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Arkansas: Las Animas to Stateline

Division 2 · Water District 67
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Arkansas: Las Animas to Stateline on the ground — the ditches, wells, reservoirs and gages of Water District 67 · clicktap anything for its record

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

32% of normal flow, week of 2026-06-29
24 calls active on it right now

The Arkansas River is well below normal for late June -- 32% of normal flow. 24 calls stand against it right now; the most senior right calling dates to 1860.

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

25,500 water-level measurements across 2601 monitored well(s) — 1104 alluvial, 887 bedrock — plus 2 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 397 well(s) with enough record for a trend test: 134 declining, 42 rising.

Fastest-declining wellsSettingft / decadeSpanp
SHP-45 TWN.OF SPRINGFIELD bedrock -41.99 61 yr 0.0005
SC02304305CAC2 unknown -36.26 15 yr 0.0
SHP-11 AUSMUS,G,& S. 1 bedrock -31.58 61 yr 0.0
SHP-30 HUME, CHARLES bedrock -28.79 88 yr 0.0001
SHP-09 COGBURN, B. bedrock -26.5 42 yr 0.0002
SHP-18 COMMERCE RANCH 3 bedrock -26.22 75 yr 0.0
SC03004513CCC bedrock -25.82 20 yr 0.0
SHP-06 MEYERS, S. bedrock -24.5 41 yr 0.0043

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.

FORT BENT DITCH: 16 alluvial well(s) nearby; pooled water table -0.7 ft (1961–2023, no_trend, p=0.3224)

GRANADA IRRIGATION CANAL AUGMENTATION STATION EAST: 31 alluvial well(s) nearby; pooled water table +619.3 ft (1955–2023, decreasing, p=0.0023)

AMITY CANAL: 28 alluvial well(s) nearby; pooled water table +140256.0 ft (1955–2018, decreasing, p=0.0)

WILD HORSE CREEK ABOVE HOLLY, CO: 31 alluvial well(s) nearby; pooled water table +0.9 ft (1955–2023, no_trend, p=0.9539)

KICKING BIRD CANAL: 0 alluvial well(s) nearby

HYDE DITCH: 36 alluvial well(s) nearby; pooled water table +47319.1 ft (1956–2018, decreasing, p=0.0002)

ARKANSAS RIVER AT LAMAR, CO.: 61 alluvial well(s) nearby; pooled water table +0.7 ft (1955–2018, no_trend, p=0.3129)

LAMAR CANAL: 65 alluvial well(s) nearby; pooled water table +0.7 ft (1955–2018, no_trend, p=0.8842)

FORT BENT DITCH AUG STATION: 25 alluvial well(s) nearby; pooled water table +95038.7 ft (1955–2018, no_trend, p=0.0506)

BIG SANDY CREEK NEAR LAMAR, CO.: 29 alluvial well(s) nearby; pooled water table +0.0 ft (1956–2023, no_trend, p=0.7591)

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: 12 parent disagreements, 14 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 29 streams, 17 agree. Know this water? Tell us →

StreamThis site routes it toDWR routes it to
Antelope Creek the mainstem Big Sandy Creek
Antelope Creek the mainstem South Rush Creek
Middle Rush Creek the mainstem Rush Creek
Rush Creek the mainstem Big Sandy Creek
Antelope Creek the mainstem West Mud Creek
Antelope Creek the mainstem Muddy Creek
Cottonwood Creek the mainstem Rule Creek
Buffalo Creek the mainstem nan

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

Caddoa Creek (55 mi) · Mud Creek (47 mi) · Wolf Creek (37 mi) · Clay Creek (33 mi) · Gageby Creek (11 mi) · Wiley Drainage Ditch (10 mi) · Cheyenne Creek (7 mi) · McRae Arroyo (6 mi)

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