About JnU Geography & Environment

Thursday, July 11, 2013

How soil is erosioned


3. Soil Erosion
3.1 Overview of processes
Soil erosion is the detachment and transportation of soil particles by the forces of water and/or wind.  It is a process that transforms soil into sediment. Sediment consists of transported and deposited particles or aggregates derived from rock, soil, or biological material.
3.1.1 Geologic vs. Accelerated Soil Erosion
Geological erosion is a natural process that wears down topographic highs (hills and mountains) and fills in topographic lows (valleys, lakes, and bays) through the deposition of eroded sediments.
3) Dissolution (or solution) water is capable of dissolving
Erosion that exceeds normal geologic erosion becomes destructive and is called accelerated erosion.  This type of erosion occurs when the soil and natural vegetation are disturbed by human activity.  Accelerated erosion is often 10 to 1000 times as destructive as geological erosion.
3.1.2 Soils Susceptible to Erosion
Soils that are susceptible to erosion include:
·         soils with low water infiltration capability
·         soils with low organic matter content
·         soils with poor (unstable) structure
·         soils on steep hills (especially in regions of high rainfall)
·         soils with hydrophobic characteristics (usually intensified by fire)
3.1.3 Effects/Consequences of Soil Erosion
Soil erosion causes two main problems: 
·         Loss of soil productivity: When topsoil erodes, the less fertile and harder B horizon becomes exposed.  This leads to lower forage production, lower water infiltration and greater runoff.
  • Sediment pollution: when eroded sediment is rich in fertilizers or pesticides, it can upset the ecosystem at its point of deposition.  In addition, sediments may damage machinery, agitate respiratory problems and reduce visibility.
3.2 Water Erosion
3.2.1 Mechanism:
There are three steps to accelerated erosion by water:
1)    Detachment or loosening of soil particles caused by flowing water, freezing and thawing of the topsoil, and/or the impact of falling raindrops.
2)    Transportation of soil particles by floating, rolling, dragging, and/or splashing.
3)    Deposition of transported particles at some place lower in elevation.
Mechanics: detachment, transportation, deposition
Description: http://www.landfood.ubc.ca/soil200/images/09images/9.2.1mechanics.jpg
The three-step process of soil erosion by water starts with the impact of raindrops on soil.
Susceptibility to wind erosion is related to the following soil properties:
  • water content
  • stability of dry soil aggregates
  • stability of soil crust
  • surface roughness
  • vegetative and/or mulch cover
Soil profile - a vertical section of soil from the ground surface to the parent rock
Profile - a vertical section of the Earth's crust showing the different horizons or layers. If there is no compaction present, the topsoil will present a crumbly face throughout the topsoil profile and, in this condition, every part of the soil profile can be accessed by the plant roots. It also helps draw nutrients into the upper regions of the soil profile where cash crops can use them the next season.
Definition of soil profile: The vertical section of the soil showing the various layers from the surface to the unaffected parent material is known as a soil profile.
Master horizons and sub horizons
O horizon: It is called as organic horizon. It is formed in the upper part of the mineral soil, dominated by fresh or partly decomposed organic materials.
  • This horizon contains more than 30% organic matter if mineral fraction has more than 50 % clay (or) more than 20 % organic matter if mineral fraction has less clay.
  • The organic horizons are commonly seen in forest areas and generally absent in grassland, cultivated soils.
        • O1 - Organic horizon in which the original forms of the plant and animal residues can be recognized through naked eye.
        • O2 - Organic horizon in which the original plant or animal matter cannot be recognized through naked eye.
  • A horizon - Horizon of organic matter accumulation adjacent to surface and that has lost clay, iron and Aluminum.
        • A1 - Top most mineral horizon formed adjacent to the surface. There will be accumulation of humified organic matter associated with mineral fraction and darker in Color than that of lower horizons due to organic matter.
        • A2 - Horizon of maximum eluviation of clay, iron and aluminium oxides and organic matter. Loss of these constituents generally results in accumulation of quartz and other sand and silt size resistant minerals. Generally lighter in Colour than horizons above and below.
        • A3 - A transitional layer between A and B horizons with more dominated properties of A1 or A2 above than the underlying B horizon. This horizon is sometimes absent. Solum.
  • B horizon - Horizon in which the dominant features are accumulation of clay, iron, aluminium or humus alone or in combination. Coating of sesquioxides will impart darker, stronger of red Colour than overlying or underlying horizons.
        • B1 - A transitional layer between A and B. More like A than B.
        • B2 - Zone of maximum accumulation of clay, iron and aluminium oxide that may have moved down from upper horizons or may have formed in situ. The organic matter content is generally higher and Colour darker than that of A2 horizon above.
        • B3 - Transitional horizon between B and C and with properties more similar to that of overlying B2 than underlying C.
  • C horizon - It is the horizon below the solum (A + B), relatively less affected by soil forming processes. It is outside the zone of major biological activity. It may contain accumulation of carbonates or sulphates, calcium and magnesium
  • R - Underlying consolidated bed rock and it may or may not be like the parent rock from which the slump is formed.
3.3 Wind Erosion
3.3.1 Mechanics       
·         Wind erosion occurs where soil is exposed to the dislodging force of wind.  The intensity of wind erosion  varies with surface roughness, slope, type of cover on the soil surface, and wind velocity, duration, and angle of incidence.  Fine soil particles can be carried to great heights and for hundreds of kilometers.
Susceptibility to wind erosion is related to the following soil properties:
           Water content
           Stability of dry soil aggregates
           Stability of soil crust
           Surface roughness
           Vegetative and/or mulch cover

