Ch 2 Shaping Of The Earth’s Surface Notes Class 9| Understanding Society India And Beyond

Ch 2 Shaping Of The Earth’s Surface Notes Class 9 is created after multiple readings and consultations with our students.

We have created the short notes from Chapter 2 Shaping of the Earth’s Surface NCERT Class 9 Understanding Society: India and Beyond.

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Also Read| Ch 1 Understanding Social Science Notes Class 9 Social Science

Ch 2 Shaping Of The Earth’s Surface Notes Class 9

Earth’s surface is changing due to :
Internal
and External forces

Plate Tectonics
Explains movement of large crustal plains over mantle
This movement creates different landforms.

Importance of Plate Tectonics:
Explains :
Earthquakes

Volcanic eruptions
Formation of continents and oceans.

A mobile-friendly 3D infographic diagram titled "The Earth's Interior" on a white background. It features two detailed illustrations: on the left, a full cross-section of the Earth displaying its inner layers, and on the right, a vertical wedge specifying depths for the Crust, Lithosphere, Asthenosphere, Mantle |Ch 2 Shaping Of The Earth's Surface Notes Class 9
The Earth’s interior|Ch 2 Shaping Of The Earth’s Surface Notes Class 9


Plate tectonics is when giant pieces of Earth’s crust move and collide.

Plate Tectonics Theory
By W. J. Morgan
Explain- movement of the Earth’s crust.

How It Works
Earth’s outer layer is divided into tectonic plates.
These plates move slowly over the semi-molten mantle.

What It Creates
Mountains
Earthquakes
Volcanoes

What are the Layers of the Earth?

LayerFeature
CrustOutermost layer. We live on it.
MantleBelow the crust. Very thick and hot.
CoreInnermost layer. Extremely hot and heavy.

Lithosphere = Crust + upper part of mantle.
Lithosphere broken into tectonic plates.
Asthenosphere lies below the lithosphere, semi-molten and it lets plates move.

A cross-section diagram of the Earth's interior showing its layers (Crust, Upper Mantle, Lower Mantle, Outer Core, and Inner Core) with circular arrows illustrating heat transport mechanisms like convection currents and interior heat flow.

Massive slabs of solid rock.
Move very slowly– few centimeters per year.

Types of Tectonic Plates
Continental plates: carry continents.
Oceanic plates: carry ocean floors.
Mixed plates: carry both continents and oceans.

Major Tectonic Plates of the World

1. Pacific Plate
2. Eurasian Plate
3. African Plate

4. North American Plate
5. South American Plate
6.Indo-Australian Plate
7.Antarctic Plate

A world map illustrating the Earth's major tectonic plates in different colors, with arrows indicating their respective directions of movement and boundaries.
movement of plates

What are Plate Boundaries?
= Edge where tectonic plates meet.
Three main types.

1. Convergent Boundary
Two plates move towards each other.
Continental + Continental collision → forms fold mountains (e.g., Himalaya).
Oceanic + Continental collision → oceanic plate sinks beneath continental plate → causes volcanic activity and earthquakes.

2. Divergent Boundary
Plates move away from each other.
Magma rises from below. Forms new crust.
Creates features like mid-ocean ridges.
Example: Mid-Atlantic Ridge.

3. Transform Boundary
Plates slide past each other.
No crust is created or destroyed.
Mainly causes earthquakes.
Example: San Andreas Fault, United States.

Convergent Boundary Divergent Boundary Transform Boundary |Class 9 Ch 2 Shaping Of The Earth's Surface Notes Class 9
Convergent Boundary Divergent Boundary Transform Boundary |Class 9 Ch 2 Shaping Of The Earth’s Surface Notes Class 9

Impact on the Earth’s Surface
Shapes the Earth’s surface.
Forms:
Mountains, Valleys, Ocean basins. Volcanoes. Earthquakes
Explains– distribution of continents and oceans.
Most earthquakes and volcanoes occur along plate boundaries.

