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  • [Prelims Spotlight] Important reports and Indices ( Part 1 )

     

    Prelims Spotlight is a part of “Nikaalo Prelims 2020” module. This open crash course for Prelims 2020 has a private telegram group where PDFs and DDS (Daily Doubt Sessions) are being held. Please click here to register.


    26 March 2020

    1.Economics

    Global Economy

    1.Report name – Asian Development Outlook

    Issuing agency – Asian Development Bank

     

    2.Report name – World Economic Outlook

    Issuing agency – International Monetary Fund

     

    3.Report name – Global Economic Prospects

    Issuing agency – World Bank

     

     2.Development

    1.Report name – World Development Report

    Issuing agency – IBRD (World Bank)

     

     2.Report name – Ease of Doing Business

    Issuing agency – IBRD (World Bank)

    Latest in news –India climbed 14 places in the World Bank’s Ease of Doing Business 2020 survey to stand at 63, among 190 countries, making it one of world’s top 10 most improved countries for the third consecutive time.

    To read in detail about the Ease of Business ranking, click here.

     

    3.Report name – Industrial Development Report

    Issuing agency – UNIDO (United Nations Industrial Development Organization)

     

    4.Report name – World Investment Report

    Issuing agency – UNCTAD (United Nations Conference on Trade and Development)

     

    5.Report name – Travel and Tourism Competitiveness Report

    Issuing agency – WEF (World Economic Forum)

     

     6.Report Name – World Cities Report

    Issuing Agency – UN-Habitat

     

    7.Index name – Logistics Performance Index

    Issuing agency – World Bank

     

    3.Global Financial System

    1.Report name – Global Financial Stability Report

    Issuing agency – International Monetary Fund

     

    2.Report name – Global Financial System Report

    Issuing agency – BIS (Bank for International Settlements)

     

    3.Report name – Global Money Laundering Report

    Issuing agency – FATF (Financial Action Task Force)

    2. Environment

    1.Report name – India State of Forest Report

    Issuing agency – Forest Survey of India

    Latest in news –  Click here to read more.

     

    2.Report name – Actions on Air Quality

    Issuing agency – UNEP (United Nations Environment Programme)

     

    3.Report name – Global Environment Outlook

    Issuing agency – UNEP (United Nations Environment Programme)

     

     4.Report name – The Rise of Environmental Crime

    Issuing agency – UNEP & INTERPOL

     

    5.Report name – Global Assessment Report

    Issuing agency – UNISDR (United Nations Office for Disaster Risk Reduction)

     

    6.Report name – The Living Planet Report

    Issuing agency – WWF (World Wildlife Fund)

    Latest in News – With wildlife disappearing at an “unprecedented” pace across the world, the Living Planet Report identifies India as an ecological black spot where around half of the wildlife lives in the danger of being wiped out. The report highlights the pressure on water and lands India faces because of unsustainable human activities. Around 70% of surface water is polluted and 60% of groundwater will reach a critical stage — where it cannot be replenished — in the next decade,

  • [Prelims Spotlight] Environment related Government bodies in India, Important Declarations,

     

    Prelims Spotlight is a part of “Nikaalo Prelims 2020” module. This open crash course for Prelims 2020 has a private telegram group where PDFs and DDS (Daily Doubt Sessions) are being held. Please click here to register.


    25 March 2020

    Government Bodies Related To Environment

    Central Pollution Control Board

    Established: It was established in 1974 under the Water (Prevention and Control of Pollution) Act, 1974.

    Objective: To provide technical services to the Ministry of Environment and Forests under the provisions of the Environment (Protection) Act, 1986.

    Key Functions:

    • Advise the Central Government on any matter concerning prevention and control of water and air pollution and improvement of the quality of air.
    • Plan and cause to be executed a nation-wide programme for the prevention, control or abatement of water and air pollution
    • Coordinate the activities of the State Board and resolve disputes among them
    • Provide technical assistance and guidance to the State Boards, carry out and sponsor investigation and research relating to problems of water and air pollution, and for their prevention, control or abatement
    • Plan and organise training of persons engaged in the programme on the prevention, control or abatement of water and air pollution
    • Organise through mass media, a comprehensive mass awareness programme on the prevention, control or abatement of water and air pollution
    • Collect, compile and publish technical and statistical data relating to water and air pollution and the measures devised for their effective prevention, control or abatement;
    • Prepare manuals, codes and guidelines relating to treatment and disposal of sewage and trade effluents as well as for stack gas cleaning devices, stacks and ducts;
    • Disseminate information in respect of matters relating to water and air pollution and their prevention and control
    • Lay down, modify or annul, in consultation with the State Governments concerned, the standards for stream or well, and lay down standards for the quality of air.
    • Perform such other functions as may be prescribed by the Government of India.

     

    National Biodiversity Authority

    Established When: It is a statutory autonomous body under the Ministry of Environment and Forests, Government of India established in 2003, after India signed Convention on Biological Diversity (CBD) in 1992

    Headquarter: Chennai

    The objective of the body: Implementation of Biological Diversity Act, 2002

    Key Functions:

    It acts as a facilitating, regulating and advisory body to the Government of India “on issues of conservation, sustainable use of biological resources and fair and equitable sharing of benefits arising out of the use of biological resources.”

    Additionally, it advises State Governments in identifying the areas of biodiversity importance (biodiversity hotspots) as heritage sites.

     

    National Tiger conservation authority

    Established: It was established in December 2005 following a recommendation of the Tiger Task Force, constituted by the Prime Minister of India for reorganised management of Project Tiger and the many Tiger Reserves in India.

    Headquarter: Delhi

    Objective:

    • Providing statutory authority to Project Tiger so that compliance of its directives become legal.
    • Fostering accountability of Center-State in management of Tiger Reserves, by providing a basis for MoU with States within our federal structure.
    • Providing for oversight by Parliament.
    • Addressing livelihood interests of local people in areas surrounding Tiger Reserves.

    Key Functions:

    • to approve the tiger conservation plan prepared by the State Government under sub-section (3) of section 38V of this Act
    • evaluate and assess various aspects of sustainable ecology and disallow any ecologically unsustainable land use such as mining, industry and other projects within the tiger reserves;
    • provide for management focus and measures for addressing conflicts of  men and wild animal and to emphasize on co-existence in forest areas outside the National Parks, sanctuaries or tiger reserve, in the working plan code
    • provide information on protection measures including future conservation plan, estimation of population of tiger and its natural prey species, the status of habitats, disease surveillance, mortality survey, patrolling, reports on untoward happenings and such other management aspects as it may deem fit including future plan conservation
    • ensure critical support including scientific, information technology and legal support for better implementation of the tiger conservation plan
    • facilitate ongoing capacity building programme for skill development of officers and staff of tiger reserves.

     

    Animal Welfare Board of India

    Established When: It was established in 1962 under Section 4 of The Prevention of Cruelty to Animals Act,1960.

    Headquarter: Ballabhgarh

    Objective: To advise Government on Animal Welfare Laws and promotes animal welfare in the country.

    Key Functions:

    • Recognition of Animal Welfare Organisations: The Board oversees Animal Welfare Organisations (AWOs) by granting recognition to them if they meet its guidelines. The organisation must submit paperwork; agree to nominate a representative of the Animal Welfare Board of India on its Executive Committee, and to submit to regular inspections. After meeting the requirements and inspection, the organisation is considered for grant of recognition.
    • The AWBI also appoints key people to the positions of (Hon) Animal Welfare Officers, who serve as the key point of contact between the people, the government and law enforcement agencies.
    • Financial assistance: The Board provides financial assistance to recognised Animal Welfare Organisations (AWOs), who submit applications to the Board. Categories of grants include Regular Grant, Cattle Rescue Grant, Provision of Shelter House for looking after the Animals, Animal Birth Control (ABC) Programme, Provision of Ambulance for the animals in distress and Natural Calamity grant.
    • Animal welfare laws and Rules: The Board suggests changes to laws and rules about animal welfare issues. In 2011, a new draft Animal Welfare Act was published for comment. Guidance is also offered to organisations and officials such as the police to help them interpret and apply the laws.
    • Raising awareness: The Board issues publications to raise awareness of various animal welfare issues. The Board’s Education Team gives talks on animal welfare subjects, and trains members of the community to be Board Certified Animal Welfare Educators.

     

    Forest Survey of India

    Established When:  It is a government organization in India under the Union Ministry of Environment, Forest and Climate Change for conducting forest surveys and studies. The organization came into being in, 1981.

    Headquarter: Dehradun, Uttarakhand

    Objective

    The objective of the organization is monitoring periodically the changing situation of land and forest resources and present the data for national planning; conservation and management of environmental preservation and implementation of social forestry projects.

    Key Functions

    • The Functions of the Forest Survey of India are:
    • To prepare State of Forest Report biennially, providing an assessment of the latest forest cover in the country and monitoring changes in these.
    • To conduct an inventory in forest and non-forest areas and develop a database on forest tree resources.
    • To prepare thematic maps on 1:50,000 scale, using aerial photographs.
    • To function as a nodal agency for collection, compilation, storage and dissemination of spatial database on forest resources.
    • To conduct training of forestry personnel in the application of technologies related to resources survey, remote sensing, GIS, etc.
    • To strengthen research & development infrastructure in FSI and to conduct research on applied forest survey techniques.
    • To support State/UT Forest Departments (SFD) in forest resources survey, mapping and inventory.
    • To undertake forestry-related special studies/consultancies and custom made training courses for SFD’s and other organizations on a project basis.

    Forest Survey of India assesses forest cover of the country every 2 years by digital interpretation of remote sensing satellite data and publishes the results in a biennial report called ‘State of Forest Report'(SFR).

    Central Zoo Authority of India

    Established: It was established in 1992 and constituted under the Wild Life (Protection) Act.

    Headquarter: Delhi

    Objective 

    The main objective of the authority is to complement the national effort in the conservation of wildlife.

    Standards and norms for housing, upkeep, health care and overall management of animals in zoos have been laid down under the Recognition of Zoo Rules, 1992.   

    Key Functions

    • Since its inception in 1992, the Authority has evaluated 513 zoos, out of which 167 have been recognized and 346 refused recognition.
    • The Authority’s role is more of a facilitator than a regulator.  It, therefore, provides technical and financial assistance to such zoos which have the potential to attain the desired standard in animal management. Only such captive facilities which have neither the managerial skills nor the requisite resources are asked to close down.
    • Apart from the primary function of the grant of recognition and release of financial assistance, the Central Zoo Authority also regulates the exchange of animals of the endangered category listed under Schedule-I and II of the Wildlife (Protection Act) among zoos.  
    • Exchange of animals between Indian and foreign zoos is also approved by the Authority before the requisite clearances under EXIM Policy and the CITES permits are issued by the competent authority.  
    • The Authority also coordinates and implements programmes on capacity building of zoo personnel, planned conservation breeding programmes and ex-situ research including biotechnological intervention for the conservation of species for complementing in-situ conservation efforts in the country.

     

     

    Major UN climate negotiations under UNFCCC- Timeline

    1992—

    The UN Framework Convention on Climate Change (UNFCCC) was adopted and opened for signatures in Rio de Janeiro, Brazil, at the UN Conference on Environment and Development, also known as the Earth Summit.

    154 signatories to the UNFCCC agreed to stabilize “greenhouse gas concentrations in the atmosphere at a level that would prevent dangerous interference with the climate system.”

    The treaty is not legally binding because it sets no mandatory limits on GHG emissions. Instead, the treaty provides for future negotiations to set emissions limits. The first principal revision is the Kyoto Protocol.

    1994—

    The UNFCCC Treaty entered into force after receiving 50 ratifications.