Monday, July 8, 2013

Rivers system of Bangladesh


Rivers

Atrai River
Atrai River (also spelt as Atreyee) (Bengali: আত্রাই/আত্রেই নদী) flows in West Bengal and northern parts of Bangladesh. In ancient times the river was called Atrei and finds a mention in the Mahabharata. It is linked with Karatoya River. It originates in West Bengal and then after flowing through Dinajpur District of Bangladesh, it enters India again. It passes through Kumarganj and Balurghat community development blocks in Dakshin Dinajpur district. The river then re-enters Bangladesh. It splits into two rivers - the Gabura and the Kankra in Dinajpur district. It crosses the Barind Tract and flows into Chalan Beel. The river serves as a perennial source of fishing, even though it is often the cause of flooding in many areas during monsoons. Total length of this river is approximately 240 miles (390 km). Maximum depth of river is 99 feet (30 m).
Balu River

The Balu is a river of Bangladesh. It runs mainly through the swamps of Beel Belai and that east of Dhaka, joining the Shitalakshya near Demra. During the flood season, the Balu is of importance for local drainage and access by small boats.

Bangali River
The Bangali River (Bengali: বাঙালি নদী) is one of the main rivers in the northern part of Bangladesh (commonly known as North Bengal). As of 2007, the river is in the news because of the possibility that it might merge with the Jamuna River, which could lead to major changes in the geography of the region. The Bangali River originates as a distributary of Teesta River in Nilphamari District. The river flows as the Ghaghot River from its source to Gaibandha, where it splits into two branches – one moves towards the west as the "Ghaghot" and empties into the Karatoya River at Sherpur, Bogra District; the other section of the Bangali River flows to the south and subsequently breaks into two sections in Bogra. These two sections join the Jamuna and Karatoa. There are a number of distributaries of the Bangali River such as the Belal, Manosh, Modhukhali, Ichamoti, and Volka among others. These distributaries often dry up in the winter season.

