124 bibliography: geology and PAL/EONTOLOGY, 1880. 



exhibited in the coast sections ; the Lower Oolites, which form the high 

 moors ; the Kellaways Rock, the highest member exposed in the district ; the 

 Cleveland Dyke ; and the Glacial and Post-Glacial deposits. A chapter is 

 devoted to physical structure, faults, etc. ; another to economic products, 

 including the celelirated Cleveland ironstone ; there is also an appendix 

 giving the bililiography]. Svo., loi pp., London, 1888. [Reviewed, Geol. 

 Mag., Dec. 1888, dec. iii. vol. v. jip. 569-570]. 

 H. C. Beasi.ey. Cheshire. 



On a Section of Upper Keuper at Oxton [stating that the red marl there 

 seen is not in situ]. Proc. Liverp. Geol. Soc, 1886, v. 134-136. 

 H. C. PjEasley. Lancashire and Cheshire. 



Some Instances of Horizontally Slickensided Joints [following described : 

 in (|uarry at Wallasey, four parallel joints running E. and \V., and a fifth 

 crossing them in a direction 20^ N. of VV. ; at Poulton, half-mile S. of above, 

 and in same beds, lowest part of Keuper Sandstone, several joints at varying 

 angles from 20° S. of W. to 25° N. of W. ; on north side of Howbeck Road, 

 Birkenhead, a joint 30° W. of N. traceable across the quarry ; on Bidston 

 Hill, at a jioint in cutting close to windmill, an indistinctly striated joint 

 about 20° N. of W. ; at Brandreth Delph, Parbold, Millstone Grit, two sets 

 of joints at right angles]. Proc. Liverpool Cieol. Soc, 1887, v. 246. 

 Henry C. Beasi.ey. Cheshire. 



Report of Field Meeting at Bidston Hill [a road has exposed a continuous 

 section of Keuper Sandstone, of which the hill is composed ; at Flaybrick 

 Hill, a section of Upper Ihniter overlain by a conglomerate, the latter being 

 the base of the Keuper]. Proc. Liverpool (.ieol. Soc, 1887, v. 290. 

 H. C. Beaslev. Cheshire. 



Some Irregularly Striated Joints in the Keuper Sandstone of Lingdale 

 Quarry [measured details of a series of slickensided faces exposed on the 

 VV. side of the quarry, showing striations in varying directions within a very 

 short distance of each other; plan and section given]. Proc. Liverpool Geol. 

 Soc, 1888, V. 386-3S8. 

 H. C. Beasley. Cheshire. 



Report of Field Meeting at Wallasey [four or five parallel joints pointed 

 out having an K. and W. direction, distinctly slickensided and striated 

 horizontally, and in some instances traceable for a considerable distance, whilst 

 they were crossed diagonally by a similar joint exposed on both sides of the 

 quarry ; a bed of conglomerate and another of grey shale, much disturbed, 

 noted], i'roc Liverpool Geol. Soc. 1888, v. 389. 

 J. E. Beui-ori). Isle of Man. 



Notes on the Isle of Man [after brief mention of geological features at Port 

 Soderick and Port Erin, visit to Stack of Scarlett and 'Chasms' described; 

 near Peel are found a great number of flint flake implements ; details of 

 .section given from which they were obtained]. Trans. Leeds Geol. Assoc, 

 1888. Part iv. pp. 177-179. 

 W. J. Bird. Durham. 



The South Durham Salt Bed and Associated Strata [strata thus classified ; 

 (I ) Surface Deposits; (2) Upper Gypseous Marls; (31 Red Sandstones and 

 Marls; (4) Lower Clypseous RLarls; (5) Saliferous Ikds (Anhydrite. Salt, 

 etc.); (6) Magnesian Limestone; details given of twenty-three borings 

 through aljove]. Trans. Manchester Geol. Soc, vol. xix. 564-584, with 

 sections and tables. 

 J. F. Blake. York N.E. 



On a Star-fish from the Yorkshire Lias [a Solaster from Huntcliff ]. Rep. 

 J5rit. Assoc, for 1887. p. 716 ; see also Nature, 1887, vol. xxxvi. p. 591. 

 Herkert liOLioN. Lancashire. 



Observations on Boulders from the High-level Drift of Bacup [rock 

 specimens obtained from drift described in detail and altitudes given ; con- 

 cludes the presence of three well-defined beds of Glacial Drift in the Bacup 



Naturalist, 



