Indian Geography Rivers Flashcards

1
Q

Drainage and Drainage system

A

The flow of water through well-defined channels is known as ‘drainage’ and the network of such channels is called a ‘drainage system’.

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2
Q

Catchment area

A

A river drains the water collected from a specific area, which is called its ‘catchment area’.

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3
Q

Drainage basin

A

An area drained by a river and its tributaries is called a drainage basin.

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4
Q

Watershed

A

The boundary line separating one drainage basin from the other is known as the watershed.

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5
Q

River basins

A

The catchments of large rivers are called river basins while those of small rivulets and rills are often referred to as watersheds. There is, however, a slight difference between a river basin and a watershed. Watersheds are small in area while the basins cover larger areas.

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6
Q

Importance of river basins and watersheds

A

River basins and watersheds are marked by unity. What happens in one part of the basin or watershed directly affects the other parts and the unit as a whole. That is why, they are accepted as the most appropriate micro, meso or macro planning regions.

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7
Q

Drainage patterns

A

(i) The drainage pattern resembling the branches of a tree is known as “dendritic” the examples of which are the rivers of northern plain.
(ii) When the rivers originate from a hill and flow in all directions, the drainage pattern is known as ‘radial’. The rivers originating from the Amarkantak range present a good example of it.
(iii) When the primary tributaries of rivers flow parallel to each other and secondary tributaries join them at right angles, the pattern is known as ‘trellis’.
(iv) When the rivers discharge their waters from all directions in a lake or depression, the pattern is know as ‘centripetal’.

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8
Q

Division of Indian drainage system on basis of discharge

A

On the basis of discharge of water (orientations to the sea), it may be grouped into: (i) the Arabian Sea drainage; and (ii) the Bay of Bengal drainage. They are separated from each other through the Delhi ridge, the Aravalis and the Sahyadris.
Nearly 77 per cent of the drainage area consisting of the Ganga, the Brahmaputra, the Mahanadi, the Krishna, etc. is oriented towards the Bay of Bengal while 23 per cent comprising the Indus, the Narmada, the Tapi, the Mahi and the Periyar systems discharge their waters in the Arabian Sea.

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9
Q

Division of Indian drainage system on basis of watershed size

A

(i) Major river basins with more than 20,000 sq. km of catchment area. It includes 14 drainage basins such as the Ganga, the Brahmaputra, the Krishna, the Tapi, the Narmada, the Mahi, the Pennar, the Sabarmati, the Barak, etc.. (ii) Medium river basins with catchment area between 2,000-20,000 sq. km incorporating 44 river basins such as the Kalindi, the Periyar, the Meghna, etc. (iii) Minor river basins with catchment area of less than 2,000 sq. km include fairly good number of rivers flowing in the area of low rainfall.

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10
Q

Major river basins of india

A

Ganga (in India)
Brahmaputra (in India) Barak and others Flowing to Meghna Sabarmati
Mahi
Narmada
Tapti
Brahmani and Baitarni Mahanadi
Godavari
Krishna
Penner
Kaveri
Suvarnarekha

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11
Q

Division of Indian drainage system on basis of source

A

Himalayan drainage and the Peninsular drainage.

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12
Q

Problems of including the Chambal, the Betwa, the Son, etc

A

much older in age and origin than other rivers that have their origin in the Himalayas

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13
Q

Characteristics of the Himalayan drainage

A

includes the Ganga, the Indus and the Brahmaputra river basins
Since these are fed both by melting of snow and precipitation, rivers of this system are perennial.

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14
Q

Evolution of the Himalayan drainage

A

During the Miocene period (5-24 million years ago), the mighty Indo-Brahma River flowed from Assam to Punjab and discharged into the Gulf of Sind. Over time, it fragmented into three main drainage systems, likely due to Pleistocene uplift in the western Himalayas, including the Potwar Plateau, which created a divide between the Indus and Ganga systems. Additionally, the Malda Gap’s down-thrusting redirected the Ganga and Brahmaputra rivers toward the Bay of Bengal.

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15
Q

The Indus System aka in other countries

A

Sindhu in Pak, In Tibet, it is known as ‘Singi Khamban; or Lion’s mouth.

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16
Q

The Indus System origin and discharge

A

glacier near Bokhar Chu in the Tibetan region in the Kailash Mountain range. Discharges into the Arabian Sea, east of Karachi.

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17
Q

The Indus System India regions flow

A

northwest direction between the Ladakh and Zaskar ranges, it passes through Ladakh and Baltistan. It cuts across the Ladakh range, forming a spectacular gorge near Gilgit in Jammu and Kashmir.

