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Bangladesh gaining 20 sq-km land a year.

Homo Sapiens

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Bangladesh gaining 20 sq-km land a year​

Every year, the country loses 32 sq-km of land due to erosion in rivers and the sea. On the other hand, 52 sq-km of new land emerges from the water​


new_lands_in_bangladesh-01.png

The landmass of Bangladesh is increasing by 20 square kilometres annually as tonnes of silts from rivers accumulate in the Bay of Bengal, forming new land, according to a study of the Bangladesh Centre for Environment and Geographical Information Service (CEGIS).

Over the last 100 years, around 2,000 sq-km of land has been added in the country, the study finds by analysing satellite images.

According to the CEGIS, every year, Bangladesh loses 32 sq-km of land due to erosion in rivers and the sea. On the other hand, 52 sq-km of new land emerges from the water.


The result has been published in a publication of "Char Development and Settlement Project- Bridging". The project is jointly financed by the land ministry, International Fund for Agricultural Development (Ifad) and the government of the Netherlands.

Rezaul Karim, land settlement officer of Ifad, said, "Bangladesh has regained 1,000 sq-km of land lost in the last 100 years due to river erosion. Of this, 93% of land is on the coast and the remaining 7% is on various rivers. The total area of the new land is about 2,000 sq-km."

However, Mohammad Shahidul Islam, director of Remote Sensing Devices, CEGIS, told The Business Standard that the rate of new land formation has decreased in recent years.

"The government has been working on the newly formed chars in the coast of Noakhali since 1973. However, the amount of sediments flowing through the Brahmaputra, Meghna and Padma rivers has decreased recently. At the same time the newly formed chars are being lost for various reasons. River erosion has also increased."

According to the Ministry of Land, the Noakhali coast of the Bay of Bengal has extended 55 km south in the 100 years from 1913 to 2013. Two cross dams built in 1957 and 1964 to protect Noakhali from the erosion of the River Meghna facilitated the formation of new chars in the surrounding areas.

Since 1980, land development work has been carried out in the newly formed chars which have now become green agricultural land.

From 1994 to June 2021, the government has allotted 83,798 acres of khas land (government-owned land) to 36,281 landless families. A target has been set to provide land to another 5,719 landless families by June 2022.


Nurul Islam, a resident of Noakhali's Char Mujib Asrayan project, said, "My grandfather was a resident of Sonapur in Noakhali. About 90 years ago, he settled in Char Badua. That is where my father was born. Later a new char Char Bhata formed in the south and he settled there. I was born in that char."

"But 20 years ago, I sold all the properties in Char Bhata for my father's cancer treatment. Now we are living in the newly formed Char Mujib's shelter project," he added.

In 2010, Alauddin and Bilkis started a new life on the 150-acre land provided by the government in Char Nangulia. The couple started farming with a small loan of only Tk5,000. At present, their capital is about Tk5 lakh.

Like them, at least 600 families have prospered in Noakhali's Chandina Union in the last one decade.

How new land is formed
According to the report of the Ministry of Land, in 1913 the coastline of Noakhali was near Sonapur. However, in the next 100 years, it spread 55 km south to Kearingchar.

Two cross dams were built in 1957 and 1964 to protect Noakhali from the erosion of the Meghna. These dams helped sediment accumulation. As a result, new land formed out of water. Besides, huge amounts of chars started to form due to the Muhuri dam at the mouth of Feni river after 1986.


Google Satellite images show that by June 2021, these lands expanded to about 20 km southeast. Many small chars in the River Meghna and the Bay of Bengal are slowly growing which will merge with the mainland of the country.

However, according to CEGIS, the 1950 Assam earthquake played the most important role in the formation of new land in Bangladesh. As a result of the landslide in that earthquake, a huge amount of silt started coming down from the Himalayas along the rivers.

From 1943 to 1973, 43 sq-km of land was formed in the territory of Bangladesh every year.

According to the Institute of Water Modeling (IWM), the area of southern Bangladesh increased by 629 sq-km in the 200 years from 1780 to 1980. In the next 41 years, another 83,798 acres of land have been developed under the Land Reclamation Project and the Char Development and Settlement Project.

In the last 100 years, many chars including Nijhum Dwip, Nolerchar, Kearingchar on the Noakhali coast; Urir Char, Bhashan Char in the Sandwip upazila of Chattogram have emerged from the water.

In Bhasanchar, which was formed almost two decades ago, 18,347 Rohingyas have already been relocated from Cox's Bazar refugee camps. Ganguria Char, formed within 1.5 km of Bhashan Char, covers an area of 100 sq-km. According to local people, cultivation would start in Ganguria Char in four to five years.


