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There is very little true granite in New England, what is taken for it commonly being syenite, a rock indeed that differs from granite only in the substitution of hornblend for mica. The so-called Quincy granite is a finer sort of syenite, and the White Mountains are composed of syenite capped with granite.

It was made up of quartz, feldspar, and mica, and there were also some isolated specimens of pyrites, hornblend, tourmaline, and serpentine. On the south side of the work, just west of Ninth Avenue, there were excellent examples of "contortions" of veins of quartz in the darker rock. On the east side of Ninth Avenue, near the north end of the work, glacial marks were found on the rock surface.

At the height of land dividing the waters that flow in different directions, into Esquimaux and Ungava Bays, the formation becomes syenitic schist, and continues so to within a short distance of the great fall on Hamilton River; when syenite succeeds; then gneiss; and along the shores of Esquimaux Bay syenitic gneiss, and pure quartz: lumps of black and red hornblend are met with everywhere.

Many fragments of red, gray, and purple basalt and porphyry were met with along the beach; talcose rock and slate, syenite, hornblend, quartz, both compact and slaty, with chalcedony, were found in pieces and large pebbles.

Further off on the same side, at a distance, the rocks continued in a range, instead of being scattered about like so many sugar-loaves placed upon a plane, as mountains are represented to children. To-day the granite became stratified, or gneiss; there were also some fine specimens of hornblend. One of our Kailouee friends amused himself on the road by giving a good beating to his female slave.