The
Boxgrove site is one of the most important Lower Palaeolithic sites in Europe. At the time of its deposition around 480,000 years ago during the relatively warm
interglacial stage at the end of
Marine Isotope Stage 13, despite now being located inland, Boxgrove was located on the coast, evolving initially from coastal
mudflats beneath chalk cliffs of the
South Downs to a mosaic of terrestrial
woodland and
grassland habitats with freshwater bodies such as springs and ponds as the sea retreated. The area at the time of deposition had a
temperate climate similar to modern Britain. Many of the animals found at the Boxgrove site are still alive in Britain today, though others are more exotic, including elephants, rhinoceroses (
Stephanorhinus hundsheimensis), hyenas (
Crocuta), lions (
Panthera fossilis) and giant deer (
Praemegaceros). Alongside the remains of "Boxgrove Man", numerous stone tools, particularly
handaxes, have been found, created using flint nodules from the chalk cliffs immediately north of the site, which display a high level of refinement indicating that they were worked by extensively experienced knappers that both had a high level of cognitive capability and dexterity, using the advanced "
soft hammer" technique where flint is worked using bone and antler hammers, which represents the oldest evidence of "soft hammer" stone working in the world. Extensive evidence of animal butchery has also been found at the site. ==Comparative study==