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Al Jalali Fort

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88-495: Al Jalali Fort , or Ash Sharqiya Fort , is a fort in the harbor of Old Muscat , Oman . The fort was built by the Portuguese under Philip I of Portugal in the 1580s on an earlier Omani fortress to protect the harbor after Muscat had twice been sacked by Ottoman forces. The fort fell to Omani forces in 1650. During the civil wars between 1718 and 1747, the fort was twice captured by Persians who had been invited to assist one of

176-581: A Greek periplus written by an unknown author around the 1st century, contains a detailed description of the Red Sea's ports and sea routes. The Periplus also describes how Hippalus first discovered the direct route from the Red Sea to India . The Red Sea was favored for Roman trade with India starting with the reign of Augustus , when the Roman Empire gained control over the Mediterranean, Egypt , and

264-501: A defensive purpose. Massive doors with protruding iron spikes protect sections of the fort. Exhibits include cannons at the gun ports with shot, ropes and firing equipment, as well as old muskets and matchlocks . There are maps and historical illustrations, including a plaque that depicts the winds and the currents in Muscat bay. One room, with a ceiling made from palm-logs, is filled with cultural relics of Oman. The central square tower holds

352-544: A fort to the west of the harbor, where al-Mirani stands today. The Portuguese built this first Muscat fort in 1550 on perhaps the foundations of an earlier existing fortress mentioned by Albuquerque in his description of Muscat. In April 1552 an Ottoman fleet of twenty four galleys and four supply ships under Piri Reis left Suez en route to Hormuz, aiming to eliminate Portuguese presence in the region. An advance force landed at Muscat in July 1552. After an eighteen-day siege of Muscat

440-543: A general revolt against Portuguese rule over Hormuz broke out in November 1521, Muscat was the one place where the Portuguese were not attacked. In 1527 the Portuguese began to construct barracks, a warehouse and chapel at Muscat, apparently completed in 1531. A force of four Ottoman galiots entered the harbor in 1546 and bombarded the town, but did not land. To make their base more secure, the Portuguese sent an engineer to build

528-400: A guard helped two members of the royal family escape, but they were caught after a few days. The prison was closed in the 1970s. Fort al-Jalali was restored in 1983. Today little remains of the Portuguese period apart from a few inscriptions in that language. It has been converted into a museum of Omani cultural history. It is open to important people such as visiting heads of state, but not to

616-570: A period by the governor of Muscat, until another of his sons managed to free him. The fort is mentioned several times in the history of 19th century Oman. While the ruler of Oman was away on a pilgrimage to Mecca early in 1803, his nephew Badr bin Saif made an attempt to get control of Fort Jalali. The story is that he was being smuggled into the fort in a large box, but was detected by a Hindu trader. He managed to escape and took refuge in Qatar . In June 1849

704-662: A popular destination for diving after the expeditions of Hans Hass in the 1950s, and later by Jacques-Yves Cousteau . Popular tourist resorts include El Gouna , Hurghada , Safaga , Marsa Alam , on the west shore of the Red Sea, and Sharm-el-Sheikh , Dahab , and Taba on the Egyptian side of Sinaï , as well as Aqaba in Jordan and Eilat in Israel in an area known as the Red Sea Riviera . The popular tourist beach of Sharm el-Sheikh

792-399: A successful assault against Muscat. He slaughtered most of the inhabitants, and then plundered and burned the town. The Portuguese continued along the coast. The governor of Sohar agreed to transfer his allegiance to the king of Portugal and to pay tribute. The Portuguese arrived at Hormuz on 26 September 1507. They took the town after fierce resistance on 10 October 1507. Albuquerque signed

880-516: A treaty under which the Portuguese were free of customs duties and could build a fort and trading factory at Hormuz. Muscat now became a regular port of call for the Portuguese. Diogo Fernandes de Beja came there in 1512 to collect the tribute. Albuquerque, now Viceroy of India, visited in March 1515. In 1520 a fleet of twenty three Portuguese ships anchored in the harbor en route from the Red Sea to Hormuz. When

968-815: Is a direct translation of the Ancient Greek Erythra Thalassa ( Ἐρυθρὰ Θάλασσα ). The sea itself was once referred to as the Erythraean Sea by Europeans. As well as Mare Rubrum in Latin (alternatively Sinus Arabicus , literally "Arabian Gulf"), the Romans called it Pontus Herculis (Sea of Hercules). Other designations include the Arabic : البحر الأحمر , romanized :  Al-Baḥr Al-Aḥmar (alternatively بحر القلزم Baḥr Al-Qulzum , literally "the Sea of Clysma "),

