The Earth is spherical and its centre is the centre of the Universe.
The elevations and depressions caused by the action of water or violence of
the winds do not affect its spheroidity. Its circumference is 5,059 yojana,*
2 kos, 1,154 daṇḍ. The ancient Greeks reckoned the circumference to be
8,000 farsakh*
and its diameter 2,545
The Hindu philosophers have the following rule for determining
the diameter and circumference To find the circumference. Multiply the
given diameter which they call biyáṇs*
by the multiplier 3,927 termed
guṇit,*
and divide the product by the divisor 1,250 called bhág;*
and the
quotient, labdhi*
will be the circumference.*
To find the diameter. Multiply
the given circumference by 1,250 the former divisor, and divide the
product by 3,927, the former multiplier, and the quotient will be the
diameter. The rule of Archimedes as given in Greek works, is accepted
by the Hindus in the same manner, as an approximate calculation. The
gist of the rule is that the relation of the diameter to the circumference is
the ratio of 7: 22, or about thrice the diameter and one-seventh. Any
given diameter is multiplied by 22, and divided by 7, the quotient being
the circumference. Again the circumference multiplied by 7 and divided
by 22 gives the diameter. The fraction, however, is really less than
Now the method of ascertaining the diameter of the (earth's) circumference was after this manner. On a level plain by means of instruments like the astrolabe, the armillary sphere or the quadrant of altitude, taking the elevation of the north pole of the Equinoctial, they proceed northwards, or southwards on the meridian line guided by the astrolabe, and raise the vertical indices above the plane of the circle so that they cover one another. And thus a distance is traversed which exceeds, or is less than the elevation above-mentioned by one degree. If the advance be to the north, it will increase; if to the south, the reverse. The distance from beginning to end is measured and the result forms a degree. Thus the circumference is found.
The ancients by this operation found the degree to be 22 farsakh and
Also on a level plain at sunrise they regulate the course of ghaṛís by means of the Siktajantra which is an instrument like an hour-glass, measured for 60 ghaṛís. With this they walk eastwards. After 84 yojanas and a fraction, there is a difference of one ghaṛí and the day advanced by that time.* This multiplied by 60 gives the circumference of the Earth.