The monitoring network within this area

Hydrionis holds 3,550 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
3,550
Values held
1889–2026
Record spans
Gauges within the Gallatin huc8 subbasin
3 monitoring points, positioned as the publisher records them.
Gauges within the Gallatin huc8 subbasinGallatin River near Gallatin Gateway, MT, Hyalite C at Hyalite R S nr Bozeman MT, Gallatin River at Logan MTGallatin River near Gallatin Gateway, MTHyalite C at Hyalite R S nr Bozeman MTGallatin River at Logan MT

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 Gallatin River at Logan MT
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1895–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at Gallatin River at Logan MTLargest measured flow of each year at Gallatin River at Logan MT: Gallatin River at Logan MT in m³/s, from 1895 to 2025.Hurricane Katrina water and sanitation collapse100200300m³/s18951933194819621976199120052019

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
PeriodGallatin River at Logan MT (m³/s)
1895115
1896185
1897183
1898207
1899279
1900137
1902125
1903127
1904153
190587.5
1929141
193079.9
193184.1
1932129
1933105
1935113
1936124
1937103
1938158
193979.0
194099.1
194156.4
1942168
1943174
1944136
194599.1
1946106
1947174
1948223
1949110
1950112
1951117
1952188
1953168
195495.7
1955115
1956204
1957141
1958103
1959173
1960122
196161.2
1962137
1963135
1964178
1965173
196698.0
1967197
1968206
1969147
1970266
1971240
1972145
1973157
1974260
1975220
1976189
197774.2
1978141
1979122
1980129
1981209
1982203
1983181
1984200
1985105
198759.5
1988113
1989106
1990124
1991230
1992122
1993182
199496.6
1995204
1996207
1997266
1998178
1999159
2000111
200173.9
2002158
2003165
2004105
2005115
2006142
2007105
2008178
2009158
2010173
2011226
2012141
2013114
2014188
2015128
2016112
2017130
2018204
2019159
2020182
2021134
2022246
2023159
2024155
2025127

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 held1895–2025
Completeness80.2% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 4 separate periods inside 1895–2025 hold no value. The longest runs from 1906 to 1928 — 23 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1895 and is not continuous from it: 131 years separate the first value from the last, and 80% 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 Gallatin River at Logan MT, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1894–2024.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above Gallatin River at Logan MT, as a depthWater leaving the catchment above Gallatin River at Logan MT, as a depth: Gallatin River at Logan MT in mm, from 1894 to 2024.Hurricane Katrina water and sanitation collapse0100200300400mm18941931194519591973198720012015

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
PeriodGallatin River at Logan MT (mm)
1894221
1895204
1896209
1897214
1898235
1899251
1900201
1901192
1902173
1903195
1904222
1905135
1929178
1930146
1931123
1932167
1933145
193472.0
1935113
1936121
1937120
1938176
1939142
1940159
1941143
1942210
1943241
1944189
1945179
1946191
1947255
1948280
1949185
1950195
1951189
1952268
1953188
1954148
1955163
1956203
1957185
1958164
1959221
1960195
1961140
1962249
1963213
1964239
1965288
1966162
1967255
1968308
1969278
1970311
1971303
1972226
1973231
1974278
1975330
1976312
1977164
1978250
1979203
1980219
1981252
1982305
1983261
1984297
1985160
1986226
1987136
1988153
1989166
1990182
1991200
1992161
1993305
1994147
1995256
1996238
1997331
1998250
1999204
2000149
2001123
2002146
2003148
2004127
2005162
2006184
2007158
2008246
2009221
2010221
2011306
2012175
2013145
2014221
2015159
2016169
2017195
2018280
2019228
2020205
2021141
2022186
2024186

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 held1894–2024
Completeness81.7% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 2 separate periods inside 1894–2024 hold no value. The longest runs from 1906 to 1928 — 23 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1894 and is not continuous from it: 131 years separate the first value from the last, and 82% 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

The snow standing above this water

4 automated snow stations sit inside this drainage area, weighing the snowpack rather than measuring how deep it is.

