Description
On the canal's western end, at Phillipsburg, a cable ferry allowed Morris Canal boats to cross the Delaware River westward to Easton, Pennsylvania, and travel up the Lehigh Canal to Mauch Chunk, in the anthracite coal regions, to receive their cargoes from the mines. From Phillipsburg, the Morris Canal ran eastward through the valley of the Musconetcong River, which it roughly paralleled upstream to its source at Lake Hopatcong, New Jersey's largest lake. From the lake the canal descended through the valley of the Rockaway River to Boonton, eventually around the northern end of Paterson's Garret Mountain, and south to its 1831 terminus at Newark on the Passaic River. From there it continued eastward across Kearny Point and through Jersey City to the Hudson River. The extension through Jersey City was at sea level and was supplied with water from the lower Hackensack River.
With its two navigable feeders, the canal was 107 mi (172 km) long. Its ascent eastward from Phillipsburg to its feeder from Lake Hopatcong was 760 ft (232 m), and the descent from there to tidewater was 914 ft (279 m). The surmounting of the height difference was considered a major engineering feat of its day, accomplished through 23 locks and 23 inclined planes — essentially, short railways that carried canal boats in open cars uphill and downhill using water-powered winchs. Inclined planes required less time and water than locks, although they were more expensive to build and maintain.
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