Every named river in the Adirondack Park — the Hudson, the Moose, the Raquette, the Sacandaga, and the rivers that drain the High Peaks.
The Salmon River runs through the town of Keene — not to be confused with the more famous Salmon River systems near Pulaski or in Franklin County — draining a forested corridor between the High Peaks and the Champlain Valley. It's a tributaried backcountry stream rather than a destination river, feeding into the broader Ausable drainage and surfacing along old logging roads and private property lines where access is limited and unmarked. No stocking records, no developed put-ins, no trail register — this is water you encounter while bushwhacking or cross-referencing old USGS quads. If you're looking for moving water to fish or paddle in Keene, the East Branch Ausable is the name you want.
The Salmon River runs north through Keene — a cold, fast tributary system that drains into the East Branch of the Ausable River below town. It's less traveled than the mainstream Ausable channels and sees more local attention than destination traffic: wade fishing for brookies in spring and early summer, mostly pocket water and short runs through mixed hardwood and hemlock. The upper tributaries push into state land west of Keene Valley, but most anglers work the mid-section crossings along back roads between NY-73 and the Styles Brook confluence. Check DEC regs — some upper reaches fall under catch-and-release wild trout management.
The Saranac River drains the entire northern Adirondack watershed — it begins at Upper Saranac Lake, flows north through the village of Saranac Lake, then bends east through Bloomingdale and Redford before emptying into Lake Champlain near Plattsburgh. The stretch near Keene picks up water from tributaries running off the north slopes of the High Peaks, cold and fast through rock channels that hold native brook trout in the pocket water. Access is scattered — some stretches border private land, others cross under Route 3 or older county roads where you can pull off and fish the runs. Most paddlers skip this upper section in favor of the calmer flatwater downstream, but anglers who know the northeast drainages work these stretches in spring and fall.
The Saranac River cuts through the northern Adirondacks in three distinct branches — West, South, and North — before converging near the village of Saranac Lake and draining northeast into Franklin County and eventually the St. Regis River system. The stretch through Keene is part of the South Branch corridor, a cold, fast-moving trout river that runs through mixed hardwood and hemlock forest before opening into farmland valleys downstream. Access is uneven — some road crossings, some posted land, some state easements — and fishing pressure is lighter than the better-known Au Sable system to the south. Paddlers looking for moving water typically wait until spring runoff settles or target the lower reaches closer to Saranac Lake village where the gradient eases.
The Saranac River threads through the northeastern Adirondacks in three distinct branches — the North, Main, and South — draining a watershed that runs from the High Peaks plateau down to Lake Champlain via Plattsburgh. The stretch near Keene sees the river in its upper character: cold, fast-moving water over bedrock and cobble, fed by mountain runoff and beaver-dammed tributaries. It's a visual corridor more than a recreation draw in this section — the kind of water you cross on a bridge between trailheads and note the clarity. Downstream toward Saranac Lake village and Franklin Falls, the river opens up for paddling, fishing (brookies, browns, and rainbows depending on reach), and a network of put-ins that make it one of the more accessible cold-water rivers in the Park.
The Saranac River drains north out of the High Peaks through a long, winding corridor — the mainstem running from the outlet of the Saranac Lakes through Franklin County to the Saranac's confluence with Lake Champlain near Plattsburgh. The stretch through the town of Keene is the uppermost reach: fast, boulder-studded water dropping through narrow gorges and occasional flat pools, a north-flowing drainage that feels remote despite paralleling roads and settlement downstream. It's part of the larger Saranac watershed that once drove lumber and tannery economies across the northern Adirondacks — still paddled in spring by whitewater boaters familiar with the drops, still fished by locals who know which pools hold trout after runoff settles. Public access points are scattered and informal; look for pull-offs near bridge crossings.
The Saranac River threads through the Keene Valley corridor as one of the major drainage systems connecting the High Peaks interior to the broader Saranac Lakes watershed to the north — a fast-moving ribbon of whitewater in spring, cobblestone riffles and pocket pools by midsummer. It's one of those waters more often *crossed* than fished — NY-73 parallels sections of it, and half a dozen trail crossings link the valley's trailhead network — but the river holds brook trout in its upper reaches and sees occasional paddling traffic during the spring melt. Access is informal: bridge crossings, roadside pull-offs, and the occasional bushwhack down to the water. The river's gradient and character shift dramatically as it drops out of the mountains — check flow levels before committing to any paddle plan.
The Saranac River winds through the Keene valley floor — a broad, steady flow that runs parallel to NY-73 for much of its middle reach before turning north toward the village of Saranac Lake. It's a working river more than a destination: visible from the highway, crossed by bridges, flanked by private land and state easements in a patchwork that makes access opportunistic rather than planned. Paddlers who know the drainage use it as a connector between the three Saranac Lakes and Lower Saranac Lake, but the Keene stretch is mostly roadside — shallow riffles, gravel bars, and the occasional deep pool under a culvert. Fish populations aren't well-documented here, but the cold headwaters upstream suggest brook trout in the tributaries if not the main stem.
The South Fork Boquet River drains the high country south and west of Keene Valley — headwaters above the Johns Brook valley, gathering tributaries from the Giant Mountain Wilderness and the eastern High Peaks before converging with the North Fork near Keene hamlet. The upper stretches run steep and rocky through remote terrain; lower sections ease into farmland and forest as the valley opens toward I-87. This is brook trout water in the tributaries, with the main stem holding browns in the accessible lower miles. Access is scattered — old logging roads, state land crossings, and bridge pull-offs between Keene Valley and Keene proper.
