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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 2
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  1. Ridge magnetic stripes on both sides age pattern and heat flow
  2. Coastline weather and rainfall
  3. River valley plain and desert
  4. Sea colour clouds and wind
Expert · Level 2
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  1. It was discontinuous slow and less accurate in deep complex areas
  2. It instantly changed the seafloor
  3. It was faster than satellites
  4. It measured magnetic stripes
Expert · Level 2
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  1. Oceanic crust is continuously formed and destroyed by subduction
  2. Oceanic crust has no rocks
  3. Continental crust forms in the sea
  4. Seawater stops age dating
Expert · Level 2
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  1. They may be abyssal hills and the floor is not completely smooth
  2. They are only surface waves
  3. They are continental glaciers
  4. They are coastal sand dunes
Expert · Level 2
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  1. Plate movement over a hotspot
  2. Seawater becoming static
  3. Sudden disappearance of shelf
  4. Trench becoming flat
Expert · Level 2
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  1. Explanation of the mechanism of continental movement
  2. Existence of fossils
  3. Existence of coastlines
  4. Cause of rainy season
Expert · Level 2
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  1. Closely spaced depth lines appear suddenly after the shelf
  2. All lines disappear near the coast
  3. Lines are circular in abyssal plain
  4. Lines change colour on a ridge
Expert · Level 2
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  1. It is a complex region with ridges trenches seamounts abyssal plains and sedimentary areas
  2. It is only a uniform flat plain
  3. It is only an extension of continental shelf
  4. It is an unmappable empty space
Expert · Level 2
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  1. Features will show correct depth but at wrong locations
  2. Depth will always become zero
  3. Seafloor will disappear
  4. The map subject will become history
Expert · Level 2
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  1. Submarine landslide
  2. Continental avalanche
  3. Coastal desertification
  4. Marine rainbow
Expert · Level 2
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  1. Recently formed new oceanic crust
  2. Very old passive continental margin
  3. Stable delta plain
  4. Old continental slope
Expert · Level 2
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  1. Young crust at ridges and destruction of old crust at trenches
  2. Crust of identical age everywhere
  3. Absence of depth lines
  4. Straight coastline
Expert · Level 2
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  1. Resource exploration and safe navigation
  2. Himalayan formation and stopping monsoon
  3. Eclipse calculation and star mapping
  4. Desert expansion and deforestation
Expert · Level 2
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  1. When map scale is too small and depth differences are generalized
  2. When map has a north arrow
  3. When colours are clear
  4. When depth unit is written
Expert · Level 2
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  1. Melting related to the subducted plate and rise of magma
  2. Evaporation at the sea surface
  3. Deposition of sand on shelf
  4. Quiet sediment on abyssal plain
Expert · Level 2
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  1. Seamount
  2. Deep trench
  3. Flat shelf
  4. Submarine canyon
Expert · Level 2
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  1. Calling it merely a quiet sedimentary plain
  2. Considering it a possible subduction zone
  3. Linking it with an active plate boundary
  4. Examining it as an oceanic trench
Expert · Level 2
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  1. Wrong colour intervals can understate or exaggerate slopes and depth differences
  2. Colour changes the seafloor
  3. Colour removes magnetism
  4. Colour stops plate motion
Expert · Level 2
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  1. To link depth measurements with correct geographic location
  2. To measure taste of seawater
  3. To cool magma
  4. To count marine organisms
Expert · Level 2
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  1. Seamount
  2. Continental rise
  3. Ocean trench
  4. Isobath
Expert · Level 2
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  1. Continental rise
  2. Mid oceanic ridge
  3. Deep oceanic trench
  4. Volcanic island arc
Expert · Level 2
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  1. Cables may be damaged by slopes landslides trenches or highs
  2. Cable will dry the ocean
  3. Cable will change latitude
  4. Cable will move into the atmosphere
Expert · Level 2
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  1. When confirming the rock type and age of a seafloor high
  2. When making only a weather forecast
  3. When counting surface waves
  4. When knowing coastal population
Expert · Level 2
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  1. It helps understand landslide zones trenches seismic zones and tsunami sources
  2. It completely stops earthquakes
  3. It makes the ocean a stable solid
  4. It ends rainfall
Expert · Level 2
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  1. Integrating depth form age sediment magnetism and plate context
  2. Concluding only from colour
  3. Understanding the floor only from coastline
  4. Keeping the map separate from geology

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