The document summarizes India's drainage systems and major rivers. It discusses the Himalayan rivers like the Indus, Ganges and Brahmaputra which are fed by rain and snowmelt. These rivers cut through mountains and have long courses. The peninsular rivers are seasonal as they depend on rainfall and have shorter routes. Some flow west into the Arabian Sea while others flow east into the Bay of Bengal, forming deltas. The document also outlines various lakes found in India and the roles rivers play in India's economy and the issues of river pollution.
This will give you an exciting and entertaining yet Informative detail about the chapter Drainage of class drainage systems OF India, drainage patterns, the Himalayan drainage, the Peninsular Drainage Basins, Lakes and River Pollution are the topics covered.
Physiography of India- northern Mountains -Himalayas -Divisions of HimalayasLalit Thakare
Physiography of India- northern Mountains -Himalayas
THE NORTHERN MOUNTAINS ; Origin of Himalayas – Plate tectonics
Highest peaks of each range, Importance of Himalayas
Importance of Himalayas
Geological History of Himalayas
Physiographic divisions of Himalayas
Trans – Himalayan ranges
Greater Himalayas
Shiwalik / Outer Himalayas
Longitudinal divisions of Himalayas
Significance of Himalayas
This will give you an exciting and entertaining yet Informative detail about the chapter Drainage of class drainage systems OF India, drainage patterns, the Himalayan drainage, the Peninsular Drainage Basins, Lakes and River Pollution are the topics covered.
Physiography of India- northern Mountains -Himalayas -Divisions of HimalayasLalit Thakare
Physiography of India- northern Mountains -Himalayas
THE NORTHERN MOUNTAINS ; Origin of Himalayas – Plate tectonics
Highest peaks of each range, Importance of Himalayas
Importance of Himalayas
Geological History of Himalayas
Physiographic divisions of Himalayas
Trans – Himalayan ranges
Greater Himalayas
Shiwalik / Outer Himalayas
Longitudinal divisions of Himalayas
Significance of Himalayas
PPT on India's Drainage System (River System) Rohan Karmakar
The following presentation is on India's drainage or river system. It includes information about some of the major river systems in India. All comments are welcomed. Please LIKE this presentation.
The Indian sub-continent is characterised by a great and diversified group of physical features.
They are classified into the following physiographic units :
1. The Himalayas and other ranges.
2. The Indo-Gangetic plain.
3. The Thar Deserts
4. The Peninsular Plateau.
5. The Coastal belts and Islands.
PPT on India's Drainage System (River System) Rohan Karmakar
The following presentation is on India's drainage or river system. It includes information about some of the major river systems in India. All comments are welcomed. Please LIKE this presentation.
The Indian sub-continent is characterised by a great and diversified group of physical features.
They are classified into the following physiographic units :
1. The Himalayas and other ranges.
2. The Indo-Gangetic plain.
3. The Thar Deserts
4. The Peninsular Plateau.
5. The Coastal belts and Islands.
Its about major rivers of north India. It helps you all to know some information about north Indian river which flows in many north Indian states including Pakistan also. It contains major information of rivers. Hope you all like it.
The term river system refers to a ‘river along with its tributaries’.
Based on their source, the Indian River system is classified in to - Himalayan Rivers and Peninsular Rivers.
The Himalayan Rivers, as the name suggests originate from the Himalayas and flow through the Northern Plains.
The major Himalayan River systems are
The Indus River System,
The Ganga River System
The Yamuna River System
The Brahmaputra River System
Peninsular River System or Peninsular Drainage emerges mainly from the Western Ghats. Since the Western Ghats form a ‘water divide’, these rivers either flow eastwards into the Bay of Bengal or into the Arabian Sea towards the west. Peninsular Rivers are basically ‘rain fed’ rivers.
