Valley of the Kings

The Valley of the Kings (Arabic: وادي الملوك Wadi Biban el-Muluk‎; "Gates of the King") is a valley in Egypt where, for a period of nearly 500 years from the 16th to 11th century BC, tombs were constructed for the kings and powerful nobles of the New Kingdom (the Eighteenth through Twentieth Dynasties of Ancient Egypt). The valley stands on the west bank of the Nile, across from Thebes (modern Luxor), within the heart of the Theban Necropolis. The wadi consists of two valleys, East Valley (where the majority of the royal tombs situated) and West Valley.

With the 2005 discovery of a new chamber, and the 2008 discovery of 2 further tomb entrances, the valley is known to contain 62 tombs and chambers (ranging in size from a simple pit to a complex tomb with over 120 chambers), and was the principal burial place of the major royal figures of the Egyptian New Kingdom, together with those of a number of privileged nobles. The royal tombs are decorated with scenes from Egyptian mythology and give clues to the beliefs and funerary rituals of the period. 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 the rulers of this time.

The area has been a focus of concentrated archaeological and egyptological exploration since the end of the eighteenth century, and its tombs and burials continue to stimulate research and interest. In modern times the valley has become famous for the discovery of the tomb of Tutankhamun (with its rumours of the Curse of the Pharaohs), and is one of the most famous archaeological sites in the world. In 1979, it became a World Heritage Site, along with the rest of the Theban Necropolis. Exploration, excavation and conservation continues in the valley, and a new tourist centre has recently been opened.

Geology

The types of soil where the Valley of Kings is located are an alternating sandwich of dense limestone and other sedimentary rock (which form the cliffs in the valley and the nearby Deir el-Bahri) and soft layers of marl. The sedimentary rock was originally deposited between 35–56 million years ago during a time when the precursor to the Mediterranean Sea covered an area that extended much further inland than today. During the Pleistocene the valley was carved out of the plateau by steady rains. There is currently little year-round rain in this part of Egypt, but there are occasional flash floods that hit the valley, dumping tons of debris into the open tombs.

The quality of the rock in the Valley is inconsistent, ranging from finely-grained to coarse stone, the latter with the potential to be structurally unsound. The occasional layer of shale also caused construction and 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 the layers of rock the builders encountered.

Builders took advantage of available geological features when constructing the tombs. Some tombs were quarried out of existing limestone clefts, others behind slopes of scree, or were at the edge of rock spurs created by ancient flood channels.

The problems of tomb construction can be seen with tombs of Ramesses III and his father Setnakhte. Setnakhte started to excavate KV11 but broke into the tomb of Amenmesse, so construction was abandoned and he instead usurped the tomb of Twosret, KV14. When looking for a tomb, Ramesses III extended the part-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 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 down to the bedrock in the valley floor.

History

The Theban Hills are dominated by the peak of al-Qurn, known to 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 complexes of the Giza plateau have come to symbolize ancient Egypt, the majority of tombs were cut into rock. Most pyramids and mastabas contain sections which are 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 would reflect their new found power. The tombs of Ahmose and his son Amenhotep I (their exact location remains unknown) were probably in the Seventeenth Dynasty necropolis of Dra' Abu el-Naga'. The first royal tombs in the valley were those of Amenhotep I (although this identification is also disputed), and Thutmose I, whose advisor Ineni notes in his tomb that he advised his 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 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, and 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 the name, the Valley of the Kings also contains the tombs of favorite nobles as well as the wives and children of both nobles and pharaohs. Around the time of Ramesses I (ca. 1301 BC) construction commenced in the separate Valley of the Queens.

--> Royal Necropolis

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