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1056-663: Is also known as the Ash Sharqiya Fort. "Muscat" means "anchorage". True to its name, Old Muscat is a natural port in a strategic location between the Persian Gulf and the Indian Ocean . It lies on the coast of the Gulf of Oman on a bay about 700 metres (2,300 ft) long, protected from the sea by a rocky island. The port is surrounded by mountains, making it difficult to access from the landward side. Muscat may have been described by

1144-475: Is considered that it will become an ocean in time (as proposed in the model of John Tuzo Wilson ). In 1949, a deep water survey reported anomalously hot brines in the central portion of the Red Sea. Later work in the 1960s confirmed the presence of hot, 60 °C (140 °F), saline brines and associated metalliferous muds. The hot solutions were emanating from an active subseafloor rift . Lake Asal in Djibouti

1232-447: Is eligible as an experimental site to study the evolution of the deep hot brines of the Red Sea. By observing the strontium isotope composition of the Red Sea brines, it is possible to deduce how these salt waters found at the bottom of the Red Sea could have evolved in a similar way to Lake Asal, which ideally represents their compositional extreme. The high salinity of the waters was not hospitable to living organisms. Sometime during

1320-418: Is protected by a wall with round towers, built in 1625, on the western and southern sides. The Gulf of Oman and the surrounding mountains form a natural boundary to the east and north. Until the mid-20th century, the gates were closed three hours after dusk. Anyone on the streets after this time had to carry a lantern with them. In addition, smoking was banned on the main streets and the public playing of music

1408-543: Is that some Asiatic languages used color words to refer to the cardinal directions . Herodotus on one occasion uses Red Sea and Southern Sea interchangeably. The name in Hebrew Yam Suph ( Hebrew : ים סוף , lit.   'Sea of Reeds') is of biblical origin. The name in Coptic : ⲫⲓⲟⲙ `ⲛϩⲁϩ Phiom Enhah ("Sea of Hah") is connected to Ancient Egyptian root ḥ-ḥ which refers to water and sea (for example

1496-416: Is the driving force in the Red Sea to transport material as suspension or as bedload. Wind-induced currents play an important role in the Red Sea in resuspending bottom sediments and transferring materials from sites of dumping to sites of burial in quiescent environment of deposition. Wind-generated current measurement is therefore important in order to determine the sediment dispersal pattern and its role in

1584-467: The 2023-2024 Israel-Hamas war . One ship was hijacked and taken back to Yemen. The Red Sea is between arid land, desert and semi-desert . Reef systems are better developed along the Red Sea mainly because of its greater depths and an efficient water circulation pattern. The Red Sea water mass-exchanges its water with the Arabian Sea , Indian Ocean via the Gulf of Aden . These physical factors reduce

1672-494: The Coptic ⲫⲓⲟⲙ ̀ⲛϣⲁⲣⲓ Phiom ̀nšari , Syriac ܝܡܐ ܣܘܡܩܐ Yammāʾ summāqā, Somali Badda cas and Tigrinya Qeyyiḥ bāḥrī (ቀይሕ ባሕሪ). The name of the sea may signify the seasonal blooms of the red-coloured Trichodesmium erythraeum near the water's surface. A theory favored by some modern scholars is that the name red is referring to the direction south, just as the Black Sea 's name may refer to north. The basis of this theory

1760-507: The Dhofar Rebellion (1962–76). It was the most notorious of Omani prisons, which were known for their appalling conditions. Colonel David Smiley , commander of the Sultan's armed forces at Muscat, called the prison "a veritable hellhole". In 1963 forty four prisoners escaped in a well-planned break-out, but most were quickly recaptured, handicapped by their weakened physical condition. In 1969

1848-753: The Mediterranean Sea . To the point that a number of them now form a significant component of the Mediterranean ecosystem. The resulting change in biodiversity, without precedent in human memory, is currently accelerating, in particular for fishes according to surveys engaged by the Mediterranean Science Commission . The rich diversity of the Red Sea is in part due to the 2,000 km (1,240 mi) of coral reef extending along its coastline; these fringing reefs are 5000–7000 years old and are largely formed of stony acropora and porites corals. The reefs form platforms and sometimes lagoons along

