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This document is a lesson about the physiography of India. It discusses the location of India in terms of latitude and longitude, and describes the significance of the relative location of India in relation to neighboring countries. It also explains the major physical divisions of India, including the Himalayan mountains, the Northern Plains, the Thar Desert, and the Peninsular Plateau.

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Physiography of India MODULE - 2 India: Natural Environ-...

Physiography of India MODULE - 2 India: Natural Environ- ment, Resources and Development 9 Notes PHYSIOGRAPHY OF INDIA Tutor : Dear learners, you will agree that the place to which we belong has many influences on our thinking and behaiour. Let us try to know which place do we belong to? Natasha : I belong to Hisar town. Farah is from Fatehabad and Rajinder comes from Bhiwani. Tutor : Do you know where all these places are located? Rajinder : Yes, they are in Haryana as well as in India. But, where is India located? Farah : What is the need to know India’s location? Tutor : Location of a country is the key to its identity. It determines the important aspects like climate, vegetation, agriculture, resources etc. This has a deep impact on the way people of that area live, what they eat and how powerful is their voice on the world stage. Therefore, to understand the various aspects of India, we need to look into its location. Let us discuss more about it in this lesson. OBJECTIVES After studying this lesson you will be able to: l describe the location of India in terms of latitude and longitude; l describe with the help of map, the significance of the relative location of India in terms of neighbouring countries; l illustrate the States and Union Territories with the help of political map of India; l explain the major physical divisions of India; l describe the drainage system in India; l compare and contrast between the Himalayan and the Peninsular drainage system; and l explain the importance of people’s participation in keeping river clean. SOCIAL SCIENCE 193 MODULE - 2 Physiography of India India: Natural Environ- ment, Resources and Development 9.1 LOCATION Teacher: Learners, when someone asks where India is, we can answer in two ways, in terms of absolute and relative location. Let us see what we mean by absolute location and relative location. Absolute location is given in degrees of latitude and longitude. Relative location depends upon point of reference, e.g., near, far etc. Notes Latitude: Latitude is the angular distance, north or south from the equator, of a point on the earth’s surface. Longitude: Longitude is an angular distance on the earth’s surface, measured east or west from the prime meridian at Greenwich. Angular distance : The angular distance between the points from the centres is called angular distance. Latitude Longitude (North/South) (west/East) 90°N 0° Tropic of Arctic 66½°N Tropic of 23½°N Cancer Prime Meridian 0° 0° Equator W E Tropic of 23½°S Capricorn Tropic of 66½°S Antarctica 90°S 0° Latitude varies from 0° Longitude varies from 0° of the equator to 90° at Greenwich to 180° North and South East and West at the poles Teacher: With the help of this map can you find out the latitudinal and the longitudianal location of Indian mainland. Natasha: The Indian mainland extends between 8°4′ North and 37°6′ North latitudes and from 68°7′ East and 97°25′ East longitudes. Thus, the latitudinal and the North-south extent is 3214 km and East-west extent is 2933 km. India accounts 2.42% of the total world land area Teacher: India lies entirely in the northern hemisphere, and eastern hemisphere. The Tropic of Cancer (23°30′ North) passes through the centre of the country. It divides the country into almost two equal parts Northward of this latitude is North India and South of it is known as south India. Similarly 194 SOCIAL SCIENCE Physiography of India MODULE - 2 India: Natural Environ- ment, Resources and Development Notes Figure 9.1 Latitudinal and Longitudinal extent of mainland of India 82°30′ East longitude passes almost from the middle of the country. It is known as Standard Meridian of India. Teacher: Now determine the relative location