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Keystone Gulch near Dillon

River gage · KEYGUDCO · USGS 09047700 · Division 5 · Water District 36 · Summit County

Live gage at DWR ↗ · USGS monitoring location ↗ · Download daily record (CSV)

Source DWR administrative record · verify at DWR station ↗ Source Independent agency measurement · verify at USGS ↗ Source Our computation, no independent reference · computed here from the screened record

Two different numbers, deliberately: Flowing now is raw 15-minute telemetry, provisional and unreviewed. Latest cached reading is the end of the verified daily record. They are never merged, and the verified series is the one the trend is computed on.

Extended record — reconstructed, not measured

This gage's own record starts in 1957. A retired gage nearby, TENMILE CREEK AT DILLON, CO., ran earlier and overlapped it, so its measurements can be translated onto this gage's scale to extend the picture back roughly 37.0 years. The result before 1957 is a reconstruction. It is not what this gage measured, because this gage did not exist.

Donor gage TENMILE CREEK AT DILLON, CO., 5.9 km away
Overlap used to fit 1,308 days, 1957-10-01 to 1961-04-30
Agreement (held out) r² 0.937
Typical error (held out) 11.6%, bias 7.6%
Grade fair
How this was built, and what it cannot tell you
  • The two gages had to overlap. Without shared days there is nothing to measure the relationship against, and no extension is offered at all — that rule rejected the overwhelming majority of candidate pairs.
  • The relationship is fitted in log space, because the ratio between two gages changes with flow. On Clear Creek the downstream gage reads 95% of the upstream one at low flow but 88% at high flow, because ditches in between take more when there is more to take. A single scale factor would get both ends wrong.
  • It is scored out of sample: fitted on half the overlap, tested on the other half. The numbers above are from the half it never saw.
  • Reconstruction never replaces a real observation. Every day in the series is labelled measured or reconstructed, and the overlap itself stays measured.
  • The trends published on this site still use the measured record only. This extension is offered for reading the longer shape, not as an input to the statistics.
  • DWR's published record is the authority. A reconstruction is an estimate of what this location would have read, not a measurement of it.

What the longer record says

Record usedYearsTrendpChange / decade
Measured only (what the site publishes) 69 1958–2026 no trend 0.97106 0.0 cfs
TENDILCO alone (measured, no reconstruction) 40 1911–1960 no trend 0.12124 -5.594 cfs
Extended (with reconstruction) 106 1911–2026 no trend 0.0814 -0.082 cfs

Both records reach the same conclusion, over 37 more years.

Extending changes the conclusion for roughly half the gages that have a reconstruction — which is why both rows are here and neither replaces the other. Every trend published elsewhere on this site uses the measured record only.

The record

Period of record
1957-10-01 → 2026-09-29
Daily values
25,179
Flowing now
1.57 cfs 2026-10-19 20:15, 2.4 h ago
Latest cached reading
1.6 cfs (2026-09-29)
Trend — measured record
no trend, 0.06 cfs/decade (0.9% of median)

Readings come from the weekly-refreshed cache, never fetched live — the date beside the value says exactly how fresh it is. The live gage is one click up.

Annual flow & trend

Chart: annual mean flow at Keystone Gulch near Dillon, water years 1957 to 2026. The measured record is no trend at 0.06 cubic feet per second per decade. Extended backwards with a reconstruction from TENDILCO, the 106-year record is no trend (p equals 0.0814). The two records are compared in the table above. The underlying yearly values are available as a CSV download linked at the top of this page.

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Where it sits

Location as DWR records it (5).

Provenance

DWR station abbreviation KEYGUDCO; recorded station name “KEYSTONE GULCH NEAR DILLON, CO.”; operated by USGS. Daily flows from the DWR HydroBase snapshot plus CDSS REST updates, refreshed on the weekly cycle. Trend statistics are Mann-Kendall (Hamed-Rao corrected) with Sen's slope in native cfs, the same numbers as the basin Trends tab.