Facts about Arabian Sea
According to geologists, during this time period Asia collided with the subcontinent of India, forming the Arabian Sea and its unique underground ridges.
The Maldive Ridge, along with other sea floor formations in the Arabian Sea, are hypothesized to be the result of seismic activity roughly 50 million years ago.
Currently, plans are being considered that would protect the delicate wildlife of the Arabian Sea, particularly the turtle and coral populations.
Smaller political areas also fringe the Arabian Sea, including Socotra off the coast of Yemen, the Khuriyya Muriyya islands and the Lakshadweep islands.
A rich and varied aquatic habitat is supported in the Arabian Sea by high levels of inorganic nutrients.
The Arabian Sea, due its seasonal weather fluctuations, offers excellent examples of biological adaptation to environment.
The Arabian is augmented by water flowing down the Indus and Narmada rivers, which are the principal means of access to the Arabian Sea.
The Arabian Sea contributes to a monsoon climate in the surrounding region by providing the water necessary for the wet storms.
The Arabian Sea reached a historical heyday in the ninth century C.E., when Arab and Persian seamen began to use the sea as a means of communication with neighboring communities.
The Arabian Sea is located in the northwestern part of the Indian Ocean, situated between the Arabian Peninsula and the Indian subcontinent.
The Arabian Sea is distinguished by its remarkably deep water level that is often maintained close to land masses.
Water transport along the Arabian Sea had been established prior to Roman times, and only grew as time went on.
The Arabian Sea is also notable for its large population of pelagic fish, or those fish which live near the surface of the water.
The Arabian Sea is considered to be one of the world's busiest shipping lanes, primarily due to its proximity to the Red Sea and the Persian Gulf.
The Arabian Sea is connected to surrounding bodies of water by a series of gulfs and straits that provide a steady avenue into the sea.
The Arabian Sea floor, while far below the surface, exhibits a startling complexity akin to standard land formations.
Perhaps most notable among the submarine features is the Maldive Ridge, which runs along the ocean floor from the Arabian Sea into the Indian Ocean.
The Arabian Sea became a major player in the international shipping scene with the construction of the Suez Canal in 1869.
Most of the ships that use the Arabian Sea for transportation purposes are large tankers, whose travels often conclude in East Asia, Europe or The Americas.
After the initial collision of the two land masses, the Arabian Sea has been shaped by a variety of highly influential factors, including erosion from water currents.
Written documentation exists that gave detailed instructions for sailing on the Arabian Sea, and the routes that had to be followed to arrive successfully at a desired location.
Occasionally in the Arabian Sea the fish population falls victim to a particularly strong upsurge of phosphate.