of India and then record it in the space given below: Remember relative location is given in relationship to other places (north of, south of, northeast of, next to, across from).India is part of Asian continent. India is surrounded by water from three sides. Arabian sea in west, Bay of Bengal in the east and Indian ocean in the south. Towards its north west is Pakistan and Afghanistan. China, Bhutan, Tibet and Nepal lies to its north. Bangladesh and Myanmar lies to its east. Srilanka and Maldives are located in the Indian Ocean towards its south. The southern most point of the country is Indira Point (Nicobar Islands) which lies on 6°4′ N latitudes and Kannya Kumari is southern most point of Indian mainland which lies on 8°4′ N latitudes. SOCIAL SCIENCE 195 MODULE - 2 Physiography of India India: Natural Environ- ment, Resources and Development The 82°30′E longitude passes through Mirzapur (in Uttar Pradesh). This is the Standard Meridian of the country. The 82°30′ East has been selected as standard Merdian because there is a time lag of almost two hours between Notes Gujarat and Arunanchal Pradesh. Therefore, a Central Meridian is selected to determine the time for the whole country. 9.1.1 Locational Significance Let’s observe the Fig. 9.2.What do you notice? India is the largest country in terms of area and population in South-Asia. It is surrounded by ocean. India is strategically located in Indian Ocean. It commands sea routes between Europe and Africa, South- East Asia, far East Asia and Oceania. It is because of this that India shares good trade relation between many countries since ancient times. India has a good location in terms of sea and also well connected by land. Various passes like Nathu-La (Sikkim), Shipki-La (Himachal Pradesh), Zoji-La and Burji la pass (Jammu & Kashmir) have their own importance. The main India-Tibet trade route that connects Kalimpong near Darjeeling with Lhasa in Tibet passes through Jelepa La. Several passes have provided a passage to many ancient travelers. These routes are not only important for trade but also to exchange ideas and culture. 40°E 60°E 80°E 100°E 120°E 140°E 40°N BLACK JAPAN SEA Tokyo ARAL SEA SEA CASPIAN Syria 30°N IRAQ CHINA AN I ST IRAN AN GH AF TIBET SAUDI Delhi ARABIA PAKISTAN NE PACIFIC OCEAN PAL 20°N RE Karachi BANGLA INDIA D DESH Kolkata MYANMAR SE Philippines A ARABIAN Mumbai THAILAND SEA BAY OF BENGAL 10°N Bangkok ETHOPIA SRI LANKA 0° MALAYSIA MALDIVES Sea Routes INDIAN OCEAN Air Routes 0 400 800 INDONSIA Kilometres AUSTRALIA Figure 9.2 Location of India with respect to important trade routes 196 SOCIAL SCIENCE Physiography of India MODULE - 2 India: Natural Environ- ment, Resources and Development INTEXT QUESTIONS 9.1 1. Look at the map 9.2 and answer the following questions. (i) Find out the names of two countries lying to the eastern side of India. (ii) Mention the names of two seas located on the eastern and western side Notes of India. (iii) Which country is connected to India by Palk Strait? (iv) Write the names of two countries having a common border with India. 9.2 STATES AND UNION TERRITORIES OF INDIA India is the seventh largest country in the world. It has land boundaries of 15,200 km and 6100km long coast line. India’s landmass covers 3.28 million square kilometer of area. This accounts for nearly 2.42 percent of the total geographical area of the world. For good governance, India has been divided into 28 states and 7 union territories. Let us study the Fig. 9.3 given below. 64° 72° 76° 80° 84° 88° 92° 32° JAMMU & KASHMIR Srinagar INDIA 32° POLITICAL H. P. Shimla C H I N A PUNJAB Dehradun 28° PAKISTAN Chandigarh TIBET UTTARAKHAND N A A RY ARUNACHAL HA DELHI NE 28° PA SIKKIM PRADESH L BHUTAN Itanagar UTTARPRADESH Gangtok Jaipur ASSAM RAJASTHAN Dispur NAGALAND 24° Lucknow Shilong Kohima Patna MEGHALAYA Imphal BIHAR BANGLADESH MANIPUR 24° JHARKHAND Agartala Bhopal TRIPURA Aizawl Gandhinagar WEST Ranchi BENGAL MIZORAM GUJARAT MADHYA PRADESH RH Kolkata 20° A SG TI Daman MYANMAR AT (D&D) ODISHA CH Diu (D&D) Silvasa Raipur Bhubaneshwar 20° D&NH Mumbai MAHARASHTRA 16° ARABIAN BAY OF BEGAL SEA Hyderabad ANDHRA PRADESH KARNATAKA 16° Panji GOA 12° REFERENCES Bangaluru H.P. - HIMACHAL PRADESH Chennai D&D - DAMAN & DIU D&NH - DADAR & NAGAR