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18
Q

The Indus System Himalayan tributaries

A

Shyok, the Gilgit, the Zaskar, the Nubra, the Hunza, the Shigar, the Gasting and the Dras.

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19
Q

The Indus System tributaries from the Sulaiman ranges

A

The other important tributaries joining the right bank of the Indus are the Khurram, the Tochi, the Gomal, the Viboa and the Sangar. They all originate in the Sulaiman ranges.

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20
Q

Which indian states does the Indus flow through

A

The Indus flows in India only through the Leh district in Jammu and Kashmir.

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21
Q

Panjnad

A

name given to the five rivers of Punjab, namely the Satluj, the Beas, the Ravi, the Chenab and the Jhelum

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22
Q

Important Indus tributaries in India

A

Jhelum, Chenab, Ravi, Satluj, Beas, Drass, Gilgit, Shigar, Hunza, Nubra, Shyok, Zaskar

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23
Q

Jhelum flows through which Indian states, rises where, flow

A

J&K only. Rises from a spring at Verinag at the foot of the Pir Panjal in the valley of Kashmir. It flows through Srinagar and the Wular lake before entering Pakistan through a gorge.

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24
Q

Chenab aka, which states

A

largest tributary of the Indus. It is formed by two streams, the Chandra and the Bhaga, which join at Tandi near Keylong in Himachal Pradesh. Hence, it is also known as Chandrabhaga. Himachal Pradesh and Jammu and Kashmir.

