[1] This area illustrates the changes in the study of ancient Egypt, beginning as antiquity hunting and ending with the scientific excavation of the whole Theban Necropolis.
Jules Baillet located over 2100 Greek and Latin graffiti, along with a smaller number in Phoenician, Cypriot, Lycian, Coptic, and other languages.
Early in the century, the area was visited by 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 next year.
[8] In 1827, John Gardiner Wilkinson was assigned to paint the entry of every tomb, giving them each a designation that is still in use today—they were numbered from KV1 to KV21, with KV standing for King's Valley, (although the maps show 28 entrances, some of which were unexplored).
Auguste Mariette's Egyptian Antiquities Service started to explore the valley, first with Eugène Lefébure in 1883,[12] then Jules Baillet and Georges Bénédite in early 1888, and finally Victor Loret in 1898 to 1899.
[14] When Gaston Maspero was reappointed to head the Egyptian Antiquities Service, the nature of the exploration of the valley changed again.
Maspero appointed 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.
[15] Around the turn of the 20th century, the American Theodore M. Davis had the excavation permit in the valley, and his team (led mostly by Edward R. Ayrton) discovered several royal and non-royal tombs (including KV43, KV46 and KV57).
"[16] After Davis's death early in 1915 Lord Carnarvon acquired the concession to excavate the valley and he employed Carter to explore it.
[17] At the end of the century, the Theban Mapping Project re-discovered and explored tomb KV5, which has since been discovered to be probably the largest in the valley (having at least 120 rooms) and was the burial for the sons of Ramesses II.
[20] On July 31, 2006, Nicholas Reeves announced that analysis of ground penetrating radar for the autumn of 2000 showed a sub-surface anomaly in the area of KV62 and KV63.