The major Peninsular River Systems are:
Mahanadi
Godavari
Krishna
Cauvery
Drain into Bay of Bengal as they flow eastwards on the plateau and make ‘deltas’ at their mouths; whereas Narmada
Tapti - the west flowing rivers fall into the Arabian Sea and make ‘estuaries’.
not originate in glaciers, but are rain fed rivers. These rivers reduce considerably or dry up during summers.
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Explore how micro-credentials are transforming Technical and Vocational Education and Training (TVET) with this comprehensive slide deck. Discover what micro-credentials are, their importance in TVET, the advantages they offer, and the insights from industry experts. Additionally, learn about the top software applications available for creating and managing micro-credentials. This presentation also includes valuable resources and a discussion on the future of these specialised certifications.
For more detailed information on delivering micro-credentials in TVET, visit this https://tvettrainer.com/delivering-micro-credentials-in-tvet/
How to Build a Module in Odoo 17 Using the Scaffold MethodCeline George
Odoo provides an option for creating a module by using a single line command. By using this command the user can make a whole structure of a module. It is very easy for a beginner to make a module. There is no need to make each file manually. This slide will show how to create a module using the scaffold method.
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Unit 8 - Information and Communication Technology (Paper I).pdfThiyagu K
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3. DRAINAGE
• Drainage: The term drainage describes the river system of an area.
• River system: A river, its tributaries and distributaries together called a river
system.
• Drainage basin: The area drained by a single river system is known as drainage
basin.
• Water divide: Any elevated area, such as a mountain or an upland, separates
two drainage basins
• The world’s largest drainage basin is of the Amazon river
5. DRAINAGE SYSTEMS IN INDIA
• The Indian rivers are divided into two major groups: the Himalayan rivers;
and the Peninsular rivers.
The Himalayan rivers:
• Most of the Himalayan rivers are perennial.
• These rivers receive water from rain as well as from melted snow from the
lofty mountains.
• They have cut through the mountains making gorges.
• The Himalayan rivers have long courses from their source to the sea.
• In the middle and the lower courses, these rivers form meanders, oxbow
lakes, and many other depositional features in their floodplains.
7. DRAINAGE SYSTEMS IN INDIA
• The Peninsular Rivers:
• The Peninsular rivers are seasonal, as their flow is dependent on rainfall.
• The volume of water in rivers fluctuates
• These rivers have shorter and shallower courses as compared to their
Himalayan counterparts.
• Some of them originate in the central highlands and flow towards the west.
E.g. Narmada and Tapi.
• Most of the rivers of peninsular India originate in the Western Ghats and
flow towards the Bay of Bengal.
9. The Himalayan Rivers
• The major Himalayan rivers are the Indus, the Ganga and the
Brahmaputra.
• These rivers are long, and are joined by many large and important
tributaries.
• A river along with its tributaries may be called a river system.
10. The Indus River System
• The river Indus rises in Tibet, near Lake Mansarowar.
• It enters India in the Ladakh district of Jammu and Kashmir.
• The important tributaries like the Zaskar, the Nubra, the Shyok and the
Hunza join in the Kashmir region.
• The Indus flows through Baltistan and Gilgit and emerges from the
mountains at Attock.
• The Satluj, the Beas, the Ravi, the Chenab and the Jhelum are the other
tributaries which join together to enter the Indus Mithankot in Pakistan
• The Indus flows southwards and eventually reaching the Arabian Sea,
east of Karachi.
11.
12. The Indus Plain
• The Indus plain has a very gentle slope.
• With a total length of 2900 km, the Indus is one of the longest
rivers of the world.
• A little over a third of the Indus basin is located in India in the states
of Jammu and Kashmir, Himachal Pradesh and Punjab and the rest is
in Pakistan.
• According to the regulations of the Indus Water Treaty (1960), India
can use only 20 per cent of the total water carried by the Indus river
system.
13. The Ganga River System
• The headwaters of the Ganga, called the ‘Bhagirathi’ is fed by the
Gangotri Glacier and joined by the Alaknanda at Devaprayag in
Uttarakhand.
• At Haridwar, the Ganga emerges from the mountains on to the
plains.
