Indeed, it appears in every commission to the governor of Nova Scotia and New Brunswick from 1763 to 1784, and after the treaty of peace of 1783, that the Province of Nova Scotia extended to the southern boundary of the Province of Quebec. It then irresistibly and inevitably follows that a west line from the Bay de Chaleurs, intersecting a due north line from the monument, is the identical northwest angle. Now a line from Mars Hill direct to Cape Rosiers, instead of being easterly, would be north of northeast, crossing the Bay de Chaleurs. But passing along its north coast, as the proclamation provides, the line from this Mars Hill must be more northerly still. Indeed, the pretense that a pyramidal spur or peak, such as this hill, should constitute the range of highlands mentioned in the treaty is so utterly visionary that it is entitled to no sort of respect.
We may now by these facts and reflections give this inquiry a right direction, to wit, to the ascertainment of the north boundary of Nova Scotia, which is the southern boundary of Canada. We have always been lured from this by the British negotiators to the left or west of this north line from the monument.
No one who is in the least conversant with the subject can suppose for a moment that this northwest angle can be found in such a direction. The question for us is, Are there any highlands north of the Bay de Chaleurs extending in a western direction toward a north line drawn from the monument? If this line westerly from the bay be not distinctly marked so far as to intersect this north line, the principle is to extend it in the same direction to the place of intersection; that is, if the line between Nova Scotia and Canada is west to within, say, 30 miles of the north line from the monument, and the rest of the way is indefinite or obscure, extend it on in the same direction until you form a point of intersection, and this will be the northwest angle of Nova Scotia. But the truth is, the highlands are there, and have been found in running due north from the monument. The elevations were taken by the British surveyor from the source of the St. Croix, at the monument, to the first waters of the Restigouche; and at Mars Hill, 40 miles, the summit of this isolated sugar loaf was 1,100 feet, and at the termination of the survey at the Restigouche waters, 100 miles farther, the elevation was I,600 feet; consequently the summit of Mars Hill, 1,100 feet above the waters