Crystal Lake (also known Jefferd-Leisler Mill Pond and Ice Pond) [1] was located in the village of New Rochelle in Westchester County, New York. It originally supplied early colonial mills with water power. It was fed by Stephenson Brook, which rises just north of Paine Lake and drains the large watershed adjacent to North Avenue from beyond Quaker Ridge Road.
The lake appears to have existed as a natural sheet of water, near the end of the brook. It had two outlets into Long Island Sound, one at the present Stephenson Boulevard, and the other at the east side of Lispenard Avenue. These outlets had an abrupt fall in the few yards between the lake's south edge and the Long Island Sound shore, of approximately 20–25 ft (6.1–7.6 m). This was the greatest natural fall of any stream emptying into the Sound between New York City and Connecticut. From very early, the value of it for water power was recognized.
According to the 1689 deed from Sir John Pell to Jacob Leisler, representing the Huguenot purchasers of New Rochelle, the area originally came under the ownership of John Jefferd. Jefferd was first to use the water power of this stream, operating a saw-mill and corn-mill until he died in the early eighteenth century. The land later came under the ownership of Jacob Leisler, who made improvements to the lake, including constructing a pool to supply an overshot wheel at the mill, [2] which needed Leisler to alter the route of the Boston Post Road, an action which he was later indicted for in 1711. This pool was south of and beside the lake, and required several new mill-dams and shifting the road to a new route over the lower dam. This raised the level of the lake and flooded a larger area than the natural lake. [3]
In 1734 the property came under the ownership of Anthony Lispenard, who erected an additional saw-mill between the lake and the pool, using the water flowing from the lake into the pool before it was drawn from the pool to the old grist-mill below. By 1750, this saw-mill was changed to a grist-mill as well. By the terms of Lispenard's will, the lake, pool and two mills became the property of his daughter Abigail, wife of Jacobus Bleecker. Before the Revolutionary War, their ownership passed to Andrew Abramse, whose wife was another daughter of Anthony Lispenard, In 1795. the lake and old mill were bought by John Searing and Samuel Wood, both Quakers. No trace has been found after the Revolutionary War of the second mill erected by Lispenard, and all knowledge of its former existence was lost. [4]
In the same year 1795, the owner of the lands adjoining the lake on the north gave permission for to raise the dam and flood more land. By 1806 the former milling industry shifted away from the area; however the lake continued to be used to impound water to operate a tannery, distillery and button factory before the factory burned while being fitted up as an ink factory for Thaddeus Davids in 1846.
An ice industry was soon set up collecting ice when the lake froze. 1849, Thomas Andrews bought the lake and mill property to further develop the ice business. Large ice houses were erected south of the Boston Road in the present City Yard, and a runway was constructed across the road for the ice. This ice industry eventually developed into one of the most important in the region. The ice was all taken for the New York City and Brooklyn markets by the Brooklyn Ice Company, being transported by boats which landed at a dock adjoining the ice-houses. Recognized for the purity of its waters, the lake became known as "Crystal Lake", with its ice marketed as "Crystal Lake Ice." [5]
By now, the very large amount of malarial fevers in the town had become a matter of public concern, and it was continually charged that the origin of the disease was traceable to the stagnant condition of this lake. Whether this was true is questionable, since the town had large areas of undrained swamp lands throughout that were the same or more threat to public health. However, as by now industrial use of the water of the lake had ceased, the water stood undisturbed by drainage for longer than ever before.
The agitation increased so much that a move was made in 1864 to have the Town Board of Health condemn the lake as a public nuisance. Failing in this, the matter was brought before the State Board of Health. The Board, however, refused to act, having found that the lake had large quantities of fish of various kinds as in other fresh water lakes of the state. Additionally, the ice shipped to New York and Brooklyn was found to be of sufficient purity to meet the health test of those cities.
