The monitoring network within this area

Hydrionis holds 1,888 values from 4 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.

4
Gauges
1,888
Values held
1905–2026
Record spans
Gauges within the North Santiam huc8 subbasin
4 monitoring points, positioned as the publisher records them.
Gauges within the North Santiam huc8 subbasinNO SANTIAM R BLW BOULDER CRK, NR DETROIT, OR, NORTH SANTIAM RIVER AT NIAGARA, OR, NORTH SANTIAM RIVER AT MEHAMA, OR, SANTIAM RIVER AT JEFFERSON, ORNO SANTIAM R BLW BOULDER CRK, NR DETROIT, ORNORTH SANTIAM RIVER AT NIAGARA, ORNORTH SANTIAM RIVER AT MEHAMA, ORSANTIAM RIVER AT JEFFERSON, OR

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 NORTH SANTIAM RIVER AT MEHAMA, OR
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1906–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at NORTH SANTIAM RIVER AT MEHAMA, ORLargest measured flow of each year at NORTH SANTIAM RIVER AT MEHAMA, OR: NORTH SANTIAM RIVER AT MEHAMA, OR in m³/s, from 1906 to 2025.Hurricane Katrina water and sanitation collapse01,0002,000m³/s19061931194519601974199020042020

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
PeriodNORTH SANTIAM RIVER AT MEHAMA, OR (m³/s)
1906586
19071,441
1910756
19121,393
1913968
19211,781
19231,781
1925892
1926963
19271,359
1929391
19311,529
19321,331
1933745
1934966
1936866
1937852
1938895
1940564
1941753
19421,606
1943515
1945946
19461,484
19481,705
19491,031
19501,107
1951660
1953674
1954498
1956716
1957501
1958527
1960425
1961487
1962742
1963583
19641,654
1966453
1967493
1968592
1970597
1971597
19721,226
1974637
1975626
1977134
1978609
1980513
1981549
1983564
1984481
1986835
1987498
1989612
1990705
1991459
1993535
1994351
19961,523
1997510
1998716
19991,005
2001244
2002646
2003464
2004343
2006549
2008425
2009728
2010665
20111,031
2012801
2014595
2015634
2017586
2019504
2020493
2022668
2023663
2025544

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 held1906–2025
Completeness67.5% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 32 separate periods inside 1906–2025 hold no value. The longest runs from 1914 to 1920 — 7 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1906 and is not continuous from it: 120 years separate the first value from the last, and 68% 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 NORTH SANTIAM RIVER AT MEHAMA, OR, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1906–2024.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above NORTH SANTIAM RIVER AT MEHAMA, OR, as a depthWater leaving the catchment above NORTH SANTIAM RIVER AT MEHAMA, OR, as a depth: NORTH SANTIAM RIVER AT MEHAMA, OR in mm, from 1906 to 2024.Hurricane Katrina water and sanitation collapse1,0002,0003,000mm19061932194619601974198820022016

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
PeriodNORTH SANTIAM RIVER AT MEHAMA, OR (mm)
19062,061
19111,505
19122,402
19132,052
19221,564
19231,866
19241,510
19251,797
19261,459
19272,178
19281,566
19291,332
19301,094
19311,277
19322,024
19332,201
19341,564
19351,268
19361,484
19371,996
19381,697
19391,277
19401,366
19411,256
19421,690
19431,790
1944948
19451,926
19462,070
19471,656
19481,928
19491,827
19502,616
19511,991
19521,442
19532,397
19541,761
19552,283
19562,239
19571,568
19582,010
19591,699
19601,905
19612,017
19621,827
19631,545
19641,999
19651,575
19661,658
19671,493
19681,949
19691,685
19701,845
19712,323
19722,389
19731,736
19742,287
19752,193
19761,540
19771,743
19781,397
19791,527
19801,590
19811,745
19822,129
19832,158
19842,173
19851,471
19861,793
19871,190
19881,644
19891,464
19901,727
19911,581
19921,133
19931,590
19941,487
19952,258
19962,663
19972,216
19981,901
19992,338
20001,540
20011,305
20021,592
20031,823
20041,664
20051,298
20062,240
20071,730
20081,999
20091,895
20102,016
20111,908
20122,606
20131,603
20142,278
20151,408
20161,921
20172,451
20181,491
20191,449
20201,794
20211,724
20222,071
20231,639
20241,899

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 held1906–2024
Completeness89.9% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 2 separate periods inside 1906–2024 hold no value. The longest runs from 1914 to 1921 — 8 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1906 and is not continuous from it: 119 years separate the first value from the last, and 90% 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

1 automated snow station sits inside this drainage area, weighing the snowpack rather than measuring how deep it is.

