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6th Apr 2022

Dear Aspirants,

This Spotlight is a part of our Mission Nikaalo Prelims-2022

Session Details

Morning 12 PM  – Prelims Spotlight Session

Evening 06:30  PM  – TIKDAM/MCQs Session

Noon 03:00 PM – CSAT Google Meet Session

Evening 08 PM  – Tests on Alternate Days

Download Habitat app from the Playstore Join our Official Civilsdaily Space for GS and CSAT Here

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However, no money can be withdrawn for meeting expenses until the government gets the approval of the Parliament.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.

Fiscal Performance Index (FPI)

• The composite FPI developed by CII is an innovative tool using multiple indicators to examine the quality of Budgets at the Central and State levels.
• The index has been constructed using UNDP’s Human Development Index methodology which comprises six components for holistic assessment of the quality of government budgets, subsidies, pensions and defence in GDP
• Quality of capital expenditure: measured by the share of capital expenditure (other than defence) in GDP
• Quality of revenue: the ratio of net tax revenue to GDP (own tax revenue in case of States)
• Degree of fiscal prudence I: fiscal deficit to GDP
• Degree of fiscal prudence II: revenue deficit to GDP and
• Debt index: Change in debt and guarantees to GDP

Other measures of FPI

• As per the new index, expenditure on infrastructure, education, healthcare and other social sectors can be considered beneficial for economic growth.

Sabka Vishwas-Legacy Dispute Resolution Scheme

• This Scheme is introduced to resolve and settle legacy cases of the Central Excise and Service Tax.
• The proposed scheme would cover all the past disputes of taxes which may have got subsumed in GST; namely Central Excise, Service Tax and Cesses.
• The Government expects the Scheme to be availed by a large number of taxpayers for closing their pending disputes relating to legacy Service Tax and Central Excise cases that are now subsumed under GST so they can focus on GST.
• The Scheme is, especially, tailored to free a large number of small taxpayers of their pending disputes with the tax administration.

Components of the Scheme

• The two main components of the Scheme are dispute resolution and amnesty.
• The dispute resolution component is aimed at liquidating the legacy cases of Central Excise and Service Tax that are subsumed in GST and are pending in litigation at various forums.
• The amnesty component of the Scheme offers an oppor­tunity to the taxpayers to pay the outstanding tax and be free of any other consequence under the law.
• The most attractive aspect of the Scheme is that it provides substantial relief in the tax dues for all categories of cases as well as full waiver of interest, fine, penalty,
• In all these cases, there would be no other liability of interest, fine or penalty. There is also a complete amnesty from prosecution.

Direct Tax Code:

• The Direct Tax Code (DTC) is an attempt by the Govern­ment of India to simplify the direct tax laws in India.
• It will revise, consolidate and simplify the structure of direct tax laws in India into a single legislation.
• When implemented, it will replace the Income-tax Act, 1961 (ITA), and other direct tax legislation like the Wealth Tax Act, 1957.
• The task force was constituted by the government to frame draft legislation for this proposed DTC in November 2017 and review the existing Income Tax Act.

Direct Tax:

• These are the taxes, paid directly to the government by the taxpayer. Under the direct tax system, the incidence and impact of taxation fall on the same entity, which cannot be transferred to another person.
• It is termed as a progressive tax because the proportion of tax liability rises as an individual or entity’s income increases.
• Examples- Income tax, corporate tax, Dividend Distri­bution Tax, Capital Gain Tax, Security Transaction Tax.
• The system of Direct taxation is governed by the Cen­tral Board of Direct Taxes (CBDT). It is a part of the Department of Revenue in the Ministry of Finance.

