India is a land of many rivers and mountains.
India’s geographical area of about 329 MHa is criss-crossed by a large number rivers. Some of the Indian rivers are figuring amongst the most notable rivers of the world. This module explain the river systems of India.
Groundwater province is an area or region in which geology and climate combine to produce groundwater conditions consistent enough to permit useful generalisations.
Groundwater province is an area or region in which geology and climate combine to produce groundwater conditions consistent enough to permit useful generalisations.
General overview about hydrosphere, water pollution and conservation methods. Also includes the water budget of India, water demand and supply and the gaps between the same.
Waterlogging Types & Causes of Waterlogging Effects & its control Salinity Ef...Denish Jangid
waterlogging with figures water resource engineering by DJ sir unit 4 WRE
Water logging, effects & its control salinity, effects & its control water logging types & causes of waterlogging
Effects of waterlogging on plant growth causes of salinity effects of salinity measures to control salinity preventive measures curative measures
How to Prevention of water logging.
Water Logging: Causes, preventive and curative measures, drainage of
irrigated lands, saline and alkaline lands, types of channels lining and design
of lined channel.
An aquifer is an underground layer of water-bearing rock. Water-bearing rocks are permeable, meaning that they have openings that liquids and gases can pass through. Sedimentary rock such as sandstone, as well as sand and gravel, are examples of water-bearing rock.
India is one of such country in the world which is bestowed with good number of rivers and tributaries, which are helpful not only in the field of agricultural but also in inland transport system of the country.Rivers also form the basis for domestic and industrial water supply, generation of hydro-electricity, inland fishing, are responsible for deposition of fertile soil in the plains as well as formation of deltas. This module explains the river systems of India.
General overview about hydrosphere, water pollution and conservation methods. Also includes the water budget of India, water demand and supply and the gaps between the same.
Waterlogging Types & Causes of Waterlogging Effects & its control Salinity Ef...Denish Jangid
waterlogging with figures water resource engineering by DJ sir unit 4 WRE
Water logging, effects & its control salinity, effects & its control water logging types & causes of waterlogging
Effects of waterlogging on plant growth causes of salinity effects of salinity measures to control salinity preventive measures curative measures
How to Prevention of water logging.
Water Logging: Causes, preventive and curative measures, drainage of
irrigated lands, saline and alkaline lands, types of channels lining and design
of lined channel.
An aquifer is an underground layer of water-bearing rock. Water-bearing rocks are permeable, meaning that they have openings that liquids and gases can pass through. Sedimentary rock such as sandstone, as well as sand and gravel, are examples of water-bearing rock.
India is one of such country in the world which is bestowed with good number of rivers and tributaries, which are helpful not only in the field of agricultural but also in inland transport system of the country.Rivers also form the basis for domestic and industrial water supply, generation of hydro-electricity, inland fishing, are responsible for deposition of fertile soil in the plains as well as formation of deltas. This module explains the river systems of India.
he Ganges or Ganga (Hindustani: [ˈɡəŋɡaː]), is a trans-boundary river of South Asia which flows through India and Bangladesh. The 2,704 km (1,680 mi) river originates from the Gangotri Glacier of western Himalayas in the Indian state of Uttarakhand, and flows south and east through the Gangetic Plain of India and Bangladesh, eventually emptying into the Bay of Bengal.
The water resources of Karnataka primarily constitutes surface and groundwater. Rainfall is the basic source of water in the state. Karnataka is blessed with seven river basins. There are 36,753 tanks in the state and they have a capacity of about 684518 hectares. The rivers, along with their tributaries, account for much of Karnataka’s surface water resources. Surface water is available in Karnataka in the form of rivers, lakes, waterfalls, reservoirs, etc. Being the seventh largest state in India (area-wise), Karnataka possesses about six percent of the country’s total surface water resources of about 17 lakh million cubic metres (Mcum).
E-content is a Comprehensive package of teaching material put into hypermedia format. Hypermedia is multimedia with internet deplorability. E-content can not be created by a teaching faculty alone . It needs the role of teacher, Video editor, production assistants, web developers (HTML 5 or Adobe captivate, etc). Analyze the learner needs and goals of the instructional material development, development of a delivery system and content, pilot study of the material developed, implementation, evaluating, refining the materials etc. In designing and development of E-content we have to adopt one of the instructional design models based on our requirements.
Pedagogy is the most commonly understood approach to teaching. It refers to the theory and practice of learning. Pedagogy is often described as the act of teaching. Pedagogy has little variations between traditional teaching and online teaching. Online teaching pedagogy is a method of effective teaching practice specifically developed for teaching via the internet. It has a set of prescribed methods, strategies, and practices for teaching academic subjects in an online (or blended) environment, where students are in a physical location separate from the faculty member.
