Geography · Class 11 Arts
Ch 18Water (Oceans) — Class 11 Geography, concept-first.
Can we think of life without water at all? There is a reason people say water is life — it is an essential component of every life form that exists on the surface of the earth. In this, the creatures of our planet are remarkably fortunate: earth is a water planet, and without that fact, none of us would exist.
Key concepts
Hover a concept to preview it and jump to its most relevant Q&A.
Water Resource Management
Think of water the way you think of your monthly allowance. You get a fixed amount, you have many demands on it, and if you spend carelessly early in the month, you run out before the next one arrives.
Most relevant Q&A
Chapter contents
The NCERT structure, section by section. Open a section to see its questions, then read the concept-first solution.
Introduction
Can we think of life without water at all? There is a reason people say water is life — it is an essential component of every life form that exists on the surface of the earth.
Hydrological Cycle
Water is the most important element for life after air. Every living form on Earth’s surface depends on it, and the planet is fortunate to have it in abundance.
Relief of the Ocean Floor
The ocean floor is not a flat, featureless plain. Just as the continents have mountains, valleys and plains, the land beneath the sea is rugged and varied, holding the world's largest mountain ranges,…
Divisions of the Ocean Floors
The ocean floor is not a flat, featureless plain. It is a vast underwater landscape with its own mountains, valleys, and plains, just like the land above sea level.
Continental Shelf
The continental shelf is the submerged edge of a continent, the part of the landmass that continues under the ocean before dropping away into the deep sea.
Continental Slope
The continental slope is the steep, transitional zone that links the shallow continental shelf with the deep ocean basins.
Deep Sea Plain
Deep sea plains are the vast, flat expanses that make up the floor of the ocean basins. Think of them as the ocean's version of a level, open field — they are the flattest and smoothest regions on the…
Oceanic Deeps or Trenches
The deepest parts of the ocean floor are not the vast abyssal plains but narrow, steep-sided gashes in the earth's crust.
Minor Relief Features
The ocean floor is not just a vast plain of abyssal depths and towering ridges. Beyond the grand, sweeping structures — the continental margins, the mid-oceanic ridges, and the deep-sea plains — lie s…
Mid-Oceanic Ridges
A mid-oceanic ridge is not a single mountain range but a structure built from two parallel chains of mountains.
Seamount
A seamount is an underwater mountain that rises from the ocean floor but never breaks the surface of the water.
Submarine Canyons
Submarine canyons are among the most dramatic features of the ocean floor — deep, steep-sided valleys that in scale rival some of the greatest gorges on land.
Guyots
A guyot is a seamount with a flat top. Think of an underwater mountain that has been levelled off at its summit, like a table rising from the ocean floor.
Atoll
An atoll is a low island found in tropical oceans. The key to understanding it lies in its structure: a ring of coral reef that surrounds a central depression.
Temperature of Ocean Waters
Ocean water, like land, is heated by solar energy — but it heats up and cools down far more slowly than land does.
Factors Affecting Temperature Distribution
The temperature of ocean surface water is not uniform. It changes from place to place, and the factors that cause this variation are the same ones that shape climate on land — latitude, the arrangemen…
Horizontal and Vertical Distribution of Temperature
The ocean is not uniformly cold or warm. Its temperature changes with depth, and it also changes across latitudes.
Salinity of Ocean Waters
All natural waters — rain water, river water, or ocean water — hold dissolved mineral salts in some quantity.
Horizontal Distribution of Salinity
The salinity of normal open ocean water is not uniform — it sits within a fairly narrow band, but local conditions can push it far outside that range.
Vertical Distribution of Salinity
Salinity is not uniform from the surface to the ocean floor. It changes with depth, but the pattern of that change is not the same everywhere — it depends on where you are in the ocean.
More questions
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- Q1Identify the element which is not a part of the hydrological cycle: (a) Evaporation (b) Hydration (c) Precipitation (d) CondensationFree
- Q2The average depth of continental slope varies between: (a) 2-20m (b) 200-2,000m (c) 20-200m (d) 2,000-20,000mFree
- Q3Which one of the following is not a minor relief feature in the oceans: (a) Seamount (b) Atoll (c) Oceanic Deep (d) GuyotPreview
- Q4Salinity is expressed as the amount of salt in grams dissolved in sea water per: (a) 10 gm (b) 1,000 gm (c) 100 gm (d) 10,000 gmPreview
- Q5Which one of the following is the smallest ocean: (a) Indian Ocean (b) Arctic Ocean (c) Atlantic Ocean (d) Pacific OceanPreview
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- Q1Why do we call the earth a Blue Planet?Free
- Q2What is a continental margin?Free
- Q3List out the deepest trenches of various oceans.Preview
- Q4What is a thermocline?Preview
- Q5When you move into the ocean what thermal layers would you encounter? Why the temperature varies with depth?Preview
- Q6What is salinity of sea water?Preview