Baral River
Baral (Bengali: বড়াল) river is one of the offshoots of the Ganges, starts its journey at Charghat Upazila or Rajshahi District of Bangladesh. The Baral flows through Natore and Pabna meets with the Gumani at the east of Bangura and finally meets with the Hurasagar after joining with the Karatoya south of Shahjadpur. The river is approximately 147 kilometers long and 410 feet (120 m) wide and 20 feet (6.1 m) deep on average. The river receives water from the Ganges only in the monsoon season. But it maintains its flow throughout the year with local runoff water and water from chalan beel. Its drainage area is about 230 km². Some important places located on the banks of the Baral are: Charghat; Baraigram, Bagatipara, Gurudaspur, Chatmohor, Bhangura and Bera. The Baral Bridge is located on this river at Bhangura Upazila.

Biskhali River
The Biskhali is a river of Bangladesh. The river flows through Barguna District.

Brahmaputra River
The Brahmaputra, also called Tsangpo-Brahmaputra, is a trans-boundary river and one of the major rivers of Asia. From its origin in southwestern Tibet as the Yarlung Zangbo River, it flows across southern Tibet to break through the Himalayas in great gorges and into Arunachal Pradesh where it is known as Dihang. It flows southwest through the Assam Valley as Brahmaputra and south through Bangladesh as the Jamuna. There it merges with the Ganges to form a vast delta. About 1,800 miles (2,900 km) long, the river is an important source for irrigation and transportation. Its upper course was long unknown, and its identity with the Yarlung Tsangpo was only established by exploration in 1884-86. This river is often called Tsangpo-Brahmaputra river. The average depth of river is 124 feet (38 m) and maximum depth is 380 feet (120 m). In Bangladesh the river merges with the Ganges and splits into two: the Padma and Meghna River. When it merges with the Ganges it forms the world's largest delta, the Sunderbans. The Sunderbans is known for tigers, crocodiles and mangroves. While most Indian and Bangladeshi rivers bear female names, this river has a rare male name, as it means "son of Brahma" in Sanskrit (putra means "son"). The Brahmaputra is navigable for most of its length. The lower part reaches are sacred to Hindus. The river is prone to catastrophic flooding in spring when the Himalayan snows melt. It is also one of the few rivers in the world that exhibit a tidal bore.

Bura Gauranga River
The Bura Gauranga River is located in the Patuakhali district in Bangladesh.

Buriganga River
The Buriganga River (Bangla: বুড়িগঙ্গা Buŗigônga "Old Ganges") is the main river flowing beside Dhaka city, capital of Bangladesh. The average depth is 39 feet (12 m) and maximum depth is 93 feet (28 m). In the distant past, a course of the Ganges river used to reach the Bay of Bengal through the Dhaleshwari river. This course gradually shifted and ultimately lost its link with the main channel of the Ganges and was renamed as the Buriganga.

Dakatua River
The Dakatua River or Dakatia is a river of Bangladesh and India. The length of the Dakatia is about 207 km. It enters the country from India in Comilla district from Tripura state and is a tributary of the Meghna River. The source of the river is at Chauddagram Khal, which connects it with the Little Feni. The river joins the Meghna at Raipur

Dhaleshwari River
The Dhaleshwari River (Bangla: ধলেশ্বরী Dhôleshshori) is a 160-km-long distributary of the Jamuna River in central Bangladesh. It starts off the Jamuna near the northwestern tip of Tangail District. After that it divides into two branches: the north branch retains the name Dhaleshwari and merges with the other branch, the Kaliganga River at the southern part of Manikganj District. Finally the merged flow meets the Shitalakshya River near Narayanganj District. This combined flow goes southwards to merge into the Meghna River. Average depth of river is 122 feet (37 m) and maximum depth is 265 feet (81 m).
The Dhaleshwari is presently a branch of the Jamuna but in the past was probably part of the main course of the Padma. The course of the Padma has changed considerably during the period 1600 to 2000 AD. It is difficult to trace accurately the various channels through which it has flowed. The probability is that it flowed past Rampur Boalia, through Chalan Beel, the Dhaleshwari and Buriganga rivers, past Dhaka into the Meghna estuary. In the 18th century, the lower course of the river flowed further south. About the middle of the 19th century the main volume of the channel flowed through this southern channel which came to be known as Kirtinasa. Gradually the Padma adopted its present course

Dhepa River
The Dhepa is a small river in northern Bangladesh. The river originates from the Atrai river in Mohanpur and falls into the Punarbhaba. The length of this river is 40 km.

