Upper South Platte
Upper South Platte on the ground — the ditches, wells, reservoirs and gages of Water District 23 · clicktap anything for its record
The well-permit cells in view, as a table
Each row is one ~1-mile cell (0.02°) with the permits the file spots inside it, split into water-supply permits and monitoring holes (DWR’s two monitoring categories: drilled to look at the water, not to pump it). These are permits, not wells: a permit is a piece of paper, and the file does not say which were drilled. Spotting is the file’s own, about a mile at best, which is why the cells are no finer.
| Lat | Lon | Water-supply permits | Monitoring holes |
|---|
Browse this district’s ditches, gages, reservoirs, wells and springs as a list.
The South Platte River is well below normal for late September -- 48% of normal flow. 1 call stands against it right now; the most senior right calling dates to 1863. DWR's statements do not settle whether 7 more calls reach it.
Schematic
Historical
Evolution of the network
Trends
Source Our computation, no independent reference · computed here from the screened DWR record Source Our computation, no independent reference · no independent reference; see /methods
This year, in context
In the weeks around 2026-09-27 (the newest reading on file), flows at the 24 ranked gages are running at a median 60% of their own long-term norm for this window — 20 below a typical year, 4 at or above. Driest relative to its record: FOUR MILE CREEK AT BEERY DITCH, ranking 1st lowest of 6 years.
How this comparison is made
Each gage's mean flow over the 3 days either side of 2026-09-27, compared with the same window in every year of its own record — so a gage is only ever measured against itself, and gages with no record in the window are counted out rather than guessed.
Gage flow trend & changepoints
What counts as a trend here
Computed 2026-10-11 19:43 from 50 gage(s) with cached period-of-record data. The series is each gage's annual mean flow in cfsCubic feet per second, a rate of flow. One cfs running for a day is about 2 acre-feet. (years with ≥300 days of record). Mann-Kendall (trend, with the Hamed–Rao correction for serial correlation — persistence can otherwise fake significance) and Pettitt (changepoint) both require at least 8 years spanning at least 10 years of record. A gage below that reports no signal — which is not the same as “no change.” The %-per-decade figure is the same Sen slope divided by the gage's median annual flow, for comparing across streams of very different size; it is omitted for near-ephemeral channels where the median is too small to divide by honestly.
Of the 50 gages with enough record, 0 are trending down and 3 up, and 4 carry a detected shift. The clearest is South Platte River near Lake George, its annual mean flow changing +6.88 cfs per decade (+7.3% of its median annual flow) over 96 years (p<0.0001). The other 46 show no clear signal either way.
Drought history, cost, and the four-century context moved to the Drought tab.
| Gage | Trend | Change / decade cfs · % of median annual flow | Significance | Years | Changepoint |
|---|---|---|---|---|---|
|
▸
South Platte River near Lake George PLAGEOCO |
↑ increasing | +6.88 cfs +7.3% | p<0.001 | 96 | ~1983 |
|
▸
South Platte River above Elevenmile Reservoir PLAHARCO |
↑ increasing | +6.96 cfs +7.3% | p<0.001 | 87 | ~1983 |
|
▸
Aurora Homestake Pipeline to Spinney Mountain Reservoir (Relief Valve) HOMSPRCO |
↑ increasing | +0.38 cfs | p=0.002 | 11 | ~2017 |
|
▸
Boreas Pass Ditch at Boreas Pass BORDITCO |
no clear trend | -0.00 cfs | p=0.642 | 84 | ~1962 |
46 other gage(s) show no significant trend or changepoint (not shown).
How the measurement network itself changed
This basin was not always measured the way it is today — the API-era record is dense and recent, the early record sparse. 32 gage(s) and 99 structure(s) report in 2026, but structure reporting only reached half its modern level around ~1950. Every historical claim below is checked against this: long-term shifts that co-move with the growth of the network carry an explicit measurement-evolution caution, and abandonment screens whose idleness begins before the modern reporting era are flagged †.
| Decade | Gages with data (median yr) | Structures reporting (median yr) |
|---|---|---|
| 1910s | 2 | 0 |
| 1920s | 1 | 0 |
| 1930s | 2 | 0 |
| 1940s | 2 | 0 |
| 1950s | 4 | 132 |
| 1960s | 4 | 32 |
| 1970s | 5 | 131 |
| 1980s | 10 | 167 |
| 1990s | 25 | 141 |
| 2000s | 28 | 114 |
| 2010s | 31 | 96 |
| 2020s | 32 | 85 |
Mass-balance (network closure) trend
Structure divrec-history backfill coverage as of the last check: 3% of 3827 schematic-relevant structures. 0 year(s) clear the 30% coverage gate so far -- the trend activates automatically once qualifying years span a full decade. No action needed; the nightly backfill keeps extending the record.
Groundwater now has its own tab: 160 monitored well(s), water-table trends, stream corridors, and the advisory depletion screen.
Reservoirs now has its own tab: 44 reservoir(s), end-of-year storage back to 1974, click-to-chart histories.
Cross-gage pattern fingerprint
Over the 51-year window with full coverage (1976–2026), the dominant shared pattern across 3 gage(s) explains 70% of year-to-year variance (almost certainly a basin-wide climate/snowpack driver).
All gages in this window move with the shared pattern -- no localized outlier.
Structures most implicated by reconciliation (as of 2026-09-01)
Which structures' data absorbed the most correction when the current mass-balance snapshot was reconciled -- see the Historical tab for the full picture on any date.
- RENSHAW SPRING 1 (return): +2.5 cfs (25% of that reach's correction)
- RENSHAW SPRING 2 (return): +2.5 cfs (25% of that reach's correction)
- EAST LAMB MTN SPRING (return): +2.5 cfs (25% of that reach's correction)
- UNION PLACER SPRING (return): +2.5 cfs (25% of that reach's correction)
- DIVINE HILL DITCH (diversion): +2.4 cfs (4% of that reach's correction)
- SPINNEY RANCH CLAIM (diversion): +2.4 cfs (4% of that reach's correction)
- HEISLER RANCH SPRING 2 (return): +2.4 cfs (4% of that reach's correction)
- FOSTER DITCH (diversion): +2.4 cfs (4% of that reach's correction)
- SPINNEY MTN RESERVOIR (diversion): +2.4 cfs (4% of that reach's correction)
- SODA POP SPRING (return): +2.4 cfs (4% of that reach's correction)
Data provenance & quality
Where these numbers come from and how far they can be trusted. Grade C (3/6 points) — the components below are the finding; the letter alone is not. Sources: DWR HydroBase snapshot HydroBase_CO_20260928 (imported 2026-10-04) for history, plus the CDSS REST API for current conditions.
| Check | State | What was measured |
|---|---|---|
| gage freshness | stale | newest gage reading is 14 day(s) old (target 7) |
| diversion record | expected-lag | newest diversion record is 346 day(s) old (DWR publishes ~1 year in arrears) |
| structure coverage | sparse | 3% of schematic structures have data |
50 gage(s) / 366,692 daily values (1911-03-01–2026-09-27); 493 structure(s) with diversion records; 2640 with decreed rights. Methodology has not yet had independent expert review — treat every figure as an advisory screen, not an administrative or legal conclusion.
Groundwater
Source DWR administrative record · verify at DWR groundwater wells ↗ Source DWR administrative record · verify at DWR well permits ↗
1,926 water-level measurements across 160 monitored well(s) — 73 alluvial, 4 bedrock — plus 3 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.
64% are constructed wells; 13% tie to a decreed structure. A permit is permission to drill, not a water right; most here are exempt household wells. More in three things called “well”, or turn on the Well permits chip on the map above to see where they sit.
