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Chapter 6_7: Geo6_7_Our Country India
OUR COUNTRY – INDIA
 In the north, it is bound by the lofty Himalayas.
 The Arabian Sea in the west,
 The Bay of Bengal in the east and
 The Indian Ocean in the south, wash the shores of the Indian peninsula.
India has an area of about 3.28 million sq. km.
 The north-south extent from Kashmir to Kanyakumari is about 3,200 km.
 And the east-west extent from Arunachal Pradesh to Kuchchh is about 2,900 km
LOCATIONAL SETTING
 India is located in the northern hemisphere.
 The Tropic of Cancer (23°30 ' N) passes almost halfway through the country
 From south to north, India extends between 8°4' N and37°6' N latitudes. From west to
east, India extends between 68°7 ' E and97°25 'E longitudes
 The local time changes by four minutes for every one degree of longitude.
 The sun rises two hours earlier in the east (Arunachal Pradesh) than in the west
(Gujarat).
 The local time of longitude of 82°30' E has been taken as the Indian Standard Time.
This meridian or longitude is also termed as the Standard Meridian of India
INDIA’S NEIGHBOURS
 There are seven countries that share land boundaries with India.
POLITICAL AND ADMINISTRATIVE DIVISIONS
 Rajasthan is the largest state and Goa is the smallest state in terms of area.
 The Himalayan Mountains are divided into three main parallel ranges.
o The northernmost is the Great Himalaya or Himadri. The world’s highest
peaks are located in this range.
o Middle Himalaya or Himachallies to the south of Himadri.
o The Shiwalik is the southernmost range.
o The Northern Indian plains lie to the south of the Himalayas.
o They are generally level and flat. These are formed by the alluvial deposits laid
down by the rivers– the Indus, the Ganga, the Brahmaputra and their tributaries.
 In the western part of India lies the Great Indian Desert.
 To the south of northern plains lies the peninsular plateau.
Aravalli hills, one of the oldest ranges of the world, border it on the north-west side.
 The Vindhyas and the Satpuras are the important ranges.
 The rivers Narmada and Tapi flow through these ranges. These are west-flowing rivers
that drain into the Arabian Sea.
 The Western Ghats or Sahyadris border the plateau in the west and the Eastern Ghats
provide the eastern boundary.
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 There are a number of east flowing rivers. The rivers Mahanadi, Godavari, Krishna and
Kaveri drain into the Bay of Bengal.
 The Sunderban delta is formed where the Ganga and Brahmaputra flow into the Bay
of Bengal
 Lakshadweep Islands are located in the Arabian Sea. These are coral islands located off
the coast of Kerala.
 The Andaman and the Nicobar Islands lie to the southeast of the Indian mainland in the
Bay of Bengal
Chapter 9_1: Geo9_1_size and location
INDIA– SIZE ANDLOCATION
LOCATION
 The main land extends between latitudes 8°4'N and 37°6'N and longitudes 68°7'E and
97°25'E.
 The Tropic of Cancer (23° 30'N) divides the country into almost two equal parts.
The southernmost point of the Indian Union– ‘Indira Point’ got submerged under the sea water
in 2004 during the Tsunami.
SIZE
 The land mass of India has an area of 3.28 million square km. India’s total area accounts
for about 2.4 per cent of the total geographical area of the world.
 Time along the Standard Meridian of India (82°30'E) passing through Mirzapur (in
Uttar Pradesh) is taken as the standard time for the whole country
 India has a land boundary of about 15,200 km and the total length of the coast line of the
mainland including Andaman and Nicobar and Lakshadweep is 7,516.6 km.
INDIA AND THE WORLD
 Since the opening of the Suez Canal in 1869, India’s distance from Europe has been
reduced by 7,000 km.
 Before 1947, there were two types of states in India – the provinces and the Princely
states. Provinces were ruled directly by British officials who were appointed by the
Viceroy. Princely states were ruled by local, hereditary rulers, who acknowledged
sovereignty in return for local autonomy.
Chapter 9_2: Geo9_2_physical
PHYSICAL FEATURES OF INDIA
The northern mountains are the major sources of water and forest wealth. The northern plains
are the granaries of the country. They provide the base for early civilisations.
The plateau is a storehouse of minerals, which has played a crucial role in the industrialisation
of the country.
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The coastal region and island groups provide sites for fishing and port activities. Thus, the
diverse physical features of the land have immense future possibilities of development.
