From the Sundays the date of any other day of the week can be readily found.

Thus, if we wish to know on what day of the week Christmas falls in 1889, we look opposite December, under the letter F (which we have found to be the dominical letter for the year), and find that the 22d of the month is a Sunday; the 25th, or Christmas, will then be Wednesday.

In the same way we may find the day of the week corresponding to any date (New Style) in history. For instance, the 17th of June, 1775, the day of the fight at Bunker Hill, is found to have been a Saturday.

These two tables then serve as a perpetual almanac.

Table I.

100200300400
500600700800
900100011001200
1300140015001600
1700180019002000
2100220023002400
—-—-—-——
CEGBA
1295785BDFG
2305886ACEF
3315987GBDE
4326088FEAGCBDC
5336189DFAB
6346290CEGA
7356391BDFG
8366492AGCBEDFE
9376593FACD
10386694EGBC
11396795DFAB
12406896CBEDGFAG
13416997ACEF
14427098GBDE
15437199FACD
164472..EDGFBACB
174573..CEGA
184674..BDFG
194775..ACEF
204876..GFBADCED
214977..EGBC
225078..DFAB
235179..CEGA
245280..BADCFEGF
255381..GBDE
265482..FACD
275583..EGBC
285684..DCFEAGBA

Table II.

ABCDEFG
1234567
Jan. 31.891011121314
15161718192021
Oct. 31.22232425262728
293031........
Feb. 28-29.......1234
567891011
March 31.12131415161718
19202122232425
Nov. 30.262728293031..
............1
April 30.2345678
9101112131415
July 3116171819202122
23242526272829
3031..........
....12345
6789101112
Aug. 31.13141516171819
20212223242526
2728293031....
..........12
Sept. 30.3456789
10111213141516
17181920212223
Dec. 31.24252627282930
31............
..123456
78910111213
May. 31.14151617181920
21222324252627
28293031......
........123
45678910
June 30.11121314151617
18192021222324
252627282930..

Weight of the Earth and Precession.

85. The Weight of the Earth.—There are several methods of ascertaining the weight and mass of the earth. The simplest, and perhaps the most trustworthy method is to compare the pull of the earth upon a ball of lead with that of a known mass of lead upon it. The pull of a known mass of lead upon the ball may be measured by means of a torsion balance. One form of the balance employed for this purpose is shown in Figs. 98 and 99. Two small balls of lead, b and b, are fastened to the ends of a light rod e, which is suspended from the point F by means of the thread FE. Two large balls of lead, W and W, are placed on a turn-table, so that one of them shall be just in front of one of the small balls, and the other just behind the other small ball. The pull of the large balls turns the rod around a little so as to bring the small balls nearer the large ones. The small balls move towards the large ones till they are stopped by the torsion of the thread, which is then equal to the pull of the large balls. The deflection of the rod is carefully measured. The table is then turned into the position indicated by the dotted lines in Fig. 99, so as to reverse the position of the large balls with reference to the small ones. The rod is now deflected in the opposite direction, and the amount of deflection is again carefully measured. The second measurement is made as a check upon the accuracy of the first. The force required to twist the thread as much as it was twisted by the deflection of the rod is ascertained by measurement. This gives the pull of the two large balls upon the two small ones. We next calculate what this pull would be were the balls as far apart as the small balls are from the centre of the earth. We can then form the following proportion: the pull of the large balls upon the small ones is to the pull of the earth upon the small ones as the mass of the large balls is to the mass of the earth, or as the weight of the large balls is to the weight of the earth. Of course, the pull of the earth upon the small balls is the weight of the small balls. In this way it has been ascertained that the mass of the earth is about 5.6 times that of a globe of water of the same size. In other words, the mean density of the earth is about 5.6.