78-559: Tomb KV10 , located in the Valley of the Kings near the modern-day Egyptian city of Luxor , was cut and decorated for the burial of Pharaoh Amenmesse of the Nineteenth Dynasty of Ancient Egypt . However, there is no proof that he was actually buried here. Later, the decoration was replaced with scenes for Takhat and Baketwernel —two royal women dating to the late 20th Dynasty . It
156-407: A focus for Egyptologists and archaeological exploration since the end of the 18th century, and its tombs and burials continue to stimulate research and interest. The Valley of the Kings garnered significant attention following the discovery of the tomb of Tutankhamun in 1922, and is one of the most famous archaeological sites in the world. In 1979, it became a UNESCO World Heritage Site alongside
234-627: A further 16 tombs to the list, and explored several tombs that had already been discovered. During this time Georges Daressy explored KV9 . When Gaston Maspero was reappointed as head of the Egyptian Antiquities Service, the nature of the exploration of the valley changed again. Maspero appointed English archaeologist Howard Carter as the Chief Inspector of Upper Egypt, and the young man discovered several new tombs and explored several others, clearing KV42 and KV20 . Around
312-414: A hard, fissile, metamorphic rock known as slate . With continued increase in metamorphic grade the sequence is phyllite , then schist and finally gneiss . Shale is the most common source rock for hydrocarbons ( natural gas and petroleum ). The lack of coarse sediments in most shale beds reflects the absence of strong currents in the waters of the depositional basin. These might have oxygenated
390-742: A period of nearly 500 years from the Eighteenth Dynasty to the Twentieth Dynasty , rock-cut tombs were excavated for pharaohs and powerful nobles under the New Kingdom of ancient Egypt . It is a wadi sitting on the west bank of the Nile , opposite Thebes (modern-day Luxor ) and within the heart of the Theban Necropolis . There are two main sections: the East Valley, where the majority of
468-512: A relatively minor king, and other burials probably had more numerous treasures. In the same central area as KV62 and KV63, is "KV64" , a radar anomaly believed to be a tomb or chamber announced on 28 July 2006. It was not an official designation, and the actual existence of a tomb at all was dismissed by the Supreme Council of Antiquities , prior to finally excavating and describing it during 2011–2012. The nearby tomb of Horemheb , ( KV57 )
546-600: A systematic search, they discovered the actual tomb of Tutankhamun (KV62) in November 1922. Various expeditions have continued to explore the valley, adding greatly to the knowledge of the area. In 2001 the Theban Mapping Project designed new signs for the tombs, providing information and plans of the open tombs. A map of the Valley of the Kings with locations of tombs marked The earliest tombs were located in cliffs at
624-474: A thousand of them. The earliest positively dated graffiti dates to 278 BC. In 1799, members of Napoleon's expedition to Egypt (especially Vivant Denon ) drew maps and plans of the known tombs, and for the first time noted the Western Valley (where Prosper Jollois and Édouard de Villiers du Terrage located the tomb of Amenhotep III , WV22 ). The Description de l'Égypte contains two volumes (out of
702-533: A time when the Mediterranean Sea sometimes extended as far south as Aswan . During the Pleistocene the valley was carved out of the plateau by steady rains. There is now little year-round rain in this part of Egypt, but there are occasional flash floods . These floods dump tons of debris into the open tombs. The quality of the rock in the Valley is inconsistent, ranging from finely grained to coarse stone,
780-465: A total of 24) on the area around Thebes. European exploration continued in the area around Thebes during the nineteenth century. Early in the century, the area was visited by Giovanni Belzoni , working for Henry Salt , who discovered several tombs, including those of Ay in the West Valley ( WV23 ) in 1816 and Seti I ( KV17 ) the following year. At the end of his visits, Belzoni declared that all of
858-411: A total of 61 sepulchers being known by the start of the 20th century. KV5 was only rediscovered in the 1990s after being dismissed as unimportant by previous investigators. Some of the tombs are unoccupied, others remain unidentifiable as regards to their owners, and still others are merely pits used for storage. Most of the open tombs in the Valley of the Kings are located in the East Valley, and this
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#1733106528392936-579: Is a low-lying structure that has been particularly prone to the flash floods that sometimes hit the area. Tonnes of debris and material has washed in over the centuries, ultimately concealing its vast size. It is not currently open to the public. Shale Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g., kaolin , Al 2 Si 2 O 5 ( OH ) 4 ) and tiny fragments ( silt -sized particles) of other minerals, especially quartz and calcite . Shale
