with the evidence found at Coro Trasito and Els Trocs. These two sites, of which
the second is paradigmatic, are in the Pyrenees in Huesca, in Sobrarbe and the
Benasque Valley (Ribagorza), respectively. The first is a west-facing entrance of a
cave filled with Holocene sediments at 1548 m a.s.l. It is now a large rock-shelter
Fig. 4.6 General image of the Cova del Sardo. Above, at the time of its location in 2004. Bottom,
in the final phase of its excavation, with the bare levels of the 5th Millennium cal BC outside the
cavity
90
E. Gassiot Ballbè et al.
the second is paradigmatic, are in the Pyrenees in Huesca, in Sobrarbe and the
Benasque Valley (Ribagorza), respectively. The first is a west-facing entrance of a
cave filled with Holocene sediments at 1548 m a.s.l. It is now a large rock-shelter
Fig. 4.6 General image of the Cova del Sardo. Above, at the time of its location in 2004. Bottom,
in the final phase of its excavation, with the bare levels of the 5th Millennium cal BC outside the
cavity
90
E. Gassiot Ballbè et al.