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PHYSICAL FEATURES OF
INDIA
 CLASS IX – SOCIAL SCIENCE
 GEOGRAPHY – CHAPTER 2
 (BY: MRS USHA JOY)
PHYSICAL FEATURES OF INDIA
 The land of India displays great physical variation.
 The Peninsular Plateau constitutes one of the ancient landmasses on
the earth’s surface.
 The Himalayas and the Northern Plains are the most recent
landforms.
GONDWANA LAND
PHYSICAL FEATURES OF INDIA
 MAJOR PHYSIOGRAPHIC DIVISIONS
 (1) The Himalayan Mountains
 (2) The Northern Plains
 (3) The Peninsular Plateau
 (4) The Indian Desert
 (5) The Coastal Plains
 (6) The Islands
Physical Map of India
The Himalayan Mountains
 The Himalayas are young and structurally fold mountains.
 They run in a west-east direction from the Indus to the Brahmaputra.
 The loftiest and one of the most rugged mountain barriers of the
 Its length is about 2,400 Km and width varies from 400 Km in
150 Km in Arunachal Pradesh.
 The Himalayas consist of three parallel ranges in its longitudinal
The Himalayas-Longitudinal divisions
 The Great or Inner Himalayas or the Himadri.
 Himachal or lesser Himalaya.
 Outer Himalayas or the Shiwaliks
The Himalayas
The Himalayas
The Great Himalayas
 The Great or Inner Himalayas or the Himadri.
 It is the most continuous range consisting of the loftiest
peaks with an average height of 6,000 metres.
 It contains all prominent Himalayan peaks and the folds are
asymmetrical in nature.
 The core is composed of granite, it is perennially snow
bound and a number of glaciers descend from this range.
Himachal or lesser Himalaya
 It is the most rugged mountain system
 The altitude varies between 3,700 and 4,500 metresand the
average width is of 50 Km.
 The Pir Panjal range, the Dhaula Dhar and the Mahabharat
ranges are the prominent ranges.
 The ranges are highly compressed and altered rocks.
 Famous valleys located here are Kashmir, the Kangra and
KulluValley.
 They are well-known for its hill stations.
The Shiwaliks
 The Shiwaliks extend over a width of 10-50 Km and an
altitude varying between 900 and 1100 metres.
 These are composed of unconsolidated sediments brought
down by rivers.
 They are covered with thick gravel and alluvium.
 The longitudinal valley lying between lesser Himalaya and
the Shiwaliks are known as Duns.
 Dehra Dun, Kotli Dun and Patli Dun are some of the well-
known Duns.
Latitudinal Division of the Himalayas
 These divisions (west to east) are demarcated by river
valleys.
 The part of Himalayas lying between
Indus and Satluj -- Punjab Himalaya
Satluj and Kali rivers-- Kumaon Himalayas
Kali and Teesta rivers-- the Nepal Himalayas.
Teesta and Dihang rivers -- Assam Himalayas
The Purvachals
 The Brahmaputra marks the eastern-most boundary
 Beyond the Dihang gorge, the Himalayas bend sharply to
the south and are known as the Purvachal or the Eastern
hills and mountains.
 These hills are mostly composed of strong sandstones,
which are sedimentary rocks and are covered with dense
forests.
 The Purvachal comprises the Patkai hills, the Naga hills,
the Manipur hills and the Mizo hills.
Gorges
The Northern Plain
• Formed by the interplay of the three major river systems — the Indus,
the Ganga and the Brahmaputra along with their tributaries.
• Formed of alluvial soil - The deposition of alluvium over millions
of years, formed this fertile plain.
• The northern plains have an area of 7 lakh sq. km, about 2400 km long
and 240 to 320 km broad.
• It is a densely populated physiographic division due to rich soil cover
combined with adequate water supply and favourable climate.
The Northern Plains
 In the lower course, the velocity of the river decreases which formation of
riverine islands.
 Majuli in Brahmaputra is the largest inhabited riverine island.
 Due to silt deposition many distributaries are there.
 It is broadly divided into three sec tions, The Punjab Plains ,the Ganga
Plains, the Brahmaputra Plains.
 The Punjab plains are formed by the Indus and its tributaries namely the
Jhelum, the Chenab, the Ravi, the Beas and the Satluj.
 This section of the plain is dominated by the doabs.
 ‘Doab’ is made up of two words ‘do’ meaning two and ‘ab’ meaning water.
Distributaries and Doabs
The Northern Plains
 These vast plains also have diverse relief features.
 Bhabar: deposit pebbles in a narrow belt of about 8 to 16 km, all the
streams disappear in this bhabar belt.
 Terai: the streams and rivers re-emerge and create a wet, swampy and
marshy region. It is a region of thick forest and wildlife, Dudhwa National
Park is located here.