1014-402: Is a tomb commencement that is thought to have been started for Akhenaten , but it is no more than a gateway and a series of steps. The tomb of Ay , Tutankhamun 's successor is close by. It is likely that this tomb was started for Tutankhamun (its decoration is of a similar style), but later usurped for Ay's burial. This would mean that KV62 may have been Ay's original tomb, which would explain
1092-1201: Is accompanied by telogenesis , the third and final stage of diagenesis. As erosion reduces the depth of burial, renewed exposure to meteoric water produces additional changes to the shale, such as dissolution of some of the cement to produce secondary porosity . Pyrite may be oxidized to produce gypsum . Black shales are dark, as a result of being especially rich in unoxidized carbon . Common in some Paleozoic and Mesozoic strata , black shales were deposited in anoxic , reducing environments, such as in stagnant water columns. Some black shales contain abundant heavy metals such as molybdenum , uranium , vanadium , and zinc . The enriched values are of controversial origin, having been alternatively attributed to input from hydrothermal fluids during or after sedimentation or to slow accumulation from sea water over long periods of sedimentation. Fossils , animal tracks or burrows and even raindrop impressions are sometimes preserved on shale bedding surfaces. Shales may also contain concretions consisting of pyrite, apatite , or various carbonate minerals. Shales that are subject to heat and pressure of metamorphism alter into
1170-420: Is characterized by its tendency to split into thin layers ( laminae ) less than one centimeter in thickness. This property is called fissility . Shale is the most common sedimentary rock. The term shale is sometimes applied more broadly, as essentially a synonym for mudrock , rather than in the narrower sense of clay-rich fissile mudrock. Shale typically exhibits varying degrees of fissility. Because of
1248-638: Is composed of about 58% clay minerals, 28% quartz, 6% feldspar , 5% carbonate minerals, and 2% iron oxides . Most of the quartz is detrital (part of the original sediments that formed the shale) rather than authigenic (crystallized within the shale after deposition). Shales and other mudrocks contain roughly 95 percent of the organic matter in all sedimentary rocks. However, this amounts to less than one percent by mass in an average shale. Black shales, which form in anoxic conditions, contain reduced free carbon along with ferrous iron (Fe ) and sulfur (S ). Amorphous iron sulfide , along with carbon, produce
1326-430: Is evidence that shale acts as a semipermeable medium, allowing water to pass through while retaining dissolved salts. The fine particles that compose shale can remain suspended in water long after the larger particles of sand have been deposited. As a result, shales are typically deposited in very slow moving water and are often found in lakes and lagoonal deposits, in river deltas , on floodplains and offshore below
1404-416: Is little more than a truncated descending corridor and a burial chamber. However, KV16 has vibrant decoration and still contains the sarcophagus of the king. Its central location makes it one of the more frequently visited tombs. It shows the development of the tomb entrance and passage and of decoration. His son and successor, Seti I 's tomb KV17 (also known as Belzoni's tomb , the tomb of Apis , or
1482-455: Is more likely to form nonfissile mudstone than shale. On the other hand, black shales often have very pronounced fissility ( paper shales ) due to binding of hydrocarbon molecules to the faces of the clay particles, which weakens the binding between particles. Lithification follows closely on compaction, as increased temperatures at depth hasten deposition of cement that binds the grains together. Pressure solution contributes to cementing, as
1560-405: Is rarely open to visitors, but it has many unique features and is extensively decorated. The decoration shows a transition from the pre-Amarna tombs to those of the 19th dynasty tombs that followed. The Nineteenth Dynasty saw a further standardisation of tomb layout and decoration. The tomb of the first king of the dynasty, Ramesses I , was hurriedly finished due to the early death of the king and
1638-452: Is reduced. In addition to this physical compaction, chemical compaction may take place via pressure solution . Points of contact between grains are under the greatest strain, and the strained mineral is more soluble than the rest of the grain. As a result, the contact points are dissolved away, allowing the grains to come into closer contact. It is during compaction that shale develops its fissility, likely through mechanical compaction of
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#17331065283921716-401: Is vast in size, about the same length, and a larger area, of the tomb of his father. At the same time, and just opposite his own tomb, Ramesses enlarged the earlier small tomb of an unknown Eighteenth Dynasty noble ( KV5 ) for his numerous sons. With 120 known rooms, and excavation work still underway, it is probably the largest tomb in the valley. Originally opened (and robbed) in antiquity, it
