The monitoring network within this area

Hydrionis holds 4,164 values from 8 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.

8
Gauges
4,164
Values held
1888–2026
Record spans
Gauges within the St. Vrain huc8 subbasin
8 monitoring points, positioned as the publisher records them.
Gauges within the St. Vrain huc8 subbasinST. VRAIN CREEK AT LYONS, CO., MIDDLE BOULDER CREEK AT NEDERLAND, CO., BOULDER CREEK NEAR ORODELL, CO., BOULDER CREEK AT MOUTH NEAR LONGMONT, CO, ST. VRAIN CREEK AT MOUTH, NEAR PLATTEVILLE, CO., NORTH ST. VRAIN CREEK NEAR ALLENS PARK, CO., LEFT HAND CREEK NEAR BOULDER, CO., SOUTH BOULDER CREEK NEAR ELDORADO SPRINGS, CO.ST. VRAIN CREEK AT LYONS, CO.MIDDLE BOULDER CREEK AT NEDERLAND, CO.BOULDER CREEK NEAR ORODELL, CO.BOULDER CREEK AT MOUTH NEAR LONGMONT, COST. VRAIN CREEK AT MOUTH, NEAR PLATTEVILLE, CO.NORTH ST. VRAIN CREEK NEAR ALLENS PARK, CO.LEFT HAND CREEK NEAR BOULDER, CO.SOUTH BOULDER CREEK NEAR ELDORADO SPRINGS, 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 ST. VRAIN CREEK AT LYONS, CO.
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1888–2013.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at ST. VRAIN CREEK AT LYONS, CO.Largest measured flow of each year at ST. VRAIN CREEK AT LYONS, CO.: ST. VRAIN CREEK AT LYONS, CO. in m³/s, from 1888 to 2013.Hurricane Katrina water and sanitation collapse0200400600800m³/s18881905191919331947196119751989

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
PeriodST. VRAIN CREEK AT LYONS, CO. (m³/s)
188815.1
188915.5
189019.1
189139.6
189532.0
189642.5
189728.9
189817.1
189933.4
190026.0
190124.3
190214.6
190348.4
190424.1
190547.0
190633.1
190731.7
190818.4
190932.6
191013.2
191118.7
191232.6
191313.9
191443.6
191527.0
191617.6
191735.1
191848.1
1919266
192020.8
192158.0
192216.3
192347.3
192463.1
192511.6
192631.1
192717.1
192828.6
192921.7
193057.8
193141.1
193224.2
193332.0
193417.8
193566.3
193623.6
193734.8
193846.7
193927.7
194019.1
1941297
194242.8
194334.8
194427.2
194528.3
194660.6
194766.8
194823.2
194984.1
195020.2
1951111
195245.6
195327.5
19548.07
195519.3
195621.2
195786.6
195836.5
195924.3
196020.3
196171.9
196232.3
196336.8
196413.0
196552.1
196634.3
196756.9
196818.0
196982.1
197027.1
197149.8
197226.6
197338.5
197418.2
197526.1
197623.6
197720.7
197844.2
197929.7
198066.0
198111.8
198245.3
198341.6
198437.9
198529.4
198631.7
198730.6
198816.1
198928.3
199025.7
199136.2
199215.5
199323.2
199424.7
1995119
199631.7
199746.4
199818.7
2013674

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 held1888–2013
Completeness86.5% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 2 separate periods inside 1888–2013 hold no value. The longest runs from 1999 to 2012 — 14 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1888 and is not continuous from it: 126 years separate the first value from the last, and 87% 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 ST. VRAIN CREEK AT LYONS, 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. 1896–1997.
Water leaving the catchment above ST. VRAIN CREEK AT LYONS, CO., as a depthWater leaving the catchment above ST. VRAIN CREEK AT LYONS, CO., as a depth: ST. VRAIN CREEK AT LYONS, CO. in mm, from 1896 to 1997.0100200300400mm18961911192419371950196319761989

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 (0 events)

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
PeriodST. VRAIN CREEK AT LYONS, CO. (mm)
1896173
1897321
1898173
1899316
1900275
1901208
1902124
1905272
1906259
1907341
1908141
1909292
1910110
1911160
1912265
1913169
1914324
1915252
1916205
1917275
1918230
1919138
1920234
1921319
1922125
1923339
1924276
1925126
1926293
1927193
1928223
1929196
1930162
1931135
1932149
1933220
1934124
1935200
1936239
1937162
1938255
1939134
1940122
1941193
1942290
1943214
1944181
1945203
1946133
1947297
1948153
1949273
1950142
1951252
1952279
1953144
195474.0
1955106
1956140
1957357
1958190
1959175
1960156
1961232
1962152
1963130
1964106
1965254
196681.0
1967178
1968143
1969305
1970210
1971224
1972143
1973226
1974156
1975198
1976120
197788.0
1978224
1979265
1980320
198192.0
1982198
1983318
1984287
1985167
1986231
1987167
1988133
1989124
1990192
1991179
1992149
1993191
1994145
1995345
1996235
1997307