• The Ganga is joined by many tributaries from the Himalayas such as
the Yamuna(originates from the Yamunotri glacier), the Ghaghara,
the Gandak and the Kosi.
• The Yamuna flows parallel to the Ganga and meets the Ganga at
Allahabad.
14.
15.
16. The Ganga River System
• The Ghaghara, the Gandak and the Kosi rise in the Nepal Himalaya
and causing widespread damage to life and property, whereas, they
enrich the soil for agricultural use.
• The other tributaries like the Chambal, the Betwa and the Son rise
from semi-arid areas peninsular uplands.
• the Ganga flows eastwards till Farakka in West Bengal and then
bifurcates here; the Bhagirathi-Hooghly flows southwards.
• The mainstream, flows southwards into Bangladesh and is joined by
the Brahmaputra. Further downstream, it is known as the Meghna.
17. The Ganga River System
• The delta formed by these rivers is known as the Sundarban Delta.
• It is the world’s largest and fastest growing delta. It is also the home
of Royal Bengal tiger.
• The length of the Ganga is over 2500 km
• Ambala water divide located between the Indus and the Ganga
river systems
• Gentle slope creates many meanders(one metre for every 6 km.)
18. The Brahmaputra River System
• The Brahmaputra rises in Tibet east of Mansarowar Lake
• It is slightly longer than the Indus and most of its course lies outside
India.
• It flows eastwards and on reaching the Namcha Barwa (7757 m), it
takes a ‘U’ turn and enters India in Arunachal Pradesh through a
gorge.
• Here, it is called the Dihang and it is joined by the Dibang, the Lohit,
and many other tributaries
• Brahmaputra is known as the Tsang Po in Tibet and Jamuna in
Bangladesh.
20. The Brahmaputra River System
• In Tibet, the river carries a smaller volume of water and less silt as it
is a cold and a dry area.
• In India it passes through a region of high rainfall, carries a large
volume of water and considerable amount of silt.
• Braided channel in its entire length in Assam forms many riverine
islands.
• In rainy season, the river overflows its banks, causing widespread
devastation due to floods in Assam and Bangladesh
21. The Peninsular Rivers
• The main water divide in Peninsular India is formed by the Western
Ghats
• West flowing rivers are Narmada and Tapi and they make estuaries.
• Esturies are the tidal mouth of a large river or partially enclosed
coastal body with a free connection to the open sea.
• East flowing rivers are Mahanadi, Krishna, Kaveri and Godavari and
these rivers make deltas.
• Delta is a landform created by the deposition of sediments.
24. The Narmada Basin
• The Narmada rises in the Amarkantak hills in Madhya Pradesh.
• It flows towards the west in a rift valley formed due to faulting.
• It creates many picturesque locations.
• The ‘Marble rocks’, near Jabalpur (a deep gorge) and the ‘Dhuadhar
falls are some of the notable ones.
• The Narmada basin covers parts of Madhya Pradesh and Gujarat.
• The Narmada river conservation mission has been undertaken by
the government of Madhya Pradesh by a scheme named Namami
Devi Narmade
25. The Tapi Basin
• Rises in the Satpura ranges, in the Betul district of Madhya Pradesh.
• It also flows in a rift valley parallel to the Narmada but it is much
shorter in length.
• Its basin covers parts of Madhya Pradesh, Gujarat and Maharashtra
• The other main west flowing rivers are Sabarmati, Mahi,
Bharathpuzha and Periyar.
26. The Godavari Basin
• The Godavari is the largest Peninsular river.
• It rises from the slopes of the Western Ghats in the Nasik district of
Maharashtra.
• Its length is about 1500 km. It drains into the Bay of Bengal.
• The basin covers parts of Maharashtra, Madhya Pradesh, Odisha
and Andhra Pradesh.
• The Purna, the Wardha, the Pranhita, the Manjra, the Wainganga
and the Penganga.
• Because of its length and the area it covers, it is also known as the
Dakshin Ganga.