1794-609: Is where most of the tourist facilities are located. The Eighteenth Dynasty tombs within the valley vary quite a bit in decoration, style, and location. It seems that at first there was no fixed plan. The tomb of Hatshepsut has a unique shape, twisting and turning down over 200 metres from the entrance, so that the burial chamber is 97 metres below the surface. The tombs gradually became more regular and formalised, and those of Thutmose III and Thutmose IV , KV34 and KV43 , are good examples of Eighteenth Dynasty tombs, both with their bent axis, and simple decoration. Perhaps
1872-559: The Book of the Heavens , which again describes the sun's journey through the twelve hours of night. Again from Seti I's time, the Litany of Re , a lengthy hymn to the sun god began to appear. Each burial was provided with equipment that would enable a comfortable existence in the afterlife . Also present in the tombs were items used to perform magic rituals, such as shabtis and divine figurines. Some of
1950-792: The Giza Plateau have come to symbolize ancient Egypt , the majority of tombs were cut into rock. Most pyramids and mastabas contain sections which were cut into ground level, and there are full rock-cut tombs in Egypt that date back to the Old Kingdom. After the defeat of the Hyksos and the reunification of Egypt under Ahmose I , the Theban rulers began to construct elaborate tombs that reflected their newfound power. The tombs of Ahmose I and his son Amenhotep I (their exact location remains unknown) were probably in
2028-471: The Seventeenth Dynasty necropolis of Dra' Abu el-Naga' . The first royal tombs in the Valley of the Kings were those of Amenhotep I (although this identification is also disputed), and Thutmose I , whose advisor, Ineni , notes in his tomb that he advised the king to place his tomb in the desolate valley (the identity of this actual tomb is unclear, but it is probably KV20 or KV38 ). I saw to
2106-462: The Turin Strike Papyrus . The valley has been a major focus of modern Egyptological exploration for the last two centuries. Prior to this time, it was a site for tourism in antiquity (especially during Roman times). The area illustrates the changes in the study of ancient Egypt, starting as antiquity hunting, and ending as scientific excavation of the whole Theban Necropolis . Despite
2184-399: The U.S. Gulf Coast . As sediments continue to accumulate, the older, more deeply buried sediments begin to undergo diagenesis . This mostly consists of compaction and lithification of the clay and silt particles. Early stages of diagenesis, described as eogenesis , take place at shallow depths (a few tens of meters) and are characterized by bioturbation and mineralogical changes in
2262-651: The wave base . Thick deposits of shale are found near ancient continental margins and foreland basins . Some of the most widespread shale formations were deposited by epicontinental seas . Black shales are common in Cretaceous strata on the margins of the Atlantic Ocean , where they were deposited in fault -bounded silled basins associated with the opening of the Atlantic during the breakup of Pangaea . These basins were anoxic, in part because of restricted circulation in
2340-569: The Ancient Egyptians as ta dehent , or "The Peak". It has a pyramid-shaped appearance, and it is probable that this echoed the pyramids of the Old Kingdom , more than a thousand years prior to the first royal burials carved here. Its isolated position also resulted in reduced access, and special tomb police (the Medjay ) were able to guard the necropolis. While the iconic pyramid complex of
2418-408: The Kings also contains the tombs of favorite nobles as well as the wives and children of both nobles and pharaohs. Therefore, only about twenty of the tombs actually contain the remains of kings. The remains of nobles and of the royal family, together with unmarked pits and embalming caches, make up the rest. Around the time of Ramesses I (ca. 1301 BC) construction commenced in the separate Valley of
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2496-668: The Queens . The official name for the site in ancient times was The Great and Majestic Necropolis of the Millions of Years of the Pharaoh, Life, Strength, Health in The West of Thebes (see below for the hieroglyphic spelling), or Ta-sekhet-ma'at (the Great Field). At the start of the Eighteenth Dynasty , only kings were buried within the valley in large tombs. When a non-royal person was buried, it
2574-416: The West Valley as WV1 through WV4. The tombs in the West Valley were later incorporated into the East Valley numbering system as WV22 through WV25 , and tombs that have been opened since Wilkinson's time have been added to the list. The numbers range from KV1 (Rameses VII) to KV64 (discovered in 2011). Since the early 19th century AD, antiquarians and archaeologists have cleared and recorded tombs, with
