Conditions
New River Headwaters LLCFlood & Environmental Monitoring

Live right now

The creek, as it is this minute.

S1 — Big Reed Island Creekour station
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Connecting to the station…
Federal gauges nearby USGS · provisional public data · updates every 15–60 min
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S1 creek level — the last 12 hours

Feet above normal at S1 on Big Reed Island Creek, straight from the station. Dashed lines are the station’s alert stages; stage 3, five feet above normal, is the top of the bank — above that line the creek is out of its banks. The words on each line say who gets an alert when the creek reaches it. Times Eastern. Updates every minute.

Right now

LIVE · ON-SITEConnecting to the weather station…
Weather station at S1 · Big Reed Island Creek
UV INDEX
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AIR TEMP
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Live from the station
UV: 1–2 Safe3–5 Moderate · sunscreen kids 6–7 High · SPF 30+ everyone8–10 Very high · limit midday 11+ Extreme
Sparklines: last 3 hours · the station reports about once a minute

Your creek rose ten feet while you slept.

Saturday night on Big Reed Island Creek, our station watched it happen — and raised its first alert at 2:04 AM, nearly five hours before the crest. You can put one of these on your own water.

A New River Headwaters sensor reaches out over Big Reed Island Creek on its mast arm, with brown floodwater filling the channel below and a log cabin on the far bank.

A New River Headwaters station watching Big Reed Island Creek come up to the top of its bank on August 2nd, 2026. The sensor is the white arm across the top of the frame, reaching out over the water.

10.2 ftabove normal at the crest, 6:54 AM Sunday
4 hrs 22 minfrom “move to higher ground” to the crest
4 ft / 40 minthe 2:05 AM surge — over 1½ ft in ten minutes
15 secbetween readings, all night, on battery power

The night, as the instruments saw it

Watch the flood happen.

Every frame below is real data off the creek — no model, no re-creation. The dashed lines are that station’s alert thresholds which are programmed by location. Each one stamps the time and level when the creek crossed it. The step at 2 AM is not rainfall — it is a dam failing fifteen miles upstream, which we were able to identify, size and time from the shape of the water alone.

Creek level in feet above normal, 8 PM Saturday to 7:30 AM Sunday. Times EDT.

10:30 PM — Heavy rain sets in, peaking near two inches an hour.
~12:20 AM — Fifteen river miles upstream, the earthen dam holding the lake at Olde Mill gives way. About 393 acre-feet — roughly 128 million gallons — starts down Stone Mountain Creek. Nobody downstream knows.
2:02 AM — The wave reaches the station. Flat water for twelve minutes, then two and a half feet in fifteen. Both sensors, laser and radar, see it together.
2:04 AM — 2.2 ft. The creek crosses stage 1 and the station raises its first advisory, then steps itself up to rapid measurement.
2:14 AM — 4.1 ft. Stage 2, ten minutes behind stage 1. The surge is moving faster than the ladder was built for.
2:31 AM — 5.1 ft. Stage 3: move to higher ground. Four hours and twenty minutes of rise still to come.
5:17 AM — 6.9 ft. Stage 4: evacuate low-lying areas along the creek.
6:54 AM — Crest at 10.2 feet above normal. It came in two waves: the water leveled off for two hours mid-flood, then climbed another four feet after the rain had stopped, as runoff drained off the mountains.

It was the same system you saw on the news — 6–7 inches of rain and washed-out roads in Ararat, flooding on Stillhouse Road in Crooked Oak, and a state of emergency in Mount Airy after the Ararat River jumped more than fifteen feet.

Days later a neighbour mentioned that the dam on the golf-course lake at Olde Mill had broken that night. Working backwards from our own record — the shape of the rise, the channel geometry, and how much water the creek must have carried to rise the way it did — we put the release at 373 acre-feet. The Army Corps of Engineers has that lake on record at 393. We put the failure between 12:06 and 12:32 AM; a passer-by's report reached police at 12:41 AM. The station never saw the dam. It only ever saw the water.