Permits issued here, by year
15,392 located water-supply permits with an issue date, 1908 to 2026; half of them had been issued by 1998, and the busiest year was 1997 with 596. The district’s 821 monitoring holes are counted apart: they are drilled to look, not to pump. A permit is not a well, and the year is the date the paper was issued, not a drilling date. The 18,045 above counts every permit on file here; 1,832 of them have no usable location or no issue date and are not in this chart.
water-supply permits issued that year monitoring holes, when shown 2 issued before 1950 are in the table, not the bars
The counts by year, as a table
| Year | Issued | Monitoring holes | Water-supply | Issued through that year |
|---|---|---|---|---|
| 1908 | 2 | 0 | 2 | 2 |
| 1953 | 2 | 0 | 2 | 4 |
| 1954 | 9 | 0 | 9 | 13 |
| 1955 | 29 | 0 | 29 | 42 |
| 1956 | 19 | 0 | 19 | 61 |
| 1957 | 8 | 0 | 8 | 69 |
| 1958 | 2 | 0 | 2 | 71 |
| 1959 | 8 | 0 | 8 | 79 |
| 1960 | 15 | 0 | 15 | 94 |
| 1961 | 12 | 0 | 12 | 106 |
| 1962 | 16 | 0 | 16 | 122 |
| 1963 | 19 | 0 | 19 | 141 |
| 1964 | 22 | 0 | 22 | 163 |
| 1965 | 34 | 0 | 34 | 197 |
| 1966 | 30 | 0 | 30 | 227 |
| 1967 | 18 | 0 | 18 | 245 |
| 1968 | 22 | 0 | 22 | 267 |
| 1969 | 58 | 0 | 58 | 325 |
| 1970 | 54 | 0 | 54 | 379 |
| 1971 | 80 | 0 | 80 | 459 |
| 1972 | 449 | 0 | 449 | 908 |
| 1973 | 282 | 1 | 281 | 1,190 |
| 1974 | 168 | 0 | 168 | 1,358 |
| 1975 | 127 | 0 | 127 | 1,485 |
| 1976 | 104 | 0 | 104 | 1,589 |
| 1977 | 165 | 0 | 165 | 1,754 |
| 1978 | 268 | 0 | 268 | 2,022 |
| 1979 | 372 | 0 | 372 | 2,394 |
| 1980 | 285 | 1 | 284 | 2,679 |
| 1981 | 293 | 0 | 293 | 2,972 |
| 1982 | 354 | 2 | 352 | 3,326 |
| 1983 | 274 | 3 | 271 | 3,600 |
| 1984 | 257 | 0 | 257 | 3,857 |
| 1985 | 213 | 0 | 213 | 4,070 |
| 1986 | 225 | 2 | 223 | 4,295 |
| 1987 | 186 | 2 | 184 | 4,481 |
| 1988 | 177 | 4 | 173 | 4,658 |
| 1989 | 162 | 10 | 152 | 4,820 |
| 1990 | 166 | 12 | 154 | 4,986 |
| 1991 | 205 | 17 | 188 | 5,191 |
| 1992 | 262 | 23 | 239 | 5,453 |
| 1993 | 301 | 12 | 289 | 5,754 |
| 1994 | 377 | 22 | 355 | 6,131 |
| 1995 | 559 | 33 | 526 | 6,690 |
| 1996 | 532 | 41 | 491 | 7,222 |
| 1997 | 625 | 29 | 596 | 7,847 |
| 1998 | 531 | 56 | 475 | 8,378 |
| 1999 | 493 | 43 | 450 | 8,871 |
| 2000 | 597 | 56 | 541 | 9,468 |
| 2001 | 533 | 32 | 501 | 10,001 |
| 2002 | 512 | 32 | 480 | 10,513 |
| 2003 | 403 | 42 | 361 | 10,916 |
| 2004 | 367 | 14 | 353 | 11,283 |
| 2005 | 366 | 23 | 343 | 11,649 |
| 2006 | 370 | 31 | 339 | 12,019 |
| 2007 | 325 | 28 | 297 | 12,344 |
| 2008 | 229 | 3 | 226 | 12,573 |
| 2009 | 147 | 5 | 142 | 12,720 |
| 2010 | 146 | 7 | 139 | 12,866 |
| 2011 | 133 | 10 | 123 | 12,999 |
| 2012 | 123 | 11 | 112 | 13,122 |
| 2013 | 133 | 9 | 124 | 13,255 |
| 2014 | 173 | 29 | 144 | 13,428 |
| 2015 | 174 | 4 | 170 | 13,602 |
| 2016 | 174 | 7 | 167 | 13,776 |
| 2017 | 202 | 26 | 176 | 13,978 |
| 2018 | 257 | 3 | 254 | 14,235 |
| 2019 | 224 | 11 | 213 | 14,459 |
| 2020 | 250 | 29 | 221 | 14,709 |
| 2021 | 364 | 17 | 347 | 15,073 |
| 2022 | 304 | 17 | 287 | 15,377 |
| 2023 | 244 | 1 | 243 | 15,621 |
| 2024 | 196 | 0 | 196 | 15,817 |
| 2025 | 178 | 1 | 177 | 15,995 |
| 2026 | 218 | 60 | 158 | 16,213 |
Every district in the file on one scale · the whole file, one year at a time · Plate 4 of the Driller’s Atlas.
What drillers reached, township by township
43 PLSS townships here where at least 5 water-supply permits naming the same aquifer filed a depth (12,752 permits in all; the 24 most-drilled are drawn, every one is in the table). Each column is one township, six miles square, on one scale to 700 ft below ground: a faint lane spans the 10th to 90th percentile of where the permits naming that aquifer stopped, the solid band their screens, the tick the median. This is the permit file’s view of the ground — the aquifer is the name the driller wrote, the band is where those holes ended — not a geologic map, and a township is as fine as it gets. Monitoring holes are left out. 8 of these townships straddle a district line and are filed here because most of their permits are.
1,583 · 73% here
1,378
993
893
786 · 84% here
776 · 50% here
627
532
526
469
433 · 76% here
419
348
260 · 86% here
240
223
203
172
165
162
131
127
127
124
unnamed alluvium fractured crystalline faint = where the permits naming it stopped (10th–90th pct) · solid = their screens · tick = median · ft below ground as filed
Every township here, as a table
| Township | Share of its permits in this district | Aquifer named | Permits with a depth | Drilled depth p10 / p50 / p90, ft | Screen top p10 / p50 / p90, ft | Screen bottom p10 / p50 / p90, ft |
|---|---|---|---|---|---|---|
| T13S R70W 6th PM | 73% | unnamed | 1,533 | 100 / 240 / 500 | 40 / 160 / 440 | 100 / 250 / 500 |
| T13S R70W 6th PM | 73% | fractured crystalline | 50 | 142 / 390 / 641 | 77 / 340 / 532 | 164 / 400 / 632 |
| T9S R75W 6th PM | 100% | unnamed | 1,327 | 194 / 355 / 587 | 85 / 230 / 440 | 193 / 360 / 580 |
| T9S R75W 6th PM | 100% | fractured crystalline | 51 | 227 / 401 / 520 | 72 / 200 / 308 | 223 / 380 / 528 |
| T9S R78W 6th PM | 100% | unnamed | 981 | 78 / 168 / 360 | 42 / 110 / 260 | 80 / 170 / 355 |
| T9S R78W 6th PM | 100% | alluvium | 6 | 158 / 238 / 320 | 91 / 190 / 282 | 147 / 235 / 336 |
| T12S R71W 6th PM | 99% | unnamed | 887 | 65 / 200 / 500 | 20 / 140 / 440 | 80 / 212 / 514 |
| T12S R71W 6th PM | 99% | fractured crystalline | 6 | 265 / 300 / 530 | — | — |
| T12S R70W 6th PM | 84% | unnamed | 770 | 125 / 300 / 500 | 50 / 215 / 440 | 131 / 300 / 500 |
| T12S R70W 6th PM | 84% | fractured crystalline | 16 | 310 / 460 / 700 | 324 / 380 / 504 | 372 / 440 / 620 |
| T8S R78W 6th PM | 50% | unnamed | 772 | 66 / 140 / 280 | 29 / 85 / 188 | 72 / 147 / 280 |
| T10S R75W 6th PM | 100% | unnamed | 608 | 140 / 285 / 476 | 75 / 185 / 350 | 145 / 280 / 475 |
| T10S R75W 6th PM | 100% | fractured crystalline | 19 | 212 / 320 / 444 | 130 / 225 / 360 | 230 / 320 / 400 |
| T9S R77W 6th PM | 100% | unnamed | 524 | 100 / 180 / 320 | 50 / 120 / 240 | 100 / 180 / 334 |
| T10S R77W 6th PM | 100% | unnamed | 512 | 92 / 160 / 295 | 58 / 100 / 200 | 100 / 160 / 296 |
| T10S R77W 6th PM | 100% | alluvium | 6 | 85 / 165 / 240 | — | — |
| T10S R77W 6th PM | 100% | fractured crystalline | 6 | 160 / 220 / 267 | 106 / 180 / 212 | 154 / 220 / 268 |
| T13S R76W 6th PM | 99% | unnamed | 450 | 120 / 205 / 420 | 60 / 140 / 321 | 120 / 202 / 420 |
| T13S R76W 6th PM | 99% | fractured crystalline | 18 | 130 / 240 / 478 | 70 / 195 / 310 | 128 / 255 / 466 |
| T13S R71W 6th PM | 76% | unnamed | 427 | 66 / 200 / 488 | 20 / 124 / 380 | 98 / 220 / 480 |
| T13S R71W 6th PM | 76% | fractured crystalline | 5 | 203 / 400 / 520 | — | — |