Technology has changed the possibilities within teaching and learning. Classes, which prior to the digital era were restricted to lectures, talks, and physical objects, no longer have to be designed in that manner. Training in a synchronous virtual classroom can only be successful with the active participation and engagement of the learners. Explore the Virtual Classroom’s features and see how they can support and enhance your tutoring style.
• The monitoring and evaluation of the institutional processes require a carefully structured system of internal and external review. The NAAC expects the Institutions to undertake continuous Academic and Administrative Audits (AAA). This presentation is intended to serve as advisory to all accredited HEIs who volunteer to undertake AAA. The pros and cons of this process are also highlighted. Academic and Administrative Audit is the process of evaluating the efficiency and effectiveness of the administrative procedure. It includes assessment of policies, strategies & functions of the various administrative departments, control of the overall administrative system, etc. This checklist gives an overview what the audit committee members may look into while visiting an institution for this purpose. It invariably follows the Quality Indicators Framework prescribed by Accreditation Council in India.
• The monitoring and evaluation of the institutional processes require a carefully structured system of internal and external review. The NAAC expects the Institutions to undertake continuous Academic and Administrative Audits (AAA). This presentation is intended to serve as advisory to all accredited HEIs who volunteer to undertake AAA.
Chemical analysis data of water samples can not be used directly for understanding. They are to be used for various calculations in order to determine the quality parameters that have a lot of significances. A. Balasubramanian and D. Nagaraju, of the Department of Studies in Earth Science, Centre for Advanced Studies, University of Mysore, Mysore-570006, Karnataka, India have recently brought out a software and its application manual as a good book for reference and execution. The Name of the software is WATCHIT meaning Water Chemistry Interpretation Techniques. This software computes more than 100 parameters pertaining to water quality interpretations. The software follows its own method of approach to determine the required results. Systems International Units are used. Limited input parameters are required. This is suitable for all scientific research, government water quality data interpretations and for understanding the quality of water before using it.
Water conservation refers to reducing the usage of water and recycling of waste water for different purposes like domestic usage, industries, agriculture etc. This technical article highlights most of the popular methods of water conservation. A special note on rainwater harvesting is also provided.
This module gives an overview of general applications of current hydrogeological aspects. It is for the basic understanding of students and research scholars.
Climate Extreme (extreme weather or climate event) refers to the occurrence of a value of a weather or climate variable above (or below) a threshold value near the upper (or lower) ends of the range of observed values of the variable. Extreme weather and climate events, interacting with exposed and vulnerable human and natural systems, can lead to disasters.
WATER RESOURCES PLANNING AND MANAGEMENT POSSIBILITIES IN CHAMARAJANAGAR TALUK...Prof. A.Balasubramanian
Any unplanned development and utilization of water resources with result in water scarcity. In many parts of the developing world. Such a situation exists. In order to do proper planning and
management of water resources, it is necessary to conduct detailed analyses of the factors, which influence the water availability and its uses. In the present study, a comprehensive analysis have been undertaken for proper utilization of water resources in Chamarajanagar Taluk, which has been identified as one of the drought hit districts of Karnataka, in India. The factors analysed in this work are, surface and groundwater availability, land use, cropping pattern, recharge potential of soils and the rainfall pattern in typical areas of Taluk. It is observed that the problem of water scarcity is mainly due to the lack of irrigation planning and management. Hence, a
modified cropping pattern is suggested by taking into consideration of all available water resources and other conditions.
In broad terms, cultural geography examines the cultural values, practices, discursive and material expressions and artefacts of people, the cultural diversity and plurality of society.
It also emphasizes on how cultures are distributed over space, how places and identities are produced, how people make sense of places and build senses of place, and how people produce and communicate knowledge and meaning.
Minerals are formed by changes in chemical energy in systems which contain one fluid or vapor phase. In nature, minerals are formed by crystallisation or precipitation from concentrated solutions. These solutions are called as ore-bearing fluids. Ore-bearing fluids are characterised by high concentration of certain metallic or other elements.
Fluids are the most effective agents for the transport of material in the mantle and the Earth's crust.
Soils are complex mixers forming the skin of the earth's surface. Soil is a dynamic layer in which many complex chemical, physical and biological activities are going on constantly. Soils become adjusted to conditions of climate, landform and vegetation, and will change internally when those controlling conditions change. Soils are products of weathering. Soils play a dominant role in earth's geomorphic processes in a cyclic manner. The characteristics of soils are very essential for several reasons. This module highlights these characteristics.
