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State Board · Class 8 · Geography

Lesson 4: Structure of Ocean Floor

5 concepts · 40 practice questions with answers · Free to read

This lesson is also in: मराठी

Ocean floor and mean sea level

From daily life

When the tide goes out at the beach, you can walk on sand that was under water a few hours ago. That shows land continues below the sea. The sea floor has hills, plains and deep valleys, just like land.

Simple definition

The ocean floor (समुद्रतळ) is the land under ocean water; its relief is decided by depth from sea level and the shape of the land.

Rule 1: Ocean floor and mean sea level — About 71% of the Earth is water, and the average depth of the oceans is about 3700 m. The ocean bed is uneven, with hills, plateaus, trenches and plains. Mean sea level is the average of the highest high tides and lowest low tides, taken as zero: heights are positive and depths negative. Mount Everest +8848 m; Mariana Trench −11034 m; vertical gap = 8848 + 11034 = 19,882 m. For survey in India the sea level at Chennai is zero.

mean sea level = 0Mount Everest+8848 mMariana Trench−11034 m

In the figure : In the figure the mean sea level is taken as zero: heights are positive and depths are negative (Mount Everest +8848 m, Mariana Trench −11034 m).

  • Easy : Easy: Sea level is zero.
  • Medium : Medium: 8848 + 11034 = 19,882 m between the peak and the trench.
  • Exam-type : Exam: Why is depth written negative?
waterland71% water29% landeach square = 1%

In the figure : In the figure about 71% of the surface of the earth is covered with water and about 29% is land; the average depth of the oceans is about 3700 m.

  • Easy : Easy: Water is 71%.
  • Medium : Medium: Land = 100 − 71 = 29%.
  • Exam-type : Exam: What is the average ocean depth?

Rule 2: A young floor — Ocean-floor rocks are not older than 200 million years, but continental rocks can be 3200 million years old, 3200 ÷ 200 = 16 times older. So the ocean floor is very young; this research led to plate tectonics. Order from the coast: continental shelf → continental slope → abyssal plains (with submerged mountains and plateaus) → deeps and trenches.

Oldest rocks (million years)Ocean floor200Continents3200

In the figure : In the figure the rocks of the ocean floor are not older than about 200 million years, but continental rocks can be up to 3200 million years old, so the ocean floor is young.

Live figure

Ocean floor and mean sea level

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  • Easy : Easy: Shelf comes first from the coast.
  • Medium : Medium: 4 zones from coast to deep.
  • Exam-type : Exam: Write the order of ocean-floor features.
Remember

71% water. Mean sea level 0. Everest +8848, Mariana −11034. Order: shelf, slope, plain, trench.

Common mistake

Thinking the sea floor is flat. It has hills, plains and trenches.

Shortcut

Memory clue: "मं-उ-मै-ख = मंच, उतार, मैदान, खंदक".

Spot the difference

ItemValue
Water cover71%
Average depth3700 m
Ocean-floor age≤ 200 million years
Continental rock ageUp to 3200 million years

Practice questions

Easy
  1. 1How much of the Earth is water?
  2. 2Average depth of oceans?
  3. 3What is mean sea level?
Medium
  1. 4Which sea level is zero in India?
  2. 5How old is the ocean floor at most?
  3. 6Which research led to plate tectonics?
Challenging
  1. 7A ship is at −500 m and a hill is at +300 m. What is the difference?
  2. 8Why do tides show land under the sea?
Show answers (try them yourself first)
  1. 1About 71%.
  2. 2About 3700 m.
  3. 3Average of high and low tides, taken as zero.
  4. 4Chennai.
  5. 5200 million years.
  6. 6Study of the age of the ocean floor.
  7. 7300 + 500 = 800 m.
  8. 8At low tide the coastal bed is exposed.

Continental shelf and continental slope

From daily life

A swimmer at the beach walks a long way in knee-deep water, then suddenly the bottom drops away. That knee-deep stretch is the shelf and the drop is the slope.

Simple definition

The continental shelf (खंडीय मंच) is the shallow, gently sloping submerged coastland; the continental slope (खंडीय उतार) is the steeper part beyond it.

Rule 1: Continental shelf — The land near the coast submerged under the sea; the shallowest part with a gentle slope; depth up to 200 m. Its width varies, narrow in some places and hundreds of km in others. It is very important: sunlight reaches the bed, so algae and plankton grow and extensive fishing grounds form. It gives natural gas, mineral oil and minerals, e.g. Mumbai High in the Arabian Sea.

ContinentalshelfContinentalslopeAbyssal plainMarine islandSubmarineplateauTrenchsea levelnot to scale

In the figure : In the figure from the coast towards the deep sea: continental shelf, continental slope, abyssal plain (with submerged hills, islands and plateaus) and trenches.