 Bhangar: Formed of older alluvium, lies above the floodplains of the
rivers and presents a terracelike feature. It contains calcareous deposits,
locally known as kankar.
 Khadar: Formed of newer and younger deposits of the floodplains. It is
renewed almost every year and so are fertile.
Relief Features of the Northern Plains
The Peninsular Plateau
 It is a tableland composed of the old crystalline, igneous and
metamorphic rocks.
 It was formed due to the drifting of the Gondwana land.
 Two broad divisions are the Central Highlands and the Deccan Plateau.
 The Central Highland- north of the Narmada river, covering a major area
of the Malwa plateau.
 The Vindhyan range is bounded by the Satpura range in the south, the
Aravalis on the northwest, westward extension gradually merges with the
desert of Rajasthan.
The Peninsular Plateau
 The Sind, the Betwa and the Ken are the rivers draining from southwest
to northeast,
 The eastward extensions are known by Bundelkhand and Baghelkhand.
 The Chotanagpur plateau marks the further eastward extension,
drained by the Damodar river.
India – Physical Features
The Peninsular Plateau
 The Deccan Plateau is a triangular landmass that lies to the south of the
river Narmada.
 The Satpura range in the north, the Mahadev, the Kaimur hills and the
Maikal range in the east.
 Northeast- the Meghalaya, Karbi-Anglong Plateau and in the north
Cachar Hills.
 Three prominent hill ranges are the Garo, the Khasi and the Jaintia Hills.
Western Ghats and Eastern Ghats
Western Ghats
 It marked the western boundary -
from Gujarat to Kerela.
 They are regular stretch of
highland.
 More in height i.e. from 900-
1600m.
 More rainfall- orographic rainfall.
 Highest peaks are Anai Mudi,
followed by Doda Betta
Eastern Ghats
 It marked the eastern boundary
from Orissa to Kerela.
 They are dissected by rivers and
irregular
 less than western ghats ranging
from 600-900m.
 Rainfall is less -the monsoon winds
move parallel to the eastern ghats
 Highest peak of eastern ghats is
Mahendragiri
Peninsular Plateau
 The distinct feature is the black soil area known as
Decean Trap.
 This is of volcanic origin, hence, the rocks are igneous.
 These rocks have denuded over time and are responsible
for the formation of black soil
 Famous hill stations are Udagamandalam, popularly
known as Ooty and the Kodaikanal.
The Indian Desert
• It lies towards the western margins of the Aravali Hills.
• It is an undulating sandy plain covered with sand dunes.
• This region receives very low rainfall below 150 mm per year.
• It has arid climate with low vegetation cover.
• Streams appear during the rainy season.
• Luni is the only large river
• Barchans (crescent-shaped dunes) cover larger areas
Barchans
The Coastal Plains
Western Coastal Plains
 lying towards west between
western ghats and Arabian sea
 belt of plains is narrow in width
 less fertile - no major rivers
 Receive more rainfall
 divided into Konkan Coast,Kannad
Coast and Malabar Coast
Eastern Coastal Plains
 lying towards the east between
eastern ghats and Bay of Bengal
 comparatively wider
 very fertile due to many rivers
 Receive comparatively less rainfall
 divided into Northern Circars and
Coromandal Coast
The Islands
 Lakshadweep Islands
 lying close to the Malabar coast of Kerala. It composed of small coral isalnds.
 Earlier they were known as Laccadive, Minicoy and Amindive.
 In 1973, these were named as Lakshadweep.
 It covers small area of 32 sq km.
 Kavaratti island is the administrative headquarters
 The Pitti island has a bird sanctuary.
Corals
 Coral polyps are short-lived microscopic organisms,
 They live in colonies, They secrete calcium carbonate.
 The coral secretion and their skeletons from coral
deposits in the form of reefs:
 E.g. barrier reef. fringing reef and atolls.
Andaman and Nicobar islands
 Bigger in size and are more numerous and scattered.
 Divided into two broad categories – The Andaman in the north and
the Nicobar in the south.
 These islands are the elevated portion of submarine mountains.
 Great diversity of flora and fauna are there and equatorial climate
and has thick forest cover.
 India’s only active volcano is found on Barren island.
India’s active volcano
Physiographic Divisions
 The mountains - major sources of water and forest wealth.
 The northern plains - the granaries of the country.