Corporate Tax

• A corporate tax also popularly known as the company tax or the corporation tax is the tax levied on the capital or income of corporations or analogous legal entities.
• In most countries, such taxes are levied at the national level, and a tax that is similar to that imposed at the na­tional level could be imposed at the local or state levels.
• The taxes could also be termed as capital tax or income tax.
• Generally, Partnership firms are not taxed at the entity level.
• In most of nations, the corporations functioning in a country are taxed for the income from that country.
• Many countries tax all income of corporations incorpo­rated in the country or those deemed to be resident for tax purposes in the country.
• The income of the company that is to be taxed is computed similarly to the taxable income for individuals.
• Tax is generally imposed on net profits.
• In India, companies, both private and public which are registered in India under the Companies Act 1956, are liable to pay corporate tax.

Securities transaction tax (STT)

• Sale of any asset (shares, property) results in loss or profit. Depending on the time the asset is held, such profits and losses are categorised as long-term or short-term capital gain/loss.
• In Budget 2004-05, the government abolished long-term capital gains tax on shares (tax on profits made on the sale of shares held for more than a year) and replaced it with STT.
• It is a kind of turnover tax where the investor has to pay a small tax on the total consideration paid/received in a share transaction.

Banking cash transaction tax (BCTT)

• Introduced in Budget 2005-06, BCTT is a small tax on cash withdrawal from bank exceeding a particular amount in a single day.
• The basic idea is to curb the black economy and generate a record of big cash transactions

Cess

• This is an additional levy on the basic tax liability Governments resort to cess for meeting specific expenditure. For instance, both corporate and individual income is at present subject to an education cess of 2%.
• In the last Budget, the government had imposed another 1% cess – secondary and higher education cess on income tax – to finance secondary and higher education.

Countervailing Duties (CVD)

• Countervailing duty is a tax imposed on imports, over and above the basic import duty CVD is at par with the excise duty paid by the domestic manufacturers of similar goods
• This ensures a level playing field between imported goods and locally-produced ones.
• An exemption from CVD places the domestic industry at the disadvantage and over long run discourages investments in affected sectors.

Export Duty

• This is a tax levied on exports. In most instances, the object is not revenue, but to discourage exports of certain items.
• In the last Budget, for instance, the government imposed an export duty of Rs 300 per metric tonne on the export of iron ores and concentrates and Rs 2,000 per metric tonne on the export of chrome ores and concentrates.

Pass-through Status

• A pass-through status helps avoid double taxation. Mutual funds, for instance, enjoy pass-through status.
• The income earned by the funds is tax-free. Since mutual funds’ income is distributed to the unit-holders, who are in turn taxed on their income from such investments any taxation of mutual funds would amount to double taxation.
• Essentially, it means the income is merely passing through the mutual funds and, therefore, should not be taxed.
• The government allows venture funds in some sectors pass-through status to encourage investments in start-ups.

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Dear Aspirants,

This Spotlight is a part of our Mission Nikaalo Prelims-2022.

You can check the broad timetable of Nikaalo Prelims here

Session Details

Morning 12 PM  – Prelims Spotlight Session

Evening 06:30  PM  – TIKDAM/MCQs Session

Noon 03:00 PM – CSAT Google Meet Session

Evening 08 PM  – Tests on Alternate Days

Join our Official Civilsdaily Space for GS and CSAT Here

04 Apr 2022

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.

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:

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.

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:

Key differences between the Eastern and Western Himalayas:

Important Passes in India:

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

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 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.

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.

2. Defence
3. Source of perennial rivers
4. Source of fertile soils
5. Generation of hydroelectricity
6. Forest wealth
7. Orchards
8. 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.
9. Tourism
10. 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.

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.

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.]

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:

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.
  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.

2. 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.

3. 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.

• 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.

• Block Mountains and Rift Valleys:
• Spurs: A marked projection of land from a mountain or a ridge

• 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.

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.

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.

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).

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:

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:

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.

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]

• 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.

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.

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

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.

• 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 1^st 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.

• 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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Context

The Rajya Sabha recently bade farewell to 72 members retiring this year as Prime Minister Narendra Modi hailed their contribution and MPs fondly reminisced on their experiences.

In this article, we will discuss and analyze the journey, significance and achievements of the Upper House of Parliament – Rajya Sabha.