According to people concerned, at least 10 times more land is being formed around Hatia than the land being lost due to erosion. The newly formed chars in the west of Hatia include Dhalchar, Char Mohammad Ali, Char Yunus, Char Awal, Moulvirchar, Tamruddirchar etc. Besides, seven chars have also risen in Hatia river.

In the next one decade, the area of these chars will be about 500 sq-km.

Besides, new lands are being formed in the southern part of the country including Barisal and Khulna. Experts estimate that the area of these lands will be about 33,000 sq-km.

Saidur Rahman Chowdhury, professor of the Institute of Marine Sciences and Fisheries, Chattogram University, told The Business Standard, "These lands have been formed due to some favourable environments. However, they can also disappear due to slight changes, Therefore, both hard and soft methods can be followed to save the lands."

"The first thing to do in a newly formed land is afforestation. It is a soft method. Mangrove afforestation plays an effective role in this. Besides, if cross dams and technological initiatives are taken, like in the Netherlands or Singapore, the area of land that will rise on our coast in a few years will be about 15,000 square miles," he added.

 
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Bangladesh gaining 20 sq-km land a year​

Every year, the country loses 32 sq-km of land due to erosion in rivers and the sea. On the other hand, 52 sq-km of new land emerges from the water​


new_lands_in_bangladesh-01.png

The landmass of Bangladesh is increasing by 20 square kilometres annually as tonnes of silts from rivers accumulate in the Bay of Bengal, forming new land, according to a study of the Bangladesh Centre for Environment and Geographical Information Service (CEGIS).

Over the last 100 years, around 2,000 sq-km of land has been added in the country, the study finds by analysing satellite images.

According to the CEGIS, every year, Bangladesh loses 32 sq-km of land due to erosion in rivers and the sea. On the other hand, 52 sq-km of new land emerges from the water.


The result has been published in a publication of "Char Development and Settlement Project- Bridging". The project is jointly financed by the land ministry, International Fund for Agricultural Development (Ifad) and the government of the Netherlands.

Rezaul Karim, land settlement officer of Ifad, said, "Bangladesh has regained 1,000 sq-km of land lost in the last 100 years due to river erosion. Of this, 93% of land is on the coast and the remaining 7% is on various rivers. The total area of the new land is about 2,000 sq-km."

However, Mohammad Shahidul Islam, director of Remote Sensing Devices, CEGIS, told The Business Standard that the rate of new land formation has decreased in recent years.

"The government has been working on the newly formed chars in the coast of Noakhali since 1973. However, the amount of sediments flowing through the Brahmaputra, Meghna and Padma rivers has decreased recently. At the same time the newly formed chars are being lost for various reasons. River erosion has also increased."

According to the Ministry of Land, the Noakhali coast of the Bay of Bengal has extended 55 km south in the 100 years from 1913 to 2013. Two cross dams built in 1957 and 1964 to protect Noakhali from the erosion of the River Meghna facilitated the formation of new chars in the surrounding areas.

Since 1980, land development work has been carried out in the newly formed chars which have now become green agricultural land.

From 1994 to June 2021, the government has allotted 83,798 acres of khas land (government-owned land) to 36,281 landless families. A target has been set to provide land to another 5,719 landless families by June 2022.


Nurul Islam, a resident of Noakhali's Char Mujib Asrayan project, said, "My grandfather was a resident of Sonapur in Noakhali. About 90 years ago, he settled in Char Badua. That is where my father was born. Later a new char Char Bhata formed in the south and he settled there. I was born in that char."

"But 20 years ago, I sold all the properties in Char Bhata for my father's cancer treatment. Now we are living in the newly formed Char Mujib's shelter project," he added.

In 2010, Alauddin and Bilkis started a new life on the 150-acre land provided by the government in Char Nangulia. The couple started farming with a small loan of only Tk5,000. At present, their capital is about Tk5 lakh.

Like them, at least 600 families have prospered in Noakhali's Chandina Union in the last one decade.

How new land is formed
According to the report of the Ministry of Land, in 1913 the coastline of Noakhali was near Sonapur. However, in the next 100 years, it spread 55 km south to Kearingchar.

Two cross dams were built in 1957 and 1964 to protect Noakhali from the erosion of the Meghna. These dams helped sediment accumulation. As a result, new land formed out of water. Besides, huge amounts of chars started to form due to the Muhuri dam at the mouth of Feni river after 1986.


