The monitoring network within this area

Hydrionis holds 313 values from 2 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.

2
Gauges
313
Values held
1909–2026
Record spans
Gauges within the Lackawaxen huc8 subbasin
2 monitoring points, positioned as the publisher records them.
Gauges within the Lackawaxen huc8 subbasinLackawaxen River at Hawley, PA, WALLENPAUPACK CREEK AT WILSONVILLE PALackawaxen River at Hawley, PAWALLENPAUPACK CREEK AT WILSONVILLE PA

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 Lackawaxen River at Hawley, PA
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1909–2023.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at Lackawaxen River at Hawley, PALargest measured flow of each year at Lackawaxen River at Hawley, PA: Lackawaxen River at Hawley, PA in m³/s, from 1909 to 2023.Hurricane Katrina water and sanitation collapse05001,0001,500m³/s19091939195219651977198820022013

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 recordA 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 collapseFlood2005-08-292005-09-30Documented record
Compiled record

Not shown on this chart

  • The 1976 droughtThis 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 droughtThis event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • Yorkshire droughtThis 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 PauloThis 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 ZeroThis event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • European droughtThis 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
PeriodLackawaxen River at Hawley, PA (m³/s)
1909198
1910129
191199.7
1912129
1913231
1914357
1915126
1916208
191799.7
1938271
1939190
1940408
1941168
19421,416
1943278
1945190
1946292
1947433
1948223
1950236
1952614
1954199
19551,470
1957221
1959230
1960241
1961215
1962140
1963210
1964260
196571.9
196683.8
1967113
1968136
1969155
1970192
1971143
1972269
1973464
1975283
1977219
1978172
1979177
1981131
1982204
1983237
1984382
1985292
1986357
1987212
1988110
1989235
1990176
1992113
1993229
1994181
1996360
1998142
1999110
2000149
2002156
2003215
2004501
2005555
2006793
2007189
2008249
2010127
2011306
2012242
2013237
2014149
2015116
2016151
2017177
2018146
2019211
2020159
2021490
2023210

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 held19092023
Completeness69.6% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 16 separate periods inside 1909–2023 hold no value. The longest runs from 1918 to 1937 — 20 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1909 and is not continuous from it: 115 years separate the first value from the last, and 70% of the years between them are held. The span is not the record.
Last read from the publisher2026-08-31
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 WALLENPAUPACK CREEK AT WILSONVILLE PA, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1926–2004.
Water leaving the catchment above WALLENPAUPACK CREEK AT WILSONVILLE PA, as a depthWater leaving the catchment above WALLENPAUPACK CREEK AT WILSONVILLE PA, as a depth: WALLENPAUPACK CREEK AT WILSONVILLE PA in mm, from 1926 to 2004.02505007501,000mm19261936194619561966197619861996WALLENPAUPACK CREEK AT WILSONVILLE PA 1926: 314 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1927: 761 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1928: 779 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1929: 428 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1930: 443 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1931: 287 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1932: 395 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1933: 616 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1934: 423 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1935: 531 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1936: 607 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1937: 436 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1938: 595 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1939: 513 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1940: 480 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1941: 421 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1942: 454 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1943: 604 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1944: 283 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1945: 676 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1946: 601 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1947: 646 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1948: 515 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1949: 392 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1950: 518 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1951: 716 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1952: 820 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1953: 619 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1954: 386 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1955: 825 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1956: 517 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1957: 466 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1958: 683 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1959: 421 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1960: 799 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1961: 428 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1962: 366 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1963: 357 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1964: 371 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1965: 185 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1966: 389 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1967: 565 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1968: 459 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1969: 416 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1970: 568 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1971: 572 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1972: 881 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1973: 729 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1974: 647 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1975: 720 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1976: 571 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1977: 698 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1978: 627 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1979: 711 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1980: 439 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1981: 371 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1982: 365 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1983: 738 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1984: 741 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1985: 449 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1986: 785 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1987: 703 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1988: 364 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1989: 603 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1990: 571 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1991: 392 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1992: 429 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1993: 625 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1994: 764 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1995: 437 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1996: 1,072 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1997: 380 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1998: 650 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 1999: 415 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 2000: 582 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 2001: 308 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 2002: 475 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 2003: 984 mmWALLENPAUPACK CREEK AT WILSONVILLE PA 2004: 774 mm

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 (0 events)

Not shown on this chart

  • The 1976 droughtThis 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 droughtThis event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • Yorkshire droughtThis 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 PauloThis 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 ZeroThis event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • European droughtThis 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
PeriodWALLENPAUPACK CREEK AT WILSONVILLE PA (mm)
1926314
1927761
1928779
1929428
1930443
1931287
1932395
1933616
1934423
1935531
1936607
1937436
1938595
1939513
1940480
1941421
1942454
1943604
1944283
1945676
1946601
1947646
1948515
1949392
1950518
1951716
1952820
1953619
1954386
1955825
1956517
1957466
1958683
1959421
1960799
1961428
1962366
1963357
1964371
1965185
1966389
1967565
1968459
1969416
1970568
1971572
1972881
1973729
1974647
1975720
1976571
1977698
1978627
1979711
1980439
1981371
1982365
1983738
1984741
1985449
1986785
1987703
1988364
1989603
1990571
1991392
1992429
1993625
1994764
1995437
19961,072
1997380
1998650
1999415
2000582
2001308
2002475
2003984
2004774

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 held19262004
Completeness100.0% of the periods in that span are held.
ContinuityContinuous: every year from 1926 to 2004 is held.
Last read from the publisher2026-08-24
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 Lackawaxen and what each holds
GaugeMeasuresValuesRecord
Lackawaxen River at Hawley, PAburned area within 50 km, catchment area, annual maximum river flow, mean river flow1971909–2026
WALLENPAUPACK CREEK AT WILSONVILLE PAburned area within 50 km, catchment area, mean river flow1161926–2026

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 — 02040103. 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
Lackawaxen River at Hawley, PAStated 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/42026-08-26
WALLENPAUPACK CREEK AT WILSONVILLE PAStated 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/42026-08-26

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 3 of them, which makes it a full profile.

Information-gain signals held for this water body
SignalHeldCounts
Gauges holding a real record2no
Years spanned118yes, 20 or more
Values held313no
Distinct measurements4yes, 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), Lackawaxen gauge records, accessed 2026-09-02, hydrionis.com/waters/united-states-lackawaxen/

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 Lackawaxen 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 confidence2023-12-18

Source: USGSNational Water Information System, USGS site 01431500, 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 31 August 2026.