The Rajya Sabha

• The Rajya Sabha or Council of States is the upper house of the bicameral Parliament.
• It currently has a maximum membership of 245, of which 233 are elected by the legislatures of the states and union territories using single transferable votes through Open Ballot.
• The President can appoint 12 members for their contributions to art, literature, science, and social services.
• Members sit for terms lasting six years, with elections every year but almost a third of the 233 designates up for election every two years, specifically in even-numbered years.

A Historical background

• The Rajya Sabha came into being on April 3, 1952, and held its first session on May 13 the same year.
• The Constituent Assembly, which was formed in 1947, after the adoption of the Constitution became the Provisional Parliament and made laws till 1952.

Before its existence

• The central legislature that came into being under the Government of India Act, 1919 was bicameral.
• Under 1919 Act, Council of States had 60 members and Legislative Assembly had 145 members.
• The membership and voting norms for the Council of States were restrictive. These restrictions meant only wealthy landowners, merchants and those with legislative experience could enter it.
• Women could neither vote nor seek membership.
• The Government of India Act, 1935 proposed an elaborate and improved version of the second chamber, but this never materialized.

Elections to the Rajya Sabha

Qualifications

Article 84 of the Constitution lays down the qualifications for membership of Parliament. A member of the Rajya Sabha must:

• Be a citizen of India;
• Be at least 30 years old. (Article 84 constitution of India)
• Be elected by the Legislative Assembly of States and UTs by means of the single transferable vote through proportional representation.
• Not be: a proclaimed criminal, a subject of an insolvent, of unsound mind.
• Not hold any other office of profit under the Government of India.
• Possess such other qualifications as may be prescribed in that behalf by or under any law made by Parliament.

In addition, twelve members are nominated by the President of India having special knowledge in various areas like arts and science. However, they are not entitled to vote in Presidential elections as per Article 55 of the Constitution.

Election procedure

• Candidates fielded by political parties have to be proposed by at least 10 members of the Assembly or 10% of the party’s strength in the House, whichever is less.
• For independents, there should be 10 proposers, all of whom should be members of the Assembly.

Voting procedure

• Voting is by single transferable vote, as the election is held on the principle of proportional representation.
• A single transferable vote means electors can vote for any number of candidates in order of their preference.
• A candidate requires a specified number of first preference votes to win. Each first choice vote has a value of 100 in the first round.
• To qualify, a candidate needs one point more than the quotient obtained by dividing the total value of the number of seats for which elections are taking place plus one.
• The formula simply is [(Number of MLAs X 100) / (Vacancies + 1)] + 1.

Example: If there are four seats and 180 MLAs voting, the qualifying number will be 180/5= 36 votes or value of 3,600.

Note: The Rajya Sabha polls have a system of the open ballot, but it is a limited form of openness. There is a system of each party MLA showing his or her marked ballots to the party’s authorised agent (called Whip), before they are put into the ballot box.

The NOTA option has been struck down by the Supreme Court in RS elections.

The Power Equation: Lok Sabha Vs. Rajya Sabha

The Indian Constitution provides for parity of powers between the Lok Sabha and the Rajya Sabha in law, making an exception in some cases.

The Money Bill or Finance Bills can be introduced only in the Lok Sabha which only can approve the Demands for Grants.

On the other hand, the Rajya Sabha has some special powers as requiring adopting a resolution allowing Parliament to legislate on subjects in the State List and creating All India Services, besides approving proclamations of Emergency and President’s Rule when the Lok Sabha is dissolved.

Renowned British philosopher and political economist John Stuart Mill as early as in 1861 said in his great treatise Considerations on Representative Government that management of free institutions requires conciliation; a readiness to compromise; a willingness to concede something to opponents and mutual give and take. Truly, Rajya sabha plays this role in Indian legislature.