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1936-585: The Red Sea slave trade from Africa to the Middle East. During the Middle Ages , the Red Sea was an important part of the spice trade route. In 1183, Raynald of Châtillon launched a raid down the Red Sea to attack the Muslim pilgrim convoys to Mecca. The possibility that Raynald's fleet might sack the holy cities of Mecca and Medina caused fury throughout the Muslim world. However, it appears that Reynald's target

2024-781: The Second World War , the Americans and Soviets exerted their influence whilst the volume of oil tanker traffic intensified. However, the Six-Day War culminated in the closure of the Suez Canal from 1967 to 1975. Today, in spite of patrols by the major 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 to piracy. Iranian -backed Yemini Houthis have attacked Western ships, including warships , during

2112-647: The Septuagint translation of the Book of Exodus from Hebrew to Koine Greek in approximately the third century BC. In that version, the Yam Suph ( Hebrew : ים סוף , lit.   'Sea of Reeds') is translated as Erythra Thalassa (Red Sea). The Red Sea is one of four seas named in English after common color terms – the others being the Black Sea , the White Sea and

2200-650: The Sinai Peninsula , the Gulf of Aqaba , and the Gulf of Suez —leading to the Suez Canal . It is underlain by the Red Sea Rift , which is part of the Great Rift Valley . The Red Sea has a surface area of roughly 438,000 km (169,000 sq mi), is about 2,250 km (1,400 mi) long, and 355 km (221 mi) wide at its widest point. It has an average depth of 490 m (1,610 ft), and in

2288-764: The Tertiary period, the Bab el Mandeb closed and the Red Sea evaporated to an empty hot dry salt-floored sink. Effects causing this would have been: A number of volcanic islands rise from the center of the sea. Most are dormant. However, in 2007, Jabal al-Tair island in the Bab el Mandeb strait erupted violently. Two new islands were formed in 2011 and 2013 in the Zubair Archipelago , a small chain of islands owned by Yemen. The first island, Sholan Island, emerged in an eruption in December 2011,

2376-615: The Yellow Sea . The direct rendition of the Greek Erythra thalassa in Latin as Mare Erythraeum refers to the north-western part of the Indian Ocean , and also to a region on Mars . The earliest known exploration of the Red Sea was conducted by ancient Egyptians , as they attempted to establish commercial routes to Punt . One such expedition took place around 2500 BC, and another around 1500 BC (by Hatshepsut ). Both involved long voyages down

2464-939: The global economy , with cargo vessels traveling between the Indian Ocean and the Mediterranean Sea every year, thus shortening the path between Asia and Europe almost by half (as compared to traveling around Africa via the Atlantic Ocean). 12% of global trade passes through the Red Sea. This includes 30% of global container traffic. The sea is known for its recreational diving sites, such as Ras Mohammed , SS Thistlegorm (shipwreck), Elphinstone Reef , The Brothers , Daedalus Reef , St. John's Reef , Rocky Island in Egypt and less known sites in Sudan such as Sanganeb , Abington , Angarosh and Shaab Rumi . The Red Sea became

2552-517: The sabkhas through a network of channels. However, south of Jeddah in the Shoiaba area, the water from the lagoon may cover 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 sheet of water as far as 2 km (1.2 mi). The prevailing north and northeast winds influence the movement of water in the coastal inlets to

2640-514: The 16th century it was becoming an important trading center. At this time the interior of Oman was ruled by an Arab Imam, but the coast on which Muscat lay was subject to the Persian King of Hormuz . In 1497 the Portuguese navigator Vasco da Gama found a route around the southern cape of Africa and east to India and the Spice Islands. The Portuguese quickly began trying to establish a monopoly on

2728-438: The 44 recorded species of shark, and by many species (over 175) of nudibranch , many of which are endemic to the Red Sea. Other coastal Red Sea habitats include sea grass beds, salt pans , mangrove and salt marsh . Furthermore the deep Red Sea brine pools have been extensively studied with regard to their microbial life, characterized by its diversity and adaptation to extreme environments. The high marine biodiversity of

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2816-588: The 6th century BC, Darius the Great , who was a prominent ruler of the Achaemenid Empire in Persia, undertook significant efforts to improve and extend navigation in the Red Sea. He sent reconnaissance missions to explore the Red Sea area and to identify its various navigational hazards, such as rocks and currents. This effort was significant, as it contributed to safer and more efficient navigation routes. In addition to

2904-521: The Achaemenid Empire's economic and political power in the region. In the late 4th century BC, Alexander the Great sent Greek naval expeditions down the Red Sea to the Indian Ocean . Greek navigators continued to explore and compile data on the Red Sea. Agatharchides collected information about the sea in the 2nd century BC. The Periplus of the Erythraean Sea (" Periplus of the Red Sea "),

