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The History of Tunbridge Wells, by Thomas Benge Burr, published 1766 (317 pp., Tunbridge Wells: E. Baker) accessible at: East Sussex Libraries View Online
The Tunbridge Wells Guide or An Account of the ancient and present state of that place to which is added a particular description of the Towns and Villages, Gentlemens Seats, Remains of Antiquity, Founderies, &c.&c. within the circumference of Sixteen Miles, by J. Sprange, published 1797 (Tunbridge Wells: J. Sprange) accessible at: East Sussex Libraries View Online
Notes on the geology and structure of the country around Tunbridge Wells: With report of excursion to Southborough, Tunbridge Wells, High Rocks and Eridge. Saturday, May 20th, 1922, by Henry B. Milner, M.A., D.I.C., F.G.S., published 1923 in The Proceedings of the Geologists' Association London (no. 34 issue 1, article, pp.47-55) View Online
Abstract:The following notes describe the geology of some forty square miles of country in the vicinity of Tunbridge Wells, stretching northward almost to Tonbridge and southward to Eridge and Boarshead in Sussex, and as far as Groombridge and Ashurst to the west, of which some of the main features were investigated by members of the Association during the excursion. The six-inch mapping of this area is a continuation of the author's work in the Weald, of which some results have already been published in these proceedings.
The Tunbridge Wells country presents many geological features meriting the attention of those interested in the Weald. Much to be learned from a detailed study of the Lower Cretaceous rocks as developed here, and from their modes of occurrence, has a wider significance than would at first be apparent from casual inspection; thus certain phases in the course of the evolution of the Weald as a whole are realised, the nature of the evidence permitting of a ready appreciation of the factors involved.
The normal Wealden sequence comprises (in descending order) Weald Clay (1200ft.), Tunbridge Wells Sand (180ft.), Wadhurst Clay (150ft.), and Ashdown Sand (400ft.); all four divisionsoccur in this region. In the paper above referred to, the author drew attention to the great practical value accruing from a petrographic study of the individual Wealden beds as an aid to geological mapping. The rocks of the district, by their general barrenness of fossils and by the marked similarities shown frequently by the clays and sands, serve to emphasize this point, especially in cases of repetition or elimination of beds by faulting, a prominent feature of the area. Consequently in the following paragraphs stress is laid on the petrographic criteria which have contributed so largely to the identification and differentiation of horizons in the field.
The Tunbridge Wells country presents many geological features meriting the attention of those interested in the Weald. Much to be learned from a detailed study of the Lower Cretaceous rocks as developed here, and from their modes of occurrence, has a wider significance than would at first be apparent from casual inspection; thus certain phases in the course of the evolution of the Weald as a whole are realised, the nature of the evidence permitting of a ready appreciation of the factors involved.
The normal Wealden sequence comprises (in descending order) Weald Clay (1200ft.), Tunbridge Wells Sand (180ft.), Wadhurst Clay (150ft.), and Ashdown Sand (400ft.); all four divisionsoccur in this region. In the paper above referred to, the author drew attention to the great practical value accruing from a petrographic study of the individual Wealden beds as an aid to geological mapping. The rocks of the district, by their general barrenness of fossils and by the marked similarities shown frequently by the clays and sands, serve to emphasize this point, especially in cases of repetition or elimination of beds by faulting, a prominent feature of the area. Consequently in the following paragraphs stress is laid on the petrographic criteria which have contributed so largely to the identification and differentiation of horizons in the field.
Old Farm House, Groombridge, by R. T. Mason, published February 1940 in Sussex Notes & Queries (vol. VIII no. 1, article, pp.16-17) accessible at: W.S.R.O. [Lib 8865][Lib 2207] & The Keep [LIB/500210] & S.A.S. library
Moving house: Court Lodge, Groombridge - a successful house transplant , by Geoffrey Clarke, published 30 October 1986 in Country Life (vol. 180 no. 4654, article, pp.1337-1339)
The Cuckoo Line, by A. G. Elliott, published 1 September 1988 (76 pp., Wild Swan Publications Ltd, ISBN-10: 0906867630 & ISBN-13: 9780906867631) accessible at: West Sussex Libraries & East Sussex Libraries