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Diamond Brook Bass Brook | |
---|---|
Location | |
Country | United States |
State | New Jersey |
County | Bergen |
Physical characteristics | |
Source | |
• location | Ridgewood, Bergen County, New Jersey, United States |
• coordinates | 40°58′40.89″N74°7′58.36″W / 40.9780250°N 74.1328778°W |
• elevation | 118 ft (36 m) |
Mouth | Passaic River |
• location | Fair Lawn, Bergen County, New Jersey, United States |
• coordinates | 40°56′26.87″N74°8′36.05″W / 40.9407972°N 74.1433472°W |
• elevation | 27 ft (8.2 m) |
Length | 3 mi (4.8 km) |
Diamond Brook, also known as Bass Brook, is a tributary of the Passaic River which flows south through a section of Bergen County in New Jersey, United States. Heading up the brook from the Passaic River, one encounters the boroughs of Fair Lawn and Glen Rock, as well as the village of Ridgewood.
Diamond Brook passes through a largely suburban setting, though its southern end runs under an industrial complex in Fair Lawn before terminating at the Passaic River. The head of Diamond Brook is located south of Godwin Ave in Ridgewood, near the border of Midland Park. Diamond Brook is considered part of the Goffle Brook drainage basin, but it has no junctions with Goffle Brook and is partly separated from it by another brook, Stevenson Brook, which flows south to the Passaic River between Goffle Brook and Diamond Brook in Hawthorne.
Another brook east of Diamond Brook, Little Diamond Brook, is considered to be in part of the same drainage basin as Diamond Brook. Little Diamond Brook and Diamond Brook terminate at the Passaic River within about five hundred feet of each other.
Diamond Brook was historically known as Bass Brook. It once traveled through a series of springs and wetlands along the western edge of Glen Rock. In the 21st century, only a few wetlands remain intact, with two preserved as parts of the Glen Rock Arboretum and Diamond Brook Park. Some natural springs also remain intact behind Orchard School in Ridgewood.
In the 1870s, Diamond Brook’s gradation was sufficient to support a water wheel operated by the Marinus Lumber Mill in Glen Rock. When the mill finally closed the wheel and its accompanying machinery were too cumbersome to move. Today the wheel remains where it once operated, buried beneath the street near the intersection of Rock Road and the Boulevard. [1]
New Jersey Meadowlands, also known as the Hackensack Meadowlands after the primary river flowing through it, is a general name for a large ecosystem of wetlands in northeastern New Jersey in the United States, a few miles to the west of New York City. During the 20th century, much of the Meadowlands area was urbanized, and it became known for being the site of large landfills and decades of environmental abuse. A variety of projects began in the late 20th century to restore and conserve the remaining ecological resources in the Meadowlands.
The Passaic River is a river, approximately 80 miles (130 km) long, in Northern New Jersey. The river in its upper course flows in a highly circuitous route, meandering through the swamp lowlands between the ridge hills of rural and suburban northern New Jersey, called the Great Swamp, draining much of the northern portion of the state through its tributaries.
Lake Passaic was a prehistoric proglacial lake that existed in northern New Jersey in the United States at the end of the last ice age approximately 19,000–14,000 years ago. The lake was formed of waters released by the retreating Wisconsin Glacier, which had pushed large quantities of earth and rock ahead of its advance, blocking the previous natural drainage of the ancestral Passaic River through a gap in the central Watchung Mountains. The lake persisted for several thousand years as melting ice and eroding moraine dams slowly drained the former lake basin. The effect of the lake's creation permanently altered the course of the Passaic River, forcing it to take a circuitous route through the northern Watchung Mountains before spilling out into the lower piedmont.
The Watchung Mountains are a group of three long low ridges of volcanic origin, between 400 and 500 feet high, lying parallel to each other in northern New Jersey in the United States. The name is derived from the American Native Lenape name for them, Wach Unks. In the 18th century, the Euro-American settlers also called them the Blue Mountains or Blue Hills. The Watchung Mountains are known for their numerous scenic vistas overlooking the skylines of New York City and Newark, New Jersey, as well as their isolated ecosystems containing rare plants, endangered wildlife, rich minerals, and globally imperiled trap rock glade communities. The ridges traditionally contained the westward spread of urbanization, forming a significant geologic barrier beyond the piedmont west of the Hudson River; the town of Newark, for example, once included lands from the Hudson to the base of the mountains. Later treaties moved the boundary to the top of the mountain, to include the springs.
