The Grotta del col de la Stria is situated on the eastern flank of the Colli Berici at circa 370 m a.s.l.

The archaeological sequence is formed by five stratigraphic units: the upper ones (1 and 2) have a loam (loess) matrix with small glacial plates; the lower units (3, 4 and 5) are constituted by colluvial clays with rounded clastics. A bone from unit 3 gave a C14 dating of 30,304±330 years ago (LTL-798A).

There were no artefacts in the upper units. Sub-unit 3b contained several waste flakes from flint working, part of a production chain for making blades. The assemblage in the upper part of unit 4 comprised waste materials from the production chain making laminae and lamelle. To date no artefacts of greater significance have been recovered.
Amongst the fauna the predominant species is the cave bear, found in almost all assemblages. Fauna typical of a wooded environment with clearings ( Capreolus capreolus, Cervus elaphus, Megaloceros giganteum ) is present in the lower part of the deposit (units 3 and 4), whilst species from open areas ( Capra ibex, Bos/Bison ) are present in the upper parts (units 1 and 2). A hare’s tooth was found in sub-unit 3a. Fish and bird remains are abundant in all assemblages, unit 3b containing a high concentration. Butchery marks are only present on the bones from unit 4, in particular from the base of layer 4 t.I., from which also comes a fragment of marine shell ( Homalopoma sanguineum ).