Google Satellite images show that by June 2021, these lands expanded to about 20 km southeast. Many small chars in the River Meghna and the Bay of Bengal are slowly growing which will merge with the mainland of the country.

However, according to CEGIS, the 1950 Assam earthquake played the most important role in the formation of new land in Bangladesh. As a result of the landslide in that earthquake, a huge amount of silt started coming down from the Himalayas along the rivers.

From 1943 to 1973, 43 sq-km of land was formed in the territory of Bangladesh every year.

According to the Institute of Water Modeling (IWM), the area of southern Bangladesh increased by 629 sq-km in the 200 years from 1780 to 1980. In the next 41 years, another 83,798 acres of land have been developed under the Land Reclamation Project and the Char Development and Settlement Project.

In the last 100 years, many chars including Nijhum Dwip, Nolerchar, Kearingchar on the Noakhali coast; Urir Char, Bhashan Char in the Sandwip upazila of Chattogram have emerged from the water.

In Bhasanchar, which was formed almost two decades ago, 18,347 Rohingyas have already been relocated from Cox's Bazar refugee camps. Ganguria Char, formed within 1.5 km of Bhashan Char, covers an area of 100 sq-km. According to local people, cultivation would start in Ganguria Char in four to five years.


According to people concerned, at least 10 times more land is being formed around Hatia than the land being lost due to erosion. The newly formed chars in the west of Hatia include Dhalchar, Char Mohammad Ali, Char Yunus, Char Awal, Moulvirchar, Tamruddirchar etc. Besides, seven chars have also risen in Hatia river.

In the next one decade, the area of these chars will be about 500 sq-km.

Besides, new lands are being formed in the southern part of the country including Barisal and Khulna. Experts estimate that the area of these lands will be about 33,000 sq-km.

Saidur Rahman Chowdhury, professor of the Institute of Marine Sciences and Fisheries, Chattogram University, told The Business Standard, "These lands have been formed due to some favourable environments. However, they can also disappear due to slight changes, Therefore, both hard and soft methods can be followed to save the lands."

"The first thing to do in a newly formed land is afforestation. It is a soft method. Mangrove afforestation plays an effective role in this. Besides, if cross dams and technological initiatives are taken, like in the Netherlands or Singapore, the area of land that will rise on our coast in a few years will be about 15,000 square miles," he added.

is it arable land or just fit for mangroves plantation ? Either way is good
 
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is it arable land or just fit for mangroves plantation ? Either way is good

It is arable. Extremely fertile and with access to plenty of water. Prime property for argriculture.

Because most of the clastical sediments deposited in the foreshore and bay have composition and grain sizes in the fine silt to clay spectrum.

Coarse material (sand etc) is deposited in the himalayas and at the foot of the mountain ranges ( Nepal, North India), then gravitational potential is reduced drastically because of the flat river plain. Only silt and clay is light enough to be transported by water to the river mouths in Bay of Bengal.

In fact the bedrock in Bangladesh is 10-15 km beneath the surface. Which means there are 10-15 km thick sedimentary soils deposited since Indian Plate crashed into Eurasia and made the Himalayas around 25 million years ago.





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Bangladesh gaining 20 sq-km land a year
Thanks to India, China, Nepal and Bhutan for sending us a huge volume of silt every year mostly during the monsoon time.

Some 140 million years ago, India was still a part of the supercontinent called Gondwana. The Gondwana was composed of modern Africa, Antarctica, Australia, and South America. A part of the landmass split from Madagascar and drifted north-eastward with a velocity of about 20 cm/year.

But, this Indian landmass was without Bengal landmass. The movement northward created the Himalayan mountain range and it started rising above the surface about 60 million years ago.

Rainfalls and melted snow created many flows. The river systems have been carrying about 4 billion tons of silt every year since the Himalayan mountain was formed.

The silts accumulated in the Sea and gradually taking millions of years a land rose above the Sea our forefathers named Bengal. The process will keep on continuing until the death of our Earth.

So, I expect many new lands would be added to our small country called Bangladesh.
 
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When hydroelectric dams are built upstream, it disrupts the transfer of slit
 
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It is arable. Extremely fertile and with access to plenty of water. Prime property for argriculture.

Because most of the clastical sediments deposited in the foreshore and bay have composition and grain sizes in the fine silt to clay spectrum.

Coarse material (sand etc) is deposited in the himalayas and at the foot of the mountain ranges ( Nepal, North India), then gravitational potential is reduced drastically because of the flat river plain. Only silt and clay is light enough to be transported by water to the river mouths in Bay of Bengal.

