The monitoring network within this area

Hydrionis holds 3,030 values from 10 gauges within it. Discharge is a property of a gauge and its reach, not of this drainage area, so this page reports the network and its records rather than a single figure.

10
Gauges
3,030
Values held
1882–2026
Record spans
Gauges within the Raritan huc8 subbasin
10 monitoring points, positioned as the publisher records them.
Gauges within the Raritan huc8 subbasinSouth Branch Raritan River near High Bridge NJ, South Branch Raritan River at Stanton NJ, North Branch Raritan River near Far Hills NJ, Lamington (Black) River near Pottersville NJ, North Branch Raritan River near Raritan NJ, Raritan River at Manville NJ, Millstone River at Blackwells Mills NJ, Raritan River below Calco Dam at Bound Brook NJ, Lawrence Brook at Farrington Dam NJ, Raritan River at Bound Brook NJSouth Branch Raritan River near High Bridge NJSouth Branch Raritan River at Stanton NJNorth Branch Raritan River near Far Hills NJLamington (Black) River near Pottersville NJNorth Branch Raritan River near Raritan NJRaritan River at Manville NJMillstone River at Blackwells Mills NJRaritan River below Calco Dam at Bound Brook NJLawrence Brook at Farrington Dam NJRaritan River at Bound Brook NJ

Flood peaks, as measured

This gauge's flood record, as measured. Unlike a daily mean it is the discharge at the moment the river was highest, which is the figure flood frequency analysis is built on.

Largest measured flow of each year at Raritan River at Manville NJ
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1903–2024.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at Raritan River at Manville NJLargest measured flow of each year at Raritan River at Manville NJ: Raritan River at Manville NJ in m³/s, from 1903 to 2024.Hurricane Katrina water and sanitation collapse01,0002,000m³/s19031925193919551969198219962013

Published by the gauge's own operator from its sub-daily record; Hydrionis stores the figure rather than recomputing it. A year the gauge did not cover produces no value rather than a low one, and the gaps are stated below the chart. A peak is a property of this gauge and its reach: a larger flood upstream or downstream of it is not in this series.

What the shaded periods are (1 event)

A shaded period marks when something was recorded, not what caused the shape of the line. Where the two coincide, they coincided.

Documented record — A documented event, compiled from cited sources after it happened. The dates are as good as the record, which for older events can mean the month rather than the day.

EventTypePeriodStandingAuthority
Hurricane Katrina water and sanitation collapseFlood2005-08-29 – 2005-09-30Documented record
Compiled record

Not shown on this chart

  • The 1976 drought — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • The 2022 drought — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • Yorkshire drought — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • Cantareira water crisis, São Paulo — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • Cape Town Day Zero — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • European drought — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
View the data behind this chart
Underlying data
PeriodRaritan River at Manville NJ (m³/s)
1903810
1905527
1906385
1909433
1910535
1911306
1912578
1914433
1915714
1922368
1923399
1924496
1925425
1926368
1927343
1929385
1930320
1931274
1932419
1933595
1934470
1935297
1936583
19381,022
1939496
1940776
1941496
1942940
1944510
1945391
1946564
1947212
1948626
1950245
1951578
1953436
1955980
1957306
1958467
1960416
1961326
1962425
1963331
1964385
1965360
1966374
1967470
1968481
1969371
1970671
19711,028
1972617
1973555
1975487
1976379
1977518
1978549
1979651
1980501
1981507
1982481
1983646
1984773
1985326
1986447
1987498
1988309
1989459
1990247
1992348
1994422
1995227
1996688
1998309
19992,197
2000189
2001340
2002300
2003311
2005547
2007861
2008558
2010818
20111,501
2013430
2014716
2015317
2016371
2017255
2018377
2020306
20211,668
2022530
2023374
2024886

About this series

Everything below is a property of the data rather than a rating of it. There is deliberately no single confidence score: how much a gap matters depends on what you are about to do with the series, and only you know that.

Source
United States Geological Survey — National Water Information System · US Government work — public domain
How the values came to existMeasured
Period held1903–2024
Completeness77.9% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 21 separate periods inside 1903–2024 hold no value. The longest runs from 1916 to 1921 — 6 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1903 and is not continuous from it: 122 years separate the first value from the last, and 78% of the years between them are held. The span is not the record.
Last read from the publisher2026-10-01
RedistributionPermitted by the upstream licences
Commercial reusePermitted by the upstream licences. No Hydrionis access tier can widen this.
MethodologyHow this was produced

How much of the rain came back out

A discharge in cubic metres per second cannot be compared with anything: the larger number may only mean the larger catchment. Divided by the area draining to the gauge it becomes a depth of water over that land, which answers a question a reader already has — of the rain that fell here, how much came back out as river?

