36 



Bibliography : Geology and Palaeontology, i8gy. 



Henry Whitehead. York S.W. 



[Boulder of Borrowdale Volcanic Ash at] Blackstone Edge [in The 



Yorkshire Boulder Committee and its Tenth Year's Work]. Naturalist, 

 March 1897, p. 66. 

 Arthur Smith Woodward. York N.E. 



On the Fossil Fishes of the Upper Lias of Whitby. Part II. 



[describing- remains of Caturus, Saurostomus, and Pachycormus\ Prpc. 

 Yorks. Geol. and Polyt. Soc, Vol. 13, Part 2, 1897, pp. 155-170. 



H. B. Woodward. Lincolnshire, etc. 



The Chalky Boulder-clay and the Glacial Phenomena of the 



Western-Midland Counties of England [a very full and clear account of 

 these beds ; after carefully examining all the evidence, states, ' If we 

 believe that the main mass of boulder-clay was deposited on the melting 

 back of the ice-sheet, or from the melting of basal portions of the ice, 

 and that there were alternations in the climate, so that the ice extended 

 and receded for some distance more than once before it finally retreated, 

 we can understand the intercalation of water-distributed sands and 

 gravels, as well as laminated muds, with boulder-clay, and more especially 

 along the margin of the glaciated area']. Geol. Mag., 1897, pp. 485-497; 

 Glac. Mag., Sept. 1897, pp. 63-65; and Brit. Assn. Report, 1897. pp. 649- 

 650. 



H. B. Woodward. Cumberland, Cheshire. 



Eminent Living Geologists: The Rev. P. B. Brodie, M.A., F.G.S. 



[referring briefly to Mr. Brodie's work on the Lower Lias of Cheshire 

 and Cumberland], Geol. Mag., 1897, pp. 481-485. 



H. B. W[OODWARD]. LlNC. X. 



The Rev. John Edward Cross, M.A., F.G.S. [obituary notice; 



referring to the late Rev. J. E. Cross's work amongst the Jurassic rocks 

 of North-west Lincolnshire]. Geol. Mag., 1897, p. 192. 



H. B. W[oodWARd], Lanc. S. and \Y, Cheshire, Westmorland. 

 Movements of Beach Sand and Shingle [discussing an article by 



W. H. Wheeler in the Proc. Inst. Civil Engineers, Vol. 125, 1896, in 

 which Wheeler maintains that the movements are practically confined 

 to the tract between low- and high-water mark, etc. ; referring to the sand- 

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 Bay, etc.]. Geol. Mag., 1897, pp. 44-46. 



D. WOOLACOTT. Dt RHAM. 



Geology i of | North-east Durham, j A Popular Work | by | 



D. Woolacott, B.Sc, | etc. | . . | . . | . . | Sunderland: . . i 1897 

 [divided into chapters as follows : — Introduction ; The Geological Series 

 and the Position of the Rocks of this district in it; The General Geological 

 Structure of this district; The Lie of the Coal-Measures ; The Coal- 

 Measures — their formation and characteristics ; The Aspect of our 

 District during the Carboniferous Period ; The Conditions that prevailed 

 after the deposition of the Coal-Measures ; The Magnesian Limestone ; 

 The 'Cannon-ball' and other structures of the Magnesian Limestone; 

 The Break in the Geological Story of this district ; The Great Ice-Age ; 

 The Raised Beaches of the District and what they teach; The Submerged 

 Forest in Whitburn Bay; and A Summary of the Geological History of 

 North-East Durham]. 8vo. , pp. xii. +84. 



D. Woolacott. Durham. 

 An Explanation of the Claxheugh Section (Co. Durham) [describing 



a section two miles west of Sunderland, at the base of which are Permian 

 Yellow Sands, succeeded by the Marl Slate, thin-bedded limestones, 

 and at the top crystalline limestones without any trace of bedding, etc.]. 

 Abstract in Geol. Mag., 1897, P- 377 5 an< ^ in Quart. Journ. Geol. Soc, 

 Vol. 54, Feb. 1898, p. 14. 



Naturalist, 