Ring of Fire
Surrounds the Pacific Ocean.
Highest concentration of earthquakes and volcanoes.

A world map illustrating the global distribution of active volcanoes and earthquake origins, highlighting major concentrations along tectonic plate boundaries such as the Pacific Ring of Fire.

Weathering breaks down rocks. Erosion moves the broken material. Together they shape mountains, valleys, plains, caves, cliffs, and river deltas.

Weathering is the process by which rocks break down into smaller pieces on the Earth’s surface.

How It Happens
Breaks rocks into smaller fragments.
Only breaking down occurs, not transportation.

Importance of Weathering
Helps shape the Earth’s surface.
Role in soil formation.

Common Confusion:
Weathering breaks rocks in place.
Erosion moves the broken pieces away. Don’t mix the two

1. Physical Weathering
Rocks break into smaller pieces.
Caused by temperature changes, frost, or wind.

2. Chemical Weathering
Minerals in rocks change.
Caused by reactions with water, air, or acids.
Leads to the formation of new substances.

3. Biological Weathering
Caused by plants, animals, or micro-organisms.
Example: plant roots grow into cracks in rocks and split them apart.

Erosion is the process by which soil, rocks, and other surface materials are worn away and transported from one place to another.

Agents of Erosion
Erosion is caused by:
Water Wind
Ice Waves

How Erosion Differs from Weathering
Weathering only breaks down rocks.
Erosion breaks down and transports the material.

Importance of Erosion
Shapes landforms.
Create and destroy features on the Earth’s surface.

Water erosion:
caused by rivers, rain, or ocean waves.

Wind erosion:
common in dry and sandy areas.

Glacial erosion:
moving ice scrapes and carries rocks.

Coastal erosion:
sea waves wear away land along the shore.

1. Impact on Farming
Removes fertile topsoil.
Reduces crop yields.

2. Impact on Settlements
Washes away land, houses, and roads.
Causes property damage.

3. Impact on Construction and Mining
Makes the land unstable.
Increases safety risks.

4. Impact on Tourism and Fishing
Damages beaches, rivers, and fertile land.
Affects tourism and fishing livelihoods.

An educational infographic illustrating landforms created by flowing water, featuring side-by-side diagrams and real-world photos of a waterfall, a river meander with an oxbow lake, and a river delta (including the Sundarbans).

Agents of gradation = natural forces that wear down, transport, and deposit materials on Earth’s surface.
They level or smooth the surface over time.

Main Agents of Gradation

AgentWork Done
Running waterErodes rocks and soils. Forms valleys and plains.
GlaciersScrape and carry material. Carve U-shaped valleys.
WindShapes deserts by eroding and depositing sand.
Sea wavesErode coastlines. Form cliffs, beaches, bays.
GroundwaterDissolves rocks like limestone. Creates caves and sinkholes.

Rivers shape land through erosion, transportation, and deposition.

River Course Stages

CourseFeatures |Landforms
Formed
Reason
Upper courseV-shaped valleys, waterfalls, rapidsSteep gradient, strong erosion
Middle courseMeanders, oxbow lakes, floodplainsRiver loses energy, deposits sediments
Lower courseDeltas, levees, alluvial fansThe river slows, deposits large sediment

These landforms are important for :
Agriculture, Settlement, and Ecosystems
.

A waterfall = landform ↦ river flows over a steep cliff or vertical drop
Forms in the upper course of rivers.
Hard rocks resist erosion. Softer rocks below get worn away. This creates a sudden drop.

Importance of Waterfalls
Attract tourists.
Hydroelectric power generation.
Recreation — trekking, photography.
Cultural or religious significance in certain regions.


A meander is a winding curve or bend in the middle or lower course of a river.
The river erodes the outer banks of bends.
The river deposits sediment on the inner banks.
This gradually creates large loops.

Importance of Meanders

Fertile soil deposited along banks supports agriculture.
Influence settlement patterns — villages/towns develop on gentle slopes near meanders.
Used for navigation, irrigation, and sometimes tourism.

