Valley Of The Queens (song)
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Valley Of The Queens (song)
The Valley of the Queens (Arabic: وادي الملكات ''Wādī al-Malekāt'') is a site in Egypt, in which queens, princes, princesses, and other high ranking officials were buried. Pharaohs themselves were buried in the Valley of the Kings. The Valley of the Queens was known anciently as ''Ta-Set-Neferu'', which has a double meaning of "The Place of Beauty" and/or "the Place of the Royal Children". Excavation of the tombs at the Valley of the Queens was pioneered by Ernesto Schiaparelli and Francesco Ballerini in the early 1900s. The Valley of the Queens consists of the main wadi, which contains most of the tombs, along with the Valley of Prince Ahmose, the Valley of the Rope, the Valley of the Three Pits, and the Valley of the Dolmen. The main wadi contains 91 tombs and the subsidiary valleys add another 19 tombs. The burials in the subsidiary valleys all date to the 18th Dynasty.Demas, Martha, and Neville Agnew, eds. 2012. Valley of the Queens Assessment Report: Volume 1. L ...
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Arabic
Arabic (, ' ; , ' or ) is a Semitic languages, Semitic language spoken primarily across the Arab world.Semitic languages: an international handbook / edited by Stefan Weninger; in collaboration with Geoffrey Khan, Michael P. Streck, Janet C. E.Watson; Walter de Gruyter GmbH & Co. KG, Berlin/Boston, 2011. Having emerged in the 1st century, it is named after the Arabs, Arab people; the term "Arab" was initially used to describe those living in the Arabian Peninsula, as perceived by geographers from ancient Greece. Since the 7th century, Arabic has been characterized by diglossia, with an opposition between a standard Prestige (sociolinguistics), prestige language—i.e., Literary Arabic: Modern Standard Arabic (MSA) or Classical Arabic—and diverse vernacular varieties, which serve as First language, mother tongues. Colloquial dialects vary significantly from MSA, impeding mutual intelligibility. MSA is only acquired through formal education and is not spoken natively. It is ...
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UNESCO
The United Nations Educational, Scientific and Cultural Organization is a specialized agency of the United Nations (UN) aimed at promoting world peace and security through international cooperation in education, arts, sciences and culture. It has 193 member states and 12 associate members, as well as partners in the non-governmental, intergovernmental and private sector. Headquartered at the World Heritage Centre in Paris, France, UNESCO has 53 regional field offices and 199 national commissions that facilitate its global mandate. UNESCO was founded in 1945 as the successor to the League of Nations's International Committee on Intellectual Cooperation.English summary). Its constitution establishes the agency's goals, governing structure, and operating framework. UNESCO's founding mission, which was shaped by the Second World War, is to advance peace, sustainable development and human rights by facilitating collaboration and dialogue among nations. It pursues this objective t ...
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Vizier (Ancient Egypt)
The vizier () was the highest official in ancient Egypt to serve the pharaoh (king) during the Old, Middle, and New Kingdoms. Vizier is the generally accepted rendering of ancient Egyptian , etc., among Egyptologists. The ''Instruction of Rekhmire'' (''Installation of the Vizier''), a New Kingdom text, defines many of the duties of the , and lays down codes of behavior. The viziers were often appointed by the pharaoh. During the 4th Dynasty and early 5th Dynasty, viziers were exclusively drawn from the royal family; from the period around the reign of Neferirkare Kakai onwards, they were chosen according to loyalty and talent or inherited the position from their fathers. Responsibilities The viziers were appointed by the pharaohs and often belonged to a pharaoh's family. The vizier's paramount duty was to supervise the running of the country, much like a prime minister. At times this included small details such as sampling the city's water supply. All other lesser supervis ...
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Thutmose I
Thutmose I (sometimes read as Thutmosis or Tuthmosis I, Thothmes in older history works in Latinized Greek; Ancient Egyptian: '' ḏḥwtj- ms'', ''Tʼaḥawtī-mīsaw'', , meaning "Thoth is born") was the third pharaoh of the 18th Dynasty of Egypt. He received the throne after the death of the previous king, Amenhotep I. During his reign, he campaigned deep into the Levant and Nubia, pushing the borders of Egypt farther than ever before in each region. He also built many temples in Egypt, and a tomb for himself in the Valley of the Kings; he is the first king confirmed to have done this (though Amenhotep I may have preceded him). Thutmose I's reign is generally dated to 1506–1493 BC, but a minority of scholars—who think that astrological observations used to calculate the timeline of ancient Egyptian records, and thus the reign of Thutmose I, were taken from the city of Memphis rather than from Thebes—would date his reign to 1526–1513 BC. He was succeeded by his son T ...
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Sitdjehuti
Sitdjehuti (or ''Satdjehuti''; “Daughter of Thoth”) was a princess and queen of the late Seventeenth Dynasty of Egypt. She was a daughter of Pharaoh Senakhtenre Ahmose and Queen Tetisheri. She was the wife of her brother Seqenenre Tao and was the mother of Princess Ahmose. Life Sitdjehuti was a daughter of Pharaoh Senakhtenre Ahmose and a sister to Pharaoh Seqenenre Tao and the queens Ahhotep and Ahmose Inhapy. She was married to her (half-)brother Seqenenre-Tao and bore him a daughter, Ahmose. On her sarcophagus, she is stated to be the daughter of Tetisheri. Her other name is given as Satibu. Titles Sitdjehuti's titles include ''King's Wife'', ''King's Sister'', and ''King's Daughter''. She is mentioned on the mummy shroud of her daughter Ahmose, which was found in the Valley of the Queens (QV47). Ahmose is called the King's Daughter and Queen's Sister. This states that Ahmose was the daughter of King Seqenenre Tao and Sitdjehuti.Grajetzki, Ancient Egyptian Queens: a ...