HAVELI Port Blair 12° Puducherry Mahe ( Puducherry) TAMIL NADU Karaikal KER Kavaratti ALA Andaman & Nicobar Islands (INDIA) 8° Lakshadweep (INDIA) Thiruvananthapuram 200 0 200 400 8° SRI Kilometres LANKA I N D I A N O C E A N 72° 76° 84° 88° 92° Figure 9.3 Political Map of India SOCIAL SCIENCE 197 MODULE - 2 Physiography of India India: Natural Environ- ment, Resources and This map clearly indicates that each state and union territory has its own capital. It Development is interesting to note that while New Delhi is the capital of India, Delhi is the capital of Union Territory Delhi. Can you identify any other capital like this? Yes, it is Chandigarh which is the capital of two states Haryana and Punjab and also a Union Territory. Notes ACTIVITY 9.1 Find out the minimum number of states you need to across, if you want to move between the following places. (Refer Fig. 9.5) (a) Kashmir to Mizoram (b) Punjab to Bihar (c) Delhi to Banglore (d) Mumabi to Kolkata (e) Chennai to Raipur INTEXT QUESTION 9.2 1. Look at the map 9.3 and answer the following questions. (i) Write the names of two States of South India. (ii) Mention the names of two states sharing international boundary. (iii) Write the names of two countries sharing their boundaries with Sikkim. (iv) Write the names of two union territories along Arabian Sea. 9.3 PHYSICAL DIVISIONS OF INDIA Natasha : What is terrain? Tutor : Terrain is an area of land which usually has a particular type of physical feature. Farah : Like, Mumbai beach is sandy and Shillong is a hilly. Teacher : Right. Do you know India is a vast country with varied land forms and topography? Rajinder : What is the meaning of topography? Teacher : Topography means the features of a place determined by nature. It is the description of various features and landscape on the surface of the earth. India has the topographical diversity. This includes the Great Himalayas, the Northern Plain, the Thar desert, the coastal plains and the Peninsular Plateau. The reasons for variation in the topography could be: l Differences in the rock formations. These landmasses have been formed in different geological periods. 198 SOCIAL SCIENCE Physiography of India MODULE - 2 India: Natural Environ- l Number of processes such as weathering, erosion and deposition has modified ment, Resources and Development these features to their present forms. Weathering: Weathering is the process of gradual destruction of rocks at or near the earth’s surface through physical, chemical and biological processes caused by wind water, climate change etc. Notes Erosion: Erosion is the process of gradual transportation of weathered rock materials through natural agencies like wind, river, streams, glaciers etc. Weathering is distinguished from Erosion as no transportation of material is involved in case of weathering. India is a country of physical diversity. There are high mountain peaks in some areas while in others, lie the flat plains formed by rivers. On the basis of physical features, India can be divided into following six divisions: 64° 72° 76° 80° 84° 88° 92° The Pamir KU NL U NM SH TS KU KA. H IND RA 8611 KO 32° RA SH In M IW du INDIA A s 32° Jhelum nab LIK h e RA PHYSICAL C NG a v i E 28° R G 7817 T R ER s ES u E nd D I 28° Yam A N GE IA T Mt. Everest D u Ga AN IN 8848 na ng H tra apu NAGA AT a IR 24° Gha I M hm RE ghar Bra bal a Gan AL A G am da L A Y A JAINTIA AV Ch twa k Ko Be GARO KHASI AR si 24° Rann of Kachchh Malwa Plateau A Chota Nagpur Plateau 20° Narmada UR TP Gir Hills SA Mahanadi Tapi Mouth of the Ganges 20° W God Chattisgarh ava S ri E T 16° A D E C C A N S H BAY T G Krishna OF 16° N E ARABIAN BENGAL R SEA R E 12° N T ALTITUDE SCALE Meters S 12° G Above 1200 A Nilgiri Hills 2637 600 - 1200 H E v eri 300 - 600 A T Ka Below 300 ANDAMAN & NICOBAR 8° LAKSHADWEEPS ISLANDS 200 0 200 400 8° S Kilometres SRI I N D I A N LANKA O C E A N 72° 76° 84° 88° 92° Figure 9.4 Physiographic Divisions of India SOCIAL SCIENCE 199 MODULE - 2 Physiography of India India: Natural Environ- ment, Resources and 1. The Northern mountains 2. The Northern Plains Development 3. The Peninsular Plateau 4. The Indian Desert 5. The Coastal Plains 6. The Islands. 