 The plateau - storehouse of minerals
 The coastal region and island groups - sites for fishing and port activities
 the diverse physical features of the land have immense future
possibilities of development
Chapter -2: Physical Features of India
Mountain Ranges: The Karakoram, The Zasker,
The Shivalik, The Aravali, The Vindhya, The Satpura,
Western & Eastern Ghats
Mountain Peaks – K2, Kanchan Junga, Anai Mudi
Plateau - Deccan Plateau, Chotta Nagpur
Plateau, Malwa Plateau
Coastal Plains - Konkan,Kannad, Malabar,
Coromandal & Northern Circar (Location and
Labelling)
Map Work

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Physical features of india

  • 1. PHYSICAL FEATURES OF INDIA  CLASS IX – SOCIAL SCIENCE  GEOGRAPHY – CHAPTER 2  (BY: MRS USHA JOY)
  • 2. PHYSICAL FEATURES OF INDIA  The land of India displays great physical variation.  The Peninsular Plateau constitutes one of the ancient landmasses on the earth’s surface.  The Himalayas and the Northern Plains are the most recent landforms.
  • 4. PHYSICAL FEATURES OF INDIA  MAJOR PHYSIOGRAPHIC DIVISIONS  (1) The Himalayan Mountains  (2) The Northern Plains  (3) The Peninsular Plateau  (4) The Indian Desert  (5) The Coastal Plains  (6) The Islands
  • 6. The Himalayan Mountains  The Himalayas are young and structurally fold mountains.  They run in a west-east direction from the Indus to the Brahmaputra.  The loftiest and one of the most rugged mountain barriers of the  Its length is about 2,400 Km and width varies from 400 Km in 150 Km in Arunachal Pradesh.  The Himalayas consist of three parallel ranges in its longitudinal
  • 7. The Himalayas-Longitudinal divisions  The Great or Inner Himalayas or the Himadri.  Himachal or lesser Himalaya.  Outer Himalayas or the Shiwaliks
  • 10. The Great Himalayas  The Great or Inner Himalayas or the Himadri.  It is the most continuous range consisting of the loftiest peaks with an average height of 6,000 metres.  It contains all prominent Himalayan peaks and the folds are asymmetrical in nature.  The core is composed of granite, it is perennially snow bound and a number of glaciers descend from this range.
  • 11. Himachal or lesser Himalaya  It is the most rugged mountain system  The altitude varies between 3,700 and 4,500 metresand the average width is of 50 Km.  The Pir Panjal range, the Dhaula Dhar and the Mahabharat ranges are the prominent ranges.  The ranges are highly compressed and altered rocks.  Famous valleys located here are Kashmir, the Kangra and KulluValley.  They are well-known for its hill stations.
  • 12. The Shiwaliks  The Shiwaliks extend over a width of 10-50 Km and an altitude varying between 900 and 1100 metres.  These are composed of unconsolidated sediments brought down by rivers.  They are covered with thick gravel and alluvium.  The longitudinal valley lying between lesser Himalaya and the Shiwaliks are known as Duns.  Dehra Dun, Kotli Dun and Patli Dun are some of the well- known Duns.
  • 13. Latitudinal Division of the Himalayas  These divisions (west to east) are demarcated by river valleys.  The part of Himalayas lying between Indus and Satluj -- Punjab Himalaya Satluj and Kali rivers-- Kumaon Himalayas Kali and Teesta rivers-- the Nepal Himalayas. Teesta and Dihang rivers -- Assam Himalayas
  • 14. The Purvachals  The Brahmaputra marks the eastern-most boundary  Beyond the Dihang gorge, the Himalayas bend sharply to the south and are known as the Purvachal or the Eastern hills and mountains.  These hills are mostly composed of strong sandstones, which are sedimentary rocks and are covered with dense forests.  The Purvachal comprises the Patkai hills, the Naga hills, the Manipur hills and the Mizo hills.
  • 16. The Northern Plain • Formed by the interplay of the three major river systems — the Indus, the Ganga and the Brahmaputra along with their tributaries. • Formed of alluvial soil - The deposition of alluvium over millions of years, formed this fertile plain. • The northern plains have an area of 7 lakh sq. km, about 2400 km long and 240 to 320 km broad. • It is a densely populated physiographic division due to rich soil cover combined with adequate water supply and favourable climate.
  • 17. The Northern Plains  In the lower course, the velocity of the river decreases which formation of riverine islands.  Majuli in Brahmaputra is the largest inhabited riverine island.  Due to silt deposition many distributaries are there.  It is broadly divided into three sec tions, The Punjab Plains ,the Ganga Plains, the Brahmaputra Plains.  The Punjab plains are formed by the Indus and its tributaries namely the Jhelum, the Chenab, the Ravi, the Beas and the Satluj.  This section of the plain is dominated by the doabs.  ‘Doab’ is made up of two words ‘do’ meaning two and ‘ab’ meaning water.
  • 19. The Northern Plains  These vast plains also have diverse relief features.  Bhabar: deposit pebbles in a narrow belt of about 8 to 16 km, all the streams disappear in this bhabar belt.  Terai: the streams and rivers re-emerge and create a wet, swampy and marshy region. It is a region of thick forest and wildlife, Dudhwa National Park is located here.  Bhangar: Formed of older alluvium, lies above the floodplains of the rivers and presents a terracelike feature. It contains calcareous deposits, locally known as kankar.  Khadar: Formed of newer and younger deposits of the floodplains. It is renewed almost every year and so are fertile.