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Seqenenre Tao
Seqenenre Tao (also Seqenera Djehuty-aa or Sekenenra Taa, called 'the Brave') ruled over the last of the local kingdoms of the Theban region of Egypt in the Seventeenth Dynasty during the Second Intermediate Period. He probably was the son and successor to Senakhtenre Ahmose and Queen Tetisheri. The dates of his reign are uncertain, but he may have risen to power in the decade ending in 1560 BC or in 1558 BC (based on the probable accession date of his son, Ahmose I, the first ruler of the Eighteenth Dynasty, see Egyptian chronology). With his queen, Ahhotep I, Seqenenre Tao fathered two pharaohs, Kamose, his immediate successor who was the last pharaoh of the Seventeenth Dynasty, and Ahmose I who, following a regency by his mother, was the first pharaoh of the Eighteenth. Seqenenre Tao is credited with starting the opening moves in a war of revanchism against Hyksos incursions into Egypt, which saw the country completely liberated during the reign of his son Ahmose I. Reign ...
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Ahmose (princess)
Ahmose (“Child of the Moon”) was a princess of the Seventeenth Dynasty of Egypt. She was the only known daughter of Seqenenre Tao (the Brave) by his sister-wife Sitdjehuti. She was the half-sister of Pharaoh Ahmose I and Queen Ahmose-Nefertari. Her titles are King's Daughter; King's Sister.Aidan Dodson & Dyan Hilton, The Complete Royal Families of Ancient Egypt, Thames & Hudson (2004) , p. 128 Tomb QV47 She was buried in the tomb QV47 in the Valley of the Queens. Her tomb is thought to be the first to be constructed in the Valley of the Queens. The tomb is fairly simple and consists of one chamber and a burial shaft. The tomb is located in a subsidiary valley named the Valley of Prince Ahmose. The mummy of Princess Ahmose was discovered by Ernesto Schiaparelli during his excavations from 1903 to 1905. Her mummy is now in the Egyptian Museum of Turin Turin ( , Piedmontese: ; it, Torino ) is a city and an important business and cultural centre in Northern Italy. It is the ...
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Halite
Halite (), commonly known as rock salt, is a type of salt, the mineral (natural) form of sodium chloride ( Na Cl). Halite forms isometric crystals. The mineral is typically colorless or white, but may also be light blue, dark blue, purple, pink, red, orange, yellow or gray depending on inclusion of other materials, impurities, and structural or isotopic abnormalities in the crystals. It commonly occurs with other evaporite deposit minerals such as several of the sulfates, halides, and borates. The name ''halite'' is derived from the Ancient Greek word for "salt", ἅλς (''háls''). Occurrence Halite dominantly occurs within sedimentary rocks where it has formed from the evaporation of seawater or salty lake water. Vast beds of sedimentary evaporite minerals, including halite, can result from the drying up of enclosed lakes and restricted seas. Such salt beds may be hundreds of meters thick and underlie broad areas. Halite occurs at the surface today in playas in regio ...
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Gypsum
Gypsum is a soft sulfate mineral composed of calcium sulfate dihydrate, with the chemical formula . It is widely mined and is used as a fertilizer and as the main constituent in many forms of plaster, blackboard or sidewalk chalk, and drywall. Alabaster, a fine-grained white or lightly tinted variety of gypsum, has been used for sculpture by many cultures including Ancient Egypt, Mesopotamia, Ancient Rome, the Byzantine Empire, and the Nottingham alabasters of Medieval England. Gypsum also crystallizes as translucent crystals of selenite. It forms as an evaporite mineral and as a hydration product of anhydrite. The Mohs scale of mineral hardness defines gypsum as hardness value 2 based on scratch hardness comparison. Etymology and history The word ''gypsum'' is derived from the Greek word (), "plaster". Because the quarries of the Montmartre district of Paris have long furnished burnt gypsum (calcined gypsum) used for various purposes, this dehydrated gypsum became known ...
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Anhydrite
Anhydrite, or anhydrous calcium sulfate, is a mineral with the chemical formula CaSO4. It is in the orthorhombic crystal system, with three directions of perfect cleavage parallel to the three planes of symmetry. It is not isomorphous with the orthorhombic barium ( baryte) and strontium ( celestine) sulfates, as might be expected from the chemical formulas. Distinctly developed crystals are somewhat rare, the mineral usually presenting the form of cleavage masses. The Mohs hardness is 3.5, and the specific gravity is 2.9. The color is white, sometimes greyish, bluish, or purple. On the best developed of the three cleavages, the lustre is pearly; on other surfaces it is glassy. When exposed to water, anhydrite readily transforms to the more commonly occurring gypsum, (CaSO4·2H2O) by the absorption of water. This transformation is reversible, with gypsum or calcium sulfate hemihydrate forming anhydrite by heating to around under normal atmospheric conditions. Anhydrite is comm ...
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Pleistocene
The Pleistocene ( , often referred to as the ''Ice age'') is the geological Epoch (geology), epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek grc, label=none, πλεῖστος, pleīstos, most and grc, label=none, καινός, kainós (latinized as ), 'new'. At the end of the preceding Pliocene, the previously isolated North and South American continents were joined by the Isthmus of Panama, causing Great American Interchang ...
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