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their existence, except the names of places. Now and then, as at Indiantown, near Princeton, you are shown the holes in the ground where they stored their maize, and sometimes on the borders of the rivers you see the trunks of trees which they felled, evidently hacked by their tomahawks, but perhaps the most remarkable of their remains are the paths across the prairies or beside the large streams, called Indian trails--narrow and well-beaten ways, sometimes a foot in depth, and many of them doubtless trodden for hundreds of years. As we went down the ridge upon which stands Dad Joe's Grove, we saw many boulders of rock lying on the surface of the soil of the prairies. The western people, naturally puzzled to tell how they came there, give them the expressive name of "lost rocks." We entered a forest of scattered oaks, and after travelling for half an hour reached the Winnebago Swamp, a tract covered with tall and luxuriant water-grass, which we crossed on a causey built by a settler who keeps a toll-gate, and at the end of the causey we forded a small stream called Winnebago Inlet. Crossing another vast prairie we reached the neighborhood of Dixon, the approach to which was denoted by groves, farm-houses, herds of cattle, and inclosed corn fields, checkering the broad green prairie. Dixon, named after an ancient settler of the place still living, is a country town situated on a high bank of Rock River. Five years ago two log-cabins only stood on the solitary shore, and now it is a considerable village, with many neat dwellings, a commodious court-house, several places of worship for the good people, and a jail for the rogues, built with a triple wall of massive logs, but I was glad to see that it had no inmate. Rock River flows through high prairies, and not, like most streams of the West, through an alluvial country. The current is rapid, and the pellucid waters glide over a bottom of sand and pebbles. Its admirers declare that its shores unite the beauties of the Hudson and of the Connecticut. The banks on either side are high and bold; sometimes they are perpendicular precipices, the base of which stands in the running water; sometimes they are steep grassy or rocky bluffs, with a space of dry alluvial land between them and the stream; sometimes they rise by a gradual and easy ascent to the general level of the region, and sometimes this ascent is interrupted by a broad natural terrace. Majestic trees grow solit
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