Water Intelligence Brief · Archive
October 26, 2026
October 26, 2026 | Sevier River Basin
Streamflows across the Sevier River Basin are stable to rising this week, with the Sevier River showing upward movement at multiple gauges and Manti Creek holding steady at modest late-October levels — conditions consistent with seasonal transition into the dormant period as irrigation demand winds down. Turkey producers, ranchers, and hay operations should note that late-season delivery reliability is the operative question heading into winter, not immediate supply stress. Reservoir storage data and 7-day forecast details are available in the full brief.
All six SNOTEL stations in and around Sanpete County are reporting at or near zero snow water equivalent, which is normal for this point on the calendar — median SWE for late October at these elevations is also effectively zero, so current readings reflect seasonal conditions, not a deficit.
Station readings as of October 25, 2026:
Early-season snowpack accumulation is just beginning at the higher elevations, with Mt. Baldy showing the most meaningful reading at 0.5" SWE. The 2026 water year context: snowpack across the region melted out approximately 4–6 weeks ahead of the historical median meltout date following an anomalous March heat wave, which shaped summer streamflow conditions. That event is now background history. The forward-looking question is how robustly accumulation builds through November and December — a metric to watch as the season progresses.
Manti Creek below Dugway Creek near Manti (the only active in-county USGS gauge) is reading 4 cfs and stable as of October 26. This is a modest but steady late-season flow consistent with the dormant season transition. No active USGS gauge exists on the San Pitch River mainstem — that remains a known monitoring gap. Contact Sanpete Water Conservancy District for any supplemental local monitoring data.
Sevier River gauges in adjacent counties provide broader basin context:
The rising trend at Hatch, Kingston, and Lynndyl is a notable signal for this time of year. Basin-wide streamflow is moving upward across all reporting gauges, which may reflect recent precipitation or regional runoff — causal attribution is beyond the scope of this brief. The Sigurd gauge data gap limits visibility into the mid-basin reach most directly relevant to Sanpete County delivery infrastructure; users dependent on that reach should contact their water district for current operational status.
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Data Sources: SNOTEL data through October 25, 2026; USGS streamflow data through October 26, 2026
Data Current As Of: Utah Division of Water Rights
Important Disclaimers: This brief provides automated analysis for informational purposes only. Specific numerical claims have not been independently verified. Consult official sources including your local water district, U.S. Bureau of Reclamation, and Utah Division of Water Rights for regulatory decisions and water rights administration.
Data & Disclaimers
Sources: NRCS SNOTEL network · USGS National Water Information System · National Weather Service
This brief provides automated analysis for informational purposes only. Consult official sources including your local water district and state Division of Water Rights for regulatory decisions. This document does not constitute legal, regulatory, or engineering advice.
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