324 



THE GEOLOGIST. 



Smyth W W. — " On tlie Gogofau Mine, Caermarthenshire." 3Iem. Oeol. Surv., 



' ■ Vol. L, p. 480. 



Stevenson, W. — " On the Gap in the Greywacke Formation of the Eastern Lammer- 

 muirs, &c." Jour. Geol. Soc, Vol. VI., p. 418. 

 „ " On the Stratified Rocks of Berwickshire." Geol. Proc, Vol. IV. 

 p. 29. 



Strickland, H. E. — " On a Protruded Mass of Upper Ludlow Rock at Hagley 

 Park, &c." Jour. Geol. Soc, Vol. VIII., p. 381. 

 „ On the Distribution and Organic Contents of the ' Ludlow 



Bone Bed.' " Jour. Geol. Soc, Vol. IX. p. 8. 

 Symonds, Rev. W. 5.— ** On the Geologic Range of the Pterygotus Problematicus." 

 Ed. New Phil. Journ., 1855, p. 269. 

 „ " Old Stones." Malvern, 1855. 



„ "On the Transition Beds from the Upper Silurian into the 



Old Red Sandstone." Ed. New Phil. Journ., 1855, 

 Vol. IIL, p. 239. 



„ " Trap Dykes in the Malverns." Phil. Mag., July, 1856, p. 



73. 



Thomson, Prof. W. — " On the Genus Acidaspis." Jour. Geol. Soc, Vol. XIII., p. 

 207 



Townson, Dr. R. — " Tracts on Natural History." 1797. 



Weaver, T. — "Geological Observations on Part of Gloucestershire, &c." Geol. 

 Trans. 2 ser., Vol. I., p. 317. 

 „ " On the Geological Relations of the South of Ireland." Geol. Trans., 

 2 ser., Vol. V., p. 1. 



Whitty, J. 1. — " Notice of the Anthracite found in the Silurian Rocks in the 

 County of Cavan." Jour. Geol. Soc Dublin, Vol. VI., p. 187. 

 Yates, J. — " On the Structure of the Border Country, &c." Geol. Trans., 2 ser. 

 Vol. II. p. 237, 



{To he conti7iued.) 



THE OYSTER CONGLOMERATE BED AT EROMLEY, IN 



KENT. 



Et George D. Gibb, M.D., M.A., E.G.S. 



Theke are many localities around London which possess features of 

 interest to the geologist, that can be reached and examined on a single 

 day. Such a one is the pretty little town of Bromley, in Kent, with a 

 population of 4,000 souls, at a distance of ten miles from London 

 Bridge, and now within easy reach by the Mid Kent Railway, only just 

 opened. A mile to the north-east of Bromley is Sunderidge Park,* in 

 which is to be seen a section of the well-known oyster-conglomerate 

 rock, in a large pit which, together with the accompanying shingle, has 

 been quarried for various purposes for many years. This spot is 

 noticed by Dr. Mantell in his charming volumes, as one of the most 



* The property of Mr. Scott. His steward, Mr. A. Black, has obligingly 

 furnished me every assistance towards examiniug the oyster-bed ou each 

 occasion of my visit to Bromley. 



