Kanyakumari Beach: Best place to visit where Bay of Bengal and Arabian Sea meet and form Indian Ocean - See traveler reviews, candid photos, and . Meeting Point of The Arabian Sea, The Bay of Bengal and The Indian Ocean - Kanyakumari. Kanyakumari or Kanniyakumari, formerly known. Kanyakumari Beach is the meeting point of Bay of Bengal, Indian Ocean and Arabian sea. Though there is no visible sign or colour of the sea water to.
However, a clear and logical approach considers its border as lying with the Atlantic Ocean, and along the Cape Agulhas at the southern tip of Africa, to the south from the meridian up to the waters of Antarctica. It is through this route that the petroleum and by-products from the Persian Gulf and Indonesia are carried to the other parts of the world. It is estimated that one third of the total cargo in the world marine trade ship through its waters.
During the Indian Ocean Dipole, the waters of the eastern half will cool down more than the waters of the western half, causing strong winds from east to west, at the equator.
Arabian Sea The Arabian Sea was originated 50 million years ago when the Indian subcontinent collided with the continent of Asia. Most parts of the sea are above 9, feet deep.
Difference Between Indian Ocean And Arabian Sea
It is interesting to note that the deep water levels and the seabeds of the Arabian Sea are very similar to the land formations we see around. The medieval Arabs called it the Sea of India.
Water transport along the Arabian Sea started prior to the Roman Empire, but it gained importance in the ninth century, when the Arabs and Persians began using it to connect the neighbouring communities. Realizing the way how the wind blows on the sea, they navigated to the southern parts of Arabia, East Africa and the ports of Red Sea.
Meeting Point of The Arabian Sea, The Bay of Bengal and Th… | Flickr
The Arabian Peninsula and the west coast of the Indian subcontinent are blessed with large deposits of petroleum and natural gas. One such deposit on the continental shelf off the west coast near Mumbai in India, are intensively being exploited, now.
The region, which contains many fish remains, is known as a fish cemetery. Below this, deposits consist of the calcareous tests shells of Globigerina a genus of protozoans belonging to the Foraminifera orderwhile basins below 13, feet 4, metres are covered by red clay. Sediment thickness decreases from 8, feet 2, metres in the north to about 1, feet metres in the south of the Arabian Basin.
Borders of the oceans - Wikipedia
Climate and hydrology The Arabian Sea has a monsoon climate. Because evaporation exceeds the combined precipitation and riverine input, the sea exhibits a net water loss annually. Pronounced upwelling of deeper waters occurs along the Somali and Arabian coasts in summer. The Somali Current weakens and reverses direction during the northeast winter monsoon.
Meeting The Bay of Bengal, the Arabian Sea, and the Indian Ocean - Kanyakumari Beach
Of the five water masses that have been distinguished in the upper 3, feet metres of the northern Indian Ocean, three have been identified as originating in the Red Sea, the Persian Gulf, and the Arabian Sea, respectively. The paths of flow of these water masses are to the south and east. Economic aspects Resources Petroleum and natural-gas deposits have been discovered in the Arabian Sea on the continental shelf off the coast of India to the west and northwest of Mumbai Bombay and have been intensively exploited.
High levels of inorganic nutrients, such as phosphate concentrate, which produce a rich fish life, have been observed in the western Arabian Sea and off the southeastern coast of the Arabian Peninsula.
Occurring in the euphotic zone zone of light, which is found in the upper feet [ metres] of the seathis fertilizing effect undoubtedly is attributable in part to coastal upwelling, which circulates settled nutrients from the seafloor. A periodic occurrence in the Arabian Sea, however, is the mass mortality of fish.
This phenomenon is attributed to a subsurface layer of water of tropical origin that is poor in oxygen but rich in phosphate.
Under certain circumstances this layer is brought to the surface by strong upwelling, resulting in the death of fish from lack of oxygen.
Extensive small-scale fishing is carried on in the Arabian Sea, particularly off the east coasts of Africa, the Arabian Peninsula, and west coast of the Indian subcontinent. These operations employ dugout and outrigger canoes, dhows, and a variety of other small craft, as well as mechanized trawlers and purse seiners.
Commercial fishing also is undertaken by larger vessels. Persian Gulf shipping largely consists of tankers, some of immense capacity, that transit the Arabian Sea en route to destinations in East Asia, Europe, and North and South America.
There are a number of ports serving the countries bordering the sea.