| T13S R72W 6th PM | 99% | unnamed | 418 | 60 / 162 / 400 | 20 / 98 / 316 | 75 / 180 / 400 |
| T8S R76W 6th PM | 99% | unnamed | 340 | 70 / 248 / 500 | 50 / 151 / 320 | 100 / 265 / 480 |
| T8S R76W 6th PM | 99% | fractured crystalline | 8 | 248 / 325 / 444 | 160 / 175 / 196 | 255 / 326 / 400 |
| T13S R77W 6th PM | 86% | unnamed | 255 | 140 / 260 / 451 | 70 / 165 / 340 | 120 / 260 / 446 |
| T13S R77W 6th PM | 86% | fractured crystalline | 5 | 200 / 320 / 363 | — | — |
| T8S R75W 6th PM | 99% | unnamed | 238 | 69 / 202 / 453 | 40 / 125 / 300 | 100 / 220 / 480 |
| T9S R74W 6th PM | 99% | unnamed | 218 | 158 / 440 / 655 | 88 / 250 / 421 | 180 / 440 / 652 |
| T11S R74W 6th PM | 99% | unnamed | 185 | 125 / 260 / 420 | 34 / 160 / 326 | 124 / 260 / 420 |
| T11S R74W 6th PM | 99% | fractured crystalline | 18 | 214 / 320 / 436 | 96 / 180 / 278 | 188 / 320 / 448 |
| T12S R75W 6th PM | 100% | unnamed | 161 | 30 / 150 / 552 | 20 / 120 / 428 | 50 / 203 / 600 |
| T12S R75W 6th PM | 100% | fractured crystalline | 9 | 380 / 440 / 549 | 124 / 150 / 312 | 390 / 460 / 526 |
| T11S R75W 6th PM | 100% | unnamed | 159 | 80 / 225 / 460 | 39 / 118 / 306 | 97 / 260 / 440 |
| T11S R75W 6th PM | 100% | fractured crystalline | 5 | 130 / 230 / 276 | — | — |
| T14S R76W 6th PM | 98% | unnamed | 153 | 180 / 280 / 400 | 120 / 202 / 336 | 180 / 280 / 400 |
| T14S R76W 6th PM | 98% | fractured crystalline | 9 | 112 / 310 / 512 | 90 / 240 / 265 | 150 / 300 / 355 |
| T11S R77W 6th PM | 99% | unnamed | 126 | 60 / 140 / 378 | 46 / 100 / 221 | 80 / 145 / 397 |
| T12S R73W 6th PM | 100% | unnamed | 122 | 77 / 200 / 384 | 26 / 115 / 302 | 80 / 200 / 394 |
| T12S R73W 6th PM | 100% | fractured crystalline | 5 | 226 / 285 / 348 | 98 / 225 / 288 | 210 / 280 / 342 |
| T9S R76W 6th PM | 99% | unnamed | 122 | 100 / 250 / 478 | 40 / 140 / 326 | 100 / 260 / 464 |
| T9S R76W 6th PM | 99% | fractured crystalline | 5 | 172 / 300 / 408 | — | — |
| T13S R75W 6th PM | 100% | unnamed | 120 | 90 / 200 / 380 | 45 / 120 / 283 | 102 / 200 / 360 |
| T12S R72W 6th PM | 98% | unnamed | 100 | 35 / 182 / 481 | 20 / 118 / 360 | 84 / 205 / 475 |
| T11S R76W 6th PM | 100% | unnamed | 100 | 40 / 120 / 280 | 32 / 88 / 248 | 76 / 133 / 318 |
| T10S R74W 6th PM | 99% | unnamed | 84 | 101 / 240 / 450 | 18 / 84 / 300 | 100 / 232 / 442 |
| T13S R74W 6th PM | 100% | unnamed | 83 | 101 / 200 / 452 | 40 / 120 / 336 | 100 / 200 / 398 |
| T13S R73W 6th PM | 99% | unnamed | 79 | 79 / 150 / 396 | 45 / 128 / 315 | 100 / 165 / 380 |
| T11S R72W 6th PM | 100% | unnamed | 77 | 44 / 140 / 376 | 22 / 82 / 320 | 62 / 180 / 385 |
| T10S R72W 6th PM | 99% | unnamed | 67 | 60 / 225 / 540 | 20 / 130 / 416 | 60 / 250 / 580 |
| T11S R78W 6th PM | 99% | unnamed | 68 | 68 / 175 / 376 | 49 / 106 / 283 | 84 / 180 / 376 |
| T11S R73W 6th PM | 100% | unnamed | 61 | 120 / 240 / 360 | 60 / 160 / 276 | 120 / 220 / 358 |
| T14S R75W 6th PM | 93% | unnamed | 43 | 100 / 240 / 492 | 40 / 160 / 340 | 110 / 220 / 480 |
| T7S R76W 6th PM | 93% | unnamed | 41 | 40 / 120 / 390 | 18 / 80 / 265 | 75 / 155 / 550 |
| T10S R76W 6th PM | 100% | unnamed | 39 | 58 / 174 / 506 | 30 / 75 / 304 | 60 / 162 / 470 |
| T12S R76W 6th PM | 99% | unnamed | 38 | 79 / 198 / 406 | 64 / 140 / 308 | 120 / 280 / 424 |
| T10S R73W 6th PM | 100% | unnamed | 32 | 21 / 179 / 295 | 70 / 140 / 252 | 154 / 185 / 370 |
| T11S R71W 6th PM | 97% | unnamed | 30 | 21 / 78 / 362 | 10 / 36 / 257 | 37 / 120 / 357 |
| T10S R78W 6th PM | 100% | unnamed | 27 | 48 / 140 / 318 | 39 / 90 / 155 | 78 / 140 / 256 |
| T14S R74W 6th PM | 66% | unnamed | 26 | 3 / 220 / 405 | 105 / 180 / 240 | 150 / 220 / 290 |
| T12S R74W 6th PM | 97% | unnamed | 19 | 54 / 200 / 320 | 30 / 100 / 240 | 58 / 200 / 319 |
| T12S R77W 6th PM | 100% | unnamed | 13 | 47 / 85 / 129 | 37 / 42 / 85 | 52 / 78 / 138 |
These columns on the map · Plate 6 of the Driller’s Atlas.
The Driller’s Atlas · Plate 2 A cross-section nobody surveyed
Every permitted well within a few miles of the line, drawn from the ground to its drilled depth as the driller filed it. The bright part of each stroke is the perforated casing — where the well actually takes water — coloured by the aquifer named on the permit. Nobody arranged these; the aquifers arrange themselves.
The ground each well hangs from is a 1-km elevation model sampled at the point the permit was spotted, so the profile is real topography smoothed to about a kilometre — peaks are shaved, valleys filled a little — and the depths are the driller’s, measured down from that ground.
Hover or arrow through the strokes to read a well.
The same corridor as a table
| Miles from A | Wells drawn | Median depth (ft) | With a screen | Most-named aquifer | No depth filed | Ground, ft above sea level (median) |
|---|
Bins run from end A to end B of the line. “Most-named aquifer” is the family most often named on permits in the bin, with its count; permits naming no aquifer are the majority of the file and are not a family.
Reservoirs
Source DWR administrative record · verify at DWR structure records ↗
44 reservoir(s) with 3,277 storage measurement(s), 1974–2026. Basin storage as of 2025-10-31 (the record's own end — reservoir records publish ~annually): 146,385 AF across 7 reservoir(s).
Why storage matters to the flow network
Storage change is real water the mass balance must credit — a losing reach beside a filling reservoir isn't losing water, it's banking it.
Reservoir map — how full is each vessel?
What “full” is measured against
Bubble size is proportional to a reservoir's record-high storage. Fill is its last recorded storage as a share of its surveyed capacity (USACE National Inventory of Dams) where a confident NID match exists — the tooltip names the matched dam — and as a share of its own record high otherwise. A wrong capacity would be worse than an honest record high, so only confident joins upgrade.
A dashed teal ring marks reservoirs reporting live DWR telemetry: their fill reflects yesterday's storage, is drawn as a dotted tail on charts, and is treated as provisional until the next verified HydroBase snapshot supersedes it.
A dashed red ring marks a dam under an active storage restriction from DWR's Dam Safety branch — the State Engineer has limited how much it may legally store, so a low fill can be an order, not a drought. Hazard class and inspection condition come from the same record, joined only where the dam carries this reservoir's WDID or a confident NID match — a wrong dam's restriction would be worse than none shown.
Basin storage, end of each water year
End-of-water-year totals; per-year reservoir counts shown because reporting coverage varies -- a total is only comparable to years with similar counts.
