.4NALYSIS TO THE DYNAMICAL THEORY OE THE TIDES. 
233 
Table II. 
Approximate value 
of 
Corj’ected value 
of 
Period of oscillation. 
Corresponding 
period 
without rotation. 
li. ni. i h. m. 
Depth, 7,260 feet {hgjAor'd^ = ; pja- = *18093. 
n = 
1 
•24095 
•15491 
30 
29-3 
59 
17 
7t — 
o 
o 
•7434U 
•70890 
14 
15-2 
22 
49 
n = 
o 
1-2002 
1-2270 
10 
50-0 
14 
13 
u = 
7 
1-8426 
1-8633 
8 
47-5 
10 
20 
n = 
9 
2'6815 
2-6951 
7 
18-6 
8 
7 
11 
11 
3-7193 
3-7287 
6 
12-9 
6 
41 
Depth, 14,520 feet {JigjAoScd' — - 
h)\ 
PICT 
= *18093. 
n = 
1 
•2819L 
•22204 
25 
28-0 
41 
55 
71 — 
3 
1-0201 
1-0160 
11 
54-3 
16 
8 
n = 
5 
1-9132 
1-9300 
8 
38-3 
10 
3 
11 = 
7 
3-1919 
3-2025 
6 
42 3 
7 
18 
n = 
9 
4-8672 
4-8741 
5 
26-1 
5 
44 
n — 
11 
6-9414 
6-9461 
4 
33-2 
4 
44 
Depth, 29,040 feet {hglAorcd 
i\.-); 
p/or 
= *18093. 
n = 
1 
-36381 
•32658 
20 
.59 9 
29 
39 
11 = 
3 
1-67362 
1-57822 
9 
33-1 
11 
25 
71 = 
5 
3-.3391 
3-34816 
6 
.33-5 
7 
h? 
/ 
U ~ 
7 
5-8906 
5-8959 
4 
56 5 
5 
10 
71 = 
9 
9-2387 
9-2421 
3 
56-8 
4 
4 
71 — 
11 
13-3856 
13-38S0 
3 
16-8 
3 
21 
Depth, 58,080 feet {ligj^oreC'' = 
i); 
p/o- 
= *18093. 
71 = 
1 
•52763 
•50650 
16 
51-7 
20 
58 
11 = 
3 
2-6806 
2-6853 
7 
19-4 
8 
4 
71 = 
5 
6-1911 
6-1957 
4 
49-3 
5 
1 
71 = 
7 
11-2879 
11-2906 
3 
34-3 
3 
39 
7^ = 
9 
17-9816 
17-9833 
2 
49-8 
2 
52 
n = 
11 
26-2742 
26-2753 
2 
20-5 
2 
22 
§ 9. Numerical Comiyutation of the Height of the Surface-Wa'vcs. 
We have next to evaluate the quantities ; when once the periods have 
been determined this will present no difficulty. Suppose we are dealing with the 
MDCCCXCVII.—A. 2 H 
