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Morris Canal
The Morris Canal (1829–1924) was a 107-mile (172 km) common carrier anthracite coal canal across northern New Jersey that connected the two industrial canals in Easton, Pennsylvania across the Delaware River from its western terminus at Phillipsburg, New Jersey to New York Harbor and New York City through its eastern terminals in Newark and on the Hudson River in Jersey City. The canal was sometimes called the Morris and Essex Canal, in error, due to confusion with the nearby and unrelated Morris and Essex Railroad.
With a total elevation change of more than 900 feet (270 m), the canal was considered an ingenious technological marvel for its use of water-driven inclined planes, the first in the United States, to cross the northern New Jersey hills.
It was built primarily to move coal to industrializing eastern cities that had stripped their environs of wood. Completed to Newark in 1831, the canal was extended eastward to Jersey City between 1834 and 1836. In 1839, hot blast technology was married to blast furnaces fired entirely using anthracite, allowing the continuous high-volume production of plentiful anthracite pig iron.
The Morris Canal eased the transportation of anthracite from Pennsylvania's Lehigh Valley to northern New Jersey's growing iron industry and other developing industries adopting steam power in New Jersey and the New York City area. It also carried minerals and iron ore westward to blast furnaces in western New Jersey and Allentown and Bethlehem in the Lehigh Valley until the development of Great Lakes iron ore caused the trade to decline.
The Morris Canal remained in heavy use through the 1860s. But railroads had begun to eclipse canals in the United States, and in 1871, it was leased to the Lehigh Valley Railroad.
Like many enterprises that depended on anthracite, the canal's revenues dried up with the rise of oil fuels and truck transport. It was taken over by the state of New Jersey in 1922, and formally abandoned in 1924.
While the canal was largely dismantled in the following five years, portions of it and its accompanying feeders and ponds have been preserved. A statewide greenway for cyclists and pedestrians is planned, beginning in Phillipsburg, traversing Warren, Sussex, Morris, Passaic, Essex, and Hudson Counties and including the old route through Jersey City. The canal was added to the National Register of Historic Places on October 1, 1974, for its significance in engineering, industry, and transportation. The boundary was increased in 2016 to include the Lake Hopatcong station in Landing.
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.
Morris Canal
The Morris Canal (1829–1924) was a 107-mile (172 km) common carrier anthracite coal canal across northern New Jersey that connected the two industrial canals in Easton, Pennsylvania across the Delaware River from its western terminus at Phillipsburg, New Jersey to New York Harbor and New York City through its eastern terminals in Newark and on the Hudson River in Jersey City. The canal was sometimes called the Morris and Essex Canal, in error, due to confusion with the nearby and unrelated Morris and Essex Railroad.
With a total elevation change of more than 900 feet (270 m), the canal was considered an ingenious technological marvel for its use of water-driven inclined planes, the first in the United States, to cross the northern New Jersey hills.
It was built primarily to move coal to industrializing eastern cities that had stripped their environs of wood. Completed to Newark in 1831, the canal was extended eastward to Jersey City between 1834 and 1836. In 1839, hot blast technology was married to blast furnaces fired entirely using anthracite, allowing the continuous high-volume production of plentiful anthracite pig iron.
The Morris Canal eased the transportation of anthracite from Pennsylvania's Lehigh Valley to northern New Jersey's growing iron industry and other developing industries adopting steam power in New Jersey and the New York City area. It also carried minerals and iron ore westward to blast furnaces in western New Jersey and Allentown and Bethlehem in the Lehigh Valley until the development of Great Lakes iron ore caused the trade to decline.
The Morris Canal remained in heavy use through the 1860s. But railroads had begun to eclipse canals in the United States, and in 1871, it was leased to the Lehigh Valley Railroad.
Like many enterprises that depended on anthracite, the canal's revenues dried up with the rise of oil fuels and truck transport. It was taken over by the state of New Jersey in 1922, and formally abandoned in 1924.
While the canal was largely dismantled in the following five years, portions of it and its accompanying feeders and ponds have been preserved. A statewide greenway for cyclists and pedestrians is planned, beginning in Phillipsburg, traversing Warren, Sussex, Morris, Passaic, Essex, and Hudson Counties and including the old route through Jersey City. The canal was added to the National Register of Historic Places on October 1, 1974, for its significance in engineering, industry, and transportation. The boundary was increased in 2016 to include the Lake Hopatcong station in Landing.
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.