Feni River
Feni River (Bangla: ফেনী নদী Feni Nodi) is a river in the Indian state of Tripura and southeastern Bangladesh. It is a trans-boundary river with an on-going dispute. Feni River originates in South Tripura district and flows through Sabroom town and then enters Bangladesh. It enters Bangladesh at Belchhari in Matiranga Upazila of Khagrachari District. It flows through Ramgarh Upazila (Khagrachari), Fatikchhari Upazila (Chittagong) and then flows along the border of Chittagong (Mirsharai Upazila) and Feni (Chhagalnaiya Upazila, Feni Sadar Upazila, Sonagazi Upazila) districts and discharges into the Bay of Bengal near Sonagazi. The length of the river is 108 km. The river forms the international boundary at some points. Muhuri River, also called Little Feni, from Noakhali District joins it near its mouth. The river is navigable throughout the year by small boats up to Ramgarh, some 80 km upstream. A 3.41-km long closure dam was constructed across the river in 1965-66 at a cost of 593.5 million takas to divert the flow through the Feni regulator. It is located between Mirsharai and Sonagazi, in the Chittagong and Feni districts respectively. It was constructed to prevent saline water intrusion from downstream and retain fresh water upstream for use in the Muhuri Irrigation Project.

Gorai-Madhumati River
The Gorai-Madhumati River (Bangla: গড়াই-মধুমতি Gôŗai-Modhumoti) is one of the longest rivers in Bangladesh and a tributary of the Ganges.

Halda River
Halda River is a river in South-Eastern Bangladesh. It originates at the Badnatali Hill Ranges in Ramgarh Upazila in the Chittagong Hill Tracts, flows through Fatikchhari Upazila, Hathazari Upazila, Raozan Upazila and Chittagong Kotwali Thana, and falls into the Karnaphuli River. The 81 km long river has a very turbulent tributary, the Dhurung River, which joins Purba Dhalai about 48.25 km downstream. The river is navigable by big boats 29 km into it (up to Nazirhat) and by small boats 16-24 km further (up to Narayanhat). The Halda river is also famous for breeding pure Indian carp. This is the only pure Indian carp breding field of Bangladesh, perhaps in South Asia.

Jaldhaka River
The Jaldhaka River (Nepali: जलढका Jalḍhaka) is a trans-boundary river, with a length of 192 kilometres, that originates in southeastern Sikkim in the eastern Himalayas and flows through the Jalpaiguri and Cooch Behar districts of West Bengal, India. At that point the river enters Bangladesh through the Lalmonirhat District and then joins with the Dharla River until the Dharla debouches into the Brahmaputra River near the Kurigram District. Due to the river's wandering over several international borders, only a small length of the river lies within Bangladesh.

Jamuna River
The Jamuna River (Bangla: যমুনা Jomuna) is one of the three main rivers of Bangladesh. It is the main channel of the Brahmaputra River when it flows out of India into Bangladesh. The Jamuna flows south, ending its independent existence as it joins the Padma River (Pôdda) near Goalundo Ghat. Merged with the Padma (Pôdda), it meets the Meghna River near Chandpur. Its waters then flow into the Bay of Bengal as the Meghna River. The river's average depth is 395 feet (120 m) and maximum depth is 1,088 feet (332 m). The Jamuna was a barrier in establishing a direct road link between capital Dhaka and northern part of Bangladesh better known as Rajshahi Division until 1996. This was mitigated by the completion of the Jamuna Multi-Purpose Bridge.

