Lewis and Clark Lake
The Reservoirs · Lake 6 of 6 · RM 810–836

Lewis and Clark Lake

The smallest and busiest of the six — 25 miles of bright water above Gavins Point Dam, filling fast with the sediment the river can no longer carry away.

The lake today
Pool ft msl
Ft below full
26
Pool miles
RM 810
to 836
Next 48 hours

Wind windows.

Calm <15 mph · Caution 15–25 · Hazardous 25+ sustained — tap any hour for detail
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Access — ramps & recreation areas All on the map →
SiteRiver mileStateType
Springfield State Recreation Area835.5NEboat ramp
Santee833.4NEboat ramp
Sand Creek Land Use Area832.6SDboat ramp
Miller Creek822.1NEboat ramp
Bloomfield820.9NEboat ramp
Weigand Marina816.0NEboat ramp
North Ramp811.1NEboat ramp
South Shore810.4NEboat ramp
Gavins Tailwaters South809.3NEboat ramp
Gavins Tailwaters North809.1NEboat ramp
Gavins Tailwaters North809.1NEboat ramp
Depths

Depths, at today's pool.

This lake IS mapped — marine-chart apps carry contours today. We're sourcing an open layer for all six pools (USACE Omaha surveys · state wildlife agencies · USGS ScienceBase). Depths will render against today's pool, not the full-pool number printed on fishing maps.

051020406080+ ft
What this water covers

The history under the lake.

Gavins Point Dam closed in 1955 to re-regulate the releases of the giants upstream, and its modest pool flooded the Missouri's braided channel between the chalkstone bluffs the expedition described in late August 1804 — Calumet Bluff, where Lewis and Clark held their first council with the Yankton Sioux.

The lake is now the river's sediment story told in fast-forward: the delta at its head grows every year as the Missouri drops its load, and engineers openly debate the reservoir's endgame. For paddlers the delta is the draw — a returning, accidental wilderness of willow islands and shifting channels immediately upstream of the last dam on the river.