Water leaving the catchment above South Branch Raritan River at Stanton NJ, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1904–2024.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above South Branch Raritan River at Stanton NJ, as a depthWater leaving the catchment above South Branch Raritan River at Stanton NJ, as a depth: South Branch Raritan River at Stanton NJ in mm, from 1904 to 2024.Hurricane Katrina water and sanitation collapse05001,000mm19041932194619601974198820022016

Computed by Hydrionis from the published annual mean flow and the catchment area the station's own publisher states. It is not a water balance: the difference between rainfall and runoff is not evaporation alone but also change in groundwater storage, water abstracted and taken elsewhere, and water imported by transfer schemes — which is why a catchment can yield more runoff than the rain that fell on it without anything being measured wrongly. A different area figure rescales every value here by the ratio between them.

What the shaded periods are (1 event)

A shaded period marks when something was recorded, not what caused the shape of the line. Where the two coincide, they coincided.

Documented record — A documented event, compiled from cited sources after it happened. The dates are as good as the record, which for older events can mean the month rather than the day.

EventTypePeriodStandingAuthority
Hurricane Katrina water and sanitation collapseFlood2005-08-29 – 2005-09-30Documented record
Compiled record

Not shown on this chart

  • The 1976 drought — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • The 2022 drought — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • Yorkshire drought — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • Cantareira water crisis, São Paulo — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • Cape Town Day Zero — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • European drought — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
View the data behind this chart
Underlying data
PeriodSouth Branch Raritan River at Stanton NJ (mm)
1904562
1905590
1920695
1921464
1922481
1923478
1924618
1925634
1926510
1927764
1928690
1929573
1930372
1931349
1932393
1933606
1934545
1935516
1936640
1937564
1938682
1939535
1940662
1941357
1942664
1943542
1944470
1945797
1946506
1947574
1948699
1949472
1950484
1951839
1952874
1953611
1954368
1955628
1956560
1957413
1958614
1959393
1960540
1961525
1962440
1963330
1964308
1965224
1966233
1967441
1968429
1969369
1970520
1971816
1972930
1973902
1974694
1975991
1976532
1977604
1978671
1979992
1980550
1981299
1982563
1983912
1984882
1985455
1986687
1987548
1988555
1989854
1990662
1991545
1992417
1993695
1994684
1995467
19961,037
1997562
1998575
1999430
2000448
2001522
2002327
2003941
2004653
2005722
2006684
2007692
2008694
2009582
2010728
20111,246
2012460
2013581
2014635
2015390
2016341
2017315
2018817
2019904
2020626
2021704
2022665
2023605
2024667

About this series

Everything below is a property of the data rather than a rating of it. There is deliberately no single confidence score: how much a gap matters depends on what you are about to do with the series, and only you know that.

Source
United States Geological Survey — National Water Information System · US Government work — public domain
How the values came to existDerived Computed by Hydrionis
Period held1904–2024
Completeness88.4% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • One period inside 1904–2024 holds no value: 1906 to 1919, 14 years with no reading. It is drawn as a break in the line and is never interpolated across.
ContinuityThe record begins in 1904 and is not continuous from it: 121 years separate the first value from the last, and 88% of the years between them are held. The span is not the record.
Inputs last read2026-10-01 · when the records this was computed from were last read from their publishers
Calculation date2026-08-24 · when the calculation method was last versioned, not a reading of any publisher
RedistributionPermitted by the upstream licences
Commercial reusePermitted by the upstream licences. No Hydrionis access tier can widen this.
MethodologyHow this was produced

Every gauge Hydrionis holds within this area

Gauges within the Raritan and what each holds
GaugeMeasuresValuesRecord
South Branch Raritan River at Stanton NJburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3631903–2026
Raritan River at Manville NJburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3621903–2026
South Branch Raritan River near High Bridge NJburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3571896–2026
Lamington (Black) River near Pottersville NJburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3491896–2026
Millstone River at Blackwells Mills NJburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3461921–2026
North Branch Raritan River near Far Hills NJburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3451919–2026
North Branch Raritan River near Raritan NJburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3401896–2026
Raritan River below Calco Dam at Bound Brook NJburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3021882–2026
Lawrence Brook at Farrington Dam NJburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2301927–2026
Raritan River at Bound Brook NJcatchment area, annual maximum river flow361882–2026

How these gauges were attached to this water

Assigned by the publisher to a numbered basin Every gauge here is assigned to this drainage area by its own publisher, which issues the area an official code — 02030105. A drainage area is not a river: it contains the tributaries as well as the main channel, and a gauge in it may be on any of them.

