The monitoring network within this area

Hydrionis holds 547 values from 5 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.

5
Gauges
547
Values held
1912–2026
Record spans
Gauges within the Little Kanawha huc8 subbasin
5 monitoring points, positioned as the publisher records them.
Gauges within the Little Kanawha huc8 subbasinHUGHES RIVER AT CISCO, WV, LITTLE KANAWHA RIVER AT GLENVILLE, WV, LITTLE KANAWHA RIVER AT GRANTSVILLE, WV, WEST FORK LITTLE KANAWHA RIVER AT ROCKSDALE, WV, SOUTH FORK HUGHES RIVER BELOW MACFARLAN, WVHUGHES RIVER AT CISCO, WVLITTLE KANAWHA RIVER AT GLENVILLE, WVLITTLE KANAWHA RIVER AT GRANTSVILLE, WVWEST FORK LITTLE KANAWHA RIVER AT ROCKSDALE, WVSOUTH FORK HUGHES RIVER BELOW MACFARLAN, 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 LITTLE KANAWHA RIVER AT GLENVILLE, WV
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1912–2024.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at LITTLE KANAWHA RIVER AT GLENVILLE, WVLargest measured flow of each year at LITTLE KANAWHA RIVER AT GLENVILLE, WV: LITTLE KANAWHA RIVER AT GLENVILLE, WV in m³/s, from 1912 to 2024.Hurricane Katrina water and sanitation collapse0200400600800m³/s19121929194319581970198820012016

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
PeriodLITTLE KANAWHA RIVER AT GLENVILLE, WV (m³/s)
19120
19130
19150
19160
19170
19190
19210
19230
19240
19250
19260
19280
1929250
1931175
1932300
1933222
1934249
1935365
1936300
1937357
1939578
1940303
1941173
1942219
1943490
1944303
1946246
1947153
1948320
1950354
1951515
1952294
1953124
1954300
1956251
1957362
1958337
1959161
1960184
1961200
1962211
1963309
1964185
1965240
1966340
1967609
1968232
1969144
1970286
1972216
1974362
1975188
1976188
1978323
1979217
1981280
1982187
1984187
1985185
1986219
1988166
1989413
1990239
1992221
1993231
1994450
1995203
1996345
1997428
1998214
1999226
2000493
2001169
20020
20030
20050
20060
20070
20080
20090
20110
20130
20140
20150
20160
20170
2018204
2020238
2021247
2022326
2023187
2024257