GIS TECHNIQUES IN WATER RESOURCES PLANNING AND MANAGEMENT IN CHAMARAJANAGAR ...Prof. A.Balasubramanian
The over-exploitation and contamination of groundwater continue to threaten the long-term sustainability of our precious water resources, in spite of the best efforts made by various agencies.
This has many serious implications to the economic development of a country like India. Lack of
judicious planning and integration of environmental consideration to ground water development
projects are primarily responsible for such a state of affair in the ground water sector. Geographical Information Systems could be of immense help in planning sustainable ground water management strategies, especially in hard rock areas with limited ground water potential. Data collected from
Satellite Imagery and through field investigations have been integrated, on a GIS platform, for demarcation and prioritization of areas suitable for ground water development and ground water augmentation. An attempt has also been made to assess the vulnerability of the area to ground water
contamination. This paper demonstrates the utility of GIS in planning judicious management of ground water resources in a typical hard rock area of Chamarajanagar Taluk, Karnataka, state India.
Nanobiomaterials are very effective components for several biomedical and pharmaceutical studies. Among the metallic, organic, ceramic and polymeric nanomaterials, metallic nanomaterials have shown certain prominent biomedical applications. Enormous works have been done to synthesize, analyse and administer the metallic nanoparticles for various kinds of medical and therapeutic applications, during the last forty years. In these analyses, the prominent biomedical applications of ten metallic nanobiomaterials have been reviewed from various sources and works. It has been found that almost nine of them are used in a very wide spectrum of medical and theranostic applications.
A variety of Nano-biomaterials are synthesised, characterised and tested to find out their potentialities by global scientific communities, during the last three decades. Among those, nanostructured ceramics, cements and coatings are being considered for major use in orthopaedic, dental and other medical applications. The development of novel biocompatible ceramic materials with improved biomedical functions is at the forefront of health-related applications, all over the world. Understanding of the potential biomedical applications of ceramic nanomaterials will provide a major insight into the future developments. This study reviews and enlists the prominent potential biomedical applications of ceramic nanomaterials, like Calcium Phosphate (CaP), Tri-Calcium Phosphate (TCP), Hydroxy-Apatite(HAP), TCP+HAP, Si substituted HAP, Calcium Sulphate and Carbonate, Bioactive Glasses, Bioactive Glass Ceramics, Titania-Based Ceramics, Zirconia Ceramics, Alumina Ceramcis and Ceramic Polymer Composites.
The present forest and tree cover of the country is 78.37 million ha in 2007 which is 23.84% of the geographical areas and it includes 2.82% tree cover. This becomes 25.25%, if the areas above tree line i.e., 4000m are excluded from the total geographical area. The forest cover is classified into 3 canopy density classes.
1. Very Dense Forest (VDF) with canopy density more than 70%
2. Moderately Dense Forest (MDF) with Canopy density between 40-70% and
3. Open Forest (OF) with Canopy density between 10-40%
This pdf is about the Schizophrenia.
For more details visit on YouTube; @SELF-EXPLANATORY;
https://www.youtube.com/channel/UCAiarMZDNhe1A3Rnpr_WkzA/videos
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Nutraceutical market, scope and growth: Herbal drug technologyLokesh Patil
As consumer awareness of health and wellness rises, the nutraceutical market—which includes goods like functional meals, drinks, and dietary supplements that provide health advantages beyond basic nutrition—is growing significantly. As healthcare expenses rise, the population ages, and people want natural and preventative health solutions more and more, this industry is increasing quickly. Further driving market expansion are product formulation innovations and the use of cutting-edge technology for customized nutrition. With its worldwide reach, the nutraceutical industry is expected to keep growing and provide significant chances for research and investment in a number of categories, including vitamins, minerals, probiotics, and herbal supplements.
Richard's entangled aventures in wonderlandRichard Gill
Since the loophole-free Bell experiments of 2020 and the Nobel prizes in physics of 2022, critics of Bell's work have retreated to the fortress of super-determinism. Now, super-determinism is a derogatory word - it just means "determinism". Palmer, Hance and Hossenfelder argue that quantum mechanics and determinism are not incompatible, using a sophisticated mathematical construction based on a subtle thinning of allowed states and measurements in quantum mechanics, such that what is left appears to make Bell's argument fail, without altering the empirical predictions of quantum mechanics. I think however that it is a smoke screen, and the slogan "lost in math" comes to my mind. I will discuss some other recent disproofs of Bell's theorem using the language of causality based on causal graphs. Causal thinking is also central to law and justice. I will mention surprising connections to my work on serial killer nurse cases, in particular the Dutch case of Lucia de Berk and the current UK case of Lucy Letby.
