The monitoring network within this area

Hydrionis holds 472 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
472
Values held
1897–2026
Record spans
Gauges within the Hiwassee huc8 subbasin
2 monitoring points, positioned as the publisher records them.
Gauges within the Hiwassee huc8 subbasinHIWASSEE RIVER ABOVE MURPHY, NC, VALLEY RIVER AT TOMOTLA, NCHIWASSEE RIVER ABOVE MURPHY, NCVALLEY RIVER AT TOMOTLA, NC

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 VALLEY RIVER AT TOMOTLA, NC
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1905–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at VALLEY RIVER AT TOMOTLA, NCLargest measured flow of each year at VALLEY RIVER AT TOMOTLA, NC: VALLEY RIVER AT TOMOTLA, NC in m³/s, from 1905 to 2025.Hurricane Katrina water and sanitation collapse0200400600m³/s19051928194219571973198720002014

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
PeriodVALLEY RIVER AT TOMOTLA, NC (m³/s)
190597.1
190675.3
190864.8
1909110
1914113
1915103
1917215
1918115
1920183
1922205
192457.5
192660.0
1928143
1929103
193153.8
1932103
1934147
193582.1
1936229
1937100
193891.7
193994.3
194040.8
194125.9
194268.0
1944110
194581.3
1946158
1947174
194889.2
1950155
1951196
1953108
1954183
1955109
1956106
1957236
195886.9
195985.5
1961122
1963193
1964165
1965155
1966189
196771.9
1969161
1971105
1972105
1973111
1975184
1976125
1977174
197874.5
1979217
1980248
198157.5
1982174
1984151
198584.4
198645.3
198781.6
198887.8
1989104
1990269
199177.6
1992142
1994337
1995343
1996168
1997177
199888.9
1999101
200068.0
200161.2
200289.8
2003170
200469.7
200660.0
200743.0
200849.0
2009147
201168.0
201253.2
2013200
2014120
2015212
201751.3
2018115
2019129
2020215
2021123
2022191
202393.7
2024108
2025106

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 held19052025
Completeness78.5% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 23 separate periods inside 1905–2025 hold no value. The longest runs from 1910 to 1913 — 4 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1905 and is not continuous from it: 121 years separate the first value from the last, and 79% 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 VALLEY RIVER AT TOMOTLA, NC, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1905–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above VALLEY RIVER AT TOMOTLA, NC, as a depthWater leaving the catchment above VALLEY RIVER AT TOMOTLA, NC, as a depth: VALLEY RIVER AT TOMOTLA, NC in mm, from 1905 to 2025.Hurricane Katrina water and sanitation collapse2505007501,0001,250mm19051927194219571972198720022017

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 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
PeriodVALLEY RIVER AT TOMOTLA, NC (mm)
1905899
19061,335
1907985
1908810
19091,102
1915680
1916811
1919743
19201,253
1921933
19221,189
1923978
1924732
1925506
1926757
1927901
19281,090
19291,329
1930591
1931528
19321,147
1933738
1934616
1935621
1936977
1937729
1938870
1939703
1940475
1941396
1942825
1943791
1944802
1945704
1946841
1947695
1948831
19491,133
1950982
1951773
1952700
1953668
1954682
1955669
1956783
19571,090
1958744
1959741
1960670
1961981
1962970
1963891
19641,085
1965795
1966802
19671,029
1968683
1969703
1970562
1971935
19721,084
19731,009
19741,119
19751,004
1976933
1977904
1978656
19791,194
1980943
1981515
19821,045
1983765
1984857
1985532
1986498
1987621
1988413
19891,325
19901,121
19911,001
1992949
1993732
19941,278
1995917
19961,104
1997988
1998817
1999742
2000508
2001554
2002881
20031,072
2004828
2005746
2006550
2007371
2008502
20091,081
2010733
2011730
2012644
20131,276
2014694
2015942
2016535
2017575
20181,033
20191,240
20201,309
20211,054
2022969
2023898
2024690
2025795

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 held19052025
Completeness94.2% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 2 separate periods inside 1905–2025 hold no value. The longest runs from 1910 to 1914 — 5 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1905 and is not continuous from it: 121 years separate the first value from the last, and 94% of the years between them are held. The span is not the record.
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 Hiwassee and what each holds
GaugeMeasuresValuesRecord
VALLEY RIVER AT TOMOTLA, NCburned area within 50 km, catchment area, annual maximum river flow, mean river flow2661905–2026
HIWASSEE RIVER ABOVE MURPHY, NCburned area within 50 km, catchment area, annual maximum river flow, mean river flow2061897–2026

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 — 06020002. 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
VALLEY RIVER AT TOMOTLA, NCStated 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
HIWASSEE RIVER ABOVE MURPHY, NCStated 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 spanned130yes, 20 or more
Values held472no
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), Hiwassee gauge records, accessed 2026-09-02, hydrionis.com/waters/united-states-hiwassee/

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 Hiwassee 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 confidence2025-04-07

Source: USGSNational Water Information System, USGS site 03550000, 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.