  • Easy : Easy: The shelf is the shallowest.
  • Medium : Medium: Shelf depth 200 m is only about 5% of the 3700 m average (200 ÷ 3700 × 100 ≈ 5.4%).
  • Exam-type : Exam: Why are fish plentiful on the shelf?

Rule 2: Continental slope — After the shelf ends, the bed becomes steeper. Depth is from 200 m to 3600 m, a span of 3600 − 200 = 3400 m. It is narrow. Its lower boundary is taken as the boundary of the continents.

ShelfSlopeDepthup to200 m200 m to3600 mSteepnessgentlesteeperWidthnarrow orbroadnarrowKnown forfishing, oiland gasboundary ofcontinents

In the figure : In the figure shelf: up to 200 m deep with a gentle slope. Slope: 200 m to 3600 m deep, steeper and narrow; its lower boundary is the boundary of the continents.

  • Easy : Easy: Slope depth is 200 to 3600 m.
  • Medium : Medium: Steeper than the shelf.
  • Exam-type : Exam: Compare shelf and slope.
Continentalshelfnot to scale

In the figure : In the figure on the shallow continental shelf sunlight reaches the bed, so plankton grows and fish feed on it; the shelf also gives natural gas, mineral oil (Mumbai High) and minerals.

  • Easy : Easy: Mumbai High gives oil.
  • Medium : Medium: Sunlight → plankton → fish.
  • Exam-type : Exam: List two benefits of the shelf.
Remember

Shelf: up to 200 m, gentle, fish, oil. Slope: 200–3600 m, steep; boundary of continents.

Common mistake

Mixing shelf and slope. Shelf is shallow and gentle; slope is steep.

Shortcut

Memory clue: "मंच = मासे + तेल; उतार = सीमा".

Spot the difference

FeatureShelfSlope
DepthUp to 200 m200–3600 m
GradientGentleSteep
UseFishing, oilEdge of continents

Practice questions

Easy
  1. 1What is the continental shelf?
  2. 2Its depth?
  3. 3Why is it good for fishing?
Medium
  1. 4Name an oil field on a shelf.
  2. 5Depth of the continental slope?
  3. 6What is the lower boundary of the slope taken as?
Challenging
  1. 7A slope goes from 200 m to 3000 m. How deep is it in total?
  2. 8Why must we protect the shelf from pollution?
Show answers (try them yourself first)
  1. 1Submerged coastland near the shore.
  2. 2Up to 200 m.
  3. 3Sunlight reaches the bed and plankton grows.
  4. 4Mumbai High.
  5. 5200 m to 3600 m.
  6. 6The boundary of the continents.
  7. 73000 − 200 = 2800 m.
  8. 8It is rich in fish and resources.

Abyssal plains, submerged mountains, islands and plateaus

From daily life

Under a calm lake, there may be a hidden hill whose top peeps out as a small island. The ocean has the same, only huge.

Simple definition

Abyssal plains (अथांग मैदाने) are the flat ocean bed beyond the slope, with submerged hills, mountains and plateaus; peaks above the sea are marine islands.

Rule 1: Plains, ridges, islands — The abyssal plain is flat with submerged hills and plateaus. Submerged mountains are hundreds of km wide and thousands of km long: the Mid-Atlantic Ridge is the longest continuous range, up to 65,000 km (about 1.6 times the Earth's circumference of nearly 40,000 km). Peaks that rise above the sea are marine islands: Iceland (Atlantic), Andaman and Nicobar (Bay of Bengal). Flat, wide summits are submarine plateaus: the Chagos Plateau (Indian Ocean).

sea levelMarineisland(Iceland)Submarineplateau(Chagos)Submergedhill belowthe seaSubmerged hills and mountainsnot to scale

In the figure : In the figure peaks of submerged hills that rise above the sea are marine islands (Iceland); flat and extensive summits are submarine plateaus (Chagos Plateau).

  • Easy : Easy: Iceland is a marine island.
  • Medium : Medium: Chagos is a plateau, not an island.
  • Exam-type : Exam: How are marine islands formed?
LandformExampleWhereMarineislandIcelandAtlanticOceanMarineislandAndaman andNicobarBay ofBengalSubmarineplateauChagosPlateauIndianOceanTrenchMarianaTrenchPacificOcean

In the figure : In the figure examples: Iceland (Atlantic Ocean), Andaman and Nicobar Islands (Bay of Bengal), Chagos Plateau (Indian Ocean), Mariana Trench (Pacific Ocean).

