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t on sanitation or fire prevention. Nor, indeed, would it achieve completeness, even on the artistic side, were it not for its crowning feature. Far off, over the roofs and above them, making an apex to the composition, and giving to the whole picture a background of beauty and of ancient dignity, rises the graceful white-columned cupola of Vicksburg's old stone courthouse, partially obscured by a feathery green tree top, hinting of space and foliage upon the summit of the hill. * * * * * Pamphlets on Vicksburg, issued by railroad companies for the enticement of tourists, give most of their space to the story of the campaign leading to Grant's siege of Vicksburg and to descriptions of the various operations in the siege--the battlefield, now a national military park, being considered the city's chief object of interest. Though I am not constitutionally enthusiastic about seeing battlefields, I must admit that I found the field of Vicksburg engrossing. The siege of a small city presents a comparatively simple and compact military problem which is, therefore, comprehensible to the civilian mind, and in addition to this the Vicksburg battlefield is splendidly preserved and marked, so that the visitor may easily reconstruct the conflict. The park, which covers the fighting area, forms a loose crescent-shaped strip over the hills which surround the city, its points abutting on the river above and below. The chief drives of the park parallel each other, the inner one, Confederate Avenue, following, as nearly as the hills permit, the city's line of defense, while the other, Union Avenue, forms an outer semicircle and follows, in a similar manner, the trenches of the attacking forces. That the battlefield is so well preserved is due in part to man and in part to Nature. Many of the hills of Warren County, in which Vicksburg is situated, are composed of a curious soft limy clay, called marl, which, normally, has not the solidity of soft chalk. Marse Harris Dickson, who knows more about Vicksburg--and also about negroes, common law, floods, funny stories, geology, and rivers--than any other man in Mississippi, tells me that this marl was deposited by the river, in the form of silt, centuries ago, and that it was later thrown up into hills by volcanic action. He did not live in Vicksburg when this took place, but deduces his facts from the discovery of the remains of shellfish in the soil
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