Examine individual changes

'{{short description|Arm of the Indian Ocean between Asia and Africa}} {{about|the body of water between Asia and Africa}} {{Infobox body of water | name = Red Sea | image = Red sea coast, Makadi bay.jpg | caption = Red Sea coast at Egyptian resort [[Makadi Bay]] | image_bathymetry = Red Sea topographic map-en.jpg | caption_bathymetry = | location = [[North Africa]], [[Horn of Africa]], and [[West Asia]] | coords = {{Coord|22|N|38|E|region:EG_type:adm1st_scale:100000000|display=inline,title}} | type = [[Sea]] | inflow = [[Barka River]], [[Haddas River]], [[Anseba River]], [[Wadi Gasus]] | outflow = [[Bab el Mandeb]] | catchment = | basin_countries = [[Djibouti]], [[Egypt]], [[Eritrea]], [[Saudi Arabia]], [[Sudan]], [[Yemen]], [[Somaliland]], [[Palestine]], and [[Jordan]] | length = {{cvt|2250|km|mi}} | width = {{cvt|355|km|mi}} | area = {{cvt|438000|km2|sqmi}} | depth = {{cvt|490|m|ft}} | max-depth = {{cvt|3040|m|ft}} | volume = {{cvt|233000|km3|cumi}} | residence_time = | shore = | elevation = | frozen = | islands = | cities = }} {{Contains special characters}} [[File:Day Pass down the Red Sea.ogv|thumb|upright=1.35|This video over the south-eastern [[Mediterranean Sea]] and down the coastline of the Red Sea was taken by the crew of Expedition 29 on board the [[International Space Station]].]] The '''Red Sea''' ({{lang-ar|البحر الأحمر - بحر القلزم |translit=Modern: al-Baḥr al-ʾAḥmar, Medieval: Baḥr al-Qulzum}}; {{Lang-he|יַם-סוּף |translit=[[Yam Suph|yam sūf]]}} or {{Lang-he|הַיָּם הָאָדְוֹם |translit=hayyām hāʾāḏōm}}; [[Coptic language|Coptic]]: ⲫⲓⲟⲙ ⲛ̀ϩⲁϩ ''Phiom Enhah'' or ⲫⲓⲟⲙ ⲛ̀ϣⲁⲣⲓ ''Phiom ǹšari''; [[Tigrinya language|Tigrinya]]: ቀይሕ ባሕሪ ''Qeyih Bahri''; {{Lang-so|Badda Cas 𐒁𐒖𐒆𐒖 𐒋𐒖𐒈}}) is a [[seawater]] [[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 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 {{cvt|438,000|km2|sqmi}},<ref>{{Cite web |date=2008-06-16 |title=State of the Marine Environment Report for the Red Sea and Gulf of Aden: 2006 |url=https://www.cbd.int/doc/meetings/mar/ebsaws-2015-02/other/ebsaws-2015-02-persga-submission1-en.pdf |url-status=live |archive-url=https://web.archive.org/web/20210421194829/https://www.cbd.int/doc/meetings/mar/ebsaws-2015-02/other/ebsaws-2015-02-persga-submission1-en.pdf |archive-date=2021-04-21 |access-date=25 January 2020}}</ref> is about {{cvt|2250|km|mi}} long, and — at its widest point — {{cvt|355|km|mi}} wide. It has an average depth of {{cvt|490|m|ft}}, and in the central ''Suakin Trough'' it reaches its maximum depth of {{cvt|3040|m|ft}}.<ref>{{Cite book |last=Dinwiddie |first=Robert |title=Ocean: The World's Last Wilderness Revealed |date=2008 |publisher=Dorling Kindersley |isbn=978-0-7566-2205-3 |editor-last=Thomas |editor-first=Louise |location=London |pages=452}}</ref> Approximately 40% of the Red Sea is quite shallow (less than 100&nbsp;m (330&nbsp;ft) deep), and about 25% is less than 50&nbsp;m (164&nbsp;ft) deep. The extensive shallow shelves are noted for their marine life and [[coral]]s. More than 1,000 [[invertebrate]] species and 200 types of soft and hard coral live in the sea. The Red Sea is the world's northernmost [[Tropics|tropical]] sea, and has been designated a [[Global 200]] [[ecoregion]]. ==Extent== The [[International Hydrographic Organization]] defines the limits of the Red Sea as follows:<ref>{{Cite web |year=1953 |title=Limits of Oceans and Seas, 3rd edition |url=https://iho.int/uploads/user/pubs/standards/s-23/S-23_Ed3_1953_EN.pdf |url-status=live |archive-url=https://web.archive.org/web/20111008191433/http://www.iho.int/iho_pubs/standard/S-23/S-23_Ed3_1953_EN.pdf |archive-date=8 October 2011 |access-date=28 December 2020 |publisher=International Hydrographic Organization}}</ref> <blockquote> ''On the North.'' The Southern limits of the [[Gulf of Suez|Gulfs of Suez]] [A line running from [[Ras Muhammad National Park|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 the coast of [[Africa]]<nowiki>]</nowiki> and [[Gulf of Aqaba|Aqaba]] [A line running from Ràs al Fasma Southwesterly to Requin Island ({{coord|27|57|N|34|36|E|display=inline}}) through [[Tiran Island]] to the Southwest point thereof and thence Westward on a parallel (27°54'N) to the coast of the [[Sinai Peninsula]]<nowiki>]</nowiki>. ''On the South.'' A line joining [[Hisn Murad|Husn Murad]] ({{coord|12|40|N|43|30|E|display=inline}}) and [[Ras Siyyan]] ({{coord|12|29|N|43|20|E|display=inline}}). </blockquote> ==Exclusive economic zone== [[Exclusive economic zones]] in Red Sea:<ref>{{Cite web |title=Sea Around Us {{!}} Fisheries, Ecosystems and Biodiversity |url=http://www.seaaroundus.org/data/#/eez |url-status=live |archive-url=https://web.archive.org/web/20160223181456/http://www.seaaroundus.org/data/#/eez |archive-date=2016-02-23 |access-date=2021-02-25 |website=www.seaaroundus.org}}</ref> {| class="wikitable" style="font-size:100%" |- !width=75|Number !width=250|Country !width=100|Area (Km²) |- | align=center|1 || '''{{KSA}}''' || align=center|186,392 |- | align=center|2 || '''{{SUD}}''' || align=center|92,513 |- | align=center|3 || '''{{EGY}}''' || align=center|91,279 |- | align=center|4 || '''{{ERI}}''' || align=center|78,383 |- | align=center|5 || '''{{YEM}}''' || align=center|35,861 |- | align=center|6 || '''{{DJI}}''' || align=center|7,037 |- style="background:#9acdff;" !Total |'''Red Sea''' || align=center|'''491,465''' |} Note: [[Halaib Triangle|Hala'ib Triangle]] disputed between Sudan and Egypt and calculated for both. ==Names== [[File:Tihama on the Red Sea near Khaukha, Yemen.jpg|thumb|[[Tihama]] on the Red Sea near Khaukha, [[Yemen]]]] ''Red Sea'' is a direct translation of the [[Ancient Greek]] ''Erythra Thalassa'' ({{lang|grc|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).