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ported by any of his brethren, and it seemed to me to be morally impossible that, without assistance, he could take half a dozen fellows, who were with difficulty restrained from whipping each other. However, his hand seemed to be as potent as the famous magic wand of Armida, for on placing it on the shoulders of the combatants, they fell into the ranks, and marched off with him as quietly as if they had been sheep. The rationale of the matter is this: those men had all exercised the franchise, if not in the election of these very constables, of others, and they therefore not only considered it to be their duty to support the constable's authority, but actually felt a strong inclination to do so. Because they _knew_ that the authority he exercised was only delegated to him by themselves, and that, in resisting him, they would resist their own sovereignty. Even in large towns in the western country, the constable has no men under his command, but always finds most powerful allies in the citizens themselves, whenever a lawless scoundrel, or a culprit is to be captured. At Flemingsburg I saw an Albino, a female about fourteen years old. Her parents were clear negros, of the Congo or Guinea race, and in every thing but colour she perfectly resembled them. Her form, face, and hair, possessed the true negro characteristics--curved shins, projecting jaw, retreating forehead, and woolly head. The skin was rather whiter than that of the generality of Europeans, but was deficient in glossiness, and although perfectly smooth, had a dry appearance. The wool on the head was of a light flaxen colour, and the iris of the eye was of a reddish-blue tinge. Her eyes were so weak as to bear with difficulty the glare of day. Most Albinos are dim sighted until twilight, when they appear to have as perfect vision as persons with the strongest sight, and in many cases, even more acute. This individual had evidently weak sight, as the eyelids were generally half closed, and she always held her head down during day light. Near the banks of the Ohio, full three hundred miles from the sea, I found conglomerations of marine shells, mixed with siliceous earth; and in nearly all the runs throughout Kentucky, limestone pebbles are found, bearing the perfect impressions of the interior of shells. The most abundant proofs are every where exhibited, that at one period the vast savannahs and lofty mountains of the New world were submerged; and perhaps
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