Snake River

Wild & Scenic🏞 National Park
Teton County, Lincoln County · 54 mi · Class I-III
Optimal: 1400–4200 CFS · USGS #13013650
Water temp: 69°F
2,792 avg
6,580CFS
11.56 ft gauge height
Above Optimal
Falling slowly (-60 cfs/hr)(-110 in 3h)
Flow data is live from USGS·Rapid classifications and CFS ranges need community verification·Know this river?
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Avg flow: 2,792 cfsHist. median: 0 cfsUSGS #13013650
National Wild & Scenic River · National Park Service

About

Notable Era — Watershed History. The river's character begins with its water. Gauge 13013650 records a mean flow of 2,792 cubic feet per second, with an optimal boating window between 1,400 and 4,200 CFS. Those numbers describe a mountain river of real volume, one whose sections span the calm and the technical: the run breaks into named reaches from Jackson Lake to Pacific Creek, Southgate to Flagg Ranch, Pacific Creek to Deadmans Bar, Deadmans Bar to Moose Landing, and, farther down, Alpine Canyon. Each reach carries its own tempo, from open valley drifts to tighter canyon water.

The watershed's distinction is its setting. The Snake River Headwaters is not a single park boundary but a mosaic — Yellowstone and Grand Teton, the John D. Rockefeller Memorial Parkway, the National Elk Refuge, and the Bridger-Teton National Forest, all stitched into one continuous system. That the river spends 42 of its first miles inside Yellowstone, and rises from the Two Ocean Plateau, means its earliest character is shaped entirely by preserved country. It is this unbroken corridor, more than any single feature, that defines the upper Snake.

The river's human history runs deep. Long before contact, this Wyoming segment flowed through ancestral Indigenous territory, used for fishing, travel, and gathering by Indigenous peoples. The name itself dates to 1812, when the Shoshone lent the word that explorers fixed to the waterway. Later came the resource era: from the 1820s through the 1920s, the surrounding stretch was worked for hardwood and softwood, with sawmills, logging drives, and downstream shipping along the main channel. The exhaustion of the old-growth stands in 1910 brought large-scale logging to an end.

Scientific attention followed the settlers. USGS survey work in the Wyoming segment ran from the 1880s into the 1910s, establishing the first comprehensive hydrological assessments of the river. Clean Water Act assessments between 1972 and 2000 built on that foundation, beginning the long accounting of a century of logging, agricultural, and industrial impacts. The survey record and the water-quality record together trace how the river was measured, then managed.

The modern chapter is one of repair. Since 2010, state environmental agencies working in partnership with Snake River Watershed partnerships have taken on more than a hundred years of cumulative impact. Streambank stabilization from 2015 to 2024, native fish restocking from 2017 to 2024, and TMDL implementation from 2020 to 2024 stand as the major recent outcomes. The arc — frontier settlement, industrial-era logging, and modern restoration — frames the river's defining historical chapters. Today the upper Snake endures as one of the West's defining mountain rivers, its origins on the Two Ocean Plateau still feeding a system that connects Yellowstone, Grand Teton, and the wild lands between them.

Solunar Fishing Activity
🌒
Waxing Crescent
26% illumination
Poor
Moon overhead
11:48 AM
Moonrise
6:10 PM
Moonset
5:26 AM
Moon underfoot
11:48 PM
Next full moon: Jul 2910 days
10-Year Flow Patterns
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Data Quality

River conditions are community-verified. CFS ranges, difficulty ratings, and access points may not reflect every flow level or seasonal change. Always check current conditions, scout unfamiliar rapids, and paddle within your skill level.

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