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of the Llanos acquires that feeling of security and enduring disposition for which he is famous. Unfortunately, it is often turned to account in disturbing the balance of power among his more enlightened countrymen; for he is always ready to join the first revolutionary movement offering him the best chance for equipping himself with arms of all descriptions. Next to the horse, the Llanero esteems those weapons which give him a superiority over his fellow-creatures,--viz., a lance, a blunderbuss, and a fine sword. If he is unprovided with either of these, he considers himself a miserable and degraded being, and all his efforts will tend to gratify this favorite vanity even at the risk of his own life. Therefore he goes to war, because he is sure, if victorious, of finding the battle-field covered with these tempting trophies of his ambition. In this, unfortunately, he is too often encouraged by a host of unprincipled politicians, who, not wishing to earn a livelihood by fair means, are eternally plotting against the powers that be. THE FORESTS OF THE AMAZON AND MADEIRA RIVERS. FRANZ KELLER. [The author of the following selection, with his father, was sent in 1867, by the Minister of Public Works at Rio Janeiro, to explore the Madeira, and to project a railroad along its banks where the rapids rendered navigation impossible. His observations during this journey are given in "The Amazon and Madeira Rivers," from which we extract his remarks concerning the Brazilian forests.] Everywhere the decomposing organisms serve as bases for new formations. No particle, however small, is ever lost in the great household of Nature; but nowhere is her restless activity so conspicuous as in the tropics, where the succession of vegetable decay and life is so much more rapid than it is in colder climes; and which will strike the reflecting student more especially in the wide, forest-clad valleys of tropical America, and on the Amazon and its affluents. On the heights of the Cordillera the process is already at work. The waste of the mountain-slopes, broken off by rills and torrents, and carried by them into the main river, slowly drifts down-stream in the form of gravel-banks, until, scattered and rent asunder in a thousand ways, it finally takes permanent form as light-green islands, which are soon covered and protected with a dense coat of vegetation. As every zone of geologic for
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