Kennebec River

Somerset County, Kennebec County, Sagadahoc County · 4 mi · Class V+
Optimal: 1350–4050 CFS · USGS #01042500
2,690 avg
474CFS
1.96 ft gauge height
Below Optimal
Stable(-125 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: 2,690 cfsHist. median: 0 cfsUSGS #01042500
Private

About

Benedict Arnold's Expedition to Quebec. The Kennebec Gorge is a short, serious run. The four-mile section carries a Class V+ rating, and the numbers explain why: USGS gauge 01042500 shows an average flow of 2,690 CFS, with an optimal window between 1,350 and 4,050 CFS. That is a lot of water moving through a confined New England gorge, and it makes the Kennebec one of the region's most demanding whitewater stretches. The river drains three Maine counties — Somerset, Kennebec, and Sagadahoc — as it works its way from Moosehead Lake toward the sea.

Long before gauges and dams, the Kennebec flowed through the ancestral territory of Indigenous peoples, serving as a primary travel corridor, hunting ground, and gathering place. The river's later history was shaped by the treaty and cession framework of the 1800s, including the 1830 Indian Removal Act and the allotment era that ran from the 1840s through the 1890s.

The river's most famous chapter came in September 1775. Arnold's 1,100 troops set out from Cambridge, Massachusetts, ascending the Kennebec through the Maine wilderness with the goal of attacking British-held Quebec. The march was brutal — portages around the Great Falls, a hurricane, and conditions that killed or stranded nearly half the men. The effort culminated in the December 31 Battle of Quebec, where Arnold was wounded but escaped.

In the century that followed, the watershed became an industrial engine. From the 1830s through the 1920s, the Kennebec's forests were logged to feed the regional timber industry and the railroad expansion of the 1860s through the 1910s. Sawmills, logging drives, and downstream lumber operations dominated the valley until the old-growth stands were exhausted around 1910, state forestry conservation began in 1915, and state forests were established in the 1930s. Meanwhile, the first comprehensive hydrological studies arrived with USGS surveys in the 1870s through 1890s, followed by gauging stations and, decades later, Clean Water Act assessments from 1972 onward that reckoned with a century of logging, agricultural, and industrial impacts.

That reckoning made the Kennebec a proving ground for restoration. The July 1, 1999 removal of the Edwards Dam in Augusta let the river run free and revived its health, becoming a national landmark for dam removal. The momentum has continued: The Nature Conservancy reached an agreement with Brookfield Renewable to purchase four dams on the lower river — Lockwood, Hydro-Kennebec, Shawmut, and Weston — with the aim of restoring the watershed while safeguarding its economic vitality. Since 2010, Maine's Department of Natural Resources and local watershed partnerships have pursued streambank stabilization, native fish restocking, nutrient reduction, and water-quality improvements. From a Revolutionary War route to a restoration model, the Kennebec keeps working.

Solunar Fishing Activity
🌒
Waxing Crescent
26% illumination
Poor
Moon overhead
9:01 AM
Moonrise
3:20 PM
Moonset
2:41 AM
Moon underfoot
9:01 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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