Goffle Brook Wagaraw Brook | |
---|---|
Location | |
Country | United States |
State | New Jersey |
Counties | Passaic, Bergen |
Physical characteristics | |
Source | Goffle Pond |
• location | Wyckoff, Bergen County, New Jersey, United States |
• coordinates | 40°59′29.25″N74°10′58″W / 40.9914583°N 74.18278°W |
• elevation | 404 ft (123 m) |
Mouth | Passaic River |
• location | Hawthorne, Passaic County, New Jersey, United States |
• coordinates | 40°56′14.21″N74°9′42.65″W / 40.9372806°N 74.1618472°W |
• elevation | 36 ft (11 m) |
Length | 7 mi (11 km) |
Basin features | |
Tributaries | |
• left | Deep Voll Brook |
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.
Goffle Brook has seen human occupation for hundreds of years, as evidenced by abundant Lenape camp sites along its banks. Two such camps are known to have existed near the brook’s mouth, while another two existed about one and a half miles upstream on the east bank. A fifth camp, still locally remembered, sat at the confluence of Deep Voll Brook and Goffle Brook. [1]
During the American Revolutionary War, General Lafayette stationed his men along the banks of the brook. In 1780, Major Lee’s Virginia light horse troop occupied the east bank of the brook, while Lafayette’s light infantry corps occupied the flanks of First Watchung Mountain to the west. Lafayette’s headquarters sat on the western bank of the brook in what is now Goffle Brook Park south of Diamond Bridge Ave in Hawthorne. [2] [3]
Prior to the twentieth century, the brook’s gradation supported saw, grain, and grist mills. It was probably instrumental in initial settlement and farming of the northern Passaic River valley. [4]
In addition to it uses as a drinking water supply and an energy source for mills, the brook has served as a focus for human creativity. New Jersey native William Carlos Williams immortalized the brook in his 1949 poem Spring is Here Again, Sir. The poem opens with the line, Goffle brook of a May day blossoms in the manner of antiquity. [5]
Today, Goffle Brook serves as the centerpiece of Goffle Brook Park and Kings Pond Park, providing fishing and ice skating opportunities to local residents. [6] [7]
The New York, Susquehanna & Western Railway parallels Goffle Brook for the majority of its route through Hawthorne, Ridgewood, Midland Park, and Wyckoff, running roughly along the centerline of the Goffle Brook drainage basin. The railroad crosses the brook only twice, once in Ridgewood and again in Midland Park.
Traveling north along the brook from its mouth, the first tributary encountered is Janes Brook, in Hawthorne. Much of this small stream, which can be found in the wooded, southern section of Goffle Brook Park, was converted to a buried sewer in the twentieth century, but a tiny portion still remains at the surface where it empties into Goffle Brook. The second tributary encountered along Goffle Brook is Deep Voll Brook or Deep Brook (captioned name used by the USGS in 1995), which joins Goffle Brook just north of Goffle Hill Road at the far northern end of Goffle Brook Park in Hawthorne. Deep Voll Brook, which flows from northwest to southeast, is the most significant tributary of Goffle Brook, draining a sizeable portion of the northeastern corner of First Watchung Mountain in Hawthorne and Wyckoff.
Beyond Deep Voll Brook are two smaller streams that join Goffle Brook relatively close to each other. Both of these less significant tributaries appear to be unnamed. After these two tributaries is yet another tiny tributary that drains a small swamp at the head of Kings Pond, a manmade lake in southwest Ridgewood.
Continuing north, past the tributary at Kings Pond, Goffle Brook splits into western and eastern branches at Maple Lake, a former manmade swimming hole that was drained in the late 1980s. Of the two branches, the eastern branch is less significant, extending a short distance through Wyckoff before ending just inside the southern limit of Waldwick. The western branch almost completely bisects the town of Wyckoff through the midsection, ending west of Russell Ave at Goffle Pond, the source of Goffle Brook.
Seven dams exist along Goffle Brook, although ten existed historically. In Hawthorne, a former dam at the southern end of Goffle Brook Park once held back Mill Pond. A dam just south of Goffle Hill Road now forms Arnold's Pond, often referred to as the Duck Pond. In Ridgewood, a dam just north of Rock Road forms Gypsy Pond, and a bigger dam just a little further upstream holds back Kings Pond. The current fourth and fifth dams exist just to the west of where Goffle Road crosses the brook in Midland Park. A dam that was destroyed during a storm lies just upstream from Sicomac Avenue bridge. This dam was held back the waters to form Morrow Pond which was a swimming hole in Midland Park. North of Canterbury Lane in Wyckoff a dam used to exist which held back Maple Lake, now a wetland in danger of development. [8] Two more dams create large lakes on the north and south sides Wyckoff Ave, again in Wyckoff.
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.
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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.
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The members of the New Jersey Legislature are chosen from 40 electoral districts. Each district elects one senator and two assemblymen.