The Theory of Plate Tectonics: According to this theory, the crust (upper part) of the earth
has been formed out of seven major and some minor plates.
Broadly, these plate movements are classified into three types
 While some plates come towards each other and form convergent boundary.
 Some plates move away from each other and form divergent boundary.
 At times, they may also move horizontally past each other and form transform boundary.
The oldest landmass, (the Peninsula part), was a part of the Gondwana land. The Gondwana
land included India, Australia, South Africa and South America as one single land mass.
Due to collision with Eurasian Plate, the sedimentary rocks which were accumulated in the
geosyncline known as the Tethys were folded to form the mountain system of western Asia and
Himalaya.
Gondwanaland: It is the southern part of the ancient super continent Pangea with Angara Land
in the northern part.
The northern plains are formed of alluvial deposits.
The peninsular plateau is composed of igneous and metamorphic rocks with gently rising
hills and wide valleys
MAJOR PHYSIOGRAPHIC DIVISIONS
(i) The Himalayan Mountains
(ii) The Northern Plains
(iii) The Peninsular Plateau
(iv) The Indian Desert
(v) The Coastal Plains
(vi) The Islands
The Himalayan Mountains
These mountain ranges run in a west-east direction from the Indus to the Brahmaputra.
The Himalaya consists of three parallel ranges in its longitudinal extent
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o The northern most range is known as the Great or Inner Himalayas or the
‘Himadri’.
o The range lying to the south of the Himadri forms the most rugged mountain
system and is known as Himachal or lesser Himalaya.
o While the Pir Panjal range forms the longest and the most important range, the
Dhaula Dhar and the Mahabharat ranges are also prominent ones
o This range consists of the famous valley of Kashmir, the Kangra and Kullu Valley
in Himachal Pradesh.
o The outer most range of the Himalayas is called the Shiwaliks.
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.
The Brahmaputra marks the eastern most boundaries of the Himalayas. They are known as the
Purvanchal or the Eastern hills and mountains.
The Purvanchal comprises the Patkai hills, the Naga Hills, Manipur hills and the Mizo hills.
The Northern Plain
The northern plain has been formed by the interplay of the three major river systems, namely–
the Indus, the Ganga and the Brahmaputra along with their tributaries. This plain is formed of
alluvial soil.
Majuli, in the Brahmaputra River is the largest inhabited riverine island in the world
The Northern Plain is broadly divided into three sections.
o The Western part of the Northern Plain is referred to as the Punjab Plains.
Formed by the Indus and its tributaries, the larger part of this plain lies in
Pakistan.
o The Indus and its tributaries–the Jhelum, the Chenab, the Ravi, the Beas and the
Satluj originate in the Himalaya. This section of the plain is dominated by the
doabs.
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o The Ganga plain extends between Ghaggar and Teesta rivers. It is spread over
the states of North India, Haryana, Delhi, U.P., Bihar, partly Jharkhand and West
Bengal to its East, particularly in Assam lays the Brahmaputra plain.
According to the variations in relief features, the Northern plains can be divided into four
regions.
i. Bhabar, all the streams disappear in this bhabar belt.
ii. South of this belt, the streams and rivers re-emerge and create a wet, swampy and
marshy region known as terai.
iii. The largest part of the northern plain is formed of older alluvium. They lie above
the flood plains of the rivers and present a terrace like feature. This part is known
as bhangar.
iv. The soil in this region contains calcareous deposits locally known as kankar. The
newer, younger deposits of the flood plains are called khadar.
The Peninsular Plateau
The Peninsular plateau is a tableland composed of the old crystalline, igneous and metamorphic
rocks.
This plateau consists of two broad divisions, namely, the Central Highlands and the Deccan
Plateau.
o The part of the peninsular plateau lying to the north of the Narmada River
covering a major area of the Malwa plateau is known as the Central Highlands.
o The Vindhyas range is bounded by the Central Highlands on the south and
o The Aravalli on the northwest
The flow of the rivers draining this region, namely the Chambal, the Sind, the Betwa and Ken is
from southwest to northeast, thus indicating the slope.
The eastward extensions of this plateau are locally known as the Bundelkhand and
Baghelkhand. The Chotanagpur plateau marks the further eastward extension, drained by
the Damodar River.
The Deccan Plateau is a triangular landmass that lies to the south of the river Narmada. The
Satpura range flanks its broad base in the north while the Mahadev, the Kaimur hills and the
Maikal range from its eastern extensions.
