HYALINIA FULVA. 121 
Geological Distribution.— Pi.nisrocenr.—In South Wilts., it is hsted 
by Mr. Kennard from the fluviatile deposits at Fisherton, near Salisbury. 
In West Sussex, according to Mr. J. P. Johnson, it is present in the 
buried river-bed deposit on the foreshore at West Wittering. 
In West Kent, it is enumerated among the list of fossils from the 
Ightham fissure by Mr. W. J. L. Abbott ; and in East Kent is recorded by 
Prof. Morris from the marls about Maidstone. 
In South Essex, it has been found associated with mammalian remains 
at Grays, Erith, and Ilford by Prof. Morris; and in North Essex has been 
procured from the freshwater marls of Copford and Clacton. 
In East Suffolk, it has been recorded as //. trochiformis from the mam- 
malian deposit at Stutton. 
In Cambridge, it has been found by the Rev. E. 8. Dewick and Mrs. 
McKenny Hughes i in the gravel-pits of Grantchester and Barnwell Abbey. 
In Yorkshire, it has been found with remains of extinct mammalia at 
Bealsbeck near Market Weighton by Mr. ‘I’. Sheppard. 
In Germany, it is cited by Sandberger as rare in the Lower Pleistocene 
sands of Mosbach and Grotzingen in Baden, and in the tufaceous beds at 
Cannstadt in Thuringia. It is also found rarely in the Mid-Pleistocene 
beds of Grotzingen and Cannstadt, but is abundant in the alluvium of 
Piirklgut in Bavaria. It is also cited by Kobelt from the loess of the 
Rheingau in Nassau. 
In Switzerland, it is cited by Sandberger on the authority of Mousson 
from the valley loess of St. Gall. 
In Austro-Hungary, it 1s quoted by Sandberger as rare in the Lower 
and Mid-Pleistocene valley loess at Nussdorf near Vienna. 
In Italy, it is recorded by Dr. Kobelt from the post-Pliocene deposits of 
Terra Rossa by Monte Pisano. 
In North America, it has been found in the loess at Muscatine, 
Iowa, by Prof. F. M. Witter, and near Iowa city by Mr. H. Prime. 
Howocene.—In Dorset, it is cited from the tufa at Blashenwell, near 
Corfe Castle, by Mr. Kennard. 
In South Hants., it is rare in tufa at Mottisfont, ‘lest Valley, and very 
rare at Southampton Docks (J. 'I’. Kemp, Proe. Hants. Club, 1889). 
In the Isle of Wight, it is reported by Kennard and Warren from the 
tufa bed to the south-west of Widdick Chine, Totlands Bay. 
In West Kent, it is noted by Mr. F. C. J. Spurrell in the sandy deposit 
on site of reservoir at the Metropolitan Southern Sewer Outfall at Crossness. 
In South Essex, it has been found in the alluvium at New Park, near 
the White Horse, Lea Marshes, by Dr. Corner; and from alluvial peat and 
marl at East London Waterworks, Walthamstow, by Mr. B. B. Woodward 
In North Essex, it has been found by Miller Christy in the post-glacial 
beds and rarely in the shell-marl, black-earth, and peat at Chignal St. 
James ; in the alluvial shell- marl of Hostage’s Farm, Felstead, by French ; 
in drain-section in the ‘ ‘Marsh,’ near Shalford Vicar age, by Rev. A. J. Law: 
and by Dr. 8. P. Woodward in a post-glacial deposit ‘ at Witham. 
In Middlesex, it has been found by Mr. J. E. Greenhill in a deposit at 
Clapton, probably of the Bronze age, and is cited by Mr. Kennard from an 
alluvial deposit of the river Colne at U xbridge of post-Roman age. 
In Berkshire, it is reported by Mr. Kennard from beds of probably 
Neolithic age at Newbury, 
