in the Bunter of West Somertset. 



163 



Williton District. — la massive conglomerate, with large limestone 

 and grit pebbles, exposed in the face of an old quarry at Vellow, 

 near Stogumber, I noticed several unaltered limestone pebbles with 

 Zaphrcntis and other fossils on the weathered surface. Owing to the 



St Margaret 



luriescornb^, 

 up lord RzvereU PaJ(X0 3oic Areas 



III t^^ MyCMXrruZ |=lC oQl-McQ5urx 



^^^^>^^ 1 ' ^CarOoniteODt 



^■B Lim.eston.e. ' 

 Illllll Cuim- Meosunes 



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Sketch -map showing the probable directions of the sediment-bearing currents in 



Bunter times. 



hardness of the stone I was unable to extract either the pebbles or the 

 fossils. Further north, in the large quarry on the north side of the 

 railway at Woolston, I found several large pebbles of very hard grey 

 limestone with Brachiopods {Froductus and Spiriferids) and crinoid 

 fi'agments. 