1. The Northern Mountain : It is divided into three groups. They are : (i) The Himalayas Notes (ii) The Trans Himalayas (iii) The Puranchal hills 1. Pass: It is a natural gap or a route between a ridge, hill. 1. The Himalayan Mountains 2. Range: large landmass consisting of Himalayas are the young fold mountains. mountains, ridges and peaks. This is the highest mountain range of the world. Himalayas act as natural 3. Peak: highest point or tip of a barrier. The extreme cold, snow and mountain range. rugged topography discourage the 4. Valley: a depression or a flat land neighbors to enter India through between two elevated areas. Himalayas. They run from west-east direction from Indus to Brahmaputra 5. Dun: Longitudinal valleys existing along the northern boundary of India beween himachal and shiwaliks. 64° 68° The Pamir 72° 76° 80° 84° 92° KU AJ NL UR UN H ND Rakaposhi MT S HI S. D KU 7788 Ka ra HIN Harmosh 7397 ko Aghil ra Pass K2 m 8126 8611S Hi lls Karakoram Pass Naga Parwat G hy ok Khyber Pass La da Za R kh Ra s ka ng rR e an E ge lum 200 0 200 400 Jhe Bara KA S n ab h Lacha Kilometres A IL he iw AS C a H li Shipkila RA L k E NG T GE S R Kamet Kailash E S i a Rav RAN n 6714 A g 7750 Mansa rover Lake R e H I M 7817 AN j Namcha tlu E Sa A Nanda Devi Barwa EM L 7756 A SUL Y A R Tsangpo s du In Annapurna Ga S h 8078 H 8848 Mt. Everest A n ga i w a l I Bomdila Y Ya i k R a M A L A m n g Kanchenjunga a un e 8598 putr a hma Bra Tis ta Ga i Go as Lun l Gh an m n ba da ti a M am gh k Ch ara nd Kos Si i et wa B n Ke Rann of Kutch Son Figure 9.5 The Himalyan Mountains 200 SOCIAL SCIENCE Physiography of India MODULE - 2 India: Natural Environ- covering a distance of 2500 KM. Their width varies from 400 in the west and 150 ment, Resources and KM in the East (Fig. 9.5). The Himalayas may be divided into three parallel ranges: Development (a) Greater Himalayas or Himadari (b) Lesser Himalayas or Himachal (c) Outer Himalayas or Siwaliks. Notes (a) The Greater Himalayas or Himadari: The Greater Himalayas comprises of the northern most ranges and peaks. It has an average height of 6000 metres and width lies between 120 to 190 Kms.It is the most continuous range. It is snow bound and many glaciers descend from this range. It has high peaks like Mt. Everest, Kanchenjunga, Makalu, Dhaulagiri, Nanga Parbat etc. having a height of more than 8000 metres. Mt. Everest (8848 m) is the highest peak of the world and Kanchenjunga is the highest peak of Himalaya in India. High Mountain passes also exist in this range, namely, Bara Lacha-La, Shipki-La, Nathu-La, Zoji-La, Bomidi-La etc. The Ganga and Yamuna rivers originates from this Himalayas. (b) The Lesser Himalayas or Himachal: The altitude of this range lies between 1000 and 4500 metres and the average width is 50 KM. The Prominent ranges in this are Pir Panjal, Dhaula Dhar and Mahabharata ranges.It compresses of many famous hill stations like Shimla, Dalhousie Darjeeling, Chakrata, Mussoorie, Nanital etc. It also comprises of famous valleys like Kashmir, Kullu, Kangra etc. (c) The Outer Himalayas or the Siwaliks: It is the outer most range of the Himalayas. The altitude varies between 900-1100 meters and the width lies between 10-50 KM. They have low hills like Jammu Hills, etc.The valleys lying between Siwalik and Lesser Himalayas (Himachal) are called ‘Duns’ like Dehra Dun, Kotli Dun and Patli Dun. (ii) The Trans-Himalayan ranges It extends north of greater Himalaya and parallel to it is called zaskar range. North of Zaskar range lies Ladakh range. The Indus river flows between Zaskar and Ladakh range. The Karakoram range lie extreme north of the country. K2 is the second highest peak of the world. (iii) The Purvanchal hills It comprises Mishami, Patkoi, Naga, Mizo hills which are located in eastern side. The Meghalaya plateau is also part of these hills which includes the hills of Garo, Khasi and Jaintia. SOCIAL SCIENCE 201 MODULE - 2 Physiography of India India: Natural Environ- ment, Resources and Development INTEXT QUESTIONS 9.3 1. Write the names of the three ranges of the Himalayas. 2. Look at the map (Fig. 9.5) and find out. Notes (i) In which state Nanga Parbat and Nanda Devi are located? (ii) Say Yes or No. (a) Mt. Everest is located in India……………………… (b) Shipki-La pass is located in Siwalik Range…………… (c) Mansarover lake is located in Kailash Range………... 