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tantially accomplished. I do not mean to allege that the work had been completed in the best manner, but it was sufficient for all practical purposes. The St. Clair flats are formed by the St. Clair River, which empties into the lake of that name by several mouths, and which forms a bar or shoal on which in its natural state there is not more than 6 or 7 feet of water. This shoal is interposed between the mouth of the river and the deep water of the lake, a distance of 6,000 feet, and in its natural condition was a serious obstruction to navigation. The obvious remedy for this was to deepen a channel through these flats by dredging, so as to enable vessels which could navigate the lake and the river to pass through this intermediate channel. This object had been already accomplished by previous appropriations, but without my knowledge, when the bill was presented to me. Captain Whipple, of the Topographical Engineers, to whom the expenditure of the last appropriation of $45,000 for this purpose in 1856 was intrusted, in his annual report of the 1st October, 1858, stated that the dredging was discontinued on the 26th August, 1858, when a channel had been cut averaging 275 feet wide, with a depth varying from 12 to 15-1/2 feet. He says: So long as the lake retains its present height we may assume that the depth in the channel will be at least 13-1/2 feet. With this result, highly creditable to Captain Whipple, he observes that if he has been correctly informed "all the lake navigators are gratified." Besides, afterwards, and during the autumn of 1858, the Canadian Government expended $20,000 in deepening and widening the inner end of the channel excavated by the United States. No complaint had been made previous to the passage of the bill of obstructions to the commerce and navigation across the St. Clair flats. What, then, was the object of the appropriation proposed by the bill? It appears that the surface of the water in Lake St. Clair has been gradually rising, until in 1858 it had attained an elevation of 4 feet above what had been its level in 1841. It is inferred, whether correctly or not it is not for me to say, that the surface of the water may gradually sink to the level of 1841, and in that event the water, which was, when the bill passed, 13-1/2 feet deep in the channel, might sink to 9-1/2 feet, and thus obstruct the passage. To provide for this contingency, Captain Whipple suggested "the propriety
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