HELIX NEMORALIS, 285 
In the Isle of Wight, it is recorded by Prof. Forbes from the lacustrine 
beds at ‘l'otlands Bay; by Bristow from subaérial beds on St. Catherine’s 
Down; by Mr. C. Ashford from a shell-layer about twenty inches beneath 
the surface, disclosed by the cutting of m yath dewn the cliffs at Orchard 
Bay ; and by Kennard and Warren from a bed of ileareous tufa, overlying 
the Potumomya sands and eight to ten feet bel. w the top of the cliff, a 
little south-west of Widdick Chine. “N07 
In Hants. 8., it is recorded by Mr. J. 'T. Kemp as common in tufa on 
site of Southamptien Docks ; also in the Test Valley at Mottisfont, and the 
Itchen Valley near *Yinchester. 
In Sussex W., it was enumerated by Mr. Alfred Bell in 1871 as amongst 
the mollusks found in the “ mud deposit.” : y Selsey ; and Mr. R. M. Christy 
found specimens 'in 1878 beneath the loos”, earth filling up the pits in the 
ancient Roman camp at Cissbury. In “ast Sussex, Mr. J. P. Johnson 
found it near the base of a Neolithic chalky rainwash, overlying the Palzeo- 
lithic rubble drift, to the east of Brighton. 
In East Kent, the Rev. R. Ashington Bullen found specimens at a depth 
of four to six feet in a section exposed by the cutting of a road under the 
South Downs. In West Kent, Mr. A. Santer Kennard found it abundantly 
with bone fragments and Roman pottery at the base of a rain-wash, from 
two to six feet thick, on the site of a large Roman building at Darenth, 
and commonly at base of tumulus, Stanley’s Quarry, [ghtham; Mr. F. C. J. 
Spurrell in ditches, Erith Marshes, and in the sections exposed by the 
excavations for sewer outfall at Crossness; and the vy. R. A. Bullen from 
deposit overlying the head or rubble drift at Bartcn Ci art, Buckland, Dover. 
In Surrey, it is recorded by Kennard and Warren from the carbonaceous 
silt of Roman age, disclosed by the excavations 1; Tooley street, Ber- 
mondsey ; by Mr. C. Evans from the excavations for the Charing Cross 
railway in Blackfriars; by Rev. R. Ashington Bullen at depths varying 
from eighteen inches to three feet in a mixture of Upper Chalk and Upper 
Greensand, in the Upper Greensand pit, east of the *\orseshoe pit, Reigate ; 
and by Mr. L. E. Adams as moderately common in “he same district from 
an old chalk-pit, the Horse-Shoe pit, and from a section at Betchworth. 
In South Essex, it is recorded by Kennard and Woodward as very 
common in the beds of loamy clay, sand, and shell-marl disclosed during 
the excavations for reservoirs at Walthamstow; and Dr. Frank Corner 
found it in layers, alternating with mud and peat, during the sewer 
excavation between Canning T'own and Stratford. In North Essex, Mr. 
Miller Christy has found the species abundantly in the black earth and 
peat beds along the banks of the river Cann, Chignal St. James; and 
Mr. J. French has recorded it from the shell marl at Felstead. Dr. S. P. 
Woodward has reported it from the post-glacial beds at Witham; Rev. 
A. J. Law from a drain-section at a depth of 3-3 feet in ‘the Marsh,” 
near Shalford Vicarage ; and Mr. R. W. Christy from alluvium exposed by 
the draining of a field on Duke’s Farm, Roxwell. 
In Herts., Mr. J. Hopkinson has recorded it from the alluvium disclosed 
by the excavations for the gas-works at Watford; and Mr. Fordham obtained 
specimens from the sub-soil of a tumulus at Highley Hill, Ashwell. 
In Middlesex, Mr. J. E. Cooper has found specimens with other species 
in the excavations near the gas-works, Staines; and Kennard and Warren 
found a single shell in a marl-bed on left bank of river Thames by the 