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25
Beas origin, flow, states
originating from the Beas Kund near the Rohtang Pass. The river flows through the Kullu valley and forms gorges at Kati and Largi in the Dhauladhar range. meets Satluj near Harike. Himachal Pradesh and Punjab.
25
Ravi states, flow, joins Chenab where
Himachal Pradesh and Punjab and one UT, Jammu & Kashmir. It rises west of the Rohtang pass in the Kullu hills of Himachal Pradesh and flows through the Chamba valley of the state. (enters Pakistan and joining the Chenab near Sarai Sidhu) from Dhauladhar range.
26
Satluj origin, flow, states
Rakas lake near Mansarovar in Tibet where it is known as Langchen Khambab. Gorge at Rupar. It passes through the Shipki La. Feeds the canal system of the Bhakra Nangal project. Himachal Pradesh and Punjab
27
Indira Gandhi canal
The rivers on which the Indira Gandhi canal has been built are Beas and Sutlej. Irrigation facilities in the Thar Desert in the northwest of Rajasthan state.
28
Ganga origin
It rises in the Gangotri glacier in Uttarkashi district. Here, it is known as the Bhagirathi. At Devprayag, the Bhagirathi meets the Alaknanda; hereafter, it is known as the Ganga.
29
Important prayags and relationship to Alaknanda
At Devprayag, the Bhagirathi meets the Alaknanda; Vishnu Prayag (Joshi Math)- Dhauli and the Vishnu Ganga meet Karna Prayag-Pindar meets Alaknanda Rudra Prayag- Mandakini/Kali Ganga meets Alaknanda
30
Ganga states
Uttarakhand, Uttar Pradesh, Bihar, Jharkhand, and West Bengal.
31
The Ganga river system characteristics
is the largest in India having a number of perennial and non-perennial rivers originating in the Himalayas in the north and the Peninsula in the south, respectively.
32
Ganga destination
splitting into two distributaries, namely the Bhagirathi and the Hugli and into the Bay of Bengal.
33
Son origin flow states
originating in the Amarkantak plateau. After forming a series of waterfalls at the edge of the plateau, it reaches Arrah to join the Ganga. Chhattisgarh, Madhya Pradesh, Uttar Pradesh, Jharkhand, and Bihar
34
Ramganga origin flow states
Garhwal hills near Gairsain. Joins the Ganga near Kannauj. Uk and UP
35
Kosi origin flow states
north of Mount Everest in Tibet, where its main stream Arun rises. After crossing the Central Himalayas in Nepal, it is joined by the Son Kosi from the West and the Tamur Kosi from the east. Bihar.
36
Gandak origin flow states
Kaligandak and Trishulganga. It rises in the Nepal Himalayas between the Dhaulagiri and Mount Everest. It enters the Ganga plain in Champaran district of Bihar and joins the Ganga at Sonpur near Patna. Uttar Pradesh and Bihar:
37
Ghaghara origin flow states
Uttar Pradesh and Bihar. The Ghaghara originates in the glaciers of Mapchachungo. After collecting the waters of its tributaries – Tila, Seti and Beri, it comes out of the mountain, cutting a deep gorge at Shishapani. The river Sarda (Kali or Kali Ganga) joins it in the plain before it finally meets the Ganga at Chhapra.
38
Sarda origin flow states
The Sarda or Saryu river rises in the Milan glacier in the Nepal Himalayas where it is known as the Goriganga. Along the Indo-Nepal border, it is called Kali or Chauk, where it joins the Ghaghara. Uttarakhand, Uttar Pradesh
39
Damodar origin flow states
The Damodar occupies the eastern margins of the Chotanagpur Plateau where it flows through a rift valley and finally joins the Hugli. The Barakar is its main tributary. Once known as the ‘sorrow of Bengal’, the Damodar has been now tamed by the Damodar Valley corporation, a multipurpose project. Jharkhand and West Bengal.
40
Mahananda origin flow states
rising in the Darjeeling hills. It joins the Ganga as its last left bank tributary in West Bengal. West Bengal and Bihar.
41
Gomati origin flow states
Uttar Pradesh
42
Yamuna origin flow states joining
The Yamuna, the western most and the longest tributary of the Ganga, has its source in the Yamunotri glacier on the western slopes of Banderpunch range. It joins the Ganga at Prayag. It is joined by the Chambal, the Sind, the Betwa and the Ken on its right bank which originates from the Peninsular plateau while the Hindan, the Rind, the Sengar, the Varuna, HRSV etc. join it on its left bank. Much of its water feeds the western and eastern Yamuna and the Agra canals for irrigation purposes.
43
Chambal origin flow states
rises near Mhow in the Malwa plateau of Madhya Pradesh and flows northwards through a gorge up wards of Kota in Rajasthan, where the Gandhisagar dam has been constructed. joins the Yamuna. The Chambal is famous for its badland topography called the Chambal ravines. Madhya Pradesh, Rajasthan, and Uttar Pradesh
44
Brahmaputra origin flow states
Origin in Chemayungdung glacier of the Kailash range near the Mansarovar lake. From here, it traverses eastward longitudinally for a distance of nearly 1,200 km in a dry and flat region of southern Tibet, where it is known as the Tsangpo, which means ‘the purifier.’ It emerges as a turbulent and dynamic river after carving out a deep gorge in the Central Himalayas near Namcha Barwa (7,755 m). The river emerges from the foothills under the name of Siang or Dihang. Flowing southwest, it receives its main left bank tributaries, viz., Dibang or Sikang and Lohit; thereafter, it is known as the Brahmaputra.
45
Dibang states
Arunachal Pradesh and Assam
46
Lohit states
Arunachal Pradesh
47
Burhi Dihing states
Arunachal Pradesh and Assam
48
Dhansari States
Assam and Nagaland
49
Kalang States
Assam
50
Subansiri States
Arunachal Pradesh and Assam
51
Kameng States
Arunachal Pradesh and Assam
52
Manas States
Assam
53
Sankosh States
Assam and West Bengal
54
What is Teesta called in Bangladesh
Yamuna
55
Tista States
Sikkim and West Bengal
56
Ken States
MP UP
57
Betwa States
MP UP
58
THE PENINSULAR DRAINAGE SYSTEM characteristics