In detail: Powers and Functions of the Rajya Sabha

[1] Legislative Powers:

• In the sphere of ordinary law-making, the Rajya Sabha enjoys equal powers with the Lok Sabha. An ordinary bill can be introduced in the Rajya Sabha and it cannot become a law unless passed by it.
• In case of a deadlock between the two Houses of Parliament over an ordinary bill and if it remains unresolved for six months, the President can convene a joint sitting of the two Houses for resolving the deadlock.
• This joint sitting is presided over by the Speaker of the Lok Sabha. But if the deadlock is not resolved, the bill is deemed to have been killed.

[2] Financial Powers:

• In the financial sphere, the Rajya Sabha is a weak House.
• A money bill cannot be introduced in the Rajya Sabha. It can be initiated only in the Lok Sabha.
• A money bill passed by the Lok Sabha comes before the Rajya Sabha for its consideration.

[3] Executive Powers:

• Members of the Rajya Sabha can exercise some control over the ministers by criticizing their policies, by asking questions and moving motions etc.
• Some of the ministers are also taken from the Rajya Sabha. The PM can also be from Rajya Sabha if the majority party in the Lok Sabha may elect/adopt him as its leader.

[4] Electoral Powers:

• The Rajya Sabha has some electoral powers also. The elected members of the Rajya Sabha along with the elected members of the Lok Sabha and all the State Legislative Assemblies together elect the President of India.
• The members of the Rajya Sabha Lok Sabha together elect the Vice- President of India.
• Members of the Rajya Sabha also elect a Deputy Chairman from amongst themselves.

[5] Judicial Powers:

• The RS acting along with the Lok Sabha can impeach the President on charges of violation of the Constitution.
• The RS can also pass a special address for causing the removal of a judge of the Supreme Court or of any High Court.
• The charges against the Vice-President can be levelled only in the RS.
• The RS can pass a resolution for the removal of some high officers like the Attorney General of India, Comptroller and Auditor General and Chief Election Commissioner.

[6] Miscellaneous Powers:

The Rajya Sabha and Lok Sabha jointly perform the following functions:

• Approval of the ordinances issued by the President,
• Ratification of an emergency proclamation,
• Making any change in the jurisdiction of the Supreme Court and the High Courts, and
• Making any change in the qualifications for the membership of the Lok Sabha and the Rajya Sabha.

[7] Exclusive Powers

The Rajya Sabha enjoys two exclusive powers:

(i) The Power to declare a Subject of State List as a subject of National Importance:

The Rajya Sabha can pass a resolution by 2/3rd majority of its members for declaring a State List subject as a subject of national importance. Such a resolution empowers the Union Parliament to legislate on such a state subject for a period of one year. Such resolutions can be repeatedly passed by the Rajya Sabha.

(ii) Power in respect of Creation or Abolition of an All India Service:

The Rajya Sabha has the power to create one or more new All India Services. It can do so by passing a resolution supported by 2/3rd majority on the plea of national interest. In a similar way, the Rajya Sabha can disband an existing All India Service.

Limitations to its powers

The Constitution places some restrictions on Rajya Sabha; the Lok Sabha is more powerful in certain areas as such:

1. Money bills

• A money bill can be introduced only in the Lok Sabha by a minister and only on recommendation of President of India.
• When the Lok Sabha passes a money bill then the Lok Sabha sends money bill to the Rajya Sabha for 14 days during which it can make recommendations.
• Even if Rajya Sabha fails to return the money bill in 14 days to the Lok Sabha, that bill is deemed to have passed by both the Houses.

Also, if the Lok Sabha rejects any (or all) of the amendments proposed by the Rajya Sabha, the bill is deemed to have been passed. Hence, Rajya Sabha can only give recommendations for a money bill but Rajya Sabha cannot amend a money bill.

There is no joint sitting of both the houses with respect to money bills, because all final decisions are taken by the Lok Sabha.

2. Joint Sitting of the Parliament

• Article 108 provides for a joint sitting of the two Houses of Parliament in certain cases.
• Considering that the numerical strength of Lok Sabha is more than twice that of Rajya Sabha, Lok Sabha tends to have a greater influence in a joint sitting of Parliament.  A joint session is chaired by the Speaker of Lok Sabha.