27. The Mahanadi Basin
• Rises in the highlands of Chhattisgarh.
• It flows through Odisha to reach the Bay of Bengal.
• The length of the river is about 860 km.
• Its drainage basin is shared by Maharashtra, Chhattisgarh,
Jharkhand, and Odisha.
28. The Krishna Basin
• Rising from a spring near Mahabaleshwar,
• Length - 1400 km and reaches the Bay of Bengal.
• The Tungabhadra, the Koyana, the Ghatprabha, the Musi and the
Bhima are some of its tributaries.
• Its drainage basin is shared by Maharasthra, Karnataka and Andhra
Pradesh.
29. The Kaveri Basin
• The Kaveri rises in the Brahmagri range of the Western Ghats
• It reaches the Bay of Bengal in south of Cuddalore in Tamil Nadu.
• The total length of the river is about 760 km.
• Its main tributaries are Amravati, Bhavani, Hemavati and Kabini.
• Its basin drains parts of Karnataka, Kerala and Tamil Nadu.
• The Damoder, the Brahmani, the Baitarni and the Subarnrekha are
some other notable east flowing rivers.
30. Water Falls
• The river Kaveri makes the second biggest waterfall in India, known as
Shivasamudram Falls
• Largest water fall is the Kunchical falls – 1493 ft (455m) – Varahi River
• Jog falls has a height of 833ft (254m)
• 71 per cent of the world’s surface is covered with water, but 97 per
cent of that is salt water. Of the 3 per cent as freshwater
32. LAKES
• Most lakes are permanent others are seasonal
• Some lakes are the result of the action of glaciers and ice sheets,
while others have been formed by wind, river action and human
activities.
• A meandering river across a floodplain forms cut-offs that later
develops into ox-bow lakes.
• Spits and bars form lagoons in the coastal areas, e.g. the Chilika
lake, the Pulicat lake and the Kolleru lake.
• Inland lakes - the Sambhar lake in Rajasthan, which is a salt water
lake.
33. Fresh Water Lakes
• Most of the freshwater lakes are in the Himalayan region.
• They are of glacial origin.
• The Wular lake in Jammu and Kashmir, in contrast, is the result of
tectonic activity. It is the largest freshwater lake in India.
• The Dal lake, Bhimtal, Nainital, Loktak and Barapani are some other
important freshwater lakes
34. Artificial Lakes
• The generation of hydel power has also led to the formation of
lakes, such as Guru Gobind Sagar (Bhakra Nangal Project)
• Uses of Lakes:
• A lake helps to regulate the flow of a river.
• Lakes can also be used for developing hydel power.
• They moderate the climate of the surroundings; maintain the
aquatic ecosystem, enhance natural beauty, help develop tourism
and provide recreation.
35. ROLE OF RIVERS IN THE ECONOMY
• Water is a basic natural resource, essential for various human
activities.
• Therefore, riverbanks have attracted settlers from ancient time
• Using rivers for irrigation, navigation, hydro-power generation
• National River Conservation Plan (NRCP)
• the Ganga Action Plan (GAP) in 1985.
• The Ganga Action Plan was expanded to cover other rivers under
the National River Conservation Plan (NRCP) in the year 1995.
36. RIVER POLLUTION
• The growing domestic, municipal, industrial and agricultural
demand for water from rivers naturally affects the quality of water.
• A heavy load of untreated sewage and industrial effluents are
emptied into the rivers.
• The increasing urbanisation and industrialization
• For example, given the adequate streamflow, the Ganga water is
able to dilute and assimilate pollution loads within 20 km of large
cities.
37. Map Work
• Chapter -3: Drainage
• Rivers: (Identification only)
• The Himalayan River Systems-
• The Indus, The Ganges, and The Satluj
• The Peninsular rivers-The Narmada, The Tapi, The Kaveri, The
Krishna, The Godavari, The Mahanadi
• Lakes: Wular, Pulicat, Sambhar, Chilika