  • 20. Relief Features of the Northern Plains
  • 21. The Peninsular Plateau  It is a tableland composed of the old crystalline, igneous and metamorphic rocks.  It was formed due to the drifting of the Gondwana land.  Two broad divisions are the Central Highlands and the Deccan Plateau.  The Central Highland- north of the Narmada river, covering a major area of the Malwa plateau.  The Vindhyan range is bounded by the Satpura range in the south, the Aravalis on the northwest, westward extension gradually merges with the desert of Rajasthan.
  • 22. The Peninsular Plateau  The Sind, the Betwa and the Ken are the rivers draining from southwest to northeast,  The eastward extensions are known by Bundelkhand and Baghelkhand.  The Chotanagpur plateau marks the further eastward extension, drained by the Damodar river.
  • 23. India – Physical Features
  • 24. The Peninsular Plateau  The Deccan Plateau is a triangular landmass that lies to the south of the river Narmada.  The Satpura range in the north, the Mahadev, the Kaimur hills and the Maikal range in the east.  Northeast- the Meghalaya, Karbi-Anglong Plateau and in the north Cachar Hills.  Three prominent hill ranges are the Garo, the Khasi and the Jaintia Hills.
  • 25. Western Ghats and Eastern Ghats Western Ghats  It marked the western boundary - from Gujarat to Kerela.  They are regular stretch of highland.  More in height i.e. from 900- 1600m.  More rainfall- orographic rainfall.  Highest peaks are Anai Mudi, followed by Doda Betta Eastern Ghats  It marked the eastern boundary from Orissa to Kerela.  They are dissected by rivers and irregular  less than western ghats ranging from 600-900m.  Rainfall is less -the monsoon winds move parallel to the eastern ghats  Highest peak of eastern ghats is Mahendragiri
  • 26. Peninsular Plateau  The distinct feature is the black soil area known as Decean Trap.  This is of volcanic origin, hence, the rocks are igneous.  These rocks have denuded over time and are responsible for the formation of black soil  Famous hill stations are Udagamandalam, popularly known as Ooty and the Kodaikanal.
  • 27. The Indian Desert • It lies towards the western margins of the Aravali Hills. • It is an undulating sandy plain covered with sand dunes. • This region receives very low rainfall below 150 mm per year. • It has arid climate with low vegetation cover. • Streams appear during the rainy season. • Luni is the only large river • Barchans (crescent-shaped dunes) cover larger areas
  • 29.
  • 30. The Coastal Plains Western Coastal Plains  lying towards west between western ghats and Arabian sea  belt of plains is narrow in width  less fertile - no major rivers  Receive more rainfall  divided into Konkan Coast,Kannad Coast and Malabar Coast Eastern Coastal Plains  lying towards the east between eastern ghats and Bay of Bengal  comparatively wider  very fertile due to many rivers  Receive comparatively less rainfall  divided into Northern Circars and Coromandal Coast
  • 31. The Islands  Lakshadweep Islands  lying close to the Malabar coast of Kerala. It composed of small coral isalnds.  Earlier they were known as Laccadive, Minicoy and Amindive.  In 1973, these were named as Lakshadweep.  It covers small area of 32 sq km.  Kavaratti island is the administrative headquarters  The Pitti island has a bird sanctuary.
  • 32. Corals  Coral polyps are short-lived microscopic organisms,  They live in colonies, They secrete calcium carbonate.  The coral secretion and their skeletons from coral deposits in the form of reefs:  E.g. barrier reef. fringing reef and atolls.
  • 33.
  • 34. Andaman and Nicobar islands  Bigger in size and are more numerous and scattered.  Divided into two broad categories – The Andaman in the north and the Nicobar in the south.  These islands are the elevated portion of submarine mountains.  Great diversity of flora and fauna are there and equatorial climate and has thick forest cover.  India’s only active volcano is found on Barren island.
  • 36. Physiographic Divisions  The mountains - major sources of water and forest wealth.  The northern plains - the granaries of the country.  The plateau - storehouse of minerals  The coastal region and island groups - sites for fishing and port activities  the diverse physical features of the land have immense future possibilities of development
  • 37. Chapter -2: Physical Features of India Mountain Ranges: The Karakoram, The Zasker, The Shivalik, The Aravali, The Vindhya, The Satpura, Western & Eastern Ghats Mountain Peaks – K2, Kanchan Junga, Anai Mudi Plateau - Deccan Plateau, Chotta Nagpur Plateau, Malwa Plateau Coastal Plains - Konkan,Kannad, Malabar, Coromandal & Northern Circar (Location and Labelling) Map Work