<ref>{{Cite journal |last1=Phillips |first1=Carl |last2=Villeneuve |first2=François |last3=Facey |first3=William |date=2004 |title=A Latin inscription from South Arabia |url=https://www.jstor.org/stable/41223821 |journal=Proceedings of the Seminar for Arabian Studies |volume=34 |pages=239–250 |jstor=41223821 |issn=0308-8421 |via=JSTOR}}</ref> Other designations include the {{lang-ar|البحر الأحمر|Al-Baḥr Al-Aḥmar}} (alternatively بحر القلزم ''Baḥr Al-Qulzum'', literally "the Sea of [[Clysma]]"), the [[Coptic language|Coptic]] ⲫⲓⲟⲙ ̀ⲛϣⲁⲣⲓ ''Phiom ̀nšari'', [[Syriac language|Syriac]] ܝܡܐ ܣܘܡܩܐ Yammāʾ summāqā, [[Somali language|Somali]] ''Badda cas'' and [[Tigrinya language|Tigrinya]] ''Qeyyiḥ bāḥrī'' (ቀይሕ ባሕሪ). The name of the sea may signify the seasonal blooms of the red-coloured ''[[Trichodesmium|Trichodesmium erythraeum]]'' near the water's surface.<ref>{{Cite encyclopedia |title=Red Sea {{!}} sea, Middle East |encyclopedia=Encyclopedia Britannica Online Library Edition |publisher=Encyclopedia Britannica |url=https://www.britannica.com/place/Red-Sea |access-date=14 January 2008 |archive-url=https://web.archive.org/web/20230123232055/https://www.britannica.com/place/Red-Sea |archive-date=23 January 2023 |url-status=live}}</ref> <!-- Some{{Who|date=October 2009}} suggest that it refers to the mineral-rich red [[mountain]]s nearby, which are called Harei Edom (Hebrew: הרי אדום). ''[[Edom]]'', meaning "ruddy complexion", is also an alternative [[Hebrew language|Hebrew]] name 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|date=February 2007}} --> 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 is that some Asiatic languages used color words to refer to the [[5 cardinal point|cardinal directions]].<ref name="ChiTra">{{Cite web |title=How the Red Sea Got its Name |url=http://www.smithsonianjourneys.org/blog/how-the-red-sea-got-its-name-180950850/ |url-status=dead |archive-url=https://web.archive.org/web/20190926131326/https://www.smithsonianjourneys.org/blog/how-the-red-sea-got-its-name-180950850/ |archive-date=2019-09-26 |access-date=2015-07-20}}</ref> [[Herodotus]] on one occasion uses Red Sea and Southern Sea interchangeably.<ref>{{Cite journal |last=Schmitt |first=Rüdiger |date=1996 |title=Considerations on the Name of the Black Sea |journal=Hellas und der griechische Osten |publisher=Saarbrücken |pages=219–224}}</ref> The name in Hebrew ''[[Yam Suph]]'' ({{lang-he|ים סוף|lit=Sea of Reeds}}) is of biblical origin. The name in {{Lang-cop|ⲫⲓⲟⲙ `ⲛϩⲁϩ}} ''Phiom Enhah'' ("Sea of Hah") is connected to [[Egyptian language|Ancient Egyptian]] root ''ḥ-ḥ'' which refers to water and sea (for example the names of the [[Ogdoad (Egyptian)|Ogdoad]] gods [[Heh (god)|Heh and Hauhet]]).<ref>{{Cite book |last=Vycichl |first=Werner |title=Dictionnaire Etymologique de La Langue Copte |publisher=Peeters |year=1983 |location=Leuven |pages=320}}</ref> Historically, it was also known to western geographers as ''Mare Mecca'' (Sea of Mecca), and ''Sinus Arabicus'' (Gulf of Arabia).<ref>{{Cite web |title=Arabia |url=http://www.wdl.org/en/item/2919/ |url-status=live |archive-url=https://web.archive.org/web/20130605202421/http://www.wdl.org/en/item/2919/ |archive-date=5 June 2013 |access-date=11 August 2013 |publisher=World Digital Library}}</ref> Some ancient geographers called the Red Sea the Arabian Gulf<ref>{{Cite book |last=Michael D. Oblath |url=https://books.google.com/books?id=c5ya9QVCpIkC&q=Red+sea+as+Arabian+gulf&pg=PA53 |title=The Exodus itinerary sites: their locations from the perspective of the biblical sources |publisher=Peter Lang |year=2004 |isbn=978-0-8204-6716-0 |page=53 |access-date=2020-11-19 |archive-url=https://web.archive.org/web/20230210065000/https://books.google.com/books?id=c5ya9QVCpIkC&q=Red+sea+as+Arabian+gulf&pg=PA53 |archive-date=2023-02-10 |url-status=live}}</ref> or Gulf of Arabia.<ref>{{Cite book |last1=Hill |first1=Andrew E. |url=http://dx.doi.org/10.1525/9780520943728-073 |title=A survey of the Old Testament |last2=Walton |first2=John H. |date=2009 |publisher=Zondervan |isbn=978-0-310-28095-8 |edition=3 |location=Grand Rapids, Mich |pages=32|doi=10.1525/9780520943728-073 |s2cid=242765347 }}</ref> The association of the Red Sea with the [[Bible|biblical]] account of the Israelites [[crossing the Red Sea]] is ancient, and was made explicit in the [[Septuagint]] translation of the [[Book of Exodus]] from [[Hebrew language|Hebrew]] to [[Koine|Koine Greek]] in approximately the third century B.C. In that version, the ''[[Yam Suph]]'' ({{lang-he|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 term]]s – the others being the [[Black Sea]], the [[White Sea]] and 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]]. ==History== ===Ancient era=== [[File:C+B-Ship-Fig1-HatshepsuSailingBoat.PNG|thumb|[[Ancient Egypt]]ian expedition to the [[Land of Punt]] on the Red Sea coast during the reign of Queen [[Hatshepsut]]]] The earliest known exploration of the Red Sea was conducted by [[ancient Egypt]]ians, as they attempted to establish commercial routes to [[Land of Punt|Punt]]. One such expedition took place around 2500 BC, and another around 1500 BC (by [[Hatshepsut]]). Both involved long voyages down the Red Sea.