Failing in both of these efforts to compel the abatement of the lake as a public nuisance, John Stephenson, who had been the leader in the movement to rid the neighborhood of the alleged menace to health, and whose estate "Clifford" was near by, bought the lake and adjacent property himself. The dams were then demolished, and the water of the lake and pool let out into Echo Bay. The bed of the lake was reclaimed as dry land and the brook was confined between stone walls constructed to control its flow from the railroad embankment to the Boston Post Road. Streets were then laid out over the lake bottom and the surrounding property was developed as residential parks. In 1913 Stephenson School was built on a high point of land which had been an island in the middle of the lake, "Vineyard Island", known for its wild grapes. Main Street was straightened so that it now runs over the mill's old supply. The brook was enclosed in a culvert and now runs under and along the side of Stephenson Boulevard, and under Main Street into the bay.
The Porter Brook is a river which flows through the City of Sheffield, England, descending over 1,000 feet (300 m) from its source on Burbage Moor to the west of the city to its mouth where it joins the River Sheaf in a culvert beneath Sheffield railway station. Like the other rivers in Sheffield, its steep gradient made it ideal for powering water mills and works associated with the metalworking and cutlery industries, and around 20 dams were constructed over the centuries to facilitate this. At its lower end, it is extensively culverted, but parts of it are gradually being restored to open channels, as part of a daylighting scheme for the city.
Hempstead Lake State Park is a 737-acre (2.98 km2) state park located in Nassau County, New York in the United States. The park is located in West Hempstead and is one of three state parks within the Town of Hempstead. There is a quick-access entrance at exit 18 from the Southern State Parkway. The park contains the largest freshwater lake in Nassau County.
Swartswood State Park is a 3,460-acre (14.0 km2) protected area located in the Swartswood section of Stillwater and Hampton townships in Sussex County, New Jersey, in the United States. Established in 1915 by the state's Forest Park Reservation Commission, it was the first state park established by the state of New Jersey for the purposes of recreation at the state's third-largest freshwater lake. Today, Swartswood State Park is operated and maintained by the New Jersey Division of Parks and Forestry.
The Garrison Grist Mill Historic District is a 13.4-acre (5.4 ha) parcel of Highlands Country Club located at the southwest corner of the intersection of NY 9D and Lower Station Road in Garrison, New York, United States. It contains three buildings, including the titular gristmill (believed to be one of the oldest in the county, and a dam, all dating to the colonial era or the early years of American independence. They are interspersed within the club's golf course, and actually come under the ownership of the Open Space Institute.
The Lispenard–Rodman–Davenport House is a historic residence dating back to the early 18th century located on the Davenport Neck peninsula in New Rochelle, New York. The house is the oldest residential structure in New Rochelle. It was listed on the National Register of Historic Places in 1986.
New Rochelle is a city in Westchester County, New York, United States, in the southeastern portion of the state. The town was settled by Huguenots in 1688 who fled France following their failed rebellions. Many of the settlers were wealthy merchants, artisans and craftsmen from the city of La Rochelle, France, thus influencing the choice of the name of "New Rochelle".
Hidden Lake is one of five villages located within the town of Haddam, Connecticut. It is governed by the bylaws of the Hidden Lake Association.
Stowe Pool is a reservoir located in the city of Lichfield, Staffordshire. Formerly a fishery, Stowe Pool was turned into a reservoir in 1856 by the South Staffordshire Waterworks Co. Before 1856, Stowe Pool existed as a mill pond, with Stowe mill located just to the west of St Chad's Church. Since 1968 the reservoir has not been used for supply and is now a public amenity used for recreation purposes. Stowe Pool is a designated SSSI site as it is home to the native white-clawed crayfish.
The Jacob Leisler Monument is a bronze sculpture created by American artist Solon Borglum and located in the city of New Rochelle, in Westchester County, New York. The monument was erected by the Huguenot Chapter of the Daughters of the American Revolution, and the Huguenot Association of New Rochelle to the memory of Jacob Leisler, 17th-century advocate of the Huguenot settlers and said to be the first chief executive of the province of New York to draw his power directly from the people. The unveiling of the statue on June 24, 1913, was the principal event in the celebration of the 250th anniversary of the founding of New Rochelle. The monument, cast by the Roman Bronze Works, is the only existing statue of Leisler.
The Pocantico River is a nine-mile-long (14 km) tributary of the Hudson River in western central Westchester County, New York, United States. It rises from Echo Lake, in the town of New Castle south of the hamlet of Millwood, and flows generally southwest past Briarcliff Manor to its outlet at Sleepy Hollow. Portions of the towns of Mount Pleasant and Ossining are within its 16-square-mile (41 km2) watershed.