3. Mention the names of the countries in which the Greater Himalayas are situated. 4. Identify two purvanchal hills. 2. The Northern Plains Let us try to locate and label the states lying in the Northern Plains of India (refer Fig. 9.5. The Northern Plains are located between south of the Himalayas and north of the Peninsular plateau. It is formed by the deposition of the sediments brought by three main river systems namely : the Indus, the Ganga and the Brahmaputra. From Punjab in the west to Assam in the east, this plain is about 2400 km long. Its width varies from about 300 km in the west to about 150 km in the east. It mainly includes the states of Punjab, Haryana, Uttar Pradesh, Bihar, West Bengal and Assam. This plain is very fertile due to alluvial sediments brought by the rivers from the Himalayas. This plain is one of the largest and most fertile plains of the world. Major crops such as wheat, rice, sugarcane, pulses, oil seeds and jute are grown here. Due to proper irrigation, the plain makes significant contribution in the production of food grains. The Northern plain is broadly divided into two parts : (a) The Western plain (b) The Ganga-Brahmaputra plain (a) The Western Plain This plain is formed by the river system of the Indus. It lies to the west of Aravallis. This plain is formed due to deposits brought by the rivers like the Satluj, the Beas and the Ravi. This part of the plain has doabs. (b) The Ganga-Brahmaputra plain It is also formed by the deposition of the sediments brought by two main river systems, the Ganga and the Brahmaputra. The early civilizations like Mohenjo-Daro and 202 SOCIAL SCIENCE Physiography of India MODULE - 2 India: Natural Environ- Harappa also called river valley civilizations, were spread over plain areas. This is ment, Resources and Development because of the availability of fertile land and water through the river networks. Doab: the alluvial land between two converging rivers. Example doab area in Punjab. Khadar: The area flooded by rivers almost every year Notes Banger: The area never flooded by rivers. 3. The Peninsular Plateau Look at the map (Fig. 9.6) given below, you will find that the Peninsular plateau is a triangular shaped table land. It is part of ancient land mass called Gondwana level. It covers an area of nearly 5 lakh sq.km. It is spread over the states of Gujarat, Maharashtra, Bihar, Karnataka and Andhra Pradesh. 72°E 76° 80° 84° 88° 28°N 28°N Ya m un l a Ga ba Luni m n a ga Ch AN Gan a tw g TH S a Be ILL AS IH AJ AL BUNDEL Son R 24° AV 24° AR KHAND ati hi MALWA PLATEAU Ma arm YA VINDH Sab CHOTA NAGPUR N GE PLATEAU Narmada RA GIR RANGE RA LA Tapi SATPU IKA MA RH GA TIS 20° AT Mahanadi SATMALA CH 20° HILLS G oda vari S BA MAHENDRA GIRI T LA A GH AT H W Kr R AN G ish GE E na S T E 16° U EA 16° AT a PL dr R ha NA BAY gb ARABIAN A N n NG OF Tu SEA LE Panneru M BENGAL TE T N A L AS E R CO A B S T GH 12° EL 12° AT A R E A ND S MA ANNAMALAI C HILLS Kaveri RO 0 100 200 300 400 500 O CO A S Kilometres CARDAMOM HILLS T I N D I A N O C E A N 8° 8° 72°E 76° 80° 84° Figure 9.6 The Peninsular plateau of India SOCIAL SCIENCE 203 MODULE - 2 Physiography of India India: Natural Environ- ment, Resources and River Narmada divides the peninsular plateau into two parts : The central highlands Development and Deccan Plateau (i) The central Highlands: It extends from Narmada river and the northern plains. A ravallis is the important mountain which extends from Gujrat through Rajasthan to Delhi. The highest peak of the Aravallis hills is Gurushikhar (1722m) near Notes Mt. Abu. The Malwa Plateau and Chhota Nagpur plateau are parts of the central highlands. River Betwa, chambal and Ken are the important river of Malwa plateau while Mahadeo, Kaimur and Maikal are the important hills of chhota Nagpur plateau. The valley of Narmada is lies between the Vindhyas and the satpura which flows east to west and joins the Arabian sea. (ii) The Deccan Plateau: The Deccan plateau is separated by a fault (A fracture in the rock along which rocks have been relatively replaced), from Chota Nagpur plateau. The black soil area in the Deccan plateau is known as Deccan trap. It is formed due to volcanic eruptions. This soil is good for cotton & sugarcane cultivation. The