Largest reservoirs on record
Click a row to chart its full storage history, or open its dossier for rights, documents and dam-safety facts.
| Reservoir | Last recorded storage (AF) | As of | Full | Dam (DWR Dam Safety) | |
|---|---|---|---|---|---|
| ▸ ELEVEN MILE RES (2303965) | 100,140 | 2025-10-31 | — | — | dossier → |
| ▸ SPINNEY MTN RESERVOIR (2304013) | 23,202 | 2025-10-31 | — | — | dossier → |
| ▸ ANTERO RES (2303904) | 18,272 | 2025-10-31 | — | — | dossier → |
| ▸ MONTGOMERY RES (2303962) | 3,942 | 2025-10-31 | — | — | dossier → |
| ▸ TARRYALL RES (2303977) | 2,353 | 1975-10-31 | — | — | dossier → |
| ▸ BAKER RES (2303982) | 800 | 1980-07-31 | — | — | dossier → |
| ▸ LIDDERDALE RES (2303966) | 734 | 1980-07-31 | — | — | dossier → |
| ▸ JEFFERSON LAKE RES (2303981) | 683 | 2025-10-31 | — | — | dossier → |
Snow and runoff
Source Independent agency measurement · fetched 2026-10-13 · verify at NRCS report generator ↗ Source Our computation, scored against a reference · NRCS forecast, graded here against the gage record
Snow-water equivalent, WY2027
| SNOTEL site | Elev (ft) | SWE (in) | Median (in) | % of median | Typical peak |
|---|---|---|---|---|---|
| Buckskin Joe | 11160 | 0.0 | 0.1 | — | May 2 (12.6 in) |
| Michigan Creek | 10700 | 0.0 | 0.0 | — | April 26 (13.2 in) |
| Rough And Tumble | 10420 | 0.8 | 0.0 | — | April 24 (8.3 in) |
NRCS SNOTEL, daily. Sites are assigned to the district whose boundary contains them — the snow that feeds this district can also sit in a neighboring headwater district.
Two ways a snow year goes wrong (1999–2026)
A bad snow year here comes in two flavors (both called snow droughtA winter that shorts the snowpack. It happens two ways: a dry one, where the snow never comes, and a warm one, where near-normal snow falls but melts off weeks early -- and the river feels them differently.), and the river feels them differently. In 8 of the last 28 winters the snow never came — the pack peaked below 80% of its median. In 0 more, the snow came but left early — a near-normal peak melted out two weeks or more ahead of its usual date, sending the water down before the season needed it.
The snow never came: 2002, 2012, 2017, 2018, 2022, 2023, 2025, 2026.
Computed by this site from 3 SNOTEL sites’ full daily records (NRCS AWDB, back to 1999). Each year is measured against each site’s own multi-decade median — not the 1991–2020 normal the chart above uses — so the 1980s grade against a fair baseline. Peak and melt-out need 85% of the season’s days on the record; thin years are dropped, not guessed. Derived from snow measurements alone — it cannot tell dry-from-warm causes apart, only what the snowpack did.
Runoff outlook — Antero Reservoir Inflow
NRCS's final issue (2026-06-01) calls it even odds that at least 5 kAF arrives over 06-01 to 09-30 — 46% of a normal season; almost certainly at least 2, probably not more than 7. New forecasts begin in January. How to read these numbers →
| 90% chance of at least | 70% chance of at least | 50% chance of at least | 30% chance of at least | 10% chance of at least | Normal |
|---|---|---|---|---|---|
| 2 | 4 | 5 | 6 | 7 | 11 |
Runoff outlook — Spinney Mountain Reservoir Inflow
NRCS's final issue (2026-06-01) calls it even odds that at least 16 kAF arrives over 06-01 to 09-30 — 37% of a normal season; almost certainly at least 7, probably not more than 22. Our own record at this gage shows 6 kAF actually delivered. New forecasts begin in January. How to read these numbers →
We test a record-based adjustment of the April benchmark at every graded point. Here it did not beat NRCS over 61 replayed seasons (24% typical miss unadjusted vs 28% adjusted), so none is shown — NRCS’s own forecast, unadjusted, is the best April benchmark available for this river. Why we test →
| 90% chance of at least | 70% chance of at least | 50% chance of at least | 30% chance of at least | 10% chance of at least | Normal | Observed |
|---|---|---|---|---|---|---|
| 7 | 12 | 16 | 18 | 22 | 43 | 6 |
How good are these forecasts here? (1994–2025)
Grading every April issue against what the river then delivered, measured at this gage’s own record — 31 seasons: the median miss of the 50% forecast is 22%, with a high bias of 1%, and the observed volume landed inside the stated 10–90% band 74% of the time (a calibrated forecast would say 80%).
Computed by this site: NRCS's archived April issues (their period as issued each year) against the observed volume in DWR’s published record; years with under 90% daily coverage are dropped, not summed. A grade of the forecast, never of the forecasters — these are hard rivers. How this point ranks among every graded Colorado forecast point →
What April snow has meant for this river (1999–2026)
Across 28 measured years, the season’s water has loosely followed the April snowpack: a year opening April with 80% of median snow has typically gone on to deliver about 81% of a normal season (a snow-to-runoff elasticityHow strongly one number moves with another. A snow-to-runoff elasticity of 1.5 means a 10% shortfall in April snowpack has typically become a 15% shortfall in the season's water. of 0.8).
Computed by this site: the district’s April 1 SWE (% of each SNOTEL site’s own-record median) against the observed April–July volume at this gage (% of its median season) — a fixed window every year, unlike the forecast grades above, which use each issue’s own period. The slope is fit so single wild years can’t steer it (Theil–Sen, log space); years missing 10% of their days are dropped.
Runoff outlook — Elevenmile Canyon Reservoir Inflow
NRCS's final issue (2026-06-01) calls it even odds that at least 18 kAF arrives over 06-01 to 09-30 — 41% of a normal season; almost certainly at least 8, probably not more than 25. New forecasts begin in January. How to read these numbers →
| 90% chance of at least | 70% chance of at least | 50% chance of at least | 30% chance of at least | 10% chance of at least | Normal |
|---|---|---|---|---|---|
| 8 | 14 | 18 | 21 | 25 | 45 |
Drought
Source Our computation, no independent reference · computed here from the screened DWR record Source Independent agency measurement · fetched 2026-10-06 · verify at U.S. Drought Monitor ↗
Right now
This is the 46th-driest week 39 in 96 years of record at SOUTH PLATTE RIVER NEAR LAKE GEORGE, CO. (as of 2026-09-21; this week’s flow sits at the 48th percentileRank against the record: a river at its 5th percentile is lower than it was in 95 of the past 100 years on this same date. for the date). On this week’s US Drought Monitor, Boulder County is 24% in D4 exceptional drought (2026-10-06). The law agrees: the most senior active call leaves 99% of this district’s decreed flow rights junior to the calling right this week.
Every year since 1929, week by week
Each thin row is a year at SOUTH PLATTE RIVER NEAR LAKE GEORGE, CO.; each cell is one week’s flow ranked against the same calendar week of every other year — warm means dry for the date, blue wet, so seasonality cancels and droughts appear as warm bands. Gaps are missing record, never a dry river. Click a year to reconstruct it on the Historical tab.
This year against its analogs
Over the 39 weeks recorded so far, 2026’s weekly trace most resembles 2018 (mean gap 15.9 percentile points; next closest 2023 (16.1), 1992 (18.2)). The analog’s remainder is drawn as context — its ending is what happened to it, not a forecast for this year.
The Drought Monitor’s view since 2000
Mean share of area in each class across Boulder, Park counties — the counties this district’s gages sit in, which overlap the district imperfectly. The Drought Monitor weighs soils, vegetation and local reports; it is CONTEXT beside the river’s own record above, not the water-rights picture.
The law’s own drought gauge
When water runs short, administration answers: calls reach further back in time, and more decreed rights go junior to the calling right. This is that response, weekly since 1957 — the share of this district’s decreed flow rights junior to the most senior active call. Watch it spike in the named droughts below, and linger after the river recovers.
Computed from DWR’s call record (754 calls touching this district) against the district’s rights index. Scoping is deliberately coarse — a call’s own district, or districts named in its comments — and this is administration’s RESPONSE, not a per-structure verdict (each dossier’s curtailment card does that, with stream miles). A deepening call can also reflect growing demand, not only shrinking supply.
