324 
THE GEOLOGIST. 
Smyth, W. W. — " On the Gogofau Mine, Caermarthenshire." Mem. Gcol. Surv., 
Vol. I., p. 480. 
Stevenson, IV. — " On the Gap in the Greywacke Formation of the Eastern Lammer- 
muirs, &c." Jo^ir. Geol. Soc, Vol. VI., p. 418. 
„ " On the Stratified Rocks of Berwickshire." Geol. Proc, Vol. IV. 
p. 29. 
Strickland, II. 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. 
Symoiuls, Rev. IF. S. — " On the Geologic Range of the Pterygotus Problematicus." 
Ed. New Phil. Journ., 1855, p. 26U. 
„ " 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." Gcol. Trans., 
2 ser., Vol. V., p. 1. 
Whitly, J. I. — " 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." Gcol. Trans., 2 8er. 
Vol. II. p. 237.. 
(To be continued.) 
THE OYSTER CONGLOMERATE BED AT EROMLEY, IN 
KENT. 
Br George D. Gibc, M.D., M.A., F.G.S. 
Theue are many localities arouud 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 
* Tlic property of Mr. Scott. His steward, Mr. A. Black, Las obligiiif,'!y 
furnished luc every assistance towards examiuing the oyster-bed ou each 
occasion of iiiy visit to Bromley. 