Seminar of U.V. Spectroscopy by SAMIR PANDASAMIR PANDA
Spectroscopy is a branch of science dealing the study of interaction of electromagnetic radiation with matter.
Ultraviolet-visible spectroscopy refers to absorption spectroscopy or reflect spectroscopy in the UV-VIS spectral region.
Ultraviolet-visible spectroscopy is an analytical method that can measure the amount of light received by the analyte.
What is greenhouse gasses and how many gasses are there to affect the Earth.moosaasad1975
What are greenhouse gasses how they affect the earth and its environment what is the future of the environment and earth how the weather and the climate effects.
Observation of Io’s Resurfacing via Plume Deposition Using Ground-based Adapt...Sérgio Sacani
Since volcanic activity was first discovered on Io from Voyager images in 1979, changes
on Io’s surface have been monitored from both spacecraft and ground-based telescopes.
Here, we present the highest spatial resolution images of Io ever obtained from a groundbased telescope. These images, acquired by the SHARK-VIS instrument on the Large
Binocular Telescope, show evidence of a major resurfacing event on Io’s trailing hemisphere. When compared to the most recent spacecraft images, the SHARK-VIS images
show that a plume deposit from a powerful eruption at Pillan Patera has covered part
of the long-lived Pele plume deposit. Although this type of resurfacing event may be common on Io, few have been detected due to the rarity of spacecraft visits and the previously low spatial resolution available from Earth-based telescopes. The SHARK-VIS instrument ushers in a new era of high resolution imaging of Io’s surface using adaptive
optics at visible wavelengths.
Observation of Io’s Resurfacing via Plume Deposition Using Ground-based Adapt...
River basins in India
1. 1
RIVER BASINS OF INDIA
By
Prof. A. Balasubramanian
Centre for Advanced Studies in Earth Science,
University of Mysore, Mysore
2. 2
Introduction:
India is a land of many rivers and mountains.
India’s geographical area of about 329 MHa is criss-
crossed by a large number rivers. Some of the Indian
rivers are figuring amongst the most notable rivers of
the world.
The rivers and mountains have a greater significance
in the history of Indian culture, economy,
development, religious and spiritual life.
3. 3
It may not be an exaggeration to say that the rivers are
the heart and soul of Indian population.
The river systems provide water
For irrigation,
Drinking and domestic consumption,
cheap transportation,
generating electricity, and
for the livelihoods for a large number of people all
over the country.
Nearly most of the major cities of India are located by
the banks of the rivers.
4. 4
The perennial rivers are considered as life supporting
resources by all the farmers in India.
Rivers are classified into major, medium and minor
types.
Most of these rivers pour their waters into the Bay of
Bengal, except some of the rivers whose courses take
them through the western part of the country
emptying the waters into the Arabian Sea.
Understanding the river basins of India is needed to
all geographers, administrators, planners and others.
5. 5
Brief introduction about the following rivers are
highlighted in this lesson:
1. INDUS RIVER BASIN
2. THE GANGA RIVER BASIN
3. BRAHMAPUTRA AND BARAK RIVER
BASIN
4. NARMADA RIVER BASIN
5. TAPTI RIVER BASIN
6. BRAHMANI-BAITARNI RIVER BASIN
7. MAHANADI RIVER BASIN
8. GODAVARI RIVER BASIN
9. KRISHNA RIVER BASIN
6. 6
10. PENNAR RIVER BASIN
11. CAUVERY RIVER BASIN
12. MAHI RIVER BASIN
13. SABARMATHI RIVER BASIN
Their geographic setting, origin, distribution and
water resources potential are highlighted in this
lesson:
7. 7
1. INDUS RIVER BASIN
The Indus River Basin extends over an area of
11,65,500 Sq. Km. It is spread over parts of Tibet
(China), India, Pakistan and Afghanistan.
The drainage area lying in India is 321,289 Sq. Km
which is nearly 9.8% of the total geographical area of
the country.
The basin lies in the states of
Jammu & Kashmir (193,762 Sq. Km),
Himachal Pradesh (51,356 Sq. Km ),
8. 8
Punjab (50,304 Sq. Km ),
Rajasthan (15,814 Sq. Km ),
Haryana (9,939 Sq. Km ) and
Union Territory of Chandigarh (114 Sq. Km ).
The Indus River rises from Mansarovar in Tibet at an
elevation of abut 5182 m.
It flows for about 2880 km upto its outfall into the
Arabian Sea. The length of the river in India is 1114
km. The principal tributaries of the river are
the Sutlej, the Beas, the Ravi, the Chenab and the
Jhelum.
