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Cache La Poudre River

Division 1 · Water District 3 · As of 2026-08-26 10:58 MDT
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Cache La Poudre River on the ground — the ditches, wells, reservoirs and gages of Water District 3 · clicktap anything for its record

Snowpack — no snow on the ground at 4 SNOTEL sites — normal for the date; the snow year begins in October and typically peaks around April 17. Runoff outlook — Cache La Poudre R at Canyon Mouth: even odds of at least 87 kAF over 06-01 to 09-30 — 51% 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
Black Mountain8940 0.00.0 April 17 (12.5 in)
Deadman Hill10240 0.00.0 May 4 (21.8 in)
Hourglass Lake9380 0.20.0 April 19 (13.0 in)
Long Draw Resv9980 0.10.0 April 27 (18.3 in)

Cache La Poudre R at Canyon Mouth — 06-01 to 09-30 volume, thousand acre-feet (chance the volume is AT LEAST this):

90%70%50%30%10%Normal
68798796110 169

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.

Topology cross-check: 10 parent disagreements, 20 sizable streams not on this network (vs DWR's route framework — under review)

This flow network was built mechanically; DWR's Source Water Route Framework disagrees with it in the places below. Each row is a question a human reviewer has not yet answered — not an error verdict. Checked 26 streams, 16 agree. Know this water? Tell us →

StreamThis site routes it toDWR routes it to
Sheep Creek the mainstem North Fork Cache La Poudre River
Fish Creek the mainstem Dale Creek
Trail Creek the mainstem North Fork Cache La Poudre River
Rabbit Creek the mainstem North Fork Cache La Poudre River
Lone Pine Creek the mainstem North Fork Cache La Poudre River
South Lone Pine Creek the mainstem Lone Pine Creek
North Lone Pine Creek the mainstem Lone Pine Creek
Manhattan Creek the mainstem Elkhorn Creek

Sizable streams DWR maps here that this network does not carry:

Coalbank Creek (24 mi) · Fossil Creek (16 mi) · Owl Creek (11 mi) · Bennett Creek (11 mi) · Joe Wright Creek (11 mi) · The Slough (10 mi) · Spring Creek (8 mi) · Lewstone Creek (8 mi)

Groundwater

11,451 water-level measurements across 1026 monitored well(s) — 912 alluvial, 4 bedrock — plus 4 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 49 well(s) with enough record for a trend test: 9 declining, 3 rising.

Fastest-declining wellsSettingft / decadeSpanp
83-1 alluvial -8.03 17 yr 0.0022
110-3 alluvial -2.03 17 yr 0.0049
SB00906834ABB alluvial -1.94 20 yr 0.004
SB00806827CBB2 alluvial -0.83 30 yr 0.0165
SB00706614AAB alluvial -0.82 55 yr 0.0413
LSP-062 06N6712BBB alluvial -0.66 85 yr 0.0003
SB00606812AAA alluvial -0.52 17 yr 0.0001
LSP-061 06N6517BBC alluvial -0.42 93 yr 0.0419

Stream corridors — the surface connection

Where a reach's gain or loss has shifted, the wells within two miles of its anchoring gage and what their water table did over the same era.

How the corridor is assembled

For each reach whose gain/loss has shifted (Trends tab): the wells within 2 miles of its anchoring gage, their pooled water-table history over the same era, and an advisory Glover screen of lagged stream depletion from nearby metered pumping. v1 proximity = distance to the reach's anchoring gage; segment-based reach join is a flagged upgrade.

LARIMER AND WELD IRRIGATION COMPANY @ 30 FT PARSHALL FLUME: 19 alluvial well(s) nearby

LARIMER COUNTY #2 @ 12 FT PARSHALL FLUME: 7 alluvial well(s) nearby

CACHE LA POUDRE RIVER BELOW NEW CACHE: 30 alluvial well(s) nearby; pooled water table -0.4 ft (1941–1992, no_trend, p=0.2946). Glover screen: 0.4 cfs of nearby metered alluvial pumping → est. lagged depletion 0.2–0.4 cfs (uncalibrated T/S ranges; flagged for SPDSS calibration, AWAS cross-check, and expert review — DWR's AWAS is the authority).

CACHE LA POUDRE RIVER AT FORT COLLINS, CO: 15 alluvial well(s) nearby

CANAL # 3 NEAR GREELEY: 30 alluvial well(s) nearby; pooled water table +0.1 ft (1941–1992, no_trend, p=0.6315). Glover screen: 0.1 cfs of nearby metered alluvial pumping → est. lagged depletion 0.1–0.1 cfs (uncalibrated T/S ranges; flagged for SPDSS calibration, AWAS cross-check, and expert review — DWR's AWAS is the authority).

LITTLE CACHE LA POUDRE DITCH: 10 alluvial well(s) nearby

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.