Deccan plateau is broadly divided into: (a) The Western Ghats (b) The Eastern Ghats (a) The Western Ghats: If you look at map (Fig. No. 9.6), we will see the Western Ghats or Sahyadris lie on the Western edge of the Deccan plateau. It runs parallel to the western coast for about 1600 km. The average elevation of the Western Ghats is 1000 metres. The famous peaks in this area are Doda Betta, Anaimudi amd Makurti. The highest peak in this region is Anaimudi (2695m.). Western ghats are continuous and can be crossed through passes like Pal Ghat, Thal Ghot and Bhor Ghat. The rivers like Godavari, Bhima and Krishna flow eastward while the river Tapti flows westward. The streams form rapids & water falls before entering the Arabian Sea. The famous water falls are Jogfalls on Sharavati, Shiva Samudram falls on Kaveri etc. (b) The Eastern Ghats: The Eastern Ghats are discontinuous low belt. Their average elevation is 600 m. They run parallel to the east coast from south of Mahanadi valley to the Nilgiri hills. The highest peak in this region is Mahendragiri (1501 m). The famous hills are Mahendragiri hills, Nimaigiri hills in Orissa, Nallamallai hills in Southern Andhra Pradesh, Kollimalai and Pachaimalai in Tamilnadu. The area is drained by the Mahanadi, Godawari, Krishna and Kaveri river systems. The Nilgiri hills join Western & Eastern Ghats in the south. 204 SOCIAL SCIENCE Physiography of India MODULE - 2 India: Natural Environ- ment, Resources and Development ACTIVITY 9.2 Trace five main differences between Western and Eastern Ghats. 1. Continuity Notes 2. Average Elevation 3. Extent 4. Highest Peak 5. Rivers 4. The Indian Desert The Indian Desert lies towards the western margin of Aravali Hills. It is also called Thar Desert. It is the ninth largest desert in the world. It spreads over the states of Gujarat and Rajasthan. This region has semi-arid and arid weather conditions. It receives less than 150 mm of rainfall per year. The vegetation cover is low with thorny bushes. Luni is the main river in this area. All other streams appear only at the time of rainfall otherwise they disappear into the sand. Figure 9.7 The Indian Desert I am Thar ‘The Indian Desert’: 1. I remain dry most of the year. The moisture bearing winds goes parallel to Aravalli so I receive scanty rainfall. 2. I am pierced by cactus and other thorny bushes on my body. 3. If you are thirsty, you will have to walk several kilometers to reach an oasis and sinduates (small water body). SOCIAL SCIENCE 205 MODULE - 2 Physiography of India India: Natural Environ- ment, Resources and 4. The sand dunes add to the beauty of my desert. Development 5. My people follow rich cultures and traditions. 5. The Coastal Plains The coastal plains in India run parallel to the Arabian Sea & Bay of Bengal along Notes the Peninsular Plateau.The western coastal plain is a narrow belt along the Arabian sea of about 10-20km wide. It stretches from Rann of Kachchh to KanyaKumari. Western coastal plains comprises of three sectors (i) Konkan Coast (Mumbai to Goa), (ii) Karnataka coast from Goa to Mangalore (iii) Malabar Coast (Mangalore to Kanya Kumari). The eastern coast runs along Bay of Bengal. It is wider than the western coastal plain. Its average width is about 120Kms. The northern part of the coast is called Northern Circar and the southern part is called Coromandal Coast. Eastern coastal plain is marked by Deltas made by the rivers Mahanadi, Godavari, Krishna amd Kaveri. The Chilka largest salt water lake in India in Odisha is located to the south of Mahanadi Delta. The coastal plains are belts for growing spices, rice, coconut, pepper etc. They are centres of trade & commerce. The coastal areas are known for fishing activities, therefore large number of fishing villages have developed along the coasts. Vembanad is famous lagoon which is located at Malabar coast. 