In fact the bedrock in Bangladesh is 10-15 km beneath the surface. Which means there are 10-15 km thick sedimentary soils deposited since Indian Plate crashed into Eurasia and made the Himalayas around 25 million years ago.





View attachment 829101View attachment 829102View attachment 829103View attachment 829104View attachment 829105View attachment 829106View attachment 829107View attachment 829108View attachment 829109

Amader desh ta koto shundor.

Shwapnopuree....

When hydroelectric dams are built upstream, it disrupts the transfer of slit

That is counter productive. Sanghi gadhas are really feeling it now. All of Bihar and anything upstream of Farakka is all silted up and floods every damn year. Bihar CM Nitish Kumar already called for breaking up the Farakka Dam.

Compunding the problem is the fact that govts. in Bihar and UP don't have the money to dredge the Ganga, or the other large tributaries that flow into it.

First rule of river hydraulics - never f*ck with flows of rivers.... unless you want it to get expensive....

Hasina should pay off Indian politicians to hold off breaking the Farakka until we build a second bridge over the Padma like the current one. Then they can do whatever.
 
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Bangladesh gaining 20 sq-km land a year​

Every year, the country loses 32 sq-km of land due to erosion in rivers and the sea. On the other hand, 52 sq-km of new land emerges from the water​


new_lands_in_bangladesh-01.png

The landmass of Bangladesh is increasing by 20 square kilometres annually as tonnes of silts from rivers accumulate in the Bay of Bengal, forming new land, according to a study of the Bangladesh Centre for Environment and Geographical Information Service (CEGIS).

Over the last 100 years, around 2,000 sq-km of land has been added in the country, the study finds by analysing satellite images.

According to the CEGIS, every year, Bangladesh loses 32 sq-km of land due to erosion in rivers and the sea. On the other hand, 52 sq-km of new land emerges from the water.


The result has been published in a publication of "Char Development and Settlement Project- Bridging". The project is jointly financed by the land ministry, International Fund for Agricultural Development (Ifad) and the government of the Netherlands.

Rezaul Karim, land settlement officer of Ifad, said, "Bangladesh has regained 1,000 sq-km of land lost in the last 100 years due to river erosion. Of this, 93% of land is on the coast and the remaining 7% is on various rivers. The total area of the new land is about 2,000 sq-km."

However, Mohammad Shahidul Islam, director of Remote Sensing Devices, CEGIS, told The Business Standard that the rate of new land formation has decreased in recent years.

"The government has been working on the newly formed chars in the coast of Noakhali since 1973. However, the amount of sediments flowing through the Brahmaputra, Meghna and Padma rivers has decreased recently. At the same time the newly formed chars are being lost for various reasons. River erosion has also increased."

According to the Ministry of Land, the Noakhali coast of the Bay of Bengal has extended 55 km south in the 100 years from 1913 to 2013. Two cross dams built in 1957 and 1964 to protect Noakhali from the erosion of the River Meghna facilitated the formation of new chars in the surrounding areas.

Since 1980, land development work has been carried out in the newly formed chars which have now become green agricultural land.

From 1994 to June 2021, the government has allotted 83,798 acres of khas land (government-owned land) to 36,281 landless families. A target has been set to provide land to another 5,719 landless families by June 2022.


Nurul Islam, a resident of Noakhali's Char Mujib Asrayan project, said, "My grandfather was a resident of Sonapur in Noakhali. About 90 years ago, he settled in Char Badua. That is where my father was born. Later a new char Char Bhata formed in the south and he settled there. I was born in that char."

"But 20 years ago, I sold all the properties in Char Bhata for my father's cancer treatment. Now we are living in the newly formed Char Mujib's shelter project," he added.

In 2010, Alauddin and Bilkis started a new life on the 150-acre land provided by the government in Char Nangulia. The couple started farming with a small loan of only Tk5,000. At present, their capital is about Tk5 lakh.

Like them, at least 600 families have prospered in Noakhali's Chandina Union in the last one decade.

How new land is formed
According to the report of the Ministry of Land, in 1913 the coastline of Noakhali was near Sonapur. However, in the next 100 years, it spread 55 km south to Kearingchar.

Two cross dams were built in 1957 and 1964 to protect Noakhali from the erosion of the Meghna. These dams helped sediment accumulation. As a result, new land formed out of water. Besides, huge amounts of chars started to form due to the Muhuri dam at the mouth of Feni river after 1986.


