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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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Sound travels to the sea floor and returns
Sound moves only on the water surface
Sound speed is measured in air
Sea floor is always flat
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It is deepest and without light
It is rich in minerals, fisheries and petroleum resources
It is made only of volcanic islands
It is steeper than oceanic trenches
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Very broad and nearly flat part
Shallow part adjoining the coast
Steep zone between shelf and deep-sea plain
Crest of a mid-oceanic ridge
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Continental shelf
Deep-sea plain
Oceanic trench
Mid-oceanic ridge
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Because they are often linked with convergent boundaries and subduction zones
Because they form only in calm seas
Because they occur only in the middle of all oceans
Because they always form on continental shelves
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Formation of high lava cones
Filling of irregular surface by sediments
Cutting of mountains by glaciers
Direct erosion by coastal waves
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Seamount has flat top and guyot is pointed
Both are formed only by rivers
Guyot has a flat top while seamount is generally conical
Guyot occurs only on continental slope
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Isobars
Isotherms
Isohyets
Isobaths
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They showed that the ocean floor has complex relief
They proved all oceans are shallow
They showed ocean water is stationary
They measured only coastal sand
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In front of active plate margins
Near passive continental margins and mouths of large rivers
Only on mid-oceanic ridges
Below all oceanic trenches
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They are cut only by wind
They always form from coral reefs
They indicate deep erosional valleys inside the sea similar to land rivers
They make ocean water fresh
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It gives depth of only one point
It measures atmosphere at light speed
It directly counts fish on the sea floor
It gives depth and shape over a wide swath at once
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The slope is steep
The slope is zero
The water is completely fresh
Depth is same everywhere
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Oceans are stationary pits
New crust forms through sea-floor spreading
Continental shelf is the deepest part
Abyssal plains are always volcanic peaks
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Near continental coasts
On trench floors
Near mid-oceanic ridges
In the farthest parts of abyssal plains
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Crust forms at ridges and is destroyed or subducted at trenches
Crust only rises at both places
Both ridges and trenches are made by continental rivers
New crust forms at trenches and sediments collect at ridges
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Light and nutrients are relatively more available here
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