The Hackensack River is a river, approximately 45 miles (72 km) long, in the U.S. states of New York and New Jersey, emptying into Newark Bay, a back chamber of New York Harbor. The watershed of the river includes part of the suburban area outside New York City just west of the lower Hudson River, which it roughly parallels, separated from it by the New Jersey Palisades. It also flows through and drains the New Jersey Meadowlands. The lower river, which is navigable as far as the city of Hackensack, is heavily industrialized and forms a commercial extension of Newark Bay.
The Rahway River is a river in Essex, Middlesex, and Union Counties, New Jersey, United States, The Rahway, along with the Elizabeth River, Piles Creek, Passaic River, Morses Creek, the Fresh Kills River, has its river mouth at the Arthur Kill.
Hatfield Swamp is a fresh water wetland area in the U.S. state of New Jersey, forming what might be considered the "second bank" of the Passaic River between Morris and Essex counties.
The Bergen County Line is a commuter rail line and service owned and operated by New Jersey Transit in the U.S. state of New Jersey. The line loops off the Main Line between the Meadowlands and Glen Rock, with trains continuing in either direction along the Main Line. It is colored on NJT system maps in grey, and its symbol is a cattail, which are commonly found in the Meadowlands where the line runs.
Bourne Eau is a short river which rises from an artesian spring in the town of Bourne in Lincolnshire, England, and flows in an easterly direction to join the River Glen at Tongue End. Within the town, it once powered three water mills, one of which is now a heritage centre. At Eastgate, it becomes much wider as it was navigable in the 18th and 19th centuries, and this was the location of the terminal basin. Below the town it is an embanked river, as its normal level is higher than that of the surrounding Fens. Navigation ceased in the 1860s and the river now forms an important part of the drainage system that enables the surrounding fen land to be used for agriculture.
The Saddle River flows south through much of Bergen County, New Jersey. The river runs through densely populated suburban areas for much of its course. The river takes its name from the river near Saddell in Argyll and Bute in Scotland.
Ho-Ho-Kus Brook is a tributary of the Saddle River in Bergen County, New Jersey, in the United States.
Stevenson Brook is a tributary of the Passaic River in Hawthorne, Passaic County, New Jersey in the United States.
Goffle Brook is a tributary of the Passaic River which flows south through a section of Passaic County and Bergen County in New Jersey and drains the eastern side of the First Watchung Mountain. Heading up the brook from the confluence with the Passaic River, one encounters the borough of Hawthorne, the village of Ridgewood, the borough of Midland Park, and the township of Wyckoff.
Little Diamond Brook is a tributary of the Passaic River which flows south through a section of Bergen County in New Jersey. Heading up the approximately two mile long brook from the Passaic River, one encounters the towns of Fair Lawn and Glen Rock.
County Route 507 is a county highway in the U.S. state of New Jersey. The highway extends 28.37 mi (45.66 km) from Harrison Avenue on the Kearny-Harrison town line to the New York state line in Mahwah. Between Ho-Ho-Kus and Mahwah, this highway is known as Franklin Turnpike. At its northern terminus, County Route 507 continues north into New York as Orange Avenue, which is a portion of U.S. Route 202 (US 202).
Saddle River County Park is a 596-acre (2.41 km2) county park in Bergen County, New Jersey, United States, stretching from Ridgewood to Rochelle Park, and extends out to Glen Rock. The park is located along the Saddle River and consists of five sections, all of which are connected by a paved path that is open to both pedestrians and bicyclists.
Molly Ann Brook is a tributary of the Passaic River which flows south between the northern ranges of First Watchung Mountain and Second Watchung Mountain in Passaic County and Bergen County, New Jersey. Traveling north from its confluence with the Passaic River, Molly Ann Brook passes through the city of Paterson and the boroughs of Haledon, Prospect Park, North Haledon and Franklin Lakes.
Goffle Brook Park is a public, county park spanning much of the length of Goffle Brook through the borough of Hawthorne in Passaic County, New Jersey, United States. Since its designation and construction between 1930 and 1932, the park has served to protect the waters of Goffle Brook while at the same time providing recreational opportunities to the residents of Passaic County and nearby Bergen County. Goffle Brook Park has been included in the National Register of Historic Places since 2002.
Goffle Hill, also referred to as Goffle Mountain and historically known as Totoway Mountain and Wagaraw Mountain, is a range of the trap rock Watchung Mountains on the western edge of the Newark Basin in northern New Jersey. The hill straddles part of the border of Bergen County and Passaic County, underlying a mostly suburban setting. While hosting patches of woodlands, perched wetlands, and traprock glades, the hill is largely unprotected from development. Extensive quarrying for trap rock has obliterated large tracts of the hill in North Haledon, and Prospect Park. Conservation efforts seeking to preserve undeveloped land, such as the local Save the Woods initiative (2007–present), are ongoing.