This basin’s droughts, by its own record
| Drought | Span | Weeks | Trough percentile | Flows recovered | Water table back |
|---|---|---|---|---|---|
| the 2002 drought | 2003-07-21 → 2004-02-16 | 30 | 17th (2003-09-22) | 49 weeks | 14 yr (5 wells, 2 still below) |
| unnamed dry spell | 1983-04-25 → 1983-11-21 | 30 | 17th (1983-07-11) | 7 weeks | — |
| the 1981 drought | 1981-07-06 → 1981-12-07 | 22 | 25th (1981-08-31) | 35 weeks | not yet (6 of 12 wells still below) |
| the 1977 drought | 1977-09-12 → 1979-03-12 | 78 | 12th (1978-08-07) | 13 weeks | — |
| unnamed dry spell | 1974-09-16 → 1975-05-26 | 36 | 16th (1974-10-28) | 8 weeks | — |
| unnamed dry spell | 1972-08-28 → 1973-05-14 | 37 | 16th (1972-12-25) | 4 weeks | — |
| unnamed dry spell | 1965-11-29 → 1968-08-12 | 141 | 9th (1967-07-31) | 48 weeks | — |
| the 1963-64 drought | 1962-11-12 → 1963-08-19 | 40 | 18th (1963-02-04) | 1 week | — |
| unnamed dry spell | 1960-08-29 → 1961-10-16 | 59 | 14th (1961-01-30) | 5 weeks | — |
| unnamed dry spell | 1958-10-27 → 1959-12-14 | 59 | 9th (1958-12-22) | 16 weeks | — |
| the 1950s drought | 1956-11-26 → 1957-04-29 | 22 | 24th (1956-12-31) | 55 weeks | — |
| the 1950s drought | 1953-11-02 → 1954-05-03 | 26 | 22nd (1954-02-08) | 7 weeks | — |
| the 1950s drought | 1953-03-02 → 1953-08-03 | 22 | 28th (1953-05-25) | 46 weeks | — |
| the 1950s drought | 1950-09-11 → 1951-04-23 | 32 | 22nd (1950-10-23) | 59 weeks | — |
Detected mechanically: the 26-week smoothed percentile below the 30th for at least 20 weeks; recovered on regaining the 50th. The water-table clock compares each monitoring well against its own pre-drought median (the 3 years before onset) and dates the year the median well got back — the aquifer remembers longest, and “still below” is a finding, not a gap. The knobs are stated because the episode list depends on them — a different reasonable choice merges or splits episodes at the edges. Names are attached where an episode overlaps a drought Colorado already talks about.
What drought has cost here
Since 1994, federal crop insurance has paid $182,449 in drought-caused claims across Boulder, Park counties — 4.2% of all insured crop losses there. The worst year was 2022 ($70,070).
USDA crop-insurance indemnities where the recorded cause of loss is drought, summed over the counties this district's gages sit in. Counties overlap water districts imperfectly, and insured-crop claims are a floor on drought damage, not a total. Source: USDA RMA cause-of-loss files.
When this basin claimed its water
Every bar is a year’s new appropriations (2,131 rights across 98 years of shared record), colored by that year’s wetness from the barcode above. Here the correlation is -0.3 — this basin tended to claim water in dry times, under scarcity pressure. Across the state both behaviors exist: ephemeral southwest basins file after wet demonstrations, transbasin-source basins under drought — and the biggest statewide filing waves sat in the 1950s drought and after 2002, not in the wet 1980s–90s.
Appropriation dates are the CLAIMED initiation of a right, not the courthouse filing date; the record is survivor-biased (abandoned claims are absent, so failed dry-era scrambles are undercounted); and the big 1960s and 2000s spikes sit on legal events — the pre-1969-Act adjudication era and 2000s legislation — not on weather. A correlation here is a description, never a cause.
New to how a dry winter becomes a call on the river? Anatomy of a drought walks the chain in four minutes — snow to rivers to reservoirs to calls to the water table.
Legal
Who serves it, who protects it
Two registers the site fetches on their own schedules, read for this district. Neither is a DWR record; each links its own page and its agency.
Public water systems here
Source Register of another agency · fetched 2026-10-06 · verify at EPA SDWIS ↗
10 systems touch this district (10 community systems reporting 4,153 people served, a figure that counts a wholesaler's customers twice); none carries an open health-based violation on EPA's record.
| System | Serves | Source | Here |
|---|---|---|---|
| FAIRPLAY TOWN OF | 909 | Groundwater under the influence of surface water | 100% of its area |
| HIGHLAND LAKES WD | 875 | Groundwater under the influence of surface water | 100% of its area |
| DIVIDE WATER PROVIDERS INC | 570 | Groundwater | 13% of its area |
| ALMA TOWN OF | 460 | Surface water | 100% of its area |
| REDHILL FOREST POMWACA | 388 | Groundwater | 100% of its area |
| ARABIAN ACRES MD | 325 | Groundwater | 100% of its area |
| FLORISSANT WSD | 250 | Groundwater under the influence of surface water | 100% of its area |
| WARM SPRINGS OWNERS MUTUAL WA | 250 | Groundwater | 100% of its area |
and 2 more; the full directory filters by district.
Instream-flow rights held by the state
Source Register of another agency · fetched 2026-10-11 · verify at CWCB instream flow program ↗
41 reaches over 313.1 miles and 6 natural lake levels, held by the Colorado Water Conservation Board so that water stays in the stream. Every reach, with its schedule and case →
- Middle Fork South Platte River, 28.8 mi: 8 (10/1 - 4/30), 16 (5/1 - 9/30) cfs (appropriated 1980, 80CW0067) · dossier
- Tarryall Creek, 26.0 mi: 20 (1/1 - 12/31) cfs (appropriated 1977, 77W8730) · dossier
- Tarryall Creek, 21.4 mi: 7 (01/01 - 12/31) cfs (appropriated 1976, 76W8229) · dossier
- Michigan Creek, 19.3 mi: 7 (1/1 - 12/31) cfs (appropriated 1976, 76W8230) · dossier
- Fourmile Creek, 17.1 mi: 8 (1/1 - 12/31) cfs (appropriated 1976, 76W8224) · dossier
- Rule Creek, 14.6 mi: 1 (1/1 - 12/31) cfs (appropriated 1980, 80CW0213) · dossier
and 41 more on the district's instream-flow page.
What the water is like -- USGS sensors right now, where it has been sampled, the impaired-waters list, and how the tap water here stands with EPA -- is on the Water quality tab.
Designated groundwater basins are on their own page.
Source Adjudicated record · verify at DWR water-right transactions ↗ Source Adjudicated record · verify at DWR net amounts ↗
Decreed rights on this network run from 1860-12-28 to 2021-05-28. Of the 20 structures with a yield estimate, the median one’s senior right was in priority 50% of a median irrigation season and 16% in a dry one. 25 abandonment screens and 98 compliance flags are listed below as leads for review — a screen is not an abandonment and a flag is not a violation.
Rights on file: 3195 across 2640 structure(s); 0 structure(s) carry 0 court-case references. Advisory reading aids on public DWR data — not administrative or legal conclusions.
Is the river getting harder to divert from?
Over 1951–2025, administration on this district has been tightening: 2 of 3 measures (days under callA senior water right demanding its water, which requires everyone junior on that stream to stop diverting until it is satisfied., calls set, seniorityColorado shares water by date: the earlier the right, the stronger its claim when the river runs short. "First in time, first in right." of the controlling call) are moving toward more administration, none the other way.
The three measures, year by year
One row per whole calendar year inside the call record's coverage (75 years); partly-covered years are omitted rather than reported as quiet. Trend is Mann-Kendall with the same significance gate as every other trend on this site. Counted from DWR's published call record, which begins in the early 2000s: earlier years are absent, not quiet. A rise in the number of calls set can also reflect how finely an administrator records one episode, which is why days under call -- insensitive to that -- is the component to read first. Advisory summary of the public record, not an administrative finding.
| Year | Days under call | Calls set | Controlling priority (median) |
|---|---|---|---|
| 2014 | 309 | 220 | 1873-06-30 |
| 2015 | 329 | 144 | 1870-06-01 |
| 2016 | 366 | 168 | 1875-06-30 |
| 2017 | 365 | 246 | 1881-02-01 |
| 2018 | 365 | 254 | 1876-05-10 |
| 2019 | 365 | 273 | 1881-02-01 |
| 2020 | 366 | 191 | 1869-04-01 |
| 2021 | 365 | 172 | 1867-04-15 |
| 2022 | 365 | 225 | 1867-04-15 |
| 2023 | 333 | 219 | 1869-04-01 |
| 2024 | 366 | 190 | 1881-02-01 |
| 2025 | 365 | 316 | 1881-02-01 |
Why diversions stopped — call-based explanations
Sustained diversion stops matched to senior administrative calls.
- PLATTE STATION DITCH (2300500) DWR↗ stopped 2024-07-11 (10+ days) — call at WESTERN MUTUAL DITCH curtailing 100% of its decreed rate [heuristic-strong, district-confirmed]
- SOUDERS WOLFE D 2 (2300503) DWR↗ stopped 2024-07-11 (108+ days) — call at WESTERN MUTUAL DITCH curtailing 100% of its decreed rate [heuristic-strong, district-confirmed]
- GARDEN DITCH (2300569) DWR↗ stopped 2024-07-10 (307+ days) — call at WESTERN MUTUAL DITCH curtailing 100% of its decreed rate [heuristic-strong, district-confirmed]
- HEELEY DITCH 2 (2300579) DWR↗ stopped 2024-07-10 (303+ days) — call at WESTERN MUTUAL DITCH curtailing 100% of its decreed rate [heuristic-strong, district-confirmed]
- HEELEY DITCH 1 (2300573) DWR↗ stopped 2024-07-08 (309+ days) — call at WESTERN MUTUAL DITCH curtailing 100% of its decreed rate [heuristic-strong, district-confirmed]
- HALL DITCH 1 (2300585) DWR↗ stopped 2024-07-06 (307+ days) — call at BIG T PLATTE R DITCH curtailing 100% of its decreed rate [heuristic-strong]
Right yield — how often could these rights actually divert?