    1997—

    KYOTO PROTOCOL

    COP 3 was held in Kyoto, Japan. On December 11, the Kyoto Protocol was adopted by consensus with more than 150 signatories.

    The Protocol included legally binding emissions targets for developed country Parties for the six major GHGs, which are-

    • Carbon dioxide.
    • Methane.
    • Nitrous oxide.
    • Hydrofluorocarbons.
    • Perfluorocarbons, and
    • Sulfur hexafluoride.

    Annex of the Kyoto Protocol

    • Annex 1 – Industrialised Countries (mainly OECD) plus economies in transition (mainly former soviet block countries) – They would mandatorily reduce GHGs, base year – 1990
    • Annex 2 – Subset of Annex 1,  Industrialised Countries (mainly OECD), would also provide finances and technology to non annex countries
    • Non annex – not included in annex, all other countries, no binding targets
    • Annex A – gases covered under Kyoto <name those 7 gases>
    • Annex B – Binding targets for each Annex 1 country i.e Japan will reduce emission by X%, Australia by Y% 

    The Protocol offered additional means of meeting targets by way of three market-based mechanisms:

    • Emissions trading.
    • Clean Development Mechanism (CDM).
    • Joint Implementation (JI).

    Under the Protocol, industrialized countries’ actual emissions have to be monitored and precise records have to be kept of the trades carried out.

    India ratified the Kyoto Protocol in 2002.

     

    2000—

    COP 6 part I was held in The Hague, Netherlands. Negotiations faltered, and parties agreed to meet again.

    COP 6part II was held in Bonn, Germany. The consensus was reached on what was called the Bonn Agreements.

    All nations except the United States agreed on the mechanisms for implementation of the Kyoto Protocol.

    The U.S. participated in observatory status only.

    2001—

    COP 7 was held in Marrakesh, Morocco. The detailed rules for the implementation of the Kyoto Protocol were adopted and called the Marrakesh Accords.

    The Special Climate Change Fund (SCCF) was established to “finance projects relating to: adaptation; technology transfer and capacity building; energy transport, industry, agriculture, forestry and waste management; and economic diversification.”

    The Least Developed Countries Fund was also “established to support a work programme to assist Least Developed Country Parties (LDCs) carry out, inter alia [among other things], the preparation and implementation of national adaptation programmes of action (NAPAs).”

    2005—

    COP 11/CMP 1 were held in Montreal, Canada. This conference was the first to take place after the Kyoto Protocol took force. The annual meeting between the parties (COP) was supplemented by the first annual Meeting of the Parties to the Kyoto Protocol (CMP).

    The countries that had ratified the UNFCCC, but not accepted the Kyoto Protocol, had observer status at the latter conference.

    The parties addressed issues such as “capacity building, development and transfer of technologies, the adverse effects of climate change on developing and least developed countries, and several financial and budget-related issues, including guidelines to the Global Environment Facility (GEF).” (UNFCCC)

    2007—

    COP 13/CMP 3 were held in Bali. COP parties agreed to a Bali Action Plan to negotiate GHG mitigation actions after the Kyoto Protocol expires in 2012. The Bali Action Plan did not require binding GHG targets for developing countries.

    2009—

    June – As part of the UN Framework Convention on Climate Change (UNFCCC) process, governments met in Bonn, Germany, to begin discussions on draft negotiations that would form the basis of an agreement at Copenhagen.

    December – COP 15 was held in Copenhagen, Denmark.

    It failed to reach agreement on binding commitments after the Kyoto Protocol commitment period ends in 2012.

    During the summit, leaders from the United States, Brazil, China, Indonesia, India and South Africa agreed to what would be called the Copenhagen Accord which recognized the need to limit the global temperature rise to 2°C based on the science of climate change.

    While no legally binding commitments were required by the deal, countries were asked to pledge voluntary GHG reduction targets. $100 billion was pledged in climate aid to developing countries.

    2012—

    COP 18 was held in Doha, Qatar.

    Parties agreed to extend the expiring Kyoto Protocol, creating a second commitment phase that would begin on January 1, 2013 and end December 31, 2020. India ratified the second commitment period in 2017.

    Parties failed to set a pathway to provide $100 billion per year by 2020 for developing countries to finance climate change adaptation, as agreed upon at COP 15 in Copenhagen.

    The concept of “loss and damage” was introduced as developed countries pledged to help developing countries and small island nations pay for the losses and damages from climate change that they are already experiencing.

    2013—

    COP 19 was held in Warsaw, Poland.

    Parties were expected to create a roadmap for the 2015 COP in Paris where a legally binding treaty to reduce greenhouse gas (GHG) emissions is expected to be finalized (in order to come into effect in 2020).

    Differences of opinion on responsibility of GHG emissions between developing and developed countries led to a flexible ruling on the wording and a plan to discuss further at the COP 20 in Peru.

    A non-binding agreement was reached among countries to set up a system tackling the “loss and damage” issue, although details of how to set up the mechanism were not discussed.

    Concerning climate finance, the United Nations’ Reducing Emissions from Deforestation and Forest Degradation (REDD+) Program, aimed at preserving the world’s forests, was formally adopted.

    Little progress was made on developed countries committing to the agreed upon plan of providing $100 billion per year by 2020 to developing countries.

     

    2015—

    PARIS AGREEMENT

    COP 21 or CMP 11 was held in Paris.

    Aims of the Paris Agreement-

    1.Keep the global temperature rise this century well below 2 degrees Celsius above the pre-industrial level.

    2.Pursue efforts to limit the temperature increase even further to 1.5 degrees Celsius.

    3.Strengthen the ability of countries to deal with the impacts of climate change.

    Nationally Determined Contributions (NDC)

    • The national pledges by countries to cut emissions are voluntary.
    • The Paris Agreement requires all Parties to put forward their best efforts through “nationally determined contributions” (NDCs) and to strengthen these efforts in the years ahead.
    • This includes requirements that all Parties report regularly on their emissions and on their implementation efforts.
    • In 2018, Parties will take stock of the collective efforts in relation to progress towards the goal set in the Paris Agreement.
    • There will also be a global stock take every 5 years to assess the collective progress towards achieving the purpose of the Agreement and to inform further individual actions by Parties.

    Some facts-

    • It entered into force in November 2016 after (ratification by 55 countries that account for at least 55% of global emissions) had been met.
    • The agreement calls for zero net anthropogenic greenhouse gas emissions to be reached during the second half of the 21st century.
    • In the adopted version of the Paris Agreement, the parties will also “pursue efforts to limit the temperature increase to 1.5 °C.”
    • The 1.5 °C goal will require zero-emissions sometime between 2030 and 2050, according to some scientists.
    • The developed countries reaffirmed the commitment to mobilize $100 billion a year in climate finance by 2020 and agreed to continue mobilizing finance at the level of $100 billion a year until 2025.
    • In 2017, United States announced that the U.S. would cease all participation in the 2015 Paris Agreement on climate change mitigation.
    • In accordance with Article 28 of the Paris Agreement, the earliest possible effective withdrawal date by the United States cannot be before November 2020. Thus, The U.S. will remain a signatory till November 2020.
  • [Prelims Spotlight] Important Keywords Regarding Budget, Fiscal Policy and Taxation

     

    Prelims Spotlight is a part of “Nikaalo Prelims 2020” module. This open crash course for Prelims 2020 has a private telegram group where PDFs and DDS (Daily Doubt Sessions) are being held. Please click here to register.


    24 March 2020

    Important keywords regarding budget, fiscal policy and taxation

     

    Annual financial statement:

    The Union Budget is the annual financial statement that contains the government’s revenue and expenditure for a fiscal year.

    It may also include planned sales volumes and revenues, resource quantities, costs and expenses, assets, liabilities and cash flows.

    The statement details the revenues from all sources, and expenditure on all activities that the government will undertake for the fiscal year. The fiscal year is calculated from 1 April-31 March.

    Under Article 112 of the Constitution, the government has to present a statement of estimated revenue and expenditure for every fiscal. This statement is called the annual financial statement. This document is divided into three sections: For each of these funds, the central government is required to present a statement of revenue and expenditure.

    1. Consolidated Fund:

    The Consolidated Fund of India, created under Article 266 of the Indian Constitution, includes the revenues received by the government and expenses made by it.

    All the revenue that the government receives through direct (income tax, corporation tax etc.) or indirect tax (Goods and Services Tax or GST) go into the Consolidated Fund of India.

    Revenue from non-tax sources like dividends, profits from the PSUs, and income from general services also contribute to the fund. Recoveries of loans, earnings from disinvestment and repayment of debts issued by the Centre also contribute to the fund.

    However, no money can be withdrawn for meeting expenses until the government gets the approval of the Parliament. Examples of expenditure include wages, salaries and pension of government employees, and other fixed costs. The repayment of debts incurred by the government is also done through the Consolidated Fund of India.

    The Consolidated Fund of India is divided into five parts:

    • Revenue account – receipts,
    • Revenue account – disbursements,
    • Capital account – receipts,
    • Capital account – disbursements, and
    • Disbursements ‘charged’ on the Consolidated Fund of India.

    Disbursements ‘charged’ on the Consolidated Fund of India is a special category within the Consolidated Fund of India which is not put to vote in the Parliament.

    This means whatever comes under this category need to be paid, whether the Budget is passed or not.

    The salary and allowances of the President, speaker and deputy speaker of the Lok Sabha, chairman and deputy chairman of the Rajya Sabha, salaries and allowances of Supreme Court judges, pensions of Supreme Court and High Court judges come under this category.

    2.Contingency fund:

    Like the Consolidated Fund of India, the Contingency Fund of India constitutes a part of the annual financial statement.

    Established under Article 267(1) of the Indian Constitution, the fund is maintained by the ministry of finance on behalf of the President of India.

    As the name suggests, the Contingency Fund of India is an account maintained for meeting expenses during any unforeseen emergencies.

    Parliamentary approval for such unforeseen expenditure is obtained, ex- post-facto, and an equivalent amount is drawn from the Consolidated Fund of India to recoup the Contingency Fund after such ex-post-facto approval.

    3. Public account.

    Article 266 of the Constitution defines the Public Account as being those funds that are received on behalf of the Government of India.

    Money held by the government in a trust — such as in the case of Provident Funds, Small Savings collections, income of government set apart for expenditure on specific objects like road development, primary education, reserve/special Funds, etc — are kept in the Public Account.

    Public Account funds do not belong to the government and have to be finally paid back to the persons and authorities that deposited them.

    Parliamentary authorisation for such payments is not required.

    However, when money is withdrawn from the Consolidated Fund with the approval of Parliament and kept in the Public Account for expenditure for a specific purpose, it is submitted for a vote in Parliament.

    Appropriation bill

    Appropriation Bill is a money bill that allows the government to withdraw funds from the Consolidated Fund of India to meet its expenses during the course of a financial year.

    As per Article 114 of the Constitution, the government can withdraw money from the Consolidated Fund only after receiving approval from Parliament.

    To put it simply, the Finance Bill contains provisions on financing the expenditure of the government, and Appropriation Bill specifies the quantum and purpose for withdrawing money.

    Vote-on-account

    The Constitution says that no money can be withdrawn by the government from the Consolidated Fund of India except under appropriation made by law.

    For that, an appropriation bill is passed during the Budget process.

    However, the appropriation bill may take time to pass through the Parliament and become a law. Meanwhile, the government would need permission to spend even a single penny from April 1 when the new financial year starts.

    Vote on the account is the permission to withdraw money from the Consolidated Fund of India in that period, usually two months.

    Vote on the account is a formality and requires no debate. When elections are scheduled a few months into the new financial year, the government seeks vote on account for four months. Essentially, vote on account is the interim permission of the parliament to the government to spend money.