<ref>{{Cite book |last=Fernandez-Armesto |first=Felipe |url=https://archive.org/details/pathfindersgloba00fern/page/24 |title=Pathfinders: A Global History of Exploration |publisher=W.W. Norton & Company |year=2006 |isbn=978-0-393-06259-5 |page=[https://archive.org/details/pathfindersgloba00fern/page/24 24]}}</ref> The biblical [[Book of Exodus]] tells the account of the [[Israelites]]' [[Crossing the Red Sea|crossing of a body of water]], which the Hebrew text calls ''[[Yam Suph]]'' ({{Lang-he|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]].<ref>''Tafsir'', Saadia Gaon, s.v. Exodus 15:22, ''et al''.</ref> [[File:Periplous of the Erythraean Sea.svg|left|thumb|upright=2.5|Settlements and commercial centers in the vicinity of the Red Sea involved in the [[spice trade]], as described in the ''[[Periplus of the Erythraean Sea]]'']] In 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.<ref>{{Cite web |title=Darius' Red Sea Canal Stele {{!}} cabinet |url=https://www.cabinet.ox.ac.uk/darius-red-sea-canal-stele |access-date=2023-06-08 |website=www.cabinet.ox.ac.uk}}</ref> In addition to 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 was constructed in the 19th century and continues to be one of the world's most important waterways.<ref>{{Cite journal |last=Colburn |first=Henry |date=2021 |title=King Darius' Red Sea Canal |url=https://hcommons.org/deposits/item/hc:44609/ |journal=FEZANA Journal |language=en-US |volume=35 |issue=4 |pages=27–30}}</ref> 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 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]]"), a [[Greek language|Greek]] [[periplus]] written by an unknown author around the 1st century, contains a detailed description of the Red Sea's ports and sea routes.<ref>{{Cite book |last=Fernandez-Armesto |first=Felipe |url=https://archive.org/details/pathfindersgloba00fern/page/32 |title=Pathfinders: A Global History of Exploration |publisher=W.W. Norton & Company |year=2006 |isbn=978-0-393-06259-5 |pages=[https://archive.org/details/pathfindersgloba00fern/page/32 32–33]}}</ref> 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 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.<ref>{{Cite book |last=East |first=W. Gordon |url=https://archive.org/details/geographybehindh0000east_z8c9/page/174 |title=The Geography behind History |publisher=W.W. Norton & Company |year=1965 |isbn=978-0-393-00419-9 |pages=[https://archive.org/details/geographybehindh0000east_z8c9/page/174 174–175]}}</ref> ===Middle Ages and modern era=== 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.<ref>{{Cite journal |last=Mallett |first=Alex |date=2008 |title=A Trip down the Red Sea with Reynald of Châtillon |url=https://www.jstor.org/stable/27755928 |journal=Journal of the Royal Asiatic Society |volume=18 |issue=2 |pages=143–144 |jstor=27755928 |issn=1356-1863}}</ref> The possibility that Raynald's fleet might sack the holy cities of Mecca and Medina caused fury throughout the Muslim world.<ref>{{Cite journal |last=Mallett |first=Alex |date=2008 |title=A Trip down the Red Sea with Reynald of Châtillon |url=https://www.jstor.org/stable/27755928 |journal=Journal of the Royal Asiatic Society |volume=18 |issue=2 |pages=146–147 |jstor=27755928 |issn=1356-1863}}</ref> However, it appears that Reynald's target were the lightly armed Muslim pilgrim convoys rather the well guarded cities of Mecca and Medina, and the belief in the Muslim world that Reynald was seeking to sack the holy cities was due to the proximity of those cities to the areas that Raynald raided.<ref>{{Cite journal |last=Mallett |first=Alex |date=2008 |title=A Trip down the Red Sea with Reynald of Châtillon |url=https://www.jstor.org/stable/27755928 |journal=Journal of the Royal Asiatic Society |volume=18 |issue=2 |pages=152–153 |jstor=27755928 |issn=1356-1863}}</ref> In 1513, trying to secure that channel to Portugal, [[Afonso de Albuquerque]] laid [[Siege of Aden|siege to Aden]]<ref>{{Cite book |last=Newitt |first=M. D. D. |title=A history of Portuguese overseas expansion, 1400–1668 |publisher=New York Routledge |year=2005 |isbn=978-0-415-23979-0 |location=London |page=87}}</ref> but was forced to retreat. They cruised 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.<ref>{{Cite book |last=Mathew |first=K. M. |url=https://books.google.com/books?id=Kl3IR3RJTIEC&q=Heitor+da+Silveira+Aden&pg=PA136 |title=History of the Portuguese Navigation in India, 1497–1600 |year=1988 |isbn=978-81-7099-046-8 |access-date=2020-11-19 |archive-url=https://web.archive.org/web/20230210065001/https://books.google.com/books?id=Kl3IR3RJTIEC&q=Heitor+da+Silveira+Aden&pg=PA136 |archive-date=2023-02-10 |url-status=live}}</ref> In 1798, [[France]] ordered General [[Napoleon I|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 the plan for a canal which had been envisaged during the reign of the [[Pharaoh]]s. 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. After 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.{{citation needed|date=January 2022}} ==Oceanography== [[File:ISS036-E-011050.jpg|thumb|upright=1.3|Annotated view of the Nile and Red Sea, with a dust storm<ref>{{Cite web |date=8 July 2013 |title=Egyptian Dust Plume, Red Sea |url=http://earthobservatory.nasa.gov/IOTD/view.php?id=81566 |url-status=live |archive-url=https://web.archive.org/web/20140222100350/http://earthobservatory.nasa.gov/IOTD/view.php?id=81566 |archive-date=22 February 2014 |access-date=4 February 2014 |website=earthobservatory.nasa.gov}}</ref>]] 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 the effect of high salinity caused by evaporation in the north and relatively hot water in the south.