An extension of the Plateau is also visible in the northeast– locally known as the Meghalaya
and Karbi-Anglong Plateau.
Three Prominent hill ranges from the west to east are the Garo, the Khasi and the Jaintia Hills.
o The highest peaks include the Anai Mudi (2,695metres) and
o The Doda Betta (2,637 metres)
o Mahendragiri (1,501 metres) is the highest peak in the Eastern Ghats.
o Shevroy Hills and the Javadi Hills are located to the southeast of the Eastern
Ghats.
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o One of the distinct features of the peninsular plateau is the black soil area known
as Deccan Trap. This is of volcanic origin hence the rocks are igneous.
The Indian Desert
 The Indian desert lies towards the western margins of the Aravali Hills.
 It has arid climate with low vegetation cover.
 Luni is the only large river in this region.
The Coastal Plains
The western coast, sandwiched between the Western Ghats and the Arabian Sea, is a narrow
plain.
It consists of three sections.
 The northern part of the coast is called the Konkan (Mumbai – Goa),
 The central stretch is called the Kannad Plain
 While the southern stretch is referred to as the Malabar Coast
The plain along the Bay of Bengal are wide and level.
 In the northern part, it is referred to as the Northern Circar,
 While the southern part is known as the Coromandal Coast.
Large rivers such as the Mahanadi, the Godavari, the Krishna and the Kaveri have farmed
extensive delta on this coast.
The Chilika Lake is the largest salt water lake in India. It lies in the state of Orissa, to the south of
the Mahanadi delta along the eastern coast.
The Islands
 The Lakshadweep Islands group lying close to the Malabar coast of Kerala.
 Earlier they were known as Laccadive, Minicoy and Amindive. In 1973 these were
named as Lakshadweep.
 Kavaratti Island is the administrative headquarters of Lakshadweep.
 The Patli Island, which is uninhabited, has a bird sanctuary.
The Andaman in the north and the Nicobar in the south.
 It is believed that these islands are an elevated portion of submarine mountains.
 India’s only active volcano is found on Barren Island in Andaman and Nicobar group
of Islands.
Chapter 9_4: Geo9_4_CLIMATE
• The word monsoon is derived from the Arabic word ‘mausim’ which literally means season.
• ‘Monsoon’ refers to the seasonal reversal in the wind direction during a year.
Climate refers to the sum total of weather conditions and variations over a large area for a long
period of time (more than thirty years).
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Weather refers to the state of the atmosphere over an area at any point of time. The elements of
weather and climate are the same, i.e. temperature, atmospheric pressure, wind, humidity and
precipitation.
In the Thar Desert the day temperature may rise to 50°C, and drop down to near 15°C the same
night.
Himalayas protect the subcontinent from extremely cold winds from central Asia. This enables
northern India to have uniformly higher temperatures when compared to other areas on the
same latitudes.
Similarly, the peninsular plateau, under the influence of the sea from three sides, has moderate
temperatures.
CLIMATIC CONTROLS
There are six major controls of the climate of any place. They are: latitude, altitude, pressure
and wind system, distance from the sea (continentality), ocean currents and relief
features.
 Due to the curvature of the earth, the amount of solar energy received varies according
to latitude
 As one goes from the surface of the earth to higher altitudes, the atmosphere becomes
less dense and temperature decreases. The hills are therefore cooler during summers
 The hills are therefore cooler during summers. The pressure and wind system of any
area depend on the latitude and altitude of the place.
 As the distance from the sea increases, its moderating influence decreases and the
people experience extreme weather conditions. This condition is known as
continentality (i.e. very hot during summers and very cold during winters).
 Ocean currents along with onshore winds affect the climate of the coastal areas
FACTORS AFFECTING INDIA’S CLIMATE
Latitude
 The Tropic of Cancer passes through the middle of the country from the Rann of
Kuchchh in the west to Mizoram in the east.
 Almost half of the country, lying south of the Tropic of Cancer, belongs to the tropical
area. All the remaining area, north of the Tropic, lies in the sub-tropics. Therefore,
India’s climate has characteristics of tropical as well as subtropical climates
Altitude
 India has mountains to the north, which have an average height of about 6,000 metres.
 The Himalayas prevent the cold winds from Central Asia from entering the
subcontinent. It is because of these mountains that this subcontinent experiences
comparatively milder winters as compared to central Asia.
