Lake levels today
30 lakes with their own page, every reading shown with its time. Newest reading: Oct 18, 2026, 8:00 AM CDT.
All lakes on lakepeek
| Keystone Lake | OK | 722.70 | −0.30 ft | +2.26 ft |
| Grand Lake | OK | 741.97 | −0.03 ft | −0.07 ft |
| Lake Eufaula | OK | 581.05 | −3.95 ft | +0.12 ft |
| Oologah Lake | OK | 640.53 | +2.53 ft | +0.22 ft |
| Kaw Lake | OK | 1,011.61 | +1.61 ft | +2.55 ft |
| Lake Texoma | OK · TX | 615.12 | −2.50 ft | +0.14 ft |
| Tenkiller Lake | OK | 624.95 | −7.05 ft | −0.47 ft |
| Fort Gibson Lake | OK | 555.43 | +1.43 ft | +0.91 ft |
| Skiatook Lake | OK | 710.91 | −3.09 ft | −0.03 ft |
| Sardis Lake | OK | 597.31 | −1.69 ft | −0.08 ft |
| Copan Lake | OK | 709.02 | −0.98 ft | +0.19 ft |
| Broken Bow Lake | OK | 591.30 | −9.53 ft | −0.91 ft |
| Hugo Lake | OK | 400.72 | −3.78 ft | −0.21 ft |
| Wister Lake | OK | 474.75 | −3.25 ft | −0.32 ft |
| Hulah Lake | OK | 732.34 | −0.66 ft | +0.15 ft |
| Cheney Lake | KS | 1,420.21 | −1.39 ft | −0.06 ft |
| Sam Rayburn Reservoir | TX | 153.42 | −10.98 ft | −0.29 ft |
| Lake Georgetown | TX | 784.47 | −6.53 ft | −0.13 ft |
| Belton Lake | TX | 592.97 | −1.03 ft | −0.22 ft |
| Somerville Lake | TX | 236.51 | −1.49 ft | −0.16 ft |
| Stillhouse Hollow Lake | TX | 621.01 | −0.99 ft | −0.29 ft |
| Proctor Lake | TX | 1,156.09 | −5.91 ft | −0.03 ft |
| Lake Texana | TX | 41.93 | −2.07 ft | −0.27 ft |
| Bull Shoals Lake | AR · MO | 653.30 | −5.70 ft | −0.46 ft |
| Beaver Lake | AR | 1,112.52 | −7.91 ft | −0.23 ft |
| Norfork Lake | AR · MO | 552.31 | −1.44 ft | −0.27 ft |
| Millwood Lake | AR | 259.38 | +0.18 ft | +0.14 ft |
| Truman Lake | MO | 705.55 | −0.47 ft | −0.04 ft |
| Pomme de Terre Lake | MO | 838.19 | −0.81 ft | +0.05 ft |
| Lake Wappapello | MO | 360.23 | +5.49 ft | −0.03 ft |
Lakes by state
How to read these numbers
Each lake has a normal pool, the top of the conservation pool set by the agency that runs the dam. Above it, the extra water is flood storage that is released over the following days or weeks; below it, the lake is lower than planned, usually after a dry spell. The difference from normal pool is the quickest way to compare lakes of very different sizes.
We also compare each reading with the typical level for the same date over the past ten years, because many lakes are held lower in winter and higher in summer. See our method and sources.