414 REPORT — 1895. 



Geological Society. ' Quarterly Journal.' Vol. L., 189i. Plate XVIII. 

 and page 371. Figs. 1-6. (From Negatives by W. W. Watts.) 



1194_1205 Tardree, Sandy Braes, kc. . Perlitic cracks in Quartz 



Geological Society. ' Quarterly Journal.' Vol. LI., 1895. Plates XX. and 

 XXI. (From Negatives by W. W. Watts.) 



1206-1215 Sulby Glen, kc. Isle of Microscopic sections of ' Crush Conglome- 

 Man rates ' 



Hertfordshire JVatural History Society. 'Transactions.' Vol. VII., Part 8. 

 February 1894. Illustrating Report on Field Meetings of the Society, 

 by John Hopkinsov, F.G.S. 



Photographed by Mr. Hopkinson. 



733 St. Albans — -Section on 1 r^u ^^ t ^- ■ j t\ -cl 



ivfji J T, ■^ ^ Chalk, Tertiaries, and Drift 



Midland Eailway J ' ' 



734 St. Albans . . . Section of Hertfordshire Conglomerate 



■ Liverpool Geological Association. ^Journal.' Fo/. A'/F., 1893-94. Illus- 

 trating Paper on ' The Fossil Footprints of Storeton,' by Osmund W. 

 Jeffs. (From Negatives by F. N. Eaton.) 



741-746 Slabs of sandstone, from the Keuper of Storeton, Cheshire, showing various 



types of saurian footprints (3 plates, 6 photographs). 



Stonesfield Slate. — Second Report of the Committee, consisting of Mr. 

 H. B. Woodward (Chairman), Mr. E. A. Walford (Secretary), 

 Professor A. H. Green, Dr. H. Woodward, and Mr. J. Windoes, 

 appointed to open further sections in the neighhourhood of Stonesfield 

 in order to show the relationship of the Stonesfield slate to the under- 

 lying a,nd overlying strata. (Drawn up hy Mr. Edwin A. Walford, 

 Secretary.) 



The shaft sunk by the Committee in 1894 was reported by the work- 

 men to be unsafe, and an unsuccessful attempt was made to find the old 

 sinking of 1830 at Peed Hill, near Stonesfield, reported upon by Professor 

 Ed. Hull. The work was ultimately continued upon the Stocky Bank 

 shaft to a depth of 60 feet. At that depth it had penetrated 13 feet into 

 one of the highest beds of the Inferior Oolite — the Clypeus-Grit (zone 

 Ammonites Parkinsoni). It has proved the continuance not only of the 

 compact barren limestones (sub-Bathonian) so well developed around 

 Chipping Norton, but also of the sandy limestone beds between them and 

 the Glypeus-Grit. 



The section, as before stated, has been made by scarping a bank for about 

 30 feet, and by sinking a shaft to a depth of 60 feet on the step of the 

 bank. It is practically a continuous section, only 2 or 3 feet intervening, 

 laterally, between the ending of the one cut and the beginning of the 

 other. 



