valley of the kings
Wādī Abwāb al Mulūk), is a valley in Egypt where, for a period of nearly 500 years from the 16th to 11th century BC, rock cut tombs were excavated for the pharaohs and powerful nobles of the New Kingdom (the Eighteenth to the Twentieth Dynasties of Ancient Egypt).
The valley stands on the west bank of the Nile, opposite 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 are situated) and West Valley.
With the 2005 discovery of a new chamber and the 2008 discovery of two further tomb entrances, the valley is known to contain 63 tombs and chambers (ranging in size from KV54, a simple pit, to KV5, a complex tomb with over 120 chambers). It was the principal burial place of the major royal figures of the Egyptian New Kingdom, as well as a number of privileged nobles. The royal tombs are decorated with scenes from Egyptian mythology and give clues as to the beliefs and funerary rituals of the period. 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 the pharaohs.
This area has been a focus of 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
Stratigraphy of the valley
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-Bahri, interspersed with soft layers of marl. The sedimentary rock was originally deposited between 35–56 million years ago during 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 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 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 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 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 reflected their newfound power. The tombs of Ahmose and his son Amenhotep I (their exact location remains unknown) were probably in the Seventeenth Dynastynecropolis 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 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)
