The site was abandoned until 1966 when Jean Combier undertook modern, systematic excavations in areas left intact by earlier trenches which continued until 1976.
The excavations pursued a double objectives . First, redefine and date the successive layers of occupations and establish their environmental context. And second, open an areas large enough to expose the remains and study their distribution to recreate the range of activities practiced at the site by its Paleolithic occupants. The latter goal was achieved with the systematic excavation of a 100 m2 block ofhe Magdalenian layers in P16. Series of test pits provided the kind of stratigraphic data required to fulfill the first objective.
A deep test pit in the area known to contain a deep sequence of deposits in Unit I11was opened in 1986 with the participation of B. Kervaso to complete the geological study of the site.
More recently (1997 and 1998) excavations undertaken in collaboration with the University of Kansas with the participation of J. Hofman and A. Montet-White reopened the I11 test pit and then concentrated on the early Upper Paleolithic components (Aurignacian in Unit M12 and Gravettian in Unit J10).
M Magdalenian
S Solutrean
G Gravettian
A Aurignacian
Mn Mousterian
Some 4000 years separate the Solutrean from the earliest Magdalenian occupation found in unit P16. An slmost 8000 year long gap separates the Solutrean from the Gravettian. There is a greater degree of continuity between the Aurignacian and the Gravettian. A long hiatus (20000 years separate theMousterian layers from the Aurignacian.