    Corporation tax:

    Corporation tax is a direct tax imposed on the net income or profit that enterprises make from their businesses. Companies, both public and privately registered in India under the Companies Act 1956, are liable to pay corporation tax. This tax is levied at a specific rate according to the provisions of the Income Tax Act, 1961.

    Fringe benefits tax (FBT):
    The taxation of perquisites – or fringe benefits – provided by an employer to his employees, in addition to the cash salary or wages paid, is fringe benefits tax. It was introduced in Budget 2005-06. The government felt many companies were disguising perquisites such as club facilities as ordinary business expenses, which escaped taxation altogether. Employers have to now pay FBT on a percentage of the expense incurred on such perquisites.

    Direct Tax:

    A direct tax is paid directly by an individual or organization to the imposing entity. A taxpayer, for example, pays direct taxes to the government for different purposes, including real property tax, personal property tax, income tax, or taxes on assets. Direct taxes are based on the ability-to-pay principle. This economic principle states that those who have more resources or earn a higher income should pay more taxes.

    Indirect Tax
    In the case of indirect taxes, the incidence of tax is usually not on the person who pays the tax. These are largely taxes on expenditure and include Customs, excise and service tax.

    Indirect taxes are considered regressive, the burden on the rich and the poor is alike. That is why governments strive to raise a higher proportion of taxes through direct taxes. Moving on, we come to the next important receipt item in the revenue account, non-tax revenue.

    Non-tax revenue:

    Other than taxation being a primary source of income, the government also earns a recurring income, which is called non-tax revenue. While sources of tax revenue are few, the sources of non-tax revenue are many, with the number of collections per source. Although there are many sources of non-tax revenue, the amount per source is much less than that for tax revenue.

    For example, when citizens use services offered by the government, they pay bills, which are categorised as non-tax revenue, as the government provides infrastructure support to implement the services. Non-tax revenue also includes the interest collected by the government on the loans or funds offered to states.

    Grants-in-aid and contributions
    The third receipt item in the revenue account is relatively small grants-in-aid and contributions. These are in the nature of pure transfers to the government without any repayment obligation.
    These include expense incurred on organs of state such as Parliament, judiciary and elections. A substantial amount goes into administering fiscal services such as tax collection. The biggest item is the interest payment on loans taken by the government. Defence and other services like police also get a sizeable share. Having looked at receipts and expenditure on revenue account we come to an important item, the difference between the two, the revenue deficit.

    Revenue deficit:

    Revenue deficit arises when the government’s revenue expenditure exceeds the total revenue receipts.

    Revenue deficit includes those transactions that have a direct impact on a government’s current income and expenditure. This represents that the government’s own earnings are not sufficient to meet the day-to-day operations of its departments. Revenue deficit turns into borrowings when the government spends more than what it earns and has to resort to the external borrowings.

                   Revenue Deficit= Total revenue receipts – Total revenue expenditure.

    Revenue Deficit deals only with the government’s revenue receipts and revenue expenditures.

    Note that revenue receipts are receipts which neither create liability nor lead to a reduction in assets.

    It is further divided into two heads:

    • Receipt from Tax (Direct Tax,  Indirect Tax)
    • Receipts from Non-Tax Revenue

    Revenue Expenditure is referred to as the expenditure that does not result in the creation of assets reduction of liabilities. It is further divided into two types

    • Plan revenue expenditure
    • Non-plan revenue expenditure

    Fiscal Deficit:
    The fiscal deficit is defined as an excess of total budget expenditure over total budget receipts excluding borrowings during a fiscal year. In simple words, it is the amount of borrowing the government has to resort to meet its expenses. A large deficit means a large amount of borrowing. The fiscal deficit is a measure of how much the government needs to borrow from the market to meet its expenditure when its resources are inadequate.

    Primary deficit:

    Primary deficit is defined as a fiscal deficit of current year minus interest payments on previous borrowings.

             Primary deficit= Fiscal deficit – Interest payment on the previous borrowing

    In other words, whereas fiscal deficit indicates borrowing requirement inclusive of interest payment, the primary deficit indicates borrowing requirement exclusive of interest payment (i.e., amount of loan).

    We have seen that borrowing requirement of the government includes not only accumulated debt, but also interest payment on the debt. If we deduct ‘interest payment on debt’ from borrowing, the balance is called the primary deficit.

    Public debt:

    Public debt receipts and public debt disbursals are borrowings and repayments during the year, respectively. The difference is the net accretion to the public debt. Public debt can be split into internal (money borrowed within the country) and external (funds borrowed from non-Indian sources). Internal debt comprises treasury bills, market stabilisation schemes, ways and means advance, and securities against small savings.

    Ways and means advance (WMA):

    One of RBI’s roles is to serve as banker to both central and state governments. In this capacity, RBI provides temporary support to tide over mismatches in their receipts and payments in the form of ways and means advances.

    CESS:
    This is an additional levy on the basic tax liability. Governments resort to cess for meeting specific expenditure.

    Dividend distribution tax:

    A dividend is a return given by a company to its shareholders out of the profits earned by the company in a particular year. Dividend constitutes income in the hands of the shareholders which ideally should be subject to income tax.

    However, the income tax laws in India provided for an exemption of the dividend income received from Indian companies by the investors by levying a tax called the Dividend Distribution Tax (DDT) on the company paying the dividend. This tax has been abolished in the 2020-21 budget.

    FRBM Act 2003:

    The Fiscal Responsibility and Budget Management Act (FRBM Act), 2003, establishes financial discipline to reduce the fiscal deficit.

    What are the objectives of the FRBM Act?

    The FRBM Act aims to introduce transparency in India’s fiscal management systems. The Act’s long-term objective is for India to achieve fiscal stability and to give the Reserve Bank of India (RBI) flexibility to deal with inflation in India. The FRBM Act was enacted to introduce a more equitable distribution of India’s debt over the years.

    Key features of the FRBM Act

    The FRBM Act made it mandatory for the government to place the following along with the Union Budget documents in Parliament annually:

    1. Medium Term Fiscal Policy Statement

    2. Macroeconomic Framework Statement

    3. Fiscal Policy Strategy Statement

    The FRBM Act proposed that revenue deficit, fiscal deficit, tax revenue and the total outstanding liabilities be projected as a percentage of gross domestic product (GDP) in the medium-term fiscal policy statement.

     

  • [Prelims Spotlight] Important keyword related to various economic Indicators

     

    Prelims Spotlight is a part of “Nikaalo Prelims 2020” module. This open crash course for Prelims 2020 has a private telegram group where PDFs and DDS (Daily Doubt Sessions) are being held. Please click here to register.


    23 March 2020

    Important Keywords related to Various Economic Indicators

    Economic indicators are key stats about the economy that can help you better understand where the economy is headed. Here are several of the different types of economic indicators and how they may be used to understand the state of the economy. The most frequently used economic indicators are- GDP, The Stock Market, Unemployment, Consumer Price Index, Balance of Trade, Interest rate, Currency strength, Income and Wages etc.

    Types of Economic Indicators

    There are three types of economic indicators: leading, lagging and coincident.

    1. Leading indicators point to future changes in the economy. They are extremely useful for short-term predictions of economic developments because they usually change before the economy changes.
    2. Lagging indicators usually come after the economy changes. They are generally most helpful when used to confirm specific patterns. You can make economic predictions based on the patterns, but lagging indicators cannot be used to directly predict economic change.
    3. Coincident indicators provide valuable information about the current state of the economy within a particular area because they happen at the same time as the changes they signal.

    Terms to economic indicators

    Asset turnover ratio-

     Asset turnover ratio is the ratio between the value of a company’s sales or revenues and the value of its assets. It is an indicator of the efficiency with which a company is deploying its assets to produce the revenue.

    Amortisation

    The running down or payment of a loan by instalments. An example is a repayment mortgage on a house, which is amortised by making monthly payments that over a pre-agreed period of time cover the value of the loan plus interest. With loans that are not amortised, the borrower pays the only interest during the period of the loan and then repays the sum borrowed in full.

    Appreciation

    A rise in the value of an asset and the opposite of depreciation. When the value of a currency rises relative to another, it appreciates.

    Balance of payment-

    The total of all the money coming into a country from abroad less all of the money going out of the country during the same period. This is usually broken down into the current account and the capital account. The current account includes:

    *visible trade (known as merchandise trade), which is the value of exports and imports of physical goods;

    *invisible trade, which is receipts and payments for services, such as banking or advertising, and other intangible goods, such as copyrights, as well as cross-border dividend and interest payments;

    *private transfers, such as money sent home by expatriate workers;

    *official transfers, such as international aid.

    The capital account includes:

    *long-term capital flows, such as money invested in foreign firms, and profits made by selling those investments and bringing the money home;

    *short-term capital flows, such as money invested in foreign currencies by international speculators, and funds moved around the world for business purposes by multinational companies. These short-term flows can lead to sharp movements in exchange rates, which bear little relation to what currencies should be worth judging by fundamental measures of value such as purchasing power parity.

    As bills must be paid, ultimately a country’s accounts must balance (although because real life is never that neat a balancing item is usually inserted to cover up the inconsistencies).

    According to the RBI, the balance of payment is a statistical statement that shows

    1. The transaction in goods, services and income between an economy and the rest of the world,

    2. Changes of ownership and other changes in that economy’s monetary gold, special drawing rights (SDRs), and financial claims on and liabilities to the rest of the world, and

    3. Unrequited transfers.

    Balanced Budget–

    When total public-sector spending equals total government income during the same period from taxes and charges for public services. Politicians in some countries, such as the United States, have argued that the government should be required to run a balanced budget in order to have sound public finances. However, there is no economic reason why public borrowing needs necessarily be bad. For instance, if the debt is used to invest in things that will increase the growth rate of the economy–infrastructure, say, or education–it may be justified. It may also make more economic sense to try to balance the budget on average over an entire economic cycle, with public-sector deficits boosting the economy during recession and surpluses stopping it overheating during booms than to balance it every year.

    Bank rate-

    Bank rate is the rate charged by the central bank for lending funds to commercial banks.

    Base rate-

    Base rate is the minimum rate set by the Reserve Bank of India below which banks are not allowed to lend to its customers.

    Basis point–

    One one-hundredth of a percentage point. Small movements in the interest rate, the exchange rate and bond yields are often described in terms of basis points. If a bond yield moves from 5.25% to 5.45%, it has risen by 20 basis points.

    Broad money to reserve money

    It is a measure of the money multiplier. Money multiplier shows the mechanism by which reserve money creates money supply in the economy. It is again dependent on two variables, namely the currency deposit ratio and reserve deposit ratio.

    It is a measure of the money multiplier. Money multiplier shows the mechanism by which reserve money creates money supply in the economy. It is again dependent on two variables, namely the currency deposit ratio and reserve deposit ratio.

    Bubble-

    When the price of an asset rises far higher than can be explained by fundamentals, such as the income likely to derive from holding the asset.

    Capacity cost-

    An expenditure or cost incurred by a company in order to expand its business operations. In other words, these are expenses incurred by an organization to increase its capacity to conduct business operations.

    Capital account–

    The capital account can be regarded as one of the primary components of the balance of payments of a nation. It gives a summary of the capital expenditure and income for a country.

    The capital expenditure and income is tracked by way of funds in the form of investments and loans flowing in and out of an economy. This account comprises foreign direct investments, portfolio investments, etc. It gives a summary of the net flow of both private and public investment into an economy.

    A capital account deficit shows that more money is flowing out of the economy along with an increase in its ownership of foreign assets and vice-versa in case of a surplus. The balance of payments contains the current account (which provides a summary of the trade of goods and services) in addition to the capital account which records all capital transactions.