9. 9
The upper part of basin is lying in the mountains of
Jammu and Kashmir and Himachal Pradesh.
In Punjab, Haryana and Rajasthan, the basin consists
of vast plains which are the fertile granary of India.
An average annual surface water potential of 73.3 Cu.
Km has been assessed in this basin. Out of this, 46.0
Cu. Km is the utilizable water.
Culturable area of the basin is about 9.6 M.ha, which
is 4.9% of the total cultivable area of the country.
The hydropower potential of the basin has been
assessed as 19,998 MW at 60% load factor.
10. 10
2. THE GANGA RIVER BASIN
Ganga River basin is a part of the composite Ganga-
Brahmaputra-Meghna basin.
The basin lies in China, Nepal, India and Bangladesh
and drains over an area of 10.86 million Sq. Km
(10,86,000 Sq. Km).
It is bounded on the north by the Himalayas, on the
west by the Aravallis as well as the ridge separating it
from Indus basin, on the south by the Vindhyas and
Chhotanagpur Plateau and on the east by the
Brahmaputra ridge.
11. 11
Its catchment lies in the states of
Uttar Pradesh (294,364 Sq. Km ),
Madhya Pradesh (198,962 Sq. Km ),
Bihar (143,961 Sq. Km ),
Rajasthan (112,490 Sq. Km ),
West Bengal (71,485 Sq. Km ),
Haryana (34,341 Sq. Km ),
Himachal Pradesh (4,317 Sq. Km ) and
Delhi (1,484 Sq. Km ).
The basin has a population of 356.8 million.
12. 12
The Ganga originates as Bhagirathi from the Gangotri
Glaciers in the Himalayas at an elevation of about
7010 m above mean sea level, in the Uttarkashi
district of Uttar Pradesh.
The Bhagirathi is joined by the Alaknanda at
Deoprayag and the combined stream under the name
Ganga flowing through the mountain region,
debouches into the plain at Rishikesh.
13. 13
It is joined by a large number of tributaries on both
the banks in the course of its total run of 2525 km
before its outfall into the Bay of Bengal.
The important tributaries are
the Yamuna, the Ramganga,
the Gomti, the Ghagra, the Stone,
the Gandak, the Burhi Gandak,
the Kosi and the Mahananda.
At Farakka in West Bengal, the river divides into two
arms namely, the Padma which flows to Bangladesh
and the Bhagirathi which flows through West Bengal.
14. 14
The basin comprises mountainous regions of the
Himalayan ranges with dense forests, sparsely
forested Sivalik hills and the fertile Gangetic plains.
The important cities and town situated on the banks of
the river Ganga are
Haridwar, Kanpur, Allahabad, Varanasi, Patna,
Bhagalpur, etc.
Deoprayag, Rishikesh, Haridwar, Garhmukteshwar,
Allahabad and Varanasi are some of the important
places located on the banks of Ganga River.
15. 15
The average annual surface water potential of the
basin has been assessed as 525.0 Cu. Km . Out of
this, 250.0 Cu. Km is utilizable water.
The hydropower potential of the basin has been
assessed as 10,715 MW at 60% load factor.
The Upper Ganga Canal and the Eastern and Western
Yamuna Canals built during the nineteenth century,
are among the oldest major projects in this basin.
16. 16
Some of the other important projects constructed
since independence are
Gandhi Sagar Dam, Rana Pratap Sagar Dam,
Narora Barrage, Rajghat Dam,
Rihand Dam, Gandak Barrage,
Tenughat Dam, Maithon Dam, Kangsabati Dam, etc.
Large scale urbanization and industrial development
brought a lot of pollution into the river waters.
17. 17
The Ganga Action Plan has been taken to reduce
the pollution of the river especially at Haridwar,
Kanpur, Allahabad and Varanasi.
Uttar Pradesh, Bihar and West Bengal are the states
affected by frequent floods.
3. THE BRAHMAPUTRA – BARAK RIVER
BASIN
Brahmaputra River basin, is a part of the composite
Ganga – Brahmaputra – Meghna basin.
18. 18
It extends over an area of 5,80,000 Sq. Km and lies in
Tibet (China), Bhutan, India and Bangladesh.
The basin is enclosed by the Himalayas on the north,
the Patkari range of hills on the east running along the
Indo-Burma border, the Assam hills on the south and
the ridge separating it from the Ganga basin on the
west.
In India, it drains over an area of 1,94,413 Sq. Km in
the states of Arunachal Pradesh, Assam, Nagaland,
Meghalaya and West Bengal and Sikkim.