Share of irrigation-season days each structure's rights were not called out, derived from the 22-year district-scoped call record (senior right = floor, junior right = ceiling constraint). Call-record-derived; DWR's own analysis governs where available.
| Structure | Senior priority | Senior right: median / dry yr | Junior right: median / dry yr |
|---|---|---|---|
| LAKE GEORGE INTAKE (2300693) DWR↗ | 1994-12-21 | 5.1% / 0.0% | 5.1% / 0.0% |
| SOUTH PLATTE RIVER ABOVE SPINNEY RESERVO (2302903) DWR↗ | 1874-06-15 | 58.0% / 16.8% | 26.1% / 0.5% |
| COMO JIM DITCH (2300715) DWR↗ | 1886-10-01 | 34.3% / 2.3% | 34.3% / 2.3% |
| MIDDLE FORK SOUTH PLATTE AT PRINCE (2302913) DWR↗ | 1868-08-01 | 86.9% / 26.6% | 46.8% / 9.8% |
| BALD HILL LK 1 MIN LEVEL (2302129) DWR↗ | 1977-01-19 | 5.6% / 0.0% | 5.6% / 0.0% |
| ROGERS NORTH DITCH (2300714) DWR↗ | 1879-05-15 | 46.8% / 15.9% | 46.8% / 15.9% |
| LAKE MAGNUSON RES (2304003) DWR↗ | 1968-06-19 | 5.6% / 0.0% | 5.6% / 0.0% |
| COLUMBIA PLACER 1 (2300651) DWR↗ | 1868-12-31 | 86.9% / 26.6% | 86.9% / 26.6% |
| MCCARTNEY SEEP DITCH (2300889) DWR↗ | 1885-05-20 | 46.8% / 6.1% | 5.1% / 0.0% |
| ANTERO FEEDER DITCH (2300964) DWR↗ | 1907-10-08 | 13.6% / 0.0% | 5.6% / 0.0% |
| SOUTH FORK OF SOUTH PLATTE ABOVE ANTERO (2302900) DWR↗ | 1873-06-25 | 60.8% / 17.3% | 15.4% / 0.0% |
| SACRAMENTO DITCH (2300760) DWR↗ | 1867-07-01 | 91.6% / 30.4% | 34.3% / 2.3% |
Abandonment radar (25 screens)
Absolute rights with 10+ years of no recorded diversions. Screens only — storage, alternate points, and plan operations can explain nonuse lawfully. And diversion REPORTING itself only reached its modern level ~1950 — idleness that begins before then may be unreported use, not nonuse (flagged † below).
- RANDALL D EXT CLAIM (2300988) DWR↗ (1878-08-01, 1.0 cfs decreed): last active 1951 — 74 years idle
- FURMAN WASTE WATER DITCH (2300981) DWR↗ (1882-05-01, 10.0 cfs decreed): last active 1958 — 67 years idle
- KESTER SWEET SPRINGS (2300543) DWR↗ (1876-12-31, 0.2 cfs decreed): last active 1962 — 63 years idle
- HAYMAN SPRG STOCK WTR DE (2301504) DWR↗ (1983-07-31, 0.0 cfs decreed): last active 1970 — 55 years idle
- HURST SPRING 1 (2301589) DWR↗ (1932-06-21, 0.1 cfs decreed): last active 1970 — 55 years idle
- TOMS SPRING 1 (2301639) DWR↗ (1961-09-02, 0.1 cfs decreed): last active 1970 — 55 years idle
- CHENEY SPRING DITCH (2300692) DWR↗ (1873-05-15, 1.8 cfs decreed): last active 1973 — 52 years idle
- SPRING CREEK DITCH (2300833) DWR↗ (1947-09-25, 8.0 cfs decreed): last active 1973 — 52 years idle
- SPRING DITCH 1 (2300834) DWR↗ (1915-12-31, 0.0 cfs decreed): last active 1973 — 52 years idle
- SILVERHEELS AUG R INLET (2300688) DWR↗ (1997-06-11, 4.8 cfs decreed): last active 1974 — 51 years idle
Compliance screens (98 advisory flags)
Screened 180 of 2640 structures with rights (229 have diversion history on file). A flag is a lead for expert review — augmentation plans, exchanges, and free-river conditions can make over-decree diversions lawful and are deliberately not modeled.
- ANTERO RES (2303904) DWR↗: Observed p99 daily rate 215.0 cfs (max 462.0) exceeds total decreed absolute 6.0 cfs across 11185 recorded day(s).
- MONTGOMERY RES (2303962) DWR↗: Observed p99 daily rate 110.5 cfs (max 261.5) exceeds total decreed absolute 0.5 cfs across 40688 recorded day(s).
- CANON DITCH (2300694) DWR↗: Observed p99 daily rate 50.0 cfs (max 50.0) exceeds total decreed absolute 35.4 cfs across 2574 recorded day(s).
- GUIRAUD 3T DITCH (2300679) DWR↗: Observed p99 daily rate 40.0 cfs (max 40.0) exceeds total decreed absolute 1.2 cfs across 3418 recorded day(s).
- PRINCE DITCH (2300680) DWR↗: Observed p99 daily rate 36.1 cfs (max 36.1) exceeds total decreed absolute 0.6 cfs across 2050 recorded day(s).
- MICHIGAN CREEK ABOVE JEFFERSON (2302907) DWR↗: Observed p99 daily rate 34.9 cfs (max 46.3) exceeds total decreed absolute 22.3 cfs across 20384 recorded day(s).
- JEFFERSON LAKE DITCH (2301080) DWR↗: Observed p99 daily rate 34.3 cfs (max 67.9) exceeds total decreed absolute 30.0 cfs across 1236 recorded day(s).
- BURLINGAME DITCH (2300510) DWR↗: Observed p99 daily rate 30.0 cfs (max 32.0) exceeds total decreed absolute 1.4 cfs across 2760 recorded day(s).
- MIDDLE FORK SOUTH PLATTE AT SANTA MARIA (2302902) DWR↗: Observed p99 daily rate 30.0 cfs (max 45.0) exceeds total decreed absolute 25.0 cfs across 10931 recorded day(s).
- GUIRAUD DITCH (2300686) DWR↗: Observed p99 daily rate 27.2 cfs (max 35.3) exceeds total decreed absolute 3.4 cfs across 2516 recorded day(s).
Seniority (top structures by decreed rate)
| Structure | Senior priority date | Rights | Decreed abs (cfs) | Decreed abs (AF) | Conditional? |
|---|---|---|---|---|---|
| LAKE GEORGE INTAKE (2300693) DWR↗ | 1994-12-21 | 1 | 600.0 | 0 | — |
| SOUTH PLATTE RIVER ABOVE SPINNEY RESERVO (2302903) DWR↗ | 1874-06-15 | 18 | 100.9 | 0 | — |
| COMO JIM DITCH (2300715) DWR↗ | 1886-10-01 | 1 | 84.0 | 0 | — |
| MIDDLE FORK SOUTH PLATTE AT PRINCE (2302913) DWR↗ | 1868-08-01 | 25 | 80.5 | 3692 | — |
| BALD HILL LK 1 MIN LEVEL (2302129) DWR↗ | 1977-01-19 | 1 | 78.0 | 0 | — |
| ROGERS NORTH DITCH (2300714) DWR↗ | 1879-05-15 | 1 | 67.2 | 0 | — |
| LAKE MAGNUSON RES (2304003) DWR↗ | 1968-06-19 | 1 | 63.4 | 0 | — |
| COLUMBIA PLACER 1 (2300651) DWR↗ | 1868-12-31 | 1 | 60.0 | 0 | — |
| MCCARTNEY SEEP DITCH (2300889) DWR↗ | 1885-05-20 | 4 | 58.6 | 0 | — |
| ANTERO FEEDER DITCH (2300964) DWR↗ | 1907-10-08 | 2 | 55.0 | 0 | — |
| SOUTH FORK OF SOUTH PLATTE ABOVE ANTERO (2302900) DWR↗ | 1873-06-25 | 22 | 45.9 | 0 | — |
| SACRAMENTO DITCH (2300760) DWR↗ | 1867-07-01 | 2 | 43.4 | 0 | — |
| THE PLACER MINE DITCH (2300602) DWR↗ | 1879-12-31 | 1 | 42.9 | 0 | — |
| FAIRPLAY LOWER OR EAST (2300759) DWR↗ | 1866-12-31 | 1 | 40.0 | 0 | — |
| CANON DITCH (2300694) DWR↗ | 1867-07-15 | 1 | 35.4 | 0 | — |
Recent inventory & legal-document changes
- 2026-10-10 — call set: SOUTH FLAT DITCH (39707)
- 2026-10-10 — call set: STERLING IRR CO DITCH 1 (39706)
- 2026-10-10 — call released: 39612
- 2026-10-09 — call released: 39680
- 2026-10-09 — call set: SOUTH PLATTE RIVER AT WATERTON (39697)
- 2026-10-09 — call set: CHATFIELD RESERVOIR (39698)
- 2026-10-09 — call released: 39678
- 2026-10-08 — call set: TRUE WEBSTER DITCH (39693)
Water-court filings this month (division-wide)
24 applications in the 2026-08 resume for this basin's division — new rights, changes, augmentation plans — from the water clerk's statutory monthly notice (C.R.S. 37-92-302), the earliest public signal of a new claim. Filings are division-wide, not district-filtered: check the county column. Full resume PDF at the Judicial Branch →
Anyone affected may file a statement of opposition until 2026-10-31 (18 days left). C.R.S. 37-92-302(3): due by the last day of the second month following the filing month — computed, not legal advice; confirm with the water clerk.
