Current Affairs UPSC

Drainage System   A river drains the water collected from a specific area, which is called its 'catchment area'.   The flow of water through well-defined channels is known.as 'drainage' and the network of such channels is called a 'drainage system'. The drainage pattern of an area is the outcome of the geological time period, nature and structure of rocks, topography, slope, amount of water flowing and the periodically of the flow.   An area drained by a river and its tributaries is called a drainage basin. The boundary line separating one drainage basin from the other is known as the watershed. The catchments of large rivers are called river basins while those of small rivulets and rills are often referred to as watersheds. There is however, a slight difference between a river basin and a watershed. Watersheds are small in area while the basins cover larger areas.   Indian drainage system may be divided on various bases. On the basis of discharge of water (orientations to the sea), it may be grouped into: (i) the Arabian Sea drainage/- and (ii) the Bay of Bengal drainage. They are separated from each other through the Delhi ridge, the Aravalis and the Sahyadris (water divide is shown by a line in Figure. Nearly 77 per cent of the drainage area consisting of the Ganga, the Brahmaputra, the Mahanadi, the Krishna, etc. is oriented towards the Bay of Bengal while 23 per cent comprising the Indus, the Narmada, the Tapi, the Mahi and the Periyar systems discharge their waters in the Arabian Sea.   On the basis of the size of the watershed, the drainage basins of India are grouped into three categories: (i) Major river basins with more than 20/000 sq. km. of catchment area. It includes 14 drainage basins such as the Ganga, the Brahmaputra, the Krishna, the Tapi, the Narmada, the Mahi, the Pennar, the Sabarmati, the Barak, etc. (ii) Medium river basins with catchment area between 2,000- 20,000 sq. km. incorporating 44 river basins such as the Kalindi, the Periyar/ the Meghna, etc. (iii) Minor river basins with catchment area of less than 2,000 sq. km. include fairly good number of rivers flowing in the area of low rainfall.   The Narmada and Tapi are two large rivers which are exceptions. They along with many small rivers discharge their waters in the Arabian Sea.   On the basis of the mode of origin, nature and characteristics, the Indian drainage may also be classified into the. Himalayan drainage and the peninsular drainage. Although it has the problem of including the Chambal, the Betwa, the Son, etc. which are much older in age and origin than other rivers that have their origin in the Himalayas/ it is the most accepted basis of classification.   Drainage systems of India Indian drainage system consists of a large number of small and big rivers. It is the outcome of the evolutionary process of the three major physiographic units more...

 Climate   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). 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. You may have observed that the weather conditions fluctuate very often even within a day. But there is some common pattern over a few weeks or months/ i.e. days are cool or hot/ windy or calm/ cloudy or bright/ and wet or dry. On the basis of the generalized monthly atmospheric conditions/ the year is divided into seasons such as winter/ summer or rainy seasons.   During the summer season the desert area of Rajasthan witnesses 50° temperature whereas Pahalgam sector of Jammu and Kashmir has 20°C temperature. During winter nights Dras sector of Jammu and Kashmir witnesses- 45°C temperature where as Thiruvananthapuram has 20°C.   Rainfall also varies in terms of quantity and distribution in the regions of Himalaya rainfall is in the from of snowy balls where .as in the rest of part of India it is a general rain. Again annual rainfall varies from 400°C in the Meghalya to 10°c in Ladakh and West Rajasthan. In the coastal area the variation of rainfall is less. Whereas in the inner part of country the seasonal variation is more. Accordingly the Indians show their unity in diversity in terms of food, clothing, housing and culture. Factors determining the climate of India India's climate is controlled by a number of factors which can be broadly divided into two groups- (a) factors related to location and relief/ and (b) factors related to air pressure and winds.   (a)        Factors related to Location and Relief Latitude: You know that the Tropic of Cancer passes through the central part of India in east-west direction. This/ northern part of the India lies in sub-tropical and temperate zone and the part lying south of the Tropic of Cancer falls in the tropical zone. The tropical zone being nearer to the equator/ experiences high temperatures throughout the year with small daily and annual range. Area north of the Tropic of Cancer being away from the equator/ experiences extreme climate with high daily and annual range of temperature.   The Himalayan Mountains: The towering mountain chain provides an invincible shield to protect the subcontinent from the cold northern winds. The Himalayas also trap the monsoon winds/ forcing them to shed their moisture within the subcontinent. Distribution of Land and Water: India is flanked by the India Ocean on three sides in the south and girdled by a high and continuous mountain-wall in the north. As compared to the landmass, water heats up or cools down slowly. This differential heating of land and sea creates different air pressure zones in different seasons in and around the Indian subcontinent. Difference in more...