2652-421: The black coloration. Because amorphous iron sulfide gradually converts to pyrite , which is not an important pigment, young shales may be quite dark from their iron sulfide content, in spite of a modest carbon content (less than 1%), while a black color in an ancient shale indicates a high carbon content. Most shales are marine in origin, and the groundwater in shale formations is often highly saline . There
2730-404: The central area of the valley. This central area appears to have been flooded at the end of the Eighteenth Dynasty , with several tombs buried under metres of debris. The tombs KV55 , KV62 , and KV63 are dug into the actual wadi bedrock rather than the debris, showing that the level of the valley was five meters below its present level. After this event, later dynasties levelled the floor of
2808-506: The clumps of clay particles produced by flocculation vary in size from a few tens of microns to over 700 microns in diameter. The floccules start out water-rich, but much of the water is expelled from the floccules as the clay minerals bind more tightly together over time (a process called syneresis ). Clay pelletization by organisms that filter feed is important where flocculation is inhibited. Filter feeders produce an estimated 12 metric tons of clay pellets per square kilometer per year along
2886-408: The color of the rock. Red, brown and green colors are indicative of ferric oxide ( hematite – reds), iron hydroxide ( goethite – browns and limonite – yellow), or micaceous minerals ( chlorite , biotite and illite – greens). The color shifts from reddish to greenish as iron in the oxidized ( ferric ) state is converted to iron in the reduced ( ferrous ) state. Black shale results from
2964-619: The cultivation facing Thebes . These mortuary temples became places visited during the various festivals held in the Theban necropolis. Most notable is the Beautiful festival of the valley , where the sacred barques of Amun-Re , his consort, Mut , and son, Khonsu , left the temple at Karnak in order to visit the funerary temples of deceased kings on the West Bank and their shrines in the Theban Necropolis . The tombs were constructed and decorated by
3042-418: The descending path of the sun god into the underworld) to the burial chamber. In the earlier tombs, the corridors turn 90 degrees at least once (such as KV43 , the tomb of Thutmose IV ), and the earliest ones had cartouche -shaped burial chambers (for example, KV43 , the tomb of Thutmose IV ). This layout is known as "Bent Axis", After the burial, the upper corridors were meant to be filled with rubble and
3120-471: The entrance to the tomb hidden. After the Amarna Period , the layout gradually straightened, with an intermediate "Jogged Axis" (the tomb of Horemheb , KV57 is typical of this layout and is one of the tombs that is sometimes open to the public), to the generally "Straight Axis" of the late Nineteenth and Twentieth Dynasty tombs ( Ramesses III 's and Ramesses IX 's tombs, KV11 and KV6 respectively). As
3198-410: The excavation of the rock-tomb of his majesty, alone, no one seeing, no one hearing. The Valley was used for primary burials from approximately 1539 BC to 1075 BC. It contains at least 63 tombs , beginning with Thutmose I (or possibly earlier, during the reign of Amenhotep I) and ending with Ramesses X or XI , although non-royal burials continued in usurped tombs. Despite its name, the Valley of
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3276-536: The exploration and investigation noted below, only eleven of the tombs have actually been completely recorded. Many of the tombs have graffiti written by those ancient tourists. Jules Baillet has located over 2,100 Greek and Latin instances of graffiti, along with a smaller number in Phoenician , Cypriot , Lycian , Coptic , and other languages. The majority of the ancient graffiti is found in KV9, which contains just under
3354-412: The items may have been used by the king during his lifetime ( Tutankhamun 's sandals for example), and some were specially constructed for the burial. The modern abbreviation "KV" stands for "Kings' Valley". In 1827, Wilkinson painted KV numbers over the entrances to the 21 tombs that lay open in the East Valley at that time, beginning at the valley entrance and moving southward, and labeled four tombs in
3432-445: The latter with the potential to be structurally unsound. The occasional layer of shale also caused construction (and in modern times, conservation) difficulties, as this rock expands in the presence of water, forcing apart the stone surrounding it. It is thought that some tombs were altered in shape and size depending on the types of rock the builders encountered. Builders took advantage of available geological features when constructing
