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vourite pursuits at Patricroft, and on his retirement became his serious study. By repeated observations with a powerful reflecting telescope of his own construction, he succeeded in making a very careful and minute painting of the craters, cracks, mountains, and valleys in the moon's surface, for which a Council Medal was awarded him at the Great Exhibition of 1851. But the most striking discovery which he has made by means of big telescope--the result of patient, continuous, and energetic observation--has been that of the nature of the sun's surface, and the character of the extraordinary light-giving bodies, apparently possessed of voluntary motion, moving across it, sometimes forming spots or hollows of more than a hundred thousand miles in diameter. The results of these observations were of so novel a character that astronomers for some time hesitated to receive them as facts.[6] Yet so eminent an astronomer as Sir John Herschel does not hesitate now to describe them as "a most wonderful discovery." "According to Mr. Nasmyth's observations," says he, "made with a very fine telescope of his own making, the bright surface of the sun consists of separate, insulated, individual objects or things, all nearly or exactly of one certain definite size and shape, which is more like that of a willow leaf, as he describes them, than anything else. These leaves or scales are not arranged in any order (as those on a butterfly's wing are), but lie crossing one another in all directions, like what are called spills in the game of spillikins; except at the borders of a spot, where they point for the most part inwards towards the middle of the spot,[7] presenting much the sort of appearance that the small leaves of some water-plants or sea-weeds do at the edge of a deep hole of clear water. The exceedingly definite shape of these objects, their exact similarity one to another, and the way in which they lie across and athwart each other (except where they form a sort of bridge across a spot, in which case they seem to affect a common direction, that, namely, of the bridge itself),--all these characters seem quite repugnant to the notion of their being of a vaporous, a cloudy, or a fluid nature. Nothing remains but to consider them as separate and independent sheets, flakes, or scales, having some sort of solidity. And these flakes, be they what they may, and whatever may be said about the dashing of meteoric stones into the su
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