Skip to main content

Flood in Assam Causes and Measures | North East India Info

Assam with its vast network of rivers is prone to natural disasters like flood and erosion which has a negative impact on the overall development of the stateThe Brahmaputra and Barak River with more than 50 numbers of tributaries feeding them, causes the flood devastation in the monsoon period each year. The flood and erosion problem of Assam is singularly different from other states so far as extent and duration of flooding and magnitude of erosion is concerned and is probably the most acute and unique in the country. 

The flood-prone area of the state as assessed by the Rashtriya Barh Ayog (RBA) is 31.05 Lakh Hectares against the total area of state 78.523 Lakh Hectares i.e. about. 39.58 % of the total land area of Assam. This is about 9.40% of total flood prone area of the country. Records show that average annual area affected by flood is 9.31 Lakh Hectares. The flood prone area of the country as a whole stands at about 10.2 % of the total area of the country, but flood prone area of Assam is 39.58 % of the area of the state. It signifies that the flood prone area of Assam is four times the national mark of the flood prone area of the country. 

During post-independence period, Assam faced major floods in 1954, 1962, 1972, 1977, 1984, 1988, 1998, 2002, 2004 and 2012. Almost every year three to four waves of flood ravage the flood prone areas of Assam. Average annual loss due to flood in Assam is to the tune of Rs. 200.00 Crores and particularly in 1998, the loss suffered was about Rs. 500.00 Crores and during the year 2004 it was about Rs. 771.00 Crores.

Assam Flood

Causes of Flood in Assam

  • Heavy Rain Fall and Snowmelt Water in Summer: throughout the Northeast India, average rainfall is very high, varying between 100cm to 1300cm. beside about 80% of the annual rainfall comes mainly in the five summer months from May to September. This is also the period when the snow over the Himalayas melt and water therefrom rolls down the rivers to the Brahmaputra valley. The supply of water thus becomes excessive in the rivers and flooding occurs.
  • Location Of the Plains: each of the Brahmaputra and Barak plains surrounded on three sides by high hills and mountains. Whenever there is rainfall in the hills and mountains water rushes down to limited plains from extensive catchment areas, flooding the plains.
  • Low Gradient of the Plains: the Brahmaputra and Barak valleys grade very gently towards their downstream. It is found that the gradient of the Brahmaputra between Sadiya and Dhuburi is 13 cm per km on average. Therefore, excessive rain and snow-melt water flow down very slow causing floods in these plains.
  • Chocking pf the River Channels: the hills and mountains of Himalayas, eastern Arunachal, Nagaland, and North Cachar hills, Manipur, Mizoram and Tripura are made of relatively soft tertiary rockes. The heavy monsoons rain that fall on them further softens the materials casing solifiluction and sheet erosion down the steep slops. The streams carry these sediment to down slop thus their carrying capacity is reduce  and the sediment deposited on their beds   and chocking the channels.
  • Sifting of the River Courses:  the rivers of Assam, especially the ones that comes down from the Himalayan and the Tertiary hills change their courses frequently. This is mainly because the rivers carrying enormous quantities of sediments from the hills and on reaching the plain the sediments are deposited on their own beds. The channels thus filled up and the water in the following summers dig out different courses abandoning the earlier once. Besides, the seismic instability of the region also contributes to such shifts.

Important  Measures

1.      Constriction of embankment in a planned manner in some selected areas only.
2.      Controlling he major rivers by constricting dams and reservoirs.
3.      Cheeking bank erosion.
4.      Stopping deforestation and take up afforestation in the catchment areas.
5.      Undertaking protection work of settlements, both rural and urban.
6.      Constriction of drainage channels, culverts and sluice gates whenever necessary.
7.    Constriction of raised platforms near the settlement of the flood pore area for taking shelter for both man and animals.

Popular posts from this blog

Northeast India Physiography and Physiographic Divisions

Northeast India located in the extreme northeast corner of the Indian subcontinent with diverse physiography and relief features. In general, the region may be divided into three physiographical regions that are Plateau region, Plain regions and Mountain region.Because of its diversity of physiography the region endowed with rich and varied biophysical environments bounded by hills and mountains on its three sides except a narrow gap in the west.

Barail Range of Assam | North East India Info

The Barail Range is a group of mountain or high ridges and watershed between the Brahmaputra and Barak rivers. The terrain ranges from flat and undulating in the river valleys, to mountainous with steep slopes. Located in Dima Hasao district of Assam a state of India (Latitude: 25° 16' 27" N - Longitude: 93° 20' 51" E)

Black Rice-Nutrition, Recipe & Benefits | Manipuri Black Rice | Forbidden Rice

Black rice is a type of rice that belongs to the Oryza sativa L. species.The rice endosperm, which is translucent with grey to almost black color, turns deep purple when cooked. [1] My first encounter with Black Rice got me very fascinated and curious about this rice. At that time I thought I'm going to cultivate this rice in our own firm land as experiments see how it performed in our agricultural land. We also cultivated Assamese Red Rice (local name is Bao Paddy ) and 10 different varieties of local (native) rice.

Soils Found in Northeast India - Classification, Distribution and Erosion

Northeast India is a place of heavy rainfall, high relative humidity and high temperature cause rapid weathering of rocks. As weathering of surface rocks of the hills and mountains proceeds, the sheet flood caused by heavy rainfall remove the weathered materials and carry them down to the headward steams of the rivers.  The rapidly flowing rivers then carry the sediments, big and small, down to the foothills and plains.