Example:
Grand Anicut (also called Kallanai), Tamil Nadu — example of rivers used for irrigation.

A delta is a landform formed at the mouth of a river, where it flows into a sea, ocean, or lake.
Rivers deposit sediments carried from upstream.
Over time, deposits form a fan-shaped or triangular area of land.

Importance of Deltas
Highly fertile due to rich alluvial soil. Good for agriculture (rice, jute).
Fishing — fresh + saltwater = diverse aquatic life.
Dense human settlements.
Trade and transportation
Risk: prone to flooding

Waves and currents reshape coastal land. They create beaches, sand bars, sea cliffs, caves, arches, and stacks.

An educational infographic illustrating coastal and glacial landforms, featuring side-by-side diagrams and real-world photos of beaches, sea arches, sea cliffs, U-shaped valleys, and moraines.

Landform made up of sand, pebbles, or rocks along the shoreline.

Created by deposition of sediments by waves.
Shaped continuously by wave action, tides, and currents.

Importance of Beaches
Tourist destinations
Boosts local economy.
Fishing areas.
People collect sand and shells.
Natural barriers against strong waves and coastal erosion.

Occurs when waves, tides, and currents wear away land along the coast.
Creates unique landforms.

Landforms of Coastal Erosion

LandformHow it Forms
CliffsSteep rock faces. Waves undercut the base of the coast.
Wave-cut platformsFlat areas left behind as cliffs retreat.
CavesWaves erode weak parts of rock.
ArchesCaves on opposite sides of headland meet.
StacksIsolated rock pillars after arches collapse.

“Cliff

Platform

Cave

Arch

Stack”
This is the order of formation; one leads to the next.

Moving ice is called a glacier

Occurs when glaciers slowly move over land.
Carves and shapes the landscape.

LandformFeature
U-shaped valleysGlaciers widen and deepen river valleys.
CirquesBowl-shaped depressions at head of glacier.
AretesSharp ridges between valleys.
Hanging valleysWhere smaller glaciers meet larger ones.
FjordsDeep, narrow inlets when sea floods glacial valleys.

Importance to Humans

U-shaped valleys & cirques: Tourist attractions — trekking, skiing, mountaineering.

Fjords: Used for harbors and fishing.

Glacial soil: Supports agriculture in some valleys.

Glaciers: Crucial source of fresh water, feed rivers.

Landforms created by deposition of rocks, soil, and debris (called till).
Formed when a glacier melts and deposits eroded material.

Types of Moraines
Lateral moraines: form along the sides of glaciers.
Terminal moraines: found at the end of glaciers. Mark the furthest advance.
Medial moraines: formed when two glaciers meet. Their lateral moraines join in the middle.

Importance of Moraines
Create fertile soil for agriculture.
Form natural dams and lakes.
Used for water supply, irrigation, sometimes hydroelectric power.

Occurs when strong winds pick up and carry away loose sand and soil particles.
Gradually shapes the landscape.

Landforms of Wind Erosion

An educational infographic illustrating landforms created by wind, featuring diagrams and real-world photos of yardangs, a deflation hollow forming a desert oasis, and various types of sand dunes including barchan, transverse, and star dunes.
LandformFeature
YardangsStreamlined rock ridges carved by wind.
VentifactsRocks polished and shaped by sandblasting.
Deflation hollows / blowoutsShallow depressions where loose material is removed.
Desert pavementsFlat surfaces left after finer particles are blown away.

Importance to Humans
Influence settlement patterns and agriculture in arid regions.
Ventifacts and yardangs attract tourists and geologists.

Dunes are hills or ridges of sand formed by wind.
Found in desert areas or along sandy coasts.

Types of Dunes

Barchan dunes: crescent-shaped. Form with limited sand, a single wind direction.
Longitudinal dunes: long ridges. Parallel to the prevailing wind.
Star dunes: multiple arms. Form where winds come from different directions.
Parabolic dunes: U-shaped. Often stabilised by vegetation.

