Picture-Writing of the American Indians: Tenth Annual Report of the Bureau of Ethnology to the Secretary of the Smithsonian Institution, 1888-89, Government Printing Office, Washington, 1893, pages 3-822Mallery, Garrick
History
Picture-Writing of the American Indians: Tenth Annual Report of the Bureau of Ethnology to the Secretary of the Smithsonian Institution, 1888-89, Government Printing Office, Washington, 1893, pages 3-822
Mallery, Garrick
Picture-writing, Indian
The Fairy rocks, as distinct from others in the lake, are three in
number, and are situated on the east side of Kejimkoojik lake and south
of the entrance to Fairy lake. The northernmost of the three rocks is
immediately at the entrance, the westernmost and central rock showing
but a small surface at high water and at the highest stage of the water
being entirely submerged. Three other inscribed rocks are about 2 miles
south of these, at Piels (a corruption of Pierre’s) point, opposite an
island called Glodes or Gload island, so named from a well-known Micmac
family. These rocks are virtually a continuation of the same formation
with depressions between them. Two other localities in the vicinity
where the rocks are engraved, as hereafter described, are at Fort Medway
river and Georges lake. As they are all of the same character, on the
same material, and were obviously made by the same people, they are all
classed together, when referred to in this paper, as at Kejimkoojik
lake. All of these rocks are of schistose slate of the Silurian
formation, and they lie with so gentle a dip that their magnitudes vary
greatly with a slight change in the height of the water. On August 27,
1887, when, according to the reports of the nearest residents, the water
was one foot above the average summer level, the unsubmerged portion of
the central rock then surrounded by water was an irregular oval, the
dimensions of which were 47 by 60 feet. The highest points of the Fairy
rocks at that date were no more than three and few were more than two
feet above the surface of the water. The inclination near the surface is
so small that a falling of the water of one foot would double the extent
of that part of the surface which, by its smoothness and softness,
is adapted to engraving. The inclination at Piels point is steeper,
but still allows a great variation of exposed surface in the manner
mentioned.
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