SOCIAL ASSIGNMENT

INDIA-SIZE & LOCATION

&

PHYSICAL FEATURES OF INDIA

Location

• India is a vast country. It is lying entirely in the northern hemisphere.

• The tropic of cancer divides the country to 2 equal halves. The main land extends between latitudes 8degree4’N and 37degree6’N and longitudes 68degree7’E and 97degree’25E.

Size

• India has a total landmass area of 3.28 million sq.kms. It is the seventh largest country . India has a coastline boundary of 15,200km and 7,516.6 km .

• The standard meridian of India is 82degree30E which passes through Mirzapur in Uttar Pradesh .

India and The World

• India’s landmass has a central location between East and West Asia. India is a southward extension of the Asian Continent. The trans Indian ocean routes which connect the countries of Europe from the west and countries of East Asia.

• Deccan plateau helps India to have contact with West Asia, Africa and Europe .

India and neighboring countries

• India shares its land boundaries with Pakistan and Afghanistan in northwest ,China ,Nepal and Bhutan in the north and Myanmar and Bangladesh in the east.

• The southern neighbors across the sea are sir lank and Maldives

• India also shares historical links with its neighbors.

Facts of India

• The southernmost point of Indian-’indira point’ got submerged in sea water in 2004 Tsunami .

• Since the opening of Suez canal in 1869,india’s distance from Europe has been reduced by 7,000km .

• Before 1947 there were 2 types of states i.e. is provinces and princely.

PHYSICAL FEATURES OF

INDIA

INTRODUCTION

India is a large landmass formed during different geological periodswhich has influenced

her relief. Besides geological formations, a number of processes such asweathering, erosion and deposition have created and modified the reliefto its present form. Earth scientists have attempted to explain theformation of physical features with the help of some theories based oncertain evidences. One such plausible theory is the “Theory of PlateTectonics”. According to this theory, the crust (upper part) of the earthhas been formed out of seven major and some minor plates.

The movement of the plates results in the building up of stresses withinthe plates and the

continental rocks above, leading to folding, faulting and volcanicactivity.

• 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. In the event of two plates coming together they may either collide and crumble, or one may slide under the other. At times, they may also move horizontally past.

• each other and form transform boundary. The movement of these plates have changed the position and size of the continents over millions of years. Such movements have also influenced the evolution of the present landform features of India.

CONVERGENT PLATE

DIVERGENT PLATE

TRANSFORM PLATE

Theory Of Plate Tectonics• The crust of the Earth is made up of seven Major plates and

some Minor plates.

• The movement of the plates results in Folding, Faulting and Volcanic Activity.

Boundaries

• Convergent – These types of Boundaries are formed when two plates come towards each other.

• Divergent – When two plates away from each other they form Divergent Boundaries.

• Transform Boundary – When two plates move horizontally past each other they form Transform Boundaries.

Major Physiographic Divisions

• The Himalayan Mountains

• The Northern Plains

• The Peninsular Plateau

• The Indian Desert

• The Coastal Plains

• The Islands

1.The Himadri2.The Himachal3.The Shiwaliks

• It is the Northernmost range of the Himalayas.

• It’s width varies from 400 km in Kashmir to 150 km in Arunachal Pradesh.

• They form an arc, which covers a distance of 2,400 km.

• The average height of its peaks are 6,000 km.

• They are made up of Granite.

Peak Country Height in Meters

Mt. Everest Nepal 8848

Kanchenjunga India 8598

Makalu Nepal 8481

Dhaulagiri Nepal 8172

Nanga Parbat India 8126

Annapurna Nepal 8078

Nanda Devi India 7817

Kamet India 7756

Namcha Barwa India 7756

Gurla Mandhata Nepal 7728

• It lies south to the Himadri.

• The average width is 50 km.

• The average height is 3,700 to 4,500 m.

• The ranges of Pir Panjal, Dhaula Dhar and the Mahabharat are found here.

• The famous Kangra(Kashmir) and Kullu(Himachal Pradesh) valleys are found here.

• Mainly composed of Highly compressed rocks.

• The southernmost range of the Himalayas.• Their width varies from 10-50 km.• Their altitude varies from 900-1,100 m.• The valleys in these ranges are composed of thick gravel and

rich alluvium which are brought down by the rivers from the Northern Himalayan ranges.

• The longitudinal valleys lying between the Himachal and the Shiwaliks are known as Duns(Dehra Dun, Kotli Dun and Patli Dun are some).

Longitudinal Divisions

• The Himalayas have been divided on the basis of regions from west to east. These divisions have been demarcated by River valleys.

• Punjab Himalayas – Indus to Satluj rivers

• Kumaon Himalayas – Satluj to Kali

rivers

• Nepal Himalayas – Kali to Tista rivers

• Assam Himalayas – Tista to Dihang

rivers

The Purvanchal

• The Brahmaputra marks the Eastern boundary of the Himalayas.

