The monitoring network within this area

Hydrionis holds 1,045 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
1,045
Values held
1909–2026
Record spans
Gauges within the San Miguel huc8 subbasin
2 monitoring points, positioned as the publisher records them.
Gauges within the San Miguel huc8 subbasinSAN MIGUEL RIVER NEAR PLACERVILLE, CO, SAN MIGUEL RIVER AT NATURITA, CO.SAN MIGUEL RIVER NEAR PLACERVILLE, COSAN MIGUEL RIVER AT NATURITA, CO.

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 SAN MIGUEL RIVER NEAR PLACERVILLE, CO
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1909–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at SAN MIGUEL RIVER NEAR PLACERVILLE, COLargest measured flow of each year at SAN MIGUEL RIVER NEAR PLACERVILLE, CO: SAN MIGUEL RIVER NEAR PLACERVILLE, CO in m³/s, from 1909 to 2025.Hurricane Katrina water and sanitation collapse0100200300m³/s19091947195919711983199520082020

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
PeriodSAN MIGUEL RIVER NEAR PLACERVILLE, CO (m³/s)
1909283
191167.4
193048.4
193120.2
193236.0
193341.6
193418.6
194241.3
194325.5
194486.6
194540.5
194634.5
194737.7
194845.6
194967.1
195024.5
195120.8
195248.4
195349.8
195417.0
195532.3
195627.8
195766.5
195861.7
195931.7
196048.7
196138.2
196229.2
196325.9
196439.6
196568.0
196624.4
196727.3
196851.5
196930.0
197065.1
197138.8
197224.7
197375.3
197431.1
197556.9
197630.9
197714.6
197850.1
197962.0
198054.7
198132.6
198250.1
1983108
198478.7
198555.2
198643.6
198750.7
198831.4
198922.3
199032.6
199129.2
199227.1
199345.9
199436.8
199559.7
199634.0
199750.7
199833.4
199962.0
200036.0
200152.7
200215.9
200347.6
200428.9
200545.9
200626.8
200851.5
200951.8
201054.1
201144.7
201216.8
201325.8
201446.4
201548.4
201646.4
201740.2
201812.8
201943.3
202026.0
202120.8
202223.6
202332.0
202440.8
202526.4

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 held1909–2025
Completeness76.9% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 4 separate periods inside 1909–2025 hold no value. The longest runs from 1912 to 1929 — 18 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1909 and is not continuous from it: 117 years separate the first value from the last, and 77% 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 SAN MIGUEL RIVER NEAR PLACERVILLE, CO, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1911–2024.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above SAN MIGUEL RIVER NEAR PLACERVILLE, CO, as a depthWater leaving the catchment above SAN MIGUEL RIVER NEAR PLACERVILLE, CO, as a depth: SAN MIGUEL RIVER NEAR PLACERVILLE, CO in mm, from 1911 to 2024.Hurricane Katrina water and sanitation collapse0200400mm19111950196119721983199520062017

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
PeriodSAN MIGUEL RIVER NEAR PLACERVILLE, CO (mm)
1911358
1931155
1932300
1933219
1943255
1944360
1945274
1946228
1947307
1948343
1949309
1950184
1951148
1952340
1953211
1954165
1955187
1956176
1957393
1958401
1959169
1960254
1961266
1962260
1963174
1964211
1965359
1966195
1967173
1968246
1969241
1970291
1971252
1972175
1973359
1974185
1975330
1976177
197798.0
1978264
1979321
1980274
1981174
1982330
1983457
1984462
1985399
1986349
1987382
1988206
1989172
1990166
1991223
1992247
1994227
1995414
1996222
1997412
1998271
1999370
2000231
2001244
2002102
2003202
2004217
2005283
2006226
2007291
2008317
2009257
2010247
2011275
2012155
2013180
2014275
2015285
2016264
2017271
201895.0
2019331
2020145
2021148
2022170
2023282
2024194

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 held1911–2024
Completeness74.6% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 3 separate periods inside 1911–2024 hold no value. The longest runs from 1912 to 1930 — 19 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1911 and is not continuous from it: 114 years separate the first value from the last, and 75% 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.

713
Fullest snowpack recorded at Lone Cone, in 1997 (mm of water)
163
Thinnest, in 1990 (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 Lone Cone
Water years 1981–2026. Each point is the fullest month of that snow season.
Peak snowpack at Lone ConePeak snowpack at Lone Cone: Lone Cone in mm, from 1981 to 2026.0200400600800mm19811987199319992005201120172023Lone Cone 1981: 262 mmLone Cone 1982: 525 mmLone Cone 1983: 486 mmLone Cone 1984: 410 mmLone Cone 1985: 494 mmLone Cone 1986: 484 mmLone Cone 1987: 486 mmLone Cone 1988: 317 mmLone Cone 1989: 476 mmLone Cone 1990: 163 mmLone Cone 1991: 425 mmLone Cone 1992: 434 mmLone Cone 1993: 613 mmLone Cone 1994: 370 mmLone Cone 1995: 586 mmLone Cone 1996: 334 mmLone Cone 1997: 713 mmLone Cone 1998: 419 mmLone Cone 1999: 306 mmLone Cone 2000: 341 mmLone Cone 2001: 353 mmLone Cone 2002: 248 mmLone Cone 2003: 350 mmLone Cone 2004: 349 mmLone Cone 2005: 443 mmLone Cone 2006: 270 mmLone Cone 2007: 351 mmLone Cone 2008: 553 mmLone Cone 2009: 417 mmLone Cone 2010: 435 mmLone Cone 2011: 339 mmLone Cone 2012: 325 mmLone Cone 2013: 326 mmLone Cone 2014: 345 mmLone Cone 2015: 278 mmLone Cone 2016: 360 mmLone Cone 2017: 513 mmLone Cone 2018: 215 mmLone Cone 2019: 537 mmLone Cone 2020: 292 mmLone Cone 2021: 305 mmLone Cone 2022: 377 mmLone Cone 2023: 591 mmLone Cone 2024: 347 mmLone Cone 2025: 265 mmLone Cone 2026: 206 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
PeriodLone Cone (mm)
1981262
1982525
1983486
1984410
1985494
1986484
1987486
1988317
1989476
1990163
1991425
1992434
1993613
1994370
1995586
1996334
1997713
1998419
1999306
2000341
2001353
2002248
2003350
2004349
2005443
2006270
2007351
2008553
2009417
2010435
2011339
2012325
2013326
2014345
2015278
2016360
2017513
2018215
2019537
2020292
2021305
2022377
2023591
2024347
2025265
2026206

Read against the river

Lone Cone and SAN MIGUEL RIVER NEAR PLACERVILLE, CO 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 San Miguel and what each holds
GaugeMeasuresValuesRecord
SAN MIGUEL RIVER NEAR PLACERVILLE, COburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2991909–2026
SAN MIGUEL RIVER AT NATURITA, CO.burned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year1921917–2026

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 — 14030003. 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
SAN MIGUEL RIVER NEAR PLACERVILLE, COStated 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
SAN MIGUEL RIVER AT NATURITA, CO.Stated 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 spanned118yes, 20 or more
Values held1,045yes, 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), San Miguel gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-san-miguel/

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 San Miguel 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 09172500, 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.