An assemblage of quartzite cobbles with attributes of cultural flaking and
utilization has been recorded at the base of a Laurentide till at the conta
ct with underlying fluvial gravels in a section face of a gravel pit near G
rimshaw in the course of Quaternary geology mapping of the Peace River area
. The geological context, with secondarily redeposited stone artifacts, doc
uments distortion of an early prehistoric site located in a nonglacial rive
rine setting by the expanding Late Wisconsinan continental ice from the nor
th. The lithic assemblage provides further evidence for an earlier (pre-las
t glacial) occupation of North America, predating the earliest postglacial
(<11 500 BP) Palaeoindian cultures, traditionally regarded as the hallmark
of peopling of the New World.