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Disappointment Creek Basin

Division 7 · Water District 69
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Disappointment Creek Basin on the ground — the ditches, wells, reservoirs and gages of Water District 69 · clicktap anything for its record

Browse this district’s ditches, gages, reservoirs, wells and springs as a list.

97% of normal flow, week of 1986-09-22
17 calls active on it right now

The Disappointment Creek is near normal for late September -- 97% of normal flow, its 2nd-wettest such week in 30 years of record. 17 calls stand against it right now; the most senior right calling dates to 1876.

Full diagnostic snapshot pending — this district's weekly-style report (system status, active calls, hydrographs, anomaly flags) is produced by the nightly rotation and appears here after its first run. The tabs above are live now.

Groundwater

6 water-level measurements across 3 monitored well(s) — 3 alluvial, 0 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 0 well(s) with enough record for a trend test: 0 declining, 0 rising.

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.

Topology cross-check: 0 parent disagreements, 8 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 1 streams, 1 agree. Know this water? Tell us →

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

Spring Creek (17 mi) · Ryman Creek (12 mi) · Hunt Creek (8 mi) · McKinney Draw (7 mi) · Pine Arroyo (6 mi) · Rabbit Creek (6 mi) · Bear Creek (5 mi) · Dugout Wash (4 mi)

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