Flood & Erosion

Flood is a recurring feature of the District which causes extensive damage almost every year. The South Salmara - Mankachar Sub-Division is worst affected by floods every year, particularly the entire South Salmara revenue Circle and Sukchar areas under Mankachar Circle. Major portion of South Salmara Circle has already been washed away by errosion.Under Golokganj revenue Circle, Golokganj Town and Pub-Kanuri village are affected by flood and erosion of river Gangadhar.Bilasipara Sub-Division is mostly affected by flash floods of River  Gaurang originating from Bhutan.

Chronological Flood History of Dhubri District

Sl. No. Year of Occurrence Intensity of Disaster
  1950 Very high flood with severe earthquake.
  1954 High flood
  1957 High flood
  1962 High flood
  1968 High flood with severe landslides from Bhutan
  1974 Very high flood, semi famine conditions. His Excellency the President of India visited Relief camps.
  1980 High flood
  1984 High flood
  1987 High flood
  1988 Highest flood level recorded ( 30.36 mtrs.)
  1998 High flood (29.98 mtrs.)
  2002 High flood ( 30.11 mtrs.)
  2003 Cyclone and Thunder storms with flood
  2004 High flood ( 30.07 mtrs.)

Details of Rivers and Tributaries

Name of the River/Tributaries
Origin
Length in Dhubri
Danger level
Maximum Water Level
No. of days above danger level
Bramhaputra Tibbet
88 Km
28.62 mtr. at Dhubri
30.36 mtr.
18
Gangadhar Bhutan
33 Km.
29.94 mtr. at Golakganj
30.37 mtr.
8
Gangadhar Bhutan
39 Km.
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Tipkai Bhutan
28 Km.
32.26 mtr. at Khoraghat
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Gaurang Bhutan
20 Km.
33.60 mtr. near Bilasipara
33.97 mtr.
7
Champamoti Bhutan
24 Km.
33.95 mtr. at Bahalpur
37.69 mtr.
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Kaloo Garo Hills
22 Km
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Jinjiram Garo Hills
49 Km.
28.70 mtr. at Molakhowa
29.98 mtr.
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