India Flashcards

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1
Q

Describe the divisions of Himalayas and their characteristic

A

Shivalik - accumulation of conglomerate initial stage, rivers cut lakes and fill with deposits= duars / duns

Lesser Himalaya - Pir Panjal, dhauladhar, Kangra Kullu valley

Great Himachal - Himadri, Granite , metamorphosed, MT Everest

Trans Himalaya = zaskar Ladakh Karakoram and Kailash range

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2
Q

Discuss the significance of Himalayas

A
  1. Precipitation at the Ganga plains
  2. Direct monsoon winds towards north west
  3. Bring the subtropical jet stream hence monsoon to India If there was no Himalayas India would be arid and cold
  4. . Fertile soil
  5. Source of perineal Rivers
  6. Hydroelectric
  7. Coniferous and alpine forests
  8. Agriculture- Shivalik tea , grapes apples mulberry walnut
  9. Coal at Kashmir copper lead zinc gold precious stones
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3
Q

How are the Ganga plains formed

A

The basin is formed as a result of the many tributaries from Ganga and Brahmaputra river.They cut and then deposited

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4
Q

What is the significance of the Ganga Brahmaputra plain

A

This 1/4 of the land of the country
hosts half of the Indian population.

Fertile alluvial soils, flat surface, slow moving perennial rivers and favorable climate facilitate 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).

The entire plain except the Thar Desert, has a close network of roads and railways which has led to large scale industrialization and urbanization.

Cultural tourism: There are many religious places along the banks of the sacred rivers like the Ganga and the Yamuna which are very dear to Hindus.

Here flourished the religions of Budha and Mahavira and the movements of Bhakti and Sufism.

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5
Q

Discuss the divisions of the Ganga Brahmaputra plane

A
Bhabhar = porous along the foothills , alluvial fans merge and rivers disappear 
Tarai = damp, and rivers re-emerged
Bhangar = old alluvium 
Khadar = new alluvium
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6
Q

State the significance of the plateau region

A

A storehouse of minerals: Most of the minerals in the world are found in plateaus. The extraction of minerals in plateaus is relatively easier on plateaus than mountains.

The major portions of industrial raw materials are obtained from plateaus.

We get gold from the plateau of Western Australia; copper, diamond and gold from the plateaus of Africa;
and coal, iron, manganese and mica from the Chottanagpur Plateau in India.

Generation of hydel-power: The edges of plateaus form waterfalls which provide ideal sites for generating hydel power.

Cool climate: The higher parts of the plateaus even in tropical and sub-tropical regions have a cool climate.

Animal rearing and agriculture: plateaus have large grassland areas suitable for animal rearing especially sheep, goat, and cattle.

The lava plateaus when compared to other plateaus are richer in minerals and hence used for agriculture as the soil is very fertile.

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7
Q

How are plateaus classified

A
Intermontane Plateaus
Piedmont plateaus- at foot of mt
Continental plateaus- due to upliftment
Volcanic plateaus
Dissected plateaus
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8
Q

State the characteristics of the eastern and the western ghats

A

Western Ghats:-
♥Height: Their height is 900 to 1,600 meters. The highest peak of this region is from Anaimudi with a height of 2,659 km.
♥Slope: They have steep slope as height increases from North to South
♥Continuity: They are continuous and can be crossed through passes only.
♥Rivers:They lie parallel to Western Coast and are source for some rivers.
♥Vegetation:Western Ghats have tropical evergreen forests.They are evergreen to deciduous forests.

