correct answer: A. They show plate motion and transform fault orientation
Explanation: Fracture zones indicate lateral displacement and plate motion in oceanic crust. Exam tip: treat linear seafloor structures as tectonic evidence.
12 If a submerged mountain has a flat top and deep floor around it what does it indicate about its earlier stage?
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Answer and explanation
Correct answer: A. It may once have been flattened by erosion near sea level
Explanation: The direct answer is A: the flat-topped submerged mountain may once have been flattened by erosion near sea level. Such a flat-topped seamount is called a guyot. The reasoning is: a volcano or underwater mountain can rise above or close to sea level; waves and weathering can erode its top and make it nearly flat; later, the sea floor or the volcanic block may subside, leaving the flat top deep underwater. Thus a flat top and deep surrounding floor provide evidence of an earlier near-sea-level stage, not proof of its present position. B is wrong because a guyot is not always a river delta. C is wrong because it need not be part of the Himalayas. D is wrong because the mountain is submerged now, and the feature specifically suggests earlier exposure or near-surface erosion. Memory cue: guyot = flat top, erosion, later sinking.
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