The monitoring network within this area

Hydrionis holds 2,785 values from 9 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.

9
Gauges
2,785
Values held
1897–2026
Record spans
Gauges within the Middle Delaware-Musconetcong huc8 subbasin
9 monitoring points, positioned as the publisher records them.
Gauges within the Middle Delaware-Musconetcong huc8 subbasinPaulins Kill at Blairstown NJ, Pequest River at Pequest NJ, Beaver Brook near Belvidere NJ, Delaware River at Belvidere NJ, Musconetcong River at outlet of Lake Hopatcong NJ, Musconetcong River near Hackettstown NJ, Musconetcong River near Bloomsbury NJ, Delaware River at Trenton NJ, Assunpink Creek at Trenton NJPaulins Kill at Blairstown NJPequest River at Pequest NJBeaver Brook near Belvidere NJDelaware River at Belvidere NJMusconetcong River at outlet of Lake Hopatcong NJMusconetcong River near Hackettstown NJMusconetcong River near Bloomsbury NJDelaware River at Trenton NJAssunpink Creek at Trenton 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 Delaware River at Trenton NJ
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1897–2023.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at Delaware River at Trenton NJLargest measured flow of each year at Delaware River at Trenton NJ: Delaware River at Trenton NJ in m³/s, from 1897 to 2023.Hurricane Katrina water and sanitation collapse02,5005,0007,50010km³/s18971914193119471964197919942011

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
PeriodDelaware River at Trenton NJ (m³/s)
18972,061
18991,960
19002,945
19012,197
19026,060
19033,794
19052,506
19063,171
19070
19090
19100
19110
19120
19134,531
19144,049
19152,407
19162,656
19172,566
19191,960
19203,426
19213,058
19232,118
19243,738
19254,361
19261,362
19273,285
19292,401
19301,342
19311,506
19321,872
19334,163
19342,265
19353,653
19366,428
19372,101
19383,540
19404,304
19411,608
19424,559
19433,370
19452,328
19462,330
19472,789
19483,568
19493,936
19502,260
19513,766
19522,701
19531,311
19559,316
19572,195
19592,401
19603,511
19612,735
19621,900
19632,472
19642,291
19651,379
1966937
19671,345
19681,934
19692,353
19702,832
19711,880
19722,917
19733,823
19752,679
19763,200
19773,313
19782,534
19793,313
19802,945
19812,263
19821,555
19833,908
19844,304
19852,469
19863,964
19872,568
19881,150
19892,359
19901,838
19921,325
19933,087
19942,141
19951,396
19965,069
19981,968
19993,171
20001,767
20021,229
20032,353
20045,692
20056,853
20066,711
20073,285
20083,058
20102,149
20115,522
20121,744
20142,271
20151,175
20161,985
20171,940
20181,775
20191,875
20202,146
20214,389
20223,313
20231,974

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 held1897–2023
Completeness86.6% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 17 separate periods inside 1897–2023 hold no value. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1897 and is not continuous from it: 127 years separate the first value from the last, and 87% 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 Delaware River at Trenton 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. 1913–2024.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above Delaware River at Trenton NJ, as a depthWater leaving the catchment above Delaware River at Trenton NJ, as a depth: Delaware River at Trenton NJ in mm, from 1913 to 2024.Hurricane Katrina water and sanitation collapse2505007501,0001,250mm19131927194119551969198319972011

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
PeriodDelaware River at Trenton NJ (mm)
1913621
1914497
1915587
1916612
1917558
1918518
1919615
1920722
1921523
1922501
1923477
1924573
1925532
1926556
1927822
1928722
1929593
1930387
1931406
1932555
1933668
1934592
1935606
1936681
1937683
1938747
1939525
1940671
1941379
1942716
1943645
1944427
1945874
1946549
1947737
1948636
1949551
1950674
1951771
1952894
1953661
1954469
1955694
1956622
1957441
1958649
1959518
1960632
1961530
1962441
1963361
1964394
1965253
1966336
1967534
1968518
1969502
1970568
1971620
1972863
1973844
1974691
1975806
1976654
1977724
1978646
1979801
1980412
1981404
1982515
1983746
1984695
1985447
1986636
1987589
1988448
1989588
1990694
1991436
1992478
1993662
1994691
1995460
1996985
1997474
1998626
1999465
2000611
2001412
2002502
20031,040
2004808
2005779
2006865
2007659
2008784
2009673
2010654
20111,217
2012508
2013527
2014570
2015454
2016397
2017524
20181,032
2019785
2020614
2021760
2022605
2023701
2024691

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 held1913–2024
Completeness100.0% of the periods in that span are held.
ContinuityContinuous: every year from 1913 to 2024 is held.
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 Middle Delaware-Musconetcong and what each holds
GaugeMeasuresValuesRecord
Musconetcong River near Bloomsbury NJburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3571903–2026
Delaware River at Trenton NJcatchment area, annual maximum river flow, mean river flow, mean river flow, water year3521897–2026
Pequest River at Pequest NJburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3491921–2026
Paulins Kill at Blairstown NJburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3441921–2026
Delaware River at Belvidere NJburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3441903–2026
Assunpink Creek at Trenton NJcatchment area, annual maximum river flow, mean river flow, mean river flow, water year3071923–2026
Musconetcong River at outlet of Lake Hopatcong NJburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2631928–2026
Beaver Brook near Belvidere NJburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2541922–2026
Musconetcong River near Hackettstown NJburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2151921–2026

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 — 02040105. 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
Musconetcong River near Bloomsbury 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
Delaware River at Trenton 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
Pequest River at Pequest 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
Paulins Kill at Blairstown 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
Delaware River at Belvidere 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
Assunpink Creek at Trenton 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
Musconetcong River at outlet of Lake Hopatcong 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
Beaver Brook near Belvidere 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
Musconetcong River near Hackettstown 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 spanned130yes, 20 or more
Values held2,785yes, 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), Middle Delaware-Musconetcong gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-middle-delaware-musconetcong/

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 Middle Delaware-Musconetcong 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 confidence2025-05-14

Source: USGS — National Water Information System, USGS site 01457000, 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.