The monitoring network within this area

Hydrionis holds 1,315 values from 7 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.

7
Gauges
1,315
Values held
1911–2026
Record spans
Gauges within the Middle Fork Feather huc8 subbasin
7 monitoring points, positioned as the publisher records them.
Gauges within the Middle Fork Feather huc8 subbasinMF FEATHER R NR CLIO CA, SF FEATHER R BL LITTLE GRASS VALLEY DAM CA, LOST C NR CLIPPER MILLS CA, PALERMO CN A ENTERPRISE CA, SF FEATHER R A ENTERPRISE CA, FEATHER R A BIDWELL BAR CA, BIG GRIZZLY C AT GRIZZLY VALLEY DAM NR PORTOLA CAMF FEATHER R NR CLIO CASF FEATHER R BL LITTLE GRASS VALLEY DAM CALOST C NR CLIPPER MILLS CAPALERMO CN A ENTERPRISE CASF FEATHER R A ENTERPRISE CAFEATHER R A BIDWELL BAR CABIG GRIZZLY C AT GRIZZLY VALLEY DAM NR PORTOLA CA

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 LOST C NR CLIPPER MILLS CA
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1928–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at LOST C NR CLIPPER MILLS CALargest measured flow of each year at LOST C NR CLIPPER MILLS CA: LOST C NR CLIPPER MILLS CA in m³/s, from 1928 to 2025.Hurricane Katrina water and sanitation collapse050100150200m³/s19281940195919711983199520062018

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
PeriodLOST C NR CLIPPER MILLS CA (m³/s)
192882.1
192915.9
193111.3
193218.4
19337.39
193411.9
193541.3
193660.6
193712.3
19397.02
194079.3
194166.8
194910.8
195086.1
195236.5
195373.6
195434.8
195510.1
195787.2
195879.0
195937.4
1960122
196115.9
196213.6
19646.63
19667.39
196717.4
196819.8
196968.0
197075.9
197119.4
197216.6
197477.0
197510.6
19760.850
197723.2
197820.6
19792.55
198052.1
19810.708
198373.9
19850.680
1986104
19870.708
198916.8
19900.651
19910.736
19920.481
199322.7
19940.340
199540.5
199653.0
1997163
199831.4
199926.7
200025.1
20020.595
200319.4
20040.566
200524.5
200643.0
20071.93
200916.7
201021.0
201130.6
201229.2
20141.05
20150.821
20160.680
201795.7
201824.6
201938.8
202011.9
20226.80
202334.5
202420.3
202532.3

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 held1928–2025
Completeness78.6% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 15 separate periods inside 1928–2025 hold no value. The longest runs from 1942 to 1948 — 7 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1928 and is not continuous from it: 98 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 publisher2026-10-01
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 LOST C NR CLIPPER MILLS CA, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1928–2024.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above LOST C NR CLIPPER MILLS CA, as a depthWater leaving the catchment above LOST C NR CLIPPER MILLS CA, as a depth: LOST C NR CLIPPER MILLS CA in mm, from 1928 to 2024.Hurricane Katrina water and sanitation collapse01,0002,000mm19281940196019721984199620082020

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
PeriodLOST C NR CLIPPER MILLS CA (mm)
1928795
1929275
1930561
193177.0
1932652
1933261
1934285
1935841
1936931
1937801
19381,719
1939229
19401,399
1949405
19501,096
19511,011
19521,597
19531,252
1954864
1955953
19561,299
1957827
19581,575
1959445
1960640
1961398
19621,102
1963306
1964174
1965517
1966148
1967188
196888.0
1969403
1970492
197116.0
197216.0
19737.00
1974472
197516.0
197614.0
197720.0
197882.0
197920.0
1980575
1981360
1982605
1983942
1984141
198517.0
1986632
198746.0
198855.0
1989355
199053.0
199156.0
199257.0
1993722
199456.0
19952,294
19961,321
19971,453
19981,471
1999464
2000424
200188.0
200297.0
2003328
2004100
2005521
20061,447
200791.0
200894.0
2009225
2010297
20111,619
2012265
2013101
201498.0
201598.0
201693.0
20171,149
2018299
20191,229
2020302
202196.0
202297.0
2023846
2024512

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 held1928–2024
Completeness91.8% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • One period inside 1928–2024 holds no value: 1941 to 1948, 8 years with no reading. It is drawn as a break in the line and is never interpolated across.
ContinuityThe record begins in 1928 and is not continuous from it: 97 years separate the first value from the last, and 92% 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 Middle Fork Feather and what each holds
GaugeMeasuresValuesRecord
LOST C NR CLIPPER MILLS CAburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3081927–2026
SF FEATHER R BL LITTLE GRASS VALLEY DAM CAburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2461927–2026
SF FEATHER R A ENTERPRISE CAburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2001911–2026
MF FEATHER R NR CLIO CAburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year1981925–2026
FEATHER R A BIDWELL BAR CAburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year1951911–2026
PALERMO CN A ENTERPRISE CAburned area within 50 km, mean river flow, mean river flow, water year1421911–2019
BIG GRIZZLY C AT GRIZZLY VALLEY DAM NR PORTOLA CAcatchment area, annual maximum river flow261926–2026

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 — 18020123. 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
LOST C NR CLIPPER MILLS CAStated 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
SF FEATHER R BL LITTLE GRASS VALLEY DAM CAStated 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
SF FEATHER R A ENTERPRISE CAStated 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
MF FEATHER R NR CLIO CAStated 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
FEATHER R A BIDWELL BAR CAStated 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
PALERMO CN A ENTERPRISE CAStated 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
BIG GRIZZLY C AT GRIZZLY VALLEY DAM NR PORTOLA CAStated 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 record6yes, 3 or more
Years spanned116yes, 20 or more
Values held1,315yes, 1000 or more
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), Middle Fork Feather gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-middle-fork-feather/

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 Middle Fork Feather 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 confidence2025-02-14

Source: USGS — National Water Information System, USGS site 11396000, 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.