598
Fullest snowpack recorded at Lick Creek, in 1970 (mm of water)
123
Thinnest, in 2026 (mm of water)
April
Month the pack is usually at its fullest
June
Month the pack has gone by, in half of years
Peak snowpack at Lick Creek
Water years 1964–2026. Each point is the fullest month of that snow season.
Peak snowpack at Lick CreekPeak snowpack at Lick Creek: Lick Creek in mm, from 1964 to 2026.0200400600mm19641972198019881996200420122020Lick Creek 1964: 486 mmLick Creek 1965: 432 mmLick Creek 1966: 227 mmLick Creek 1967: 479 mmLick Creek 1968: 451 mmLick Creek 1969: 214 mmLick Creek 1970: 598 mmLick Creek 1971: 545 mmLick Creek 1972: 274 mmLick Creek 1973: 474 mmLick Creek 1974: 426 mmLick Creek 1975: 577 mmLick Creek 1976: 428 mmLick Creek 1977: 396 mmLick Creek 1978: 257 mmLick Creek 1979: 326 mmLick Creek 1980: 336 mmLick Creek 1981: 275 mmLick Creek 1982: 395 mmLick Creek 1983: 334 mmLick Creek 1984: 342 mmLick Creek 1985: 275 mmLick Creek 1986: 218 mmLick Creek 1987: 208 mmLick Creek 1988: 317 mmLick Creek 1989: 266 mmLick Creek 1990: 286 mmLick Creek 1991: 375 mmLick Creek 1992: 219 mmLick Creek 1993: 258 mmLick Creek 1994: 214 mmLick Creek 1995: 344 mmLick Creek 1996: 270 mmLick Creek 1997: 442 mmLick Creek 1998: 275 mmLick Creek 1999: 294 mmLick Creek 2000: 255 mmLick Creek 2001: 243 mmLick Creek 2002: 211 mmLick Creek 2003: 316 mmLick Creek 2004: 238 mmLick Creek 2005: 231 mmLick Creek 2006: 225 mmLick Creek 2007: 285 mmLick Creek 2008: 327 mmLick Creek 2009: 329 mmLick Creek 2010: 237 mmLick Creek 2011: 387 mmLick Creek 2012: 261 mmLick Creek 2013: 270 mmLick Creek 2014: 441 mmLick Creek 2015: 196 mmLick Creek 2016: 242 mmLick Creek 2017: 161 mmLick Creek 2018: 365 mmLick Creek 2019: 254 mmLick Creek 2020: 343 mmLick Creek 2021: 282 mmLick Creek 2022: 248 mmLick Creek 2023: 356 mmLick Creek 2024: 184 mmLick Creek 2025: 304 mmLick Creek 2026: 123 mm

A water year runs October to September and is named for the year it ends, so the snow of one winter stays in one point. The value is the fullest month, not the fullest day: a pack that peaked sharply mid-month reads lower here than a single measurement taken at the right moment would.

View the data behind this chart
Underlying data
PeriodLick Creek (mm)
1964486
1965432
1966227
1967479
1968451
1969214
1970598
1971545
1972274
1973474
1974426
1975577
1976428
1977396
1978257
1979326
1980336
1981275
1982395
1983334
1984342
1985275
1986218
1987208
1988317
1989266
1990286
1991375
1992219
1993258
1994214
1995344
1996270
1997442
1998275
1999294
2000255
2001243
2002211
2003316
2004238
2005231
2006225
2007285
2008327
2009329
2010237
2011387
2012261
2013270
2014441
2015196
2016242
2017161
2018365
2019254
2020343
2021282
2022248
2023356
2024184
2025304
2026123

Read against the river

Lick Creek and Gallatin River near Gallatin Gateway, MT both sit in this drainage area, and their records overlap by 61 years. That is the span the two have in common, not a count of years both actually hold — either record may have gaps inside it. The two are shown separately rather than on one axis: millimetres of stored water and cubic metres per second are not commensurable, and a difference between them would mean nothing.

Being in the same drainage area does not put the snowpack upstream of the gauge. A subbasin is an area, and snow on one tributary can join the river below a gauge on another — so a weak relationship here may say more about which tributary was measured than about the snow.

Every gauge Hydrionis holds within this area

Gauges within the Gallatin and what each holds
GaugeMeasuresValuesRecord
Gallatin River at Logan MTburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3571893–2026
Gallatin River near Gallatin Gateway, MTburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3181889–2026
Hyalite C at Hyalite R S nr Bozeman MTburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2491895–2026

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 — 10020008. 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
Gallatin River at Logan MTStated 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
Gallatin River near Gallatin Gateway, MTStated 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
Hyalite C at Hyalite R S nr Bozeman MTStated 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 spanned138yes, 20 or more
Values held3,550yes, 1000 or more
Distinct measurements6yes, 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), Gallatin gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-gallatin/

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 Gallatin 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 confidence2025-06-02

Source: USGS — National Water Information System, USGS site 06052500, 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.