472 MR. A. C. SAVIN ON RECENT EXPOSURES OF THE FOREST-BED. 
opposite the old church, during the present winter I have found a 
canine of Hippopotamus, second milk molar of E. antiquus, Cervus 
jaw, metatarsal of Canis vulpes, upper and lower molars of Equus, 
astragalus of Ehinoceros, various limb bones of Cervus and Equus, 
and a frontal with one horn-core of Bison. This specimen is now in 
the hands of Mr. E. T. Newton for indentification. 
Turning now to the north side of Cromer, several good exposures 
have been noted about half way to East Runton, many cakes of 
peat and a few stools of trees in the same condition as those at 
Overstrand, all the roots broken short. It is remarkable that no 
bones are found in this section. I have explored here for 
years, but never discovered any remains of animals. Travelling 
onward in the direction of East Runton, the bed of “ Pan ” is 
reached from whence the large tusk was obtained. This deposit was 
Avell shown a short time back, in many places being quite 6 feet in 
thickness, resting on finely laminated clays. Very few bones occur 
in the above bed, and those in a fragmentary condition, and very 
difficult to extract. Midway between the last-mentioned deposit 
and the gangway large patches of pan were seen on the foreshore, 
chiefly composed of sand, and not so hard as that forming the base 
of the cliff. The fossils obtained from this section are : - A fine upper 
molar of E. antiquus, the plates just coming into wear; a foot bone 
of Elephas, metatarsal of Cervus, and a fine frontal with the 
left antler complete of C. hovides ( Alces latifrons, Dawkins^. This 
is an interesting specimen of the above rare species : the great 
thickness of the frontal, the extreme shortness of the pedicle, and 
total absence of tines, separates it from all other known forms. I 
possess several good specimens of this species, but the last found 
has a greater ogee curvature than any of the others. Many curious 
red sandy concretions occur near the gangway: they are about 1^ 
inches in thickness and from 2 to 8 feet in length, and quite hollow, 
resembling the trunks of trees. Immediately on the north-west 
side of the gap a ledge of rocks run out to sea at right angles to tlie 
coast, and after storms, when the flints have been disturbed, forms 
a good collecting ground. When the Forest-bed is denuded the 
Weybourn Crag is given to view, and large quantities of shells can 
be procured. Several colonies of Gyprina islandica, Astarte borea- 
lis, Tellina halthica and ohliqiia, &c., were found. The first 
mentioned are difficult to extract whole. Many bones of Platax 
