|Bay of Bengal|
|Primary sources||Indian Ocean|
|Basin countries||India, Bangladesh, Myanmar (Burma), Thailand, Indonesia, Sri Lanka|
|Max length||2,090 km; c.1,300 mi|
|Max width||1,610 km; 1,000 mi|
|Surface area||2,172,000 km¬≤|
|Average depth||2,600 m ; 8,500 feet|
|Max depth||4,694 m ; 15,400 feet|
The Bay of Bengal (Bangla: ŗ¶¨ŗ¶ôŗßćŗ¶óŗßčŗ¶™ŗ¶łŗ¶ĺŗ¶óŗ¶į)IPA:ňąb…íŇč…°opo É…Ďňźňągo…Ĺ), the largest bay of the world, forms the northeastern part of the Indian Ocean. It resembles a triangle in shape, and is bordered by Bangladesh and the Indian state of West Bengal to the north (where the name comes from), India and Sri Lanka to the west and Burma (Myanmar) and the Andaman and Nicobar Islands to the east.
The Bay of Bengal occupies an area of 2,172,000 km¬≤. A number of large rivers ‚Äď Padma (distributary of Ganges), Meghna (distributary of Brahmaputra), Jamuna (branch of Brahmaputra, Ayeyarwady, Godavari, Mahanadi, Krishna and Kaveri) ‚Äď flow into the Bay of Bengal. Among the important ports are Cuddalore, Chennai, Kakinada, Tuticorin, Machilipatnam, Vishakapatnam, Paradip, Kolkata, Mongla, Chittagong and Yangon.
On the East. A line running from Cape Negrais (16¬į03'N) in Burma through the larger islands of the Andaman group, in such a way that all the narrow waters between the islands lie to the Eastward of the line and are excluded from the Bay of Bengal, as far as a point in Little Andaman Island in latitude 10¬į48'N, longitude 92¬į24'E and thence along the Southwest limit of the Burma Sea [A line running from Oedjong Raja ( ) in Sumatra to Poeloe Bras (Breu√ęh) and on through the Western Islands of the Nicobar Group to Sandy Point in Little Andaman Island, in such a way that all the narrow waters appertain to the Burma Sea].
In the 10th century the explosion of Indianized kingdoms, led by the Chola Empire, resulted in the Bay of Bengal being known as the Chola Lake. It later came to be known as Bangal ki Khadi in Hindi after the region of Bengal. Bengal comes from the Sanskrit Banga or Vanga which refers to the delta waters of the river Ganga.
Many major rivers of India and Bangladesh flow west to east into the Bay of Bengal: in the north, the Ganges River (or Ganga), Meghna River and Brahmaputra River rivers, and in the south Mahanadi River through the Mahanadi River Delta, Godavari River, Krishna River, Irrawaddy and Kaveri River (sometimes written as Cauvery) rivers. The shortest classified river which drains into the Bay of Bengal is Cooum River at 64 km. Brahmaputra is the 28th longest River in the World (2,948 km or 1,832 mi), and it discharges into the 'Bay of Bengal' and travels through India, P.R. China, Nepal, Bangladesh and Bhutan. The Sundarbans mangrove forest is formed at the delta of the Ganga, Brahmaputra and Meghna rivers on the Bay of Bengal. The Ayeyarwady River of Myanmar also flows into the bay.
Major Bangladesh ports on the bay include Chittagong and Mongla. Major Indian ports on the bay include Krishnapatnam, Chennai (formerly Madras), Vishakhapatnam, Kolkata (formerly Calcutta), and Pondicherry. Yangon, the largest city and former capital of Myanmar is also an important port in the bay.
The islands in the bay are very numerous, including the Andaman, Nicobar and Mergui groups. The group of islands, Cheduba and others, in the north-east, off the Burmese coast, are remarkable for a chain of mud volcanoes, which are occasionally active. Great Andaman is the main archipelago or island group of the Andaman Islands, whereas Ritchie's Archipelago consists of smaller islands. Only 37 of the 572 islands and islets of the Andaman and Nicobar Islands are inhabited, or 6.5%.
The lithosphere of the earth is broken up into what are called tectonic plates. Underneath the Bay of Bengal is the Indian Plate which is part of the great Indo-Australian Plate and is slowly moving north east. This plate meets the Burma Microplate at the Sunda Trench. The Nicobar Islands, and the Andaman Islands are part of the Burma Microplate. The India Plate subducts beneath the Burma Plate at the Sunda Trench or Java Trench. Here, the pressure of the two plates on each other increase pressure and temperature resulting in the formation of volcanoes such as the volcanoes in Myanmar, and a volcanic arc called the Sunda Arc. Sumatra-Andaman earthquake and Asian Tsunami was a result of the pressure at this zone causing a submarine earthquake which then resulted in a huge Tsunamai.