All 24 filings, with excerpts
| Case | What it asks | County | Excerpt |
|---|---|---|---|
2026CW3039
|
— | — | CASE NO. 20 26CW3039; STATE ENGINEER AND WATER DIV 2 ENGINEER vs. ANDREW STOREY – Verified Complaint for Injunctive Relief, Penalties, and Costs. This case is being listed in the resume to account for the case number in consecutive order. ---------------------… |
2026CW3040
|
plan for augmentation, new underground right | — | CASE NO. 2026CW3040 , Water Division 2 and CASE NO. 2026CW3135, Water Division 1; JANICE L DUNCAN, 6440 Highline Place, Colorado Springs, CO, 80908 (Please address all pleadings and inquiries regarding this matter to Applicant’s attorney: Philip E. Lopez, Eric… |
2026CW3088
|
plan for augmentation | — | CASE NUMBER 2026CW3088 NORTH RANCH, LLC, c/o Robert L. Myers, 944 Cheyenne Blvd., Colorado Springs, CO 80905; Please direct all correspondence concerning the application to: Ryan W. Farr, Sedona E. Chavez, Monson, Cummins, Shohet & Farr, LLC, 13511 Northgate E… |
2026CW3089
|
— | — | CASE NUMBER 20 26CW3089 ROBERSON LIVING TRUST, c/o Tamara Roberson -George, Rex Roberson, Kevin Roberson, Co-Trustees, 18235 Black Forest Road, Colorado Springs, CO 80908; Please direct all correspondence concerning this application to: David M. Shohet, and Se… |
2026CW3119
|
change of water right, plan for augmentation, new storage right | — | CASE NUMBER 2026CW3119 SHARON AND MARK WEATHERFORD, 12328 S. State Hwy 83, Franktown, CO 80116. (Forward all pleadings and correspondence to Chris D. Cummins and Sedona E. Chavez, Monson, Cummins, Shohet & Farr, LLC, 13511 Northgate Estates Dr., Ste. 250, Colo… |
2026CW3120
4404471 |
reasonable diligence | THE CITY AND | CASE NUMBER 2026CW3120 THE CITY AND COUNTY OF DENVER, ACTING BY AND THROUGH ITS BOARD OF WATER COMMISSIONERS (“Denver Water” or “Applicant”), 1600 West 12th Avenue, Denver, Colorado 80204. Jessica R. Brody, General Counsel, Daniel J. Arnold, James M. Wittler, … |
2026CW3121
|
— | — | CASE NUMBER 2026CW3121 (2018CW3222)… |
2026CW3122
|
plan for augmentation, new underground right | — | CASE NUMBER 2026CW3122 DOUBLE S CONSTRUCTION & DESIGN LLC, ATTN: Scott Berry, 42631 Sager Lane, Parker, CO, 80138. APPLICATION FOR UNDERGROUND WATER RIGHTS FROM NONTRIBUTARY AND NOT-NONTRIBUTARY SOURCES AND APPROVAL OF PLAN FOR AUGMENTATION, IN THE NONTRIBUTAR… |
2026CW3123
|
reasonable diligence | THE CITY AND | CASE NUMBER 2026CW3123 THE CITY AND COUNTY OF DENVER, ACTING BY AND THROUGH ITS BOARD OF WATER COMMISSIONERS (“Denver Water” or “Applicant”), 1600 West 12th Avenue, Denver, Colorado 80204. Jessica R. Brody, General Counsel, Daniel J. Arnold, James M. Wittler, … |
2026CW3124
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reasonable diligence, make absolute, new underground right | — | CASE NUMBER 2026CW3124 WESTERN EQUIPMENT AND TRUCK, INC. , 2055 1 st Ave., Greeley, CO 80631, 970 -353-6682. P. Andrew Jones, Law Office of P. Andrew Jones, 1213 Founders Circle, Windsor, CO 80550, 970 -297-0570, ajones@pandrewjones.com. APPLICATION TO MAKE CO… |
2026CW3125
0600538 0600565 0600576 |
reasonable diligence | EASONABLE DILIGENCE IN BOULDER | CASE NUMBER 2026CW3125 (90CW108) (99CW125) (12CW72) (20CW3017) APPLICATION FOR FINDING OF REASONABLE DILIGENCE IN BOULDER COUNTY . 1. Name, Mailing Address, Phone Number, and E -mail Address of Applicant . CITY OF LAFAYETTE , c/o Cari Bischoff, Water Resources… |
2026CW3126
0815262 0815263 0815264 |
reasonable diligence, make absolute | — | CASE NUMBER 2026CW3126 MARY GUENZEL CHARITABLE TRUST, P.O. Box 9, Woodland Park, Colorado 80866; Please direct all correspondence concerning this application to: Ryan W. Farr, Monson, Cummins, Shohet & Farr, LLC, 13511 Northgate Estates Drive, Suite 250, Color… |
2026CW3127
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new underground right | UPPER LARAMIE AQUIFER IN WELD | CASE NUMBER 2026CW3127 THE CITY OF GREELEY, ACTING BY AND THROUGH ITS WATER AND SEWER BOARD, AND THE COLORADO STATE BOARD OF LAND COMMISSIONERS. APPLICATION FOR NONTRIBUTARY UNDERGROUND WATER RIGHTS IN THE UPPER LARAMIE AQUIFER IN WELD COUNTY. I. Name, mailing… |
2026CW3128
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reasonable diligence, make absolute | — | CASE NUMBER 2026CW3128 Applicant. CHRIS DINSDALE, P.O. Box 1807, Sterling, CO 80751, 970-522-9052 with all correspondence connected herewith being sent to Applicant’s Counsel, David P. Jones, Lawrence Custer Grasmick Jones & Donovan, LLP., 5245 Ronald Regan Bl… |
2026CW3129
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plan for augmentation, new underground right | PLAN FOR AUGMENTATION IN ELBERT | CASE NUMBER 2026CW3129 VANCE ROBERT ANDRUS & TONI COLLEEN ANDRUS , 6414 Sherman Peak, Castle Rock, Colorado 80108. APPLICATION FOR UNDERGROUND WATER RIGHTS FROM NONTRIBUTARY AND NOT-NONTRIBUTARY SOURCES AND APPROVAL OF PLAN FOR AUGMENTATION IN ELBERT COUNTY . … |
2026CW3130
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— | — | CASE NUMBER 2026CW 3130 THE CITY OF GREELEY, ACTING BY AND THROUGH ITS WATER AND SEWER BOARD c/o Leah Hubbard, Deputy Director of Water Resources, 1001 – 11th Avenue, 2nd Floor, Greeley, Colorado 80631, leah.hubbard@greeleygov.com, (970) 350-9811. Please send … |
2026CW3131
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reasonable diligence | — | CASE NUMBER 2026CW3131 CITY OF LOVELAND , Colorado (“Loveland”), c/o Noah Cecil, Assistant City Attorney, 500 East Third Street, #330, Loveland, Colorado 80537, Telephone: (970) 962 - 2434. APPLICATION FOR FINDING OF REASONABLE DILIGENCE IN LARIMER AND WELD CO… |
2026CW3132
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— | — | CASE NUMBER 2026CW3132 Applicants. THE CENTRAL COLORADO WATER CONSERVANCY DISTRICT AND THE GROUNDWATER MANAGEMENT SUBDISTRICT OF THE CENTRAL COLORADO WATER CONSERVANCY DISTRICT , 3209 West 28 th Street, Greeley, Colorado, 80634, 970-330-4540 with all future co… |
2026CW3133
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reasonable diligence | — | CASE NUMBER 2026CW3133 CHELEY LAND, LLC AND CHELEY COLORADO CAMPS, LLC (f.k.a. Cheley Colorado Camps, Inc.) , 601 Steele Street, P.O. Box 6525, Denver, CO 80206. c/o Karen L. Henderson, Bushong & Holleman PC, 1966 13th Street, Suite 270, Boulder, CO 80302; (30… |
2026CW3139
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change of water right | — | CASE NUMBER 2026CW3139 ALBERT WENDELL NELSON REVOCABLE TRUST c/o Wendell Nelson, Trustee 5537 N. County Road 9 Fort Collins, CO 80524 303 -921-4750 Sally Jean Nelson Revocable Trust c/o Wendell Nelson, Trustee 5537 N. County Road 9 Fort Collins, CO 80524 303 -… |
2026CW3140
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plan for augmentation | PLAN FOR AUGMENTATION IN ELBERT | CASE NUMBER 2026CW3140 DAVID JOE KRAXNER III, 754 Highway 86, Elizabeth, CO, 80107. Philip E. Lopez, Eric K. Trout, Fairfield and Woods, P.C., 1801 California St, Suite 2600, Denver, CO, 80202. APPLICATION FOR A PLAN FOR AUGMENTATION IN ELBERT COUNTY. Subject … |
2026CW3141
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plan for augmentation | — | CASE NUMBER 2026CW3141 KELTY COLORADO FAMILY LLLP, C/o Bruff Shea, P.O. Box 21, Franktown, Colorado 80166. Please direct all pleadings and correspondence to Applicants counsel: Michael A. Kopp, Trout Raley PC, 1120 Lincoln St., Suite 1600, Denver, CO 80203, (3… |
2026CW3142
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new underground right | — | CASE NUMBER 2026CW3142 1. Name, address, and telephone number of Applicant and Landowner: 1.1. Applicant and Landowner: CAP LAND LLC, a Colorado limited liability company 47 (“CAP Land”) c/o Lena Vander Laan P.O. Box 105 Henderson, CO 80640 Please direct all c… |
2026CW9
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reasonable diligence, make absolute | LARIMER | CASE NUMBER 2026CW9 SPRING44 DISTILLING, INC. (“Spring44”), 505 West 66th Street, Loveland, Colorado 80538, Telephone: (970) 445 -7109. APPLICATION FOR FINDINGS OF REASONABLE DILIGENCE AND CLAIM TO MAKE CERTAIN AMOUNTS ABSOLUTE IN LARIMER COUNTY. 2. Lindauer S… |
Active substitute water supply plans in this district
Temporary State Engineer approvals to divert out of priority (37-92-308 / 37-90-137). A structure operating under one behaves differently under a call than its decreed rights alone suggest — the priority tables above don't know about these; this list does. Source: DWR’s active-SWSP register, refreshed nightly.