<ref>{{Cite journal |last1=Sofianos |first1=Sarantis S. |last2=Johns |first2=William E. |date=2002 |title=An Oceanic General Circulation Model (OGCM) investigation of the Red Sea circulation, 1. Exchange between the Red Sea and the Indian Ocean |journal=Journal of Geophysical Research: Oceans |language=en |volume=107 |issue=C11 |page=3196 |bibcode=2002JGRC..107.3196S |doi=10.1029/2001JC001184 |doi-access=free}}</ref> <span class="anchor" id="Climate"></span>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 the world. The average surface water temperature of the Red Sea during the summer is about {{cvt|26|C|F|0|lk=on}} in the north and {{cvt|30|C|F|0|}} in the south, with only about {{cvt|2|C-change}} variation during the winter months. The overall average water temperature is {{cvt|22|C|F|0|}}. Temperature and visibility remain good to around {{cvt|200|m|ft}}. The sea is known for its strong winds and unpredictable local currents.{{citation needed|date=February 2019}} The [[rainfall]] over the Red Sea and its coasts is extremely low, averaging {{cvt|60|mm|in|2}} per year. The rain is mostly short showers, often with thunderstorms and occasionally with dust [[storm]]s. The scarcity of rainfall and no major source of fresh water to the Red Sea result in excess evaporation as high as {{cvt|2050|mm|in|0}} per year and high salinity with minimal seasonal variation. A recent{{When|date=June 2023}} underwater expedition to the Red Sea offshore from [[Sudan]] and [[Eritrea]]<ref>[[BBC 2]] television program "''Oceans 3/8 The Red Sea''", 8 pm–9 pm Wednesday 26 November 2008</ref>{{Verify source|date=June 2023}} found surface water temperatures {{cvt|28|C|F|0|lk=on}} in winter and up to {{cvt|34|C|F|0|lk=on}} 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|''Favia favus'']] coral there harbours a virus, BA3, which kills ''T. loyana''.<ref>{{Cite web |title=Virus power harnessed to protect Red Sea coral |url=https://www.newscientist.com/article/mg21528725-700-virus-power-harnessed-to-protect-red-sea-coral/ |url-status=live |archive-url=https://web.archive.org/web/20150423092252/http://www.newscientist.com/article/mg21528725.700-virus-power-harnessed-to-protect-red-sea-coral.html |archive-date=2015-04-23 |access-date=2023-06-04 |website=New Scientist |language=en-US}}</ref> Scientists are investigating the unique properties of these coral and their [[commensal]] [[algae]] to see if they can be used to salvage bleached coral elsewhere.<ref>{{Cite web |last=Fitzgerald |first=Sunny |date=8 April 2020 |title=The super-corals of the Red Sea |url=https://www.bbc.com/future/article/20200408-the-middle-eastern-corals-that-could-survive-climate-change |url-status=live |archive-url=https://web.archive.org/web/20220507075625/https://www.bbc.com/future/article/20200408-the-middle-eastern-corals-that-could-survive-climate-change |archive-date=7 May 2022 |access-date=24 May 2022 |publisher=[[BBC Future]]}}</ref> ===Salinity=== 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.<ref>{{Cite book |last=Por |first=F. D. |url=https://books.google.com/books?id=syn0CAAAQBAJ&q=salinity+of+the+Red+Sea+is+greater+than+the+world+average,&pg=PA65 |title=The Legacy of Tethys: An Aquatic Biogeography of the Levant |date=2012-12-06 |publisher=Springer Science & Business Media |isbn=978-94-009-0937-3 |language=en |access-date=2020-11-19 |archive-url=https://web.archive.org/web/20230210065003/https://books.google.com/books?id=syn0CAAAQBAJ&q=salinity+of+the+Red+Sea+is+greater+than+the+world+average,&pg=PA65 |archive-date=2023-02-10 |url-status=live}}</ref> Its [[salinity]] ranges from between ~36&nbsp;[[per mil|‰]] in the southern part and 41&nbsp;‰ in the northern part around the [[Gulf of Suez]], with an average of 40&nbsp;‰. (Average salinity for the world's [[seawater]] is ~35&nbsp;‰ on the Practical Salinity Scale, or PSU; that translates to 3.5% of actual dissolved salts).<ref>{{Cite book |last=Hanauer |first=Eric |url=https://books.google.com/books?id=uh6mcZC8yWIC&q=salinity+of+the+Red+Sea+is+greater+than+the+world+average,&pg=PA67 |title=The Egyptian Red Sea: A Diver's Guide |date=1988 |publisher=Aqua Quest Publications, Inc. |isbn=978-0-922769-04-9 |language=en |access-date=2020-11-19 |archive-url=https://web.archive.org/web/20230210065001/https://books.google.com/books?id=uh6mcZC8yWIC&q=salinity+of+the+Red+Sea+is+greater+than+the+world+average,&pg=PA67 |archive-date=2023-02-10 |url-status=live}}</ref> ===Tidal range=== In general, tide ranges between {{cvt|0.6|m|ft|1}} in the north, near the mouth of the Gulf of Suez and {{cvt|0.9|m|ft|1}} in the south near the Gulf of Aden, but it fluctuates between {{cvt|0.20|m|ft|2}} and {{cvt|0.30|m|ft|2}} 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 [[sabkha]]s as a thin sheet of water up to a few hundred metres rather than flooding the [[sabkha]]s 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 {{cvt|3|km|mi|0}}, whereas north of Jeddah in the [[Al-Kharrar]] area the sabkhas are covered by a thin sheet of water as far as {{cvt|2|km|mi|1}}. The prevailing north and northeast winds influence the movement of water in the coastal inlets to the adjacent sabkhas, especially during storms. Winter mean sea level is {{cvt|0.5|m|ft|1}} higher than in summer. Tidal velocities passing through constrictions caused by reefs, sand bars and low islands commonly exceed {{cvt|1–2|m/s|0}}. Coral reefs in the Red Sea are near Egypt, Eritrea, Israel, Saudi Arabia, and Sudan.