FORTY-SIXTH ANNUAL REPORT, FOR 1907. 
17 
Other Members — J. N. Coombe, Sheffield ; Prof. A. Denny, 
Sheffield; F. W. Mills, Huddersfield ; and Dr. H. C. 
Sorby, Sheffield. 
The Yorkshire Coleoptera Committee.— The wet 
weather during the past summer has been anything but advan- 
tageous to Yorkshire Coleopterists. Nevertheless, as the result 
of the efforts of the members, several important records have been 
made, including about a dozen additions to the County List. Full 
particulars of these are appearing in the " Naturalist." 
The constitution of the Committee for 1908 is as follows : — 
I Chairman — Mr. L. Thompson, 20, Emerald Street, Saltburn- 
by-the-Sea. 
Convener — H. H. Corbett, 9, Priory Place, Doncaster. 
Representative — H. Ostheide, 91, Harehills Avenue, Leeds. 
Other Members — E. G. Bayford, Barnsley ; J. W. Carter, Brad- 
ford ; W. Foggitt, Thirsk ; J. Gardner, Hartlepool ; 
Rev. W. C. Hey, West Ayton ; W. Denison Roebuck, 
I Leeds ; E. W. Morse, Leeds ; and T. Stainforth, 
Hull. 
Glacial Committee.— Mr. J. W. Stather writes :— Up to 
the present, the only records that have come to hand are from 
members of the Hull Geological Society as follows : — 
Mr. G. W. B. Macturk reports the finding of two Upper Lias 
Ammonites in superficial deposits near South Cave. 
(1) A. comviunis, east of village, 125 feet O.D. 
(2) A fihulattis, in a bed of rounded gravel at Kettlethorpe^ 
200 feet O.D. 
In connection with the above notes, it should be remembered 
that the present outcrop of Middle Lias is one mile to the west of 
the localities mentioned above, and at a much lower level, and 
there is no outcrop of Upper Lias known in the neighbourhood. 
Mr. C. Thompson and Mr. H. A. Denham report the following 
items from Aldborough, on the Holderness coast : — 
(1) "A large block of what we take to be Old Red con- 
glomerate, 4 ft. 9 in. X 4 ft. 2 in. X 2 ft. 7 in. It contains many 
large pebbles of quartzite and other hard materials, with many 
rolled fragments of volcanic ash and porphyrites akin to the well- 
known Cheviot types." 
(2) A big block of Carboniferous Limestone, 6 ft. 5 in. x 
3 ft. 6 in. X 2 ft. 4 in. It lies on the shore close to the cliff. 
j (3) A large transported mass of Speeton Clay, 12 ft. x 7 ft. x 
I I ft. 6 in., embedded in the boulder clay which occupies the 
hcach. Many typical fossils were obtained from it, including 
B 