Eastern Ghats:-
♥Height: The Eastern Ghats are lower in height than the Western Ghats. It ranges from 600 to 900 meters. Mahendragri 1501 m is the highest peak in Eastern Ghats.
♥Slope :They have a gentle slope.
♥Continuity: They are irregular and discontinuous and dissected by the rivers.
♥Rivers: hey stretch from Mahanadi valley to Niligiris in South. The rivers flow through easily.
♥Vegetation: Eastern Ghats have scrub vegetation due to over-grazing and deforestation…

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9
Q

Why is the western ghats continuous and the eastern ghats dissected

A

The slope of the Penninsular Plateau of India is from west to east
Godavari Krishna Kaveri rivers emerge from the western cards and flow to the east they come about the hills of the Eastern Ghats and made the Bay of Bengal

There is no large river in the western guards hence it is continuous

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10
Q

Draw a diagram of ocean relief

A
Abyssal plains 
Continental shelf 
Continental slope
Submarine canyon, 
seamount, 
guyot
 Volcanic island
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11
Q

What is SHOAL

A

Natural submerged ridge

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12
Q

What are marginal seas give example

A

A marginal sea basin, also called a back-arc basin, is a series of small sea basins located between a continent and island arc or among island arcs
South China Sea, black sea,

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13
Q

What are the concerns regarding marginal sees

A

Marginal seas are more susceptible to pollution than open ocean regions because of the high concentration of human activities near coastlines and rivers.

human impact on marginal seas is related to the fisheries industry.

Ninety percent of the world’s fisheries exist within coastal waters that are located less than 200 kilometers (124 miles) from the shoreline.

industrial sewage disposal, offshore oil drilling, and accidental releases of pollutants, including petroleum products, radioactive waste, detergents, and plastics

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14
Q

What is the gulf

A

A gulf is a large body of water, sometimes with a narrow mouth, that is almost completely surrounded by land. The world’s largest gulf is the Gulf of Mexico.

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15
Q

What is a Strait

A

A strait is a narrow passageway of water, usually between continents or islands, or between two larger bodies of water.

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16
Q

What is ithmus

A

Isthmus is the land-equivalent of a strait. i.e., a narrow strip of land connecting two larger land masses.

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17
Q

What is a bay

A

A bay is a body of water partially surrounded by land. A bay is usually smaller and less enclosed than a gulf. The mouth of the bay, where meets the ocean or lake, is typically wider than that of a gulf.

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18
Q

The Indus river system consists of which states

A

Jammu Kashmir Himachal Pradesh and Punjab

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19
Q

Discuss the origin of each river in the Indus river system

A
Indus at glacier in Kailash
 Jhelum at verinag in Kashmir
Chenab  at Bara lacha pass at zaskar range
 Ravi at Kullu 
Beas @ Punjab 
Satluj at mana Sarovar
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20
Q

Discuss the important dams on the Indus river system

A

Bhakra Dam on Gobind Sagar on the Sutlej river

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21
Q

The Ganga river system involves which states

A
Rajasthan 
Haryana
 Madhya Pradesh
 Uttar Pradesh 
Bihar 
Jharkhand 
West Bengal
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22
Q

Discuss the important tributaries of Ganga

A

Left tributaries= Sharda ,Bhangra rapti , Gandak Kosi

Right tributaries- Son

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23
Q

Draw a map of the Ganga river system

A

See notes

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24
Q

State the important dams in the Ganga river system

A
Chambal river
 Kota barrage Dam- irrigation
Jawahar Sagar Dam= Power generation
Rana Pratap Sagar Dam= Power generation
Gandhi Sagar Dam= Power generation
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25
Q

Draw a diagram of the Brahmaputra river system

A

See notes

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26
Q

Draw a map of the peninsular drainage into the Bay of Bengal

A

See notes

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27
Q

Draw a diagram of the Arabian Sea drainage

A

See noltes

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28
Q

Why are there no deltas in the Arabian Sea drainage

A

The rivers flow through hard rocks hence do not collect siltThe tributaries are small and hence the silt is low in quantity

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29
Q

Why are the Arabian Sea drainage west flowing

A

This exceptional behavior is because these rivers didn’t form valleys and instead they flow through faults (linear rift, rift valley, trough) created due to the bending of the northern peninsula during the formation process of the Himalayas.
These faults run parallel to the Vindhyas and the Satpuras.