2992-640: The Persian forces. The Persians reembarked for Persia, taking their loot with them. A few years later Saif bin Sultan II, who had been deposed, again called for help. A Persian expedition arrived at Julfar around October 1742. The Persians made an unsuccessful attempt to take Muscat, defeated by a stratagem of the new Imam Sultan bin Murshid . Later in 1743 the Persians returned, bringing Saif bin Sultan II with them. They took

3080-706: The Persian market was closed to them until 1630. By then the Dutch and English dominated trade in the Persian Gulf. Nasir bin Murshid (r. 1624–49) was the first Imam of the Yaruba dynasty in Oman, elected in 1624. He was able to unify the tribes with a common goal of expelling the Portuguese. Nasir bin Murshid drove the Portuguese out of all their bases in Oman except Muscat. He was succeeded by his cousin Sultan bin Saif in 1649. In December 1649

3168-423: The Red Sea and its coasts is extremely low, averaging 60 mm (2.36 in) per year. The rain is mostly short showers, often with thunderstorms and occasionally with dust storms . The scarcity of rainfall and no major source of fresh water to the Red Sea result in excess evaporation as high as 2,050 mm (81 in) per year and high salinity with minimal seasonal variation. A recent underwater expedition to

3256-487: The Red Sea inside the Bab al-Mandab , as the first fleet from Europe in modern times to have sailed these waters. Later in 1524 the city was delivered to Governor Heitor da Silveira as an agreement for protection from the Ottomans . In 1798, France ordered General Napoleon to invade Egypt and take control of the Red Sea. Although he failed in his mission, the engineer Jean-Baptiste Lepère , who took part in it, revitalised

3344-408: The Red Sea is dominated by persistent north-west winds , with speeds ranging between 7 km/h (4.3 mph) and 12 km/h (7.5 mph). The rest of the Red Sea and the Gulf of Aden are subjected to regular and seasonally reversible winds. The wind regime is characterized by seasonal and regional variations in speed and direction with average speed generally increasing northward. Wind

3432-465: The Red Sea offshore from Sudan and Eritrea found surface water temperatures 28 °C (82 °F) in winter and up to 34 °C (93 °F) in the summer, but despite that extreme heat, the coral was healthy with much fish life with very little sign of coral bleaching , with only 9% infected by Thalassomonas loyana , the 'white plague' agent. Favia favus coral there harbours a virus, BA3, which kills T. loyana . Scientists are investigating

3520-566: The Red Sea. The biblical Book of Exodus tells the account of the Israelites ' crossing of the sea , which the Hebrew text calls Yam Suph ( Hebrew : יַם סוּף ). Yam Suph was traditionally identified as the Red Sea. Rabbi Saadia Gaon (882‒942), in his Judeo-Arabic translation of the Pentateuch , identifies the crossing place of the Red Sea as Baḥar al-Qulzum , meaning the Gulf of Suez . In

3608-460: The Red Sea. The net value of the latter predominates, resulting in an overall drift to the north end of the Red Sea. Generally, the velocity of the tidal current is 50–60 cm/s (20–24 in/s) with a maximum of 1 m/s (3.3 ft/s) at the mouth of the al-Kharrar Lagoon. However, the range of the north-northeast current along the Saudi coast is 8–29 cm/s (3–11 in/s). The north part of

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3696-418: The adjacent sabkhas, especially during storms. Winter mean sea level is 0.5 m (1.6 ft) higher than in summer. Tidal velocities passing through constrictions caused by reefs, sand bars and low islands commonly exceed 1–2 m/s (3–7 ft/s). Coral reefs in the Red Sea are near Egypt, Eritrea, Israel, Saudi Arabia, and Sudan. Detailed information regarding current data is lacking, partially because

3784-526: The area is recognized by the Egyptian government, which set up the Ras Mohammed National Park in 1983. The rules and regulations governing this area protect local marine life, which has become a major draw for diving enthusiasts who should be aware that although most Red Sea species are innocuous, a few are hazardous to humans. There is extensive demand for desalinated water to meet the needs of

3872-523: The battlements. Old Muscat Old Muscat is the original historic city of Muscat , the capital of Oman , on the coast in the Gulf of Oman . The old city of Muscat is separated from the rest of modern Muscat by coastal mountains. It is located along the Muttrah Corniche coastal road (entering via the Muscat Gate Museum ) between Port Sultan Qaboos and Al Bustan Beach . The city

