Why is the Red Sea called the sea

Red sea(1)

Information about Red Sea

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Red Sea Global

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It is a narrow body of water in the Indian Ocean, located between the continents of Africa and Asia. The Red Sea connects to the ocean from the south, through the Bab al-Mandeb Strait and the Gulf of Aden. To its north lies the Sinai Peninsula, the Gulf of Aqaba, and the Gulf of Suez (leading to the Suez Canal). It is bordered by the Red Sea Fault, which is part of the

larger Rift Valley.

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Red Sea Surface Area

The Red Sea has a surface area of 438,000 km2, [1] and is approximately 2,250 km long, with a maximum width of 355 km. The average depth of water in the Red Sea is 490 meters, and in Gore Swakin, the maximum depth of water is 3040 meters.[2]

The Red Sea also has extensive shallow shelves, known for marine life and coral. The Red Sea is home to more than 1,000 invertebrate species and 200 hard and soft coral species. It is the world's most tropical sea and has been designated an ecological zone under the Billboard Global Plan 200.

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Location

The Red Sea is surrounded by Jordan, Palestine, Egypt to the north, Saudi Arabia and the Republic of Yemen to the east, and Egypt, Sudan and Eritrea to the west. It operates a narrow, long crater. Its length is 1932 km and its maximum width is 306 km and covers an area of 450 thousand km2 and the volume of a hundred at least 251 thousand km³ and its average depth is 558 m, and the maximum is 2635 m، Sea coasts are sandy and rocky, often surrounded by coral reefs. It ends north in the Gulf of Aqaba and Suez and the first has a length of 180 km and a width of 15-28 km, while its depth does not exceed 1828 m. The length of the Gulf of Suez is 325 km and its width is 15 to 46 km and its depth does not exceed 80 m. The Gulf is linked to the Suez Canal, which connects the Red and Mediterranean seas. At sea are the main islands of the Suakin archipelago, the Knights and Dahlak.

The southernmost strait of Bab al-Mandab, which connects it with the Indian Ocean, is not deep, but at least 140 m deep, its width is about 27.7 km and the origin of the sea basin is due to a group Complicated by the fissures and fractures that separated Asia from Africa within the Great Syrian-African Rift, and as a result the sides of the sea consist of steep, and sometimes even standing, gradient foothills, Throwing cracks or steps in them reach 500-700 m and sometimes exceed 1,500 m, especially in the south. The rift is also severe in the Gulf of Aqaba. Sediments in the seafloor, the most biogenic, originate from coral reefs and the breaking of limescale by adding continental dust particles.[3]

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Extension

At the centre of the sea is a long, narrow, steep creek that runs deep between 2000 and 2500 m and at the centre of which are the greatest depths of the sea that diminish as we head south. The sea threshold is increasingly displayed from north to south, 10-20km wide in the north and 35-40km in the south and over 100km at the Knights Islands.

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Label

The Arabs called the Red Sea the Sea of Nuts.

Date

The ancient Egyptians to the land of Punt on the coast of the Red Sea.

The commercial and population centers on the Red Sea coast associated with the spice trade, as described in Priplus of the Red Sea.

The Red Sea was first explored by the ancient Egyptians because they tried to establish trade routes to Puntland. One of these campaigns took place around 2500 BC.M, and the other about 1500 BC.M (by hutchingsot). Both flights were along the Red Sea.[4]

In the sixth century BC, Darius I of Persia sent reconnaissance missions to the Red Sea, improving and expanding mobility by locating many dangerous rocks and currents. A canal was built between the Nile and the northern tip of the Red Sea at Suez.

Alexander the Great was sent in the late fourth century.Greek sea voyages down the Red Sea towards the Indian Ocean. Greek sailors continued to explore and collect data from the Red Sea. Historian Agatharchides collected information about the sea in the second century BC.M. The guide 'Pereplus of the Irish Sea' written by the 1st-century Greeks shows a detailed description of Red Sea ports and sea routes.[5] It also describes how Hubalos first discovered the direct route from the Red Sea to India.

