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Rh and after that become so small and sparse that a stranger riding across the line could hardly remark that they were artificially disposed, but would merely regard it as a stony piece of land. They again cease entirely before we reach the brook, to recommence at Kerlescant, where thirteen rows are found; but these are composed of stones of less dimensions and more irregularly spaced than those at Maenec, and die out much more rapidly. At a distance of less than 500 yards from the head of the column they disappear entirely. It may be suggested that these gaps arise from the stones having been removed for agricultural and other purposes. I think, however, that any one who carefully examines the spot will be convinced that we really now possess all, or nearly all, that were ever placed here. They are thickest and best preserved in the village of Maenec, and at Kermario, where buildings are most frequent, and they disappear exactly in those places where there are no buildings or walls, but where the ground is an open, barren heath, without roads, and whence it would be very difficult to transport them; and in so stony a country it is very improbable that the attempt would be made. Besides this, the gradual way in which they diminish in size before disappearing shows a regularity of design, regarding which there can be no mistake. In addition to this, the heads of the three divisions are all marked by monuments of different kinds, but which are easily recognizable. At the head of the Maenec division there is a curvilinear enclosure of smaller stones, none of them being more than 6 feet in height, but set much closer together than the rows (woodcut No. 136). It probably was once complete, and, if so, joined the centre stone row. At Kermario, a dolmen stands in front of the alignment, not remarkable for its size, but conspicuous from its position; and at Kerlescant there is a quadrangular enclosure, three sides of which are composed of stones of smaller size and set closely together, like those at Maenec. The fourth side is formed by a tumulus or long