Agency Canal Tailwaste near Hardin MT Water Level
Live river level, flow, historical records and forecast for Agency Canal Tailwaste near Hardin MT in MT, United States, built from official government gauge data.
- Location MT, United States
- Watershed little bighorn
- Primary gauge 06293890 (USGS)
About Agency Canal Tailwaste near Hardin MT
Agency Canal Tailwaste near Hardin MT sits in the Little Bighorn watershed in Montana.
The watershed
This station is on a small reach in the Little Bighorn watershed, so the local signal matters more than the wider basin label. For people watching this water, the useful questions are how high it gets in late spring, how low it can fall in late summer, and how much room the channel needs between those two states.
The long record here is 40 years. That gives a useful span for seeing the same seasonal pattern repeat and for judging whether a current level is close to the upper or lower end of what this site usually sees.
What the numbers say
The record high is 6.13 ft (1.87 m), set in June 2018. The record low is 1.27 ft (0.39 m), set in July 2013.
The seasonal peak usually comes in June at 3.07 ft (0.94 m), and the seasonal low usually comes in March at 1.82 ft (0.55 m). That is a typical annual swing of 15 in (38.2 cm). For a dock, pump intake, or shallow crossing, that spread is the range the site has to accommodate from season to season.
The seasonal shape here fits a northern plains pattern: higher water in late spring, then lower water through the colder months and into summer. At this station, the record low arriving in July 2013 sits below the usual March minimum, so the record does not simply mirror the average seasonal cycle.
Reading the hero number
The hero number on this page is today’s reading compared with the median for this calendar day across the station record. That is more useful than raw elevation because it tells you whether today is typical for this date, not just how high the water sits on an arbitrary scale.
This station is published by the USGS, and the record spans more than 40 years.
How this page is built
Readings come from official government gauges and are rolled into daily records: the daily mean, high and low for every day on record. Each calendar day gets its own baseline from the full history, so the level you see is compared against what this specific date usually looks like rather than an annual average.
How Nibi Metrics works · Water stories
Nibi Metrics - live water levels, flow, and forecasts for lakes and rivers across Canada, the US and the UK
Real-time water levels, forecasts, and alerts for lakes and rivers across Canada, the US and the UK. Built on official government data.
Nibi Metrics tracks more than 13,000 gauged lakes and rivers across Canada, the United States and the United Kingdom, reading directly from official federal monitoring networks: the Water Survey of Canada, the United States Geological Survey, Quebec's provincial hydrometric network, and the Environment Agency for England. Every number on the platform is measured, not modelled - taken from a government gauge on the water itself and compared against that location's own historical record for this exact date.
What you can see for any monitored lake or river
The level right now, in feet or metres, updated as the source agency publishes new readings - for many stations that is every five to fifteen minutes. How today compares to typical: every location carries its own typical-for-this-date band built from its historical record, so a reading is never just a number - it is above, below, or near what this water usually does on this calendar day. Which way it is moving: a measured RISING, FALLING, or STEADY verdict computed from the gauge's own recent readings, with the rate of change - the difference between a flood ending and one beginning. What comes next: level forecasts up to 72 hours ahead, driven by the gauge's recent behaviour, upstream water, and quantitative precipitation forecasts, alongside live radar, lightning, and weather for the surrounding region.
Alerts that watch the water for you
Set a threshold on any location - a level, a distance above typical, or a rate of climb - and Nibi emails or notifies you the moment the gauge crosses it. Cottagers use it for spring freshet, anglers for river conditions, marinas and municipalities for operations. The scanning runs around the clock against the same measured data shown on every page.
Where Nibi comes from
Nibi means water in Anishinaabemowin. The platform began at a family cottage on Lake Muskoka, Ontario, where the spring melt floods the shoreline most years and the only forecast was standing on the dock, looking, and guessing. It grew into an independent, member-funded platform run by Muskoka Research Inc. - no investors, no data resale, and a privacy policy shorter than most cookie banners. The core data is free for everyone, forever; paid plans add automation like multi-location alerts, deep history, and reports.
Coverage
Nibi spans the continent: every Canadian province and territory with active federal gauges - from Vancouver Island rivers to the Muskoka lakes, prairie reservoirs, and Quebec's hydrometric network - and the United States from Maine to the Texas Hill Country, the Ohio Valley, and the Pacific Northwest. Coverage grows where the water news is: when a basin floods, its gauges join the platform with their full historical records attached. Many stations report every five to fifteen minutes; most report at least hourly; every page states exactly when its gauge last spoke.
Free forever, funded by members
The core promise is simple: the water data is free, for everyone, forever. Live levels, maps, radar, and recent history never sit behind a paywall. Paid plans fund the platform by adding automation - multi-location alerts, decades of history, longer forecasts, and PDF reports - so the people who need more carry the cost for everyone who just needs to check the lake before driving up. There are no investors and no advertising deals shaping what the data says.
Water Stories
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How every number is computed - About the platform