    Capital adequacy ratio

    The ratio of a BANK’s CAPITAL to its total ASSETS, required by regulators to be above a minimum (“adequate”) level so that there is little RISK of the bank going bust. How high this minimum level is may vary according to how risky a bank’s activities are.

    Capital flight

    When CAPITAL flows rapidly out of a country, usually because something happens which causes investors suddenly to lose confidence in its economy. (Strictly speaking, the problem is not so much the MONEY leaving, but rather that investors in general suddenly lower their valuation of all the assets of the country.) This is particularly worrying when the flight capital belongs to the country’s own citizens. This is often associated with a sharp fall in the EXCHANGE RATE of the abandoned country’s currency.

    Capital gains

    The PROFIT from the sale of a capital ASSET, such as a SHARE or a property. Capital gains are subject to TAXATION in most countries. Some economists argue that capital gains should be taxed lightly (if at all) compared with other sources of INCOME. They argue that the less tax is levied on capital gains, the greater is the incentive to put capital to productive use. Put another way, capital gains tax is effectively a tax on CAPITALISM. However, if capital gains are given too friendly a treatment by the tax authorities, accountants will no doubt invent all sorts of creative ways to disguise other income as capital gains.

    Call money rate-

    Call money rate is the rate at which short term funds are borrowed and lent in the money market.
    The duration of the call money loan is 1 day. Banks resort to these type of loans to fill the asset-liability mismatch, comply with the statutory CRR and SLR requirements and to meet the sudden demand of funds. RBI, banks, primary dealers etc are the participants of the call money market. Demand and supply of liquidity affect the call money rate. A tight liquidity condition leads to a rise in call money rate and vice versa.

    Consumer surplus-

    Consumer surplus is defined as the difference between the consumers’ willingness to pay for a commodity and the actual price paid by them, or the equilibrium price.

    Total social surplus is composed of consumer surplus and producer surplus. It is a measure of consumer satisfaction in terms of utility.

    Graphically, it can be determined as the area below the demand curve (which represents the consumer’s willingness to pay for a good at different prices) and above the price line. It reflects the benefit gained from the transaction based on the value the consumer places on the good. It is positive when what the consumer is willing to pay for the commodity is greater than the actual price.

    Consumer surplus is infinite when the demand curve is inelastic and zero in case of a perfectly elastic demand curve.

    Contractionary policy

    Contractionary policy is a kind of policy which lays emphasis on reduction in the level of money supply for lesser spending and investment thereafter so as to slow down an economy.

    Core inflation

    An inflation measure which excludes transitory or temporary price volatility as in the case of some commodities such as food items, energy products etc. It reflects the inflation trend in an economy.

    Cost-push inflation

    Cost-push inflation is inflation caused by an increase in prices of inputs like labour, raw material, etc. The increased price of the factors of production leads to a decreased supply of these goods. While the demand remains constant, the prices of commodities increase causing a rise in the overall price level. This is in essence cost-push inflation.

    Countervailing Duties

    Duties that are imposed in order to counter the negative impact of import subsidies to protect domestic producers are called countervailing duties.

    In cases foreign producers attempt to subsidize the goods being exported by them so that it causes domestic production to suffer because of a shift in domestic demand towards cheaper imported goods, the government makes mandatory the payment of a countervailing duty on the import of such goods to the domestic economy.

    This raises the price of these goods leading to domestic goods again being equally competitive and attractive. Thus, domestic businesses are cushioned. These duties can be imposed under the specifications given by the WTO (World Trade Organization) after the investigation finds that exporters are engaged in dumping. These are also known as anti-dumping duties.

    Collateral

    An ASSET pledged by a borrower that may be seized by a lender to recover the value of a loan if the borrower fails to meet the required INTEREST charges or repayments.

    Crowding out effect

    A situation when increased interest rates lead to a reduction in private investment spending such that it dampens the initial increase of total investment spending is called crowding out effect.

    Sometimes, the government adopts an expansionary fiscal policy stance and increases its spending to boost economic activity. This leads to an increase in interest rates. Increased interest rates affect private investment decisions. A high magnitude of the crowding-out effect may even lead to lesser income in the economy.

    Currency Deposit ratio

    The currency deposit ratio shows the amount of currency that people hold as a proportion of aggregate deposits.

    Deflation

    When the overall price level decreases so that inflation rate becomes negative, it is called deflation. It is the opposite of the often-encountered inflation.

    Depreciation

    The monetary value of an asset decreases over time due to use, wear and tear or obsolescence. This decrease is measured as depreciation.

    Depression

    Depression is defined as a severe and prolonged recession. A recession is a situation of declining economic activity. Declining economic activity is characterized by falling output and employment levels. Generally, when an economy continues to suffer a recession for two or more quarters, it is called depression.

    The level of productivity in an economy falls significantly during a depression. Both the GDP (gross domestic product) and GNP (gross national product) show a negative growth along with greater business failures and unemployment.

    When a recession continues to take its toll on any economy, the built-in process triggers further cuts in investment as well as consumption spending due to loss of confidence among investors and consumers. Also, the financial crisis may lead to decreased availability for credit. Excessive fluctuations happen in the relative value of the currency. Overall trade and commerce get reduced. The Great Depression of 1929 is considered to be the most classic example of depression in economic history.

    ETF

    ETFs or exchange-traded funds are similar to index mutual funds. However, they trade just like stocks.

    ETFs were started in 2001 in India. They comprise a portfolio of equity, bonds and trade close to its net asset value. These funds mainly track an index, a commodity, or a pool of assets.

    They have the following advantages over mutual funds and equity/debt funds:

    1. Lower Costs: An investor who buys an ETF doesn’t have to pay an advisory/management fee to the fund manager and taxes are relatively lower in ETFs.

    2. Lower Holding Costs: As commodity ETFs are widely traded in, there isn’t any physical delivery of the commodity. The investor is just provided with an ETF certificate, similar to a stock certificate.

    Gross Domestic Saving

    Gross Domestic Saving is GDP minus the final consumption expenditure. It is expressed as a percentage of GDP.

    Gross National Product

    Gross National Product (GNP) is the Gross Domestic Product (GDP) plus net factor income from abroad.

    GNP measures the monetary value of all the finished goods and services produced by the country’s factors of production irrespective of their location. Only the finished or final goods are considered as factoring intermediate goods used for manufacturing would amount to double counting. It includes taxes but does not include subsidies.

    Inferior goods

    An inferior good is a type of good whose demand declines when income rises. In other words, the demand of inferior goods is inversely related to the income of the consumer.

    Libor

    LIBOR, the acronym for London Interbank Offer Rate, is the global reference rate for unsecured short-term borrowing in the interbank market. It acts as a benchmark for short-term interest rates. It is used for pricing of interest rate swaps, currency rate swaps as well as mortgages. It is an indicator of the health of the financial system and provides an idea of the trajectory of impending policy rates of central banks.

    LIBOR is administered by the Intercontinental Exchange or ICE. It is computed for five currencies with seven different maturities ranging from overnight to a year. The five currencies for which LIBOR is computed are Swiss franc, euro, pound sterling, Japanese yen and US dollar. ICE benchmark administration consists of 11 to 18 banks that contribute for each currency.

    Liquidity

    Liquidity means how quickly you can get your hands on your cash. In simpler terms, liquidity is to get your money whenever you need it.

    Liquidity trap

    A liquidity trap is a situation when expansionary monetary policy (increase in the money supply) does not increase the interest rate, income and hence does not stimulate economic growth.

    The liquidity trap is the extreme effect of monetary policy. It is a situation in which the general public is prepared to hold on to whatever amount of money is supplied, at a given rate of interest. They do so because of the fear of adverse events like deflation, war.

    In that case, a monetary policy carried out through open market operations has no effect on either the interest rate or the level of income. In a liquidity trap, the monetary policy is powerless to affect the interest rate.

    Marginal standing facility

    Marginal standing facility (MSF) is a window for banks to borrow from the Reserve Bank of India in an emergency situation when inter-bank liquidity dries up completely.

    Banks borrow from the central bank by pledging government securities at a rate higher than the repo rate under liquidity adjustment facility or LAF in short.

    Moral hazard

    Moral hazard is a situation in which one party gets involved in a risky event knowing that it is protected against the risk and the other party will incur the cost. It arises when both parties have incomplete information about each other.

    Net interest income

    Net interest income (NII) is the difference between the interest income a bank earns from its lending activities and the interest it pays to depositors.

    Net interest income = Interest earned – interest paid

    Net interest margin

    Net interest margin or NIM denotes the difference between the interest income earned and the interest paid by a bank or financial institution relative to its interest-earning assets like cash.

    Net interest margin = (Investment returns – interest expenses) / average earning on assets

    NIM measures the effectiveness of a company’s investment decisions, particularly for financial institutions.

    Non-performing asset

    A non-performing asset (NPA) is a loan or advance for which the principal or interest payment remained overdue for a period of 90 days.

    Banks are required to classify NPAs further into Substandard, Doubtful and Loss assets.

    1. Substandard assets: Assets which has remained NPA for a period less than or equal to 12 months.

    2. Doubtful assets: An asset would be classified as doubtful if it has remained in the substandard category for a period of 12 months.

    3. Loss assets: As per RBI, “Loss asset is considered uncollectible and of such little value that its continuance as a bankable asset is not warranted, although there may be some salvage or recovery value.”

    Phillips curve

    The inverse relationship between the unemployment rate and inflation when graphically charted is called the Phillips curve. William Phillips pioneered the concept first in his paper “The Relation between Unemployment and the Rate of Change of Money Wage Rates in the United Kingdom, 1861-1957,’ in 1958. This theory is now proven for all major economies of the world.

    Producer surplus

    Producer surplus is defined as the difference between the amount the producer is willing to supply goods for and the actual amount received by him when he makes the trade.

    Purchasing power parity

    The theory aims to determine the adjustments needed to be made in the exchange rates of two currencies to make them at par with the purchasing power of each other. In other words, the expenditure on a similar commodity must be the same in both currencies when accounted for the exchange rate. The purchasing power of each currency is determined in the process.

    Quantitative easing

    Quantitative easing is an occasionally used monetary policy, which is adopted by the government to increase the money supply in the economy in order to further increase lending by commercial banks and spending by consumers. The central bank (Read: The Reserve Bank of India) infuses a pre-determined quantity of money into the economy by buying financial assets from commercial banks and private entities. This leads to an increase in banks’ reserves.

    Real GDP at factor cost

    Real GDP is the nominal GDP after adjusting for any price changes attributable to either inflation or deflation.

     Nominal GDP or the GDP at current price can present a distorted picture of the actual growth in GDP owing to price changes. However, if we consider the price of the base year as constant and compute the GDP growth rate of the current year using that constant price, the value so arrived at will give a true picture of the actual growth rate in GDP. This measure is called the Real GDP or the GDP at a constant price. It does not factor taxes and subsidies.

    A new indicator called GDP deflator is derived by dividing nominal GDP by real GDP. It is a measure of price changes in the economy.

    Recession

    Recession is a slowdown or a massive contraction in economic activities. A significant fall in spending generally leads to a recession.

    Such a slowdown in economic activities may last for some quarters thereby completely hampering the growth of an economy. In such a situation, economic indicators such as GDP, corporate profits, employment, etc., fall.

    Recessionary gap

    This is a situation wherein the real GDP is lower than the potential GDP at the full employment level. The economy operates below the full employment level in a recessionary gap.

    A recessionary gap is also termed as a contractionary gap. An economy doesn’t necessarily operate at the full employment level. So the difference that exists between the potential full-employment equilibrium and the actual ones is the recessionary gap.

