The monitoring network within this area

Hydrionis holds 1,082 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
1,082
Values held
1907–2026
Record spans
Gauges within the Tygart Valley huc8 subbasin
3 monitoring points, positioned as the publisher records them.
Gauges within the Tygart Valley huc8 subbasinTYGART VALLEY RIVER NEAR DAILEY, WV, TYGART VALLEY RIVER AT BELINGTON, WV, BUCKHANNON RIVER AT HALL, WVTYGART VALLEY RIVER NEAR DAILEY, WVTYGART VALLEY RIVER AT BELINGTON, WVBUCKHANNON RIVER AT HALL, WV

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 TYGART VALLEY RIVER AT BELINGTON, WV
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1908–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at TYGART VALLEY RIVER AT BELINGTON, WVLargest measured flow of each year at TYGART VALLEY RIVER AT BELINGTON, WV: TYGART VALLEY RIVER AT BELINGTON, WV in m³/s, from 1908 to 2025.Hurricane Katrina water and sanitation collapse02505007501,000m³/s19081924193919541968198519992016

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
PeriodTYGART VALLEY RIVER AT BELINGTON, WV (m³/s)
1908271
1909153
1910303
1911337
1912521
1913237
1915249
1916303
1917379
1918484
1920379
1921303
1923253
1924382
1925198
1926235
1927253
1928292
1929328
1931174
1932479
1933253
1934303
1935280
1936379
1937283
1939365
1940229
1941153
1942255
1943183
1944309
1946163
1947294
1948374
1950303
1951274
1952256
1953146
1954168
1956320
1957357
1958234
1959242
1960300
1961181
1962272
1963396
1964294
1965214
1966289
1967487
1968286
1969180
1970337
1972447
1974323
1975211
1976230
1978391
1979273
1981274
1982399
1983248
1984309
1985230
1987194
1988181
1989311
1990348
1991221
1992320
1993260
1994566
1995219
1996600
1997357
1998331
1999251
2000428
2001210
2002368
2003365
2004416
2005202
2007374
2009260
2010267
2011279
2013317
2015428
2016239
2017198
2018416
2019225
2021286
2022309
2023161
2024391
2025385

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 held1908–2025
Completeness84.7% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 18 separate periods inside 1908–2025 hold no value. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1908 and is not continuous from it: 118 years separate the first value from the last, and 85% 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 TYGART VALLEY RIVER AT BELINGTON, WV, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1908–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above TYGART VALLEY RIVER AT BELINGTON, WV, as a depthWater leaving the catchment above TYGART VALLEY RIVER AT BELINGTON, WV, as a depth: TYGART VALLEY RIVER AT BELINGTON, WV in mm, from 1908 to 2025.Hurricane Katrina water and sanitation collapse5001,0001,500mm19081923193819531968198319982013

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
PeriodTYGART VALLEY RIVER AT BELINGTON, WV (mm)
1908737
1909542
1910615
1911847
1912702
1913832
1914610
1915553
1916658
1917628
1918781
1919602
1920656
1921609
1922595
1923681
1924814
1925603
1926832
1927940
1928753
1929749
1930264
1931552
1932680
1933794
1934479
1935882
1936733
1937789
1938571
1939612
1940611
1941390
1942725
1943579
1944715
1945712
1946483
1947463
1948855
1949674
1950876
1951692
1952499
1953513
1954659
1955491
1956879
1957588
1958742
1959541
1960571
1961815
1962664
1963601
1964576
1965502
1966547
1967826
1968560
1969553
1970658
1971712
19721,220
1973717
1974797
1975705
1976608
1977578
1978758
1979923
1980757
1981744
1982775
1983667
1984859
1985800
1986768
1987539
1988495
1989972
1990773
1991607
1992618
1993628
1994898
1995535
19961,300
1997550
1998734
1999501
2000568
2001509
2002743
20031,022
2004832
2005654
2006581
2007716
2008724
2009662
2010532
2011922
2012606
2013779
2014569
2015740
2016658
20181,196
2019641
2020802
2021464
2022733
2023620
2024604
2025626

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 held1908–2025
Completeness99.2% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • One period inside 1908–2025 holds no value: 2017. It is drawn as a break in the line and is never interpolated across.
ContinuityThe record begins in 1908 and is not continuous from it: 118 years separate the first value from the last, and 99% 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 Tygart Valley and what each holds
GaugeMeasuresValuesRecord
TYGART VALLEY RIVER AT BELINGTON, WVburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3881907–2026
BUCKHANNON RIVER AT HALL, WVburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3661908–2026
TYGART VALLEY RIVER NEAR DAILEY, WVburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3281915–2026

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 — 05020001. 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
TYGART VALLEY RIVER AT BELINGTON, WVStated 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
BUCKHANNON RIVER AT HALL, WVStated 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
TYGART VALLEY RIVER NEAR DAILEY, WVStated 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 record3yes, 3 or more
Years spanned120yes, 20 or more
Values held1,082yes, 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), Tygart Valley gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-tygart-valley/

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 Tygart Valley 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 confidence2025-02-01

Source: USGS — National Water Information System, USGS site 03051000, 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.