iSg2.] 
469 
[De Geer. 
As to places in other tracts where I have made determinations 
of the marine limit, I must for the present confine myself to a 
mere statement of the heights obtained, but I hope that I shall 
be able to add a more complete description of the different 
localities. 
Determinations of the Late Glacial Marine Limit. 
With 
With 
Probable 
Localities. 
handlevel. 
Feet. Meter. 
barometer. height. 
Feet. Meter. Feet. Meter. 
1. Perth Amboy, N. Y. 
— 
— 
— 
— 
0 
0 
2. New Haven, Conn. 
<17 
<5.2 
— 
— 
c. 10? 
c. 3? 
3. Martha’s Vineyard, Mass. 
— 
— 
— 
0 
0 
4. Boston, Mass. 
— 
— 
c. 10-20 
c. 3-6 
5. Mount Desert Island, Maine 
) 
( a ) N. E. of Somes Sound. 
— 
— 
204 
62 | 
(a) “ 
— 
— 
208 
64 V 
c. 210 
c. 64 
6. (6) S. W. of Bar Harbor. 
— 
— 
210 
64 | 
7. (c) S. of Bar Harbor. 
— 
— 
209 
64 J 
8. Stockton, Maiue. 
— 
— 
274 
84 
c. 280 
c. 86 
9. Bucksport, Maine, at Port Knox, 
305 
93.0 
298 
91 
305 
93 
10. St. John, N. B. («) western point. 
11. “ “ “ (6) eastern “ 
z 
— 
267 
271 
82 \ 
83/ 
c. 269 
c. 82 
12. Digby, N. S. 
>35 
>10.7 
— 
— 
c. 40 
c. 12 
13. Annapolis, N. S. 
42 
12.7 
46 
14 
42 
12.7 
14. Wolfville, N. S. 
15. Moncton, N. B. (Berry Mill 
<49 
<15 
— 
— 
c. 50? 
c. 15? 
Station, I.R., being 208 ft.) 
— 
— 
325? 
99? 
c. 325? 
c. 99? 
16. Bathurst, N. B. 
— 
— 
196 
60 
c. 196 
c. 60 
17. Dalhousie, N. B. 
175 
53.4 
175 
54 
175 
53.4 
18. Dalhousie Junction, N. B. 
19. Riviere du Loup, Quebec (the 
— 
— 
174 
53 
c. 174 
c. 53 
station I. R., 322.5 ft.) 
373 
113.9 
— 
— 
373 
113.9 
20. Montreal, Quebec (a leveled 
point being 565 ft.) 
— 
625 
190 
c. 625 
c.190 
21. St. Albans, Vt. (the station 
being 390 ft.) 
658 
200.5 
656 
200 
658 
200.5 
22. Alburgh, N. Y. (Moira station, 
C. V. R. being 357 feet) 
— 
— 
662 
202 
c. 662 c. 202 
23. Ottawa, near Kingsmeer Lake, 
Quebec (Hull st’n C.P.R. 185 ft.) — 
— 
705 
215 
c. 705 c. 215 
Unless the contrary is stated all the above heights refer to high- 
water mark, and the uplifted shore-lines were probably formed at 
least at or rather above ordinary highwater. As the high tide 
might have been somewhat lower in the Bay of Fundy when the 