Check your creek

Would we have warned you?

This is the Big Reed Island Creek basin — 267 square miles of mountain water, mapped from elevation data. Teal creeks are watched today by our live station. Amber lights up when the planned sites go in. Gray water: nobody is watching it yet. Drop a pin anywhere on the map — or use your location, or type your address — to see your warning time.

…or just tap the map to drop a pin anywhere
watched now with planned sites unwatched live station (S1) planned site Carroll County Eastern Continental Divide USGS gauge (public data)

Warning times are travel-time estimates (a flood wave moving ~7 mph down the channel) from each station to your point — they will be calibrated against real events, starting with Aug 1–2. Your location is computed in your browser and never stored. Estimates are not a substitute for official warnings.

A station on your land

Host a station. Close the gap on your creek.

Every gray creek on that map is water nobody watches. If one of them runs through your land, you're the person who can change that — a station on your creek measures the water and publishes what it measures — to you, and to anyone downstream who subscribes. Here's what a monitored site is:

  • Creek-level sensing from above the water Nothing in the current to be torn out by debris. Reads as often as every 15 seconds when water is rising.
  • A full weather station Rainfall, temperature, wind, humidity, soil moisture — the conditions that tell you what's coming, not just what's here.
  • Solar powered, on its own radio No mains power, no Wi-Fi at the creek, nothing to plug in. It ran all through Saturday night's storm on its own.
  • Automatic alerts that escalate Text or push, from first advisory to evacuate, to you and anyone you add — family, neighbors, a farm manager.
  • All of your land's data, yours Every reading the station takes, live and going back. Your rainfall, your levels, your record.
I'm interested — contact me Or email us directly

No price list, no pressure — every site is different (terrain, creek access, radio line-of-sight), so it starts with a conversation. We'll look at your creek together and tell you honestly what it would take. Or just write to [email protected].

For everyone downstream

Flood alerts, free.

You don't need to own a station to get warned by one. When a monitored creek starts rising, we send escalating alerts by text or push notification to anyone signed up below it. Free, and they always will be.

Sign up for alerts

For counties & towns

Cover a whole watershed.

One station warns one creek. A network of them warns a county — and every station added upstream buys warning time for everyone below it. We work with emergency management on siting, coverage and alert routing to your dispatch.

Talk about coverage

For coverage, write to [email protected].

Where the water comes from

Every inch of rain has to travel.

Our station watches about 41 square miles of the Blue Ridge plateau — wooded ridges, steep hollows and pasture — drained by Big Reed Island Creek and branches like Pine Creek and Grassy Creek. Downstream, the whole creek gathers 267 square miles before it meets the New River at Claytor Lake.

The ground drinks first. Most rain soaks in. Thin mountain soil over rock holds only so much, and the wetter it already is, the sooner it fills and starts shedding water. A hard cloudburst can outrun even dry ground.
Two roads downhill. Water that can’t soak in runs off fast — down hollows, ditches and side branches. Water that does soak in creeps underground and seeps back out for days. That’s why the creek stays up long after a storm and keeps running through a dry spell.
Distance is time. That’s why a heavy downpour doesn’t show up on the gauge right away: the water has to make the trip first. Rain on the slopes near the station reaches it within the hour. Rain near the headwaters has close to 20 miles of winding channel to cover, so it arrives hours later. The higher the water, the faster it moves.
Snow and ice hold water back — with one exception. Snow doesn’t run off; it sits on the ground and melts out as the air warms, so it reaches the creek slowly. Frozen ground is the exception: rain can’t soak into it, so it runs off faster.
So the creek can keep rising after the rain stops. On August 2nd the last heavy rain fell around 1 AM, yet the creek crested at 6:54 AM — the far end of the basin was still draining.

Blue Ridge Twin, our flood model, follows these same steps hour by hour: how full the soil is, how much water runs off now and how much later, whether it fell as rain or snow and when that snow will melt, whether the ground is frozen, and how long each part of the basin takes to reach the station — then it checks itself against what the station actually reads.