3510-592: The mineral dissolved from strained contact points is redeposited in the unstrained pore spaces. The clay minerals may be altered as well. For example, smectite is altered to illite at temperatures of about 55 to 200 °C (130 to 390 °F), releasing water in the process. Other alteration reactions include the alteration of smectite to chlorite and of kaolinite to illite at temperatures between 120 and 150 °C (250 and 300 °F). Because of these reactions, illite composes 80% of Precambrian shales, versus about 25% of young shales. Unroofing of buried shale
3588-414: The modern surface, the Valley's cliffs descend beneath the scree in a series of abrupt, natural "shelves", arranged one below the other, descending several metres to the bedrock in the valley floor. The area of the Theban hills is subject to infrequent, violent thunderstorms causing flash floods in the valley. Recent studies have shown that there are at least seven active flood stream beds leading down into
3666-411: The most imposing tomb of this period is that of Amenhotep III , WV22 , located in the West Valley. It was re-investigated in the 1990s by a team from Waseda University , Japan , but it is not open to the public. At the same time, powerful and influential nobles began to be buried with the royal family; the most famous of these tombs is the joint tomb of Yuya and Tjuyu , KV46 . They were possibly
3744-433: The narrow Atlantic, and in part because the very warm Cretaceous seas lacked the circulation of cold bottom water that oxygenates the deep oceans today. Most clay must be deposited as aggregates and floccules, since the settling rate of individual clay particles is extremely slow. Flocculation is very rapid once the clay encounters highly saline sea water. Whereas individual clay particles are less than 4 microns in size,
3822-415: The original open framework of clay particles. The particles become strongly oriented into parallel layers that give the shale its distinctive fabric. Fissility likely develops early in the compaction process, at relatively shallow depth, since fissility does not seem to vary with depth in thick formations. Kaolinite flakes have less tendency to align in parallel layers than other clays, so kaolinite-rich clay
3900-631: The parallel orientation of clay mineral flakes in shale, it breaks into thin layers, often splintery and usually parallel to the otherwise indistinguishable bedding planes . Non-fissile rocks of similar composition and particle size (less than 0.0625 mm) are described as mudstones (1/3 to 2/3 silt particles) or claystones (less than 1/3 silt). Rocks with similar particle sizes but with less clay (greater than 2/3 silt) and therefore grittier are siltstones . Shales are typically gray in color and are composed of clay minerals and quartz grains. The addition of variable amounts of minor constituents alters
3978-410: The parents of Queen Tiy . Until the discovery of the tomb of Tutankhamun, this was the best-preserved of the tombs that had been discovered in the Valley. The return of royal burials to Thebes after the end of the Amarna Period marks a change to the layout of royal burials, with the intermediate 'jogged axis' gradually giving way to the 'straight axis' of later dynasties. In the Western Valley, there
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#17331065283924056-817: The presence of greater than one percent carbonaceous material and indicates a reducing environment. Pale blue to blue-green shales typically are rich in carbonate minerals . Clays are the major constituent of shales and other mudrocks. The clay minerals represented are largely kaolinite , montmorillonite and illite. Clay minerals of Late Tertiary mudstones are expandable smectites , whereas in older rocks (especially in mid-to early Paleozoic shales) illites predominate. The transformation of smectite to illite produces silica , sodium , calcium , magnesium , iron and water. These released elements form authigenic quartz , chert , calcite , dolomite , ankerite , hematite and albite , all trace to minor (except quartz) minerals found in shales and other mudrocks. A typical shale
4134-507: The rest of the Theban Necropolis. Exploration, excavation, and conservation continues in the area and a new tourist centre has recently been opened. The Valley of the Kings is situated over 1,000 feet of limestone and other sedimentary rock, which form the cliffs in the valley and the nearby Deir el-Bahari , interspersed with soft layers of marl . The sedimentary rock was originally deposited between 35 and 56 million years ago during
4212-444: The richest source rocks may contain as much as 40% organic matter. The organic matter in shale is converted over time from the original proteins, polysaccharides , lipids , and other organic molecules to kerogen , which at the higher temperatures found at greater depths of burial is further converted to graphite and petroleum. Before the mid-19th century, the terms slate , shale and schist were not sharply distinguished. In
4290-565: The royal necropolis. The Nineteenth and Twentieth Dynasties saw an increase in the number of burials (both here and in the Valley of the Queens), with Ramesses II and later Ramesses III each constructing a massive tomb used for the burial of their sons ( KV5 and KV3 respectively). There are some kings that are not buried within the valley or whose tomb has not been located: Thutmose II may have been buried in Dra' Abu el-Naga' (although his mummy