What each gauge’s link to this water rests on
GaugeEvidenceEstablished
South Branch Raritan River at Stanton NJStated by the publisher — USGS site service, huc_cd field — https://waterservices.usgs.gov/nwis/site/ ; named from the USGS Watershed Boundary Dataset 8-digit HU (Subbasin) layer — https://hydro.nationalmap.gov/arcgis/rest/services/wbd/MapServer/42026-10-02
Raritan River at Manville NJStated by the publisher — USGS site service, huc_cd field — https://waterservices.usgs.gov/nwis/site/ ; named from the USGS Watershed Boundary Dataset 8-digit HU (Subbasin) layer — https://hydro.nationalmap.gov/arcgis/rest/services/wbd/MapServer/42026-10-02
South Branch Raritan River near High Bridge NJStated by the publisher — USGS site service, huc_cd field — https://waterservices.usgs.gov/nwis/site/ ; named from the USGS Watershed Boundary Dataset 8-digit HU (Subbasin) layer — https://hydro.nationalmap.gov/arcgis/rest/services/wbd/MapServer/42026-10-02
Lamington (Black) River near Pottersville NJStated by the publisher — USGS site service, huc_cd field — https://waterservices.usgs.gov/nwis/site/ ; named from the USGS Watershed Boundary Dataset 8-digit HU (Subbasin) layer — https://hydro.nationalmap.gov/arcgis/rest/services/wbd/MapServer/42026-10-02
Millstone River at Blackwells Mills NJStated by the publisher — USGS site service, huc_cd field — https://waterservices.usgs.gov/nwis/site/ ; named from the USGS Watershed Boundary Dataset 8-digit HU (Subbasin) layer — https://hydro.nationalmap.gov/arcgis/rest/services/wbd/MapServer/42026-10-02
North Branch Raritan River near Far Hills NJStated by the publisher — USGS site service, huc_cd field — https://waterservices.usgs.gov/nwis/site/ ; named from the USGS Watershed Boundary Dataset 8-digit HU (Subbasin) layer — https://hydro.nationalmap.gov/arcgis/rest/services/wbd/MapServer/42026-10-02
North Branch Raritan River near Raritan NJStated by the publisher — USGS site service, huc_cd field — https://waterservices.usgs.gov/nwis/site/ ; named from the USGS Watershed Boundary Dataset 8-digit HU (Subbasin) layer — https://hydro.nationalmap.gov/arcgis/rest/services/wbd/MapServer/42026-10-02
Raritan River below Calco Dam at Bound Brook NJStated by the publisher — USGS site service, huc_cd field — https://waterservices.usgs.gov/nwis/site/ ; named from the USGS Watershed Boundary Dataset 8-digit HU (Subbasin) layer — https://hydro.nationalmap.gov/arcgis/rest/services/wbd/MapServer/42026-10-02
Lawrence Brook at Farrington Dam NJStated by the publisher — USGS site service, huc_cd field — https://waterservices.usgs.gov/nwis/site/ ; named from the USGS Watershed Boundary Dataset 8-digit HU (Subbasin) layer — https://hydro.nationalmap.gov/arcgis/rest/services/wbd/MapServer/42026-10-02
Raritan River at Bound Brook NJStated by the publisher — USGS site service, huc_cd field — https://waterservices.usgs.gov/nwis/site/ ; named from the USGS Watershed Boundary Dataset 8-digit HU (Subbasin) layer — https://hydro.nationalmap.gov/arcgis/rest/services/wbd/MapServer/42026-10-02

What this record holds

Hydrionis decides which waters get a page, and which of those are offered to search, from what is actually held rather than from how the page reads. Five signals are counted; this record has 5 of them, which makes it a full profile.

Information-gain signals held for this water body
SignalHeldCounts
Gauges holding a real record9yes, 3 or more
Years spanned145yes, 20 or more
Values held3,030yes, 1000 or more
Distinct measurements5yes, 2 or more
Publishers measuring it2yes, 2 or more
Official identifiers1recorded, not counted

Use this data

Use this data

No bulk download is offered here, which is a licence position rather than a product one: at least one contributing publisher does not permit redistribution. The values can be read on the page, cited, and pointed to at source.

Attribution and citation

Suggested citation for Hydrionis

Hydrionis (2026), Raritan gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-raritan/

Cite Hydrionis where you rely on values Hydrionis computed, on the method that produced them, or on the compilation itself. The underlying measurements remain the publishers’ and their attribution requirements apply to you directly.

Recommended, not required. Hydrionis does not claim rights over unmodified public data it relayed, and doing arithmetic on somebody else’s measurements does not make them Hydrionis’s. Cite the version and the access date: the Raritan gauge records changes as publishers release and as methods are revised, and a citation without both cannot be checked later. Full guidance is on cite and reuse.

None of the contributing licences requires attribution. Crediting the publishers is still good practice and they are listed above.

Where these figures come from

MeasuredHigh confidence2025-04-06

Source: USGS — National Water Information System, USGS site 01397000, annual peak streamflow. Licence: Open.

Method: The instantaneous maximum discharge of each water year as published by USGS, dated to the day it occurred. One value per October-to-September water year; where the publisher lists both a systematic and a historic peak for a year, the larger is the annual maximum. Values the publisher marks as maximum daily averages are not held here, because they are not instantaneous peaks. Values marked as bounded rather than measured are held as censored observations carrying the bound. Cubic feet per second are converted to cubic metres per second and the publisher unit is recorded alongside.

Rating curves are extrapolated at extreme discharges, so the largest values in a peak series carry the largest measurement uncertainty. Data from the U.S. Geological Survey National Water Information System, a work of the United States government and therefore in the public domain.

Retrieved 1 October 2026.