ON THE CIRCULATION OF UNDERGROUND WATERS. Sra 
Character of Strata iad } Depth Remarks 
Ft. in. | Ft. in. 
Strong marl,mingledwithredrock| 3 0 — 
Hard red rock - ; An a — 
Strong marl, with ballsofredrock| 2 9 = 
Hard red sandstone (a little} 1 9 — 
water) 
Marl . 0 6 —- 
Redrock . : : - mee LOne02) 4 
Marl, mingled with light rock .| 35 8 | 238 0 
Light rock . : : . lel 6 leaao) <6 
Sandstone rock . ES emia [A done 
Peldon (with water) 4 0| 252 3 ale i aN abel 
. ell sunk to this dept 
Sandstone rock 8 9] 261 0 { yielded 35,000 galls. daily. 
Fine light rock, very strong 6 ~6 | 267 6 
Red rocky marl 6° O73 6 
Light soft marl . : : ries!) Gale2io: 0 
Red marl, with balls of whiterock | 29 6 | 305 6 
Well sunk to this depth and 
Light red rock, very hard 24 6 330 0 | ie cate ea yi oak 
: 150,000 galls. daily. 
Marl . : . c 6 0} 336 0} Floor of well. 
Hard red rock : -| 2 0} 338 0 
Marl . - : ; : .| 30 0] 368 O 
Hard light rock (with water) 6 0 | 374 (0 
White rock, very strong 9 0O| 388 0 
Strong marl. a TAS) PF S8a ee 
Red rock : 2 0} 386 9 
Strong rocky marl 4 9] 391 6 
Marl e . 2 6) 394 0 
If pumping is stopped for 48 hours the water rises about 100 feet in the 
well; above that the rise is very slow. Ordnance level of top of well, 
4740 feet. 
Final Report of the Committee, consisting of Mr. J. W. Davis, Mr. 
W. Casu, Dr. H. Hicks, Mr. G. W. Lampiuau, Mr. C. REID, 
Dr. H. Woopwarp, and Mr. T. Boynton, appointed for the 
purpose of investigating an Ancient Sea-beach near Bridlington 
Quay. (Drawn up by G. W. LampLuau, Secretary.) 
Trp abundant material obtained during the excavation of the Sewerby 
Cliff-beds two years ago has, at the cost of much time and trouble, been 
thoroughly dealt with. All the bones have undergone a hardening pro- 
cess by immersion in weak glue, and the most promising specimens have 
been pieced together, being thus, in most cases, rendered determinable. 
The results, however, have been somewhat disappointing, as the bones 
have proved to belong in nearly every case to the species whose presence 
was already known. 
Nevertheless, several doubtful-points have been cleared up and a good 
foundation laid for further investigation. 