The Red Sea was a favorite of Roman trade with India beginning with the reign of Emperor Augustus, when the Roman Empire controlled the Mediterranean, Egypt, and the northern Red Sea. The route was used by the former states but increased in volume of traffic under the Romans. Chinese goods were supplied from Indian ports to the Roman world. The connection between Rome and China is based on the Red Sea, but the route was broken by the Axumite Empire in almost the third century AD.[6]

During the Middle Ages, the Red Sea was an important part of the spice route. In 1513, Alfonso de Albuquerque imposed a blockade on Aden to try to secure that route to Portugal.[7] But he had to retreat. The Red Sea flew into Bab al-Mandab, and the European fleet was the first to sail in these waters.

In 1798, France ordered General Bonaparte to invade Egypt and take control of the Red Sea. Although he failed in his mission, the engineer Jean-Baptiste Lauper, who took part in this mission, reinstated the channel that was conceived during the reign of the pharaohs. Many canals were built in ancient times from the Nile to the Red Sea along or near the line of the present Sweet Water Canal, but they did not last long. The Suez Canal was opened in November 1869. At that time the British, Italians and French shared trading posts. These centres were gradually dismantled following the First World War. After the Second World War, American and Soviet influence dominated the volume of oil tanker traffic. However, the Six-Day War culminated in the closure of the Suez Canal between 1967 and 1975. Today, despite patrols by major navies in the waters of the Red Sea and the Suez Canal, it has not discarded its sovereignty over the Green Route, which is thought to be less

vulnerable to the line

Why is the Red Sea famous for

Was the Red Sea in Egypt

Surface water temperature

They remain relatively constant throughout the year between 21 and 25 m. Visibility is good and reaches 200 m but the sea is known for its strong winds and deceptive weather conditions. The Red Sea is the distance of Africa from the Arabian Peninsula in a movement that began 30 million years ago and continues. The Red Sea has volcanic features that appear in its deep parts and it is believed that the Red Sea will turn into an ocean over time - according to Tozo Wilson's theory.

The water is sky green, with the amount of oxygen dissolved in it reaching 2-3pc and its lowest values located 300-500m deep.

It is noticeable that the depth of the oxygen microelement increases as we head north, and the amount of oxygen in the north is greater than in the south. This difference is due to the increasing effectiveness of vertical north-fusion water mixing. And he recently discovered the presence of high-temperature mineral water in the deep central part of the sea with water reaching 44-72C، This water is at least 200-300m thick but very little oxygen in it. The composition of salts found in the water here differs from typical seawater, and its composition is reminiscent of brines extracted from deep mines and boreholes. The quality of the rock deposits in the bottom suggests they may have been formed at the expense of water deposits in the higher aquifers, with iron, zinc and copper deposits abounding. Some scientists believe that complex underground chemical processes take place in the lower sea and recall those that were taking place in bygone geological times and later led to the emergence of various mineral deposits around the globe.

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Red Sea map

Climate

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A view of the Nile River and Red Sea accompanied by a dust storm.[8]

The location of the Red Sea between the Arabian Peninsula and Africa determines its climatic characteristics, with winter atmospheric pressure rising over northern Africa, while atmospheric frontal activity intensifies over [[the Mediterranean basin، The north-east winds in the northern section of the sea dominate, while the south section is dominated by winds from the south-east. In the summer, a high pressure arm of an Assur pressure center stretches over northern Africa against low pressure in southern Asia and the Arabian Peninsula. The pressures over the Mediterranean stay higher, so over the whole Red Sea are dominated by northwesterly winds of origin, and so monsoon control is seen in the southern part of the sea, They are south-eastern in origin winter and north-western in summer. In the north, winds from the north dominate.

The heat is always high and the seasons are clear in the north, with the average January heat of 24C at Bab al-Mandab and in the north at 15.5C، In July, it's a 32.5 in the south and 27.5 in the north. Rains are few and even rare, equivalent to 200-300mm per year near the Bab el Mandeb Strait and 30-50mm in the north, which is winter rain. Given the lack of sea-thriving fresh water and the large evaporation of 2,200-3,000mm per year، The sea loses large amounts of its water, which is compensated by the sea-origin waters coming through Bab al-Mandab from the Indian Ocean and the Gulf of Aden, which supplies about 10.1 thousand km3 of water per year، It receives 9.1 thousand km3. This exchange is equivalent to 0.25 water exchanges between the Mediterranean and the Atlantic.