19. 19
The Brahmaputra river known as the Tsangpo in
Tibet, the Siang or Dihang in Arunachal Pradesh and
the Jamuna in Banglaesh.
It is one of the largest rivers of the world.
The 2880 km long Brahmaputra traverses its first
1,625 km in Tibet, the next 918 km in India and the
remaining 337 km in Bangladesh.
The average width of the Brahmaputra valley is about
86 km, of which the river itself occupies 15-19 km.
20. 20
The river forms almost a trough receiving the flows of
its tributaries both from north and south.
Some of the important tributaries of the river in India
are
the Dibang,
the Luhit,
the Subansiri,
the Manas,
the Sankosh,
the Tista,
the Dhansiri and the Champamati.
21. 21
The annual rainfall in the Indian portion of the basin
varies from 100 cm to 400 cm, most of which occurs
during the monsoon months of June to September.
Due to several geomorphic factors, the river carries
heavy sediment load of the order of 735 million tones
per annum.
The Barak river rises in the Manipur hills and enters
the plains near Lakhipur.
22. 22
The Barak basin lies in India, Myanmar and
Bangladesh and drains over an area of 41,723 Sq. Km
in India.
The basin is bounded on the north by the Barail range,
on the east by the Naga and Lushai hills and on the
south and west by Bangladesh.
In India, the basin lies in the states of Mehalaya,
Manipur, Mizoram, Assam, Tripura and Nagaland
with a total population of 6.2 million.
23. 23
Before entering Bangladesh, the river bifurcates into
two streams called Surma and Kushiara.
Further lower down, the river is called Mehna and
receives the combined flow of the Ganga and the
Brahmaputra.
The principal tributaries of the Barak in India are
the Jiri, the Dhaleshwari, the Singla, the Longai,
the Sonai and the Katakhal.
24. 24
Most portion of the Brahmaputra – Barak basin
consists of hills, forests, cultivated lands and tea
gardens.
The basin has a wide variety of flora and fauna.
The famous wild life sanctuaries of Manas and
Kaziranga, the Buxa tiger reserve, the Phibsoo reserve
forest (Bhutan) etc. provide glimpses of rare species
of plant and animal life.
An average annual surface water potential of 585.6
Cu. Km has been assessed in this basin. Out of this,
24.0 Cu. Km is utilialble water.
25. 25
Cultivable area of the basin is about 13.04 M.ha.
which is 7.1% of the total cultivable area of the
country.
The hydropower potential of the basin has been
assessed as 33,054 MW at 60% load factor.
Some of important schemes implemented in this river
are the Tista, Champamati and Dhansiri barrages.
Floods are an annual feature in the Brahmaputra –
Barak basin. The maximum flood prone area is of the
order of 4.33 Million ha.
26. 26
Brahmaputra Board has been setup to look into the
problems of floods, erosion and drainage congestion
in the basin.
4. NARMADA RIVER BASIN
Narmada basin extends over an area of 98,796 sq.
Km which is nearly 3.0% of total geographical area of
the country. The basin lies in the states of Madhya
Pradesh (85,859 km2 ), Gujarat (11,300km2 ) and
Maharashtra (1,538km2 ).
27. 27
Narmada river rises near Anarkantak in Madhya
Pradesh at an elevation of about 900 m and flows for
about 1312 km before outfalling into the Arabian Sea
through the Gulf of Cambay.
Its principal tributaries are
the Burhner,
the Tawa,
the Hiran,
the Barna,
the Kolar and the Orsang.
28. 28
An average annual surface water potential of 45.6
Cu. Km has been assessed in this basin. Out of this ,
34.5 Cu. Km is utilizable water.
Cultivable area in the basin is about 5.9 M.ha, which
is 3.0% of the total cultivable area of the country.
Present use of surface water in the basin is 8.0 Cu.
Km.
Live storage capacity in the basin has increased
significantly since independence.
29. 29
The hydropower potential of the basin has been
assessed as 1321 MW at 60% load factor.
5. TAPI RIVER BASIN
Tapi River Basin extends over an area of 65,145 Cu.
Km which is nearly 2.0% of total geographical area of
the country.
The basin lies in the states of Maharashtra (51,504Sq.
Km ), Madhya Pradesh (9,804Sq. Km ) and
Gujarat (3,837 Sq. Km ).
30. 30
Tapi river rises near Multai in the Betual district of
Madhya Pradesh at an elevation of about 752 m and
flows for about 724 km before outfalling into the
Arabian sea through the Gulf of Cambay.
Its principal tributaries are
the Pruna, the Girna, the Panjhra, the Vaghur,
the Bori and the Aner.