Pressure and Winds
• Pressure and surface winds;
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• Upper air circulation; and
• Western cyclonic disturbances and tropical cyclones
 These jet streams are located approximately over 27°-30° north latitude, therefore, they
are known as subtropical westerly jet streams
 An easterly jet stream, called the tropical easterly jet stream blows over peninsular
India, approximately over 14°N during the summer months
Jet stream
These are a narrow belt of high altitude (above 12,000 m) westerly winds in the troposphere.
Their speed varies from about 110 km/h in summer to about 184 km/h in winter. A number of
separate jet streams have been identified. The most constant are the mid-latitude and the sub-tropical
jet stream.
Western Cyclonic Disturbances
The western cyclonic disturbances are weather phenomena of the winter months brought in by
the westerly flow from the Mediterranean region. They usually influence the weather of the
north and north-western regions of India. Tropical cyclones occur during the monsoon as well
as in October -November, and are part of the easterly flow
Coriolis force
An apparent force caused by the earth’s rotation. The Coriolis force is responsible for deflecting
winds towards the right in the northern hemisphere and towards the left in the southern
hemisphere. This is also known as ‘Ferrel’s Law’.
THE INDIAN MONSOON
 The differential heating and cooling of land and water creates low pressure on the
landmass of India while the seas around experience comparatively high pressure.
 The shift of the position of Inter Tropical Convergence Zone (ITCZ)in summer, over the
Ganga plain (this is the equatorial trough normally positioned about 5°N of the equator
– also known as the monsoon trough during the monsoon season).
 The presence of the high-pressure area, east of Madagascar, approximately at 20°S over
the Indian Ocean. The intensity and position of this high-pressure area affects the Indian
Monsoon.
 The Tibetan plateau gets intensely heated during summer, which results in strong
vertical air currents and the formation of high pressure over the plateau at about 9 km
above sea level.
 The movement of the westerly jet stream to the north of the Himalayas and the presence
of the tropical easterly jet stream over the Indian peninsula during summer
Inter Tropical Convergence Zone
The Inter Tropical Convergence Zone (ITCZ,) is a broad trough of low pressure in equatorial
latitudes. This is where the northeast and the southeast trade winds converge. This convergence
zone lies more or less parallel to the equator but moves north or south with the apparent
movement of the sun.
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El Nino
This is a name given to the periodic development of a warm ocean current along the coast of
Peru as a temporary replacement of the cold Peruvian current. ‘El Nino’ is a Spanish word
meaning ‘the child’, and refers to the baby Christ, as this current starts flowing during
Christmas. The presence of the El Nino leads to an increase in sea-surface temperatures and
weakening of the trade winds in the region
THE ONSET OF THE MONSOON AND WITHDRAWAL
 The duration of the monsoon is between 100-120 days from early June to mid-
September.
 The monsoon arrives at the southern tip of the Indian peninsula generally by the first
week of June. Subsequently, it divides into two – the Arabian Sea branch and the Bay of
Bengal branch. The Arabian Sea branch reaches Mumbai about ten days later on
approximately the 10 th of June. This is a fairly rapid advance. The Bay of Bengal branch
also advances rapidly and arrives in Assam in the first week of June.
 The Arabian Sea and the Bay of Bengal branches of the monsoon merge over the north
western part of the Ganga plains.
 The withdrawal of the monsoon begins in north western states of India by early
September.
 By early December, the monsoon has withdrawn from the rest of the country
THE SEASONS
Four main seasons can be identified in India – the cold weather season, the hot weather season,
the advancing monsoon and the retreating monsoon with some regional variations.
The Cold Weather Season (winter)
 The cold weather season begins from mid-November in northern India and stays till
February. December and January are the coldest months in the northern part of India.
 A characteristic feature of the cold weather season over the northern plains is the inflow
of cyclonic disturbances from the west and the northwest. These low-pressure systems,
originate over the Mediterranean Sea and western Asia and move into India, along with
the westerly flow.
The Hot Weather Season (summer)
 Due to the apparent northward movement of the sun, the global heat belt shifts
northward. As such, from March to May, it is hot weather season in India
 A striking feature of the hot weather season is the ‘loo’. These are strong, gusty, hot, dry
winds blowing during the day over the north and north western India.
 Towards the close of the summer season, pre-monsoon showers are common especially,
in Kerala and Karnataka. They help in the early ripening of mangoes, and are often
referred to as ‘mango showers’.
