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THE APPLICATION OF THE KALENDAR TO HISTORY<br />

THE APPLICATION OF THE KALENDAR TO HISTORY.<br />

i8. The extended recalculations of the elements<br />

of the Ec:yptian kalcndar by Mr. E. B. Knobcl,<br />

which he has favoured us with in this volume, call for<br />

some general account of their sources and applications<br />

which may be suited to archaeological readers.<br />

The basis of all kalcndar changes in Egypt is the<br />

broad main fact of ignoring leap year, and having<br />

a year of 365 days, continuously reckoned onward<br />

through long ages. That the year of 360 days had<br />

disappeared very early is shewn by the five additional<br />

days—or epagomenae—being named the birthdays<br />

of Osiris, Horus, Set, Isis, and Nephthys, the Osiride<br />

family. This shews that the year of 365 days is as<br />

old as the introduction of the Osiride religion. Also<br />

it is most probable that the festival of the Osirification<br />

of the king, and installing a crown prince, took place<br />

at intervals connected with the leap-year shift of the<br />

kalcndar ; and as this festival appears at the beginning<br />

of the 1st dynasty, and is obviously of older origin,<br />

it shews that the quarter of a day was recognised,<br />

and the extra five days already added, long before<br />

that. For all historic periods we have only to consider<br />

a continuous year of 365 days, down to Roman<br />

times.<br />

19. This reckoning came into relation to two<br />

astronomical elements : (i) the position of the sun<br />

in relation to the stars, always viewed by the Egyp-<br />

tians as defined by the day in the year of the first<br />

visibility of Sirius (Sothis) before the rising of the<br />

sun, commonly called the heliacal rising of Sirius ;<br />

(2) the seasons, which are best viewed as midsummer<br />

and midwinter. That these two relations do not<br />

keep step together is due to the wobbling round of<br />

the earth's pole (like a spinning top wobbling) during<br />

a period of about 25,800 years (slightly variable in<br />

length), commonly called the precessional period.<br />

Thus if we imagine the earth passing round a hori-<br />

zontal orbit, with its pole tilted 23" from the upright,<br />

each time that it comes to the same spot between<br />

the sun and a star, the pole will have turned to a<br />

point nearly 1' different ; or in a thousand years the<br />

pole will point about 14° different, and midsummer<br />

will be two weeks earlier in the orbit than before.<br />

By W. M. FLINDERS PETRIE.<br />

As the Egyptian kalendar ignored the fractional<br />

day beyond 365, it follows that in relation to the<br />

stars it retrograded "25636 of a day (or the fraction<br />

over 365 in the sidereal year) in each year, so that it<br />

agreed with the position of sun and stars after 1425<br />

years, the first element named above. It retrograded<br />

in relation to the seasons -24224 of a day (or the<br />

fraction over 365 in the tropical year) in each year, so<br />

that the kalendar agreed with the seasons after 1508<br />

years, the second element named above.<br />

20. So far we have dealt with the kalendar and<br />

the earth alone. But we have in the Sothic period to<br />

deal also with Sirius as well as the earth. This<br />

involves two other considerations. The sun's appar-<br />

ent path in winter is much nearer to Sirius than it is<br />

in summer. The distance on the Egyptian horizon<br />

{i.e. distance in azimuth) between the sun and Sirius<br />

was<br />

'

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