John Magens Mello, Quarterly Journal of the Geological Society of London (1877)
“ At a depth of 3 feet, the unproductive white calcareous sand with limestone blocks forming the lowest bed in the interior was met with; above this was a deposit of cave- earth, 1 foot thick, in which, near the mouth of the cavern, were a few flint chips, a fragment or two of worked flakes, and a few teeth and a portion of the jaw of Cervus megaceros, together with two or three teeth of Hyæna and Rhinoceros tichorhinus. Over the cave-earth was an old floor full of bits of charcoal, with pieces of coarse Roman earthenware in the lower part, and with more modern remains at the top. ”