3960-450: The central Suakin Trough it reaches its maximum depth of 3,040 m (9,970 ft). Approximately 40% of the Red Sea is quite shallow at less than 100 m (330 ft) deep, and about 25% is less than 50 m (160 ft) deep. The extensive shallow shelves are noted for their marine life and corals . More than 1,000 invertebrate species and 200 types of soft and hard coral live in

4048-531: The coast and occasional other features such as cylinders (such as the Blue Hole (Red Sea) at Dahab ). The Red Sea also hosts many offshore reefs, including several true atolls. Many of the unusual offshore reef formations defy classic (i.e., Darwinian) coral reef classification schemes, and are generally attributed to the high levels of tectonic activity that characterize the area. Both offshore and coastal reefs are visited by pelagic species of fish, including many of

4136-1425: The coast of Africa ] and Aqaba [A line running from Ràs al Fasma Southwesterly to Requin Island ( 27°57′N 34°36′E  /  27.950°N 34.600°E  / 27.950; 34.600 ) through Tiran Island to the Southwest point thereof and thence Westward on a parallel (27°54'N) to the coast of the Sinai Peninsula ]. On the South. A line joining Husn Murad ( 12°40′N 43°30′E  /  12.667°N 43.500°E  / 12.667; 43.500 ) and Ras Siyyan ( 12°29′N 43°20′E  /  12.483°N 43.333°E  / 12.483; 43.333 ). Exclusive economic zones in Red Sea: Note: Hala'ib Triangle disputed between Sudan and Egypt and calculated for both. Red Sea has names in many languages (Modern Arabic : البحر الأحمر , romanized :  al-Baḥr al-ʾAḥmar , Medieval Arabic: بحر القلزم , romanized:  Baḥr al-Qulzum ; Biblical Hebrew : יַם-סוּף , romanized:  Yam Sūp̄ or Hebrew : הַיָּם הָאָדוֹם , romanized :  hayYām hāʾĀḏōm ; Coptic : ⲫⲓⲟⲙ ⲛ̀ϩⲁϩ Phiom Enhah or ⲫⲓⲟⲙ ⲛ̀ϣⲁⲣⲓ Phiom ǹšari ; Tigrinya : ቀይሕ ባሕሪ Qeyih Bahri ; Somali : Badda Cas ; Afar : "Qasa Bad". Red Sea

4224-524: The commander of al Mirani to fire on al Jalali while his ships joined in from the east of the fort. While this was in progress Said bin Ahmad bribed his jailer and escaped. Isolated and without a hostage, the two brothers agreed to surrender. The Imam took Saif and held him under surveillance to prevent a fresh rebellion. Said bin Ahmad ruled from 1783 to 1789. During his reign his son was held prisoner in Fort al-Jalali for

4312-417: The currents are weak and both spatially and temporally variable. The variation of temporal and spatial currents is as low as 0.5 m (1.6 ft) and are governed all by wind. During the summer, northwesterly winds drive surface water south for about four months at a velocity of 15–20 cm/s (6–8 in/s), whereas in winter the flow is reversed resulting in the inflow of water from the Gulf of Aden into

4400-423: The effect of high salinity caused by evaporation in the north and relatively hot water in the south. The climate of the Red Sea is the result of two monsoon seasons: a northeasterly monsoon and a southwesterly monsoon. Monsoon winds occur because of differential heating between the land and the sea. Very high surface temperatures and high salinities make this one of the warmest and saltiest bodies of seawater in

4488-427: The erosion and accretion of the coastal rock exposure and the submerged coral beds. The Red Sea was formed by the Arabian Peninsula being split from the Horn of Africa by movement of the Red Sea Rift . This split started in the Eocene and accelerated during the Oligocene . The sea is still widening (in 2005, following a three-week period of tectonic activity it had grown by 8 m [26 ft]), and it

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4576-402: The fifth Yaruba Imam of Oman, Sultan bin Saif II , a struggle began between rival contenders for the Imamate. Fort al-Jalali was damaged during this civil war. The country became divided between Saif bin Sultan II and his cousin Bal'arab bin Himyar , rival Imams. Finding his power dwindling, Saif bin Sultan II asked for help from Nader Shah of Persia. In 1738 the two forts were surrendered to

4664-422: The first ruler of the Al Said dynasty, blockaded Muscat and captured the forts in 1749. He renovated them, particularly al-Jalali. The function of al-Jalali changed from passive defense of the harbor to a base from which troops could be dispatched. In the decades that followed the large central buildings and the round towers were added. Early in 1781 two of Ahmad bin Said's sons, Sultan and Saif, took control of