Advancing Monsoon (The Rainy Season)
 These winds are strong and blow at an average velocity of 30 km per hour.
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 The inflow of the south-west monsoon into India brings about a total change in the
weather.
 Early in the season, the windward side of the Western Ghats receives very heavy rainfall,
more than 250 cm. The Deccan Plateau and parts of Madhya Pradesh also receive some
amount of rain in spite of lying in the rain shadow area. The maximum rainfall of this
season is received in the north-eastern part of the country. Mawsynram in the southern
ranges of the Khasi Hills receives the highest average rainfall in the world
Retreating Monsoon (The Transition Season)
 During October-November, The south-west monsoon winds weaken and start
withdrawing gradually. By the beginning of October, the monsoon withdraws from the
Northern Plains
 Owing to the conditions of high temperature and humidity, the weather becomes rather
oppressive during the day. This is commonly known as ‘October heat’
 The low-pressure conditions, over north western India, get transferred to the Bay of
Bengal by early November. This shift is associated with the occurrence of cyclonic
depressions, which originate over the Andaman Sea.
DISTRIBUTION OF RAINFALL
 The western coast and north eastern India receive over about 400 cm of rainfall
annually
 Rainfall is equally low in the interior of the Deccan plateau, and east of the Sahyadris.
 A third area of low precipitation is around Leh in Jammu and Kashmir. The rest of the
country receives moderate rainfall. Snowfall is restricted to the Himalayan region
 Mawsynram, the wettest place on the earth is also reputed for its stalagmite and
stalactite caves
Chapter 11_1: Geo11_1_India_Location
INDIA– LOCATION
The southern part of the country lies within the tropics and the northern part lies in the sub-tropical
zone or the warm temperate zone.
Our southern boundary extends upto 6°45' N latitude in the Bay of Bengal.
The latitudinal and longitudinal extent of India, they are roughly about 30 degrees, whereas the
actual distance measured from north to south extremity is 3,214 km, and that from east to west
is only 2,933 km.
This location is responsible for large variations in land forms, climate, soil types and natural
vegetation in the country.
 The presence of lofty mountains in the north;
 Large rivers such as Ganga, Brahmaputra, Mahanadi, Krishna, Godavari and Kaveri;
 Green forested hills in northeast and south India; and the vast sandy expanse of
Marusthali.
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 Bounded by the Himalayas in the north, Hindukush and Sulaiman ranges in the
northwest, Purvachal hills in the north-east and
 By the large expanse of the Indian ocean in the south, it forms a great geographic entity
known as the Indian subcontinent.
 Peninsular part of India extends towards the Indian Ocean. This has provided the
country with a coastline of 6,100 km in the mainland and 7,517 km in the entire
geographical coast of the mainland
The sea upto 12 nautical miles (about 21.9 km) from the coast.
There is a general understanding among the countries of the world to select the standard
meridian in multiples of 7°30' of longitude.
Chapter
PHYSIOGRAPHY
STRUCTURE AND PHYSIOGRAPHY
Based on the variations in its geological structure and formations, India can be divided into
three geological divisions. These geological regions broadly follow the physical features
(i) The Peninsular Block
(ii) The Himalayas and other Peninsular Mountains
(iii) Indo-Ganga-Brahmaputra Plain
THE PENINSULAR BLOCK
 The northern boundary of the Peninsular Block may be taken as an irregular line
running from Kachchh along the western flank of the Aravali Range near Delhi and then
roughly parallel to the Yamuna and the Ganga as far as the Rajmahal Hills and the Ganga
delta. Apart from these, the Karbi Anglong and the Meghalaya Plateau in the northeast
and Rajasthan in the west are also extensions of this block.
 The north-eastern parts are separated by the Malda fault in West Bengal from the
Chotanagpur plateau. In Rajasthan, the desert and other desert–like features overlay this
block
 The Indo-Australian Plate
 The rift valleys of the Narmada, the Tapi and the Mahanadi and the Satpura block
mountains are some examples of it.
 The Peninsula mostly consists of relict and residual mountains like the Aravali hills, the
Nallamala hills, the Javadi hills, the Veliconda hills, the Palkonda range and the
Mahendragiri hills, etc.
