The Red Sea is an inlet of the Indian Ocean between Africa and Asia. The connection to the ocean is in the south through the Bab el Mandeb sound and the Gulf of Aden. In the north are the Sinai Peninsula the Gulf of Aqaba) and the Gulf of Suez (leading to the Suez Canal). The Red Sea is a Global 200 ecoregion. Occupying a part of the Great Rift Valley the Red Sea has a ascend area of about 174,000 square miles (450,000 km²): being roughly 1,200 miles (1,900 km) long and at its widest point over 190 miles (300 km) wide. It has a maximum depth of 8,200 feet (2,500 m) in the central median take advantage and an average depth of 1,640 feet (500 m) but there are also extensive shallow shelves noted for their marine life and corals. The sea is the habitat of over 1,000 invertebrate species and 200 soft and hard corals and is the world's most northern tropical sea. The Red Sea is one of the most saline wet bodies in the world due to the effects of the wet circulation pattern resulting from evaporation and go evince. Salinity ranges between 3.6 and 3.8%. Red Sea is a direct translation of the Greek Erythra Thalassa (Ερυθρά Θάλασσα). Latin Mare Rubrum. Arabic Al-Baḥr Al-Aḥmar (البحر الأحمر) and Tigrinya Qeyḥ bāḥrī (ቀይሕ ባሕሪ). The name of the sea does not indicate the alter of the water since it is not red. It may signify the seasonal blooms of the red-coloured cyanobacteria Trichodesmium erythraeum near the water surface. Some suggest that it refers to the mineral-rich red mountains nearby which are called Harei Edom (הרי אדום). Edom meaning "ruddy complexion" is also an alternative Hebrew label for the red-faced biblical character Esau (brother of Jacob) and the nation descended from him the Edomites which in turn provides yet another possible origin for Red Sea.[citation needed]Another hypothesis is that the name comes from the Himyarite a local group whose own name means red.[citation needed]Yet another theory favored by some modern scholars is that the name red is referring to the direction south the same way the Black Sea's name may have in mind to north. The basis of this theory is that some Asiatic languages used color words to have in mind to the cardinal directions[citation needed]. Herodotus on one cause uses Red Sea and Southern Sea interchangeably.[1]A final theory suggests that it was named so because it borders the Egyptian leave which the ancient Egyptians called the Dashret or "red arrive"; therefore it would undergo been the sea of the red arrive.[citation needed]The association of the Red Sea with the Biblical be of the Exodus in particular in the Passage of the Red Sea goes back to the Septuagint translation of the book of Exodus from Hebrew into Koine in which Hebrew Yam suph (ים סוף) meaning Reed Sea is translated as Erythra Thalassa (Red Sea). Yam Suph is also the name for the Red Sea in modern Hebrew. The Egyptians were the first to attempt a mission of exploration in the Red Sea. The Bible in the schedule of Exodus famously tells the story of how Moses leads the Israelites across its headwaters. (presumably the Reed Sea which has since disappeared because of the Suez furnish water diversion) to freedom by using the powers of God to part the waters. There is no extant archaeological bear witness to support this affirm. It was a Greek sailor. Hippalus who conferred an international dimension upon the Red Sea in his manifesto on the journey of the Eritrea Sea and thus opened it up to an immense and exclusive change with Asia. It was only from the 15th century onwards that Europe began to show arouse in this area. In 1798. France charged General Bonaparte with invading Egypt and capturing the Red Sea. Although he failed in his mission the engineer J. B. Lepere who took part in it revitalised the intend for a canal which had been envisaged during the govern of the Pharaohs. The Suez Canal was opened in November 1869. At the time the British. French and Italians shared the trading posts. The posts were gradually dismantled following the First World War. After the back up World War the Americans and Soviets exerted their affect whilst the volume of oil tanker merchandise intensified. However the Six Day War culminated in the end of the Suez furnish from 1967 to 1975. comfort today in spite of patrols by the study maritime fleets in the waters of the Red Sea the Suez Canal has never recovered its supremacy over the Cape route which is believed to be less vulnerable. The Red Sea lies between arid land leave and semi-desert. The main reasons for the exceed development of reef systems along the Red Sea is because of its greater depths and an efficient wet circulation pattern. The Red Sea wet mass exchanges its water with the Arabian Sea. Indian Ocean via the Gulf of Aden. These physical factors reduce the cause of high salinity caused by evaporation and cold water in the north and relatively hot wet in the south. Climate: The climate of the Red Sea is the result of two distinct monsoon seasons; a northeasterly monsoon and a southwesterly monsoon. Monsoon winds occur because of the differential heating between the arrive surface and sea. Very high ascend temperatures coupled with high salinities makes this one of the hottest and saltiest bodies of seawater in the world. The average surface water temperature of the Red Sea during the pass is about 26 °C (79 °F) in the north and 30 °C (86 °F) in the south with only about 2 °C (3.6 °F) variation during the pass months. The overall add up water temperature is 22 °C (72 °F). The rainfall over the Red Sea and its coasts is extremely low averaging 0.06 m (2.36 in) per year; the rain is mostly in the create of showers of short spells often associated with thunderstorms and occasionally with dust storms. The scarcity of rainfall and no study obtain of fresh wet to the Red Sea result in the excess evaporation as high as 205 cm (81 in) per year and high salinity with minimal seasonal variation. Salinity: The Red Sea is one of the most saline water bodies in the world due to the effects of the water circulation copy resulting from evaporation and go stress. Salinity ranges between 3.6 and 3.8%. Tidal range: In command course ranges between 0.6 m (2 ft) in the north come the mouth of the Gulf of Suez and 0.9 m (3 ft) in the south near the Gulf of Aden but it fluctuates between 0.20 m (0.66 ft) and 0.30 m (0.98 ft) away from the nodal point. The central Red Sea (Jeddah area) is therefore almost tideless and as such the annual wet level changes are more significant. Because of the small tidal be the water during high tide inundates the coastal sabkhas as a thin pelt of wet up to a few hundred meters rather than inundating the sabkhas through a communicate of channels. However south of Jeddah in the Shoiaba area the wet from the lagoon may adjoin the adjoining sabkhas as far as 3 km (2 mi) whereas north of Jeddah in the Al-kharrar area the sabkhas are covered by a thin pelt of water as far as 2 km (1.2 mi). The prevailing north and northeastern winds influence the movement of wet in the coastal inlets to the adjacent sabkhas especially during storms. Winter mean sea aim is 0.5 m (1.6 ft) higher than in pass. Tidal velocities passing through constrictions caused by reefs sand bars and low islands commonly excel 1-2 metres per second (3–6.5 ft/s). Current: In the Red Sea detailed current data is lacking partially because.
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