    Regressive risk

    Under this system of taxation, the tax rate diminishes as the taxable amount increases. In other words, there is an inverse relationship between the tax rate and taxable income. The rate of taxation decreases as the income of taxpayers increases.

    This system of taxation generally benefits the higher sections of the society having higher incomes as they need to pay tax at lesser rates. On the other hand, people with lesser incomes are burdened with a higher rate of taxation.

    Repo rate

    Repo rate is the rate at which the central bank of a country (Reserve Bank of India in case of India) lends money to commercial banks in the event of any shortfall of funds.

    REPO means Re Purchase Option – the rate by which RBI gives loans to other banks. Bank re-purchase the securities deposited with RBI at the REPO rate.

    Repo rate is used by monetary authorities to control inflation.

    Reserve ratio

    Also known as Cash Reserve Ratio, it is the percentage of deposits which commercial banks are required to keep as cash according to the directions of the central bank.

    Reverse repo rate

    Reverse repo rate is the rate at which the central bank of a country (Reserve Bank of India in case of India) borrows money from commercial banks within the country. It is a monetary policy instrument which can be used to control the money supply in the country.

    Secondary market

    This is the market wherein the trading of securities is done. Secondary market consists of both equity as well as debt markets.

    Securities issued by a company for the first time are offered to the public in the primary market. Once the IPO is done and the stock is listed, they are traded in the secondary market. The main difference between the two is that in the primary market, an investor gets securities directly from the company through IPOs, while in the secondary market, one purchases securities from other investors willing to sell the same.

    Securitization

    Securitization is a process by which a company clubs its different financial assets/debts to form a consolidated financial instrument which is issued to investors. In return, the investors in such securities get interest.

    This process enhances liquidity in the market. This serves as a useful tool, especially for financial companies, as it helps them raise funds. If such a company has already issued a large number of loans to its customers and wants to further add to the number, then the practice of securitization can come to its rescue.

    Shorting or short selling

    In capital markets, the act of selling a security at a given price without possessing it and purchasing it later at a lower price is known as shorting. This is also termed as short selling.

    Social capital

    In capital markets, the act of selling a security at a given price without possessing it and purchasing it later at a lower price is known as shorting. This is also termed as short selling.

    Social capital is an important constituent of the prosperity of a company. Social networks in an organization include the trust among the employees, their satisfaction level with the job and also the quality of communications that take place with the peers, seniors and subordinates.

    Strong social networking, coupled with an efficient performance by the workforce, signifies a healthy state of affairs for the company. Social capital stresses the importance of these social networks and relationships and aims to use it in the best possible way for achieving organizational goals.

    Social capital might have its share of pros and cons, but if it is utilized properly, it can pave the way for an organization’s prosperity.

    Soft currency

    Soft currency is a currency which is hypersensitive and fluctuates frequently. Such currencies react very sharply to the political or the economic situation of a country.

    Soft loans

    A soft loan is basically a loan on comparatively lenient terms and conditions as compared to other loans available in the market. These easier conditions might be in the form of lower interest rates, prolonged repayment duration, etc.

    Special Drawing Rights

    This is a kind of reserve of foreign exchange assets comprising leading currencies globally and created by the International Monetary Fund in the year 1969.

    SDR is often regarded as a ‘basket of national currencies’ comprising four major currencies of the world – US dollar, Euro, British Pound and Yen (Japan). The composition of this basket of currencies is reviewed every five years wherein the weightage of currencies sometimes get altered.

    Statutory liquidity ratio

    The ratio of liquid assets to net demand and time liabilities (NDTL) is called the statutory liquidity ratio (SLR).

    Stimulus package

    The stimulus package is a package of tax rebates and incentives used by the governments of various countries to stimulate the economy and save their country from a financial crisis.

    Underwriting

    Underwriting is one of the most important functions in the financial world wherein an individual or an institution undertakes the risk associated with a venture, an investment, or a loan in lieu of a premium. Underwriters are found in banking, insurance, and stock markets.

    The nomenclature ‘underwriting’ came about from the practice of having risk takers to write their name below the total risk that s/he undertakes in return for a specified premium in the early stages of the industrial revolution.

    Velocity of circulation

     Velocity of circulation is the amount of units of money circulated in the economy during a given period of time.

    Velocity of circulation is measured by dividing GDP by the country’s total money supply. A high velocity of circulation in a country indicates a high degree of inflation. It helps in determining how vigorous a country’s economy is.

    Venture capital

    Start up companies with a potential to grow need a certain amount of investment. Wealthy investors like to invest their capital in such businesses with a long-term growth perspective. This capital is known as venture capital and the investors are called venture capitalists.

    Windfall gain

    Windfall gain (or windfall profit) is an unexpected gain in income which could be due to winning a lottery, unforeseen inheritance or shortage of supply. Windfall gains are transitory in nature.

     

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  • [Prelims Spotlight] Physiographic Divisions of India

     

    Prelims Spotlight is a part of “Nikaalo Prelims 2020” module. This open crash course for Prelims 2020 has a private telegram group where PDFs and DDS (Daily Doubt Sessions) are being held. Please click here to register.


    21 March 2020

    Let’s begin with the first physiographic division. It consists of:

    • THE HIMALAYAS, and
    • The Northeastern hills (Purvanchal).

    A) The Himalayas:

    The Himalayas are the highest and longest of all young fold mountains of the world. The Pamir, known as the roof of the world, connects the Himalayas with the high ranges of Central Asia.

    Let’s begin by understanding how the Himalayas came into being:

    About 40 to 50 million years ago, two large landmasses, India and Eurasia, driven by plate movement, collided. As a result, the sediments accumulated in Tethys Sea (brought by rivers) were compressed, squeezed and series of folds were formed, one behind the other, giving birth to folded mountains of the Himalayas.

    Recent studies show that India is still moving northwards at the rate of 5cm/year and crashing into the rest of Asia, thereby constantly increasing the height of Himalayas.

    The North-South division of the Himalayas

    The Himalayas consist of a series of parallel mountain ranges:

    1. The Greater Himalayan range, which includes:
      • The Great Himalayas(Himadri), and
      • The Trans-Himalayan range
    2. The Lesser Himalayas (or Himachal), and
    3. The Outer Himalayas (or Shiwalik).

    • Formation of these ranges: The Himadri and Himachal ranges of the Himalayas have been formed much before the formation of Siwalik range. The rivers rising in the Himadri and Himachal ranges brought gravel, sand and mud along with them, which was deposited in the rapidly shrinking Tethys Sea. In the course of time, the earth movements caused the folding of these relatively fresh deposits of sediments, giving rise to the least consolidated Shiwalik range.
    • Characteristic Features:
      • Notice in the map shown above that the Himalayas form an arcuate curve which is convex to the south. This curved shape of the Himalayas is attributed to the maximum push offered at the two ends on the Indian peninsula during its northward drift. In the north-west, it was done by Aravalis and in the Northeast by the Assam ranges.
      • Syntaxis/ Syntaxial bends: The gently arching ranges of the Himalayan mountains on their Western and Eastern extremities are sharply bent southward in deep Knee-bend flexures that are called syntaxial bends. On both the ends, the great mountains appear to bend around a pivotal point. The western point is situated south of the Pamir where the Karakoram meets the Hindu Kush. A similar sharp, almost hairpin bend occurs on the eastern limit of Arunachal Pradesh where the strike of the mountain changes sharply from the Easterly to Southerly trend. Besides these two major bends, there are a number of minor syntaxial bends in other parts of Himalayas.

        Syntaxial Bends of Himalayas

      • The Himalayas are wider in the west than in the east. The width varies from 400 km in Kashmir to 150 km in Arunachal Pradesh. The main reason behind this difference is that the compressive force was more in the east than in the west. That is why high mountain peaks like Mount Everest and Kanchenjunga are present in the Eastern Himalayas.
      • The ranges are separated by deep valleys creating a highly dissected topography.
      • The southern slopes of the Himalayas facing India are steeper and those facing the Tibetan side are generally gentler.
    • Let’s take up these Himalayan mountain ranges one by one:

      The Himalayan Ranges | the Greater Himalayan Range, the Lesser Himalayas, the Shivaliks

      Indus-Tsangpo Suture Zone: It represents a belt of tectonic compression caused by the underthrusting of the Indian shield/ plate against the Tibetan mass. It marks the boundary between the Indian and Eurasian plates. The suture zone stretches from the North-Western Himalayan syntaxis bordering the Nanga Parbat to the East as far as the Namche Barwa Mountain. The Karakoram Range and the Ladakh plateau lie to the north of ITSZ and originally formed a part of the European plate. Main Central Thrust Zone: This separates the Higher Himalayas in the north from lesser Himalayas in the south. It has played an important role in the tectonic history of these mountains. Main Boundary Thrust: It is a reverse fault of great dimensions which extends all the way from Assam to Punjab and serves to separate the outer Himalayas from the lesser Himalayas.Himalayan Frontal Fault: It is a series of reverse faults that demarcates the boundary of the Shivalik from of the Himalayan province from the alluvial expanse of the Indo-Gangetic plains.

    Major Faults of the Himalayas – ITSZ, MCT, MBT, HFF
    The Himalayan Complex: A Cross-sectional View

    Besides the longitudinal divisions, the Himalayas have been divided on the basis of regions from west to east:

    These divisions have been demarcated by river valleys:

    The Regional Divisions of Himalayas – the Western and Eastern Himalayas.
    1. Punjab Himalayas:
      • A large portion of Punjab Himalayas is in Jammu and Kashmir and Himachal Pradesh. Hence they are also called the Kashmir and Himachal Himalaya.
      • Major ranges: Karakoram, Ladakh, Pir Panjal, Zaskar and Dhaola Dhar.
      • The general elevation falls westwards.
      • The Kashmir Himalayas are also famous for Karewa formations.
        • ‘Karewas’ in Kashmiri language refer to the lake deposits, found in the flat-topped terraces of the Kashmir valley and on the flanks of the Pir Panjal range.
        • These deposits consist of clays, silts and sands, these deposits also show evidence of glaciation.
        • The occurrence of tilted beds of Karewas at the altitudes of 1500-1800m on the flanks of the Pir Panjal strongly suggests that the Himalayas were in process of uplift as late as Pliocene and Pleistocene (1.8mya to 10kyears ago)
        • Karewas are famous for the cultivation of Zafran, a local variety of saffron.
    2. Kumaon Himalayas
    3. Nepal Himalayas:
      • Tallest section of Himalayas
    4. Sikkim Himalayas:
      • Teesta river originates near Kanchenjunga
      • Jelep la pass- tri-junction of India- China-Bhutan
    5. Assam Himalayas:
      • The Himalayas are narrower in this region and Lesser Himalayas lie close to Great Himalayas.
      • Peaks: Namcha Barwa, Kula Kangri
      • Bengal ‘Duars’
      • Diphu pass- tri-junction of India- China-Myanmar
      • The Assam Himalayas show a marked dominance of fluvial erosion due to heavy rainfall.
    The West-East Division of Himalayas

    Glaciers and Snowline:

    Snowline: The lower limit of perpetual snow is called the ‘snowline’. The snowline in the Himalayas has different heights in different parts, depending on latitude, altitude, amount of precipitation, moisture, slope and local topography.

    1. The snowline in the Western Himalaya is at a lower altitude than in the Eastern Himalaya. E.g. while the glaciers of the Kanchenjunga in the Sikkim portion hardly move below 4000m, and those of Kumaon and Lahul to 3600m, the glaciers of the Kashmir Himalayas may descend to 2500m above the sea level.