An average annual surface water potential of 18 Cu.
Km has been assessed in this basin. Out of this, 14.5
Cu. Km is utilizable water.
31. 31
Cultivable area in the basin is about 4.3 Million ha,
which is 2.2% of the total cultivable area of the
country.
The hydropower potential of the basin is 119.7MW at
60% load factor.
6. BRAHMANI-BAITARNI RIVER BASIN
Brahmani and Baitarni basin jointly extends over an
area of 51,822 Sq. Km which is nearly 1.7% of the
total geographical area of the country.
32. 32
The independent drainage areas of Brahmani and
Baitarni are 39,033 Sq. Km and 12,879Sq. Km
respectively.
The basin lies in the state of
Orissa (34,749Sq. Km ),
Bihar (15,757Sq. Km ) and
Madhya Pradesh (1,316Sq. Km ).
The Brahmani river rises near Nagri village in Ranchi
district of Bihar at an elevation of about 600 m and
has a total length of 799 km.
33. 33
The Baitarni river rises in the hill ranges of Keonjhar
district of Orissa at an elevation of about 900 m and
has a length of about 355 km.
Both river systems outfall into the Bay of Bengal
forming a common delta area.
The important tributaries of Brahmani are
the Karo,
the Sankh, and
the Tirka and those of Baitarni are
the Salandi and
the Matai.
34. 34
An average annual surface water potential of 28.5
Cu. Km has been assessed in this basin.
Out of this, 18.3 Cu. Km is utilizable water.
Cultivable area in the basin is about 3.2 M.ha, which
is 1.6% of the total cultivable area of the country.
The hydropower potential of the basin has been
assessed as 548 MW at 60% load factor.
35. 35
7. MAHANADI RIVER BASIN
Mahanadi Basin extends over an area of 141,589 Sq.
Km which is nearly 4.3% of total geographical area of
the country.
The basin lies in the states of
Chhattissgarh
Madhya Pradesh (75, 136 Sq. Km),
Orissa (65, 580 Sq. Km),
Bihar (635 Sq. Km) and
Maharashtra (238 Sq. Km).
36. 36
Mahanadi river rises from Raipur district of Madhya
Pradesh and flows for about 851 km before its outfall
into the Bay of Bengal.
Its main tributaries are
the Seonth,
the Jonk,
the Hasdeo,
the Mand,
the Ib,
the Ong and
the Telen.
37. 37
Physiographically the basin can be divided into four
regions, namely,
the Norther Plateau,
the Eastern Ghats,
the Coastal Plain and
the Erosional Plains of Central tableland.
An average annual surface water potential of 66.9
Cu. Km has been assessed in this basin. Out of this,
50.0 Cu. Km is utilizable water.
38. 38
Cultivable area in the basin is about 8.0 Million ha,
which is 4.0% of the total cultivable area of the
country.
The hydropower potential of the basin has been
assessed as 627 MW at 60% load factor.
8. GODAVARI RIVER BASIN
Godavari Basin extends over an area of 312,812 Sq.
Km, which is nearly 9.5% of the total geographical
area o f the country.
39. 39
The basin lies in the states of
Maharashtra (152,199 Sq. Km),
Andhra Pradesh (73,201 Sq. Km),
Madhya Pradesh (65,255 Sq. Km),
Orissa (17,752 Sq. Km) and
Karnataka (4,405 Sq. Km).
Godavari river rises near Nasik in Maharashtra at an
elevation of 1067 m and flows for a length of about
1465 km before outfalling into the Bay of Bengal.
40. 40
The principal tributaries of the river are
the Parvara,
the Purna,
the Manjra,
the Penganga,
the Wardha,
the Wainganga,
the Indravati and
the Kolab.
An average annual surface water potential of 110.5
Cu. Km has been assessed in this basin.
41. 41
Out of this, 76.3 Cu. Km is utilizable water.
Cultivable area in the basin is about 18.9 Million ha,
which is 9.7% of the total cultivable area of the
country.
The hydropower potential of the basin has been
assessed as 5091 MW at 60% load factor.
42. 42
9. KRISHNA RIVER BASIN
Krishna Basin extends over an area of 258,948 Sq.
Km which is nearly 8% of total geographical area of
the country.
The basin lies in the state of
Karntaka (113,271 Sq. Km),
Andhra Pradesh (76,252 Sq. Km) and
Maharashtra (69,425 Sq. Km).
43. 43
Krishna river rises in the Western Ghats at an
elevation of about 1337 m just north of
Mahabaleshwar, about 64 km from the Arabian Sea
and flows for about 1400 km and outfalls into the Bay
of Bengal.