 Natural Vegetation   Natural vegetation refers to a plant community that has been left undisturbed over a long time. So as to allow its individual Species to adjust themselves to climate and soil conditions as fully as possible.   India is a land of great variety of natural vegetation. Himalayan heights are marked with temperate vegetation; the Western Ghats and the Andaman Nicobar Islands have tropical rain forests, the deltaic regions have tropical forests and mangroves; the desert and semi desert areas of Rajasthan are known for cacti/ a wide variety of bushes and thorny vegetation. Depending upon the variations in the climate and the soil, the vegetation of India changes from one region to another.   On the basis of certain common features such as predominant vegetation type and climatic regions, Indian forests can be divided into the following groups:   Types of Forests             (i)Tropical Evergreen and Semi Evergreen forests             (ii) Tropical Deciduous forests             (iii) Tropical Thorn forests             (iv) Montane forests             (v) Littoral and Swamp forests.   Tropical Evergreen and Semi Evergreen Forests             These forests are found in the western slope of the Western Chats, hills of the northeastern region and the Andaman and Nicobar Islands. They are found in warm and humid areas with an annual precipitation of over 200 cm and mean annual temperature above 22°C. Tropical evergreen forests are well stratified, with layers closer to the ground and are covered with shrubs and creepers, with short structured trees followed by tall variety of trees. In these forests, trees reach great heights up to 60 m or above. There is no definite time for trees to shed their leaves, flowering and fruition. As such these forests appear green all the year round. Species found in these forests include rosewood, mahogany, aini, ebony, etc.   The semi evergreen forests are found in the less rainy parts of these regions. Such forests have a mixture of evergreen and moist deciduous trees. The under growing climbers provide an evergreen character to these forests. Main species are white cedar, hillock and kail.   The British were aware of the economic value of the forests in India, hence, large scale exploitation of these forests was started. The structure of forests was also changed. The oak forests in Garhwal and Kumaon were replaced by pine (chirs) which was needed to lay railway lines. Forests were also cleared fur introducing plantations of tea, rubber and coffee. The British also used timber of construction activities as it acts as an insulator of heat. The protection use of forests was, thus, replaced by commercial use.   Tropical Deciduous Forests These are the most widespread forests in India. They are also called the monsoon forests. They spread over regions which receive rainfall between 70-200 cm. On the basis of the availability of water, these forests are further divided into moist and dry deciduous. The Moist deciduous forests are more pronounced in more...

  Soil   Soil is the most important layer of the earth's crust. It is a valuable resource. Soil is the mixture of rock debris and organic materials which develop on the earth's surface. The major factors affecting the formation of soil are relief, parent material, climate/ vegetation and other life-forms and time. Besides these, human activities also influence it to a large extent. Components of the soil are mineral particles, humus, water and air. The actual amount of each of these depend upon the type of soil. Some soils are deficient in one or more of these, while there are some others that have varied combinations.             If we dig a pit on land and look at the soil, we find that it consists of three layers which are called horizons. 'Horizon A' is the topmost zone, where organic materials have got incorporated with the mineral matter, nutrients and water, which are necessary for the growth of plants. 'Horizon B' is a transition zone between the 'horizon A' and 'horizon C', and contains matter derived from below as well as from above. It has some organic matter in it, although the mineral matter is noticeably weathered. 'Horizon C' is composed of the loose parent material. This layer is the first stage in the soil formation process and eventually forms the above two layers. This arrangement of layers is known as the soil profile. Underneath these three horizons is the rock which is also known as the parent rock or the bedrock. Soil, which is a complex and varied entity, has always drawn the attention of the scientists.   Classification of Soils India has varied relief features, landforms, climatic realms and vegetation types. These have contributed in the development of various types of soils in India.   On the basis of genesis, colour, composition and location, the soils of India have been classified into: (i) Alluvial soils, (ii) Black soils, (iii) Red and Yellow soils, (iv) Laterite soils, (v) arid soils, (vi) Saline soils, (vii) Peaty soils, (viii) Forest soils.   ICAR has classified the soils of India into the following order as per the USDA soil taxonomy    
Sr. No. Order Area (In Thousand Hectares) Percentage
(i)      Inceptisols   more...