• The Himalayas bend sharply after the Dihang gorge towards the South and spread along the Eastern boundary of India.

• They consist of the Patkai hills, the Naga hills, Manipur hills and the Mizo hills.

• They are covered with dense forests and run parallel to valleys.

• They are made up of Strong Sandstones and Sedimentary rocks.

The Northern Plains

• They have been formed by the alluvial soil brought down by the Indus, The Ganga, The Brahmaputra and their Tributaries.

• The Alluvial soil is millions of years old.

• It covers an area of 7 lakh sq. km.

• The plain is 2,400 km long and 240-320 km wide.

• This plain is widely used for Farming.

• The rivers split into numerous Distributaries in their lower courses due to the deposition of silt.

• Punjab Plains– Western Northern Plain

• Punjab plains are formed by Indus and its Tributaries.

• The Ganga Plains – Ghaggar to Tista rivers

• Brahmaputra Plains – Assam and Eastern plain

Relief features

• The descending rivers from the Shiwaliks deposit pebbles 8-16 km wide belt parallel to the slopes of Shiwaliks known as bhabar.

• The streams and rivers re-emerge south of this belt to create a wet, swampy and marshy region known as terai.

• The terai is used for Agricultural.• The older alluvium lies above the flood plains like a terrace

known as bhangar.• The soil in this region contains calcareous deposits known as

kankar.• The newer deposits of the Flood plains are known as

khaddar.

• The plateau is made up of old crystalline, igneous and metamorphic rocks.

• It was formed due to the drifting and breaking of the Gondwana landmass.

• It consists of two broad divisions known as the Central Highlands and the Deccan Plateau.

The Central Highlands

• Lies north to the Narmada.

• The Vindhyan range lies on the south and the Aravalis range lies on the Northwest.

• They are wider in the west but narrower in the East.

• The eastward extensions are known as Bundelkhand and Baghelkhand.

• The Chotanagpur plateau marks the further eastward extension, drained by the Damodar.

The Deccan Plateau

• Triangular landmass south to the Narmada.

• The Satpura range in the North and the Mahadev, the Kaimur hills and the Maikal range in its eastward extension.

• Higher in the west and slopes gently eastwards.

• Meghalaya, Karbi-Anglong plateau and North Cachar hills form the Northwest extension.

• Separated from the Chotanagpur plateau by a fault.

• Three prominent ranges from west to east are the Garo, the Khasi and the Jaintia Hills.

Western and Eastern Ghats• They form Western and Eastern edges of the Deccan plateau.• The Western Ghats are higher than the Eastern

Ghats.• Western Ghats :- Their average elevation is 900-1,600 m. Their height increases from North to South. Highest peaks are the Anai Mudi(2,695 m) and the

Doda Betta(2,637 m).• Eastern Ghats:- Their average elevation is 600 m. They stretch from the Mahanadi Valley to the Nilgiris in the South. They are continuously dissected by the rivers draining into the Bay

of Bengal. Mahendragiri(1,501 m) is the highest peak. Shevroy and Javadi Hills are located in the Southeast.

Extra Features

• The Peninsular plateau has black soil known as the Deccan Trap.

• They are made up of Igneous rocks.

• The Aravalis range form the North and Northwestern margins.

• They are highly eroded hills and extend from the Gujarat to Delhi.

• Lies west to the Aravali range.

• Covered with sand dunes it

receives low rainfall of 150 mm per year.

• Has arid climate with low vegetation cover.

• Luni is the only large river in this Desert.

• The Western Coast lies between the Western Ghats and the Arabian Sea.

• It consists of three sections.

• The northern part is called the Konkan(Mumbai to Goa), the central stretch is called the Kannad plain and the southern stretch is known as the Malabar Coast.

• The Eastern Coasts are wide and level.

• The Northern Circar(North) and the Coromandel Coast(South) are its two sections.

• The rivers Mahanadi, Godavari, Kaveri and Krishna have formed their Deltas here.

• Lake Chilika is an important feature along the Eastern Coast.

• The Lakshadweep island lie close to the Malabar coast.

• They are composed of Small coral islands.

• They cover an area of 32 sq. km.

• Kavaratti island is its administrative Headquarters.

• The uninhabited Pitti island has a Bird Sanctuary.

• The Andaman and Nicobar islands are located in the Bay of Bengal.

• They are divided into the Andaman in the north and Nicobar in the south.

• It is believed that these mountains are elevated portions of Submarine Mountains.

• These Islands display a great diversity of flora and fauna.

• Due to the presence of Equatorial Climate, they have thick forest cover.

FROM :- ALEFIYA MOHAMED

CLASS :- IX

ROLL NO :- 04

SCHOOL:- MANSUKBHAI KOTHARI NATIONAL SCHOOL