ZONITOIVES NITIDUS. 145 
In West Sussex, Mr. J. P. Johnson found it in the spring of 1900 in 
the deposits on the fore-shore, exposed at low tide, near West Wittering, 
at the extremity of Bracklesham Bay. 
In West Kent, it has been found in the beds in the vicinity of Erith 
and Crayford by Mr. A. 'I'ylor. 
In South Essex, it is recorded by Prof. Morris from the freshwater mavls 
at Grays ; by Kennard and Woodward as found by Dr. Corner in the 
brick-earth of Sam Green’s Pit, Ilford; and by Mr. J. P. Johnson from 
the paleolithic beds at the Uphall Pit, Ilford: In North Essex, it is 
recorded from the freshwater marls at Copford and Clacton by Prof. Morris. 
In Middlesex, it is cited by Mr. Kennard as present in the fluviatile 
deposits at Clapton and Westminster. 
In East Suffolk, it is recorded from Stutton by Prof. Morris. 
In Cambridge, Mrs. McKenny Hughes and the Rev. EH. 8. Dewick have 
found it in the eravels of Grantehester and Barnwell Abbey. 
In Germany, it is recorded by Sandberger as found in the Lower 
Pleistocene tufa beds of Canth in Silesia and Mithlhausen im Thuringia ; 
it is also quoted from the valley loess of Lower and Mid-Pleistocene age 
at Robschutz near Dresden dita Cannstadt in ‘Thuringia, as well as from 
the sands of Mosbach in Baden. In the Upper Pleistocene series it is 
cited from the tufa beds of Miihlhausen, Canth, and Weimar. It is 
reported by Mr. Kennard from Vitzenburg, and from Battendorf near 
Rossleben in the Harz Mountain district, and by Clessin from the 
alluvium at Piirklgut, Bavaria. 
In Austro-Hungary, Sandberger cites it from tufa of Lower Pleistocene 
age, and the Mid-Pleistocene valley loess at Nussdorf near Vienna. 
In Denmark, Dr. A. C. Johansen quotes it from the Corbicula beds by the 
Free Harbour, Copenhagen. 
Hoxrocene.—In the Isle of Wight, this species is reported fossilized 
from the tufa bed to the south-east of Widdick Chine, 'lotlands Bay, by 
Kennard and Warren. 
In East Kent, it has been found by the Rev. R. Ashington Bullen in a 
deposit overlying the head or rubble drift at Barton Court, Buckland, near 
Dover. In West Kent, it is recorded by Mr. Kennard fron Charlton, and 
from a rain-wash of probably the Bronze age at Greenhithe, and was found 
by Mr. Spurrell in the sandy beds exposed in the excavations for the 
Metropolitan Sewer Outfall at Crossness near Woolwich. 
In Surrey, it is reported by Mr. A. 8. Kennard from the fluviatile 
carbonaceous silt and the underlying sandy loam deposits disclosed 
by the excavations in 'l'ooley street, Bermondsey. It has also been 
found by Mr. 'I’. Belt in the alluvial loamy clay deposit by the side of 
the river Thames at Kew. 
In South Essex, Mr. B. B. Woodward has recorded that it has been 
found on the site of the Albert Docks, also at the Tilbury Docks, and in 
a section at the East London Waterworks, Walthamstow. Mr. Kennard 
cites it from Dagenham. In North Essex, Mr. Miller Christy records it 
from the deposits along the banks of the river Cann at Chignal St. James, 
and Mr. French from the alluvium at Felstead. 
In Middlesex, it was discovered by Mr. Loydell in the old river bed, 
one mile west of Staines, on the tow-path to Old Windsor; by Mr. Meyer 
in the section on the site of Charing Cross Railway Station; by Mr. 
Greenhill in a sandy deposit of probably Bronze age at Clapton ; by 
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