 Most of the east flowing rivers form deltas before entering into the Bay of Bengal. The
deltas formed by the Mahanadi, the Krishna, the Kaveri and the Godavari are important
examples
THE HIMALAYAS AND OTHER PENINSULAR MOUNTAINS
 These mountains are tectonic in origin, dissected by fast-flowing rivers which are in
their youthful stage.
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 Various landforms like gorges, V-shaped valleys, rapids, waterfalls, etc. are indicative of
this stage.
INDO-GANGA-BRAHMAPUTRA PLAIN
 The third geological division of India comprises the plains formed by the river Indus, the
Ganga and the Brahmaputra. Originally, it was a geo-synclinal depression which attained
its maximum development
 During the third phase of the Himalayan mountain formation approximately about 64
million years ago.
 Since then, it has been gradually filled by the sediments brought by the Himalayan and
Peninsular rivers. Average depth of alluvial deposits in these plains ranges from 1,000-
2,000 m.
PHYSIOGRAPHY
‘Physiography’ of an area is the outcome of structure, process and the stage of development.
Based on these macro variations, India can be divided into the following physiographic
divisions:
(i) The Northern and North-eastern Mountains
(ii) The Northern Plain
(iii) The Peninsular Plateau
(iv) The Indian Desert
(v) The Coastal Plains
(vi) The Islands.
The approximate length of the Great Himalayan range, also known as the central axial range, is
2,500 km from east to west, and their width varies between 160-400 km from north to south.
On the basis of relief, alignment of ranges and other geomorphological features, the Himalayas
can be divided into the following sub-divisions:
(i) Kashmir or Northwestern Himalayas
(ii) Himachal and Uttaranchal Himalayas
(iii) Darjiling and Sikkim Himalayas
(iv) Arunachal Himalayas
(v) Eastern Hills and Mountains.
Kashmir or North-western Himalayas
 It comprises a series of ranges such as the Karakoram, Ladakh, Zaskar and Pir Panjal.
The north-eastern part of the Kashmir Himalayas is a cold desert, which lies between
the Greater Himalayas and the Karakoram ranges
 Between the Great Himalayas and the Pir Panjal range, lie the world famous valley of
Kashmir and the famous Dal Lake.
 some famous places of pilgrimage such as Vaishno Devi, Amarnath Cave, Charar -e-
Sharif, etc. are also located here and large number of pilgrims
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 Srinagar, capital city of the state of Jammu and Kashmir is located on the banks of
Jhelum River. Dal Lake in Srinagar presents an interesting physical feature.
In Kashmir Valley, the meanders in Jhelum river are caused by the local base level provided by
the erstwhile larger lake of which the present Dal Lake is a small part
The Himachal and Uttaranchal Himalayas
 This part lies approximately between the Ravi in the west and the Kali (a tributary of
Ghaghara) in the east. It is drained by two major river systems of India, i.e. the Indus and
the Ganga. Tributaries of the Indus include the river Ravi, the Beas and the Satluj, and
the tributaries of Ganga flowing through this region include the Yamuna and the
Ghaghara.
 All the three ranges of Himalayas are prominent in this section also. These are the Great
Himalayan range, the Lesser Himalayas (which is locally known as Dhaoladhar in
Himachal Pradesh and Nagtibha in Uttaranchal) and the Shiwalik range from the North
to the South.
 some of the important hill stations such as Dharamshala, Mussoorie, Shimla, Kaosani
and the cantonment towns and health resorts such as Shimla, Mussoorie, Kasauli,
Almora, Lansdowne and Ranikhet, etc. were developed in this region.
 Some important duns located in this region are the Chandigarh-Kalka dun, Nalagarh
dun, Dehra Dun, Harike dun and the Kota dun, etc. Dehra Dun is the largest of all the
duns with an approximate length of 35-45 km and a width of 22-25 km.
 The famous ‘Valley of flowers’ is also situated in this region. The places of pilgrimage
such as the Gangotri, Yamunotri, Kedarnath, Badrinath and Hemkund Sahib are also
situated in this part. The region is also known to have five famous Prayags.
The Shiwalik
The word shiwalik has its origin in the geological formation found in and around a place called
Sivawala near Dehra Dun which was once a headquarter of the Imperial Survey and which
subsequently established its permanent headquarters at Dehra Dun
The Darjiling and Sikkim Himalayas
 They are flanked by Nepal Himalayas in the west and Bhutan Himalayas in the east. It is
relatively small but is a most significant part of the Himalayas. Known for its fast-flowing
rivers such as Tista, it is a region of high mountain peaks like Kanchenjunga
(Kanchengiri), and deep valleys.