Karnaphuli River
Karnaphuli (Bangla: কর্ণফুলি Kôrnophuli) (also spelt Karnafuli) is a 667 metres (2,190 ft) wide river in the south-eastern part of Bangladesh. Originating from the Lushai hills in Mizoram, India, it flows 270 km (170 miles) southwest through Chittagong Hill Tracts and Chittagong into the Bay of Bengal. A large hydroelectric power plant using Karnaphuli river was built in the Kaptai region during the 1960s. The mouth of the river hosts Chittagong sea port, the main port of Bangladesh. The depth of river is 102 metres (330 ft), in average and 147 metres (480 ft), on maximum.

Kaptai dam
The Kaptai Dam is the location of the Karnaphuli Hydro-power station, the only hydro-electric power plant in Bangladesh, was constructed in Kaptai in 1962. An earth-filled dam on the Karnaphuli River, the Kaptai Dam created the Kaptai Lake, which acts as the water reservoir for the hydropower station. The power plant produces a total of 230 megawatts of electricity.

Karotoa River
The Karotoa River is a river of Bangladesh. The depth of river is approximately 6 feet (1.8 m), in origin of Mahasthangarh, Bogra.

Khowai River
Khowai River originates from the eastern part of the Atharamura Hills of Hill Tripura in India. Flowing west and northward, the Khowai enters Bangladesh at Balla in Sylhet district. The river further flows beside the east of Habiganj town and debouches into the Meghna near the mouth of the Kalni at Nabiganj.

Kopothakho River
The Kopothakho River is a river of Bangladesh.

Kushiyara River
The Kushiyara River is one of the many rivers in Bangladesh that crosses international boundaries. It originates in the northern hill country of Assam, India and runs along the border of the Indian states of Nagaland and Manipur before entering Bangladesh. The total length of the Kushiyara is about 161 km. The average width of the river is 830 feet (250 m) and in the rainy season the mean depth of the Kushiyara reaches up to 33 feet (10 m), the maximum depth of river is 40 feet (12 m). The river carries a huge amount of water as well as sediments from Karimganj in Assam and the hilly areas of Hill Tripura. The highest and lowest discharges have been measured at Sherpur amounting to 3,700 cumecs and 33 cu mecs respectively.

Mahananda River
The Mahananda River (Bangla: মহানন্দা Môhanônda) is a river the originates in the district of Darjeeling in West Bengal in the Himalayas. It flows through northern part of West Bengal, Bihar in India and Bangladesh. It again enters India in the Malda district of West Bengal before entering into Bangladesh to join the Ganges near the town of Chapai Nawabganj. This river is mainly fed by rainwater. During summer or winter it has very low water level and during monsoon it carries large amount of rainwater often causing floods. Some major places by the side of the river are Siliguri and Malda both in West Bengal, India. In Bangladesh this rivers total length is 36 km.

Manu River, Tripura
The Manu River originates in the mountains of Tripura (India) and plunges downward through dramatic gorges and steep escarpments until it reaches a broad plain where it becomes slow and meandering, going northward until it reaches the Sylhet plains. The river enters Bangladesh through Kulaura Upazila in Maulvi Bazar district, when it changes its course to northwest and north to meet the Kushiyara at Manumuk

