Bibliography : Geology and Palceontology , 1902. 9 
William Hill. Lines., N. 
Note on the Upper Chalk of Lincolnshire. [Gives evidence of the occur- 
rence of upper chalk in the county, though the exact horizon of its 
base is not ascertained]. ' Geo]. Mag.', Sep. 1902, pp. 404-406. 
Edwin Hill. Yorks., S.E., Lines., N. 
On the Matrix of the Suffolk Chalky Boulder-clay. [Briefly refers to 
the Yorkshire coast sections, etc.]. ' Quart. Jour. Geoh Soc.', 
\o\. LVIH., May 1902, pp. 179-184. 
Wheeltox Hind. Northern Counties. 
Life-zones in the British Carboniferous Rocks. Report of the Com- 
mittee. [Gives tables and classifications as results of work by 
collectors in the Pendle District, and at Hawes]. ' Report Brit. 
Assoc.', 1901 (Glasgow), published 1902, pp. 288-296. 
Wheelton Hind. Yorks., North'd, Derbys., etc. 
On the Characters of the Carboniferous Rocks of the Pennine System. 
[Compares and correlates the beds in different localities, gives 
lists of fossils, etc.]. ' Proc. Yorks. Geo!, and Polyt. Soc.', Vol. 
XIV., part 3, 1902, pp. 422-464. 
P. Holland, See T. M. Reade. 
J. H. HowARTH. Yorkshire. 
[Note to Mr. Sheppard's paper on * The Yorkshire Boulder Committee 
and its work— a Retrospect]. ' Naturalist,' July 1902, pp. 221-222. 
J. H. HowARTH. See Percy F. Kendall. 
J. Allen Howe. See C. Fox-Strangways. 
T. McKexny Hughes. Yorks., Mid. W. 
Ingleborough. Part II. Stratigraphy [with plans, sections, lists of 
fossils, etc.], 'Proc. Yorks. Geol. and Polyt. Soc.', Vol. XIV., 
part 3, 1902, pp. 323-343. 
A. Jukes-Browne. Northern Counties. 
The Student's Hand-Book of Stratigraphical Geology, 1907, pp. 5 and 
58Q. (maps). 
P. F. Kendall. Yorks., Mid. W. 
Saccammina cnrteri Brady in Yorkshire. [At Bolton Woods and Clap- 
ham]. ' Naturalist,' July 1902, p. 222. 
P. F. Kendall. Yorks., Mid. W. 
Current Bedding in the Carboniferous Limestone. [Above the waterfall 
at Gordale Scar]. ' Naturalist,' July 1902, p. 217. 
Percy F. Kendall. Yorks., N.E. 
A System of Glacier-Lakes in the Cleveland Hills. rFrom the evidence 
of borings and drift-fdled channels, considers that during or 
before the glacial period, the land was considerably above the 
present level ; the drift beds are described in detail, from sections 
and borings, and seem to indicate : (i) the unobstructed passage 
of the Teesdale Glacier to the coast ; (2) the arrival of the Scandi- 
navian Ice ; (3) the invasion of the Scottish Ice. A series of 
glacier-dammed lakes was formed along the ice-margins]. ' Quart. 
Journ. Geol. Soc.', Aug. 1903, Vol. LVIII., pp. 471-571. Maps and 
Plates. See also ' Naturalist,' Jan. 1903, pp. 14-16 ; Abstract ni 
' Geol. Mag.', Feb. 1902, pp. 83-84. 
