TimeMotion.TimeMotion.TimeMotion.
HoursDegreesMinutesSeconds*Min.Deg.Min.Sec.*Min.Deg.Min.Sec.
Sec.Min.Sec.Th.Sec.Min.Sec.Th.
Th.Sec.Th.ʺʺTh.Sec.Th.ʺʺ
115228101523174616
23045620305328119
345724304573381621
460951410103483124
57512195115 123584626
690144761301536 9129
710517157145173791631
81201943820203893134
913522119215223994636
10150243810230254010139
11165276112452741101641
12180293412303042103143
13195322133153243104646
14210343014330344411148
152253658153453745111651
16240392616403946113153
172554153174154147114656
18270442118430444812158
19285464919445474912171
2030049172050495012323
21315514521515525112476
2233054132253054521328
233455640235455753131711
2436059824605954133213
2537613625616255134716
26391442663145614218
2740663227646757141721
28421902871958143223
294361128297161159144726
30451135630731146015228

Accelerations of the Fixed Stars.

D.H.M.S.
10356
20752
301148
401544
501939
602335
702731
803127
903523
1003919
1104315
1204711
130517
140553
1505858
161254
171650
1811046
1911442
2011838
2112234
2212630
2313026
2413422
2513817
2614213
271469
281505
291541
3015757

[PLATE III].
An absolute Turn of the Earth on it’s Axis never finishes a
solar day.
Fig. II.

222. Thus it is plain, that an absolute turn of the Earth on it’s Axis (which is always completed when the same Meridian comes to be parallel to it’s situation at any time of the day before) never brings the same Meridian round from the Sun to the Sun again; but that the Earth requires as much more than one turn on it’s Axis to finish a natural day, as it has gone forward in that time; which, at a mean state is a 365th part of a Circle. Hence, in 365 days the Earth turns 366 times round it’s Axis; and therefore, as a turn of the Earth on it’s Axis compleats a sidereal day, there must be one sidereal day more in a year than the number of solar days, be the number what it will, on the Earth, or any other Planet. One turn being lost with respect to the number of solar days in a year, by the Planet’s going round the Sun; just as it would be lost to a traveller, who, in going round the Earth, would lose one day by following the apparent diurnal motion of the Sun: and consequently, would reckon one day less at his return (let him take what time he would to go round the Earth) than those who remained all the while at the place from which he set out. So, if there were two Earths revolving equably on their Axes, and if one remained at A until the other travelled round the Sun from A to A again, that Earth which kept it’s place at A would have it’s solar and sidereal days always of the same length; and so, would have one solar day more than the other at it’s return. Hence, if the Earth turned but once round it’s Axis in a year, and if that turn was made the same way as the Earth goes round the Sun, there would be continual day on one side of the Earth, and continual night on the other.

To know by the Stars whether a Clock goes true or not.

223. The first part of the preceding Table shews how much of the celestial Equator passes over the Meridian in any given part of a mean solar day, and is to be understood the same way as the Table in the 220th article. The latter part, intitled, Accelerations of the fixed Stars, affords us an easy method of knowing whether or no our clocks and watches go true: For if, through a small hole in a window-shutter, or in a thin plate of metal fixed to a window, we observe at what time any Star disappears behind a chimney, or corner of a house, at a little distance; and if the same Star disappears the next night 3 minutes 56 seconds sooner by the clock or watch; and on the second night, 7 minutes 52 seconds sooner; the third night 11 minutes 48 seconds sooner; and so on, every night, as in the Table, which shews this difference for 30 natural days, it is an infallible Sign that the machine goes true; otherwise it does not go true; and must be regulated accordingly: and as the disappearing of a Star is instantaneous, we may depend on this information to half a second.

Pl. VI.

J. Ferguson inv. et delin.