4368-468: The royal tombs are situated; and the West Valley, otherwise known as the Valley of the Monkeys. With the 2005 discovery of a new chamber and the 2008 discovery of two further tomb entrances, the Valley of the Kings is known to contain 65 tombs and chambers, ranging in size from the simple pit that is KV54 to the complex tomb that is KV5 , which alone has over 120 chambers for the sons of Ramesses II . It
4446-433: The sediments, with only slight compaction. Pyrite may be formed in anoxic mud at this stage of diagenesis. Deeper burial is accompanied by mesogenesis , during which most of the compaction and lithification takes place. As the sediments come under increasing pressure from overlying sediments, sediment grains move into more compact arrangements, ductile grains (such as clay mineral grains) are deformed, and pore space
4524-420: The smaller size and unusual layout for a royal tomb. The other Amarna Period tombs are located in a smaller, central area in the centre of the East Valley, with a possible mummy cache ( KV55 ) that may contain the burials of several Amarna Period royals – Tiy and Smenkhkare or Akhenaten . In close proximity is the burial of Tutankhamun, perhaps the most famous discovery of modern Western archaeology . It
4602-477: The start of the 20th century, American explorer Theodore M. Davis held the excavation permit for the valley. His team (led mostly by Edward R. Ayrton ) discovered several royal and non-royal tombs (including KV43 , KV46 and KV57 ). In 1907, they discovered the possible Amarna Period cache in KV55. After finding what they thought was all that remained of the burial of Tutankhamun (items recovered from KV54 and KV58), it
4680-472: The sun god passing through the twelve gates that divide the nighttime and ensures the tomb owner's own safe passage through the night. These earliest tombs were generally sparsely decorated, and those of a non-royal nature were totally undecorated. Late in the Nineteenth Dynasty the Book of Caverns , which divided the underworld into massive caverns containing deities as well as the deceased waiting for
4758-489: The sun to pass through and restore them to life, was placed in the upper parts of tombs. A complete version appears in the tomb of Ramesses VI. The burial of Ramesses III saw the Book of the Earth , where the underworld is divided into four sections, climaxing in the sun disc being pulled from the earth by Naunet . The ceilings of the burial chambers were decorated (from the burial of Seti I onwards) with what became formalised as
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#17331065283924836-542: The tomb of Twosret , KV14 . When looking for a tomb, Ramesses III extended the partly excavated tomb started by his father. The tomb of Ramesses II returned to an early style, with a bent axis, probably due to the quality of the rock being excavated (following the Esna shale). Between 1998 and 2002, the Amarna Royal Tombs Project investigated the valley floor using ground-penetrating radar and found that, below
4914-508: The tomb of Psammis, son of Necho ), is usually regarded as the finest tomb in the valley. It has extensive relief work and paintings. When it was rediscovered by Belzoni in 1817, he referred to it as "a fortunate day." The son of Seti, Ramesses II (Ramesses the Great), constructed a massive tomb, KV7 , but it is in a ruinous state. It is currently undergoing excavation and conservation by a Franco-Egyptian team led by Christian Leblanc . The tomb
4992-486: The tombs had been located and nothing of note remained to be found. Working at the same time was Bernardino Drovetti , the French Consul-General and a great rival of Belzoni and Salt. John Gardner Wilkinson , who lived in Egypt from 1821 to 1832, copied many of the inscriptions and artwork in the tombs that were open at the time. The decipherment of hieroglyphs , though still incomplete during Wilkinson's stay in
5070-414: The tombs' axes straightened, the slopes also lessened. They almost disappeared in the late Twentieth Dynasty. Another feature that is common to most tombs is the "well", which may have originated as an actual barrier intended to stop flood waters from entering the lower parts of the tomb. It seems to have developed a "magical" purpose later as a symbolic shaft. In the later Twentieth Dynasty, the well itself
5148-433: The tombs. Some tombs were quarried out of existing limestone clefts, others behind slopes of scree , and some were at the edge of rock spurs created by ancient flood channels. The problems of tomb construction can be seen with the tombs of Ramesses III and his father Setnakhte . Setnakhte started to excavate KV11 but unintentionally broke into the tomb of Amenmesse , so construction was abandoned and he instead usurped
