Chalan Beel

Chalan Beel (Bengali: চলনবিল) is a wetland in Bangladesh. It is a large inland depression, marshy in character, with rich flora and fauna. Forty-seven rivers and other waterways flow into the Chalan Beel.[1] As silt builds up in the beel, its size is being reduced.[2]

Chalan Beel
Chalan Beel in Natore District
Chalan Beel
LocationRajshahi Division
Coordinates24.52°N 89.01°E / 24.52; 89.01
Primary inflowsAtrai River and 46 others
Basin countriesBangladesh
Surface area26 km2 (10 sq mi)
Average depth2 m (6.6 ft)
Max. depth4 m (13 ft)

Location and extent

Overview map showing Chalan Beel among the main rivers in North Bengal

Chalan Beel is an extensive lowland area in the lower Atrai basin, and spreads across Singra and Gurudaspur upazilas on Natore District, Chatmohar, Bhangura and Faridpur upazilas of Pabna District, and Ullahpara, Raiganj and Tarash upazilas of Sirajganj District. It consists of a series of beels connected to one another by various channels to form a continuous water body during the rainy season. Although the beel area expands into a vast water body with dense aquatic vegetation as long as the Jamuna remains flooded during the monsoon months, it dries out in the winter months, leaving only patches of water in the central parts of this zone.[3]

Chalan Beel is fast silting up. In the past it covered an area of about 1,085 km2 but was reduced to 368 km2 in 1909, of which only 85 km2 remained underwater throughout the year. It has since shrunk to only 26 km2.[2]

History

The most important factor dominating the river history in Bengal is the large proportion of silt carried by its rivers. It is the silt which has created the land and made it habitable by building it up through the centuries. It is silt which is fertilising the land, but the silt, which has been the most beneficial gift of nature, has also produced most of the river problems now confronting the people of Bengal. Silt deposited in the old river channel beds has forced them to change course, creating problems for abandoned areas while assisting in developing new areas.[4]

The main volume of water from the Ganges River began flowing through the Padma channel in the sixteenth century. Silt from the Padma helped in building up the southern portion of north Bengal. This is the most plausible explanation for the existence of a depression around Chalan Beel. The Teesta was active in the region until it changed its course in 1787. This territory lies in between the land raised in the north by the Teesta system when it was active and that in the south by the Padma.[5]

However, there is another explanation for the creation of the depression. The Padma has been changing its course over the centuries. In Ven den Brouck's map of Bengal, prepared in 1660, the main channel of the Padma is shown as flowing through Faridpur-Bakharganj, but there also is a suggestion of another, possibly earlier channel. This channel runs through Rampur Boalia in Rajshahi, Chalan Beel, Dhaleswari and Buriganga before meeting the Meghna. At that time the Jamuna was virtually non-existent and the Brahmaputra used to flow through its old channel.[6]

Historical depictions of Chalan Beel
Van den Brouck's map of 1660
James Rennell's map of 1776

Impact of railways

An estimate taken in 1945 found about 47 rivers and other waterways flowed into the Chalan Beel, a watershed of about 1,547 square miles (4,010 km2). In addition to being a crossroads for the many waterways it also served as the origin for the many rivers flowing south or east that eventually meet with the Padma or Jamuna. In the early 1900s, Chalan Beel began to be hemmed in by the construction of the Eastern Bengal Railway main line on the west and the Santahar-Bogra branch line on the north. The natural pattern of the water's drainage channels in this area were disrupted by the obstruction caused by the railway construction since railways in these low lands had to be built on embankments.[1]

Flora and fauna

The banks of the beel are covered with dense stands of kash, babla, nol, dhol kolmi, simul, and date palm. Seven species of frogs and one species of toad represent the amphibian fauna. Chalan Beel has a total of 34 species of reptiles, including ten turtles and tortoises, nine lizards and various snake species. There are 27 species of mammals from 12 families.[3]

Pollution

Chalan Beel has experienced the negative effects of pesticide use in the surrounding farmlands. In 2010, Bangladesh Agricultural University research, found pesticide use has increased sixfold since 1982, and the fish population of Chalan Beel has halved in the same period. A 25 kilometre highway constructed on the Beel has divided into two and caused havoc on the fish breeding by disrupting their movement. Commercial overfishing, grill and drag net and other destructive fishing have harmed the fish population.[7]

References

  1. Srinivasan, Roopa; Tiwari, Manish; Silas, Sandeep (2006). Our Indian Railway: Themes in India's Railway History. New Delhi: Foundation Books. ISBN 81-7596-330-1. Retrieved 29 November 2007.
  2. Alam, Mohd Shamsul; Hossain, Md Sazzad (2012). "Chalan Beel". In Islam, Sirajul; Jamal, Ahmed A. (eds.). Banglapedia: National Encyclopedia of Bangladesh (Second ed.). Asiatic Society of Bangladesh.
  3. Nishat, Ainun; Huq, S. M. Inamul; Barua, Shuvasish P.; Reza, Ali A. H. M.; Khan, A. S. Monirazzaman, eds. (2002). Bio-ecological zones of Bangladesh. International Union for Conservation of Nature Bangladesh Country Office. ISBN 978-984-31-1090-9. Retrieved 29 November 2007.
  4. Majumdar, S.C., Chief Engineer, Bengal, Rivers of the Bengal Delta, Government of Bengal, 1941, reproduced in Rivers of Bengal, Vol I, 2001, p. 101, published by Education Department, Government of West Bengal.
  5. Majumdar, S.C., p. 46
  6. Roy, Niharranjan, Bangalir Itihas, Adi Parba, (in Bengali), first published 1972, reprint 2005, p. 83, Dey’s Publishing, 13 Bankim Chatterjee Street, Kolkata, ISBN 81-7079-270-3
  7. "Bangladesh's once plentiful rivers run low on fish". The Independent. London. Agence France-Presse. 26 December 2010. Archived from the original on 22 July 2015. Retrieved 12 July 2015.
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