 Introduced tea plantations in this region
 In place of the Shiwaliks here, the ‘duar formations’ are important, which have also been
used for the development of tea gardens.
 Sikkim and Darjiling Himalayas are also known for their scenic beauty and rich flora and
fauna, particularly various types of orchids.
The Arunachal Himalayas
 Some of the important mountain peaks of the region are Kangtu and Namcha Barwa.
 Some of the important rivers are the Kameng, the
 Subansiri, the Dihang, the Dibang and the Lohit.
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 The highest hydro-electric power potential in the country.
 An important aspect of the Arunachal Himalayas is the numerous ethnic tribal
communities inhabiting in these areas. Some of the prominent ones from west to east
are the Monpa, Daffla, Abor, Mishmi, Nishi and the Nagas.
 Most of these communities practise Jhumming.
The Eastern Hills and Mountains
 They are known by different local names. In the north, they are known as Patkai Bum,
Naga Hills, and the Manipur hills and in the south as Mizo or Lushai hills.
 These are low hills, inhabited by numerous tribal groups practising Jhum cultivation.
 The Barak is an important river in Manipur and Mizoram
 The physiography of Manipur is unique by the presence of a large lake known as
‘Loktak’ lake at the centre, surrounded by mountains from all sides. Mizoram which is
also known as the ‘Molassis basin’ which is made up of soft unconsolidated deposits.
 Most of the rivers in Nagaland form the tributary of the Brahmaputra. While two rivers
of Mizoram and Manipur are the tributaries of the Barak river
The Northern Plains
 The northern plains are formed by the alluvial deposits brought by the rivers – the
Indus, the Ganga and the Brahmaputra
 These can be divided into three major zones: the Bhabar, the Tarai and the alluvial
plains. The alluvial plains can be further divided into the Khadar and the Bhangar.
 Bhabar is a narrow belt ranging between 8-10 km parallel to the Shiwalik foothills at the
break-up of the slope. As a result of this, the streams and rivers coming from the
mountains deposit heavy materials of rocks and boulders
 South of the Bhabar is the Tarai belt, with an approximate width of 10-20 km where
most of the streams and rivers re-emerge without having any properly demarcated
channel, thereby, creating marshy and swampy conditions known as the Tarai. This has
a luxurious growth of natural vegetation and houses a varied wild life
 The south of Tarai is a belt consisting of old and new alluvial deposits known as the
Bhangar and Khadar respectively. These plains have characteristic features of mature
stage of fluvial erosional and depositional landforms such as sand bars, meanders,
oxbow lakes and braided channels.
 The mouths of these mighty rivers also form some of the largest deltas of the world, for
example, the famous Sunderbans delta.
The Peninsular Plateau
 Rising from the height of 150 m above the river plains up to an elevation of 600-900 m is
the irregular triangle known as the peninsular plateau.
 Delhi ridge in the northwest, (extension of Aravalis), the Rajmahal hills in the east, Gir
range in the west and the Cardamom hills in the south constitute the outer extent of the
peninsular plateau.
 The Peninsular India is made up of a series of patland plateaus such as the Hazaribagh
plateau, the Palamu plateau, the Ranchi plateau, the Malwa plateau, the Coimbatore
plateau and the Karnataka plateau, etc. This is one of the oldest and the most stable
landmass of India.
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 The western and north-western part of the plateau has an emphatic presence of black
soil.
 The north-western part of the plateau has a complex relief of ravines and gorges. The
ravines of Chambal, Bhind and Morena are some of the well-known examples
On the basis of the prominent relief features, the peninsular plateau can be divided into three
broad groups:
(i) The Deccan Plateau
(ii) The Central Highlands
(iii) The North-eastern Plateau
The Deccan Plateau
 Western Ghats are locally known by different names such as Sahyadris in Maharashtra,
Nilgiri hills in Karnataka and Tamil Nadu and Anaimalai hills and Cardamom hills in
Kerala.
 This is bordered by the Western Ghats in the west, Eastern Ghats in the east and the
Satpura, Maikal range and Mahadeo hills in the north.
 ‘Anaimudi’ (2,695 m), the highest peak of Peninsular plateau is located on the Anaimalai
hills of the Western Ghats followed by Dodabetta (2,637 m) on the Nilgiri hills.
