Figures illustrating1 direction and showing varieties of rotations2.
Versorium on loadstone.
P assing from the probable cause of motion toward fixed3 points (according to magnetick laws and principles), it remains4 for us to indicate those motions. Above a round loadstone (whose poles are A, B) let a versatory needle be placed whose cusp has been excited by the pole A; that cusp is certainly directed toward A, and is strongly attracted by A; because, having been touched by A, it is in true harmony with A, and combines with it; and yet it is called contrary, because when the versorium is separated from the stone, it is seen to be moved toward the opposite part of the earth to that toward which the pole A of the loadstone is moved.
For if A be the northern pole of the terrella, the cusp is the southern end of the needle, of which the other end (namely, the cross) is pointed5 to B; so B is the southern pole of the loadstone, but the cross is the northern end of the versorium. So also the cusp is attracted by E, F, G, H, and by every part of a meridian6, from the æquator toward the pole, by the faculty7 disponent; and when the versorium is on the same parts of the meridian, the cusp is directed toward A. For it is not the point A that turns the versorium toward it, but the whole loadstone; as also the whole earth does, in the turning of loadstones to the earth.
Figures illustrating magnetick directions in a right sphere208 of stone, and in the right sphere of the earth, as well as the polar directions to the perpendicular8 of the poles. All these cusps have been touched by the pole A; all the cusps are turned toward A, excepting that one which is repelled9 by B.
Figures illustrating horizontal directions above the body of a loadstone. All the cusps that have been made southern by rubbing on the boreal pole, or some place round the northern pole A, turn toward the pole A, and turn away from the southern pole B, toward which all the crosses look. I call the direction horizontal, because it is arranged along the plane of the horizon; for nautical10 and horological instruments are so constructed that the iron hangs or is supported in æquilibrium on the point of a sharp pin, which prevents the dipping of the versorium, about which we intend to speak later. And in this way it is of the greatest use to man, indicating and distinguishing all the points of the horizon and the winds. Otherwise on every oblique sphere (whether of stone or the earth) versoria and all magnetick substances would have a dip by their own nature below the horizon; and at the poles the directions would be perpendicular, which appears in our discussion On Declination.
A round stone (or terrella) cut in two at the æquator; and all the cusps have been touched by the pole A. The points at the centre of the earth, and between the two parts of the terrella which has been cut in two through the plane of the æquator, are directed as in the present209 diagram. This would also happen in the same way if the division of the stone were through the plane of a tropick, and the mutual12 separation of the divided parts and the interval13 between them were the same as before, when the loadstone was divided through the plane of the æquator, and the parts separated. For the cusps are repelled by C, are attracted by D; and the versoria are parallel, the poles or the verticity in both ends mutually requiring it.
Half a terrella by itself and its directions, unlike the directions of the two parts close to one another as shown in the figure above. All the cusps have been touched by A; all the crosses below except the middle one tend toward the loadstone, not straight, but obliquely14; because the pole is in the middle of the plane which before was the plane of the æquator. All cusps touched by places distant from the pole move toward the pole (exactly the same as if they had been rubbed upon the pole itself), not toward the place where they were rubbed, wherever that may have been in the undivided stone in some latitude15 between the pole and the æquator. And for this reason there are only two distinctions of regions, northern and southern, in the terrella, just as in the general terrestrial globe, and there is no eastern nor western place; nor are there any eastern or western regions, rightly speaking; but they are names used in respect of one another toward the eastern or western part of the sky. Wherefore it does not appear that Ptolemy did rightly in his Quadripartitum, making eastern and western districts and provinces, with which he improperly16 connects the planets, whom the common crowd of philosophizers and the superstitious17 soothsayers follow.
1 illustrating | |
给…加插图( illustrate的现在分词 ); 说明; 表明; (用示例、图画等)说明 | |
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2 rotations | |
旋转( rotation的名词复数 ); 转动; 轮流; 轮换 | |
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3 fixed | |
adj.固定的,不变的,准备好的;(计算机)固定的 | |
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4 remains | |
n.剩余物,残留物;遗体,遗迹 | |
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5 pointed | |
adj.尖的,直截了当的 | |
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6 meridian | |
adj.子午线的;全盛期的 | |
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7 faculty | |
n.才能;学院,系;(学院或系的)全体教学人员 | |
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8 perpendicular | |
adj.垂直的,直立的;n.垂直线,垂直的位置 | |
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9 repelled | |
v.击退( repel的过去式和过去分词 );使厌恶;排斥;推开 | |
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10 nautical | |
adj.海上的,航海的,船员的 | |
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11 oblique | |
adj.斜的,倾斜的,无诚意的,不坦率的 | |
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12 mutual | |
adj.相互的,彼此的;共同的,共有的 | |
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13 interval | |
n.间隔,间距;幕间休息,中场休息 | |
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14 obliquely | |
adv.斜; 倾斜; 间接; 不光明正大 | |
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15 latitude | |
n.纬度,行动或言论的自由(范围),(pl.)地区 | |
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16 improperly | |
不正确地,不适当地 | |
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17 superstitious | |
adj.迷信的 | |
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