The monitoring network within this area

Hydrionis holds 2,764 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
2,764
Values held
1903–2026
Record spans
Gauges within the Snake Headwaters huc8 subbasin
3 monitoring points, positioned as the publisher records them.
Gauges within the Snake Headwaters huc8 subbasinSNAKE RIVER NEAR MORAN, WY, Pacific Creek at Moran, WY, SPREAD CREEK NEAR MORAN, WYSNAKE RIVER NEAR MORAN, WYPacific Creek at Moran, WYSPREAD CREEK NEAR MORAN, WY

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 SNAKE RIVER NEAR MORAN, WY
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1904–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at SNAKE RIVER NEAR MORAN, WYLargest measured flow of each year at SNAKE RIVER NEAR MORAN, WY: SNAKE RIVER NEAR MORAN, WY in m³/s, from 1904 to 2025.Hurricane Katrina water and sanitation collapse0200400m³/s19041918193719511966198019952012

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
PeriodSNAKE RIVER NEAR MORAN, WY (m³/s)
1904225
1905141
1906168
1907209
1908178
1909300
1910343
1911275
1912265
1913286
1914271
1915272
1916265
1917340
1918428
1919331
1920311
1921309
1922314
1923303
1924257
1925261
1926273
1927402
1928323
1929220
1935236
1936166
1937215
1938211
1939209
1940231
1941193
1942221
1943377
1944240
1945197
1946265
1947245
1948248
1949207
1950229
1951166
1952218
1953199
1954303
1955212
1956177
1958125
1959193
1960149
1961178
1962121
1963229
1964151
1965138
1966140
1967133
1968161
1969126
1970163
1971197
1972147
1973130
1974191
1975152
1976173
1977142
1978164
1979139
1980169
1981323
1982207
1983257
1984259
1985215
1986297
1987118
1988175
1989131
1991201
1992145
199388.3
1994170
1995143
1996260
1997343
1998174
1999187
2000166
2004195
2005129
2006190
2007131
2008174
2009162
2010317
2011239
2012174
2013146
201496.3
2015132
201695.1
2017188
2018207
2019133
2020159
2021150
2022110
202369.4
2024175
2025112

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 held1904–2025
Completeness91.8% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 4 separate periods inside 1904–2025 hold no value. The longest runs from 1930 to 1934 — 5 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1904 and is not continuous from it: 122 years separate the first value from the last, and 92% 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 SNAKE RIVER NEAR MORAN, WY, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1904–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above SNAKE RIVER NEAR MORAN, WY, as a depthWater leaving the catchment above SNAKE RIVER NEAR MORAN, WY, as a depth: SNAKE RIVER NEAR MORAN, WY in mm, from 1904 to 2025.Hurricane Katrina water and sanitation collapse2505007501,000mm19041920193619521968198420002016

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
PeriodSNAKE RIVER NEAR MORAN, WY (mm)
1904755
1905422
1906501
1907842
1908654
1909907
1910637
1911846
1912768
1913845
1914623
1915443
1916614
1917669
1918841
1919506
1920501
1921616
1922551
1923620
1924467
1925556
1926684
1927598
1928731
1929575
1930556
1931481
1932369
1933624
1934483
1935494
1936481
1937543
1938577
1939576
1940557
1941426
1942472
1943686
1944643
1945374
1946718
1947632
1948743
1949632
1950530
1951697
1952904
1953603
1954650
1955605
19561,034
1957338
1958543
1959526
1960535
1961673
1962397
1963499
1964615
1965729
1966632
1967603
1968571
1969594
1970667
1971869
1972821
1973498
1974878
1975667
1976745
1977464
1978493
1979563
1980542
1981514
1982840
1983742
1984853
1985659
1986928
1987386
1988407
1989329
1990515
1991502
1992724
1993328
1994553
1995556
1996915
19971,118
1998754
1999771
2000519
2001671
2002475
2003603
2004553
2005341
2006474
2007616
2008484
2009666
2010483
2011895
2012608
2013746
2014406
2015477
2016477
2017801
2018727
2019628
2020496
2021693
2022470
2023301
2024445
2025488

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 held1904–2025
Completeness100.0% of the periods in that span are held.
ContinuityContinuous: every year from 1904 to 2025 is held.
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.