 Some of the important ranges include the Javadi hills, the Palconda range, the Nallamala
hills, the Mahendragiri hills, etc.
 The Eastern and the Western Ghats meet each other at the Nilgiri hills.
The Central Highlands
 It is a classic example of the relict mountains which are highly denuded and form
discontinuous ranges.
 This region has undergone metamorphic processes in its geological history, which can
be corroborated by the presence of metamorphic rocks such as marble, slate, gneiss, etc
 The general elevation of the Central Highlands ranges between 700-1,000 m above the
mean sea level and it slopes towards the north and northeastern directions. Most of the
tributaries of the river Yamuna have their origin in the Vindhyan and Kaimur ranges.
 Banas is the only significant tributary of the river Chambal that originates from the
Aravalli in the west. An eastern extension of the Central Highland is formed by the
Rajmahal hills, to the south of which lies a large reserve of mineral resources in the
Chotanagpur plateau
The Northeastern Plateau
Today, the Meghalaya and Karbi Anglong plateau stand detached from the main Peninsular
Block. The Meghalaya plateau is further sub-divided into three:
(i) The Garo Hills;
(ii) The Khasi Hills;
(iii) The Jaintia Hills, named after the tribal groups inhabiting this region.
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An extension of this is also seen in the Karbi Anglong hills of Assam. Similar to the Chotanagpur
plateau, the Meghalaya plateau is also rich in mineral resources like coal, iron ore, sillimanite,
limestone and uranium.
This area receives maximum rainfall from the south west monsoon. As a result, the Meghalaya
plateau has a highly eroded surface. Cherrapunji displays a bare rocky surface devoid of any
permanent vegetation cover.
The Indian Desert
 This region receives low rainfall below 150 mm per year; hence, it has arid climate with
low vegetation cover. It is because of these characteristic features that this is also known
as Marusthali.
 To the northwest of the Aravali hills lies the Great Indian Desert. It is a land of
undulating topography dotted with longitudinal dunes and barchans.
 On the basis of the orientation, the desert can be divided into two parts: the northern
part is sloping towards Sindh and the southern towards the Rann of Kachchh. Most of
the rivers in this region are ephemeral. The Luni River flowing in the southern part of
the desert is of some significance. Low precipitation and high evaporation makes it a
water deficit region.
The Coastal Plains
It can be broadly divided into two:
(i) the western coastal plains;
(ii) The eastern coastal plains.
It is believed that the city of Dwaraka which was once a part of the Indian mainland situated
along the west coast is submerged under water. Because of this submergence it is a narrow belt
and provides natural conditions for the development of ports and harbours.
Kandla, Mazagaon, JLN port Navha Sheva, Marmagao, Mangalore, Cochin, etc. are some of the
important natural ports located along the west coast.
The Kachchh and Kathiawar coast in Gujarat, Konkan coast in Maharashtra, Goan coast and
Malabar Coast in Karnataka and Kerala respectively.
 Every year the famous Nehru Trophy Vallamkali (boat race) is held in Punnamada
Kayalin Kerala
There are well developed deltas here, formed by the rivers flowing eastward in to the Bay of
Bengal. These include the deltas of the Mahanadi, the Godavari, the Krishna and the Kaveri.
Because of its emergent nature, it has less number of ports and harbours.
The Islands
The Bay of Bengal island groups consist of about 572 islands/islets.
 These are situated roughly between 6°N-14°N and 92°E -94°E.
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 The two principal groups of islets include the Ritchie’s archipelago and the Labrynth
Island.
 The entire group of island is divided into two broad categories – the Andaman in the
north and the Nicobar in the south. They are separated by a water body which is called
the Ten degree channel.
 Some important mountain peaks in Andaman and Nicobar Islands are
o Saddle peak (North Andaman – 738 m),
o Mount Diavolo (Middle Andaman – 515 m),
o Mount Koyob (South Andaman – 460 m) and
o Mount Thuiller (Great Nicobar – 642 m).
 Barren Island, the only active volcano in India is also situated in the Nicobar Islands
The islands of the Arabian Sea include Lakshadweep and Minicoy.
 These are scattered between 8°N-12°N and 71°E -74°E longitude
 There are approximately 36 islands of which 11 are inhabited.
 Minicoy is the largest island with an area of 453 sq. km.
 The entire group of islands is broadly divided by the Eleventh degree channel, north of
which is the Amini Island and to the south of the Canannore Island.
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