{{citation needed|date=February 2019}} ===Current=== Detailed information regarding current data is lacking, partially because the currents are weak and both spatially and temporally variable. The variation of temporal and spatial currents is as low as {{cvt|0.5|m|ft|1}}{{clarify|what does this mean?|date=October 2021}} and are governed all by wind. During the summer, northwesterly winds drive surface water south for about four months at a velocity of {{cvt|15–20|cm/s|0}}, whereas in winter the flow is reversed resulting in the inflow of water from the Gulf of Aden into 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 {{cvt|50–60|cm/s|0}} with a maximum of {{cvt|1|m/s|ft/s|1}} at the mouth of the al-Kharrar Lagoon. However, the range of the north-northeast current along the Saudi coast is {{cvt|8–29|cm/s|0}}.{{citation needed|date=February 2019}} ===Wind regime=== The north part of the Red Sea is dominated by persistent north-west [[winds]], with speeds ranging between {{cvt|7|km/h|mph|1}} and {{cvt|12|km/h|mph|1}}. 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 (geometry, geography)|direction]] with average speed generally increasing northward.<ref>{{Cite journal |last=Patzert |first=William C. |date=1974-02-01 |title=Wind-induced reversal in Red Sea circulation |url=https://dx.doi.org/10.1016/0011-7471%2874%2990068-0 |journal=Deep Sea Research and Oceanographic Abstracts |language=en |volume=21 |issue=2 |pages=109–121 |doi=10.1016/0011-7471(74)90068-0 |bibcode=1974DSRA...21..109P |issn=0011-7471}}</ref> Wind 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 the erosion and accretion of the coastal rock exposure and the submerged coral beds.<ref>{{Cite journal |last=Morcos |first=S. A. |date=1970 |title=Physical and chemical oceanography of the Red Sea |journal=Oceanography and Marine Biology Annual Review}}</ref> ==Geology== [[File:Dust red sea.jpg|thumb|upright|[[Dust storm]] over the Red Sea]] 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 8m),<ref>{{Cite book |last1=Rose |first1=Paul |title=Oceans: Exploring the hidden depths of the underwater world |last2=Laking |first2=Anne |publisher=BBC Books |year=2008 |isbn=978-1-84-607505-6 |location=London}}</ref> and it 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, {{cvt|60|C|F}}, saline brines and associated metalliferous muds. The hot solutions were emanating from an active subseafloor [[Rift (geology)|rift]]. Lake Asal in Djibouti is eligible as an experimental site to study the evolution of the deep hot brines of the Red Sea.<ref name="Boschetti-1">{{Cite journal |last1=Boschetti |first1=Tiziano |last2=Awaleh |first2=Mohamed Osman |last3=Barbieri |first3=Maurizio |date=2018 |title=Waters from the Djiboutian Afar: a review of strontium isotopic composition and a comparison with Ethiopian waters and Red Sea brines |journal=Water |volume=10 |issue=11 |pages=1700 |doi=10.3390/w10111700 |doi-access=free}}</ref> 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.<ref name="Boschetti-1" /> The high salinity of the waters was not hospitable to living organisms.<ref>{{Cite book |url=http://link.springer.com/10.1007/978-3-662-28603-6 |title=Hot Brines and Recent Heavy Metal Deposits in the Red Sea |date=1969 |publisher=Springer Berlin Heidelberg |isbn=978-3-662-27120-9 |editor-last=Degens |editor-first=Egon T. |location=Berlin, Heidelberg |language=en |doi=10.1007/978-3-662-28603-6 |editor-last2=Ross |editor-first2=David A.}}</ref>{{Failed verification|date=June 2023}} Sometime during 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 "race" between the Red Sea widening and [[Perim Island]] [[volcano|erupting]] filling the Bab el Mandeb with [[lava]]. *The lowering of world [[sea level]] during the [[Ice age|Ice Age]]s because of much water being locked up in the [[ice cap]]s. 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 Group|Zubair Archipelago]], a small chain of islands owned by Yemen. The first island, Sholan Island, emerged in an eruption in December 2011, the second island, Jadid, emerged in September 2013.<ref>{{Cite web |date=2011-12-28 |title=MSN - Outlook, Office, Skype, Bing, Breaking News, and Latest Videos |url=http://www.nbcnews.com/id/45807839 |url-status=live |archive-url=https://web.archive.org/web/20230210065003/https://www.nbcnews.com/id/wbna45807839 |archive-date=2023-02-10 |access-date=2019-11-10 |website=NBC News}}</ref><ref>{{Cite web |last=Israel |first=Brett |date=December 28, 2011 |title=New Island Rises in the Red Sea |url=http://www.livescience.com/31004-red-sea-volcanic-island.html |url-status=live |archive-url=https://web.archive.org/web/20220128081422/https://www.livescience.com/31004-red-sea-volcanic-island.html |archive-date=2022-01-28 |access-date=2015-07-31 |website=LiveScience.com}}</ref><ref>{{Cite web |last1=Oskin |first1=Becky |last2=SPACE.com |date=May 30, 2015 |title=Red Sea Parts for 2 New Islands |url=http://www.scientificamerican.com/article/red-sea-parts-for-2-new-islands |url-status=live |archive-url=https://web.archive.org/web/20150803072542/http://www.scientificamerican.com/article/red-sea-parts-for-2-new-islands/ |archive-date=3 August 2015 |access-date=31 July 2015 |website=Scientific American}}</ref> ===Oil and gas=== 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.<ref>Schenk, Christopher. ''World Petroleum Resources Project Assessment of Undiscovered Oil and ...'' https://pubs.usgs.gov/fs//2010/3119/pdf/FS10-3119.pdf .</ref> Most of these plays are controlled by the structure of the basin.