Google Satellite images show that by June 2021, these lands expanded to about 20 km southeast. Many small chars in the River Meghna and the Bay of Bengal are slowly growing which will merge with the mainland of the country.

However, according to CEGIS, the 1950 Assam earthquake played the most important role in the formation of new land in Bangladesh. As a result of the landslide in that earthquake, a huge amount of silt started coming down from the Himalayas along the rivers.

From 1943 to 1973, 43 sq-km of land was formed in the territory of Bangladesh every year.

According to the Institute of Water Modeling (IWM), the area of southern Bangladesh increased by 629 sq-km in the 200 years from 1780 to 1980. In the next 41 years, another 83,798 acres of land have been developed under the Land Reclamation Project and the Char Development and Settlement Project.

In the last 100 years, many chars including Nijhum Dwip, Nolerchar, Kearingchar on the Noakhali coast; Urir Char, Bhashan Char in the Sandwip upazila of Chattogram have emerged from the water.

In Bhasanchar, which was formed almost two decades ago, 18,347 Rohingyas have already been relocated from Cox's Bazar refugee camps. Ganguria Char, formed within 1.5 km of Bhashan Char, covers an area of 100 sq-km. According to local people, cultivation would start in Ganguria Char in four to five years.


According to people concerned, at least 10 times more land is being formed around Hatia than the land being lost due to erosion. The newly formed chars in the west of Hatia include Dhalchar, Char Mohammad Ali, Char Yunus, Char Awal, Moulvirchar, Tamruddirchar etc. Besides, seven chars have also risen in Hatia river.

In the next one decade, the area of these chars will be about 500 sq-km.

Besides, new lands are being formed in the southern part of the country including Barisal and Khulna. Experts estimate that the area of these lands will be about 33,000 sq-km.

Saidur Rahman Chowdhury, professor of the Institute of Marine Sciences and Fisheries, Chattogram University, told The Business Standard, "These lands have been formed due to some favourable environments. However, they can also disappear due to slight changes, Therefore, both hard and soft methods can be followed to save the lands."

"The first thing to do in a newly formed land is afforestation. It is a soft method. Mangrove afforestation plays an effective role in this. Besides, if cross dams and technological initiatives are taken, like in the Netherlands or Singapore, the area of land that will rise on our coast in a few years will be about 15,000 square miles," he added.


They should name the chars after the prevalent activity in those areas.

- Jor-dokholer char
- Dandar Bari char
- Matha fatafatir char
 
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When hydroelectric dams are built upstream, it disrupts the transfer of slit
To maintain hydroelectric dam function properly, a major riverbed dredging needs to be done every 50-100 years to remove the siltation upstream. So the end effect is more or less the same. If India or any other country doesn't want to 'kill' their rivers they have no option but to flush all those silt towards Bangladesh, dam or not. And those silt is going to diposit on the Meghna estuary and giving rise to new islands.
 
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It is arable. Extremely fertile and with access to plenty of water. Prime property for argriculture.

Because most of the clastical sediments deposited in the foreshore and bay have composition and grain sizes in the fine silt to clay spectrum.

Coarse material (sand etc) is deposited in the himalayas and at the foot of the mountain ranges ( Nepal, North India), then gravitational potential is reduced drastically because of the flat river plain. Only silt and clay is light enough to be transported by water to the river mouths in Bay of Bengal.

In fact the bedrock in Bangladesh is 10-15 km beneath the surface. Which means there are 10-15 km thick sedimentary soils deposited since Indian Plate crashed into Eurasia and made the Himalayas around 25 million years ago.





View attachment 829101View attachment 829102View attachment 829103View attachment 829104View attachment 829105View attachment 829106View attachment 829107View attachment 829108View attachment 829109
very interesting ,
researchers are developing a genetically modified breed of rice crop that can grow under very saline conditions.
 
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When hydroelectric dams are built upstream, it disrupts the transfer of slit
A barrage/ dam certainly slows the flowing of silt downwards. But, it happens mostly in the dry season anyway because the quantity of water is small and the water flow is slow.

When the gates are open during the rainy season, most of the silts come down with the the water flow and finally accumulate down stream in or near the coasts of BoB.

BD gets about 2 billion tons of silt every year and the thread opened by @Homo Sapiens says that about 20 sq. km. of new land is surfacing above the water every year.

I think, this silt accumulating process is common in the north of the BoB that we cannot see from the shore. However, during the few times I rode planes from Chittagong Airport, I could see many shades of islands below the water surface.

Some of these shades have already come up above the sea level and many more will come up soon. So, I think this yearly 20 sq. km. new islands will increase in the near future.
 
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