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See also:DELAWARE See also:RIVER , a stream of the See also:Atlantic slope of the See also:United States; See also:meeting See also:tide-See also:water at Trenton, New See also:Jersey,130 M. above its mouth. Its See also:total length, from the See also:head of the longest See also:branch to the capes, is 410 m., and above the head of the See also:bay its length is 36o m- It constitutes in See also:part the boundary between See also:Pennsylvania and New See also:York, the boundary between New Jersey and Pennsylvania, and, for a few See also:miles, the boundary between Delaware and New Jersey. The See also:main, See also:west or See also:Mohawk branch rises in Schoharie See also:county, N.Y., about 1886 ft. above the See also:sea, and flows tortuously through the See also:plateau in a deep trough until it emerges from the Catskills. Other branches rise in See also:Greene and Delaware counties. In the upper portion of its course the varied scenery of its hilly and wooded See also:banks is exquisitely beautiful. After leaving the mountains and plateau, the river flows down broad Appalachian valleys, skirts the Kittatinny range, which it crosses at Delaware Water-See also:Gap, between nearly See also:vertical walls of See also:sandstone, and passes through a quiet and charming See also:country of See also:farm and See also:forest, diversified with plateaus and escarpments, until it crosses the Appalachian See also:plain and enters the hills again at See also:Easton, Pa. From this point it is flanked at intervals by See also:fine hills, and in places by cliffs, of which the finest are the Hockamixon Rocks, 3 M. See also:long and above 200 ft. high. At Trenton there is a fall of 8 ft. Below Trenton the river becomes a broad, sluggish inlet of the sea, with many marshes along its See also:side, widening steadily into its See also:great See also:estuary, Delaware Bay. Its main tributaries in New York are Mongaup and Neversink See also:rivers and Callicoon See also:Creek; from Pennsylvania, Lackawaxen, Lehigh and Schuylkill rivers; and from New Jersey, Rancocas Creek and Musconetcong and See also:Maurice rivers. See also:Commerce was once important on the upper river, but only before the beginning of railway competition (1857). The Delaware See also:division of the Pennsylvania See also:Canal, See also:running parallel with the river from Easton to See also:Bristol, was opened in 183o. A canal from Trenton to New See also:Brunswick unites the See also:waters of the Delaware and Raritan rivers; the See also:Morris and the Delaware and See also:Hudson canals connect the Delaware and Hudson rivers; and the Delaware and Chesapeake canal joins the waters of the Delaware with those of the Chesapeake Bay. The mean tides below See also:Philadelphia are about 6 ft. The magnitude of the commerce of Philadelphia has made the improvements of the river below that See also:port of great,importance. Small improvements were attempted by Pennsylvania as See also:early as 1771, but apparently never by New Jersey. The See also:ice floods at Easton are normally 10 to 20 ft., and in 1841 attained a height of 35 ft. These floods constitute a serious difficulty in the improvement of the See also:lower river. In the " project of 1885 " the United States See also:government undertook systematically the formation of a 26-ft. channel 600 ft. wide from Philadelphia to deep water in Delaware Bay; $1,532,688.81 was expended—about $200,000 of that amount for maintenance—before the 1885 project was superseded by a See also:paragraph of the River and Harbor See also:Act of the 3rd of See also: Additional information and CommentsThere are no comments yet for this article.
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