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rsory inspection of any of the maps of the territory in question, that the line claimed for Great Britain in the argument before the King of the Netherlands fulfills no more than one of the two conditions, while that of Messrs. Featherstonhaugh and Mudge fulfills neither; and as the line claimed on the part of the United States is denied to be capable of meeting the terms of the treaty of 1783 by Great Britain, there is no line that, in conformity with the British argument, can be drawn within the disputed territory or its vicinity that will comply with either of the conditions. This is as well and as distinctly shown in the map of Mitchell as in the map of the British commission. It would therefore appear, if, these views be correct, that the framers of the treaty of 1783 went through the solemn farce of binding their respective Governments to a boundary which they well knew did not and could not exist. V.--NORTHWEST HEAD OF CONNECTICUT RIVER. The true mode of determining the most northwesterly of any two given points need no longer be a matter of discussion. It has already been a matter adjudicated and assented to by both Governments, in the case of the Lake of the Woods. The point to be considered as most to the northwest is that which a ruler laid on a map drawn according to Mercator's projection in a direction northeast and southwest and moved parallel to itself toward the northwest would last touch. In this view of the subject the Eastern Branch of the Connecticut, which forms the lake of that name, is excluded, for its source, so far from lying to the northwest of those of the other two branches which have been explored, actually lies to the south of the source of the Indian Stream. The question must therefore lie between the two others, and it is as yet impossible to decide which of them is best entitled to the epithet, as their sources lie very nearly in the same northeast and southwest rhomb line. Another circumstance would, however, render the decision between them easy. The forty-fifth parallel of latitude, as laid out by the surveyors of the Provinces of Quebec and New York in conformity with the proclamation of 1763, crosses Halls Stream above its junction with the united current of the other two. In this case the latter is the Connecticut River of the treaty of 1783, and Halls Stream, which has not yet joined it, must be excluded. The parallel, as corrected by the united operations of the British
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