Mahlstedt's Ice Pond, commonly referred to as Huguenot Lake, is a man-made lake located in central New Rochelle in Westchester County, New York. Constructed in 1885, the lake is impounded by the Mahlstedt Reservoir Dam on a tributary of Pine Brook. The dam is of earthen construction and rock fill, with a height of 15 feet (4.6 m) and a length of 7,000 feet (2,100 m). It has a normal surface area of 14 ares (15,000 sq ft), a capacity of 70 acre-feet (86,000 m3), and normal storage of 56 acre-feet (69,000 m3).
Cooper's Corners is a historic section of the city of New Rochelle in Westchester County, New York. For over two centuries Cooper's Corners served as an outpost for residents who lived in rural 'Upper New Rochelle', an area miles from the business center of town.
Titus Mill Pond & New York State Tidal Wetlands is located at the northeastern end of New Rochelle Harbor in the city of New Rochelle in Westchester, New York. The waters in the harbor and pond flow from Long Island Sound, with tides up to eight feet in the inlet and with no fresh water stream entering into it.
Echo Bay is an embayment located off Long Island Sound in the city of New Rochelle in Westchester County, New York. It is an anchorage for small craft and is generally fully occupied during the summer. The depths at the anchorage range from 4 to 15 feet, and launches can anchor in the shallow cove on the northeast side of the harbor, entering between Harrison Islands and the rocky, grassy islet off the northwest side of Echo Island. Vessels frequently anchor between the entrance of Echo Bay and Hicks Ledge, in depths of 20 to 24 feet. On the northwest side of Echo Bay a dredged channel 100 feet wide and 15 feet deep, marked by buoys, leads to the New Rochelle Municipal Marina at Beaufort Point.
Davenport Neck is a peninsula in New Rochelle, New York, extending southwesterly from the mainland into Long Island Sound, and running parallel to the main shore. It divides the city's waterfront into two, with New Rochelle Harbor to the south and southwest, and Echo Bay, to the north and northeast. Glen Island and Neptune Island lie just to the west of the Neck, and Davids and Huckleberry islands lie to the south.
Sheldrake Lake is a man-made body of water located in the north-eastern section of New Rochelle in Westchester County, New York. It has a surface area of 25 acres and formerly served as the water supply for neighboring Larchmont village. The lake is the result of Larchmont Water Company Dam #2 on the Sheldrake River. The dam, constructed in 1935, is masonry with a height of 31 feet (9.4 m) and a length of 1,000 feet (300 m). The dam has a maximum discharge is 987 cubic feet (27.9 m3) per second and drains an area of 2.66 square miles (6.9 km2).
Premium Mill-Pond is located in the communities of New Rochelle and Mamaroneck in Westchester County, New York. The mill-pond is situated northeast of Echo Bay, between the Premium Point peninsula and the mainland. It is fed by the Premium River and is separated from Echo Bay by a dam that creates a waterfall into the harbor.
Tibbetts Brook, originally Tippett's Brook or Tibbitt's Brook, is a stream in the southern portion of mainland New York, flowing north to south from the city of Yonkers in Westchester County into the borough of the Bronx within New York City. Originally emptying into Spuyten Duyvil Creek as part of the Harlem River system, the stream is now partially subterranean, ending above ground at the south end of Van Cortlandt Lake within Van Cortlandt Park. There it proceeds into city sewers, draining into either the northern end of the Harlem River or the Wards Island Water Pollution Control Plant. The brook provides significant watershed to both Van Cortlandt Park at its south end and Tibbetts Brook Park at its north end. There have been modern proposals to daylight the southern portion of the brook back onto the surface.
Oaks Creek is a river that drains Canadarago Lake, which is situated in the north central region of Otsego County, New York. The creek begins by the Hamlet of Schuyler Lake and flows southeast approximately 9.32 miles (15.00 km), dropping only 105 feet (32 m) in elevation, before converging with the Susquehanna River south of the Village of Cooperstown, by the Hamlet of Index. From the source to Oaksville the creek flows along Panther Mountain. Fly Creek is a main tributary, that converges with Oaks Creek south of the Hamlet of Fly Creek.