    • It is because of the increase in latitude from 28°N in Kanchenjunga to 36°N in the Karakoram (Lower latitude —> warmer temperatures —> higher snowline).
    • Also, the Eastern Himalayas rise abruptly from the planes without the intervention of High ranges.
    • Though the total precipitation is much less in the western Himalayas, it all takes place in the form of snow.

    2. In the Great Himalayan ranges, the snowline is at a lower elevation on the southern slopes than on the northern slopes. This is because the southern slopes are steeper and receive more precipitation as compared to the northern slopes.

    Glaciers: The main glaciers are found in the Great Himalayas and the Trans-Himalayan ranges (Karakoram, Ladakh and Zaskar). The Lesser Himalayas have small glaciers, though traces of large glaciers are found in the Pir Panjal and Dhauladhar ranges. Some of the important glaciers are:

    Important Glaciers and their Locations

    Key differences between the Eastern and Western Himalayas:

    Key Difference between the Western and Eastern Himalayas.

    Important Passes in India:

    A pass is a narrow gap in a mountain range which provides a passageway through the barrier.

    Important Passes in India
    1. Pir Panjal Pass – It provides the shortest and the easiest metal road between Jammu and the Kashmir Valley. But this route had to be closed down as a result of partition of the subcontinent.
    2. Banihal Pass – It is in Jammu and Kashmir. The road from Jammu to Srinagar transversed Banihal Pass until 1956 when Jawahar Tunnel was constructed under the pass. The road now passes through the tunnel and the Banihal Pass is no longer used for road transport.
    3. Zoji La (Pass) – It is in the Zaskar range of Jammu and Kashmir. The land route from Srinagar to Leh goes through this pass.
    4. Shipki La (Pass) – It is in Himachal Pradesh. The road from Shimla to Tibet goes through this pass. The Satluj river flows through this pass.
    5. Bara Lacha Pass – It is also in Himachal Pradesh. It links Mandi and Leh by road.
    6. Rohtang Pass – It is also in Himachal Pradesh. It cuts through the Pir Panjal range. It links Manali and Leh by road.
    7. Niti Pass – It is in Uttarakhand. The road to the Kailash and the Manasarovar passes through it.
    8. Nathu La (Pass) – It is in Sikkim. It gives way to Tibet from Darjeeling and Chumbi valley. The Chumbi river flows through this pass.
    9. Jalep La (Pass) – At the tri-junction of India- China-Bhutan. The Teesta river has created this pass.

    B) The North-Eastern Hills and Mountains

    The North-Eastern Hills (Purvanchal): Patkai Bum, Naga Hills, Mizo Hills

    The Brahmaputra marks the eastern border of Himalayas. Beyond the Dihang gorge, the Himalayas bend sharply towards the south and form the Eastern hills or Purvanchal.

    • These hills run through the northeastern states of India.
    • These hills differ in scale and relief but stem from the Himalayan orogeny.
    • They are mostly composed of sandstones (i.e. Sedimentary rocks).
    • These hills are covered with dense forests.
    • Their elevation decreases from north to south. Although comparatively low, these hill ranges are rather forbidding because of the rough terrain, dense forests and swift streams.
    • Purvanchal hills are convex to the west.
    • These hills are composed of:
      • Patkai Bum – Border between Arunachal Pradesh and Myanmar
      • Naga Hills
      • Manipuri Hills – Border between Manipur and Myanmar
      • Mizo Hills.
    • Patkai Bum and Naga Hills form the watershed between India and Myanmar.
    • Extension of Purvanchal continues in Myanmar as Arakan Yoma –then Andaman and Nicobar Islands.
    Arakan Yoma – An Extension of Purvanchal in Myanmar

    The importance of Himalayan Region:

    1. Climatic Influence – The altitude of the Himalayas, their sprawl and extension intercept the summer monsoon. They also prevent the cold Siberian air masses from entering into India.
    1. Defence
    2. Source of perennial rivers
    3. Source of fertile soils
    4. Generation of hydroelectricity
    5. Forest wealth
    6. Orchards
    7. Minerals – The Himalayan region is rich in minerals e.g. gold, silver, copper, lead etc. are known to occur. Coal is found in Kashmir. But at the present level of technological advancement, it is not possible to extract these minerals. Also, it is not economically viable.
    8. Tourism
    9. Pilgrimage

    NORTHERN PLAINS

    Location and Extent:

    Northern plains are the youngest physiographic feature in India. They lie to the south of the Shivaliks, separated by the Himalayan Frontal Fault (HFF). The southern boundary is a wavy irregular line along the northern edge of the Peninsular India. On the eastern side, the plains are bordered by the Purvanchal hills.

    The Physiographic Divisions of India: the Northern Plains

    Formation of Northern Plains:

    Due to the uplift of the Himalayas in the Tethys Sea, the northern part of the Indian Peninsula got subsided and formed a large basin.

    northern-plains
    Source

    That basin was filled with sediments from the rivers which came from the mountains in the north and from the peninsula in the south. These extensive alluvial deposits led to the formation of the northern plains of India.

    Chief Characteristics:

    • The northern plain of India is formed by three river systems, i.e. the Indus, the Ganga and the Brahmaputra; along with their tributaries.
    • The northern plains are the largest alluvial tract of the world. These plains extend approximately 3200 km from west to east.
    • The average width of these plains varies between 150 and 300 km. In general, the width of the northern plains increases from east to west (90-100km in Assam to about 500km in Punjab).
    • The exact depth of alluvium has not yet been fully determined. According to recent estimates, the average depth of alluvium in the southern side of the plain varies between 1300-1400m, while towards the Shiwaliks, the depth of alluvium increases. The maximum depth of over 8000m has been reached in parts of Haryana.
    • The extreme horizontality of this monotonous plain is its chief characteristic (200m – 291m). The highest elevation of 291 m above mean sea level near Ambala forms a watershed between the Indus system and Ganga system).
    • The monotony of the physical landscape is broken at the micro-level by the river bluffs, levees etc.
      • [Floodplain – That part of a river valley, adjacent to the channel, over which a river flows in times of a flood.
      • Levee – An elevated bank flanking the channel of the river and standing above the level of the flood plain.
      • Bluff – A river cut cliff or steep slope on the outside of a meander. A line of bluffs often marks the edge of a former floodplain.]
    slide_34
    Source

    Physiographic Divisions of the Northern Plains:

    From the north to the south, the northern plains can be divided into three major zones:

    1. The Bhabar
    2. The Tarai
    3. The alluvial plains.

    The alluvial plains can be further divided into the Khadar and the Bhangar as illustrated below:

    Geomorphology of the Northern Plains

    Let’s understand these divisions one by one:

    Bhabar:

    • Bhabar is a narrow belt (8-10km wide) which runs in the west-east direction along the foot of the Himalayas from the river Indus to Teesta.
      alluvial-fan

      Source

    • Rivers which descend from the Himalayas deposit their load along the foothills in the form of alluvial fans.
    • These fans consisting of coarser sediments have merged together to build up the piedmont plain/the Bhabar.
    • The porosity of the pebble-studded rock beds is very high and as a result, most of the streams sink and flow underground. Therefore, the area is characterized by dry river courses except in the rainy season.
    • The Bhabar track is not suitable for cultivation of crops. Only big trees with large roots thrive in this region.
    • The Bhabar belt is comparatively narrow in the east and extensive in the western and north-western hilly region.

    Tarai:

    • It is a 10-20 km wide marshy region in the south of Bhabar and runs parallel to it.
    • The Tarai is wider in the eastern parts of the Great Plains, especially in the Brahmaputra valley due to heavy rainfall.
    • It is characterized by the re-emergence of the underground streams of the Bhabar belt.
    • The reemerged water transforms large areas along the rivers into badly drained marshy lands.
    • Once covered with dense forests, most of the Tarai land (especially in Punjab, Uttar Pradesh and Uttarakhand) has been reclaimed and turned into agricultural land over a period of time.

    Bhangar:

    • It is the older alluvium along the river beds forming terraces higher than the flood plain.
    • Dark in colour, rich in humus content and productive.
    • The soil is clayey in composition and has lime modules (called kankar)
    • Found in doabs (inter-fluve areas)
    • ‘The Barind plains’ in the deltaic region of Bengal and the ‘bhur formations’ in the middle Ganga and Yamuna doab are regional variations of Bhangar. [Bhur denotes an elevated piece of land situated along the banks of the Ganga river especially in the upper Ganga-Yamuna Doab. This has been formed due to accumulation of wind-blown sands during the hot dry months of the year]
    • In relatively drier areas, the Bhangar also exhibits small tracts of saline and alkaline efflorescence known as ‘Reh’, ‘Kallar’ or ‘Bhur’. Reh areas have spread in recent times with an increase in irrigation (capillary action brings salts to the surface).
    • May have fossil remains of even those plants and animals which have become extinct.

    Khadar:

    • Composed of newer alluvium and forms the flood plains along the river banks.
    • Light in colour, sandy in texture and more porous.
    • Found near the riverbeds.
    • A new layer of alluvium is deposited by river flood almost every year. This makes them the most fertile soils of Ganges.
    • In Punjab, the Khadar rich flood plains are locally known as ‘Betlands’ or ‘Bets’.
    • The rivers in Punjab-Haryana plains have broad flood plains of Khadar flanked by bluffs, locally known as Dhayas. These bluffs are as high as 3metres.

    Northern Plain: Regional Divisions

    The Regional Divisions of the Northern Plains: Punjab, Ganga and the Brahmaputra Plains.
    1. Punjab Plains:
    • The Punjab plains form the western part of the northern plain.
    • In the east, the Delhi-Aravalli ridge separates it from the Ganga plains.
    • This is formed by the Indus and its tributaries; like Jhelum, Chenab, Ravi, Beas and Sutlej. A major portion of these plains is in Pakistan.
    • It is divided into many Doabs (do-“two” + ab- “water or river” = “a region or land lying between and reaching to the meeting of the two rivers”).
      Khadar and Bhangar
    • Important features:
      • Khadar rich flood plains known as ‘Betlands’ or ‘Bets’.
      • The rivers in Punjab-Haryana plains have broad flood plains of Khadar flanked by bluffs, locally known as Dhayas.
      • The northern part of this plane adjoining the Shivalik hills has been heavily eroded by numerous streams, which are called Chhos.
      • The southwestern parts, especially the Hisar district is sandy and characterized by shifting sand-dunes.
    1. Ganga Plains:
    • The Ganga plains lie between the Yamuna catchment in the west to the Bangladesh border in the East.
    • The lower Ganga plain has been formed by the down warping of a part of Peninsular India between Rajmahal hills and the Meghalaya plateau and subsequent sedimentation by the Ganga and Brahmaputra rivers.
    • The main topographical variations in these plains include Bhabar, Tarai, Bhangar, Khadar, levees, abandoned courses etc.
    • Almost all the rivers keep on shifting their courses making this area prone to frequent floods. The Kosi river is very notorious in this respect. It has long been called the ‘Sorrow of Bihar’.
    • The northern states, Haryana, Delhi, UP, Bihar, part of Jharkhand and West Bengal in the east lie in the Ganga plains.
    • The Ganga-Brahmaputra delta: the largest delta in the world. A large part of the coastal delta is covered tidal forests called Sunderbans. Sunderbans, the largest mangrove swamp in the world gets its name from the Sundari tree which grows well in marshland. It is home to the Royal Tiger and crocodiles.
    1. Brahmaputra Plains:
    • This plain forms the eastern part of the northern plain and lies in Assam.
    • Its western boundary is formed by the Indo-Bangladesh border as well as the boundary of the lower Ganga Plain. Its eastern boundary is formed by Purvanchal hills.
    • The region is surrounded by high mountains on all sides, except on the west.
    • The whole length of the plain is traversed by the Brahmaputra.
    • The Brahmaputra plains are known for their riverine islands (due to the low gradient of the region) and sand bars.
    • The innumerable tributaries of the Brahmaputra river coming from the north form a number of alluvial fans. Consequently, the tributaries branch out in many channels giving birth to river meandering leading to the formation of bill and ox-bow lakes.
    • There are large marshy tracts in this area. The alluvial fans formed by the coarse alluvial debris have led to the formation of terai or semi-terai conditions.