Meghna River
The Meghna River (Bengali: মেঘনা নদী) is an important river in Bangladesh, one of the three that forms the Ganges Delta, the largest on earth fanning out to the Bay of Bengal. The Meghna is formed inside Bangladesh by the joining of different rivers originating from the hilly regions of eastern India. The river meets Padma River in Chandpur District. The river ultimately flows into the Bay of Bengal in Bhola District.
The Meghna is the widest river among those that flow completely inside the boundaries of Bangladesh. At one point near Bhola, Meghna is 12 km wide. In its lower reaches this river follows almost a straight line in its path. Despite its very calm and quiet look, this river is the cause of many deaths every year. The place near Chandpur is a very dangerous one. The river's average depth is 1,012 feet (308 m) and maximum depth is 1,620 feet (490 m) The Meghna is formed inside Bangladesh by the joining of different rivers originating from the hilly regions of eastern India. The Meghna is formed inside Bangladesh above Bhairab Bazar by the combination of the Surma and Kushiyara rivers. Down to Chandpur, Meghna is hydrographically referred to as the Upper Meghna. After the Padma joins, it is referred to as the Lower Meghna. Near Muladhuli in Barisal district, the Safipur River is an offshoot of the Surma that creates one of the main rivers in South Bengal. 1.5 km wide, this river is one of the widest in the country as well. This river is the widest in Bangladesh and one of the widest of the world.
At Ghatalpur of Brahmanbaria District, the river Titas emerges from Meghna and after circling two large bends by 240 km, falls into the Meghna again near Nabinagar Upazila. Titas forms as a single stream but braids into two distinct streams which remain separate before re-joining the Meghna.

Muhuri River
Muhuri River (Bangla: মুহুরী Muhuri) one of the trans-boundary rivers of Bangladesh. The river takes its rise on the Lushai hills of Tripura in India and enters Bangladesh through Parshuram upazila of Feni district after flowing over the hilly regions of India. As such the river is wild in nature and often causes flash floods. At some places it demarcates the boundary between India and Bangladesh and falls into the Bay of Bengal after dividing the Feni and the Chittagong district. The Muhuri is not wide enough and it is only 150 to 200 metres wide. But the width increases towards the sea. Close to the sea, the river is under tidal influence. There is a closure dam on the river about 4 km upstream from the estuary for irrigation purpose and a 20-vent regulator has also been constructed. During high tide, the dam along with the regulator controls the influx of saline water. This river is also a line of contention between the two neighbouring countries, India and Bangladesh. The border of the two nation (India-Bangladesh) according to Indira - Mujib treaty is defined as the mid of the river. There is a huge and advanced dam in one side of it (this part belongs to India, Belonia- Bankar area). Thus in the rainy seasons the flood water cannot cause much disaster in this portion, whereas most of the times it causes a menace in the lower areas. In course of time the river engulfed a huge area of Bangladesh provience, increasing the boundary of Indian part. This is the main reason of border dispute.

Naf River
Naf River (নাফ নদী) is a river marking the border of Bangladesh and Myanmar. It is an elongated estuary in the extreme southeast of Cox's Bazar district dividing the district from Arakan, Myanmar. It rises in the Arakan hills on the southeastern borders of the district and flows into the Bay of Bengal. Its width varies from 1.61 km to 3.22 km. The river is influenced by tide. Akyab in Myanmar is on the eastern bank and Teknaf upazila of Cox's Bazar district is on the western bank of the river. The Naf River is deepest. Is average depth is 128 feet (39 m) and maximum depth is 400 feet (120 m).

Padma River
The Padma (Bengali: পদ্মা Pôdda) is a major trans-boundary river in Bangladesh. It is the main distributary of the Ganges (Bengali: গঙ্গা Gôngga), which originates in the Himalaya. The Padma enters Bangladesh from India near Chapai Nababganj. It meets the Jamuna (Bengali: যমুনা Jomuna) near Aricha and retains its name, but finally meets with the Meghna (Bengali: মেঘনা) near Chandpur and adopts the name 'Meghna' before flowing into the Bay of Bengal. Rajshahi, a major city in western Bangladesh, is situated on the north bank of the Padma. Its maximum depth is 1,571 feet (479 m) and average depth is 968 feet (295 m).

Punarbhaba River
The Punarbhaba (Bengali: পুনরভব নদী) is a river of Bangladesh and West Bengal in India, of total length about 160 km and a width of 3–8 km. It originates from the lowlands of Thakurgaon District. The river's upper part is a few kilometres west of Atrai. It flows through Gangarampur and Tapan community development blocks of Dakshin Dinajpur district of West Bengal. After flowing to the south, this river meets with the Dhepa River. Ultimately it flows into the Ganges. The length of this river is 160 km (99 mi).