| Plan | Type | Status | Expires | Structure | Documents |
|---|---|---|---|---|---|
| BRANNAN SAND & GRAVEL COMPANY | 37-90-137(11) GRAVEL PIT PLAN | Approved | — | 2302537 | plan file |
Water quality
The water itself, in this district
Four registers, each on its own schedule: what USGS sensors read right now, where samples have been taken, which stretches the state lists as impaired, and how the tap water of the systems here stands with EPA. None is a DWR record; each links its own page.
Right now
Source Provisional telemetry · fetched 2026-10-13 · verify at USGS current conditions ↗
No USGS continuous water-quality sensor reports from inside this district. Statewide sensors →
Where water has been sampled
Source Register of another agency · fetched 2026-10-08 · verify at Water Quality Portal ↗
The portal lists 1,047 sampling stations in this district's watershed (South Platte Headwaters 10190001), of which 22 reported a sample in the last 5 years on the state and tribal side (USGS activity is in the station count, not in that figure). Most active: Colorado Dept. of Public Health & Environment-WQCD (18), Colorado River Watch (4). Most-sampled groups: Inorganics, Major, Metals, Physical, Nutrient, Inorganics, Minor, Non-metals. Every station as a file ↗
Results themselves are not fetched here; USGS samples added after March 2024 may not be in the portal's legacy profiles yet.
Drinking water
Source Register of another agency · fetched 2026-10-07 · verify at EPA SDWIS ↗
10 community systems touch this district. None carries an open health-based violation on EPA's record. EPA sampled 0 of them for PFAS in 2023–25.
| System | Serves | EPA record | PFAS (UCMR 5) | Lead, latest 90th pct |
|---|---|---|---|---|
| FAIRPLAY TOWN OF | 909 | 2 of 12 quarters with a violation | not sampled | 0.001 mg/L |
| HIGHLAND LAKES WD | 875 | 12 of 12 quarters with a violation | not sampled | 0.002 mg/L |
| DIVIDE WATER PROVIDERS INC | 570 | 1 of 12 quarters with a violation | not sampled | 0.0005 mg/L |
| ALMA TOWN OF | 460 | 1 of 12 quarters with a violation | not sampled | 0.002 mg/L |
| REDHILL FOREST POMWACA | 388 | clean, last 12 quarters | not sampled | 0.0 mg/L |
| ARABIAN ACRES MD | 325 | 12 of 12 quarters with a violation | not sampled | 0.0 mg/L |
| WARM SPRINGS OWNERS MUTUAL WA | 250 | 2 of 12 quarters with a violation | not sampled | 0.0095 mg/L |
| FLORISSANT WSD | 250 | 11 of 12 quarters with a violation | not sampled | 0.0012 mg/L |
| FOREST GLEN SPORTS ASSOC INC | 76 | 12 of 12 quarters with a violation | not sampled | 0.004 mg/L |
| SHAWNEE WCA | 50 | 1 of 12 quarters with a violation | not sampled | 0.0 mg/L |
EPA's record carries violations and lead/copper percentiles; nitrate and disinfection by-product results are not in it. UCMR 5 samples are monitoring, not compliance, and the 2024 PFOA/PFOS limits equal its reporting limit, so any detection of those two is at or above them.
Impaired waters
Source Register of another agency · verify at EPA ATTAINS ↗
The state's 303(d) impaired-waters list has not been joined to this basin's own watershed boundary yet, so nothing is shown rather than a guess; the basins with a join carry the full list here. Why the join is geometry, not a name match.
Call cascade
If a call were placed at a given seniority, which structures in this basin would be out of priority, and how much of their decreed rate would be curtailed? Computed from this basin's cached decrees.
What this does and doesn't model. Seniority arithmetic only: every right junior to the call is treated as curtailed. It does not model reach applicability — structures downstream of the calling point are not administered by it — and it applies no futile-call judgment. Read it as “who is junior to this date, and by how much,” not as a prediction of what the Division Engineer would actually order.
Pick a calling right
Real decrees from this basin, ordered by administration number — that is, by actual seniority. The years will look out of order, and that is correct: an administration number encodes the adjudication date as well as the appropriation date, so a right appropriated in 1970 can be administered ahead of one from 1950. A senior call curtails almost everything; a junior one curtails almost nothing.
Or enter an administration number directly
DWR administration numbers encode appropriation and adjudication dates; lower is more senior.
This week's diagnostic
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System status
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Active river calls
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Hydrographs vs. historical envelope
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Anomaly flags
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Snowpack — 3 SNOTEL sites report here. Runoff outlook — Antero Reservoir Inflow: even odds of at least 5 kAF over 06-01 to 09-30 — 46% of a normal season, per NRCS, issued 2026-06-01 — the season’s final; new forecasts begin in January. Runoff outlook — Spinney Mountain Reservoir Inflow: even odds of at least 16 kAF over 06-01 to 09-30 — 37% of a normal season, per NRCS, issued 2026-06-01 — the season’s final; new forecasts begin in January. Runoff outlook — Elevenmile Canyon Reservoir Inflow: even odds of at least 18 kAF over 06-01 to 09-30 — 41% 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 site | Elev (ft) | SWE (in) | Median (in) | % of median | Typical peak |
|---|---|---|---|---|---|
| Buckskin Joe | 11160 | 0.0 | 0.1 | — | May 2 (12.6 in) |
| Michigan Creek | 10700 | 0.0 | 0.0 | — | April 26 (13.2 in) |
| Rough And Tumble | 10420 | 0.8 | 0.0 | — | April 24 (8.3 in) |
Antero Reservoir Inflow — 06-01 to 09-30 volume, thousand acre-feet (chance the volume is AT LEAST this):
| 90% | 70% | 50% | 30% | 10% | Normal |
|---|---|---|---|---|---|
| 2 | 4 | 5 | 6 | 7 | 11 |
Spinney Mountain Reservoir Inflow — 06-01 to 09-30 volume, thousand acre-feet (chance the volume is AT LEAST this):
| 90% | 70% | 50% | 30% | 10% | Normal |
|---|---|---|---|---|---|
| 7 | 12 | 16 | 18 | 22 | 43 |
Elevenmile Canyon Reservoir Inflow — 06-01 to 09-30 volume, thousand acre-feet (chance the volume is AT LEAST this):
| 90% | 70% | 50% | 30% | 10% | Normal |
|---|---|---|---|---|---|
| 8 | 14 | 18 | 21 | 25 | 45 |
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.