Summary

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.
Source: Wikisource

John Magens Mello Quarterly Journal of the Geological Society of London (1877)

At about 120 feet from the door a small fissure was found opening out of Chamber A to the right, below the original level of the floor. As in the case of the fissure at the extremity of Chamber F in the Robin-Hood Cave, this was filled with red sand nearly but not quite in contact with the roof. The surface of the sand was also dry and powdery, and it was destitute of fossil contents. The digging has not been carried on beyond this point in Chamber A, the few remaining feet giving little promise of having any thing of sufficient value to repay the work of exploration.
Source: Wikisource

John Magens Mello Quarterly Journal of the Geological Society of London (1877)

The few remains found in the breccia consisted, as before, of bones of the Hare, a few teeth of the larger Pleistocene Mammalia (R. tichorhinus, Hyæna, Bear, and Horse) , together with fragmentary flint implements and a small piece of ruddle.
4. The Cave-Earth.—The succeeding deposit, that of cave-earth (3) , was very uniformly distributed throughout the cavern, although varying very considerably in thickness in different parts. Near to the entrance, as has been observed in a previous paper, it was very thin where the breccia attained its greatest development
Source: Wikisource

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