Pasur River
The Pusur River is a river in southwestern Bangladesh and a tributary of the Ganges.

Shitalakshya River
Shitalakshya River (Bengali: শীতলক্ষ্যা নদী Shitalokkha Nodi) (also known as Lakhya River) is a distributary of the Brahmaputra. In its initial stages it flows in a southwest direction and then east of the city of Narayanganj in central Bangladesh until it merges with the Dhaleswari near Kalagachhiya. A portion of its upper course is known as Banar River. The river is about 110 km long and at it widest, near Narayangani, it is 300 meters in width. Its highest discharge has been measured at 2,600 cusec at Demra. It remains navigable year round. The river flows through Ghazipur forming its border with Narsingdi for some distance and then through Narayanganj. The river's maximum depth is 70 feet (21 m) and average depth is 33 feet (10 m). The length of this river is 110 km (68 mi).

Surma River
The Surma River (Bengali: সুরমা নদী Shurma Nodi) is a major river in Bangladesh, part of the Surma-Meghna River System. It starts when the Barak River from northeast India divides at the Bangladesh border into the Surma and the Kushiyara rivers. It ends in Kishoreganj District, above Bhairab Bazar, where the two rivers rejoin to form the Meghna River. The waters from the river ultimately flow into the Bay of Bengal. The average depth of river is 282 feet (86 m) and maximum depth is 550 feet (170 m).

Teesta River
The River Teesta or Tista (Nepali: टिस्टा खोला TisTa Khola, is said to be the lifeline of the Indian state of Sikkim, flowing for almost the entire length of the state and carving out verdant Himalayan temperate and tropical river valleys. The emerald-coloured river then forms the border between Sikkim and West Bengal before joining the Brahmaputra as a tributary in Bangladesh. The river originates from Cholamo Lake at an elevation of 5,330 m (17,487 ft) above sea level in the Himalayas. This lake lies to the north of the Donkia pass near Shetschen, where the summit of the pass is about eight kilometres north-east of Darjeeling.
The Teesta River is then fed by rivulets which arise in the Thangu, Yumthang and Donkia-La ranges. The river then flows past the town of Rangpo where it forms the border between Sikkim and West Bengal up to Teesta Bazaar. At Teesta Suspension Bridge, which joins Kalimpong with Darjeeling, the river is met by its main tributary, the Rangeet River. At this point, it changes course southwards flowing entirely into West Bengal. The river hits the plains at Sevoke, where it is spanned by the Coronation Bridge which links the north east states to the rest of India. The river then courses its way to Jalpaiguri and then to Rangpur District of Bangladesh, before finally merging with the mighty Brahmaputra at Fulcherry.

Titas River
Titas River (Bangla: তিতাস Titash) is a trans-boundary river of south-eastern Bangladesh. It originates in the state of Tripura in India where it is known as Haora River in Bengali and Saidra in the local Kokborok language. Flowing near Agartala, (India), it enters Bangladesh through Akhaura Upazila in the Brahmanbaria District of Bangladesh, then merges with the Meghna River to the south near Ashuganj. The length of the river is about 98 km. There is another river of the same name which starts as a distributary of the Meghna and flows back into it.

Turag River
The Turag River (Bengali: তুরাগ নদী Turag Nɔdī; IPA: [T̪uraɡ Nɔd̪i]) is the upper tributary of the Buriganga, a major river in Bangladesh. The Turag originates from the Bangshi River, the latter an important tributary of the Dhaleshwari River, flows through Gazipur and joins the Buriganga at Mirpur in Dhaka District. It is navigable by boat all year round.
Exemplifying the riverine character of Dhaka, the Turag is abundant in fish but suffers from acute water pollution. While attempts have been made to marginally widen the river, the majority of industry has made little effort to follow environmental law and the water has become visibly discolored.