3 
MAMMALIAN REMAINS. 
The mammalian bones exhibited in Cases A 3, B i to s, C i, 
and 3, and E i, are, with few exceptions, from the brick-fields 
at Fisherton, about a mile to the west of Salisbury. The clay 
from which they were obtained belongs to that division of the 
tertiary formations known as the Mammaliafi drift or Pleistoceiie. 
A 2. 
Contains a series of lower molar teeth of cave lion {Felis spelcBo), 
from the brick-earth of Menchecourt, in the valley of the Somme^ 
France. 
Portions of the lower tusks of hippopotamus {^Hippopotamus 
major), from the drift of Sussex and Bedford. 
Upper and lower molar teeth of Rhinoceros tichorhinus, from 
Sherborne (Dorset) ; Bath ; Erith (Kent) ; and Bedford. 
One lower and part of upper molar of Elephas meridionalis, 
from Dewlish, Dorset. 
Lower molar teeth of Elephas antiqtms, from the forest bed at 
Cromer, Bedford. 
Also upper and lower molar teeth and portions of tusks of 
Mammoth {Elephas primigenius), from Bedford ; Ashford, near 
Fordingbridge ; Wishford, near Salisbury; Cambridge; and the 
''Elephant bed" of the late Dr. Mantell, on the coast, near 
Brighton. 
A 3- 
All the fossils in this Case are from Fisherton Anger, near 
Salisbury, and consist of — 
Two lower molar teeth of wolf {Canis lupus). 
Portion of humerus and lower jaw containing teeth of fox 
{Canis vulpes). 
A perfect series of upper molar teeth of reindeer {Cervus 
tarandus), belonging to an old animal. 
Both upper and lower molar teeth of Rhinoceros tichorhinus, 
showing different stages of wear. 
Molar teeth of mammoth {Elephas primigenius), including three 
examples of the old worn-down or used-out molars, also a fine 
lower molar from the lower level gravel of South Burcombe, near 
Fisherton. The fragment of tusk illustrates its formation of 
hollow cones, one fitting within the other. This arrangement is 
produced by the hardening of the cement-forming capsule. 
v> 2 
