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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.
TOPIC PRACTICE
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New crust forms at the ridge and spreads on both sides
New crust forms in trenches and moves toward ridges
Continental shelf alone forms oceanic crust
Seawater decreases the age of rocks
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Depth becomes half
Depth doubles
Depth becomes zero
Depth remains unchanged
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A dipping belt of earthquakes along the trench
Constant temperature lines above the trench
A wide sandy coast far from the trench
A fishing ground near the trench
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Ridge crest is relatively gentle and flank is steep
The whole region has equal depth
The ridge must be a continental shelf
Isobaths do not indicate slope
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They show plate motion and transform fault orientation
They are only remnants of river meanders
They are salinity lines of seawater
They are boundaries of fish species
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Seafloor away from ridge is older so it had more time for sediment accumulation
Sediment always makes mountains on ridges
The distant floor must be continental
Sediment thickness has no relation with time
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Tiny sea surface bulges relate to gravity mass variations
It sends a camera inside the ocean
It measures chemical age of every rock
It makes the ocean transparent
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When making a detailed model of a complex trench and seamount area
When only one well depth is needed
When measuring sea surface colour
When counting coastal population
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Magnetic reversals were recorded in new crust and the floor spread both ways
Seawater always flows in one direction
Continental shelf forms the oldest crust
Trenches cannot have magnetism
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Because slope change may be gradual and covered by sediments
Because shelf is not found in oceans
Because isobaths are always absent
Because sound cannot travel in water
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Wide shelf thick sediments and absence of deep trench
Narrow shelf deep trench and intense earthquake belt
Rift at ridge center and high heat flow
Trench parallel to island arc
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It may once have been flattened by erosion near sea level
It was always a river delta
It is currently part of the Himalaya
It was never submerged in the ocean
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Because submarine currents carry sediment down the slope and spread it
Because sunlight reaches there the most
Because tides stop there permanently
Because only corals grow there
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They change sound speed in water
They change ridges into trenches
They erase seafloor age instantly
They stop satellites
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Mid oceanic ridge with a central rift valley
Deep trench in front of an island arc
Marine beach on continental shelf
Delta at river mouth
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New hot crust forms at the ridge and cools away from it
Solar heat accumulates in trenches
No temperature change occurs on shelves
Abyssal plain is always volcanic
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Because fine sediments cover older relief
Because there are no rocks there
Because seawater never erodes the floor
Because all depths are artificial
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Subduction of an oceanic plate
Expansion of continental shelf
Glaciation of abyssal plain
Evaporation of seawater
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It explains relief and tectonic processes from depth patterns
It only tells sweetness of seawater
It is only the art of colouring maps
It only gives coastline length
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Small seamounts or trenches may be missed
Sea surface will disappear
All measurements will be completely true
Continent will turn into ocean
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Subduction and steep slopes may drag or destabilize sediments
Trenches are outside the ocean
Trenches have no gravity
Trenches have no water
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Upwelling of material from mantle and formation of new crust
Only breaking of surface waves
Rivers bringing sand
Reduction of atmospheric pressure
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Bottom relief can control or deflect deep water pathways
Bottom relief stops wind
Mapping removes salinity
Ridges create rainfall
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A submarine route carrying sediment to deep sea
Permanent glacial plain
Tidal island on sea surface
Atmospheric pressure belt
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Convergent plate boundary and subduction
Divergent plate boundary and new crust
Passive margin and thick shelf
Flat abyssal plain and sediment
Question 1ExpertLevel 1
If a seafloor map shows rock age increasing on both sides away from a mid oceanic ridge what is the most accurate interpretation?
Correct answer: A
Symmetrical age pattern is strong evidence of seafloor spreading. Exam tip: read distance from ridge with crustal age.
On a bathymetric map if isobaths are widely spaced on a ridge top but closely spaced on its flank what does it mean?
Correct answer: A
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.
If a submerged mountain has a flat top and deep floor around it what does it indicate about its earlier stage?
Correct answer: A
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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