HAZZLEDINE WARREN : STUDY OF PRE-HISTORY IN ESSEX. 15I 
Ilford, visit to (E. N., vii., 1893, p. 47). Elephas primigenius 
is the common species here, E. anliquus at Grays. 24 
Ilford, visit to (W. Crouch, E.N., vii., 1893, pp. 93-94). Notes 
on the mammalian remains. 25 
Ilford, visit to, by the Geologists’ Association (T. V. Holmes, 
E.N., xi., 1899, pp. 149-151). Note on the “ Cauliflower 
Pit.” ■ 26 
Ilford (J. P. Johnson and G. White, E.N., xi., 1899, pp. 157- 
160). New sections on the old Uphall site, with an 
important list of mollusca. (J. P. Johnson, E.N., xi., 
1900, pp. 209-212) Further mollusca from same site, 
also contemporary flint flakes, and a revised complete 
list of mammalia from Uphall. 27 
Ilford, Mollusca (A. S. Kennard and B. B. Woodward, E.N., 
xi., 1900, pp. 213-215) [20]. 28 
Rhinoceros hemilcechus, Falc. (M. A. C. Hinton, E.N., xii., 
1902, pp. 231-236, plate). This is the R. leptorhinus of 
Owen. The characters of the molars are carefully 
described and well shown in the plate. Ilford. 29 
Hippopotamus ( E.N. , xiii., 1904, p. 259, brief note). Ilford 
Cemetery. - 30 
Elephas primigenius, etc. ( E.N. , xv., 1908, p. 258, brief note). 
Ilford. 31 
Elephas, Barking ( E.N., xiv., 1907, pp. 272 ; xv., 1908, pp. 30- 
31, Plate and fig.). A pelvis found on the “ Kennedy 
Estate.” 32 
Ilford-Woodford, new railway (T. V. Holmes, E.N., xii., 
1902, pp. 202-206, map and sections). Mid Terrace group 
of river gravels about Ilford and Ley Street, from 45 to 
85 feet above O.D. 33 
Barking Side (W. Crouch, E.N., iv., 1890, p. 18). Bones 
of Equus and Bos, from gravel at St. Swithin’s Farm. 34 
Barking Side, Wanstead, Walthamstow (H. W. 
Monckton, E.N., vii., 1893, pp. 115-120). Describes the 
gravels of these districts, and the rocks they contain : 
no records of palaeoliths or mammalia. 35 
Walthamstow (T. V. Holmes, E.N., vi., 1892, p. 97) Visit 
to sections on new railway, showing gravels at surface 
level of 40 to 50 feet O.D. 36 
Romford [16]. 
Upminster(W. H. Dalton, E.N., iv., 1890, pp. 186-7, section). 
The brickearth here stands at over 150 feet O.D., and 
probably belongs to a tributary stream. 37 