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30
Q

What are the characteristics of inland drainage

A

In inland drainage streams join lakes or inland seas.They are fed by rainy water.During rains they experience flash floods.During dry season they get dried up.

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31
Q

What are the challenges regarding inland water transport in India

A

Water Flow: Due to Industrial, Agriculture and habitation the water flows have been decreased over the years this also may have decreased due to impact of dams of on the rivers.

Inadequate water channel Depth: Large vessels cannot traverse without adequate waters in the rivers. This along with the seasonal dependency of rivers makes operation of many ports difficult

Excessive Siltation:-Deforestation and erosion activity of the river leads to problem of siltation making navigation difficult.

Poor Skills and low technology adaptation:-Lack of automation in processes and low multi operation skills affect efficient utilisation of portsIt is a slower mode as compared to Rail and Road by its very nature. So improper navigational aids further hurt its competitiveness with other modes.

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32
Q

What are the advantages of inland water transport in India

A

Water transport is not only environment-friendly but also cheaper than other modes of transport.

Currently, logistics cost in India is one of the highest among major countries –as per the reports it is 18% in India versus 8-10% in China and 10-12% in European Union.

The acquisition of land for national and State highways is difficult and the cost of construction of roads, flyovers and bridges is high.

So, water transport is good alternative.It will help in the generation of millions of job opportunities.It will boost the maritime trade of the states and augment their economies

.There is a huge potential for domestic cargo transportation as well as for cruise, tourism and passenger traffic.

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33
Q

What are the steps taken towards the inland water transport in India

A

Jal Marg Vikas Project (JMVP) and Sagarmala are measures taken by Government to support inland water transportation

The Indian Government should focus more and put some special efforts and funds on the development of commercially significant IWT.

It requires the maintenance of a specified water depth and width depending upon the size of vessels expected to use that waterway.

This necessitates the release of adequate discharges.There is a strong need to provide effective rail, road and coastal connections from the waterways for multi-modal logistics.

The terminals should be located close to industrial hubs or consumption centers and should provide connectivity to both rail and Road.

Preservation of existing canals, lakes etc. is an essential ingredient of environmental protection. Inland waterway should not pollute the water way itself.

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34
Q

Discuss the pollution in Ganga the causes and the effects

A

Causes= urbanisation industries agricultural run-off

Withdrawal of Water: ​According to a ​report of the ​Ministry of ​Water Resources ​on the study of ​minimum flows ​in the Ganga, ​impact on river ​water quality ​resulting from ​discharges of ​treated or ​untreated ​wastewater into ​the river will ​depend on the ​dilution ​offered by the ​quantum of ​flows in the ​river.
​However, River Ganga gets ​starved of ​water when they ​enter the plain ​area.
​​For instance, the Upper Ganga ​Canal and the ​Lower Ganga ​Canal have left ​the Ganga ​downstream ​almost dry.

Religious practises

Effects =
The results of mercury analysis in various specimens collected along the basin indicated that some fish muscles tended to accumulate high levels of mercury.
Of it, approximately 50–84% was organic mercury. The Ganges river dolphin is one of few species of fresh water dolphins in the world.
Listed as an endangered species, their population is believed to be less than 2000.
The Ganges softshell turtle

Some of the dams being constructed along the Ganges basin will submerge substantial areas of nearby forest.
For example, the Kotli-Bhel dam at Devprayag will submerge 1200 hectares of forest, wiping out the forest area
During the summer and monsoon, hospital wards teem with children who need treatment for waterborne diseases

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35
Q

What are the steps taken for Ganga purification

A

Public Policy:
In 2016, the government issued a notification to authorize the National Mission for Clean Ganga (NMCG) to exercise powers under the Environment (Protection) Act, 1986.

NMCG also issued directives regulating mining activities on river banks, prohibiting encroachment, and regulating activities like the immersion of idols.