  • Easy : Easy: Andaman is in the Bay of Bengal.
  • Medium : Medium: Four examples in four oceans or seas.
  • Exam-type : Exam: Name the longest submerged range.
Remember

Plain, ridge, island, plateau. Mid-Atlantic Ridge up to 65,000 km.

Common mistake

Thinking all islands are made by volcanoes only. Many are peaks of submerged mountains.

Shortcut

Memory clue: "शिखर वर = बेट; माथा सपाट = पठार".

Spot the difference

LandformExample
Marine islandIceland
Marine islandAndaman and Nicobar
Submarine plateauChagos
Longest rangeMid-Atlantic Ridge

Practice questions

Easy
  1. 1What is an abyssal plain?
  2. 2What landforms are on it?
  3. 3Which is the longest submerged range?
Medium
  1. 4What is a marine island?
  2. 5Name two marine islands.
  3. 6Which plateau is in the Indian Ocean?
Challenging
  1. 7A ridge is 65,000 km. How many times does it span 13,000 km?
  2. 8Why is a plateau called flat-topped?
Show answers (try them yourself first)
  1. 1The flat ocean bed beyond the slope.
  2. 2Submerged hills and plateaus.
  3. 3Mid-Atlantic Ridge.
  4. 4A submerged hill's peak above sea level.
  5. 5Iceland and the Andaman Islands.
  6. 6Chagos.
  7. 765,000 ÷ 13,000 = 5.
  8. 8Its summit is wide and level.

Marine deeps and trenches

From daily life

A crack in the road is a small gap; a canyon is a huge one. On the sea floor, narrow and deep gaps are called trenches, and the earth there is restless.

Simple definition

Marine deeps and trenches (महाखोलगटे व खंदक) are deep, narrow, steep landforms; the Mariana Trench is the deepest.

Rule 1: Trenches — Shallower ones are deeps; deeper ones extending far are trenches, thousands of metres deep. The Mariana Trench in the Pacific is about 11,034 m deep; even Mount Everest (8848 m) would be submerged with 11034 − 8848 = 2186 m of water above its peak.

Mount Everest: height 8848 mMariana Trench: depth 11034 msea levelMount EverestMariana TrenchEverest placed in the trench · not to scale

In the figure : In the figure Mount Everest (8848 m) would be completely submerged in the Mariana Trench (about 11,034 m deep), the deepest trench of the world, in the Pacific Ocean.

  • Easy : Easy: Mariana is the deepest.
  • Medium : Medium: 11034 − 8848 = 2186 m above Everest's peak.
  • Exam-type : Exam: Where is the Mariana Trench?

Rule 2: Active zones — Mid-oceanic ridges and trenches are the geologically most active parts of the sea bed: many active volcanoes and earthquakes. Quakes and eruptions there cause tsunamis on nearby coasts. At trenches the oceanic plate sinks and melts; away from ridges rocks get older. This is why the ocean floor is young.

Mid-oceanic ridgeOlder rocksPlate sinksand meltsolderMantlelandnot to scale

In the figure : In the figure new rock forms at the mid-oceanic ridges and becomes older away from them; at the trenches the oceanic plate sinks and melts, so the ocean floor is young.

  • Easy : Easy: New rock forms at ridges.
  • Medium : Medium: Rock is oldest far from ridges.
  • Exam-type : Exam: Why is the ocean floor young?
Ridges and trenches aregeologically active1Earthquakes and eruptionsoccur on the ocean bed2Tsunamis are producedin the sea3Nearby coastal areasare hit by the waves4

In the figure : In the figure ridges and trenches are geologically active (volcanoes, earthquakes); their eruptions and quakes produce tsunamis in the nearby coastal areas.

  • Easy : Easy: Quakes cause tsunamis.
  • Medium : Medium: Coasts near trenches are at risk.
  • Exam-type : Exam: Name two active features.
Remember

Mariana −11034 m. Ridges and trenches: volcanoes, quakes, tsunamis.

Common mistake

Thinking the deep sea is calm. Ridges and trenches are the most active.

Shortcut

Memory clue: "रांग बनवते, खंदक गिळतो".

Spot the difference

FeatureWhat happens
Mid-oceanic ridgeNew rock forms
TrenchPlate sinks and melts
BothVolcanoes, quakes, tsunamis

Practice questions

Easy
  1. 1What is a trench?
  2. 2Which is the deepest trench?
  3. 3In which ocean?
Medium
  1. 4How deep is it?
  2. 5What do quakes on the sea bed cause?
  3. 6Where does new ocean rock form?
Challenging
  1. 7A trench is 10,000 m deep and a mountain is 8000 m high. How much water covers the peak if the mountain stands in it?
  2. 8Why do rocks get older away from ridges?
Show answers (try them yourself first)
  1. 1A deep, narrow, steep valley on the ocean bed.
  2. 2Mariana Trench.
  3. 3Pacific.
  4. 4About 11,034 m.
  5. 5Tsunamis.
  6. 6At mid-oceanic ridges.
  7. 710,000 − 8,000 = 2,000 m.
  8. 8New rock forms at ridges and moves outward.

