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Subjects

Geography

Mapping of the ocean floor

महासागर तल का मानचित्रण

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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Up to 25 questions from this page. Select your focus, then start.

25 questions

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

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