™ 
424 HELICIGONA ARBUSTORUM. 
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In Saxony, it is recorded from the Lower and Middle strata at Priesa 
and other places near Meissen, and at Robschutz near Dresden. 
In Wurtemburg, it has been found in the lower and middle Pleistocene 
beds at Cannstadt, Ludwigsburg, and Rappenau in the Neckar Valley ; 
the var. trochoidalis being known from Cannstadt only. 
In Bavaria, it is recorded by Prof. Sandberger from the Lower and Middle 
Pleistocene of the Danubian Valley at Passau, Regensburg, and Oellingen. 
Herr Clessin records it from the old alluvial beds of Piirklgut ; the type 
and var. a/lpicola from the loess of Regensburg, and the type and vars. 
trochoidalis, depressa, alpestris, and fuscescens from the tufaceous deposits 
of the Black Laaber. 
In Franconia, the typical form is recorded by Dr. von [Ihering from the 
diluvial deposits of Streitberg and by Prof. Sandberger as found in the 
beds from the earliest to the latest Pleistocene periods near Wurzburg. 
In Thuringia, it is known from the tufaceous beds of Lower and Upper 
Pleistocene age at Weimar, Grafentonna, and Burgtonna ; and in Nassau, 
is found plentifully in deposits of Lower and Middle Pleistocene time at 
Heigelsbachthal and Oberissigheim near Hanau, and rarely at Bad Ems. 
In France, it is recorded by Locard from the Mid-Pleistocene beds of 
Dauphiny; and the Upper Pleistocene of the environs of Paris, and of 
Bas Boulonnais, and according to Sandberger in the valley loess of Lyons 
and the Upper Pleistocene of Montreuil, and Clichy. The type and var. 
alpestris are recorded from the gravels of Joinville-le-Pont, Seine, by 
Laville; in the tufa of La Celle, near Moret, Seine-et-Marne, by 'Tour- 
noiier ; and in the base of the loess or fluvio-marine sand of Menchecourt, 
Somme, by Picard. 
In Austria, according to Sandberger, it has been found in the valley of 
the Danube at Waidling and Wolkersdorf, also at Nussdorf near Vienna, 
the var. w/pestris has also been found at the latter place. 
In Switzerland, the var. a/pestris is recorded by Sandberger from St. Gallen. 
Hotocene.—In Wiltshire, the type form, vars. fuscescens and cincta 
found in 1909 by Mr. Harold St. George Grey in the superficial deposit 
in the fosse of the Great Circle at Avebury, and the var. céucta at a depth 
of six feet in the deposit of Roman age at the same place. It is recorded 
by the Rey. R. A. Bullen from a rain-wash in a chalk-pit at West Harnham 
near Salisbury. 
In the Isle of Wight, it is reported by Mr. Kennard from the tufaceous 
lime beds at T'otland’s Bay and from St. Catherine’s Down. 
In Hampshire, Mr. Kemp records it from the Itchen Valley, from mole 
hills in the Anton Valley, and as rare in the tufa at Southampton Dock. 
In Kent, it is recorded by Mr. Santer Kennard from the base of a 
tumulus of early Romano-British age at Stanley’s Quarry, Ightham, 
mixed with bone fragments and Roman pottery from the base of a rain- 
wash, two to six feet in thickness, on the site of a large Roman building 
at Darenth ; in the sandy clay alluvium at Crossness ; in the early holocene 
bed at Cuxton, and in the deposits at Charlton, Greenhithe, and Otford. 
It is recorded by the Rev. R. A. Bullen from the rubble drift at Barton 
Court, Buckland, near Dover. 
In Surrey, it is recorded by Kennard and Woodward from deposits of 
carbonaceous silt of Roman age, and the pre-Roman stratum of marsh clay 
disclosed by excavations in 'T'ooley street, Bermondsey. ‘The Rev. R. A. 
Bullen also collected specimens at depths varying from 2ft. 6in. to 4ft. im 