Marine deposits

From daily life

The beach after a festival holds coconut shells, plastic bottles and flowers. Flowers rot soon, but the bottles stay for years. The sea floor collects such things too.

Simple definition

Marine deposits (सागरी निक्षेप) are materials that settle on the sea bed: from continents, from volcanoes and living things, and from humans.

Rule 1: Natural deposits — (1) From the continents: pebbles, clay and soil brought by rivers and glaciers settle mainly on the continental shelf; the Ganga's sediments are seen up to about 2000 km into the sea. (2) Volcanic and organic: lava, ash, fine soil, remains of marine plants and animals. Fine clay with 30% or more remains of sea organisms is marine ooze, found in the deep sea away from the coast (in a 500 g sample, 30% = 150 g). Layers pressed by sea water form sedimentary rocks. These deposits tell us about marine life and minerals.

From thecontinentsVolcanicash and lavaRemains ofmarine lifeHuman-induced

In the figure : In the figure deposits: from the continents (pebbles, clay and soil brought by rivers and glaciers), volcanic and organic (ash, lava and remains of marine life; marine ooze has 30% or more) and human-induced (sewage, plastics, waste).

  • Easy : Easy: Rivers bring soil to the sea.
  • Medium : Medium: Ooze needs at least 30% sea-life remains.
  • Exam-type : Exam: What is marine ooze?

Rule 2: Human-induced deposits — Sewage, solid waste, radioactive material, waste chemicals and plastics are hazardous to the hydrosphere and extremely harmful to marine life; though small in quantity, their nuisance value is high. Seas have higher biodiversity than land, so we must not dump waste in them. Plants and dead animals are perishable; plastics, glass and metals are non-perishable and stay long. We should run coast-cleaning campaigns.

plantsperishabledead animalsperishableplasticnon-perishablemetalnon-perishableglassnon-perishable

In the figure : In the figure plants and dead animals are perishable; plastics, glass and metals are non-perishable and stay for a long time, so we must not dump waste in the sea.

  • Easy : Easy: Plastic is non-perishable.
  • Medium : Medium: A flower rots in days; a bottle lasts years.
  • Exam-type : Exam: Why not dump waste in the sea?
Remember

Deposits: continental, volcanic and organic, human-induced. Ooze ≥ 30%. Plastic stays long.

Common mistake

Thinking the sea can absorb any waste. Non-perishable waste harms marine life.

Shortcut

Memory clue: "खंड - ज्वाला/जीव - माणूस" = तीन निक्षेप.

Spot the difference

DepositExamples
From continentsPebbles, clay, soil
Volcanic and organicLava, ash, ooze
Human-inducedSewage, plastics, waste

Practice questions

Easy
  1. 1Name the three kinds of marine deposits.
  2. 2Where do river sediments settle mainly?
  3. 3What is marine ooze?
Medium
  1. 4Where is ooze found?
  2. 5Give two human-induced deposits.
  3. 6Which wastes are non-perishable?
Challenging
  1. 7A 800 g sample has 40% organic remains. How many grams?
  2. 8How can students help keep coasts clean?
Show answers (try them yourself first)
  1. 1From continents, volcanic and organic, human-induced.
  2. 2On the continental shelf.
  3. 3Fine clay with 30% or more remains of sea organisms.
  4. 4In the deep sea away from the coast.
  5. 5Plastics and sewage.
  6. 6Plastics, glass and metals.
  7. 7800 × 40 ÷ 100 = 320 g.
  8. 8Join cleaning campaigns and not litter.

Quick revision

  • 71% of the earth is water. Average ocean depth ≈ 3700 m. Mean sea level = 0. Everest +8848 m, Mariana −11034 m. Chennai = zero for survey in India.
  • Shelf (up to 200 m, gentle, fishing, Mumbai High) → slope (200–3600 m, steep, boundary of continents) → abyssal plain → deeps and trenches.
  • Marine islands = peaks of submerged mountains (Iceland, Andaman and Nicobar). Plateau = flat summit (Chagos). Mid-Atlantic Ridge ≈ 65,000 km.
  • Mariana Trench (Pacific) is the deepest. Ridges and trenches have volcanoes, earthquakes and tsunamis.
  • Deposits: from rivers and glaciers, volcanic and organic (ooze ≈ 30%), human-induced.