<ref>{{Cite journal |last1=Dolson |first1=John C. |last2=Shann |first2=Mark V. |last3=Matbouly |first3=Sayed I. |last4=Hammouda |first4=Hussein |last5=Rashed |first5=Rashed M. |year=2001 |title=Egypt in the Twenty-First Century: Petroleum Potential in Offshore Trends |url=https://doi.org/10.2113/geoarabia0602211 |journal=GeoArabia |volume=6 |issue=2 |pages=211–230 |bibcode=2001GeoAr...6..211D |doi=10.2113/geoarabia0602211 |s2cid=221322448|doi-access=free }}</ref> 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 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 (geology)|Formation]] is an oil source rock in the basin. [[Oil seep]]s 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.<ref>{{Cite book |last=Lindquist |first=Sandra |title=The Red Sea Province: Sudr-Nubia(!) and Maqna(!) Petroleum Systems, USGS Open File Report 99-50-A |date=1998 |publisher=US Dept. of the Interior |pages=6–7, 9}}</ref> ===Mineral resources=== {{unreferenced section|date=May 2022}} [[File:Red sea stony beach taba egypt.jpg|thumb|Red Sea coast in [[Taba, Egypt|Taba]], [[Egypt]]]] In terms of mineral resources the major constituents of the Red Sea sediments are as follows: *Biogenic constituents: :Nanofossils, [[foraminifera]], [[pteropod]]s, siliceous fossils *[[Volcanogenic lake|Volcanogenic]] constituents: :[[Tuff]]ites, [[volcanic ash]], [[montmorillonite]], [[cristobalite]], [[zeolite]]s *Terrigenous constituents: :[[Quartz]], [[feldspar]]s, rock fragments, [[mica]], heavy minerals, [[clay minerals]] *Authigenic minerals: :[[Sulfide mineral]]s, [[aragonite]], [[calcite]], protodolomite, [[Dolomite (mineral)|dolomite]], quartz, [[chalcedony]]. *Evaporite minerals: :[[Magnesite]], [[gypsum]], [[anhydrite]], [[halite]], [[polyhalite]] *Brine precipitate: :Fe-montmorillonite, [[goethite]], [[hematite]], [[siderite]], [[rhodochrosite]], [[pyrite]], [[sphalerite]], anhydrite. ==Ecosystem== [[File:Hawksbill turtle at Elphinstone Reef, Red Sea, Egypt (35150034493).jpg|thumb|[[Hawksbill sea turtle]] in the [[Elphinstone Reef]]]] [[File:Nudibranch egg ribbon at Shaab Mahmoud.JPG|thumb|upright|Nudibranch egg ribbon at Shaab Mahmoud]] The Red Sea is a rich and diverse [[ecosystem]]. More than [[Fish of the Red Sea|1200 species of fish]]<ref name="fishbase">{{Cite web |last1=Froese |first1=Ranier |last2=Pauly, Daniel |year=2009 |title=FishBase |url=http://www.fishbase.org/TrophicEco/FishEcoList.php?ve_code=5 |url-status=live |archive-url=https://web.archive.org/web/20201217070339/http://www.fishbase.org/TrophicEco/FishEcoList.php?ve_code=5 |archive-date=2020-12-17 |access-date=2009-03-12}}</ref> have been recorded in the Red Sea, and around 10% of these are found nowhere else.<ref>{{Cite book |last=Siliotti |first=A. |title=Fishes of the red sea |year=2002 |isbn=978-88-87177-42-8 |editor-last=Verona, Geodia}}</ref> This also includes 42 species of [[List of deep water fish of the Red Sea|deepwater fish]].<ref name="fishbase" /> [[File:Red sea coral reef.jpg|thumb|Red Sea coral and marine fish]] The rich diversity is in part due to the {{cvt|2000|km|mi|-1}} of [[coral reef]] extending along its [[coastline]]; these [[fringing reef]]s are 5000–7000 years old and are largely formed of stony [[acropora]] and [[porites]] corals. The reefs form platforms and sometimes [[lagoon]]s along the coast and occasional other features such as cylinders (such as the [[Blue Hole (Red Sea)]] at [[Dahab]]). These coastal reefs are also visited by [[pelagic]] species of Red Sea fish, including some of the [[List of sharks in the Red Sea|44 species of shark]]. Other marine habitats include [[sea grass]] beds, [[Dry lake|salt pans]], [[mangroves|mangrove]] and [[salt marshes|salt marsh]]. It contains 175 species of [[nudibranch]], many of which are only found in the Red Sea.<ref name="SAW Yonow">{{Cite magazine |last=Yonow |first=Nathalie |year=2012 |title=Nature's Best-Dressed |url=http://archive.aramcoworld.com/issue/201204/nature.s.best-dressed.htm |url-status=live |magazine=Saudi Aramco World |publisher=Aramco Services Company |volume=63 |pages=2–9 |archive-url=https://web.archive.org/web/20181220045032/http://archive.aramcoworld.com/issue/201204/nature.s.best-dressed.htm |archive-date=20 December 2018 |access-date=11 December 2018 |number=4}}</ref> The Red Sea also contains many offshore reefs including several true atolls. Many of the unusual offshore reef formations defy [[coral reef#Types|classic (i.e., Darwinian) coral reef classification schemes]], and are generally attributed to the high levels of tectonic activity that characterize the area. The special [[biodiversity]] of the area is recognized by the [[Egypt]]ian government, who set up the [[Ras Mohammed|Ras Mohammed National Park]] in 1983. The rules and regulations governing this area protect local marine life, which has become a major draw for [[Scuba diving|diving]] enthusiasts. [[Scuba diving|Divers]] and [[snorkeller]]s should be aware that although most Red Sea species are innocuous, a few are [[Red Sea species hazardous to humans|hazardous to humans]].<ref name="Lieske-1">{{Cite book |last1=Lieske |first1=Ewald |title=Coral reef guide: Red Sea to Gulf of Aden, South Oman |last2=Myers |first2=Robert F. |last3=Fiedler |first3=Klaus E. |publisher=Collins |year=2004 |isbn=978-0-00-715986-4 |location=London}}</ref>{{Page needed|date=June 2023}} The U.N. is working to mitigate the threat from the [[FSO Safer|FSO ''Safer'']], a derelict oil tanker off the coast of Yemen that could possibly cause an enormous ecological disaster in the Red Sea.