The principal tributaries joining Krishna are
the Ghataprabha,
the Malaprabha,
the Bhima,
the Tungabhadra and
the Musi.
44. 44
An average annual surface water potential of 78.1
Cu. Km has been assessed in this basin. Out of this,
58.0 Cu. Km is utilizable water.
Cultivable area in the basin is about 20.3 Million ha,
which is about 10.4% of the total cultivable area of
the country.
The hydropower potential of the basin has been
assessed as 2997 MW at 60% load factor.
45. 45
10. PENNAR RIVER BASIN
Pennar Basin extends over an area of 55, 213 Sq. Km
which is nearly 1.7% of total geographical area of the
country.
The basin lies in the states of
Andhra Pradesh (48,276 Sq. Km) and
Karantaka (6,937 Sq. Km).
Pennar river rises from the Chenna Kesava hills of the
Nandi range of Karnataka and flows for about 597 km
before outfalling into Bay of Bengal.
46. 46
The principal tributaries of the river are
the Jayamangal,
the Kunderu,
the Saileru,
the Chitravati,
the Papagni and
the Cheyyeru.
An average annual surface water potential of 6.3 Cu.
Km has been assessed in this basin which is
completely utilizable.
47. 47
Cultivable area in the basin is about 3.5 Million ha,
which is 1.8% of the total cultivable area of the
country.
The hydropower potential of the basin has been
assessed as 1359 MW at 60% load factor.
11. CAUVERY RIVER BASIN
Cauvery Basin extends over an area of 87,900 Sq. Km
which is nearly 2.7% of total geographical area of the
country.
48. 48
The basin lies in the states of
Tamil Nadu (48, 730 Sq. Km),
Karnataka (36,240 Sq. Km) and
Kerala (2,930 Sq. Km).
Cauvery river rises at Talakaveri on the Brahmagiri
range in the Western Ghats in Karnataka at an
elevation of about 1341 m and flows for about 800
km before its outfall into the Bay of Bengal.
The important tributaries joining the Cauvery are
the Harangi, the Hemavati, the Kabini, the
Suvarnavathi and the Bhavani.
49. 49
Physiographically, the basin can be divided into three
parts-the Western Ghats, the Plateau of Mysore and
the Delta.
The delta area is the most fertile tract in the basin.
An average annual surface water potential of 21.4
Cu. Km has been assessed in this basin. Out of this,
19.0 Cu. Km is utilizable water.
50. 50
Cultivable area in the basin is about 5.8 Million ha,
which is about 3.0% of the total cultivable area of the
country.
The hydropower potential of the basin has been
assessed as 1359 MW at 60% load factor.
12. MAHI RIVER BASIN
Mahi Basin extends over an area of 34, 842 Sq. Km
which is nearly 1.1% of total geographical area of the
country.
51. 51
The basin lies in the states of Rajasthan (16,453 Sq.
Km), Gujarat (11,694 Sq. Km) and Madhya Pradesh
(6,695 Sq. Km).
Mahi river rises from the northern slopes of Vindhyas
in Madhya Pradesh at an elevation of about 500m and
flows for about 583 km before outfalling into the
Arabian Sea through the Gulf of Cambay.
The principal tributaries of the river are
the som, the Anas and the Panam.
52. 52
The upper part of the basin mostly lies in Rajasthan
and Madhya Pradesh and comprises mostly hills and
forests except the lower half in Madhya Pradesh
which is fairly plain.
The central part lying in Gujarat consists of developed
lands.
An average annual surface water potential of 11.0
Cu. Km has been assessed in this basin. Out of this
5.2 Cu. Km is utilizable water. Cultivable area in
the basin is about 2.2 Million ha, which is 1.1% of the
total cultivable area of t he country.
53. 53
The hydropower potential of the basin has been
assessed as 68.6 MW at 60% load factor.
13. SABARMATI RIVER BASIN
Sabarmati River Basin extends over an area of 21,674
Sq. Km which is nearly 0.7% of total geographical
area of the country. Sabarmati river rises from
Aravalli hills in Rajasthan at an elevation of about
762 m and flows for about 371 Km before outfalling
into the Arabian sea through the Gulf of Cambay.
54. 54
The principal tributaries of Sabarmati are
the Sei,
the Wakal,
the Harnav,
the Hathmati, and
the Wartak.
An average annual surface water potential of 3.8 Cu.
Km has been assessed in this basin. Out of this, 1.9
Cu. Km is utilizable water.
55. 55
Cultivable area in the basin is about 1.6 Million ha,
which is 0.8% of the total cultivable area of the
country.