Skip to content
← Geography

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.

14

Q&A

9

Concepts

~2m

Unit weightage

Start learning — read this chapter →

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.

Start with this concept →

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.

12.2

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.

12.3

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,…

12.3.1

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.

12.3.2

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.

12.3.3

Continental Slope

The continental slope is the steep, transitional zone that links the shallow continental shelf with the deep ocean basins.

12.3.4

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…

12.3.5

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.

12.3.6

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…

12.3.7

Mid-Oceanic Ridges

A mid-oceanic ridge is not a single mountain range but a structure built from two parallel chains of mountains.

12.3.8

Seamount

A seamount is an underwater mountain that rises from the ocean floor but never breaks the surface of the water.

12.3.9

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.

12.3.10

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.

12.3.11

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.

12.4

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.

12.4.1

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…

12.4.2

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.

12.5

Salinity of Ocean Waters

All natural waters — rain water, river water, or ocean water — hold dissolved mineral salts in some quantity.

12.5.1

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.

12.5.2

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

14 Q