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 held1912–2024
Completeness81.4% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 21 separate periods inside 1912–2024 hold no value. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1912 and is not continuous from it: 113 years separate the first value from the last, and 81% 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 HUGHES RIVER AT CISCO, 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. 1929–1993.
Water leaving the catchment above HUGHES RIVER AT CISCO, WV, as a depthWater leaving the catchment above HUGHES RIVER AT CISCO, WV, as a depth: HUGHES RIVER AT CISCO, WV in mm, from 1929 to 1993.200400600800mm19291945195319611969197719851993HUGHES RIVER AT CISCO, WV 1929: 455 mmHUGHES RIVER AT CISCO, WV 1930: 200 mmHUGHES RIVER AT CISCO, WV 1939: 431 mmHUGHES RIVER AT CISCO, WV 1940: 446 mmHUGHES RIVER AT CISCO, WV 1941: 252 mmHUGHES RIVER AT CISCO, WV 1942: 477 mmHUGHES RIVER AT CISCO, WV 1943: 444 mmHUGHES RIVER AT CISCO, WV 1944: 510 mmHUGHES RIVER AT CISCO, WV 1945: 656 mmHUGHES RIVER AT CISCO, WV 1946: 443 mmHUGHES RIVER AT CISCO, WV 1947: 323 mmHUGHES RIVER AT CISCO, WV 1948: 689 mmHUGHES RIVER AT CISCO, WV 1949: 452 mmHUGHES RIVER AT CISCO, WV 1950: 737 mmHUGHES RIVER AT CISCO, WV 1951: 629 mmHUGHES RIVER AT CISCO, WV 1952: 383 mmHUGHES RIVER AT CISCO, WV 1953: 323 mmHUGHES RIVER AT CISCO, WV 1954: 334 mmHUGHES RIVER AT CISCO, WV 1955: 374 mmHUGHES RIVER AT CISCO, WV 1956: 567 mmHUGHES RIVER AT CISCO, WV 1957: 424 mmHUGHES RIVER AT CISCO, WV 1958: 572 mmHUGHES RIVER AT CISCO, WV 1959: 325 mmHUGHES RIVER AT CISCO, WV 1960: 364 mmHUGHES RIVER AT CISCO, WV 1961: 542 mmHUGHES RIVER AT CISCO, WV 1962: 479 mmHUGHES RIVER AT CISCO, WV 1963: 405 mmHUGHES RIVER AT CISCO, WV 1964: 363 mmHUGHES RIVER AT CISCO, WV 1965: 345 mmHUGHES RIVER AT CISCO, WV 1966: 278 mmHUGHES RIVER AT CISCO, WV 1967: 464 mmHUGHES RIVER AT CISCO, WV 1968: 425 mmHUGHES RIVER AT CISCO, WV 1969: 267 mmHUGHES RIVER AT CISCO, WV 1970: 445 mmHUGHES RIVER AT CISCO, WV 1971: 406 mmHUGHES RIVER AT CISCO, WV 1972: 612 mmHUGHES RIVER AT CISCO, WV 1973: 390 mmHUGHES RIVER AT CISCO, WV 1974: 565 mmHUGHES RIVER AT CISCO, WV 1975: 617 mmHUGHES RIVER AT CISCO, WV 1976: 434 mmHUGHES RIVER AT CISCO, WV 1977: 293 mmHUGHES RIVER AT CISCO, WV 1978: 608 mmHUGHES RIVER AT CISCO, WV 1979: 661 mmHUGHES RIVER AT CISCO, WV 1980: 438 mmHUGHES RIVER AT CISCO, WV 1981: 369 mmHUGHES RIVER AT CISCO, WV 1982: 328 mmHUGHES RIVER AT CISCO, WV 1983: 467 mmHUGHES RIVER AT CISCO, WV 1984: 373 mmHUGHES RIVER AT CISCO, WV 1985: 451 mmHUGHES RIVER AT CISCO, WV 1986: 385 mmHUGHES RIVER AT CISCO, WV 1987: 225 mmHUGHES RIVER AT CISCO, WV 1988: 229 mmHUGHES RIVER AT CISCO, WV 1989: 708 mmHUGHES RIVER AT CISCO, WV 1990: 627 mmHUGHES RIVER AT CISCO, WV 1991: 458 mmHUGHES RIVER AT CISCO, WV 1992: 314 mmHUGHES RIVER AT CISCO, WV 1993: 378 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 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
PeriodHUGHES RIVER AT CISCO, WV (mm)
1929455
1930200
1939431
1940446
1941252
1942477
1943444
1944510
1945656
1946443
1947323
1948689
1949452
1950737
1951629
1952383
1953323
1954334
1955374
1956567
1957424
1958572
1959325
1960364
1961542
1962479
1963405
1964363
1965345
1966278
1967464
1968425
1969267
1970445
1971406
1972612
1973390
1974565
1975617
1976434
1977293
1978608
1979661
1980438
1981369
1982328
1983467
1984373
1985451
1986385
1987225
1988229
1989708
1990627
1991458
1992314
1993378

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 held1929–1993
Completeness87.7% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • One period inside 1929–1993 holds no value: 1931 to 1938, 8 years with no reading. It is drawn as a break in the line and is never interpolated across.
ContinuityThe record begins in 1929 and is not continuous from it: 65 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 Little Kanawha and what each holds
GaugeMeasuresValuesRecord
HUGHES RIVER AT CISCO, WVburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2171915–2026
LITTLE KANAWHA RIVER AT GLENVILLE, WVcatchment area, annual maximum river flow1111912–2026
LITTLE KANAWHA RIVER AT GRANTSVILLE, WVcatchment area, annual maximum river flow941929–2026
WEST FORK LITTLE KANAWHA RIVER AT ROCKSDALE, WVcatchment area, annual maximum river flow921929–2026
SOUTH FORK HUGHES RIVER BELOW MACFARLAN, WVcatchment area, annual maximum river flow331915–2026

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 — 05030203. 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
HUGHES RIVER AT CISCO, 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
LITTLE KANAWHA RIVER AT GLENVILLE, 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
LITTLE KANAWHA RIVER AT GRANTSVILLE, 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
WEST FORK LITTLE KANAWHA RIVER AT ROCKSDALE, 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
SOUTH FORK HUGHES RIVER BELOW MACFARLAN, 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 4 of them, which makes it a full profile.

Information-gain signals held for this water body
SignalHeldCounts
Gauges holding a real record4yes, 3 or more
Years spanned115yes, 20 or more
Values held547no
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), Little Kanawha gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-little-kanawha/

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 Little Kanawha 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 confidence1994-01-29

Source: USGS — National Water Information System, USGS site 03155500, 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.