Technology Intervention:
NMCG adopted cutting-edge technologies like satellite imagery, remote sensing, and geospatial solutions which facilitated real-time monitoring of pollutants in Ganga and its tributaries.

Scientific forecast models were deployed for designing new sewage treatment infrastructure.

Community Participation: To encourage community participation in cleaning the river, an awareness campaign is regularly carried out in cities, towns, and villages alongside Ganga through a newly-established community force called “Ganga Praharis”.
Through them, the government seeks to transform “jal chetna” into “jan chetna” and turn it into a “jal aandolan”.

36
Q

Distinguish between himalayan and peninsular rivers

A

Perennial
Non-perennial

Form
…Delta
Some rivers form delta while others form Estuary

Shape
…Meandering
Straight

Rocks
…Bed rocks are soft, sedimentary and easily erodible
Bed rocks are hard, resistant and not easily erodible

Fed by
…Snow and rain
RainDrainage

basin…
Large
Small

Irrigate
….Northern Plains
Deccan Plateau

Valley
….V-shaped valley is formed
U-shaped val

37
Q

State the importance of rivers in India

A

Fresh water source Navigation on Narmada and Tapi
Power production
Hydroelectric
Irrigation

38
Q

What is groundwater

A

What are present in the spaces of permeable rock below the surface is called groundwater

39
Q

Discuss the status of groundwater in India locations

A
Aluviall and sedimentary northern plains
Peninsular rivers
Babar at foothills of Himalayas
East and west coastal plain
Penninsular Plateau difficult to recharge
40
Q

Rank Indian rivers in the order of groundwater reserves

A

Ganga Godavari Brahmaputra Krishna Indus

41
Q

Rank the Indian rivers in terms of facility and development of groundwater reserves

A

Indus Kaveri Kutch Ganga Pennar

42
Q

What causes the South West and the North East monsoon

A

South-west monsoon is caused because of low pressure at the Tibetan plateau and it affects India Indonesia and Myanmar

North East monsoon is caused due to high pressure at the Tibetan and east Siberian plateau and it affects south-east China and Japan

43
Q

Discuss the mechanism of Indian monsoons according to the Edmund Halley theory

A

In the summer the sun is at Tropic of Cancer and hence there is high temperature at Central Asia This result in lower pressure
Higher pressure pressure at the Arabian Sea. Hence wind go from Arabian Sea to the Central Asia
Drop the moisture from the sea at the western coast of India
In winter the sun is at Capricorn and the winds reverse hence low-pressure at the Arabian Sea and the Bay of Bengal and the winds move from the Tibetan plateau towards the lower pressure regions and deposit their moisture and the eastern coast

44
Q

What is the significance of ITCZ in the formation of Indian monsoon

A

The ITCZ is the meeting Place of the South East trade winds and the North Eastern winds
In the summer the ITCZ is in the north and hence the winds me up north
In the winters the ITCZ moves towards the south and hence the easterly trade winds move towards the south and calls rains on the eastern margins

Diagram

45
Q

Discuss the formation of Indian monsoons according to the ITCZ

A

South East trade winds cross the equator and become south-west due to coriolis force they meet the north-east trade winds and create a monsoon front which is known as the ITCZ
there is rainfall along this front
in July the ITCZ move towards the north at 20 to 25° north that is the Ganga plain the south-west monsoon winds moisture from the Arabian Sea and the Bay of Bengal there is maximum rain

46
Q

What is the significance of Tibetan plateau in India and climate

A

Tibetan Heating creates a low pressure in summer which gets coupled with Massacarene High pressure area and thus helps in initiation of Monsoon.

The vast mountain range also acted as a tall barrier, preventing cold, dry air in the northern latitudes from entering the subcontinent and subduing the warm, moisture-laden winds from the oceans that drive the monsoon.

During southwest monsoon, a thermal anticyclone appears over Tibet, which the resultant formation of dynamic anti-cyclogenesis.

