The monitoring network within this area

Hydrionis holds 317 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
317
Values held
1928–2026
Record spans
Gauges within the Rush-Vermillion huc8 subbasin
2 monitoring points, positioned as the publisher records them.
Gauges within the Rush-Vermillion huc8 subbasinMISSISSIPPI RIVER AT PRESCOTT, WI, SOUTH BRANCH VERMILLION RIVER AT EMPIRE, MNMISSISSIPPI RIVER AT PRESCOTT, WISOUTH BRANCH VERMILLION RIVER AT EMPIRE, MN

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 MISSISSIPPI RIVER AT PRESCOTT, WI
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1929–2024.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at MISSISSIPPI RIVER AT PRESCOTT, WILargest measured flow of each year at MISSISSIPPI RIVER AT PRESCOTT, WI: MISSISSIPPI RIVER AT PRESCOTT, WI in m³/s, from 1929 to 2024.Hurricane Katrina water and sanitation collapse02,0004,0006,0008,000m³/s19291940195119621973198520032014

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
PeriodMISSISSIPPI RIVER AT PRESCOTT, WI (m³/s)
19291,405
1930954
1931634
1932858
1933561
1934425
19351,025
19361,487
1937878
19381,719
19391,841
1940957
19411,914
19421,201
19432,271
19442,398
19452,478
19461,855
19471,787
19481,787
19491,523
19502,860
19513,625
19524,389
19531,917
19542,345
19551,280
19561,775
19572,662
1958804
19591,000
19601,529
19611,311
19622,161
19631,172
19641,631
19656,456
19662,118
19672,486
19681,138
19695,635
19701,555
19712,350
19722,704
19732,217
19741,846
19753,171
19762,061
1977739
19781,852
19792,832
19801,220
19822,455
19832,384
19842,574
19852,078
19933,681
19942,064
19951,841
19962,339
19974,559
19981,994
19992,053
2000906
20015,295
20021,926
20031,676
20041,657
20051,603
20062,061
20071,934
20081,900
20092,144
20102,888
20113,540
20122,750
20132,379
20143,710
20151,303
20162,325
20172,076
20182,917
20194,163
20203,115
20211,651
20222,611
20234,021
20240

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 held1929–2024
Completeness91.7% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 2 separate periods inside 1929–2024 hold no value. The longest runs from 1986 to 1992 — 7 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1929 and is not continuous from it: 96 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 MISSISSIPPI RIVER AT PRESCOTT, WI, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1929–2023.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above MISSISSIPPI RIVER AT PRESCOTT, WI, as a depthWater leaving the catchment above MISSISSIPPI RIVER AT PRESCOTT, WI, as a depth: MISSISSIPPI RIVER AT PRESCOTT, WI in mm, from 1929 to 2023.Hurricane Katrina water and sanitation collapse0100200300400mm19291941195319651977198920012013

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
PeriodMISSISSIPPI RIVER AT PRESCOTT, WI (mm)
192993.0
193064.0
193147.0
193255.0
193347.0
193435.0
193563.0
193676.0
193771.0
1938114
193994.0
194065.0
1941138
1942125
1943172
1944193
1945162
1946154
1947141
1948108
194994.0
1950147
1951202
1952209
1953193
1954151
1955102
1956106
1957155
195882.0
195970.0
1960110
196176.0
1962154
196398.0
196497.0
1965240
1966169
1967130
1968151
1969182
1970117
1971170
1972213
1973162
1974135
1975173
197680.0
197787.0
1978154
1979206
198096.0
1981118
1982183
1983213
1984235
1985211
1986309
198795.0
198865.0
198988.0
1990109
1991196
1992170
1993282
1994195
1995215
1996184
1997215
1998157
1999174
2000108
2001240
2002182
2003131
2004141
2005181
2006139
2007135
2008140
2009132
2010238
2011284
2012143
2013160
2014249
2015162
2016250
2017240
2018266
2019378
2020216
2021118
2022165
2023164

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 held1929–2023
Completeness100.0% of the periods in that span are held.
ContinuityContinuous: every year from 1929 to 2023 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

Every gauge Hydrionis holds within this area

Gauges within the Rush-Vermillion and what each holds
GaugeMeasuresValuesRecord
MISSISSIPPI RIVER AT PRESCOTT, WIburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3161928–2026
SOUTH BRANCH VERMILLION RIVER AT EMPIRE, MNcatchment area12026–2026

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 — 07040001. 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
MISSISSIPPI RIVER AT PRESCOTT, WIStated 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 BRANCH VERMILLION RIVER AT EMPIRE, MNStated 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 3 of them, which makes it a full profile.

Information-gain signals held for this water body
SignalHeldCounts
Gauges holding a real record1no
Years spanned99yes, 20 or more
Values held317no
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), Rush-Vermillion gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-rush-vermillion/

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 Rush-Vermillion 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 confidence2024-06-30

Source: USGS — National Water Information System, USGS site 05344500, 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.