ITofacep. 214. 



Table III. 

 The Correlation of the Dcnort Strata with the Rocks of the Cotteswold amp Dorset-Somekset Areas. 



Zii/zag' .... 



Tnu'llii' .... 

 Gitranliaiuc . 



Soniiiiiiir 



DisciUe 



Concavi 



BradfonUnsis 



Murchicontr .. 



Opalini 

 Aaleiisis 



Dispa7isi 



llifronlis 



FulciJ'en 

 Spinati ... 



COITESWOLDS. 



Limestones above the Clijpcui-gnt. 



The Clypcus-siit. 



The Upper Trigonia-giit. 



aud Cleeve Hill, with Terebratula 

 Wrighti. 



The Notgrove Freestoue. 



The Giyphite-gtitol Leckhampton 



The Buckmani-grit. 



The Lower Trigoiiia-grit. 



The Harford Sands. 



The Upper Freestone. 

 The Oolite Marl. 

 The Lower Freestone. 

 The Pea-grit. 



The sandy ferruginous beds. 



\The upper part of the Cephalopod- 

 / bed. 



The middle part of the Cephalopod- 

 beds of the Froeester district = the 

 sands of North Stoke ( Bath district. ) 



The lower part of the Cotteswold 

 Cephalopod-bed = the lower part of 

 Midford Sands at Bath. 



The base of the Cotteswold Cephalo- 

 pod-bed = the bed below the Mid- 

 ford Sands at Bath. 



The upper part of the Cotteswold 

 Sands. 



The lower part of the Cotteswold 

 Sands and the upperpart of the un 

 derlying clay called " Upper Lias." 



The clay above the Marlstone. 



The Marlstone. 



Ddndbt. 



(?) The strata at Barns Batch. 

 The Coralline-beds. 

 The Dundry Freestone. 



The Conglomerate-bed of Maes 

 Knoll = the thin bed below the 

 Freestone at other places. 



The Ironshot Oolite of Dundry. 



The U'ilrhellia-hed—the Upper 

 White Ironshot. 



The Lower White Ironshot — the 

 fusiluhahi-ovaiiit horizon. 



The upper part of the Grey 

 Limestone and Marl-beds. 



The lower part of the Grey 

 Limestone and Marl-beds. 



The hard, irony, massive beds. 



- The bottom beds of stone. 



The Upper Clay-beds— the Du 

 mortieria-heia. 



The Blue Ironshot-beds. 



The pink bed. 

 The Marlstone. 



DORSET-SOMEBSET. 



The ziiizag-heds of Broad Windsor, 

 Dorset. 



The fossil-bed of Halfway House witli 

 'TruelUi and dursetensis. 



The Freestones of Sherborne. 



The upper part of the road-stone of 

 Oborne = Bifurcaten Suhichten of 

 Wiirttemburg. 



The lower part of the road-stone of 

 Oborne = Coronaten Schichten of 

 Wiirttemburg. 



The upper part of the Sandford Lane 

 Fossil-bed. 



The middle part of the Sandford Lane 

 Fossil-bed. 



The lower part of the Sandford Lane 

 Fossil-bed. 



The upper part of the Fossil-bed of 

 Bradford Abbas. 



The lower part of the Fossil-bed of 

 Bradford Abbas. 



The Paving-bed of Bradford Abbas. 



The brachiopoda-beds in the Sand at 

 Stoke Knap ; absent at Bradford Abbas 



I The Freestone of Ham Hill = upper 

 I part of Yeovil Sands at Bradford 

 V Abbas and Stoford. 



The Yeovil Sands = the Blue Clay of 

 Down Cliffs (South Dorset coast), 

 so-called " Upper Lias." 



The Clay below the Yeovil Sands at 

 White Lackington, near Ilminster, 

 so-called " Upper Lias." 



The rest of the so- 

 called" Upper Lias" 

 around Ilminster. 



The Marlstone. 



The Junction- 

 bed of the South 

 Dorset coast, 



' These dates, so far as the Cotteswold aud Dundry strata are concerned, must be regarded as merely suggestions. The sam«^^ljB I' 

 remark applies to the correlation of the deposits with Dorset. 



