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liant in contrast with the surrounding plain, but out of that plain, about forty miles toward the east, projects a small mountain which is also remarkable for its reflecting properties, as if the gray ground were underlain by a stratum of some material that flashes back the sunlight wherever it is exposed. The crater mountain, Sulpicius Gallus, on the border of the _Mare_, north of Manilius and east of Menelaus, is another example of the strange shining quality of certain formations on the moon. Follow next the Haemus range westward until the attention falls upon the great ring mountain Plinius, more than thirty miles across, and bearing an unusual resemblance to a fortification. Mr. T. G. Elger, the celebrated English selenographer, says of Plinius that, at sunrise, "it reminds one of a great fortress or redoubt erected to command the passage between the _Mare Tranquilitatis_ and the _Mare Serenitatis_." But, of course, the resemblance is purely fanciful. Men, even though they dwelt in the moon, would not build a rampart 6,000 feet high! Mount Argaeus, at the southwest corner of the _Mare Serenitatis_, is a very wonderful object when the sun has just risen upon it. This occurs five days after the new moon. Returning to the eastern extremity of the _Mare_, we glance, in passing, at the precipitous Mount Hadley, which rises more than 15,000 feet above the level of the _Mare_ and forms the northern point of the Apennine range. Passing into the region of the _Mare Imbrium_, whose western end is divided into the _Palus Putredinis_ on the south and the _Palus Nebularum_ on the north, we notice three conspicuous ring mountains, Cassini near the Alps, and Aristillus and Autolycus, a beautiful pair, nearly opposite the strait connecting the two _Maria_. Cassini is thirty-six miles in diameter, Aristillus thirty-four, and Autolycus twenty-three. The first named is shallow, only 4,000 feet in depth from the highest point of its wall, while Aristillus carries some peaks on its girdle 11,000 feet high. Autolycus, like Cassini, is of no very great depth. Westward from the middle of an imaginary line joining Aristillus and Cassini is the much smaller crater Theaetetus. Outside the walls of this are a number of craterlets, and a French astronomer, Charbonneaux, of the Meudon Observatory, reported in December, 1900, that he had repeatedly observed white clouds appearing and disappearing over one of these small craters. Sout
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