4752-409: The forces of Sultan bin Saif captured the town of Muscat. About 600 Portuguese managed to escape by sea, while others fled into Forte do Almirante (al Mirani). They surrendered on 23 January 1650. The capture of Muscat from the Portuguese marked the beginning of an expansion of Omani sea power in which the Portuguese possessions in India and East Africa soon came under threat. After the death in 1718 of

4840-618: The forts of al-Mirani and al-Jalali. When the governor of Muscat tried to recover the forts, Sultan and Saif began a damaging bombardment of the town. The two brothers gained the support of the powerful Sheikh Saqar, who marched on the capital in April 1781. Their father agreed to an amnesty, letting his rebellious sons hold both the forts. He changed his mind and took al Mirani, while the brothers held al Jelali for some months. Sultan and Saif then kidnapped their brother Said bin Ahmad and imprisoned him in al Jalali. The Imam, their father, hurried to Muscat which he reached in January 1782. He ordered

4928-400: The geographer Ptolemy in the 2nd century, who noted a "concealed harbor" in the region. Al Jalali Fort lies on a rocky outcrop on the east side of the Muscat harbor. It faces Fort Al-Mirani , which is built on another outcrop on the west side. Muscat was strongly defended against attack from the sea by these twin forts, by the Muttrah fort further to the west and by other fortifications on

5016-409: The governor of Sohar made a treaty with the British resident to suppress the slave trade. This triggered a revolt by the religious party in which the governor was killed and his father, Hamad, was made governor. The Sultan of Oman, then residing in Zanzibar , arranged for Hamad to be seized and thrown in jail in Fort al Jalali. Hamad died on 23 April 1850, either from starvation or from poison. In 1895

5104-527: The intention of making it the main fort. However, in 1623 Forte do Almirante (today's Fort Al-Mirani ) was still considered the more important of the two forts, and was used as a residence in the hot weather by the governor of Muscat. In 1625 the Portuguese built walls and towers around Muscat to improve the defenses. Remains of these fortifications exist today. Muscat was a drain on Portuguese finances, with its requirement to maintain large military and naval forces to defend it. Trade did not prosper as hoped since

5192-426: The main museum exhibits including rugs, pottery, jewelry, weapons, household utensils and incense holders. A dining hall overlooks the courtyard for use by the distinguished visitors. An old breeze-maker has been preserved in this room, once manually operated but now mechanized. The fort plays a role in special events where the royal dhow and yacht sail in through the harbor, fireworks are launched and bagpipers play on

5280-425: The major constituents of the Red Sea sediments are as follows: The Red Sea is a rich and diverse ecosystem. For example more than 1200 fish species have been recorded in the Red Sea, of which 10% are endemic, found nowhere else. Since the opening of the Suez Canal in November 1869, over a thousand marine species from the Red Sea—from plankton, seaweeds, invertebrates to fishes—have migrated northward and settled in

5368-416: The maritime explorations, during the reign of Darius the Great, a canal was constructed linking the Nile River to the northern end of the Red Sea at Suez. This canal is sometimes referred to as the ancient Suez Canal. It played a pivotal role in improving trade and communication between the Nile Valley and the Red Sea, and beyond to the Indian Ocean. This canal was a predecessor to the modern Suez Canal , which

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5456-400: The names of the Ogdoad gods Heh and Hauhet ). Historically, it was also known to western geographers as Mare Mecca (Sea of Mecca), and Sinus Arabicus (Gulf of Arabia). Some ancient geographers called the Red Sea the Arabian Gulf or Gulf of Arabia. The association of the Red Sea with the biblical account of the Israelites crossing the Red Sea is ancient, and was made explicit in

5544-404: The northern Red Sea. The route had been used by previous states but grew in the volume of traffic under the Romans. From Indian ports goods from China were introduced to the Roman world. Contact between Rome and China depended on the Red Sea, but the route was broken by the Aksumite Empire around the 3rd century AD. From antiquity until the 20th-century , the Red Sea was also a trade route of

5632-439: The objective. The Portuguese sailed along the Oman coast destroying ships and looting the towns. At Qurayyat , which they took after a hard fight, the Portuguese mutilated their captives, killed the inhabitants regardless of sex or age, and despoiled and burned the town. Muscat, at first, surrendered unconditionally to avoid the same fate. However, the people withdrew their submission when reinforcements arrived. Albuquerque launched

