Muft Shiksha™ एक 100% Free Education Portal है 🇮🇳, जिसका उद्देश्य Class 9–12 के हर विद्यार्थी तक High-Quality Education को पूरी तरह मुफ्त पहुँचाना है। 🇮🇳 हम मानते हैं कि अच्छी शिक्षा किसी student की आर्थिक स्थिति पर निर्भर नहीं होनी चाहिए। 🇮🇳 हर विद्यार्थी को वही Quality Study Material, MCQs, Quizzes, Exam Preparation, Concept-Based Learning और Bilingual Support मिलना चाहिए, जो आमतौर पर महंगी Coaching या Premium Platforms में मिलता है। Muft Shiksha™ 🇮🇳 इसी सोच के साथ बनाया गया है
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
Quiz this set
Up to 25 questions from this page. Select your focus, then start.
25 questions
Choose questions
Hard · Level 5View options
For sea-surface temperature
For imaging texture and objects on the floor
For atmospheric pressure
For coastal population
Hard · Level 5View options
It measures only water salinity
It uses reflected waves from layers to reveal sediments and rock structure
It records fish sounds
It shows cloud height
Hard · Level 5View options
Because tides change sea-surface level
Because tides always erase the sea floor
Because tides stop sound
Because tides occur only in the atmosphere
Hard · Level 5View options
As long linear troughs and ridges
As circular farm fields
As floating icebergs
As coastal towns
Hard · Level 5View options
Because sound speed in water changes with temperature, salinity and pressure
Because sound always travels in vacuum
Because there is no light on the sea floor
Because the ship does not remain stationary
Hard · Level 5View options
Where the shelf begins to change sharply into the continental slope
Where sea water becomes fresh
Where the mid-oceanic ridge ends
Where only coral islands form
Hard · Level 5View options
Transport and deposition of sediments from the slope
Effect of lunar eclipse
Formation of atmospheric ozone
Expansion of a land desert
Hard · Level 5View options
It is a broad elevated area, while the plain is relatively flat and deep
It is always a sandy coastal part
It is only a river delta
It floats above sea level
Hard · Level 5View options
Ordered crust formation and spreading on the sea floor
Rice farming on coasts
Irregularity of air pressure
Complete stability of the sea floor
Hard · Level 5View options
As small irregular rises on deep plains
As sandy strips on continental coasts
Only as waves on sea surface
As river meanders
Hard · Level 5View options
Seamount or dense crustal rise
Flight direction of seabirds
Taste of sea water
Coastal language zone
Hard · Level 5View options
To convert scattered measurements into a regular surface and map
To make the ship invisible
To change ocean colour
To stop waves permanently
Hard · Level 5View options
Ship measures depth directly using sound, satellite estimates indirectly from sea surface and gravity
Satellite lands on the sea floor and cuts rocks
Ship measures only clouds
Both count only coastal population
Hard · Level 5View options
Fracture zones
Continental shelf
Coral lagoon
River delta
Hard · Level 5View options
New floor has had less time for sediment accumulation
Young floor is always covered by fresh water
Sediments form only in land deserts
Old floor never has sediments
Hard · Level 5View options
To show different depths and elevations
To show fish species
To show taste of seawater
To show coastal language
Hard · Level 5View options
Because fine particles can remain suspended in water for a long time
Because they always burn in air
Because they disappear as soon as they form on the sea floor
Because they come only from the Himalayas
Hard · Level 5View options
Submarine rise or seamount
Oceanic trench
Perfectly flat floor
River delta
Hard · Level 5View options
Deep depression or trench-like basin
Summit of a seamount
Continental coast
Flat coral rock
Hard · Level 5View options
Wide shelf and greater sedimentation
Very narrow shelf and many deep trenches
Only mid-oceanic ridge
Absence of sea floor
Hard · Level 5View options
Because slope may be steep and trenches may be near the plate boundary
Because there is no sea water there
Because there is only desert there
Because all sediments immediately go into the sky
Hard · Level 5View options
Because a profile clearly shows slope and changes with distance
Because a profile makes seawater fresh
Because a profile makes a ship fly
Because a profile shows only weather
Hard · Level 5View options
Movement of a plate over a fixed hotspot
River flood
Stopping of tides
Change in coastal sand colour
Hard · Level 5View options
Its top may have been flattened by wave erosion and later submerged
It always forms at a river mouth
It is formed by falling from clouds
It never has volcanic material
Hard · Level 5View options
Risk of damage to undersea cables and pipelines
Pest attack in farms
Urban traffic jam
Desert sandstorm
Question 1HardLevel 5
For which information is side-scan sonar considered more useful in ocean-floor mapping?
Correct answer: B
Side-scan sonar is useful for imaging sea-floor texture and roughness. Exam tip: connect it with floor imaging, not only depth.
Google Analytics helps us understand site usage. Google may send limited cookie-free signals before your choice. The Live Visitors widget operates independently of this analytics choice; see the privacy policy for its provider and fallback details. Essential site features work without analytics cookies. You can change your choice later in Privacy choices. Privacy policy