6. The Islands India has two main groups of Islands. There are 204 islands in Bay of Bengal called as Andaman and Nicobar islands and 43 islands in Arabian Sea called as Lakshadweep islands The Andaman & Nicobar island extend from north to south in Bay of Bengal. They are bigger in size. An active volcano is located on the Barren Island in Andaman & Nicobar group of islands. Lakshadweep islands are located near Malabar coast of Kerala in the Arabian sea. They cover an area of 32 sq km. Kavarati is the capital of Lakshdweep. These islands are formed by corals and endowed with variety of flora and fauna. These islands are important tourist attraction under water activities like snokling, such diving, deep sea diving and other sports make these island more popular. INTEXT QUESTIONS 9.4 1. Answer the following questions briefly (not more than two sentences) (i) How was Deccan Trap formed? (ii) State any two economic activities of coastal plains. (iii) Why does Andman and Nicobar Islands attract more tourists? (iv) Write the names of the rivers which help to form the western plain. 206 SOCIAL SCIENCE Physiography of India MODULE - 2 India: Natural Environ- ment, Resources and 9.4 DRAINAGE SYSTEMS IN INDIA Development The drainage system refers to the system of flow of surface water mainly through rivers. An area drained by a river and its tributaries is called a drainage basin. The drainage system is related to a number of factors like slope of land, geological structure, amount and velocity of water. A river through its drainage system performs several tasks. These are excess water removal from a particular area, transportation Notes of sediments from one place to other, providing natural source for irrigation and maintaining the water table of a region. Traditionally, rivers were useful as a source of abundant fresh water and navigation. In today’s world rivers importance has risen to include hydro power generation and setting up water-based industries. These are also important tourist attraction for activities such as boating, river rafting and cliff jumping. Because of their utility, rivers are important for life and hence regarded as lifeline. Many cities are located along the rivers and are densely populated. Delhi on the banks of Yamuna, Patna along Ganga, Guwahati along Brahmaputra, Nasik along Godavari and Cuttack along Mahanadi are some examples (Fig. 9.8). On the basis of the origin the drainage can be divided in to two parts: (a) The Himalayan drainage system (b) The Peninsular drainage system Tributary: A stream or river that flows into a larger river. e.g. Yamuna Delta: A triangular shaped land at the mouth of a river formed from the deposition of silt, sand and small rocks that flow downstream in the river. eg. Ganga delta. Estuary: A partially enclosed coastal body of water where the salty tidal water mixes with the fresh water of the river. eg. Narmada river makes an estuary. 9.5 MAJOR DRAINAGES SYSTEMS As mentioned earlier on the basis of origin, the Indian river have been classified into two major drainage systems. Let us discuss the comparision between the two drainage systems. Himalayan River System 1. They are Perennial rivers originating from glaciers. 2. Rivers form valleys by the process of erosion. 3. The rivers are ideal for irrigation purposes as they pass through plain fertile tracts. 4. These rivers have meandering courses which shift over time. 9.5.1 The Himalayan Drainage System Most of the Himalayan Rivers are perennial. This means they have water throughout the year. This is because most of these rivers originate from the glaciers and snowy SOCIAL SCIENCE 207 MODULE - 2 Physiography of India India: Natural Environ- ment, Resources and peaks. They also receive water from the rainfall. The main river system in this category Development are: 1. The Indus River System Jhelum, Ravi, Beas and Satluj 2. The Ganga Rivers System Yamuna, Ramganga, Ghaghara, Gomti, Gandak and Kosi etc. Notes 3. The Brahmaputra River System Dibang, Lohit, Tista and Meghna etc. 9.5.2 The Peninsular Drainage System You have already studied about Peninsular Plateau. Most of the Peninsular rivers flow eastwards and enters into Bay of Bengal. Only Narmada and Tapi rivers which flow westwards of the Western Ghats. They are good for generating hydropower because these rivers form rapids & water falls. The major peninsular rivers are Mahanadi, Godavari, Krishna and Kaveri. 64° 68° 72° 76° 80° 84° 88° 92° 32° Ind us R. INDIA 32° Ch en MAJOR RIVERS ab R. R. m elu R. vi Jh 28° Ra. uj R Satl. 28° u sR Ind Ya R. m 24° un tra aR pu. ma ah G R. Br an bal ga am R. Ch

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