862
Fullest snowpack recorded at Marion Forks, in 2008 (mm of water)
6
Thinnest, in 2015 (mm of water)
March
Month the pack is usually at its fullest
May
Month the pack has gone by, in half of years
Peak snowpack at Marion Forks
Water years 1981–2026. Each point is the fullest month of that snow season.
Peak snowpack at Marion ForksPeak snowpack at Marion Forks: Marion Forks in mm, from 1981 to 2026.02505007501,000mm19811987199319992005201120172023Marion Forks 1981: 34.0 mmMarion Forks 1982: 488 mmMarion Forks 1983: 109 mmMarion Forks 1984: 152 mmMarion Forks 1985: 574 mmMarion Forks 1986: 234 mmMarion Forks 1987: 84.0 mmMarion Forks 1988: 263 mmMarion Forks 1989: 433 mmMarion Forks 1990: 421 mmMarion Forks 1991: 110 mmMarion Forks 1992: 25.0 mmMarion Forks 1993: 412 mmMarion Forks 1994: 92.0 mmMarion Forks 1995: 272 mmMarion Forks 1996: 84.0 mmMarion Forks 1997: 349 mmMarion Forks 1998: 88.0 mmMarion Forks 1999: 640 mmMarion Forks 2000: 341 mmMarion Forks 2001: 132 mmMarion Forks 2002: 629 mmMarion Forks 2003: 47.0 mmMarion Forks 2004: 309 mmMarion Forks 2005: 59.0 mmMarion Forks 2006: 216 mmMarion Forks 2007: 154 mmMarion Forks 2008: 862 mmMarion Forks 2009: 396 mmMarion Forks 2010: 67.0 mmMarion Forks 2011: 196 mmMarion Forks 2012: 396 mmMarion Forks 2013: 299 mmMarion Forks 2014: 98.0 mmMarion Forks 2015: 6.00 mmMarion Forks 2016: 174 mmMarion Forks 2017: 452 mmMarion Forks 2018: 172 mmMarion Forks 2019: 324 mmMarion Forks 2020: 222 mmMarion Forks 2021: 198 mmMarion Forks 2022: 285 mmMarion Forks 2023: 410 mmMarion Forks 2024: 208 mmMarion Forks 2025: 61.0 mmMarion Forks 2026: 21.0 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
PeriodMarion Forks (mm)
198134.0
1982488
1983109
1984152
1985574
1986234
198784.0
1988263
1989433
1990421
1991110
199225.0
1993412
199492.0
1995272
199684.0
1997349
199888.0
1999640
2000341
2001132
2002629
200347.0
2004309
200559.0
2006216
2007154
2008862
2009396
201067.0
2011196
2012396
2013299
201498.0
20156.00
2016174
2017452
2018172
2019324
2020222
2021198
2022285
2023410
2024208
202561.0
202621.0

Read against the river

Marion Forks and NO SANTIAM R BLW BOULDER CRK, NR DETROIT, OR 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 North Santiam and what each holds
GaugeMeasuresValuesRecord
NORTH SANTIAM RIVER AT MEHAMA, ORburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3621905–2026
NO SANTIAM R BLW BOULDER CRK, NR DETROIT, ORburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3331907–2026
NORTH SANTIAM RIVER AT NIAGARA, ORburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3241909–2026
SANTIAM RIVER AT JEFFERSON, ORburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3171907–2026

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 — 17090005. 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
NORTH SANTIAM RIVER AT MEHAMA, ORStated 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
NO SANTIAM R BLW BOULDER CRK, NR DETROIT, ORStated 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
NORTH SANTIAM RIVER AT NIAGARA, ORStated 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
SANTIAM RIVER AT JEFFERSON, ORStated 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 record4yes, 3 or more
Years spanned122yes, 20 or more
Values held1,888yes, 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), North Santiam gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-north-santiam/

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 North Santiam 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 confidence2025-02-23

Source: USGS — National Water Information System, USGS site 14183000, 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.