Join me as I explore the Valley of the Kings in Luxor, Egypt, but with 65 tombs to choose from and entry included in to only three of them! Which ones will I choose?
The Valley of the Kings (Egyptian Arabic: وادى الملوك Wādī el-Mulūk; Coptic: ϫⲏⲙⲉ Džēme [ˈʃɪ.mæ]), also known as the Valley of the Gates of the Kings (وادى ابواب الملوك Wādī Ebwāb el-Mulūk), is an area in Egypt where, for 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 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 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 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 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 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, 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 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 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 to the bedrock in the valley floor.
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