On the south side of the anticyclone, the tropical jet stream is from.
The plateau pushes the jet stream north in the middle of the October.

Themovement sub-tropical westerly jet stream to the north Himalayas marks the onset of monsoon season in India.

The tropical easterly jet stream is formed at an eastern longitude of India then moves towards westwards across India and the Arabian Sea to eastern Africa.
This upper-level easterly jet stream creates a flow of air on the south side of Tibetan Plateau that reaches down to low levels over northernmost India.

During summer, the insolation heating of air above Tibet Plateau weakens the western subtropical jet stream south of the Himalayas with the resultant reversal of pressure gradient and wind flow over northern India.

47
Q

Describe the jet stream theory of Indian monsoon

A

The western cyclonic disturbances which enter the Indian subcontinent from the west and the northwest during the winter months, originate over the Mediterranean Sea and are brought into India by the WESTERLY jet stream.

The SUB TROPICAL Jet stream plays a significant role in both hindering the monsoon winds as well as in quick onset of Indian monsoons.

The burst of monsoons depends upon the upper air circulation which is dominated by Sub Tropical Jet Streams (STJ).

During summer, there is a presence of EASTERLY jet streams.

An easterly jet stream flows over the southern part of the Peninsula in June and has a maximum speed of 90 km per.

In August, it is confined to 15N latitude, and

in September up to 22 N latitudes.

The easterlies normally do not extend to the north of 30N latitude in the upper atmosphere.

The easterly jet stream steers the tropical depressions into India. These depressions play a significant role in the distribution of monsoon rainfall over the Indian subcontinent.

The tracks of these depressions are the areas of highest rainfall in India.

The frequency at which these depressions visit India, their direction and intensity, all go a long way in determining the rainfall pattern during the southwest monsoon period.

At times, Jet Streams bring about some moisture to the stratosphere, leading to the formation of cloudlike phenomena in the upper atmosphere which are made of ice crystals visible in a deep twilight

48
Q

Discuss the mechanism of the Indian winters

A

The sun is at the south of equator the daily range is high
dras Valley in Kashmir
Western disturbances at Northwest cause intense weather at Rajasthan Punjab and Haryana there is light rain in Indus Ganga plains and snowfall in Himalayas
The least number of tropical cyclones since the surface temperature is low and. ITCZ is in the south

49
Q

Latitude : expanse of india

A

N = 37° 6’N Indira Col
S= 8° 4’N
E= 68° 7’E
W=97° 25’E

50
Q

Standard meridian of India

A

82° 30’E

51
Q

India and Sri Lanka are seperated by?

A

Gulf of Mannar and Palk Strait

52
Q

Coastal Lenght : Total lenght and Land Frontier

A

7500km and 15,200km respectively

53
Q

India : areawise world ranking

A

7th largest ( approx 32,90,000sq km)2.4% of total land area of the world

54
Q

North South Extent, East West Extent of india

A

3214km, 2933km.

55
Q

Southern most point of mainland

A

Kanyakumari

56
Q

Southern most point of Indian Territory

A

Indira Point

57
Q

Eastern Most Point

A

Walong Town (AnP)

58
Q

Western Most Point

A

Rajheer Creek( Rann of Kutch )

59
Q

UP borders how many states?

A

8 (Uttarakhand, HP, Haryana, Rajasthan, MP, Chhattisgarh, Jharkhand, Bihar)maximum

60
Q

Assam borders how many states?

A

7 states ( 2nd Highest)

61
Q

Tropic of Cancer passes through

A

8 States : Gujarat, Rajasthan, MP, Chhattisgarh, Jharkhand, WB, Tripuro, Mizoram.

62
Q

Indian Standard Meridian passes through

A

5 States : UP, MP, Chhattisgarh, Orissa, AP.

63
Q

9 States form the coast of India. They are ?

A

Gujarat, Maharashtra, Goa, Karnataka, Kerala, Tamil Nadu. Andhra Pradesh, Orissa and West Bengal.