 Land Use and Agriculture   Different types of lands are suited to different uses. Human beings thus/ use land as a resource for production as well as residence and recreation.   Land-use records maintained by land revenue department. The land use categories add up to reporting area, which is somewhat different from the geographical area. The Survey of India is responsible for measuring geographical area of administrative units in India. The difference between the two concepts are that while the former changes somewhat depending on the estimates of the land revenue records/ the latter does not change and stays fixed as per Survey of India measurements. The land-use categories as maintained in the Land Revenue are as follows:             (i)         Forests: It is important to note that area under actual forest cover is different from area classified as forest. The latter is the area which the Government has identified and demarcated for forest growth. The land revenue records are consistent with the latter definition. Thus/ there may be an increase in this category without any increase in the actual forest cover.             (ii)         Land put to Non-agricultural Uses: Land under settlements (rural and urban)/ infrastructure (roads, canals, etc.), industries, shops, etc. are included in this category. An expansion in the secondary and tertiary activities would lead to an increase in this category of land-use. (iii)        Barren and Wastelands: The land which may be classified as a wasteland such as barren hilly terrains, desert lands, ravines, etc. normally cannot be brought under cultivation with the available technology.             (iv)        Area under Permanent pastures and Grazing Lands: Most of this type land is owned by the village 'Panchayat' or the Government. Only a small proportion of this land is privately owned. The land owned by the village panchayat comes under   'Common   Property Resources'.             (v)        Area under Miscellaneous Tree Crops and Goves (Not included is Net sown Area): The land under orchards and fruit trees are included in this category. Much of this land is privately owned.             (vi)        Culturable Waste-Land: Any land which is left fallow.(uncultivated) for more than five years is included in secondly, since even the reporting area has been relatively constant over the years, a decline in one category usually leads to an this category. It can be brought Si under cultivation after improving it b through reclamation practices,       (vii)       Current Fallow: This is the land which is left without cultivation for one or less than one agricultural year, Fallowing is a, cultural practice adopted for giving the land rest. The: land recoups the lost fertility through natural processes.             (viii)      Fallow other than Current Fallow: This is also a cultivable land which is left uncultivated for more than five years/ it would be categorized as culturable wasteland.              (ix)        Net Area Sown: The physical extent of land on which crops are sown and harvested is known as net sown area.   Land-use Changes in more...

  Mineral and Energy Resources             India is endowed with a rich variety of mineral resources due ‘to its varied geological structure. Bulk of the valuable minerals are products of pre-Paleozoic age mainly associated with metamorphic and igneous rocks of the peninsular India. The vast alluvial plain tract of north India is devoid of minerals of economic use.               The mineral resources provide the country with the necessary base for industrial development. The availability of various types of mineral and energy resources in the country.   Mode of Occurrence of Minerals Minerals generally occur in these forms: (i)         In igneous and metamorphic rocks minerals may occur in the cracks/ crevices, faults or joints. The smaller occurrences are called veins and the larger are called lodes. In most cases, they are formed when minerals in liquid/molten and gaseous forms are forced upward through cavities towards the earth's surface. They cool and solidify as they rise. Major metallic minerals like tin, copper, zinc and lead etc. are obtained from veins and lodes. (ii)         In sedimentary rocks a number of minerals occur in beds or layers. They have been formed as a result of deposition, accumulation and concentration in horizontal strata. Coal and some forms of iron ore have been concentrated as a result of long periods under great heat and pressure. Another group of sedimentary minerals include gypsum. Potash salt and sodium salt. These are formed as a result of evaporation especially in arid regions. (iii)        Another mode of formation involves the decomposition of surface rocks, and the removal of soluble constituents, leaving a residual mass of weathered material containing ores. Bauxite is formed this way. (iv)        Certain minerals may occur as alluvial deposits in sands of valley floors and the base of hills. These deposits are called 'placer deposits' and generally contain minerals, which are not corroded by water. Gold, silver, tin and platinum are most important among such minerals. (v)        The ocean waters contain vast quantities of minerals, but most of these are too widely diffused to be of economic significance. However, common salt/ magnesium and bromine are largely derived from ocean waters. The ocean beds, too, are rich in manganese nodules.   Rat-Hole Mining. Do you know that most of the minerals in India are nationalized and their extraction is possible only after obtaining due permission from the government? But in most of the tribal areas of the north-east India, minerals are owned by individuals or communities. In Meghalaya, there are large deposits of coal, iron ore, limestone and dolomite etc. Coal mining in Jowai and Cherapunjee is done by family member in the form of a long narrow tunnel, known as 'Rat hole' mining.   Agencies Involved in the exploration of minerals In India, systematic surveying, prospecting and exploration for minerals is undertaken by the Geological Survey of India (GSI), Oil and Natural Gas Commission (ONGC), Mineral Exploration Corporation Ltd. (MECL), National Mineral Development Corporation (NMDC), Indian Bureau of Mines more...

