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Nibi Metrics

Real-time water levels, forecasts, and alerts for lakes and rivers across Canada and the US. Built on official government data.

Nibi Metrics turns raw gauge readings from official hydrometric networks into something a person standing on a dock can actually use: is the water high or low for today, which way is it moving, and how unusual is this? This page explains where every number on the platform comes from and what we do to it along the way.

Water Stories

The flood of record that was overtaken

For five years, spring 2019 was the mark every Lake Muskoka decision answered to. In April 2026 the lake went two centimeters higher - and the official books have not caught up yet.

Why the Assiniboine floods every spring

Inside the freshet cycle that puts Manitoba shorelines at risk each year - and why 2026 broke the script.

How snowpack becomes summer water

The science of snow water equivalent and why it drives the season ahead.

Reading a staff gauge like a hydrologist

What the numbers on the measuring stick actually tell you.

Flash Flood Alley: how Texas rivers rise in hours

Why Central and South Texas rivers go from gravel beds to fifty-year records in an afternoon - including July 2026 on the Nueces.

What a "100-year flood" actually means

One percent, every year, forever - unwrapping hydrology's most misunderstood phrase, and how it differs from our own percentiles.

Credit River Erin Branch at Hillsburgh Water Level

Live river level, flow, historical records and forecast for Credit River Erin Branch at Hillsburgh in Canada, ON, Canada, built from official government gauge data.

About Credit River Erin Branch at Hillsburgh

Credit River Erin Branch - A vital watercourse in Ontario's Credit watershed.

The Credit River Erin Branch at Hillsburgh flows through Ontario's rich landscape, serving as an important tributary of the larger Credit River system. Spanning a catchment area of approximately 12.8 square kilometers, this section of the river is integral not only for the local ecosystem but also for the communities that rely on its waters.

The watershed context

The Credit River Erin Branch is part of the Credit - 16 Mile watershed, which encompasses a network of rivers and creeks. This tributary connects to other regional peers, including Cooksville Creek near Cooksville and the Credit River near Orangeville. The seasonal dynamics of the watershed reflect Ontario's snowmelt-driven hydrology, with significant flows typically observed during the spring freshet from late April through May, followed by a natural drawdown during the summer months. Early winter typically sees a gradual decline in water levels as ice begins to form.

Why the data matters here

Monitoring the river's discharge is essential for understanding its health and its role in the broader watershed. The current readings help water resource managers and local communities respond to changing conditions, especially during peak flows in the spring and low flows in summer and winter months. Today’s data for the Credit River Erin Branch at Hillsburgh is crucial; it contributes to our understanding of how this stream is performing compared to historical averages. With a record spanning over 20 years, this information, provided by the Water Survey of Canada, allows for informed decision-making regarding land use and conservation efforts, ensuring the sustainability of this important waterway.

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