The monitoring network within this area

Hydrionis holds 583 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
583
Values held
1912–2026
Record spans
Gauges within the Lamoille River huc8 subbasin
2 monitoring points, positioned as the publisher records them.
Gauges within the Lamoille River huc8 subbasinLAMOILLE RIVER AT JOHNSON, VT, LAMOILLE RIVER AT EAST GEORGIA, VTLAMOILLE RIVER AT JOHNSON, VTLAMOILLE RIVER AT EAST GEORGIA, VT

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 LAMOILLE RIVER AT JOHNSON, VT
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1912–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at LAMOILLE RIVER AT JOHNSON, VTLargest measured flow of each year at LAMOILLE RIVER AT JOHNSON, VT: LAMOILLE RIVER AT JOHNSON, VT in m³/s, from 1912 to 2025.Hurricane Katrina water and sanitation collapse0200400600800m³/s19121938195119651977199020032017

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
PeriodLAMOILLE RIVER AT JOHNSON, VT (m³/s)
1912345
1913241
1929131
1930176
1931195
1932192
1933255
1934234
1935148
1936368
1937219
1938258
1939212
1940323
1941157
1942300
1943190
1945174
1946152
1947254
1948174
1950201
1951225
1952257
1953195
1954194
1955171
1956178
1957136
1959136
1961142
1962207
1964155
196578.2
1966139
1967167
1968166
1969261
1970206
1971196
1972248
1973408
1975232
1976323
1977208
1979202
1981121
1982306
1983124
1984368
198599.7
1986229
1987246
1988127
1989243
1990209
1992166
1993151
1994280
1995538
1996270
1997365
1998215
1999158
2000257
2002289
2003206
2005219
2006241
2007214
2008252
2009139
2011391
2013175
2014263
2015199
2016217
2017201
2018223
2019263
2021143
2023697
2024473
2025212

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 held1912–2025
Completeness73.7% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 16 separate periods inside 1912–2025 hold no value. The longest runs from 1914 to 1928 — 15 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1912 and is not continuous from it: 114 years separate the first value from the last, and 74% 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 LAMOILLE RIVER AT JOHNSON, VT, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1929–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above LAMOILLE RIVER AT JOHNSON, VT, as a depthWater leaving the catchment above LAMOILLE RIVER AT JOHNSON, VT, as a depth: LAMOILLE RIVER AT JOHNSON, VT in mm, from 1929 to 2025.Hurricane Katrina water and sanitation collapse2505007501,000mm19291942195519681981199420072020

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
PeriodLAMOILLE RIVER AT JOHNSON, VT (mm)
1929610
1930502
1931453
1932593
1933505
1934496
1935587
1936769
1937629
1938613
1939581
1940572
1941389
1942608
1943709
1944478
1945816
1946583
1947652
1948520
1949439
1950506
1951609
1952630
1953513
1954696
1955604
1956541
1957535
1958636
1959563
1960533
1961509
1962620
1963485
1964404
1965434
1966516
1967546
1968502
1969729
1970516
1971613
1972676
19731,006
1974735
1975560
1976865
1977696
1978626
1979658
1980472
1981627
1982606
1983789
1984635
1985505
1986627
1987491
1988416
1989576
1990982
1991570
1992481
1993549
1994616
1995576
1996802
1997642
1998778
1999528
2000721
2001446
2002717
2003705
2004677
2005756
2006913
2007747
2008862
2009664
2010693
2011962
2012515
2013692
2014623
2015630
2016561
2017721
2018657
2019835
2020590
2021426
2022542
2023958
2024743
2025558

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 held1929–2025
Completeness100.0% of the periods in that span are held.
ContinuityContinuous: every year from 1929 to 2025 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 Lamoille River and what each holds
GaugeMeasuresValuesRecord
LAMOILLE RIVER AT JOHNSON, VTcatchment area, annual maximum river flow, mean river flow, mean river flow, water year2941912–2026
LAMOILLE RIVER AT EAST GEORGIA, VTcatchment area, annual maximum river flow, mean river flow, mean river flow, water year2891929–2026

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 — 04300105. 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
LAMOILLE RIVER AT JOHNSON, VTStated 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
LAMOILLE RIVER AT EAST GEORGIA, VTStated 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 2 of them, which makes it a profile, not indexed.

Information-gain signals held for this water body
SignalHeldCounts
Gauges holding a real record2no
Years spanned115yes, 20 or more
Values held583no
Distinct measurements4yes, 2 or more
Publishers measuring it1no
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), Lamoille River gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-lamoille-river/

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 Lamoille River 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 confidence2025-03-17

Source: USGS — National Water Information System, USGS site 04292000, 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.