1,494
Fullest snowpack recorded at Lewis Lake Divide, in 1982 (mm of water)
445
Thinnest, in 1987 (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 Lewis Lake Divide
Water years 1981–2026. Each point is the fullest month of that snow season.
Peak snowpack at Lewis Lake DividePeak snowpack at Lewis Lake Divide: Lewis Lake Divide in mm, from 1981 to 2026.05001,0001,500mm19811987199319992005201120172023Lewis Lake Divide 1981: 473 mmLewis Lake Divide 1982: 1,494 mmLewis Lake Divide 1983: 957 mmLewis Lake Divide 1984: 738 mmLewis Lake Divide 1985: 762 mmLewis Lake Divide 1986: 1,160 mmLewis Lake Divide 1987: 445 mmLewis Lake Divide 1988: 699 mmLewis Lake Divide 1989: 1,113 mmLewis Lake Divide 1990: 685 mmLewis Lake Divide 1991: 736 mmLewis Lake Divide 1992: 579 mmLewis Lake Divide 1993: 818 mmLewis Lake Divide 1994: 517 mmLewis Lake Divide 1995: 1,052 mmLewis Lake Divide 1996: 1,212 mmLewis Lake Divide 1997: 1,380 mmLewis Lake Divide 1998: 812 mmLewis Lake Divide 1999: 1,044 mmLewis Lake Divide 2000: 622 mmLewis Lake Divide 2001: 460 mmLewis Lake Divide 2002: 773 mmLewis Lake Divide 2003: 841 mmLewis Lake Divide 2004: 752 mmLewis Lake Divide 2005: 590 mmLewis Lake Divide 2006: 1,113 mmLewis Lake Divide 2007: 582 mmLewis Lake Divide 2008: 967 mmLewis Lake Divide 2009: 851 mmLewis Lake Divide 2010: 464 mmLewis Lake Divide 2011: 1,312 mmLewis Lake Divide 2012: 809 mmLewis Lake Divide 2013: 754 mmLewis Lake Divide 2014: 1,040 mmLewis Lake Divide 2015: 530 mmLewis Lake Divide 2016: 672 mmLewis Lake Divide 2017: 1,180 mmLewis Lake Divide 2018: 1,100 mmLewis Lake Divide 2019: 940 mmLewis Lake Divide 2020: 717 mmLewis Lake Divide 2021: 624 mmLewis Lake Divide 2022: 580 mmLewis Lake Divide 2023: 978 mmLewis Lake Divide 2024: 765 mmLewis Lake Divide 2025: 776 mmLewis Lake Divide 2026: 715 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
PeriodLewis Lake Divide (mm)
1981473
19821,494
1983957
1984738
1985762
19861,160
1987445
1988699
19891,113
1990685
1991736
1992579
1993818
1994517
19951,052
19961,212
19971,380
1998812
19991,044
2000622
2001460
2002773
2003841
2004752
2005590
20061,113
2007582
2008967
2009851
2010464
20111,312
2012809
2013754
20141,040
2015530
2016672
20171,180
20181,100
2019940
2020717
2021624
2022580
2023978
2024765
2025776
2026715

Read against the river

Lewis Lake Divide and SNAKE RIVER NEAR MORAN, WY both sit in this drainage area, and their records overlap by 44 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 Snake Headwaters and what each holds
GaugeMeasuresValuesRecord
SNAKE RIVER NEAR MORAN, WYburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3941903–2026
Pacific Creek at Moran, WYburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2711918–2026
SPREAD CREEK NEAR MORAN, WYcatchment area, annual maximum river flow21918–2026

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 — 17040101. 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
SNAKE RIVER NEAR MORAN, WYStated 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
Pacific Creek at Moran, WYStated 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
SPREAD CREEK NEAR MORAN, WYStated 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 record2no
Years spanned124yes, 20 or more
Values held2,764yes, 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), Snake Headwaters gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-snake-headwaters/

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 Snake Headwaters 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 confidence2025-06-03

Source: USGS — National Water Information System, USGS site 13011000, 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.