<ref>{{Cite news |date=2023-03-09 |title=UN buys huge ship to avert catastrophic oil spill off Yemen |language=en-GB |work=BBC News |url=https://www.bbc.com/news/world-middle-east-64904985 |access-date=2023-03-09}}</ref> The [[brine pools]] Red Sea have been extensive studied in terms of their microbial life. The [[Red Sea brine pool microbiology]] is characterized by its diversity and adaptation to extreme environments. == Desalination plants == There is extensive demand for [[Desalination|desalinated]] water to meet the needs of 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-fouling agent|anti-scalants]]) that [[Coral bleaching|bleach]] and kill [[coral]]s and cause diseases in the fish. This is only localized, but it may intensify with time and profoundly impact the fishing industry.<ref>{{Cite journal |last=Mabrook |first=Badr |date=1994-08-01 |title=Environmental impact of waste brine disposal of desalination plants, Red Sea, Egypt |url=https://dx.doi.org/10.1016/0011-9164%2894%2900108-1 |journal=Desalination |series=Proceedings of the IDA and WRPC World Conference On Desalination and Water Treatment |language=en |volume=97 |issue=1 |pages=453–465 |doi=10.1016/0011-9164(94)00108-1 |issn=0011-9164}}</ref> ==Trade== The Red Sea serves an important role in 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).<ref>{{Cite web |last=Rodrigue |first=Jean-Paul |date=2017-11-01 |title=Geographical Impacts of the Suez and Panama Canals |url=https://transportgeography.org/contents/chapter1/emergence-of-mechanized-transportation-systems/suez-panama-canal-geography-impacts/ |access-date=2023-06-04 |publisher=Hofstra University |language=en-US |publication-place=New York}}</ref> ===Tourism=== [[File:Elath Eilat Israel Strand Hotel datafox.jpg|thumb|Hotels in [[Eilat]], [[Israel]]]] The sea is known for its [[recreational diving]] sites, such as [[Ras Mohammed]], [[SS Thistlegorm]] (shipwreck), [[Elphinstone Reef]], [[The Brothers, Egypt|The Brothers]], [[Daedalus Reef]], [[St.John's Reef]], [[Rocky Island (Egypt)|Rocky Island]] in [[Egypt]]<ref>{{Cite web |title=Scuba Diving in Egypt - Red Sea - Dive The World Vacations |url=http://www.dive-the-world.com/diving-sites-red-sea.php |url-status=live |archive-url=https://web.archive.org/web/20130623214316/http://www.dive-the-world.com/diving-sites-red-sea.php |archive-date=2013-06-23 |access-date=2013-03-15 |website=www.dive-the-world.com}}</ref> and less known sites in [[Sudan]] such as [[Sanganeb]], [[Abington, Sudan|Abington]], [[Angarosh]] and [[Shaab Rumi]]. The Red Sea became a popular destination for diving after the expeditions of [[Hans Hass]] in the 1950s, and later by [[Jacques-Yves Cousteau]].<ref name="Cousteau">{{Cite AV media |url=https://www.youtube.com/watch?v=0mTCj-DUHro |title=Jacques Cousteau's underworld village in the Red Sea |date=23 April 2010 |publisher=BBC Earth |access-date=11 December 2018 |archive-url=https://web.archive.org/web/20180627162343/https://www.youtube.com/watch?v=0mTCj-DUHro |archive-date=27 June 2018 |url-status=live |people=Philippe Cousteau Jnr}}</ref> 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, Egypt|Taba]] on the [[Egypt]]ian 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 was closed to all swimming in December 2010 due to several serious [[2010 Sharm El Sheikh shark attacks|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 a geography where large deep-water sharks can roam in hundreds of meters of water, yet be within a hundred meters of swimming areas. The Red Sea Project is building highest quality accommodation and a wide range of facilities on the coast line in Saudi Arabia. This will allow people to visit the coastline of the Red Sea by the end of 2022 but will be fully finished by 2030.<ref>{{Cite web |date=2020-04-20 |title=Saudi Arabia's 'The Red Sea Project' breaks ground on coastal village |url=https://english.alarabiya.net/en/life-style/travel-and-tourism/2020/04/20/Saudi-Arabia-s-The-Red-Sea-Project-breaks-ground-on-coastal-village |url-status=live |archive-url=https://web.archive.org/web/20201209103910/https://english.alarabiya.net/en/life-style/travel-and-tourism/2020/04/20/Saudi-Arabia-s-The-Red-Sea-Project-breaks-ground-on-coastal-village |archive-date=2020-12-09 |access-date=2020-12-04 |website=Al Arabiya English |language=en}}</ref> {{see also|2016 Hurghada attack|2017 Hurghada attack|2006 Dahab bombings|2005 Sharm El Sheikh bombings|2004 Sinai bombings|Metrojet Flight 9268}} Tourism to the region has been threatened by occasional terrorist attacks, and by incidents related to food safety standards.<ref name="WalshKaraszDeath">{{Cite news |last1=Walsh |first1=Declan |last2=Karasz |first2=Palko |date=24 August 2018 |title=Hundreds of Tourists Evacuated From Hotel in Egypt After Britons' Sudden Death |work=[[The New York Times]] |url=https://www.nytimes.com/2018/08/24/world/middleeast/egypt-hotel-thomas-cook.html |url-status=live |access-date=26 August 2018 |archive-url=https://web.archive.org/web/20180825225328/https://www.nytimes.com/2018/08/24/world/middleeast/egypt-hotel-thomas-cook.html |archive-date=25 August 2018}}</ref><ref name="RegevCriticalBlow">{{Cite news |last=Regev |first=Dana |date=15 July 2017 |title=Egypt's tourism industry suffers a critical blow |publisher=DW |url=http://www.dw.com/en/egypts-tourism-industry-suffers-a-critical-blow/a-39705321 |url-status=live |access-date=26 August 2018 |archive-url=https://web.archive.org/web/20170716032022/http://www.dw.com/en/egypts-tourism-industry-suffers-a-critical-blow/a-39705321 |archive-date=16 July 2017}}</ref> ===Security=== The Red Sea is