Importance of Dunes
Natural barriers against desertification and wind erosion.
Tourism and adventure sports.
Protect coastal settlements from strong sea winds and waves.
Sand used for construction purposes.

An educational diagram illustrating landforms created by underground water, featuring a cross-section of a limestone cave with Karst topography features such as stalactites, stalagmites, sinkholes, and underground rivers.

Underground water, especially in limestone or soluble rocks, creates Karst topography.
Formed through chemical weathering and erosion.

LandformFeature
CavesHollow spaces. Acidic water dissolves rock.
StalactitesIcicle-shaped formations hanging from the cave ceiling.
StalagmitesFormations rising from the cave floor.
Sinkholes / dolinesDepressions when ground collapses into underground cavity.
Underground riversFlow-through cave systems.

Importance to Humans

Fresh water.
Tourism opportunities.
Cultural or religious significance .
Stalagmites/stalactites attract geologists and adventurers.

Different landforms can cause disasters. Four common ones are landslides, avalanches, GLOFs, and dust storms.

Natural Causes

Heavy and continuous rainfall — water seeps into soil/rocks. Increases weight. Reduces friction.
Earthquakes and volcanic eruptions — shake ground. Weaken slopes.
Steep slopes with loose or weathered rocks — increase risk.

Human Causes

Deforestation, mining, road construction — disturb slope balance.
Unplanned construction on hillsides.
Poor drainage systems and improper land use — water accumulates. Leads to slope failure.

Sudden instability of snow on steep slopes.
Weak or loosely bonded layers of snow make snowpack unstable.
Sudden temperature rise — causes partial melting. Reduces friction holding snow together.
Strong winds — pile up snow unevenly. Creates fragile layers.

Triggers
Natural: earthquakes and vibrations.
Human: skiing, trekking, construction in mountainous areas.

GLOFs = Glacial Lake Outburst Floods.
Caused by sudden release of large volumes of water from glacial lakes.

Ch 2 Shaping Of The Earth's Surface Notes Class 9An educational infographic diagram detailing the "Formation of a GLOF" (Glacial Lake Outburst Flood) presented in a vertical, step-by-step numbered flowchart from 1 to 7 on a clean white background. Each numbered step on the left features a concise textual explanation paired with a corresponding high-definition, dark-colored 3D-effect landscape illustration on the right, showing the progression from rapid glacier melting and rising water levels to the eventual dramatic collapse of the natural dam and the resulting flood rushing downstream.| Ch 2 Shaping Of The Earth's Surface Notes Class 9
GLOF|Ch 2 Shaping Of The Earth’s Surface Notes Class 9

How GLOFs Happen

Formation of a GLOF
Rising temperatures cause rapid glacier melting.
Glacial lakes grow larger and their water level rises.
The increased water puts pressure on natural dams made of ice or moraines.
Heavy rainfall or snowfall adds more water.
Earthquakes, avalanches, or landslides can weaken or breach the dam.
The dam suddenly collapses.
The stored water rushes downstream, causing a Glacial Lake Outburst Flood (GLOF).

Caused by strong winds lifting large amounts of loose, dry soil and sand into the air.

Contributing Factors

Prolonged drought and low rainfall
Dries out soil. Makes it easy for wind to lift particles.
Desert and semi-arid regions
Soil is loose and dry.
Sparse vegetation cover
Due to deforestation, overgrazing, poor farming practices. Leaves land exposed.
Climate change and extreme weather
Increases frequency and intensity.

DisasterMain TriggerRegion
LandslideRainfall, earthquakes, deforestationSlopes, hills
AvalancheTemperature rise, wind, vibrationsSnow-covered mountains
GLOFGlacier melting, dam collapseGlacial lake areas
Dust StormStrong winds, droughtDesert, semi-arid regions

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19 thoughts on “Ch 2 Shaping Of The Earth’s Surface Notes Class 9| Understanding Society India And Beyond”

  1. The notes are excellent but can you make them a little shorter , while writing in the notebook it takes very much time and pages .

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