  Sugar Industry     The sugar industry is the second most important agro-based industry in the country. India is the largest producer of both sugarcane and cane sugar and contributes about 8 per cent of the total sugar production in the world. Besides, khandasari and gur or jaggery are also prepared from sugarcane. This industry provides employment for more than 4 lakh persons directly and a large number of farmers indirectly. Sugar industry is a seasonal industry because of the seasonality of raw materials.   Development of the industry on modern lines dates back to 1903, when a sugar mill was started in Bihar. Subsequently, sugar mills were started in other parts of Bihar and Uttar Pradesh. In 1950-51,139 factories were in operation producing 11.34 lakh tons of sugar. The number of sugar factories rose to 506 and production to 176,99 lakh tones in. 2000-01.   Location of the Sugar Industry Sugarcane is a weight-losing crop. The ratio of sugar to sugarcane varies between 9 to 12 per cent depending on its variety. Its sucrose content begins to dry during haulage after it has been harvested from the field. Better recovery of sugar is dependent upon its being crushed within 24 hours of its harvesting. Sugar factories hence, are located within the cane producing regions.   Maharashtra has emerged as a leading sugar producer in the country and produces more than one-third of the total production of the sugar in the country. There are 119 sugar mills in the state in a narrow belt extending from Manmad in the north to Kolhapur- in me south. There are 87 mills in the cooperative sector.   Uttar Pradesh is the second largest producer of sugar. The sugar factories are concentrated in two belts-the Ganga-Yamuna doab and the taria region. The major sugar producing centres in- the Ganga- Yamuna doab are Saharanpur, Muzaffarnagar, Meerut, Ghaziabad Baghpat and Bulandshehr districts; 'while Kheri Lakhimpur, Basti, Gonda, Gorakhpur, Bahraich are important sugar producing districts in me Tarai region.   In Tamil Nadu, sugar factories are located   in, Coimbatore, Vellore Tiruvanamalai, Villupuram and. Tiruchchirappalli districts. Belgaum, Bellary, Mandya, Shimoga, Bijapur, and Chitradurg districts are the major producers in Karnataka. The industry is distributed in the coastal regions i.e. East Godawari, West, Godavari, Vishakhapatnam districts and Nizamabad, and Medak districts of Telangana along with Chittoor district of Rayalseema;   The other States which produce sugar are Bihar, Punjab Haryana, Madhya Pradesh and Gujarat.  Saran Chainparan, Muzaffarnagar Siwan Darbhanga, and Gaya are -the important, sugarcane producing districts in Bihar the relative significance of. Punjab has declined, although Gurdaspur Jalandhar, Sangartir, Patiala and Amritsar are major sugar ‘producers. In Haryana, sugar factories, are located in Yamuna Nagar, Rohtak, Hissar and Faridabad districts. Sugar industry is comparatively new in Gujarat. Sugar mills are. Located in the carie growing tracts of Surat, Jamnagar Rajkot, Amreli Valsad and Bhavnagar districts.   Petrochemicai Industries This group of industries has been growing very fast in India. A variety more...