part of the [[sea road]]s between [[Europe]], the [[Persian Gulf]] and [[East Asia]], and as such has heavy [[shipping|shipping traffic]]. Government-related bodies with responsibility to police the Red Sea area include the [[Port Said Port Authority]], [[Suez Canal Authority]] and [[Red Sea Ports Authority]] of [[Egypt]], [[Jordan Maritime Authority]], [[Israel Port Authority]], [[Saudi Ports Authority]] and [[Sea Ports Corporation, Sudan|Sea Ports Corporation]] of [[Sudan]]. ==Bordering countries== [[File:Red Sea map.svg|thumb|A four color map of the Red Sea and its bordering countries]] The Red Sea may be geographically divided into three sections: the Red Sea proper, and in the north, the Gulf of Aqaba and the Gulf of Suez. The six countries bordering the Red Sea proper are: *Eastern shore: **[[Saudi Arabia]] **[[Yemen]] *Western shore: **[[Egypt]] **[[Sudan]] **[[Eritrea]] **[[Djibouti]] The Gulf of Suez is entirely bordered by Egypt. The Gulf of Aqaba borders Egypt, [[Israel]], [[Jordan]] and Saudi Arabia. In addition to the standard geographical definition of the six countries bordering the Red Sea cited above, areas such as [[Somaliland]] are sometimes also described as Red Sea territories. This is primarily due to their proximity to and geological similarities with the nations facing the Red Sea and/or political ties with said areas.<ref name="Barth">{{Cite book |last=Barth |first=Hans-Jörg |title=Sabkha ecosystems, Volume 2 |publisher=Springer |year=2002 |isbn=978-1-4020-0504-6 |page=148}}</ref><ref name="Makinda">{{Cite book |last=Makinda |first=Samuel M. |url=https://books.google.com/books?id=5cYOAAAAQAAJ |title=Superpower diplomacy in the Horn of Africa |publisher=Routledge |year=1987 |isbn=978-0-7099-4662-5 |page=37}}</ref> ==Towns and cities== Towns and cities on the Red Sea coast (including the coasts of the Gulfs of Aqaba and Suez) include: {{div col|colwidth=22em}} *[[Al Hudaydah]], Yemen (الحديدة) *[[Al Lith]], Saudi Arabia (الليِّث) *[[Al Qunfudhah]], Saudi Arabia (القنفذة) *[[Al-Qusayr, Egypt|Al-Qusair]], Egypt (القصير) *[[Al Wajh]], Saudi Arabia (الوجه) *[[Aqaba]], Jordan (العقبة) *[[Asseb]], Eritrea (ዓሰብ / عصب) *[[Dahab]], Egypt (دهب) *[[Duba, Saudi Arabia|Duba]], Saudi Arabia (ضباء) *[[Eilat]], Israel (אילת) *[[El Gouna]], Egypt (الجونة) *[[Suez|El Suweis]], Egypt (السويس) *[[Hala'ib]], Egypt and Sudan (حلايب) (disputed) *[[Haql]], Saudi Arabia (حقل) *[[Hirgigo]], Eritrea (ሕርጊጎ / حرقيقو) *[[Hurghada]], Egypt (الغردقة) *[[Jeddah]], Saudi Arabia (جدة) *[[Jizan|Jazan]], Saudi Arabia (جازان) *[[Marsa Alam]], Egypt (مرسى علم) *[[Massawa]], Eritrea (ምጽዋዕ / مصوع) *[[Mokha]], Yemen (المُخا) *[[Moulhoule]], Djibouti (مول هولة) *[[Nuweiba]], Egypt (نويبع) *[[Port Safaga]], Egypt (ميناء سفاجا) *[[Port Sudan]], Sudan (بورت سودان) *[[Rabigh]], Saudi Arabia (رابغ) *[[Sharm el Sheikh]], Egypt (شرم الشيخ) *[[Soma Bay]], Egypt (سوما باي) *[[Suakin]], Sudan (سواكن) *[[Taba (Egypt)|Taba]], Egypt (طابا) *[[Thuwal]], Saudi Arabia (ثول) *[[Yanbu]], Saudi Arabia (ينبع) {{div col end}} ==See also== {{Portal|Ocean|Water|Asia|Africa}} *[[Benjamin Kahn]] *{{MS|al-Salam Boccaccio 98}} ferry disaster *[[Crossing the Red Sea]], a Biblical tale from the [[Book of Exodus]] *[[Red Sea Dam]] *[[Robert Moresby]] ==References== {{Reflist|33em}} ==Further reading== * {{Cite EB1911|wstitle= Red Sea | volume= 22 |last1= Dickson |first1= Henry Newton |author1-link= Henry Newton Dickson | pages = 970&ndash;971 |short=1}} *{{Cite book |last1=Hamblin |first1=W. Kenneth |title=Earth's Dynamic Systems |last2=Christiansen |first2=Eric H. |publisher=Prentice-Hall |year=1998 |isbn=978-0-13-745373-3 |edition=8th |location=Upper Saddle River |name-list-style=amp}} *Miran, Jonathan. (2018). "The Red Sea," in David Armitage, Alison Bashford and [[Sujit Sivasundaram]] (eds.), ''Oceanic Histories'' (Cambridge: Cambridge University Press), pp.&nbsp;156–181. ==External links== {{sister project links}} *[http://www.coral-reef-info.com/red-sea-coral-reefs.html Red Sea Coral Reefs] *[https://web.archive.org/web/20120326031330/http://www.redseadivinghurghada.co.uk/underwater-photography.html Red Sea Photography] *{{Cite web |last1=Potts |first1=D.T. |last2=Gillies |first2=Sean |last3=Scalfano |first3=Perry |last4=Talbert |first4=R. |last5=Elliott |first5=Tom |last6=Becker |first6=Jeffrey |date=March 2, 2021 |title=Places: 39290 (Arabicus Sinus/Erythr(ae)um/Rubrum Mare) |url=http://pleiades.stoa.org/places/39290 |access-date=June 2, 2023 |publisher=Pleiades}} {{List of African seas}} {{List of seas}} {{Countries bordering the Red Sea}} {{Authority control}} [[Category:Red Sea| ]] [[Category:Tourist attractions in Egypt]] [[Category:Egypt–Sudan border]] [[Category:Eritrea–Sudan border]] [[Category:Great Rift Valley]] [[Category:Marine ecoregions]] [[Category:Saudi Arabia–Yemen border]] [[Category:Suez Canal]] [[Category:Underwater diving sites]] [[Category:Marginal seas of the Indian Ocean]] [[Category:Gulfs of the Indian Ocean]] [[Category:Geography of East Africa]] [[Category:Geography of North Africa]] [[Category:Geography of the Middle East]] [[Category:Geography of West Asia]] [[Category:Horn of Africa]] [[Category:Seas of Africa]] [[Category:Seas of Asia]] [[Category:Bodies of water of Egypt]] [[Category:Bodies of water of Eritrea]] [[Category:Bodies of water of Israel]] [[Category:Bodies of water of Jordan]] [[Category:Bodies of water of Saudi Arabia]] [[Category:Bodies of water of Sudan]] [[Category:Seas of Yemen]] [[Category:Inlets of Asia]] [[Category:Articles containing video clips]]'