5720-413: The plan for a canal which had been envisaged during the reign of the Pharaohs . Several 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 none lasted for long. The Suez Canal was opened in November 1869. During the first half of the 20th-century, the Red Sea slave trade attracted substantional international condemnation. After

5808-428: The population and the industries along the Red Sea. There are at least 18 desalination plants along the Red Sea coast of Saudi Arabia which discharge warm brine and treatment chemicals ( chlorine and anti-scalants ) that bleach and kill corals and cause diseases in the fish. This is only localized, but it may intensify with time and profoundly impact the fishing industry. The Red Sea serves an important role in

5896-427: The public. The fort is made up of two towers with a connecting wall pierced by gun ports for cannon. The interior is now landscaped with fountains and pools, trees and gardens. The result has been described as "Disneyfication". In the center of the fort there is a courtyard planted with trees. Around it on various levels are rooms, enclosures and towers accessible through a complex set of stairways that may have once had

5984-514: The rival Imams. The fort was extensively rebuilt later. At times, Al Jalali served as a refuge or a jail for a member of the royal family. For much of the 20th century it was used as Oman's main prison, but this function ended in the 1970s. Fort al-Jalali was restored in 1983 and converted into a private museum of Omani cultural history that is accessible only to dignitaries visiting the country. Exhibits include cannons, old muskets and matchlocks , maps, rugs and other artifacts. The Portuguese called

6072-399: The rocky ridges surrounding the bay. Until recently, the fort was only accessible from the harbor side by way of a steep flight of stone steps. Land reclamation on the seaward side of the rock has now provided space for a heliport. A funicular railway makes the fort more accessible. In the early 15th century Muscat was a minor port, used by ships as a place to collect water. By the start of

6160-413: The sea. The Red Sea is the world's northernmost tropical sea, and has been designated a Global 200 ecoregion. The International Hydrographic Organization defines the limits of the Red Sea as follows: On the North. The Southern limits of the Gulfs of Suez [A line running from Ràs Muhammed (27°43'N) to the South point of Shadwan Island (34°02'E) and thence Westward on a parallel (27°27'N) to

6248-469: The second island, Jadid, emerged in September 2013. Approximately 40% of the Red Sea is quite shallow at less than 100 m (330 ft) deep, with about 25% less than 50 m (160 ft) deep. Undiscovered oil reserves in the region have been estimated at 5,041 MMBO. Undiscovered gas reserves in the region have been estimated at 112,349 BCFG. Undiscovered natural gas reserves have been estimated at 3,077 MMBNGL. Most of these plays are controlled by

6336-484: 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 water level changes are more significant. Because of the small tidal range the water during high tide inundates the coastal sabkhas as a thin sheet of water up to a few hundred metres rather than flooding

6424-469: The southern part and 41 ‰ in the northern part around the Gulf of Suez , with an average of 40 ‰. (Average salinity for the world's seawater is ~35 ‰ on the Practical Salinity Scale, or PSU; that translates to 3.5% of actual dissolved salts). In general, tide ranges between 0.6 m (2.0 ft) in the north, near the mouth of the Gulf of Suez and 0.9 m (3.0 ft) in

6512-457: The structure Forte de São João (Fort St. John). The origin of the present name "Al Jalali" is disputed. One theory is that it comes from the Arabic Al Jalal , which means "great beauty". Legend states that it was named after a Baluchi commander called Mir Jalal Khan from the tribe of Hooth , so was Fort Al-Mirani named after his brother, Mir Miran, who also a commander. Al Jalali Fort

6600-621: The structure of the basin. Normal faults are common as the Red Sea occupies an active diverging margin. These targets are commonly found below the Salt deposits of the Middle Miocene . Modern development is focused on the following fields. The Durwara 2 Field was discovered in 1963, while the Suakin 1 Field and the Bashayer 1A Field were discovered in 1976, on the Egyptian side of the Red Sea. The Barqan Field

6688-611: The town fell and the fort was destroyed. The commander, João de Lisboa, and 128 Portuguese were taken captive. The main Ottoman fleet arrived, and the combined fleet went on to Hormuz. The Portuguese regained the town two years later, and in 1554 repulsed another attack by the Turks. Fort Al Jalali was built after the Ottomans sacked Muscat for a second time in 1582. In 1587 Captain Belchior Calaça