64
Q

`2 Union Territories which are on the coast.

A

Daman & Diu and Pondicherry

65
Q

Bhangar

A

Older alluvium of the plains. Studded with calcareous formations called ‘kankar’

66
Q

Khadar

A

New alluvium and forms the flood plains along the river banks.

67
Q

Volcanic Islands in india

A

Barren and Narcondam Islands. Barren is in the process of eruption these days after lying dormant for 200 years.

68
Q

Ten Degree Channel

A

separates Andamans from Nicobars (Little Andaman from Car Nicobar)

69
Q

Duncan Passage

A

lies between South Andaman and Little Andaman.

70
Q

Nine Degree Channel separates which island

A

separates Kavaratti from Minicoy Island.

71
Q

Andaman and Nicobar Group

A

204 islands of which the largest is Middle Andaman.Saddle Peak (737 m) in N.Andaman is the highest peak.

72
Q

Nicobars

A

group of 19 islands of which the largest is Great Nicobar. Most of them are volcanic in nature.

73
Q

Great Nicobar

A

southernmost island and is only 147 km away from Sumatra island of Indonesia.

74
Q

Arabian Sea Group

A

ll the islands in the Arabian Sea (Total 25) are coral islands and are surrounded by Fringing Reefs (North : Lakshadweep, South: Minicoy).

75
Q

ALLUVIAL SOIL

A

They are by far the largest and the most important soil group of India.
They are composed of sediments deposited by rivers and the waves.
Their chemical composition makes them one of the most fertile in the world.
Usually deficient in nitrogen and humus (thus fertilizers are needed).

Occupy the plains (from Punjab to Assam) and also occur in the valleys of Narmada and Tapti in M.P. & Gujarat, Mahanadi in the MP and Orissa, Godawari in A.R and Cauvery in T.N.Can be divided into Khadar (new) and Bhangar (older, more clayey and kankary) alluvium.

76
Q

BLACK SOIL

A

Also called Regur and is ideal for cotton crop.

These soils have been formed due to the solidification of lava spread over large areas during volcanic activity in the Deccan Plateau, thousands of years ago.

They are black due to compounds of iron and aluminium (also because of titaniferous magnetite).

Mainly found in Deccan Plateau – Maharashtra, Gujarat, M.P, Karnataka, Andhra Pradesh, Tamil Nadu.

Apart from cotton cultivation, these fertile soils are suitable for growing cereals, oilseeds, citrus fruits and vegetables, tobacco and sugarcane.

They have high moisture retention level.

Lack in phosphorus, nitrogen and organic matter.

77
Q

RED SOIL

A

They are mainly formed due to the decomposition of ancient crystalline rocks like granites and gneisses and from rock types rich in minerals such as iron and magnesium.

The term ‘red soil’ is due to the wide diffusion of iron oxides through the materials of the soil.

Covers almost the whole of Tamil Nadu, Karnataka, Andhra Pradesh, S.E. Maharashtra, Chhatisgarh, parts of Orissa, Jharkhand and Bundelkhand.

Generally deficient in nitrogen, humus and phosphorus, but rich in potash.

Suitable for rice, millets, tobacco and vegetables (also groundnuts and potatoes at higher elevations).

78
Q

LATERITE SOIL

A

Found in typical monsoon conditions – under conditions of high temperature and heavy rainfall with alternate wet and dry periods.

The alterations of wet and dry season leads to the leaching away of siliceous matter and lime of the rocks and a soil rich in oxides of iron and aluminium compounds is left behind.

Found in parts of Western Ghats, Eastern Ghats, Rajmahal hills, Maharashtra, Karnataka, Kerala, Orissa, West Bengal, Assam, Tamil Nadu, etc.

Poor in nitrogen and minerals.Best for tea, coffee, rubber, cinchona, coconut and suitable for rice and millet cultivation if manured.

