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Bear Creek

Division 1 · Water District 9 · As of 2026-08-18 03:02 MDT
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Bear Creek on the ground — the ditches, wells, reservoirs and gages of Water District 9 · clicktap anything for its record

Snowpack — no snow on the ground at 1 SNOTEL site — normal for the date; the snow year begins in October and typically peaks around April 29. Runoff outlook — Bear Ck ab Evergreen: even odds of at least 7 kAF over 06-01 to 09-30 — 66% of a normal season, per NRCS, issued 2026-06-01 — the season’s final; new forecasts begin in January. Full snow & runoff picture — charts, forecast history and how the forecasts have verified →

Sites, exceedance bands and sources
SNOTEL siteElev (ft)SWE (in)Median (in)% of medianTypical peak
Echo Lake10660 0.00.0 April 29 (9.0 in)

Bear Ck ab Evergreen — 06-01 to 09-30 volume, thousand acre-feet (chance the volume is AT LEAST this):

90%70%50%30%10%Normal
467912 10

Snow-water equivalent and medians (1991–2020) from NRCS SNOTEL; seasonal volume forecasts from the NRCS National Water and Climate Center. Sites and forecast points are assigned to the district whose boundary contains them — snowpack that feeds this district can also sit in a neighboring headwater district. Toggle the Snow chip on the map above to see the sites.

Groundwater

31,450 water-level measurements across 332 monitored well(s) — 77 alluvial, 52 bedrock — plus 0 administered well(s) reporting metered pumping.

What is being counted

Observation wells and pumping wells are different populations and are never conflated: water levels come from monitored observation wells, and metered pumping comes from administered wells reporting through diversion records. Click any well to chart its own record.

Well map

3D aquifer x-ray

Every aquifer unit as its own head surface, animated through time.

How the surfaces are built, and what they are not

Alluvial water table on top, Denver Basin members (Dawson, Denver, Arapahoe, Laramie–Fox Hills) stacked beneath where measured, interpolated from measured water levels. Units are never mixed; a surface exists only inside its own unit's well coverage, with no extrapolation; thin epochs are suppressed and say why. Vertical scale is exaggerated for readability and z is head elevation in feet. These are measured heads, not a calibrated groundwater model.

Water-table trends

Of 14 well(s) with enough record for a trend test: 5 declining, 3 rising.

Fastest-declining wellsSettingft / decadeSpanp
WP243773 unknown -151.77 11 yr 0.0049
WP233156 unknown -15.79 21 yr 0.0075
SC00607102BBD alluvial -8.36 10 yr 0.0127
WP41198 alluvial -1.0 21 yr 0.0321
WP139298 unknown -0.72 21 yr 0.0408

Wells labeled by administrative world before anything else is said about them: tributary alluvium participates in the priority system; designated-basin and Denver Basin bedrock aquifers are governed differently and are excluded from stream-connection reasoning. Read bedrock declines differently too: deep bedrock aquifers recharge negligibly on human timescales, so a falling bedrock level is storage mining — effectively permanent — not a drought response that a wet year undoes. All screens advisory.