years before my first visit to Maine. Since then the lumber of the upper Allegash and its lakes has been run down the Penobscot, that is, up the Allegash, which here consists principally of a chain of large and stagnant lakes, whose thoroughfares, or river-links, have been made nearly equally stagnant by damming, and then down the Penobscot. The rush of the water has produced such changes in the canal that it has now the appearance of a very rapid mountain stream flowing through a ravine, and you would not suspect that any digging had been required to persuade the waters of the St. John to flow into the Penobscot here. It was so winding that one could see but little way down.
It is stated by Springer, in his "Forest Life," that the cause of this canal being dug was this. According to the treaty of 1842 with Great Britain, it was agreed that all the timber run down the St. John, which rises in Maine, "when within the Province of New Brunswick . . . . shall be dealt with as if it were the produce of the said Province," which was thought by our side to mean that it should be free from taxation. Immediately, the Province, wishing to get something out of the Yankees, levied a duty on all the timber that passed down the St. John; but to satisfy its own subjects "made a corresponding discount on the stumpage charged those hauling timber from the crown lands." The result was that the Yankees made the St. John run the other way, or down the Penobscot, so that the Province lost both its duty and its water, while the Yankees, being greatly enriched, had reason to thank it for the suggestion.
It is wonderful how well watered this country is. As you paddle across a lake, bays will be pointed out to you, by following up which, and perhaps the tributary
