Troy lies in north-west *Asia Minor 5 km. from the *Hellespont. The site consists of a mound with c. 25 m. of deposits and a 1 km. sq. skirt to the south. It was noted by F. Kauffer (1793), identified as classical Ilion by E. D. Clarke (1810) and as Homeric Troy by C. Maclaren (1820). Soundings by Frank Calvert (1863, 1865) revealed prehistoric strata. H. Schliemann excavated much of the mound (1870–90), further excavations being by W. Dörpfeld (1893–94), C. W. Blegen (1932–38), M. O. Korfmann (1988–2006) with C. B. Rose, and since 2006 by E. Pernicka.The site was occupied from c. 2900 bce to the 6th cent. ce. The numerous phases are conventionally, but variously, grouped into nine bands. As now defined, I–III (from c. 2900 bce) represent the early bronze age, IV–V (from c.