79
Q

FOREST AND MOUNTAIN SOILS

A

Such soils are mainly found on the hill slopes covered by forests.

The formation of these soils is mainly governed by the characteristic deposition of organic matter derived from forest growth.

In the Himalayan region, such soils are mainly found in valley basins, depressions and less steeply inclined slopes.

Apart from the Himalayan region, the forest soils occur in higher hills in south and the peninsular region.

Very rich in humus but are deficient in Potash, phosphorous and lime and needs fertilizers.

Plantation of tea, coffee, spices and tropical fruits.

80
Q

ARID AND DESERT SOILS

A

A large part of the arid and semi-arid region in Rajasthan and adjoining areas of Punjab and Haryana lying between the Indus and the Aravallis receiving less than 50 cm of annual rainfall is affected by desert conditions
.This area is covered by a mantle of sand which inhibits soil growth.

The phosphate content of these soils is as high as in normal alluvial soils.

Nitrogen is originally low but its deficiency is made up to some extent by the availability of nitrogen in the form of nitrates.

Thus the presence of phosphates and nitrates make them fertile soils wherever moisture is available.
The changes in the cropping pattern in the Indira Gandhi Canal Command Area are a living example of the utility of the desert soils.

81
Q

SALINE AND ALKALINE SOILS

A

In the drier parts of Bihar, Up Haryana, Punjab, Rajasthan and Maharashtra, are the salt-impregnated or alkaline soils.

Known by different names: Reh, kallar, USAR, etc.

Some of the salts are transported in solution by the rivers and canals, which percolates in the sub-soils of the plains.

The accumulation of salts makes the soil infertile and renders it unfit for agriculture.

82
Q

PEATY AND MARSHY SOILS

A

Originate in the humid regions as a result of accumulation of large amounts of organic matter in the soil.

They contain considerable amounts of soluble salts and 10 – 40% of organic matter.

Peaty soils are found in Kottayam and Alappuzha districts of Kerala, where it is called Kari.

Marshy soils, high in vegetable matter, are found in northern Bihar, coastal parts of Orissa, Tamil Nadu and West Bengal and parts of UP

83
Q

What are the factors that influence the onset of south-west monsoon in India

A

The onset needs a trigger in the form of a weather system in the proximity of the coastline. These are ocean born phenomena which accentuate the monsoon surge around the normal time of onset. These include:

  1. The low-pressure area or depression in the Bay of Bengal during the last days of May or the beginning of June.
  2. There are such systems in the Arabian Sea as well around the same time which results in onset over the mainland.
  3. ‘Cyclonic Vortex’ is another factor which appears in the Southeast Arabian Sea, off Kerala and Lakshadweep region. They also shift along the west coast to push the monsoon current.
  4. The formation of ‘trough’ off the west coast due to temperature differential between land and sea. This situation could be for a mild start and weak progress.
  5. Lastly the cross-equatorial flow, wherein the trade
    winds from the Southern Hemisphere crossover to the
    Northern Hemisphere can bring a strong monsoon surge towards the Indian mainland.
84
Q

why are the Arabian Sea river courses short

A

The rivers flowing towards the Arabian Sea have short courses ( Because their origins lie closer to the sea, and the Western Ghats act as a water divide). Several of these small rivers are important for the production of hydroelectricity because of steep slopes and waterfalls.

85
Q

name the west flowing rivers of india

A

Narmada and the Tapi.Sabarmati, Mahi, and Luni

86
Q

why are Himalayan rivers perennial in nature

A

Most of the Himalayan Rivers are perennial in nature because the rivers get a continuous supply of water as the snow melts, especially in the summer. The peninsular rivers mostly depended on the rains only. So, they get dried up in the summer.

87
Q

why does the ITCZ shift

A

The shifting of ITCZ is the result of the
Earth’s rotation,
axis inclination and
the translation of Earth around the Sun.

Seasons are the result of this.

ITCZ moves toward the hemisphere with most heat, wich are either hemisphere summers.