Why this works

Mountain creeks rise faster than a regional forecast can resolve.

A flash flood on a small, steep creek is a local event. By the time it registers in a county-wide forecast, the water is already up. The warning that gets people out has to be local, automatic, and awake at two in the morning — measured on the creek itself, not interpolated from a gauge twenty miles downstream.

So we build the measurement. Every New River Headwaters station also feeds Blue Ridge Twin, the predictive flood model behind this — which is how a station on your creek turns into advance warning for your neighbors, and how their stations turn into advance warning for you. The model gets sharper with every site added to the basin.

Our first full deployment is going into the Rocky Broad valley above Bat Cave and Chimney Rock, North Carolina — one of the areas hit hardest by Hurricane Helene, where the creek gave almost no warning at all. Once our stations are on that water, the model projects up to 79 minutes of warning.

The technology

Built for water that rises in minutes.

Stream monitoring covers a lot of ground — staff gauges, pressure transducers, bubblers, acoustic and radar sensors, all of them good at the job they were built for. We designed ours around the hardest case we know of: a small mountain creek that can come up faster than anyone downstream expects. A station that keeps up with that is more than equal to a river, a larger stream, or any water that moves more slowly. Here's what that took.

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Two kinds of eyes on the water

Every station reads the creek two ways at once — laser (LiDAR) and millimeter-wave radar — from above the water, where debris can't tear it out. The two sensors cross-check every reading: fog blinds a laser, so the radar carries it; each covers the other's weaknesses. We're not aware of another creek-monitoring system that runs both. All of this technology was developed right here in Carroll County.

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It wakes up when the water moves

In quiet weather the station reads every 15 minutes to save power. The moment the creek starts rising, it steps itself up — all the way to a reading every 15 seconds — and starts issuing staged alerts on its own, no human in the loop. Federal gauges report every 15 to 60 minutes; in a flash flood that's the difference between a warning and a description of what already happened.

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Nothing to plug in, nothing to cut off

Solar powered with days of battery reserve, reporting over its own long-range radio network — no Wi-Fi at the creek, no phone line, no mains power to fail in a storm. On the night of Aug 1–2 it ran through the entire flood on its own battery, taking thousands of readings.

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A model that learns your creek

Blue Ridge Twin is our forecasting engine: a digital twin of the basin built from elevation data — every ridge, every tributary, all 267 square miles — fused with on-site readings of rainfall, humidity, temperature, dewpoint, soil moisture, water quality and creek level. It doesn't just report the water; it projects travel time from measured flow — an estimate, not a guarantee. Every real flood recalibrates it: Aug 1–2 is already in the model, tuning its travel times against what the creek actually did. It gets smarter with every storm and sharper with every station added.

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Every source, one picture

Our stations are the sharp local eyes, but the Twin drinks from everything: federal USGS river gauges, on-site weather stations measuring rainfall, soil moisture, temperature and wind — conditions that decide how fast a basin sheds water into its creeks. Where a federal gauge already watches a river, we use it; where nobody watches, we build.

✓

Proven on a real flood, first try

This isn't a lab claim. On its first major flood the system detected the rise at 2:02 AM, escalated through four alert stages on schedule, tracked a 4-foot surge in 40 minutes, and caught a 10.2-foot crest at 6:54 AM — on a creek no federal gauge watches. The nearest federal gauges sit miles away on neighboring forks; this one was ours alone. Scroll up and watch the recording. That's the product.

Host a stationCheck your creek

A safety note: never drive or walk into floodwater. Two feet of moving water can carry a vehicle, and most flood deaths happen in cars. If a creek near you is rising, don't wait to see how high it gets — turn around and go up.

New River Headwaters LLC · flood & environmental monitoring · predictive modeling by Blue Ridge Twin
All data on this page was recorded by our Big Reed Island Creek station, Carroll County, Virginia, August 1–2, 2026.