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heights and dimensions for mountains on _Venus_ which were, to say the least, extravagant. The adjective will not seem too strong when we say that the very existence of the mountains themselves is to-day more than doubtful. The appearances seen by SCHROETER were described by him in perfectly good faith, and similar ones have been since recorded. His reasoning upon them was defective, and the measures which he made were practically valueless. This paper, printed in the _Transactions_ of the Royal Society, to which SCHROETER had not before contributed, appears to have irritated HERSCHEL. No doubt there were not wanting members of his own society who hinted that on the Continent, too, there were to be found great observers, and that here, at least, HERSCHEL had been anticipated even in his own field. I have always thought that the memoir of HERSCHEL which appeared in the next volume of the _Transactions_ (1793), _Observations on the Planet Venus_, was a rejoinder intended far more for the detractors at home than for the astronomer abroad. The review is conceived in a severe spirit. The first idea seems to be to crush an opposition which he feels. The truth is established, but its establishment is hardly the _first_ object. It seems as if HERSCHEL had almost allowed himself to be forced into a position of arrogance, which his whole life shows was entirely foreign to his nature. All through the review he does not once mention SCHROETER'S name. He says: "A series of observations on _Venus_, begun by me in April, 1777, has been continued down to the present time. . . . The result of my observations would have been communicated long ago if I had not flattered myself with the hope of some better success concerning the diurnal motion of _Venus_, which has still eluded my constant attention as far as concerns its period and direction. . . . Even at this present time I should hesitate to give the following extracts if it did not seem incumbent on me to examine by what accident I came to overlook mountains in this planet of such enormous height as to exceed four, five, or even six times the perpendicular height of Chimboraco, the highest of our mountains. . . . The same paper contains other particulars concerning _Venus_ and _Saturn_. All of which being things of which I have never taken any notice, it will not be amiss to show, by what follows, that neither want of a
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