    Significance of this region:

    • The plains constitute less than one-third of the total area of the country but support over 40 percent of the total population of the country.
    • Fertile alluvial soils, flat surface, slow-moving perennial rivers and favourable climate facilitate an intense agricultural activity.
    • The extensive use of irrigation has made Punjab, Haryana and western part of Uttar Pradesh the granary of India (Prairies are called the granaries of the world).
    • Cultural tourism: Several sacred places and centres of pilgrimage are situated in these plains e.g. Haridwar, Amritsar, Varanasi, Allahabad, Bodh Gaya etc.
    • The sedimentary rocks of plains have petroleum and natural gas deposits.
    • The rivers here have very gentle gradients which make them navigable over long distances.

     

    PENINSULAR PLATEAU

    A. Location and Extent

    • The Peninsular Plateau lies to the south of the Northern Plains of India.
    • It is bordered on all sides by the hill ranges:
    • Delhi ridge in the north-west (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 Physiographic Divisions of India | The Peninsular Plateau
    • Outlier:
      • Shillong and Karbi-Anglong plateau.

    Note: Kutchch Kathiawar region – The region, though an extension of Peninsular plateau (because Kathiawar is made of the Deccan Lava and there are tertiary rocks in the Kutch area), they are now treated as an integral part of the Western Coastal Plains as they are now levelled down.

    • The Garo-Rajmahal Gap:
      • The two disconnected outlying segments of the plateau region are seen in the Rajmahal and Garo-Khasi Jaintia hills.
      • It is believed that due to the force exerted by the northeastward movement of the Indian plate at the time of the Himalayan origin, a huge fault was created between the Rajmahal hills and the Meghalaya plateau
      • Later, this depression got filled up by the deposition activity of the numerous rivers.
      • As a result, today the Meghalaya and Karbi Anglong plateau stand detached from the main Peninsular Block.

    Geological History and Features:

    The peninsular plateau is a tableland which contains igneous and metamorphic rocks. It is one of the oldest and the most stable landmass of India.

    In its otherwise stable history, the peninsula has seen a few changes like:

    1. Gondwana Coal Formation.
    2. Narmada-Tapi rift valley formation.
    3. Basalt Lava eruption on Deccan plateau:

    During its journey northward after breaking off from the rest of Gondwana, the Indian Plate passed over a geologic hotspot, the Réunion hotspot, which caused extensive melting underneath the Indian Craton. The melting broke through the surface of the craton in a massive flood basalt event, creating what is known as the Deccan Traps (Its various features have been discussed in the later portion of the article).

    Chief Characteristics:

    The entire peninsular plateau region is an aggregation of several smaller plateaus and hill ranges interspersed with river basins and valleys. The Chhattisgarh plain occupied by the dense Dandakaranya forests is the only plain in the peninsula.

    1. General elevation and flow of rivers:

    • The average elevation is 600-900 metres.
    • The general elevation of the plateau is from the west to the east, which is also proved by the pattern of the flow of rivers.
    • Barring Narmada and Tapti all the major rivers lying to the south of the Vindhyas flow eastwards to fall into the Bay of Bengal.
    • The westward flow of Narmada and Tapi is assigned to the fact that they have been flowing through faults or rifts which were probably caused when the Himalayas began to emerge from the Tethys Sea of the olden times.

    2. Some of the important physiographic features of this region are:

    • Tors – Prominent, isolated mass of jointed, weathered rock, usually granite.
    A granite tor near Ranchi
    A granite tor near Ranchi
    • Block Mountains and Rift Valleys:
    • Spurs: A marked projection of land from a mountain or a ridge
    spur
    Image Source
    • Bare rocky structures,
    • Series of hummocky hills and wall-like quartzite dykes offering natural sites for water storage.
    • Broad and shallow valleys and rounded hills
    • Ravines and gorges: The northwestern 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.

    3. The Deccan Traps:

    • One of the most important features of the peninsular plateau is the black soil area in the western and northwestern part of the plateau, which is known as the Deccan Trap.
    • From the end of the Cretacious until the beginning of the Eocene, numerous fissure-type eruptions took place in the north-western part of the Deccan plateau. It is believed that the lava outpourings were more than the mass comprising the present-day Himalayas.
    • It covers a major portion of the Maharashtra plateau and parts of Gujarat, northern Karnataka and Malwa plateau. Some parts of Tamil Nadu, Andhra Pradesh, UP, and Jharkhand have some outliers of Deccan trap.
    • Basalt is the main rock of the region.
    • The region has black cotton soil as a result of weathering of this lava material and this soil is one of the finest examples of the parent material controlled soils.

    Physiographic Divisions:

    On the basis of prominent relief features, the peninsular plateau can be divided into three broad groups:

    • The Central Highlands
    • The Deccan Plateau
    • The Northeastern Plateau.
    Physiographic Divisions and Important Mountain Ranges of the Peninsular Plateau

    Let’s take up these divisions one by one:

    1. The Central Highlands

    • The northern segment of the peninsular plateau is known as the Central Highlands.
    • Location:
      1. North of Narmada river.
      2. They are bounded to the west by the Aravallis.
      3. Satpura ranges (formed by a series of scarped plateaus) lie in the South.
    • General Elevation: 700-1,000 m above the mean sea level and it slopes towards the north and northeastern directions.
    • These highlands consist of the:
      1. Marwar upland – to the east of Aravallis in Rajasthan
        • A rolling plain carved by Banas river. [Rolling Plain: ‘Rolling plains’ are not completely flat; there are slight rises and fall in the landform. Ex: Prairies of USA]
        • The average elevation is 250-500 m above sea level.
      2. Madhya Bharat Pathar – to the east of Marwar upland.
      3. Malwa plateau – It lies in Madhya Pradesh between Aravali and Vindhyas. It is composed of the extensive lava flow and is covered with black soils.
      4. Bundelkhand plateau – It lies along the borders of UP and MP. Because of intensive erosion, semi-arid climate and undulating area, it is unfit for cultivation.
      5. Baghelkhand plateau – It lies to the east of the Maikal range.
      6. Chhotanagpur plateau – the northeast part of Peninsular plateau.
        • It Includes Jharkhand, parts of Chhattisgarh and West Bengal.
        • This plateau consists of a series of step-like sub-plateaus (locally called peatlands – high-level plateau). It is thus famous as the Patland plateau and known as Ruhr of India.
        • Rajmahal Hills are the northeastern projection of Chhota Nagpur Plateau.
        • It is a mineral-rich plateau.
    • The extension of the Peninsular plateau can be seen as far as Jaisalmer in the West, where it has been covered by the longitudinal sand ridges and crescent-shaped sand dunes called barchans.
    • 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.
    • 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.
    Physiographic Divisions of the Peninsular Plateau – the Central Highlands and the Deccan Plateau

    2. The Deccan Plateau

    • The Deccan Plateau lies to the south of the Narmada River and is shaped as an inverted triangle.
    • It is bordered by:
      1. The Western Ghats in the west,
      2. The Eastern Ghats in the east,
      3. The Satpura, Maikal range and Mahadeo hills in the north.
    • It is volcanic in origin, made up of horizontal layers of solidified lava forming trap structure with step-like appearance. The sedimentary layers are also found in between the layers of solidified lava, making it inter–trapping in structure.
    • Most of the rivers flow from west to east.
    • The plateau is suitable for the cultivation of cotton; home to rich mineral resources and a source to generate hydroelectric power.
    • The Deccan plateau can be subdivided as follows:
      1. The Maharashtra Plateau – it has typical Deccan trap topography underlain by basaltic rock, the regur.
      2. The Karnataka Plateau (also known as Mysore plateau) – divided into western hilly country region of ‘Malnad’ and plain ‘Maidan’
      3. Telangana Plateau

    3. The Northeastern Plateau:

    • The Meghalaya (or Shillong) plateau is separated from peninsular rock base by the Garo-Rajmahal gap.
    • Shillong (1,961 m) is the highest point of the plateau.
    • The region has the Garo, Khasi, Jaintia and Mikir (Rengma) hills.
    • An extension of the Meghalaya plateau is also seen in the Karbi Anglong hills of Assam.
    • 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.

    Hill ranges of the peninsula:

    Most of the hills in the peninsular region are of the relict type (residual hills). They are the remnants of the hills and horsts formed many million years ago (horst: uplifted block; graben: subsided block).

    The plateaus of the Peninsular region are separated from one another by these hill ranges and various river valleys.

    Hill Ranges of the Peninsula

    1. The Aravalli Mountain Range:

    • It is a relic of one of the oldest fold mountains of the world.
    • Its general elevation is only 400-600 m, with few hills well above 1,000 m.
    • At present, it is seen as a discontinuous ridge from Delhi to Ajmer and rising up to 1722m (Gurushikhar peak in Mount Abu) and thence southward.
    • It is known as ‘Jarga’ near Udaipur and ‘Delhi Ridge’ near Delhi.
    • Dilwara Jain Temple, the famous Jain temple is situated on Mt. Abu.

    2. Vindhyan Ranges:

    • They rise as an escarpment running parallel to the Narmada-Son valley.
    • General elevation: 300 to 650 m.
    • Most of them are made up of sedimentary rocks of ancient ages.
    • They act as a watershed between Gangetic and peninsular river systems.

    3. Satpura ranges:

    • Satpura range is a series of seven mountains (‘Sat’ = seven and ‘pura’ = mountains).
    • The seven mountain ranges or folds of Satpura’s are:
      • Maikal Hills
      • Mahadeo Hills near Pachmarhi
      • Kalibhit
      • Asirgarh
      • Bijagarh
      • Barwani
      • Arwani which extends to Rajpipla Hills in Eastern Gujarat.
    • Satpura ranges run parallel between Narmada and Tapi, parallel to Maharashtra-MP border.
    • Dhupgarh (1,350 m) near Pachmarhi on Mahadev Hills is the highest peak of the Satpura Range.
    • Amarkantak (1,127 m) is another important peak. Amarkantak is the highest peak of the Maikal Hills from where two prominent rivers – the Narmada and the Son originate.
    • Note that three rivers originate from the three sides of Maikal hills (as shown in the following map) but, from Amarkantak, only two rivers (the Narmada and the Son) originate (and not Mahanadi).
    The Satpura Mountain Range

    4. Western and Eastern Ghats:

    • The Western Ghats:
      • These are a faulted part of the Deccan plateau running parallel from the Tapi valley to a little north of Kanyakumari (1600km). Their western slope is like an escarpment while eastern slope merges gently with the plateau.
      • Their average elevation is about 1,500 m with the height increasing from north to south.
    • The Eastern Ghats are in the form of residual mountains which are not regular but broken at intervals.
    • The Eastern and the Western Ghats meet each other at the Nilgiri hills.
    • A brief comparison between them:
    Differences between the Western and Eastern Ghats.
    A cross-sectional view through the Peninsular Plateau showing sharp relief contrast between the western and eastern margins

    Note: The Western Ghats are continuous and can be crossed through passes only. There are four main passes which have developed in the Western Ghats. These are:

    1. Thal Ghat – It links Nasik to Mumbai.
    2. Bhor Ghat – It links Mumbai to Pune.
    3. Pal Ghat – This pass is located between the Nilgiris and the Annamalai mountains. It is in Kerala and connects Kochi and Chennai.
    4. Senkota Pass – This pass located between the Nagercoil and the Cardamom hills links Thiruvananthapuram and Madurai.

