Several years ago Mr. H. R. Taylor, of Machias, who made the original sketch in 1868 and kindly furnished it to the Bureau of Ethnology, applied to a resident Indian there (Peter Benoit, then nearly 80 years old) for assistance in deciphering the characters. He gave little information, but pointed out that the figures must not all be read “from one side only,” thus, the one near the center of the sketch, which seen from the south was without significance, became from the opposite point a squaw with sea fowl on her head, denoting, as he said, “that squaw had smashed canoe, saved beaver-skin, walked one-half moon all alone toward east, just same as heron wading alongshore.” Also that the three lines below the figure mentioned, which together resemble a bird track or a trident, represent the three rivers, the East, West, and Middle rivers of Machias, which join not far above the locality. The mark having a rough resemblance to a feather, next on the right of this river-sign, is a fissure in the rock. Most of the figures of human beings and other animals are easily recognizable. Peckings of a character similar to those on the Picture rock at Clarks point, above described, were found and copied 600 feet south of it at high-water mark on a rock near Birch point. Others were discovered and traced on a rock on Hog island, in Holmes bay, a part of Machias bay. All these petroglyphs were without doubt of Abnaki origin, either of the Penobscot or the Passamaquoddy divisions of that body of Indians. The rocks lay on the common line of water communication between those divisions and were convenient as halting places. MARYLAND. In the Susquehanna river, about half a mile south of the state line, is a group of rocks, several of the most conspicuous being designated as the “Bald Friars.” Near by are several mound-shaped bowlders of the so-called “nigger-head” rock, which is reported as a dark-greenish chlorite schist. Upon the several bowlders are deep sculpturings, apparently finished by rubbing the depression with stone, or wood and sand, thus leaving sharp and distinct edges to the outlines. Some of these figures are an inch in depth, though the greater number are becoming more and more eroded by the frequent freshets, and by the running ice during the breaking up in early spring of the frozen river. The following account is given by Prof. P. Frazer (_a_): Passing the Pennsylvania state line one reaches the southern barren serpentine rocks, which are in general tolerably level for a considerable distance. About 700 yards, or 640 meters, south of the line, on the river shore, are rocks which have been named the Bald Friars. French’s tavern is here, at the mouth of a small stream which empties into the Susquehanna. About 874 yards (800 meters) south of this tavern are a number of islands which have local names, but which are curious as containing inscriptions of the aborigines.