5226-436: The top of scree slopes, under storm-fed waterfalls ( KV34 and KV43 ). As these locations were filled, burials descended to the valley floor, gradually moving back up the slopes as the valley bottom filled with debris. This explains the location of the tombs KV62 and KV63 buried in the valley floor. The usual tomb plan consisted of a long inclined rock-cut corridor, descending through one or more halls (possibly mirroring
5304-559: The valley, enabled him to assemble a chronology of New Kingdom rulers based on the inscriptions in the tombs. He also established the system of tomb numbering that has been in use, with additions, ever since. The second half of the century saw a more concerted effort to preserve, rather than simply gather, antiquities. Auguste Mariette 's Egyptian Antiquities Service started to explore the valley, first with Eugène Lefébure in 1883, then Jules Baillet and Georges Bénédite in early 1888, and finally Victor Loret in 1898 to 1899. Loret added
5382-473: The valley, making the floods deposit their load further down the valley, and the buried tombs were forgotten and only discovered in the early 20th century. This was the area that was the subject of the Amarna Royal Tombs Project ground-scanning radar investigation, which showed several anomalies, one of which was proved to be KV63. The Theban Hills are dominated by the peak of al-Qurn , known to
5460-414: The waters and destroyed organic matter before it could accumulate. The absence of carbonate rock in shale beds reflects the absence of organisms that might have secreted carbonate skeletons, also likely due to an anoxic environment. As a result, about 95% of organic matter in sedimentary rocks is found in shales and other mudrocks. Individual shale beds typically have an organic matter content of about 1%, but
5538-426: The workers of the village of Deir el-Medina , located in a small wadi between this valley and the Valley of the Queens , facing Thebes . The workers journeyed to the tombs through various routes over the Theban hills. The daily lives of these workers are quite well known due to their being recorded in tombs and official documents. Amongst the events documented is perhaps the first recorded workers' strike, detailed in
5616-400: Was announced that the valley was completely explored and that no further burials were to be found. Davis's 1912 publication, The Tombs of Harmhabi and Touatânkhamanou closes with the comment, "I fear that the Valley of Kings is now exhausted." After Davis's death early in 1915, Lord Carnarvon acquired the concession to excavate the valley, and he employed Howard Carter to explore it. After
5694-401: Was discovered by Howard Carter on 4 November 1922, with clearance and conservation work continuing until 1932. This was the first royal tomb to be discovered that was still largely intact, although tomb robbers had entered. Until the excavation of KV63 on 10 March 2005, it was considered the last major discovery in the valley. The opulence of his grave goods notwithstanding, Tutankhamun was
5772-472: Was in a small rock cut chamber, close to the tomb of their master. Amenhotep III 's tomb was constructed in the Western Valley, and while his son Akhenaten moved his tomb's construction to Amarna , it is thought that the unfinished WV25 may have originally been intended for him. With the return to religious orthodoxy at the end of the Eighteenth Dynasty, Tutankhamun , Ay , and Horemheb returned to
5850-512: Was in the Deir el-Bahari tomb cache ), Smenkhkare's burial has never been located, and Ramesses VIII seems to have been buried elsewhere. In the Pyramid Age , the pyramid tomb of a king was associated with a mortuary temple located close to the pyramid. Since the tombs of the kings in the Valley of the Kings were hidden, the kings' mortuary temples were located away from their burial sites, closer to
5928-482: Was sometimes not excavated (by the builders), but the well room was still present. The majority of the royal tombs were decorated with religious texts and images. The early tombs were decorated with scenes from Amduat ('That Which is in the Underworld'), which describes the journey of the sun god through the twelve hours of the night. From the time of Horemheb, tombs were decorated with the Book of Gates , which shows
6006-497: Was the principal burial place for the New Kingdom's major royal figures as well as a number of privileged nobles. The royal tombs are decorated with traditional scenes from Egyptian mythology and reveal clues to the period's funerary practices and afterlife beliefs . Almost all of the tombs seem to have been opened and robbed in antiquity, but they still give an idea of the opulence and power of Egypt's pharaohs. This area has been
6084-668: Was visited by Richard Pococke , Jean-François Champollion and Karl Richard Lepsius , and briefly studied by Edward R. Ayrton before being properly examined by a team from the University of Memphis in the United States under Otto Schaden in 1992. Valley of the Kings The Valley of the Kings , also known as the Valley of the Gates of the Kings , is an area in Egypt where, for
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