1. The Peninsular drainage system is older than the Himalayan one. This is evident from the broad, largely-graded shallow valleys, and the maturity of the rivers. 2. The Western Ghats running close to the western coast act as the water divide between the major Peninsular rivers, discharging their water in the Bay of Bengal and as small rivulets joining the Arabian Sea. 3. Most of the major Peninsular rivers except Narmada and Tapi flow from west to east due to rift valley. 4. The Chambal, the Sind, the Betwa, the Ken, the Son, originating in the northern part of the Peninsula belong to the Ganga river system. 5. The other major river systems of the Peninsular drainage are – the Mahanadi the Godavari, the Krishna and the Kaveri. 6. Peninsular rivers are characterized by fixed course, absence of meanders and non- perennial flow of water.
58
Flooding in Brahmaputra why
The Brahmaputra is well-known for floods, channel shifting and bank erosion. This is due to the fact that most of its tributaries are large, and bring large quantity of sediments owing to heavy rainfall in its catchment area.
59
The Evolution of Peninsular Drainage System
Three major geological events in the distant past have shaped the present drainage systems of Peninsular India: (i) Subsidence of the western flank of the Peninsula leading to its submergence below the sea during the early tertiary period. Generally, it has disturbed the symmetrical plan of the river on either side of the original watershed. (ii) Upheaval of the Himalayas when the northern flank of the Peninsular block was subjected to subsidence and the consequent trough faulting. The Narmada and The Tapi flow in trough faults and fill the original cracks with their detritus materials. Hence, there is a lack of alluvial and deltaic deposits in these rivers. (iii) Slight tilting of the Peninsular block from northwest to the southeastern direction gave orientation to the entire drainage system towards the Bay of Bengal during the same period.
60
Mahanadi river origin flow end states
The Mahanadi rises near Sihawa in Raipur district of Chhattisgarh and runs through Orissa to discharge its water into the Bay of Bengal. Chhattisgarh, Madhya Pradesh, and Odisha
61
Godavari
The Godavari is the largest Peninsular river system. It is also called the Dakshin Ganga. It rises in the Nasik district of Maharashtra and discharges its water into the Bay of Bengal. The Penganga, the Indravati, the Pranhita, and the Manjra are its principal tributaries. The Godavari is subjected to heavy floods in its lower reaches to the south of Polavaram, where it forms a picturesque gorge. Maharashtra, Chhattisgarh, Telangana, AP.
62
Krishna
second largest east- flowing Peninsular river which rises near Mahabaleshwar in Sahyadri. The Koyna, the Tungbhadra and the Bhima major tributaries. Maharashtra, Karnataka, Andhra Pradesh, and Telangana.
63
Kaveri
The Kaveri rises in Brahmagiri hills, Kogadu district in Karnataka. Kerala, Karnataka and Tamil Nadu. Its important tributaries are the Kabini, the Bhavani and the Amravati.
64
Narmada
originates on the western flank of the Amarkantak plateau, meets the Arabian sea south of Bharuch. The Sardar Sarovar Project has been constructed on this river. Madhya Pradesh, Maharashtra, and Gujarat
64
Tapi
The Tapi is the other important westward flowing river. It originates in the Betul district of Madhya Pradesh. Madhya Pradesh, Maharashtra, and Gujarat
64
Luni
Luni is the largest river system of Rajasthan, west of Aravali. It originates near Pushkar in two branches, i.e. the Saraswati and the Sabarmati, which join with each other at Govindgarh. From here, the river comes out of Aravali and is known as Luni. It flows to join the Rann of Kuchchh. Raj and Guj. ephemeral river.
65
Smaller Rivers Flowing Towards the West
The Shetruniji, The Bhadra ,The Dhadhar, Sabarmati and Mahi are famous rivers of Gujarat. The Vaitarna rises from the Trimbak hills in Nasik district. The Kalinadi, The Bedti river, The Sharavati are important rivers in Karnataka flowing towards the west. Goa has two important rivers which can be mentioned here. One is Mandovi and the other is Juari. Kerala has a narrow coastline. The longest river of Kerala, Bharathapuzha rises near Annamalai hills. It is also known as Ponnani. The Periyar, Pamba.
65
The rivers flowing towards the Arabian sea have short courses. Why do they have short courses?
because their origins lie closer to the sea, and the Western Ghats act as a water divide. It is interesting to note that the Peninsular rivers which fall into the Arabian Sea do not form deltas, but only estuaries
66
smaller rivers flowing east
The Subarnrekha (Jharkhand, West Bengal, and Odisha), the Baitarni (Odisha Jharkhand), the Brahmani, the Vamsadhara (AP Odisha), the Penner(Karnataka and Andhra Pradesh), the Palar (Karnataka, Andhra Pradesh, and Tamil Nadu) and the Vaigai (Kerala TN) are important rivers.
67
The discharge
is the volume of water flowing in a river measured over time. It is measured either in cusecs (cubic feet per second) or cumecs (cubic metres per second).
68
Regime
The pattern of flow of water in a river channel over a year is known as its regime. The north Indian rivers originating from the Himalayas are perennial as they are fed by glaciers through snow melt and also receive rainfall water during rainy season. The rivers of South India do not originate from glaciers and their flow pattern witnesses fluctuations. The flow increases considerably during monsoon rains.
69
comparision between Himalayan and Peninsular rivers
see notes
69
Deltas vs estuaries
Deltas are located at the mouth of a river where it meets a larger body of water, while estuaries are where rivers meet the ocean or a lake.
70
Periyar Diversion Scheme
Periyar river Kerala
71
Indira Gandhi Canal Project
The Indira Gandhi Canal is the longest canal of India. It starts from the Harike Barrage. At Harike, a few kilometers below the confluence of the Satluj and Beas rivers in the Indian state of Punjab and terminates in irrigation facilities in the Thar Desert in the north west of Rajasthan state.
72
Kurnool-Cuddapah Canal
This canal interconnects the rivers Penner and Tungabhadra in AP
73
Beas-Satluj Link Canal
Satluj Yamuna Link Canal or SYL as it is popularly known, is a proposed 214-kilometer (133 mi) long canal in India to connect the Sutlej and Yamuna rivers. It defines river water sharing between the states of Punjab and Haryana
74
Ganga-Kaveri Link Canal
as name suggests