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 held1896–1997
Completeness98.0% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • One period inside 1896–1997 holds no value: 1903 to 1904, 2 years with no reading. It is drawn as a break in the line and is never interpolated across.
ContinuityThe record begins in 1896 and is not continuous from it: 102 years separate the first value from the last, and 98% 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

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

549
Fullest snowpack recorded at Lake Eldora, in 1996 (mm of water)
102
Thinnest, in 1981 (mm of water)
March
Month the pack is usually at its fullest
June
Month the pack has gone by, in half of years
Peak snowpack at Lake Eldora
Water years 1979–2026. Each point is the fullest month of that snow season.
Peak snowpack at Lake EldoraPeak snowpack at Lake Eldora: Lake Eldora in mm, from 1979 to 2026.0200400600mm19791985199119972003200920152021Lake Eldora 1979: 253 mmLake Eldora 1980: 416 mmLake Eldora 1981: 102 mmLake Eldora 1982: 228 mmLake Eldora 1983: 338 mmLake Eldora 1984: 393 mmLake Eldora 1985: 219 mmLake Eldora 1986: 251 mmLake Eldora 1987: 243 mmLake Eldora 1988: 286 mmLake Eldora 1989: 307 mmLake Eldora 1990: 355 mmLake Eldora 1991: 225 mmLake Eldora 1992: 293 mmLake Eldora 1993: 345 mmLake Eldora 1994: 317 mmLake Eldora 1995: 299 mmLake Eldora 1996: 549 mmLake Eldora 1997: 442 mmLake Eldora 1998: 354 mmLake Eldora 1999: 233 mmLake Eldora 2000: 299 mmLake Eldora 2001: 210 mmLake Eldora 2002: 157 mmLake Eldora 2003: 383 mmLake Eldora 2004: 149 mmLake Eldora 2005: 240 mmLake Eldora 2006: 298 mmLake Eldora 2007: 316 mmLake Eldora 2008: 318 mmLake Eldora 2009: 345 mmLake Eldora 2010: 247 mmLake Eldora 2011: 415 mmLake Eldora 2012: 241 mmLake Eldora 2013: 216 mmLake Eldora 2014: 436 mmLake Eldora 2015: 281 mmLake Eldora 2016: 305 mmLake Eldora 2017: 312 mmLake Eldora 2018: 241 mmLake Eldora 2019: 306 mmLake Eldora 2020: 353 mmLake Eldora 2021: 279 mmLake Eldora 2022: 234 mmLake Eldora 2023: 259 mmLake Eldora 2024: 306 mmLake Eldora 2025: 292 mmLake Eldora 2026: 142 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
PeriodLake Eldora (mm)
1979253
1980416
1981102
1982228
1983338
1984393
1985219
1986251
1987243
1988286
1989307
1990355
1991225
1992293
1993345
1994317
1995299
1996549
1997442
1998354
1999233
2000299
2001210
2002157
2003383
2004149
2005240
2006298
2007316
2008318
2009345
2010247
2011415
2012241
2013216
2014436
2015281
2016305
2017312
2018241
2019306
2020353
2021279
2022234
2023259
2024306
2025292
2026142

Read against the river

Lake Eldora and ST. VRAIN CREEK AT LYONS, CO. both sit in this drainage area, and their records overlap by 18 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 St. Vrain and what each holds
GaugeMeasuresValuesRecord
ST. VRAIN CREEK AT LYONS, CO.burned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3471888–2026
BOULDER CREEK NEAR ORODELL, CO.burned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2961888–2026
MIDDLE BOULDER CREEK AT NEDERLAND, CO.burned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2601907–2026
ST. VRAIN CREEK AT MOUTH, NEAR PLATTEVILLE, CO.burned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2491927–2026
BOULDER CREEK AT MOUTH NEAR LONGMONT, COburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2481927–2026
SOUTH BOULDER CREEK NEAR ELDORADO SPRINGS, CO.catchment area, annual maximum river flow1041888–2026
NORTH ST. VRAIN CREEK NEAR ALLENS PARK, CO.catchment area, annual maximum river flow171926–2026
LEFT HAND CREEK NEAR BOULDER, CO.catchment area, annual maximum river flow171929–2026

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 — 10190005. 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
ST. VRAIN CREEK AT LYONS, 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
BOULDER CREEK NEAR ORODELL, 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
MIDDLE BOULDER CREEK AT NEDERLAND, 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
ST. VRAIN CREEK AT MOUTH, NEAR PLATTEVILLE, 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
BOULDER CREEK AT MOUTH NEAR LONGMONT, 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
SOUTH BOULDER CREEK NEAR ELDORADO SPRINGS, 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
NORTH ST. VRAIN CREEK NEAR ALLENS PARK, 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
LEFT HAND CREEK NEAR BOULDER, 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 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 spanned139yes, 20 or more
Values held4,164yes, 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), St. Vrain gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-st-vrain/

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 St. Vrain 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 confidence2013-09-12

Source: USGS — National Water Information System, USGS site 06724000, 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.