The site is the remnant of a
solutional cave filled with of deposits from the
Pleistocene era, located on the eastern side of a
karstic outcrop of
limestone at an elevation of . It was discovered in 1961 when the area was being mined for the mineral
baryte. A miner discovered a skull in the wall of the cave, extracted it, and gave it to an engineer, who kept it as a souvenir for a time. Eventually, it was handed over to the
University of Rabat, which organized a joint French-Moroccan expedition to the site that was headed by anthropologist
Émile Ennouchi.
Excavation history Ennouchi and his team began their excavation of Jebel Irhoud in 1961. Before beginning excavation, Ennouchi's team removed 2000 tons of debris that covered the archaeological layers using low-level explosives. The excavation completed by Ennouchi's team used horizontal arbitrary 50 cm stratigraphic layers, or spits. These excavations continued the work of the 1960s excavations, performing a more detailed study of site stratigraphy and context. This event occurred between 310 and 280 Ma and created westward
vergent folds. Three primary geological formation contributing to the Jebel Irhoud landscape: (1)
Barite veins, (2) zones of barite or "substitution," and (3)
karst deposits. == Dating ==