What is the Bengal fan?
At first, you may visit the head that Bengal means Bengal and fan money fan. The meaning of the Bengali fan. Then you have been totally wrong. Then let's know about it. Bengal fan is the landroom of the sea. Meaning of the land or land that is located in the sea. A landmark in the sea is called Bengal Fan. The formation or sub-formation of Bengal Fan We know that Bengal fan is a land beneath the sea. Originally Bengal fan is formed by riverbed poly. It was formed in the sea flowing through the river. And the polyles are just the structure that the polygs are made of the veins of the veins together. As a result, large-shaped hills are made like sea. In Bangladesh, Bengal fan has a lot of ocean bay in the world. But Bengal fan is only located in Bangladesh. There is no other sea or ocean in the world. Its position in the Bay of Bengal. The country of riverine is our Bangladesh. There are more than 405 rivers, including branch branches in Bangladesh. The main rivers are Padma, Meghna, Jamuna, Brahmaputra. Only water will be seen if the length of the river is calculated. There are poly spleen. Think of a bar so many of these rivers of the river goes. The question may come in mind. Yes there is yes. If you are questioning where the river flows flowing, you must say in the sea. Yes, it's right, then where does the poly go? Surely tell the sea. Yes, Palio goes with water, but the silt is not flowing, but in less speed, it flows down. Now there is no way to go from the sea and somewhere. Is there? Therefore, it is made like a monotonous mountain to gather in the sea. That is "Bengal Fan".
Bengal Fan or Ganges Fan, Ganges Peninsula:
Bengal Fan, Ganges Fan, Gangetic Peninsula, the names of the Bengal Peninsula refers to all the same objects. Which is known as different. We can also tell these deep sea canyons and yes the world's deepest tyranny sea canyon. The length of the ranges of the length of the canyon is 3000 km (1900 miles) and width 1430 km (890 miles). Depth is 16.5 km (10.3 miles), three plates have played a role behind this sector. These are the Tibetan Plates, Indian Plates, Eurasian Plateate. This sector is created by three plates as a result of the journalist clash. The Tibetan Plate hit the Eurasian and Indian plates by hitting the Himalayas Mountains and erosion through the erosion. Turbidi is the currents and these streams are carrying silvery through just one series or trend of submarine canyon. That is in the silt of 30 ° latitude of the Bay of Bengal. The gentleman has confirmed that the oldest poly of Bengal fan is in the early side of the Miaosin era. So I can understand how old these polyles are.
Bengal Fan and Himalayas Relationships:
Bengal Fan, Gangetic Peninsula, Ganges fan with all the Himalayas with all the Himalayas. I can identify the Himalayas through the mineral and underground chemical features of the canyon. As the result, the Himalayan was just 20 million years ago, there was only one mountain in the mountain that today a huge height of a huge height. Bengal fan detection Bengal fan himself did not identify itself. The hand behind it In the 60s, two sea researchers Bruce C. Hijen and Marie Thier conducted a survey called Bathimetric. By bathimetric they can see the sector shape. In 1968, Joseph Kura and David Moore gave the names of these two geologic surveys by a monastery of Bengal fan. Which we are coming now and I have come to know. The Bengal Fan helps to maintain balance between plants and organisms of the sea.
The last word:
"Bengal fan" is an important object in Bangladesh although it is located in the deep sea. There are various types of marine animals in the center of this sector. The sector is beside the "Swaches of No Ground". The depth of the Bay of Bengal is located. Swaches of No Ground is a place that is observed by very low land.
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