6776-456: The town of Muscat, but the al-Jalali and al-Mirani forts held out and Saif bin Sultan II would not order them to yield. Omani historians say that the Persian commander, Mirza Taki, invited Saif to a banquet on his ship. Saif became stupefied by wine and his seal was taken from him. It was used to forge orders to the forts' commanders to surrender, a ruse that was successful. Ahmad bin Said al-Busaidi ,

6864-456: The trade in spices, silk and other goods. They came into conflict with Mamluk Egypt , whose trade with Europe through the Red Sea was threatened. Hormuz was the main center for the trade route with modern Iraq and Iran through the Persian Gulf. The Portuguese wanted control of this route, too. On 10 August 1507, an expedition of six ships under Admiral Afonso de Albuquerque left the newly established Portuguese base on Socotra with Hormuz as

6952-516: The tribes sacked Muscat. Sultan Faisal bin Turki took refuge in Fort al-Jalali until his brother, who was holding Fort al-Mirani, regained control of the town. For most of the 20th century Fort al-Jalali was the main prison in Oman, holding about 200 prisoners. Some were Omanis from the interior captured during the Jebel Akhdar War (1954–59), or taken after that war. Other prisoners were taken during

7040-493: The twin Fort al-Mirani were both completed between 1586 and 1588. The Portuguese faced growing competition in the region from English and Dutch traders. In 1622 a joint Persian-English force took Hormuz. After this the Portuguese built forts in other ports on the Omani coast, although they abandoned most of them in 1633–34, concentrating on defending Muscat. After 1622 the Portuguese began to strengthen Fort al Jalali, apparently with

7128-442: The unique properties of these coral and their commensal algae to see if they can be used to salvage bleached coral elsewhere. The Red Sea is one of the saltiest bodies of water in the world, owing to high evaporation and low precipitation; no significant rivers or streams drain into the sea, and its southern connection to the Gulf of Aden , an arm of the Indian Ocean, is narrow. Its salinity ranges from between ~36  ‰ in

7216-481: The world. The average surface water temperature of the Red Sea during the summer 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 winter months. The overall average water temperature is 22 °C (72 °F). Temperature and visibility remain good to around 200 m (660 ft). The sea is known for its strong winds and unpredictable local currents. The rainfall over

7304-507: Was also banned. Tourist attractions in Old Muscat include: 23°36′50″N 58°35′38″E  /  23.61389°N 58.59389°E  / 23.61389; 58.59389 Red Sea The Red Sea is a sea inlet of the Indian Ocean , lying between Africa and Asia. Its connection to the ocean is in the south, through the Bab-el-Mandeb strait and the Gulf of Aden . To its north lie

7392-514: Was closed to all swimming in December 2010 due to several serious shark attacks , including a fatality. As of December 2010, scientists are investigating the attacks and have identified, but not verified, several possible causes including over-fishing which causes large sharks to hunt closer to shore, tourist boat operators who chum offshore for shark-photo opportunities, and reports of ships throwing dead livestock overboard. The sea's narrowness, significant depth, and sharp drop-offs, all combine to form

7480-481: Was constructed in the 19th century and continues to be one of the world's most important waterways. The construction of the canal during Darius's reign is evidenced by ancient records, including inscriptions. Darius commemorated the completion of the canal by creating stelae (stone monuments) with inscriptions in several languages, describing the construction and its benefits. The canal not only facilitated trade but also solidified Darius's control over Egypt and enhanced

7568-702: Was discovered in 1969, and the Midyan Field in 1992, both within the Midyan Basin on the Saudi Arabian side of the Red Sea. The 20-m thick Middle Miocene Maqna Formation is an oil source rock in the basin. Oil seeps occur near the Farasan Islands , the Dahlak Archipelago , along the coast of Eritrea, and in the southeastern Red Sea along the coasts of Saudi Arabia and Yemen. In terms of mineral resources

7656-427: Was sent to Muscat to build the fortress, which was named Forte de São João . The top of the prominence on which the fort stands was first leveled, and the rock was scarped. Calaça built a cistern to hold water for the occupants and armed the fort with cannon. It seems to have been built on older foundations. The main improvement made by the Portuguese was to construct a gun deck looking over the harbor. Fort al-Jalali and

7744-399: Was the lightly armed Muslim pilgrim convoys, rather than the well guarded cities of Mecca and Medina, and the belief in the Muslim world that Reynald was seeking to sack the holy cities, due to the proximity of those cities to the areas that Raynald raided. In 1513, trying to secure that channel to Portugal, Afonso de Albuquerque laid siege to Aden but was forced to retreat. They cruised

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