A zone 50 m wide extending from the island of Ceylon and the Coromandel coast to the head of the bay, and thence southwards through a strip embracing the Andaman and Nicobar islands, is bounded by the 100 fathom line of sea bottom; some 50 m. beyond this lies the Soo-fathom limit. Opposite the mouth of the Ganges, however, the intervals between these depths are very much extended by deltaic influence.
Swatch of No Ground is a 14 km-wide deep sea canyon of the Bay of Bengal. The deepest recorded area of this valley is about 1340 m.
The Bay of Bengal is full of biological diversity, diverging amongst coral reefs, estuaries, fish spawning and nursery areas, and mangroves. The Bay of Bengal is one of the World's 64 largest marine ecosystems.
Kerilia jerdonii is a sea snake of the Bay of Bengal. Glory of Bengal Cone (Conus bengalensis) is just one of the seashells which can be photographed along beaches of the Bay of Bengal. An endangered species, the Olive Ridley sea turtle can survive because of the nesting grounds made available at the Gahirmatha Marine Wildlife Sanctuary, Gahirmatha Beach, Orissa, India. Marlin, barracuda, skipjack tuna, (Katsuwonus pelamis), yellowfin tuna, Indo-Pacific humpbacked dolphin (Sousa chinensis) , and Bryde's whale (Balaenoptera edeni) are a few of the marine animals. Bay of Bengal Hogfish (Bodianus neilli) is a type of Wrass which live in turbid lagoon reefs or shallow coastal reefs. Schools of dolphins can be seen, whether they are the bottle nose dolphin (Tursiops truncatus), Pantropical spotted dolphin (Stenella attenuata) or the spinner dolphin (stenella longirostris) . Tuna and dolphins are usually residing in the same waters. In shallower and warmer coastal waters the Irrawaddy Dolphins (Orcaella brevirostris) can be found.
The Great Nicobar Biosphere Reserve proides sanctuary to many animals some of which include the saltwater crocodile (Crocodylus porosus) , giant Leatherback Sea Turtle (Dermochelys coriacea) , and Malayan box turtle (Cuora amboinensis kamaroma) to name a few.
Coastal regions bordering the Bay of Bengal are rich in minerals. Sri Lanka, Serendib, or Ratna ‚Äď Dweepa which means Gem Island. Amethyst, beryl, ruby, sapphire, topaz, and garnet are just some of the gems of Sri Lanka. Garnet and other precious gems are also found in abundance in the Indian states of Orissa and Andhra Pradesh.
From January to October, the current is northward flowing, and the clockwise circulation pattern is called the "East Indian Current." The Bay of Bengal monsoon moves in a northwest direction striking the Nicobar Islands, and the Andaman Islands first end of May, then the North Eastern Coast of India by end of June.
The remainder of the year, the counterclockwise current is southwestward flowing, and the circulation pattern is called the East Indian Winter Jet. September and December see very active weather, season varsha (or monsoon), in the Bay of Bengal producing severe Cyclones which affect Eastern India. Several efforts have been initiated to cope with Storm surge.
A tropical storm with rotating winds blowing at speeds of 74 miles (119 kilometres) per hour are called cyclones when they originate over the Bay of Bengal; they are hurricanes in the Atlantic. Between 100,000 and 500,000 residents of East Pakistan (Bangladesh) were killed because of the 1970 Bhola cyclone.
One of the first trading ventures along the Bay of Bengal was The Company of Merchants of London Trading into the East Indies more commonly referred to as British East India Company. Gopalpur was one of their main trading centers. Other trading companies along the Bay of Bengal shorelines were English East India Company and French East India Company.
BIMSTEC Bay of Bengal Initiative for MultiSectoral Technical and Economic Cooperation (BIMSTEC) supports free trade internationally around the Bay of Bengal between Bangladesh, Bhutan, India, Myanmar, Nepal, Sri Lanka, and Thailand.
The Sethusamudram Shipping Canal Project is a new venture proposed which would create a channel for a shipping route to link the Gulf of Mannar with the Bay of Bengal. This would connect India east to west without the necessity of going around Sri Lanka.
Thoni and catamaran fishing boats of fishing villages thrive along the Bay of Bengal shorelines. Fishermen can catch between 26-44 species of marine fish. In one year, the average catch is 2 million tons of fish from the Bay of Bengal alone.