    For the geographical location of these passes, see the following map:

    Important Passes in India

    Significance of the Peninsular Region:

    • Rich in mineral resources: The peninsular region of India is rich in both metallic and non-metallic minerals. About 98% of the Gondwana coal deposits of India are found in the peninsular region.
    • Agriculture: Black soil found in a substantial part of the peninsula is conducive for the cultivation of cotton, maize , citrus fruits etc. Some areas are also suitable for the cultivation of tea, coffee, groundnut etc.
    • Forest Products: Apart from teal, sal wood and other forest products, the forests of Western and Eastern Ghats are rich in medicinal plants and are home to many wild animals.
    • Hydel Power: many rivers, which have waterfalls. They help in the generation of hydroelectric power.
    • Tourism: There are numerous hill stations and hill resorts like Ooty, Mahabaleshwar, Khandala, etc.

    THE INDIAN DESERT

    The Indian desert is also known as the Thar Desert or the Great Indian Desert.

    Location and Extent:

    • Location – To the north-west of the Aravali hills.
    • It covers Western Rajasthan and extends to the adjacent parts of Pakistan.
    The Physiographic Divisions of India | The Indian Desert

    Geological History and Features

    • Most of the arid plain was under the sea from Permo-Carboniferous period and later it was uplifted during the Pleistocene age. This can be corroborated by the evidence available at wood fossils park at Aakal and marine deposits around Brahmsar, near Jaisalmer (The approximate age of the wood fossils is estimated to be 180 million years).
    • The presence of dry beds of rivers (eg Saraswati) indicates that the region was once fertile.
    • Geologically, the desert area is a part of the peninsular plateau region but on the surface, it looks like an aggradational plain.

    Chief Characteristics:

    • The desert proper is called the Marusthali (dead land) as this region has an arid climate with low vegetation cover. In general, the Eastern part of the Marushthali is rocky, while its western part is covered by shifting sand dunes.
    • Bagar: Bagar refers to the semi-desert area which is west of Aravallis. Bagar has a thin layer of sand. It is drained by Luni in the south whereas the northern section has a number of salt lakes.
    • The Rajasthan Bagar region has a number of short seasonal streams which originate from the Aravallis. These streams support agriculture in some fertile patches called Rohi.
    • Even the most important river ‘Luni’ is a seasonal stream. The Luni originates in the Pushkar valley of the Aravalli Range, near Ajmer and flows towards the southwest into the Rann of Kutch.
    • The region north of Luni is known as the Thali or sandy plain.
    • There are some streams which disappear after flowing for some distance and present a typical case of inland drainage by joining a lake or playa e.g. the Sambhar Lake. The lakes and the playas have brackish water which is the main source of obtaining salt.
    • Well pronounced desert land features:
      • Sand dunes: It is a land of undulating topography dotted with longitudinal dunes, transverse dunes and barchans. [Barchan – A crescent-shaped sand dune, the horns of which point away from the direction of the dominant wind; Longitudinal dune – A sand dune with its crest running parallel to the direction of prevailing wind]
    sand-dunes
    Image Source
    • Mushroom rocks
    • Shifting dunes (locally called Dhrians)
    • Oasis (mostly in its southern part)

     

    THE COASTAL PLAINS

    Of the total coastline of India (7517 km), that of the peninsula is 6100 km between the peninsular plateau and the sea. The peninsular plateau of India is flanked by narrow coastal plains of varied width from north to south.

    The Physiographic Divisions of India | The Coastal Plains

    On the basis of the location and active geomorphologic processes, these can be broadly divided into two parts:

    • The western coastal plains
    • The eastern coastal plains.

    We now take them up one by one:

    The Western Coastal Plain

    1. Extent: The Western Coastal Plains are a thin strip of coastal plains with a width of 50 km between the Arabian Sea and the Western Ghats.

    2. Subdivisions: Extending from the Gujarat coast in the north to the Kerala coast in the south, the western coast may be divided into following divisions:

    • Kachchh and Kathiawar coast in Gujarat,
    • Konkan coast in Maharashtra,
    • Goan Coast in Karnataka, and
    • Malabar coast in Kerala

    Note: Kutch and Kathiawar, though an extension of Peninsular plateau (because Kathiawar is made of the Deccan Lava and there are tertiary rocks in the Kutch area), they are still treated as an integral part of the Western Coastal Plains as they are now levelled down.

    Subdivisions of the eastern and Western Coastal Plains

    3. A coastline of submergence: The western coastal plains are an example of the submerged coastal plain. It is believed that the city of Dwaraka which was once a part of the Indian mainland situated along the west coast is submerged underwater.

    4. Characteristic Features:

    • The western coastal plains are narrow in the middle and get broader towards north and south. Except for the Kachchh and Kathiawar coastal region, these are narrower than their eastern counterpart.
    • The coast is straight and affected by the South-West Monsoon winds over a period of six months. The western coastal plains are thus wetter than their eastern counterpart.
    • The western coast being more indented than the eastern coast 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 western coastal plains are dotted with a large number of coves (a very small bay), creeks (a narrow, sheltered waterway such as an inlet in a shoreline or channel in a marsh) and a few estuaries. The estuaries, of the Narmada and the Tapi are the major ones.
    • The rivers flowing through this coastal plain do not form any delta. Many small rivers descend from the Western Ghats making a chain of waterfalls.
    • The Kayals – The Malabar coast has a distinguishing feature in the form of ‘Kayals’ (backwaters). These backwaters are the shallow lagoons or the inlets of the sea and lie parallel to the coastline. These are used for fishing, inland navigation and are important tourist spots. The largest of these lagoons is the Vembanad lake. Kochi is situated on its opening into the sea.

    The Eastern Coastal Plain

    1. Extent: The Eastern Coastal Plains is a strip of coastal plain with a width of 100 – 130 km between the Bay of Bengal and the Eastern Ghats

    2. Subdivisions: It can be divided into two parts:

    • Northern Circar: The northern part between Mahanadi and Krishna rivers. Additionally, the coastal tract of Odisha is called the Utkal plains.
    • Coromandel Coast (or Payan Ghat): The southern part between Krishna and Kaveri rivers.

    3. A coastline of emergence: The eastern coastal plain is broader and is an example of an emergent coast.

    4. Characteristic features:

    • The eastern coastal plains are wider and drier resulting in shifting sand dunes on its plains.
    • 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 continental shelf extends up to 500 km into the sea, which makes it difficult for the development of good ports and harbours.
    • Chilika lake is an important feature along the eastern coast. It is the largest saltwater lake in India.

    Significance of the Coastal Plains region:

    1. These plains are agriculturally very productive. The western coast grows specialized tropical crops while eastern coasts witnessed a green revolution in rice.
    2. The delta regions of eastern coastal plains have a good network of canals across the river tributaries.
    3. Coastal plains are a source of salt, monazite (used for nuclear power) and mineral oil and gas as well as centres of fisheries.
    4. Although lacking in adequate natural harbours, with a number of major and minor ports, coastal plains are centres of commerce and have attracted dense human settlements.
    5. The coastal regions of India are noted for tourist centres, fishing and salt making.

     

    THE ISLANDS

    There are two major island groups in India

    1. The island groups of Bay of Bengal: Andaman & Nicobar Islands
    2. The island groups of Arabian Sea: Lakshadweep and Minicoy Islands
    The Physiographic Divisions of India | The Islands

    Let’s take these up one by one:

    Andaman & Nicobar Islands:

    • Also called the emerald islands.
    • Location and Extent:
      • These are situated roughly between 6°N-14°N and 92°E -94°E.
      • The most visible feature of the alignment of these islands is their narrow longitudinal extent.
      • These islands extend from the Landfall Island in the north (in the Andamans) to the Indira Point (formerly known as Pygmalion Point and Parsons Point) in the south (In the Great Nicobar).
    • Origin: The Andaman and Nicobar islands have a geological affinity with the tertiary formation of the Himalayas, and form a part of its southern loop continuing southward from the Arakan Yoma.
    • The entire group of islands 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.

    • The Andaman islands are further divided into:
      • Great Andamans
        • North Andaman
        • Middle Andaman
        • South Andaman
      • Little Andaman

    Little Andaman is separated from the Great Andamans by the Duncan Passage.

    The Andaman and Nicobar Islands
    • Chief Characteristics:
      • These are actually a continuation of Arakan Yoma mountain range of Myanmar and are therefore characterized by hill ranges and valleys along with the development of some coral islands.
      • Some smaller islands are volcanic in origin e.g. the Barren island and the Narcondam Island. Narcondam is supposed to be a dormant volcano but Barren perhaps is still active.
      • These islands make an arcuate curve, convex to the west.
      • These islands are formed of granitic rocks.
      • The coastal line has some coral deposits and beautiful beaches.
      • These islands receive convectional rainfall and have an equatorial type of vegetation.
      • These islands have a warm tropical climate all year round with two monsoons.
      • The Saddle peak (North Andaman – 738 m) is the highest peak of these islands.
      • The Great Nicobar is the largest island in the Nicobar group and is the southernmost island. It is just 147 km away from the Sumatra island of Indonesia.

    Lakshadweep Islands:

    • These islands were earlier (before 1st November 1973) known as Laccadive, Minicoy and Amindivi Islands.
    • Location:
      • These are scattered in the Arabian Sea between 8°N-12°N and 71°E -74°E longitude.
      • These islands are located at a distance of 280 km-480 km off the Kerala coast.
    • Origin: The entire island group is built of coral deposits.
    • Important islands:
      • Amindivi and Cannanore islands in the north.
      • Minicoy (lies to the south of the nine-degree channel) is the largest island with an area of 453 sq. km.
    map_of_lakshadweep-en-svg
    Source
    • Chief Characteristics:
      • These consist of approximately 36 islands of which 11 are inhabited.
      • These islands, in general, have a north-south orientation (only Androth has an East-West orientation.
      • These islands are never more than 5 metres above sea level.
      • These islands have calcium-rich soils- organic limestones and scattered vegetation of palm species.
      • One typical feature of these islands is the formation of the crescentic reef in the east and a lagoon in the west.
      • Their eastern seaboard is steeper.
      • The Islands of this archipelago have storm beaches consisting of unconsolidated pebbles, shingles, cobbles and boulders on the eastern seaboard.
      • The islands form the smallest Union Territory of India.

    Other than the above mentioned two major groups, the important islands are:

    1. Majauli: in Assam. It is:
      1. The world’s largest freshwater (Brahmaputra river) island.
      2. India’s first island district
    2. Salsette: India’s most populous island. Mumbai city is located on this island.
    3. Sriharikota: A barrier island. On this island is located the satellite launching station of ISRO.
    4. Aliabet: India’s first off-shore oil well site (Gujarat); about 45 km from Bhavnagar, it is in the Gulf of Khambat.
    5. New Moore Island: in the Ganga delta. It is also known as Purbasha island. It is an island in the Sunderban deltaic region and it was a bone of contention between India and Bangladesh. In 2010, it was reported to have been completely submerged by the rising seawater due to Global warming.
    6. Pamban Island: lies between India and Sri Lanka.
    7. Abdul Kalam Island: The Wheeler Island near the Odisha coast was renamed as Abdul Kalam island in 2015. It is a missile launching station in the Bay of Bengal. The first successful land-to-land test of the Prithvi Missile was conducted from the mainland and it landed on the then uninhabited ‘Wheeler Island’ on November 30, 1993.
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