 Transport and Communication   The use of transport and communication depends upon our need to move things from place of their availability to the place of their use.   Land Transport Road Transport: India has .one of the largest road networks in the world with a total length. Of 33.1 lakh km (2005). About 85 per Cent of passenger and 70 per cent of freight traffic are carried by roads every year. Road transport is relatively suitable for shorter distance travel.   Road transport in modern sense was very limited in India before World War-11. The first serious attempt was made in 1943 when 'Nagpur Plan' was drawn. This plan could not be implemented; due to lack of coordination among the princely states and British India. After Independence/twenty- year road plan (1961:) was introduced to. improve the conditions of roads in India. However/ roads continue to concentrate in and around urban centers. Rural and remote areas had the least connectivity by road.   For the purpose of construction and maintenance/ roads are classified as National Highways (NH)/ State Highways (SH)/ Major District Roads and Rural Roads:   National Highways: The main roads which are constructed and maintained by the Central Government are known as the National Highways. These roads are meant for inter-state transport and movement of defence men and material in strategic areas. These also connect the state capitals/ major cities/ important ports/ railway junctions/ etc. The length of the National Highways has increased from 19/700 km in 1951 to 65,769 km in 2005. The National Highways constitute only two per cent of the total road: length but carry 40 per cent of the road traffic.   The National Highways Authority of India (NHAI) was operationalized in 1995. It is an autonomous body under the Ministry of Surface Transport. It is entrusted with the responsibility of development/ maintenance and operation of National Highways. This is also the apex body to improve the .quality of the roads designated as National Highways.   Indian Road Network (2005)  
Sr. No. Road No. Length in Category more...
  Our Solar System   Our Solar system consists. Of eight planets. The nine planet 2003 UB313 has also been recently sighted. The nebula from which our Solar system is supposed to have been formed, started; its collapse and core formation sometimes 5-5.6 billion ago and the planets formed about 4.6 billion years ago. Our solar system consists of the sun (the star), 8 planets 63 moons, millions of smaller bodies like asteroids and comets and huge quantity of dust-grams and gases.   A light year is a measure of distance and not of time, Light travels at a speed of 300, 00 km/ second. Considering ‘this, the distances the light will travel in' one year is taken to be one light year this equals to 9.461x1012 km; the mean distance between the sun and the earth is 149,598,000 km in terms of light years, it is 8.311 minutes of a year. Out of the eight planets, mercury, Venus, earth and mars are called as the inner planets as the lie between the sun and the belt of asteroids the other five planets are called the outer planets. Alternatively, the first four are called Terrestrial, meaning earth-like as they are made up of rock and metals, and have relatively high.' densities. The rest five are called Jovian or Gas Giant planets. Jovian means Jupiter-like. Most of them are much larger than the terrestrial planets and have thick atmosphere, mostly of helium and hydrogen. All the planets were formed in the same period sometime about 4.6 billion years ago. Some data regarding our solar system are given in the box below.  
The Solar System
  Mercury Venus Earth Mars Jupiter more...
 Composition and Structure of Atmosphere     Composition and Structure of Atmosphere Atmosphere is a mixture of different gases and it envelopes the earth all round. It contains life-giving gases like oxygen for humans and animals and carbon dioxide for plants. The air is an integral part of the earth’s mass and 99 per cent of the total mass of the atmosphere is confined to the height of 32 km from the earth's surface. The air is colorless and odorless and can be felt only when it blows as wind.   Composition of the Atmosphere The atmosphere is composed of gases, water vapor and dust particles. Table shows details of various gases in the air, particularly in the lower atmosphere. The proportion of gases changes in the higher layers of the atmosphere in such a way that oxygen will be almost in negligible quantity at the height of 120 kin. Similarly, carbon dioxide and water vapor are found only up to 90 km from the surface of the earth.  
Constituent Formula Percentage by Volume
Nitrogen \[{{N}_{2}}\] 78.08
Oxygen \[{{O}_{2}}\] 20.95
Argon Ar 0.93
Carbon dioxide \[C{{o}_{2}}\] 0.93
Neon Ne 0.002
Helium He 0.0005
Krypton  Kr 0.001
Xenon Xe 0.00009
Hydrogen \[{{H}_{2}}\] 0.00005
  Gases:    Carbon dioxide is meteorologically a very important gas as it is transparent to the incoming solar radiation but opaque to the outgoing terrestrial radiation. It absorbs a part of terrestrial radiation and reflects back some part of it towards the earth's surface. It is largely responsible for the greenhouse effect. The volume of other gases is constant but the volume of carbon dioxide has been rising in the past few decades mainly because of the burning of fossil fuels. This has also increased the temperature of the air. Ozone is another important component of the atmosphere found between 10 and 50 km above the earth's surface and acts as a filter and absorbs the ultra-violet rays radiating from the sun and prevents them from reaching the surface of the earth.   Water Vapour: Water vapour is also more...


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