Being Bangladesh's only sea boundary, the Bay of Bengal has a significant role in the country. Bangladesh navy performs annual exercise in the bay  and exercise with international navy is also frequent. Bangladesh navy's last joint exercise with the US navy held on early 2009.
Rumor exists that China has a naval base in Myanmar's Coco island of Bay of Bengal. 
The Bay of Bengal is strategically crucial for India because of the presence of outlying islands, namely Andaman islands and Nicobar islands and several major ports such as Kolkata, Chennai, Vizag, and Tuticorin along its coast with the Bay of Bengal. Much of the naval operations of the 1971 Indo-Pakistani War took place in the Bay of Bengal.
The growing influence of China, due to support provided by Myanmar, has created geo-political implications for India. India has held several major naval exercises with friendly countries, especially United States, to counter increasing Chinese presence in the Indian Ocean. The largest ever wargame in Bay of Bengal, known as Malabar 2007, was held in 2007 and naval warships from India, US, Singapore, Japan and Australia took part in it. This exercise was widely viewed as "strategic encirclement of China". India has forged naval cooperation agreements with Malaysia, Thailand and Indonesia to increase its strategic reach in the region. India also established Far Eastern Naval Command off Port Blair to increase surveillance in the adjoining Andaman Sea.
The potential of natural gas exploitation also makes the Bay of Bengal important for India, Bangladesh and Myanmar. Disputes over rights of some oil and gas blocks have caused brief diplomatic spats between India and Bangladesh.
The Asian brown cloud, a layer of air pollution that covers much of South Asia and the Indian Ocean every year between January and March, and possibly also during earlier and later months, hangs over the Bay of Bengal. It is considered to be a combination of vehicle exhaust, smoke from cooking fires, and industrial discharges.
Northern Circars occupied the western coast of the Bay of Bengal and is now considered to be India's Madras state. The Kakatiya dynasty reached the western coastline of the Bay of Bengal between the Godavari and the Krishna rivers. Kushanas about the middle of the 1st century AD invaded northern India perhaps extending as far as the Bay of Bengal. Chola dynasty (9th century to 12th century) when ruled by Rajaraja Chola I occupied the western coastline of the Bay of Bengal circa AD 1014 Chandragupta Maurya extended the Maurya Dynasty across Northern India to the Bay of Bengal. Hajipur was a stronghold of Portuguese Pirates. In the 1500s the Portuguese built trading posts in the North of the Bay of Bengal at Chittagong (Porto Grande) and Satgaon (Porto Pequeno).
Cellular Jail or "Black Waters" built in 1896 on Ross Island, a part of the Andaman Island Chain. As early as 1858 this island was used as a British penal colony for political prisoners facing life imprisonment.
Maritime archaeology or marine archaeology is the study of material remains of ancient peoples. A specialized branch, Archaeology of shipwrecks studies the salvaged artifacts of ancient ships. Stone anchors, amphorae shards, elephant tusks, hippopotamus teeth, ceramic pottery, a rare wood mast and lead ingots are examples which may survive the test of time for archaeologists to study and place the salvaged findings into a time line of history. Coral reefs, tsuanamis, cyclones, mangrove swamps, battles and a criss cross of sea routes in a high trading area combined with pirating have all contributed to shipwrecks in the Bay of Bengal.
BAY OF BENGAL, a portion of the Indian Ocean, resembling a triangle in shape, lying between India and Burma. A zone 50 m. wide extending from the island of Ceylon and the Coromandel coast to the head of the bay, and thence southwards through a strip embracing the Andaman and Nicobar islands, is bounded by the ioo fathom line of sea bottom; some 50 m. beyond this lies the Soo-fathom limit. Opposite the mouth of the Ganges, however, the intervals between these depths are very much extended by deltaic influence. The bay receives many large rivers, of which the most important are the Ganges and Brahmaputra on the north, the Irrawaddy on the east, and the Mahanadi, Godavari, Kistna and Cauvery on the west. On the west coast it has no harbours, Madras having a mere open roadstead, but on the east there are many good ports, such as Akyab, Moulmein, Rangoon and Tavoy river. The islands in the bay are very numerous, including the Andaman, Nicobar and Mergui groups. The group of islands, Cheduba and others, in the north-east, off the Burmese coast, are remarkable for a chain of mud volcanoes, which are occasionally active. Thus in December 1906 a new island of mud was thrown up, and measured 3 07 by 217 yds.
Bay of Bengal
The Bay of Bengal is a bay. It is in the northeastern part of the Indian Ocean. The bay is also east of the Malay Peninsula and west of India. It looks like a triangle. It is called the "Bay of Bengal", because to the north are the Indian state of West Bengal and the country of Bangladesh.