HydrionisGlobal Water Intelligence
HUC8 subbasin

Hoh-Quillayute

3 monitoring stations within this area in United States, holding 106 values between 1897 and 2026. A United States federal hydrologic unit at the eight-digit subbasin level — a drainage area, not a river. Many subbasins take the name of the largest river within them, and the gauges below are anywhere inside the area, including on tributaries.

United StatesHUC8 subbasin

The monitoring network within this area

Hydrionis holds 106 values from 3 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.

3
Gauges
106
Values held
1897–2026
Record spans
Gauges within the Hoh-Quillayute huc8 subbasin
3 monitoring points, positioned as the publisher records them.
Gauges within the Hoh-Quillayute huc8 subbasinSOLEDUCK RIVER NEAR FAIRHOLM, WA, SOLEDUCK RIVER NEAR QUILLAYUTE, WA, CALAWAH RIVER NEAR FORKS, WASOLEDUCK RIVER NEAR FAIRHOLM, WASOLEDUCK RIVER NEAR QUILLAYUTE, WACALAWAH RIVER NEAR FORKS, WA

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 SOLEDUCK RIVER NEAR FAIRHOLM, WA
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1917–1979.
Largest measured flow of each year at SOLEDUCK RIVER NEAR FAIRHOLM, WALargest measured flow of each year at SOLEDUCK RIVER NEAR FAIRHOLM, WA: SOLEDUCK RIVER NEAR FAIRHOLM, WA in m³/s, from 1917 to 1979.0200400600800m³/s19171934194219491955196119681975SOLEDUCK RIVER NEAR FAIRHOLM, WA 1917: 447 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1918: 374 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1919: 283 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1921: 323 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1933: 561 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1934: 532 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1936: 112 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1936: 246 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1937: 345 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1939: 267 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1939: 267 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1941: 229 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1941: 256 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1942: 133 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1943: 189 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1945: 413 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1945: 179 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1947: 209 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1947: 224 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1948: 136 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1949: 665 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1951: 306 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1952: 134 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1953: 245 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1954: 229 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1954: 306 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1955: 510 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1956: 462 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1957: 201 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1959: 262 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1960: 255 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1961: 433 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1962: 163 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1962: 394 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1963: 236 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1964: 227 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1966: 169 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1966: 294 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1968: 274 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1968: 217 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1970: 210 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1971: 193 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1972: 276 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1972: 337 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1974: 351 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1974: 300 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1975: 425 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1976: 118 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1977: 408 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1979: 135 m³/sSOLEDUCK RIVER NEAR FAIRHOLM, WA 1979: 416 m³/s

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 (0 events)

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
PeriodSOLEDUCK RIVER NEAR FAIRHOLM, WA (m³/s)
1917447
1918374
1919283
1921323
1933561
1934532
1936112
1937345
1939267
1941229
1942133
1943189
1945413
1947209
1948136
1949665
1951306
1952134
1953245
1954229
1955510
1956462
1957201
1959262
1960255
1961433
1962163
1963236
1964227
1966169
1968274
1970210
1971193
1972276
1974351
1975425
1976118
1977408
1979135

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 held1917–1979
Completeness61.9% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 14 separate periods inside 1917–1979 hold no value. The longest runs from 1922 to 1932 — 11 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1917 and is not continuous from it: 63 years separate the first value from the last, and 62% 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

Every gauge Hydrionis holds within this area

GaugeMeasuresValuesRecord
SOLEDUCK RIVER NEAR FAIRHOLM, WAcatchment area, annual maximum river flow521917–2026
CALAWAH RIVER NEAR FORKS, WAcatchment area, annual maximum river flow501897–2026
SOLEDUCK RIVER NEAR QUILLAYUTE, WAcatchment area, annual maximum river flow41977–2026

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 — 17100101. 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.

GaugeEvidenceEstablished
SOLEDUCK RIVER NEAR FAIRHOLM, WAStated 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
CALAWAH RIVER NEAR FORKS, WAStated 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
SOLEDUCK RIVER NEAR QUILLAYUTE, WAStated 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 2 of them, which makes it a profile, not indexed.

SignalHeldCounts
Gauges holding a real record2no
Years spanned130yes, 20 or more
Values held106no
Distinct measurements2yes, 2 or more
Publishers measuring it1no
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), Hoh-Quillayute gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-hoh-quillayute/

Cite Hydrionis where you rely on the compilation, the normalisation, the eligibility judgements or a chart. Where you use an unmodified published value, the publisher’s attribution is the one that is required; crediting Hydrionis as well is welcome and is not something Hydrionis can require of you.

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 Hoh-Quillayute 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 confidence1979-12-17

Source: USGS — National Water Information System, USGS site 12041500, 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.

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