Joint sessions of Parliament are a rarity, and have been convened only three times in last 71 years, for the purpose of passage of a specific legislative act, the latest time being in 2002:

• 1961: Dowry Prohibition Act, 1958
• 1978: Banking Services Commission (Repeal) Act, 1977
• 2002: Prevention of Terrorism Act, 2002

 3. No confidence motion:

• The Union Council of Ministers is collectively responsible before the Lok Sabha and not the Rajya Sabha.
• Lok Sabha alone can cause the fall of the Council of Ministers by passing a vote of no-confidence.

Rajya Sabha: A destructionist?

• An analysis by the Secretariat revealed that the productivity of the Rajya Sabha till 1997 has been 100% and above and the past 23 years have thrown up a disturbing trend of rising disruptions.
• This decline is primarily on account of disruptions forcing cancellation of Question Hour frequently.
• Disruptions also dent the quality of law-making as seen in passing of Bills without discussion sometimes.
• However, the Rajya Sabha is proving to be more and more a ‘deliberative’ body with increasingly more time being spent on this function.
• According to various members of Lok Sabha, Rajya Sabha has done nothing except stalling legislative works and causing policy paralysis in the country.
• For critics, the Upper House serves no purpose as its members are not directly elected and hence are not accountable to the people.
• Rajya Sabha often has members from the party defeated in various elections, or are from political families, and due to political differences, they do not allow passage of important bills.
• So many extra members are an added burden on exchequer which can be done away with.
• Politics of boycotting and creating ruckus in the house and toeing on the party-line even on the issue that won’t attract disqualification provisions is a worrying thing.
• At the same time, in terms of working, Rajya Sabha does not have sufficient powers in financial matters to bring any change and they are without any direct public interaction. Hence its purpose in modern democracy seems outdated.

Importance of Rajya Sabha and Why It Should Continue

• According to President Radhakrishnan, there are functions, which a revising chamber like Rajya Sabha can fulfil fruitfully. Parliament is not only a legislative but a deliberative body. So far as its deliberative functions are concerned, Rajya Sabha has made very valuable contributions time and again.
• It’s true that party dynamics affects the working of Rajya Sabha. But in democracy passion often defeat the normal rationality. Thus a revising house is needed to check such adrenal rush.
• While the argument of members not able to win in direct elections holds true, but retaining talent is essential for any democratic system. Losing valuable talent during election fervours has mostly been corrected by Rajya Sabha. It has also given entry to other experts like scientist, artist, sportsmen etc that can rarely face the electoral politics.
• While Lok Sabha have members for each state, the Hindi belt domination is a constant theme. Hence other state interests, like those in North East, have always been taken up by the Rajya Sabha.
• While it can’t bring no confidence motion or amend money bill, its role in checking arbitrariness of government as reflected in Land Ordinance, is necessary in democracy. Besides its special role in All India Services, legislation in State List too necessitates its existence.
• Men and women of prodigious talent and calibre have adorned the benches of the upper house and have contributed significantly towards realising the vision of the founding fathers of the Constitution.
• A permanent Upper House is also a check against any abrupt changes in the composition of the Lower House.
• Rajya Sabha has continuity and is a permanent house.
• Unlike Lok Sabha, it cannot be dissolved by anyone. Thus it has, time and often, carried out some administrative functions even when the lower house is dissolved. It has members with experienced players while there may be new entrants in the Lok Sabha.

By virtue of this, Rajya Sabha can’t be said to be ‘obstructive’.

Conclusion

A study of the powers of the Rajya Sabha leads us to the conclusion that it is neither a very weak house like the British House of Lords nor a very powerful house as the American Senate. Its position is somewhat mid-way between the two. It has been less powerful than Lok Sabha but it has been not a very weak or insignificant House.

Instead of engaging in the debate of if we need upper house or not, more constructive outlook would be improve it’s functioning. Clearly, the recommendations are present from NCRWC to 2nd ARC. The need is implementation and political support.